FN Thomson Reuters Web of Science™
VR 1.0
PT J
AU Irikura, KK
AF Irikura, Karl K.
TI Thermochemistry of Ammonium Nitrate, NH4NO3, in the Gas Phase
SO JOURNAL OF PHYSICAL CHEMISTRY A
LA English
DT Article
ID NITRIC-ACID; AB-INITIO; WAVE-FUNCTIONS; BASIS-SETS; HYDROGEN; CLUSTERS;
WATER; INVERSION; COMPLEX; TABLES
AB Hildenbrand and co-workers have shown recently that the vapor above solid ammonium nitrate includes molecules of NH4NO3, not only NH3 and HNO3 as previously believed. Their measurements led to thermochemical values that imply an enthalpy change of D-298 = 98 +/- 9 kJ mol(-1) for the gas-phase dissociation of ammonium nitrate into NH3 and HNO3. Using updated spectroscopic information for the partition function leads to the revised value of D-298 = 78 +/- 21 kJ mol(-1) (accompanying paper in this journal, Hildenbrand, D. L.; Lau, K. H.; Chandra, D. J. Phys. Chem. B 2010, DOI: 10.1021/jp105773q). In contrast, high-level ab initio calculations, detailed in the present report, predict a dissociation enthalpy half as large as the original result, 50 +/- 3 kJ mol(-1). These are frozen-core CCSD(T) calculations extrapolated to the limiting basis set aug-cc-pV infinity Z using an anharmonic vibrational partition function and a variational treatment of the NH3 rotor. The corresponding enthalpy of formation is Delta H-f(298)o(NH4NO3,g) = 230.6 +/- 3 kJ mol(-1). The origin of the disagreement with experiment remains unexplained.
C1 Natl Inst Stand & Technol, Chem & Biochem Reference Data Div, Gaithersburg, MD 20899 USA.
RP Irikura, KK (reprint author), Natl Inst Stand & Technol, Chem & Biochem Reference Data Div, Gaithersburg, MD 20899 USA.
RI Irikura, Karl/A-4266-2009
OI Irikura, Karl/0000-0001-7515-6761
NR 30
TC 4
Z9 4
U1 0
U2 11
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 1089-5639
J9 J PHYS CHEM A
JI J. Phys. Chem. A
PD NOV 4
PY 2010
VL 114
IS 43
BP 11651
EP 11653
DI 10.1021/jp105770d
PG 3
WC Chemistry, Physical; Physics, Atomic, Molecular & Chemical
SC Chemistry; Physics
GA 671AO
UT WOS:000283471900032
PM 20929227
ER
PT J
AU Olmschenk, S
Chicireanu, R
Nelson, KD
Porto, JV
AF Olmschenk, S.
Chicireanu, R.
Nelson, K. D.
Porto, J. V.
TI Randomized benchmarking of atomic qubits in an optical lattice
SO NEW JOURNAL OF PHYSICS
LA English
DT Article
AB We perform randomized benchmarking on neutral atomic quantum bits (qubits) confined in an optical lattice. Single-qubit gates are implemented using microwaves, resulting in a measured error per randomized computational gate of 1.4(1) x 10(-4) that is dominated by the system T(2) relaxation time. The results demonstrate the robustness of the system and its viability for more advanced quantum information protocols.
C1 [Olmschenk, S.] Natl Inst Stand & Technol, Joint Quantum Inst, Gaithersburg, MD 20899 USA.
Univ Maryland, Dept Phys, Gaithersburg, MD 20899 USA.
RP Olmschenk, S (reprint author), Natl Inst Stand & Technol, Joint Quantum Inst, Gaithersburg, MD 20899 USA.
EM steven.olmschenk@gmail.com
RI Olmschenk, Steven/D-4960-2011
OI Olmschenk, Steven/0000-0003-0105-7714
FU National Research Council (NRC); DARPA
FX We thank E Knill, C A Ryan and A Meier for useful discussions regarding
the randomized benchmarking procedure and E Knill, T M Hanna and A Meier
for comments on this paper. Specific product citations are for the
purpose of clarification only and are not an endorsement by the authors,
JQI or NIST. SO and KDN acknowledge support from the National Research
Council (NRC) Research Associateship program. This work was partially
supported by the DARPA QUEST program. This paper is a contribution of
NIST and is not subject to US copyright.
NR 25
TC 25
Z9 25
U1 0
U2 7
PU IOP PUBLISHING LTD
PI BRISTOL
PA DIRAC HOUSE, TEMPLE BACK, BRISTOL BS1 6BE, ENGLAND
SN 1367-2630
J9 NEW J PHYS
JI New J. Phys.
PD NOV 4
PY 2010
VL 12
AR 113007
DI 10.1088/1367-2630/12/11/113007
PG 10
WC Physics, Multidisciplinary
SC Physics
GA 687IP
UT WOS:000284772500002
ER
PT J
AU Dai, X
Bristow, AD
Karaiskaj, D
Cundiff, ST
AF Dai, X.
Bristow, A. D.
Karaiskaj, D.
Cundiff, S. T.
TI Two-dimensional Fourier-transform spectroscopy of potassium vapor
SO PHYSICAL REVIEW A
LA English
DT Article
ID OPTICALLY DENSE MEDIA; GAAS QUANTUM-WELLS; PHASE; ECHO; PROPAGATION;
RELAXATION; SPECTRUM; GASES
AB Optical two-dimensional Fourier-transform (2DFT)spectroscopy is used to study the coherent optical response of potassium vapor in a thin transmission cell. Rephasing and nonrephasing spectra of the D-1 and D-2 transitions are obtained and compared to numerical simulations. Non-perturbative calculations using the optical Bloch equations give very good agreement with the experimental peak strengths and line shapes. Nonradiative Raman-like coherences are isolated using a different 2DFT projection. Comparison between the optical and Raman linewidths shows that dephasing is due to partially correlated energy fluctuations. Density-dependent measurements show distortion of 2DFT spectra due to pulse propagation effects.
C1 [Dai, X.] Univ Colorado, JILA, Boulder, CO 80309 USA.
Natl Inst Stand & Technol, Boulder, CO 80309 USA.
RP Dai, X (reprint author), Univ Colorado, JILA, Boulder, CO 80309 USA.
EM cundiffs@jila.colorado.edu
RI Cundiff, Steven/B-4974-2009; Bristow, Alan/F-9703-2013; Dai,
Xingcan/B-3556-2014
OI Cundiff, Steven/0000-0002-7119-5197;
FU NIST; National Science Foundation's Physics Frontier Center
FX The authors thank T. Asnicar and H. Green for technical assistance. The
financial support is provided by NIST and the National Science
Foundation's Physics Frontier Center Program.
NR 44
TC 24
Z9 25
U1 0
U2 14
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 1050-2947
J9 PHYS REV A
JI Phys. Rev. A
PD NOV 3
PY 2010
VL 82
IS 5
AR 052503
DI 10.1103/PhysRevA.82.052503
PG 6
WC Optics; Physics, Atomic, Molecular & Chemical
SC Optics; Physics
GA 674SI
UT WOS:000283769700003
ER
PT J
AU Kumar, A
Perlwitz, J
Eischeid, J
Quan, XW
Xu, TY
Zhang, T
Hoerling, M
Jha, B
Wang, WQ
AF Kumar, Arun
Perlwitz, Judith
Eischeid, Jon
Quan, Xiaowei
Xu, Taiyi
Zhang, Tao
Hoerling, Martin
Jha, Bhaskar
Wang, Wanqui
TI Contribution of sea ice loss to Arctic amplification
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID ATMOSPHERIC RESPONSE; SURFACE-TEMPERATURE; CIRCULATION; ANOMALIES;
WINTER; MODEL; CCM3
AB Atmospheric climate models are subjected to the observed sea ice conditions during 2007 to estimate the regionality, seasonality, and vertical pattern of temperature responses to recent Arctic sea ice loss. It is shown that anomalous sea ice conditions accounted for virtually all of the estimated Arctic amplification in surface-based warming over the Arctic Ocean, and furthermore they accounted for a large fraction of Arctic amplification occurring over the high-latitude land between 60 degrees N and the Arctic Ocean. Sea ice loss did not appreciably contribute to observed 2007 land temperature warmth equatorward of 60 degrees N. Likewise, the observed warming of the free atmosphere attributable to sea ice loss is confined to Arctic latitudes, and is vertically confined to the lowest 1000 m. The results further highlight a strong seasonality of the temperature response to the 2007 sea ice loss. A weak signal of Arctic amplification in surface based warming is found during boreal summer, whereas a dramatically stronger signal is shown to develop during early autumn that persisted through December even as sea ice coverage approached its climatological values in response to the polar night. Citation: Kumar, A., J. Perlwitz, J. Eischeid, X. Quan, T. Xu, T. Zhang, M. Hoerling, B. Jha, and W. Wang ( 2010), Contribution of sea ice loss to Arctic amplification, Geophys. Res. Lett., 37, L21701, doi:10.1029/2010GL045022.
C1 [Kumar, Arun; Jha, Bhaskar] NOAA, NCEP, Camp Springs, MD 20746 USA.
[Perlwitz, Judith; Eischeid, Jon; Quan, Xiaowei; Xu, Taiyi; Zhang, Tao; Hoerling, Martin; Wang, Wanqui] NOAA, ESRL, Boulder, CO 80305 USA.
RP Kumar, A (reprint author), NOAA, NCEP, 5200 Auth Rd, Camp Springs, MD 20746 USA.
EM arun.kumar@noaa.gov
RI Perlwitz, Judith/B-7201-2008
OI Perlwitz, Judith/0000-0003-4061-2442
NR 22
TC 56
Z9 59
U1 3
U2 16
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
EI 1944-8007
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD NOV 3
PY 2010
VL 37
AR L21701
DI 10.1029/2010GL045022
PG 6
WC Geosciences, Multidisciplinary
SC Geology
GA 676TO
UT WOS:000283941700011
ER
PT J
AU Li, T
Kwon, M
Zhao, M
Kug, JS
Luo, JJ
Yu, WD
AF Li, Tim
Kwon, MinHo
Zhao, Ming
Kug, Jong-Seong
Luo, Jing-Jia
Yu, Weidong
TI Global warming shifts Pacific tropical cyclone location
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID WESTERN NORTH PACIFIC; CLIMATE-CHANGE; FREQUENCY; VARIABILITY;
INTENSITY; SIMULATION; ORIGIN; MODEL; WAVES; GCM
AB A global high-resolution (similar to 40 km) atmospheric general circulation model (ECHAM5 T319) is used to investigate the change of tropical cyclone frequency in the North Pacific under global warming. A time slice method is used in which sea surface temperature fields derived from a lower-resolution coupled model run under the 20C3M (in which historical greenhouse gases in 20th century were prescribed as a radiative forcing) and A1B (in which carbon dioxide concentration was increased 1% each year from 2000 to 2070 and then was kept constant) scenarios are specified as the lower boundary conditions to simulate the current and the future warming climate, respectively. A significant shift is found in the location of tropical cyclones from the western to central Pacific. The shift to more tropical cyclones in the central and less in the western Pacific is not attributable to a change in atmospheric static stability, but to a change in the variance of tropical synoptic-scale perturbations associated with a change in the background vertical wind shear and boundary layer divergence. Citation: Li, T., M. Kwon, M. Zhao, J.-S. Kug, J.-J. Luo, and W. Yu (2010), Global warming shifts Pacific tropical cyclone location, Geophys. Res. Lett., 37, L21804, doi:10.1029/2010GL045124.
C1 [Li, Tim; Kwon, MinHo] Univ Hawaii Manoa, Int Pacific Res Ctr, Honolulu, HI 96822 USA.
[Kug, Jong-Seong] Korea Ocean Res & Dev Inst, Ansan 426744, Gyeonggi, South Korea.
[Kwon, MinHo; Zhao, Ming] NOAA, GFDL, Princeton, NJ 08542 USA.
[Luo, Jing-Jia] JAMSTEC, Res Inst Climate Change, Kanazawa Ku, Kanagawa 2360001, Japan.
[Yu, Weidong] State Ocean Adm, Inst Oceanog 1, Qingdao 266061, Shandong, Peoples R China.
RP Li, T (reprint author), Univ Hawaii Manoa, Int Pacific Res Ctr, 1680 East West Rd, Honolulu, HI 96822 USA.
EM timli@hawaii.edu
RI Luo, Jing-Jia/B-2481-2008; KUG, JONG-SEONG/A-8053-2013; Zhao,
Ming/C-6928-2014;
OI Luo, Jing-Jia/0000-0003-2181-0638; Kwon, MinHo/0000-0002-5298-131X
FU ONR [N000140810256, N000141010774]; NRL [N00173-09-1-G008]; Japan Agency
for Marine-Earth Science and Technology (JAMSTEC); NASA [NNX07AG53G];
NOAA [NA17RJ1230]; KORDI [PE98537]
FX This work was supported by ONR grants N000140810256 and N000141010774
and NRL grant N00173-09-1-G008 and by the International Pacific Research
Center that is sponsored by the Japan Agency for Marine-Earth Science
and Technology (JAMSTEC), NASA (NNX07AG53G) and NOAA (NA17RJ1230). MK
was supported by KORDI grant PE98537. This is SOEST contribution 8016
and IPRC contribution 720.
NR 38
TC 38
Z9 39
U1 1
U2 13
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD NOV 3
PY 2010
VL 37
AR L21804
DI 10.1029/2010GL045124
PG 5
WC Geosciences, Multidisciplinary
SC Geology
GA 676TO
UT WOS:000283941700013
ER
PT J
AU Padman, L
Costa, DP
Bolmer, ST
Goebel, ME
Huckstadt, LA
Jenkins, A
McDonald, BI
Shoosmith, DR
AF Padman, Laurie
Costa, Daniel P.
Bolmer, S. Thompson
Goebel, Michael E.
Huckstadt, Luis A.
Jenkins, Adrian
McDonald, Birgitte I.
Shoosmith, Deborah R.
TI Seals map bathymetry of the Antarctic continental shelf
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID SOUTHERN ELEPHANT SEALS; FORAGING ECOLOGY; PENINSULA; OCEAN; WEST;
CIRCULATION; ENERGETICS; BEHAVIOR; LION
AB We demonstrate the first use of marine mammal dive-depth data to improve maps of bathymetry in poorly sampled regions of the continental shelf. A group of 57 instrumented elephant seals made on the order of 2 x 10(5) dives over and near the continental shelf on the western side of the Antarctic Peninsula during five seasons, 2005-2009. Maximum dive depth exceeded 2000 m. For dives made near existing ship tracks with measured water depths H<700 m, similar to 30% of dive depths were to the seabed, consistent with expected benthic foraging behavior. By identifying the deepest of multiple dives within small areas as a dive to the seabed, we have developed a map of seal-derived bathymetry. Our map fills in several regions for which trackline data are sparse, significantly improving delineation of troughs crossing the continental shelf of the southern Bellingshausen Sea. Citation: Padman, L., D. P. Costa, S. T. Bolmer, M. E. Goebel, L. A. Huckstadt, A. Jenkins, B. I. McDonald, and D. R. Shoosmith (2010), Seals map bathymetry of the Antarctic continental shelf, Geophys. Res. Lett., 37, L21601, doi:10.1029/2010GL044921.
C1 [Padman, Laurie] Earth & Space Res, Corvallis, OR 97333 USA.
[Costa, Daniel P.; Huckstadt, Luis A.] Univ Calif Santa Cruz, Santa Cruz, CA 95060 USA.
[Bolmer, S. Thompson] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.
[Goebel, Michael E.] NOAA, Antarctic Ecosyst Res Div, SWFSC, Natl Marine Fisheries Serv, La Jolla, CA 92037 USA.
[Jenkins, Adrian; Shoosmith, Deborah R.] British Antarctic Survey, Cambridge CB3 0ET, England.
[McDonald, Birgitte I.] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA.
RP Padman, L (reprint author), Earth & Space Res, 3350 SW Cascade Ave, Corvallis, OR 97333 USA.
EM padman@esr.org
RI Logger, Satellite/C-1379-2010
FU NASA [NNG05GR58G, NNX06AD40G, NNG06GA69G]; ONR [N00014-05-1-0645]; NSF
[OPP-0338101, ANT-0440687, ANT-0523332]; U.S.-AMLR
FX We thank David Sandwell for providing the high-resolution bathymetry
grid TOPO12.1; Yann Tremblay and Patrick Robinson for calibration and
preparation of the seal CTD tags; and Mike Dinniman for discussions on
the role of bathymetry in modeling performance. We appreciate the
detailed comments from two anonymous reviewers. This work was supported
by: NASA grants NNG05GR58G, NNX06AD40G and NNG06GA69G to LP; ONR grant
N00014-05-1-0645 to DPC; NSF grants OPP-0338101 to ESR, and ANT-0440687
and ANT-0523332 to DPC and MEG; and the U.S.-AMLR program. This is ESR
contribution 134.
NR 26
TC 18
Z9 18
U1 0
U2 13
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD NOV 3
PY 2010
VL 37
AR L21601
DI 10.1029/2010GL044921
PG 5
WC Geosciences, Multidisciplinary
SC Geology
GA 676TO
UT WOS:000283941700007
ER
PT J
AU Salawitch, RJ
Canty, T
Kurosu, T
Chance, K
Liang, Q
da Silva, A
Pawson, S
Nielsen, JE
Rodriguez, JM
Bhartia, PK
Liu, X
Huey, LG
Liao, J
Stickel, RE
Tanner, DJ
Dibb, JE
Simpson, WR
Donohoue, D
Weinheimer, A
Flocke, F
Knapp, D
Montzka, D
Neuman, JA
Nowak, JB
Ryerson, TB
Oltmans, S
Blake, DR
Atlas, EL
Kinnison, DE
Tilmes, S
Pan, LL
Hendrick, F
Van Roozendael, M
Kreher, K
Johnston, PV
Gao, RS
Johnson, B
Bui, TP
Chen, G
Pierce, RB
Crawford, JH
Jacob, DJ
AF Salawitch, R. J.
Canty, T.
Kurosu, T.
Chance, K.
Liang, Q.
da Silva, A.
Pawson, S.
Nielsen, J. E.
Rodriguez, J. M.
Bhartia, P. K.
Liu, X.
Huey, L. G.
Liao, J.
Stickel, R. E.
Tanner, D. J.
Dibb, J. E.
Simpson, W. R.
Donohoue, D.
Weinheimer, A.
Flocke, F.
Knapp, D.
Montzka, D.
Neuman, J. A.
Nowak, J. B.
Ryerson, T. B.
Oltmans, S.
Blake, D. R.
Atlas, E. L.
Kinnison, D. E.
Tilmes, S.
Pan, L. L.
Hendrick, F.
Van Roozendael, M.
Kreher, K.
Johnston, P. V.
Gao, R. S.
Johnson, B.
Bui, T. P.
Chen, G.
Pierce, R. B.
Crawford, J. H.
Jacob, D. J.
TI A new interpretation of total column BrO during Arctic spring
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID LOWER STRATOSPHERE; BROMINE MONOXIDE; TROPOSPHERIC BRO; OZONE DEPLETION;
POLAR SUNRISE; LAYER; GOME; CLIMATOLOGY; CHEMISTRY; CANADA
AB Emission of bromine from sea-salt aerosol, frost flowers, ice leads, and snow results in the nearly complete removal of surface ozone during Arctic spring. Regions of enhanced total column BrO observed by satellites have traditionally been associated with these emissions. However, airborne measurements of BrO and O-3 within the convective boundary layer (CBL) during the ARCTAS and ARCPAC field campaigns at times bear little relation to enhanced column BrO. We show that the locations of numerous satellite BrO "hotspots" during Arctic spring are consistent with observations of total column ozone and tropopause height, suggesting a stratospheric origin to these regions of elevated BrO. Tropospheric enhancements of BrO large enough to affect the column abundance are also observed, with important contributions originating from above the CBL. Closure of the budget for total column BrO, albeit with significant uncertainty, is achieved by summing observed tropospheric partial columns with calculated stratospheric partial columns provided that natural, short-lived biogenic bromocarbons supply between 5 and 10 ppt of bromine to the Arctic lowermost stratosphere. Proper understanding of bromine and its effects on atmospheric composition requires accurate treatment of geographic variations in column BrO originating from both the stratosphere and troposphere. Citation: Salawitch, R. J., et al. (2010), A new interpretation of total column BrO during Arctic spring, Geophys. Res. Lett., 37, L21805, doi:10.1029/2010GL043798.
C1 [Salawitch, R. J.; Canty, T.] Univ Maryland, Dept Atmospher & Ocean Sci, College Pk, MD 20742 USA.
[Salawitch, R. J.] Univ Maryland, Dept Chem & Biochem, College Pk, MD 20742 USA.
[Salawitch, R. J.] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20742 USA.
[Kurosu, T.; Chance, K.; Liu, X.] Harvard Smithsonian Ctr Astrophys, Cambridge, MA 02138 USA.
[Liang, Q.; Liu, X.] Univ Maryland Baltimore Cty, GEST, Greenbelt, MD 20771 USA.
[da Silva, A.; Pawson, S.; Rodriguez, J. M.; Bhartia, P. K.] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
[Nielsen, J. E.] Sci Syst & Applicat Inc, Lanham, MD 20706 USA.
[Huey, L. G.; Liao, J.; Stickel, R. E.; Tanner, D. J.] Georgia Inst Technol, Sch Earth & Atmospher Sci, Atlanta, GA 30332 USA.
[Dibb, J. E.] Univ New Hampshire, Complex Syst Res Ctr, Durham, NH 03824 USA.
[Simpson, W. R.; Donohoue, D.] Univ Alaska Fairbanks, Dept Chem & Biochem, Fairbanks, AK 99775 USA.
[Weinheimer, A.; Flocke, F.; Knapp, D.; Montzka, D.; Kinnison, D. E.; Tilmes, S.; Pan, L. L.] Natl Ctr Atmospher Res, Boulder, CO 80305 USA.
[Neuman, J. A.; Nowak, J. B.] Univ Colorado, CIRES, Boulder, CO 80309 USA.
[Neuman, J. A.; Nowak, J. B.; Ryerson, T. B.; Oltmans, S.; Gao, R. S.; Johnson, B.] NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA.
[Blake, D. R.] Univ Calif Irvine, Dept Chem, Irvine, CA 92697 USA.
[Atlas, E. L.] Univ Miami, RSMAS, Miami, FL 33149 USA.
[Hendrick, F.; Van Roozendael, M.] Belgian Inst Space Aeron, B-1180 Brussels, Belgium.
[Kreher, K.; Johnston, P. V.] NIWA Lauder, Omakau, New Zealand.
[Bui, T. P.] NASA, Ames Res Ctr, Moffett Field, CA 94035 USA.
[Chen, G.; Crawford, J. H.] NASA, Langley Res Ctr, Hampton, VA 23681 USA.
[Pierce, R. B.] NOAA, NESDIS, Madison, WI 53706 USA.
[Jacob, D. J.] Harvard Univ, Sch Engn & Appl Sci, Cambridge, MA 02138 USA.
RP Salawitch, RJ (reprint author), Univ Maryland, Dept Atmospher & Ocean Sci, 2403 Comp & Space Sci Bldg, College Pk, MD 20742 USA.
EM rjs@atmos.umd.edu
RI Liu, Xiong/P-7186-2014; Atlas, Elliot/J-8171-2015; Simpson,
William/I-2859-2014; Bhartia, Pawan/A-4209-2016; Pawson,
Steven/I-1865-2014; Manager, CSD Publications/B-2789-2015; Crawford,
James/L-6632-2013; Pan, Laura/A-9296-2008; Neuman, Andy/A-1393-2009;
Nowak, John/B-1085-2008; Liang, Qing/B-1276-2011; Canty,
Timothy/F-2631-2010; Salawitch, Ross/B-4605-2009; Pierce, Robert
Bradley/F-5609-2010; da Silva, Arlindo/D-6301-2012; Rodriguez,
Jose/G-3751-2013; Liao, Jin/H-4865-2013; Gao, Ru-Shan/H-7455-2013;
Ryerson, Tom/C-9611-2009
OI Liu, Xiong/0000-0003-2939-574X; Simpson, William/0000-0002-8596-7290;
Bhartia, Pawan/0000-0001-8307-9137; Pawson, Steven/0000-0003-0200-717X;
Chance, Kelly/0000-0002-7339-7577; Crawford, James/0000-0002-6982-0934;
Pan, Laura/0000-0001-7377-2114; Neuman, Andy/0000-0002-3986-1727; Nowak,
John/0000-0002-5697-9807; Canty, Timothy/0000-0003-0618-056X; Salawitch,
Ross/0000-0001-8597-5832; Pierce, Robert Bradley/0000-0002-2767-1643; da
Silva, Arlindo/0000-0002-3381-4030; Rodriguez, Jose/0000-0002-1902-4649;
FU ARCTAS; ACMAP; Aura; MAP; National Aeronautics and Space Administration;
ARCPAC National Oceanic and Atmospheric Administration; National Science
Foundation; PRODEX; EC [FP6-2005-Global-4-036677, 226224-FP7-ENV-2008-1]
FX Research of many of the investigators has been supported by the ARCTAS,
ACMAP, Aura, MAP, and Tropospheric Chemistry programs of the National
Aeronautics and Space Administration, the ARCPAC program of the National
Oceanic and Atmospheric Administration, and the START08 program of the
National Science Foundation. The ground-based BrO activities at the
Belgian Institute for Space Aeronomy (BIRA-IASB) are funded by the
PRODEX contract SECPEA and the EC projects GEOmon
(FP6-2005-Global-4-036677) and SHIVA (226224-FP7-ENV-2008-1); BIRA-IASB
thanks M. P. Chipperfield for providing SLIMCAT output used in the
retrieval. We thank the pilots, flight crews, and OMI scientific
leadership and data processing teams for their wonderful efforts. We
appreciate the three extensive and careful reviews that led to a much
improved manuscript.
NR 29
TC 54
Z9 54
U1 4
U2 38
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
EI 1944-8007
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD NOV 3
PY 2010
VL 37
AR L21805
DI 10.1029/2010GL043798
PG 9
WC Geosciences, Multidisciplinary
SC Geology
GA 676TO
UT WOS:000283941700001
ER
PT J
AU Kline, MC
Duewer, DL
Butler, JM
AF Kline, M. C.
Duewer, D. L.
Butler, J. M.
TI Characterizing the Electrophoretic Mobility of Huntington Disease
Alleles 13 77 Are the Deviations from the Theoretical Values Intrinsic
or Internal Sizing Standard Artifacts?
SO JOURNAL OF MOLECULAR DIAGNOSTICS
LA English
DT Meeting Abstract
CT Annual Meeting of the Association-for-Molecular-Pathology
CY NOV 18-20, 2010
CL San Jose, CA
SP Assoc Mol Pathol
C1 [Kline, M. C.; Duewer, D. L.; Butler, J. M.] Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
NR 0
TC 0
Z9 0
U1 0
U2 0
PU AMER SOC INVESTIGATIVE PATHOLOGY, INC
PI BETHESDA
PA 9650 ROCKVILLE PIKE, BETHESDA, MD 20814-3993 USA
SN 1525-1578
J9 J MOL DIAGN
JI J. Mol. Diagn.
PD NOV
PY 2010
VL 12
IS 6
BP 858
EP 859
PG 2
WC Pathology
SC Pathology
GA 677FE
UT WOS:000283973700025
ER
PT J
AU Chan, J
Kidd, D
Burke, B
Harriott, L
Williams, K
AF Chan, Jack
Kidd, Deborah
Burke, Brian
Harriott, Lloyd
Williams, Keith
TI Noise analysis of carbon nanotube field effect transistors irradiated by
electron beam
SO JOURNAL OF VACUUM SCIENCE & TECHNOLOGY B
LA English
DT Article
ID 1/F NOISE
AB Using current noise measurement techniques, the authors have studied the effects of electron beam exposure on field effect transistors based on carbon nanotube channels. In the case of p-type semiconducting nanotubes, the authors find that high doses induce a potential barrier along the channel, and transport is dominated by the tunneling events across this barrier. The authors suggest that the barrier is induced by charges trapped in the underlying SiO(2) barrier. Complementary studies on metallic nanotubes do not exhibit this behavior. (C) 2010 American Vacuum Society. [DOI: 10.1116/1.3517517]
C1 [Chan, Jack; Williams, Keith] Univ Virginia, Dept Phys, Charlottesville, VA 22904 USA.
[Kidd, Deborah; Harriott, Lloyd] Univ Virginia, Dept Elect & Comp Engn, Charlottesville, VA 22904 USA.
[Burke, Brian] NIST, Funct Properties Grp, Gaithersburg, MD 20899 USA.
RP Chan, J (reprint author), Univ Virginia, Dept Phys, Charlottesville, VA 22904 USA.
EM lrharriott@virginia.edu
NR 11
TC 1
Z9 1
U1 0
U2 3
PU A V S AMER INST PHYSICS
PI MELVILLE
PA STE 1 NO 1, 2 HUNTINGTON QUADRANGLE, MELVILLE, NY 11747-4502 USA
SN 1071-1023
J9 J VAC SCI TECHNOL B
JI J. Vac. Sci. Technol. B
PD NOV
PY 2010
VL 28
IS 6
BP C6P66
EP C6P69
DI 10.1116/1.3517517
PG 4
WC Engineering, Electrical & Electronic; Nanoscience & Nanotechnology;
Physics, Applied
SC Engineering; Science & Technology - Other Topics; Physics
GA 690OX
UT WOS:000285015200116
ER
PT J
AU Cannara, RJ
Sebastian, A
Gotsmann, B
Rothuizen, H
AF Cannara, Rachel J.
Sebastian, Abu
Gotsmann, Bernd
Rothuizen, Hugo
TI Scanning Thermal Microscopy for Fast Multiscale Imaging and Manipulation
SO IEEE TRANSACTIONS ON NANOTECHNOLOGY
LA English
DT Article
DE Metrology; microfabricated probes; multiscale imaging; nanomanipulation;
noncontact imaging; thermal sensing
ID FORCE MICROSCOPE; LITHOGRAPHY; PROBE; SILICON; DESIGN; WEAR;
NANOLITHOGRAPHY; NANOSCALE; STORAGE; TIP
AB Multiscale resolution imaging and manipulation are essential for applications ranging from defect screening in circuits to nanoscale manipulation, patterning, and lithography. In this paper, we introduce a variant of scanning thermal microscopy to image surfaces at both the micro-and nanoscale. Electrothermal imaging at the microscale is performed in a completely out-of-contact, i.e., "noncontact" or "off-contact," mode with a microscale heater, followed by higher resolution nanoscale imaging in contact mode with a nanoscale probe tip. Using this methodology, the imaging and manipulation functions of a single probe can be decoupled completely. This off-contact imaging mode is useful for avoiding tip wear and can be performed safely at high velocities. We demonstrate imaging of microscale features at speeds of up to 2 mm/s. The lateral resolution is determined by the dimensions of the heater used for imaging. For the flying heights and heater dimensions used here, the 1-sigma lateral spatial resolution limit in the off-contact mode is less than 10 mu m for 10-nm-tall features. A silicon nanowire attached to microscale electrodes is imaged to demonstrate the efficacy of this scheme.
C1 [Cannara, Rachel J.; Sebastian, Abu; Gotsmann, Bernd; Rothuizen, Hugo] IBM Corp, Zurich Res Lab, CH-8803 Ruschlikon, Switzerland.
RP Cannara, RJ (reprint author), NIST, Ctr Nanoscale Sci Technol, Gaithersburg, MD 20899 USA.
EM rachel.cannara@nist.gov; ase@zurich.ibm.com
RI Cannara, Rachel/C-9128-2013
OI Cannara, Rachel/0000-0002-2984-5475
NR 34
TC 5
Z9 5
U1 0
U2 6
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 1536-125X
J9 IEEE T NANOTECHNOL
JI IEEE Trans. Nanotechnol.
PD NOV
PY 2010
VL 9
IS 6
BP 745
EP 753
DI 10.1109/TNANO.2010.2045232
PG 9
WC Engineering, Electrical & Electronic; Nanoscience & Nanotechnology;
Materials Science, Multidisciplinary; Physics, Applied
SC Engineering; Science & Technology - Other Topics; Materials Science;
Physics
GA 678PJ
UT WOS:000284091300015
ER
PT J
AU Lovas, FJ
Plusquellic, DF
Weaver, SLW
McGuire, BA
Blake, GA
AF Lovas, F. J.
Plusquellic, D. F.
Weaver, S. L. Widicus
McGuire, B. A.
Blake, G. A.
TI Organic compounds in the C3H6O3 family Microwave spectrum of cis-cis
dimethyl carbonate
SO JOURNAL OF MOLECULAR SPECTROSCOPY
LA English
DT Article
DE Ab initio calculation; Dipole moment; Dimethyl carbonate; Microwave
spectrum; Rotational spectrum; Structure
ID GAUSSIAN-BASIS SETS; CORRELATED MOLECULAR CALCULATIONS; ROTATIONAL
SPECTRUM; ETHYLENE-GLYCOL; BEAM; SPECTROMETER; 1,3-DIHYDROXYACETONE;
MILLIMETER; ATOMS; CONFIRMATION
AB Geometry optimization calculations on 13 members of the C3H6O3 family of organic species have been carried out to determine their relative binding energies Dimethyl carbonate RCH3)(2)CO3] is one of the lower energy species in this family which Includes the C-3-sugars 1 3-dihydroxyacetone and glyceralde hyde The microwave spectrum of dimethyl carbonate has been measured over the frequency range 8 4-25 3 GHz with several pulsed-beam Fourier-transform microwave spectrometers and from 227 GHz to 350 GHz with direct absorption spectrometers The spectrum of the lowest-energy cis-cis conformer of dimethyl carbonate has been assigned and ab initio electronic structure calculations of the three possible conformers have been performed Stark effect measurements were carried out on the cis-cis conformer to provide accurate determinations of the dipole moment components (C) 2010 Elsevier Inc All rights reserved
C1 [Lovas, F. J.; Plusquellic, D. F.] NIST, Opt Technol Div, Gaithersburg, MD 20899 USA.
[Weaver, S. L. Widicus; McGuire, B. A.] Emory Univ, Dept Chem, Atlanta, GA 30322 USA.
[Blake, G. A.] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA.
RP Lovas, FJ (reprint author), NIST, Opt Technol Div, Gaithersburg, MD 20899 USA.
FU NSF Centers for Chemical Innovation [0847919]; NASA [NAG5-11423,
NAG5-13457]; Emory University
FX The authors gratefully acknowledge P Groner for the use of his Erham
program and some advice on its use S LW W and B A M thank M Heaven for
his input on the electronic structure calculations This work was
supported in part by NSF Centers for Chemical Innovation through grant
0847919 The Caltech experimental work and the original computational
work were funded in part by the NASA Exobiology and SARA programs Grant
Nos NAG5-11423 and NAG5-13457 The additional computational work was
supported by SLWW s startup funds provided by Emory University
NR 37
TC 5
Z9 5
U1 1
U2 11
PU ACADEMIC PRESS INC ELSEVIER SCIENCE
PI SAN DIEGO
PA 525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA
SN 0022-2852
J9 J MOL SPECTROSC
JI J. Mol. Spectrosc.
PD NOV
PY 2010
VL 264
IS 1
BP 10
EP 18
DI 10.1016/jjms.2010.08.006
PG 9
WC Physics, Atomic, Molecular & Chemical; Spectroscopy
SC Physics; Spectroscopy
GA 679SS
UT WOS:000284181700002
ER
PT J
AU Maki, A
Weber, A
Nibler, JW
Masiello, T
Blake, TA
Kirkpatrick, R
AF Maki, Arthur
Weber, Alfons
Nibler, Joseph W.
Masiello, Tony
Blake, Thomas A.
Kirkpatrick, Robynne
TI High resolution infrared spectroscopy of [111]propellane The region of
the v(9) band
SO JOURNAL OF MOLECULAR SPECTROSCOPY
LA English
DT Article
DE Propellane; High resolution infrared spectrum; Rovibrational constants;
Ab initio DFT study; Anharmonic frequencies
ID MOLECULAR-STRUCTURE; VIBRATIONAL-SPECTRUM; ELECTRON-DIFFRACTION;
BICYCLO<1.1.1>PENTANE
AB The region of the Infrared active band of the v(9) CH2 bending mode [1 1 1]propellane has been recorded at a resolution (0 0025 cm(-1)) sufficient to distinguish individual rovibrational lines This region includes the partially overlapping bands v(9) (e')= 1459 cm(-1) 2v(18) (l = 2 E)= 1430 cm(-1) v(6) + v(12) (E')= 1489 cm(-1) and v(4) + v(15) (A(2))= 1518 cm(-1) In addition the difference band v(4) -v(15) (A(2)') was observed in the far Infrared near 295 cm(-1) and analyzed to give good constants for the upper v(4) levels The close proximities of the four bands in the v(9) region suggest that Coriolis and Fermi resonance couplings could be significant and theoretical band parameters obtained from Gaussian ab initio calculations were helpful in guiding the band analyses The analyses of all four bands were accomplished based on our earlier report of ground state constants determined from combination differences involving more than 4000 pairs of transitions from five fundamental and four combination bands This paper presents the analyses and the determination of the upper state constants of all four bands in the region of the v(9) band Complications were most evident in the 2v(18) (l = 2 E) band which showed significant perturbations due to mixing with the nearby 2v(18) (l = 0 A(1)) and v(4) + v(12) (E') levels which are either infrared inactive as transitions from the ground state or in the latter case too weak to observe These complications are discussed and a comparison of all molecular constants with those available from the ab mina calculations at the anharmonic level is presented (C) 2010 Elsevier Inc All rights reserved
C1 [Nibler, Joseph W.; Kirkpatrick, Robynne] Oregon State Univ, Dept Chem, Corvallis, OR 97332 USA.
[Weber, Alfons] NIST, Opt Technol Div, Gaithersburg, MD 20899 USA.
[Masiello, Tony] Calif State Univ Hayward, Dept Chem & Biochem, Hayward, CA 94542 USA.
[Blake, Thomas A.] Pacific NW Natl Lab, Richland, WA 99352 USA.
RP Nibler, JW (reprint author), Oregon State Univ, Dept Chem, Corvallis, OR 97332 USA.
FU Department of Energy 's Office of Biological and Environmental Research;
Oregon State University
FX The research described here was performed in part in the Environmental
Molecular Sciences Laboratory a national scientific user facility
sponsored by the Department of Energy 's Office of Biological and
Environmental Research and located at Pacific Northwest National
Laboratory We thank Robert Sams for helpful advice and assistance in
recording the infrared spectra of propellane in this facility and Dr Tim
Hubler also at PNNL for his advice on synthesis techniques J Nibler
acknowledges a Camille and Henry Dreyfus Senior Scientist Mentor Award
which was used in part to support undergraduates N Jariyasopit M Martin
and A Perry for this and other studies of propellane [1 2] and
bicyclopentane[18] R Kirkpatrick is grateful for Shoemaker and Harris
Fellowships at Oregon State University
NR 20
TC 6
Z9 6
U1 2
U2 6
PU ACADEMIC PRESS INC ELSEVIER SCIENCE
PI SAN DIEGO
PA 525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA
SN 0022-2852
J9 J MOL SPECTROSC
JI J. Mol. Spectrosc.
PD NOV
PY 2010
VL 264
IS 1
BP 26
EP 36
DI 10.1016/j.jms.2010.08.008
PG 11
WC Physics, Atomic, Molecular & Chemical; Spectroscopy
SC Physics; Spectroscopy
GA 679SS
UT WOS:000284181700004
ER
PT J
AU Wang, LZ
Dols, WS
Chen, QY
AF Wang, Liangzhu (Leon)
Dols, W. Stuart
Chen, Qingyan
TI Using CFD Capabilities of CONTAM 3.0 for Simulating Airflow and
Contaminant Transport in and around Buildings
SO HVAC&R RESEARCH
LA English
DT Article
ID COMPUTATIONAL FLUID-DYNAMICS; MULTIZONE; MODELS
AB CONTAM is a multizone building airflow and contaminant transport computer program often used for ventilation and indoor air quality analysis. The program was recently enhanced to incorporate CFD capabilities for both outdoor and indoor environmental analysis. This paper introduces the CFD features implemented within the most recent version, CONTAM 3.0. The outdoor or external CFD link predicts wind pressure coefficients and contaminant concentrations for airflow paths at the building surface. A converter computer program translates the wind pressure coefficients to the CONTAM data format. This external CFD link is useful for parametric studies of the impact of outdoor air quality on indoor environment when considering different wind directions or contaminant locations, especially simulations under transient conditions. The ability to embed a single CFD zone in a CONTAM network model has also been implemented. This enables the detailed modeling of a zone when the well-mixed multizone assumption is not appropriate and then uses the multizone approach for the rest of a building, thus capturing the local distribution of air and contaminant properties in a zone and their impacts on other zones of a building. CFD capabilities are demonstrated using a generic residential house model to show how these two new CFD features enhance the existing CONTAM capabilities for both indoor and outdoor air quality analysis.
C1 [Wang, Liangzhu (Leon)] Concordia Univ, Dept Bldg Civil & Environm Engn, Montreal, PQ, Canada.
[Dols, W. Stuart] Natl Inst Stand & Technol, Bldg & Fire Res Lab, Indoor Air Qual & Ventilat Grp, Gaithersburg, MD 20899 USA.
[Chen, Qingyan] Purdue Univ, Sch Mech Engn, W Lafayette, IN 47907 USA.
RP Wang, LZ (reprint author), Concordia Univ, Dept Bldg Civil & Environm Engn, Montreal, PQ, Canada.
NR 32
TC 20
Z9 22
U1 2
U2 15
PU AMER SOC HEATING REFRIGERATING AIR-CONDITIONING ENG, INC,
PI ATLANTA
PA 1791 TULLIE CIRCLE NE, ATLANTA, GA 30329 USA
SN 1078-9669
J9 HVAC&R RES
JI HVAC&R Res.
PD NOV
PY 2010
VL 16
IS 6
BP 749
EP 763
DI 10.1080/10789669.2010.10390932
PG 15
WC Thermodynamics; Construction & Building Technology; Engineering,
Mechanical
SC Thermodynamics; Construction & Building Technology; Engineering
GA 675KG
UT WOS:000283828900003
ER
PT J
AU Toman, B
Possolo, A
AF Toman, Blaza
Possolo, Antonio
TI Laboratory effects models for interlaboratory comparisons (vol 14, pg
553, 2009)
SO ACCREDITATION AND QUALITY ASSURANCE
LA English
DT Correction
C1 [Toman, Blaza; Possolo, Antonio] NIST, Stat Engn Div, Informat Technol Lab, US Dept Commerce, Gaithersburg, MD 20899 USA.
RP Toman, B (reprint author), NIST, Stat Engn Div, Informat Technol Lab, US Dept Commerce, Gaithersburg, MD 20899 USA.
EM blaza.toman@nist.gov
NR 1
TC 6
Z9 6
U1 0
U2 2
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0949-1775
J9 ACCREDIT QUAL ASSUR
JI Accredit. Qual. Assur.
PD NOV
PY 2010
VL 15
IS 11
BP 653
EP 654
DI 10.1007/s00769-010-0707-4
PG 2
WC Chemistry, Analytical; Instruments & Instrumentation
SC Chemistry; Instruments & Instrumentation
GA 680NW
UT WOS:000284242700009
ER
PT J
AU Kelly, JY
Albert, JNL
Howarter, JA
Kang, SH
Stafford, CM
Epps, TH
Fasolka, MJ
AF Kelly, Jennifer Y.
Albert, Julie N. L.
Howarter, John A.
Kang, Shuhui
Stafford, Christoplher M.
Epps, Thomas H., III
Fasolka, Michael J.
TI Investigation of Thermally Responsive Block Copolymer Thin Film
Morphologies Using Gradients
SO ACS APPLIED MATERIALS & INTERFACES
LA English
DT Article
DE block copolymer; thermal deprotection; surface energetics; surface
chemistry; gradient; morphology; thin film; film thickness
ID PHASE-BEHAVIOR; TEMPERATURE; TRANSITION; TEMPLATES; CYLINDER; KINETICS;
ARRAYS; ROUTE
AB We report the use of a gradient library approach to characterize the structure and behavior of thin films of a thermally responsive block copolymer (BCP) poly(styrene b-tert-butyl acrylate) (PS-b-PtBA) which exhibits chemical deprotection and morphological changes above a thermal threshold. Continuous gradients in temperature and film thickness, as well as discrete susbstrate chemistry conditions, were used to exam the trends in deprotection nanoscale morphology and chemical structure. Thermal gradient annealing permitted the extraction of transformation rate constants (k(i)) for the completion of thermal deprotection and rearrangement of the film morphology from a single BCP library on hydroxyl and alkyl surfaces, respectively. The transformation rate constants ranged from 1.45 x 10(-4) s(-1) to 5.02 x 10(-5) s(-1) for temperatures between 185 and 140 degrees C for hydroxyl surfaces. For the same temperature range, the alkly surfaces yielded k(i) values ranging from 4.76 x 10(-5) s(-1) to 5.73 x 10(-6) s(-1), an order of magnitude slower compared to hydroxyl surfaces. Activation energies of the thermal deprotection and film transformation on these surfaces were also extrapolated from linear fits to Arrhenius behavior. Moreover, we noted a morphology shift and orientation transformation from parallel lamellae to perpendicular cylinders at the free surface because of changes in volume fraction and surface energetics of the initially symmetric BCP. Using gradient techniques we are able to correlate morphological and chemical structure changes in a rapid fashion, determine kinetics of transitions and demonstrate the effect of surface chemistry on the deprotection reaction in thermally responsive BCP thin films,
C1 [Albert, Julie N. L.; Epps, Thomas H., III] Univ Delaware, Dept Chem Engn, Newark, DE 19716 USA.
[Kelly, Jennifer Y.; Howarter, John A.; Kang, Shuhui; Stafford, Christoplher M.; Fasolka, Michael J.] Natl Inst Stand & Technol, Div Polymers, Gaithersburg, MD 20899 USA.
RP Epps, TH (reprint author), Univ Delaware, Dept Chem Engn, Newark, DE 19716 USA.
EM thepps@udel.edu; michael.fasolka@nist.gov
RI Epps, Thomas/B-7337-2012
FU NIST [70NANB9H8150]; NSF [0645586]; NIST/NRC
FX This work was funded by NIST MSEL 70NANB9H8150 and NSF DMR CAREER -
0645586. J.Y.K. was supported by a NIST/NRC ARRA Postdoctoral Fellowship
Program. J.N.L.A. was supported by a NSF Graduate Research Fellowship.
J.A.H. was supported by the NIST/NRC Postdoctoral Fellowship Program.
The authors thank Dr. T. Beebe, Jr., Department of Chemistry, University
of Delaware, for use of his contact angle measuring system. This work is
an official contribution of the National Institute of Standards and
Technology.
NR 37
TC 18
Z9 18
U1 3
U2 32
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 1944-8244
J9 ACS APPL MATER INTER
JI ACS Appl. Mater. Interfaces
PD NOV
PY 2010
VL 2
IS 11
BP 3241
EP 3248
DI 10.1021/am100695m
PG 8
WC Nanoscience & Nanotechnology; Materials Science, Multidisciplinary
SC Science & Technology - Other Topics; Materials Science
GA 683EL
UT WOS:000284454400039
PM 20961126
ER
PT J
AU Pease, LF
Feldblyum, JI
Lacaerda, SHD
Liu, YL
Walker, ARH
Anumolu, R
Yim, PB
Clarke, ML
Kang, HG
Hwang, J
AF Pease, Leonard F., III
Feldblyum, Jeremy I.
Lacaerda, Silvia H. DePaoli
Liu, Yonglin
Walker, Angela R. Hight
Anumolu, Rajasekhar
Yim, Peter B.
Clarke, Matthew L.
Kang, Hyeong Gon
Hwang, Jeeseong
TI Structural Analysis of Soft Multicomponent Nanoparticle Clusters
SO ACS NANO
LA English
DT Article
DE composite nanoparticles; electrospray differential mobility analysis;
quantum dot; virus; phage; streptavidin
ID DIFFERENTIAL MOBILITY ANALYSIS; NONCOVALENT PROTEIN COMPLEXES; QUANTUM
DOTS; SURFACE COVERAGE; PARTICLES; SIZE; NANOTECHNOLOGY; SPECTROMETRY;
VIRUSES; CORONA
AB Quantitative techniques are essential to analyze the structure of soft multicomponent nanobioclusters Here, we combine electrospray differential mobility analysis (ES DMA), which rapidly measures the size of the entire duster, with transmission electron microscopy (TEM), which detects the hard components to determine the presence and composition of the soft components Coupling analysis of TEM and ES-DMA derived I data requires the creation and use of analytical models to determine the size and number Of constituents In nanoparticle complexes from the difference between the two measurements Previous ES DMA analyses have been limited to dusters of identical spherical particles-Here, we,dramatically extend the ES DMA analysis framework to accommodate more challenging geometries, including protein corona coated nanorods, clusters, composed of heterogeneously sized nanospheres, and nanobioclusters composed of both nanospheres and The latter is critical to determining the number of quantum dot's attached to lambda (lambda) phage a key element of a rapid method to detect bacterial pathogens in environmental and clinical samples
C1 [Pease, Leonard F., III; Anumolu, Rajasekhar] Univ Utah, Dept Chem Engn, Salt Lake City, UT 84112 USA.
[Pease, Leonard F., III; Feldblyum, Jeremy I.; Lacaerda, Silvia H. DePaoli; Liu, Yonglin; Walker, Angela R. Hight; Yim, Peter B.; Clarke, Matthew L.; Kang, Hyeong Gon; Hwang, Jeeseong] NIST, Gaithersburg, MD 20899 USA.
[Pease, Leonard F., III] Univ Utah, Dept Pharmaceut & Pharmaceut Chem, Salt Lake City, UT 84112 USA.
[Feldblyum, Jeremy I.] Univ Maryland, Dept Chem, College Pk, MD 20742 USA.
RP Pease, LF (reprint author), Univ Utah, Dept Chem Engn, Salt Lake City, UT 84112 USA.
RI Feldblyum, Jeremy/B-9600-2009; Hight Walker, Angela/C-3373-2009
OI Feldblyum, Jeremy/0000-0001-6667-9587; Hight Walker,
Angela/0000-0003-1385-0672
FU NSF
FX The authors would like to express sincere appreciation to Suvajyoti Guha
for his assistance with exploratory ES DMA experiments (not included)
and Richard E Cavic chi for thoughtful discussions The authors also
express appreciation to Michael R Zachariah of the University of
Maryland and Michael J Tarlov for use of their equipment facilities know
how and shared wisdom The authors also acknowledge the Mary land Nano
Center and its NispLab which is partially supported by NSF as a MRSEC
Shared Experimental Facility Reference to commercial equipment supplies
or software neither implies its endorsement by the National Institute of
Standards and Technology (NIST) nor implies it to be necessarily the
best suited for this purpose
NR 44
TC 13
Z9 13
U1 1
U2 38
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 1936-0851
J9 ACS NANO
JI ACS Nano
PD NOV
PY 2010
VL 4
IS 11
BP 6982
EP 6988
DI 10.1021/nn102106f
PG 7
WC Chemistry, Multidisciplinary; Chemistry, Physical; Nanoscience &
Nanotechnology; Materials Science, Multidisciplinary
SC Chemistry; Science & Technology - Other Topics; Materials Science
GA 682YD
UT WOS:000284438000077
PM 21049904
ER
PT J
AU Cho, TJ
Hackley, VA
AF Cho, Tae Joon
Hackley, Vincent A.
TI Fractionation and characterization of gold nanoparticles in aqueous
solution: asymmetric-flow field flow fractionation with MALS, DLS, and
UV-Vis detection
SO ANALYTICAL AND BIOANALYTICAL CHEMISTRY
LA English
DT Article
DE Field flow fractionation; Gold nanoparticle; Fractionation; Size
characterization; Light scattering; Particle characterization
ID SURFACE-PLASMON RESONANCE; CARBON NANOTUBES; LIGHT-SCATTERING;
BACTERIAL-CELLS; COLLOIDAL GOLD; CANCER; SIZE; DNA; PROTEINS; NANORODS
AB Asymmetrical-flow field flow fractionation (AFFF) separates constituents based on hydrodynamic size and is emerging as a powerful tool for obtaining high-resolution information on the size, molecular weight, composition, and stability of nanoscale particles in liquid media. We employ a customized AFFF system combining on-line detectors for multi-angle light scattering, dynamic light scattering, and UV-Vis absorption. Our objective is to develop optimized measurement protocols for the characterization of gold nanoparticles (GNPs), which are widely utilized in biomedical research and other nanotechnology applications. Experimental conditions have been optimized by controlling key parameters, including injection volume and solids concentration, mobile phase composition, membrane type and pore size, and ratio of channel-to-cross-flow rates. Individual citrate-stabilized GNP components (nominally 10, 20, 30, 40, and 60 nm) and GNPs functionalized with polyethylene glycol were separated from multicomponent GNP mixtures by AFFF and subsequently characterized. We discuss the effects due to variations in measurement parameters and GNP surface modification on observed retention, recovery, and peak resolution.
C1 [Cho, Tae Joon; Hackley, Vincent A.] NIST, Mat Sci & Engn Lab, Gaithersburg, MD 20899 USA.
RP Hackley, VA (reprint author), NIST, Mat Sci & Engn Lab, 100 Bur Dr,Stop 8520, Gaithersburg, MD 20899 USA.
EM vince.hackley@nist.gov
OI Hackley, Vincent/0000-0003-4166-2724
NR 58
TC 38
Z9 38
U1 5
U2 63
PU SPRINGER HEIDELBERG
PI HEIDELBERG
PA TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY
SN 1618-2642
J9 ANAL BIOANAL CHEM
JI Anal. Bioanal. Chem.
PD NOV
PY 2010
VL 398
IS 5
BP 2003
EP 2018
DI 10.1007/s00216-010-4133-6
PG 16
WC Biochemical Research Methods; Chemistry, Analytical
SC Biochemistry & Molecular Biology; Chemistry
GA 668BV
UT WOS:000283244500022
PM 20803340
ER
PT J
AU Yack, TM
Barlow, J
Roch, MA
Klinck, H
Martin, S
Mellinger, DK
Gillespie, D
AF Yack, Tina M.
Barlow, Jay
Roch, Marie A.
Klinck, Holger
Martin, Steve
Mellinger, David K.
Gillespie, Douglas
TI Comparison of beaked whale detection algorithms
SO APPLIED ACOUSTICS
LA English
DT Article; Proceedings Paper
CT 4th International Workshop on Detection, Classification and Localization
of Marine Mammals using Passive Acoustics/1st International Workshop on
Density Estimation of Marine Mammals Using Passive Acoustics
CY SEP 10-13, 2009
CL Univ Pavia, Collegio Cairoli, ITALY
HO Univ Pavia
DE Beaked whale; Detection; Classification; Towed-array; Passive acoustic
monitoring; Echolocationl
ID MESOPLODON-DENSIROSTRIS
AB Due to recent advances in passive acoustic monitoring techniques, beaked whales are now more effectively detected acoustically than visually during vessel-based (e.g. line-transect) surveys. Beaked whales signals can be discriminated from those of other cetaceans by the unique characteristics of their echolocation clicks (e.g. duration >175 mu s, center frequencies between 30 and 40 kHz, inter-click intervals between 0.2 and 0.4 s and frequency upsweeps). Furthermore, these same characteristics make these signals ideal candidates for testing automated detection and classification algorithms. There are several different beaked whale automated detectors currently available for use. However, no comparative analysis of detectors exists. Therefore, comparison between studies and datasets is difficult. The purpose of this study was to test, validate, and compare algorithms for detection of beaked whales in acoustic line-transect survey data. Six different detection algorithms (XBAT, Ishmael, PAMGUARD, ERMA, GMM and FMCD) were evaluated and compared. Detection trials were run on three sample days of towed-hydrophone array recordings collected by NOAA Southwest Fisheries Science Center (SWFSC) during which were confirmed visual sightings of beaked whales (Ziphius cavirostris and Mesoplodon peruvianus). Detections also were compared to human verified acoustic detections for a subset of these data. In order to measure the probabilities of false detection, each detector was also run on three sample recordings containing clicks from another species: Risso's dolphin (Grampus griseus). Qualitative and quantitative comparisons and the detection performance of the different algorithms are discussed. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Yack, Tina M.; Barlow, Jay] Natl Marine Fisheries Serv, SW Fisheries Sci Ctr, La Jolla, CA 92037 USA.
[Yack, Tina M.] San Diego State Univ, Joint Doctoral Program Ecol, San Diego, CA 92182 USA.
[Yack, Tina M.] UC Davis, San Diego, CA 92182 USA.
[Yack, Tina M.] Biowaves Inc, Encinitas, CA 92024 USA.
[Roch, Marie A.] San Diego State Univ, Dept Comp Sci, San Diego, CA 92182 USA.
[Klinck, Holger; Mellinger, David K.] Oregon State Univ, NOAA, Cooperat Inst Marine Resource Studies, Pacific Marine Environm Lab, Newport, OR 97365 USA.
[Martin, Steve] SPAWAR Syst Ctr San Pacific Code 71510, San Diego, CA 92152 USA.
[Gillespie, Douglas] Univ St Andrews, Scottish Oceans Inst, Sea Mammal Res Unit, St Andrews KY16 8LB, Fife, Scotland.
RP Yack, TM (reprint author), Natl Marine Fisheries Serv, SW Fisheries Sci Ctr, 3333 N Torrey Pines Court, La Jolla, CA 92037 USA.
EM tina.yack@noaa.gov
NR 9
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U1 2
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PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0003-682X
J9 APPL ACOUST
JI Appl. Acoust.
PD NOV
PY 2010
VL 71
IS 11
SI SI
BP 1043
EP 1049
DI 10.1016/j.apacoust.2010.04.010
PG 7
WC Acoustics
SC Acoustics
GA 654YM
UT WOS:000282207200008
ER
PT J
AU Jang, HJ
Appelbaum, I
AF Jang, Hyuk-Jae
Appelbaum, Ian
TI Magnetocurrent of ballistically injected electrons in insulating silicon
SO APPLIED PHYSICS LETTERS
LA English
DT Article
AB By using ballistic hot-electron injection to achieve lateral conduction through an otherwise fully insulating undoped silicon channel, we are able to study magnetic field suppression of charge transport in a regime normally excluded in Ohmic magnetoresistance measurements. Exceptionally large magnetocurrent changes of >16 000% at 45 K in magnetic fields of approximate to 2 T are observed, with differential reduction of over 6.2 T-1. Temperature-, electrostatic back-gate-, and magnetic field angle-dependence are presented. This phenomenon is attributed to strong space-charge effects in the dilute three-dimensional electron gas created by nonequilibrium injection. (c) 2010 American Institute of Physics. [doi:10.1063/1.3511681]
C1 [Jang, Hyuk-Jae; Appelbaum, Ian] Univ Maryland, Dept Phys, Ctr Nanophys & Adv Mat, College Pk, MD 20742 USA.
RP Jang, HJ (reprint author), NIST, Gaithersburg, MD 20899 USA.
EM appelbaum@physics.umd.edu
RI Appelbaum, Ian/E-4056-2012; Jang, Hyuk-Jae/H-7904-2013
FU Office of Naval Research; Maryland NanoCenter; FabLab; National Science
Foundation
FX We gratefully acknowledge helpful discussions on these results with S.
Crooker and D. Smith. This work was supported by the Office of Naval
Research and the National Science Foundation. We acknowledge the support
of the Maryland NanoCenter and its FabLab.
NR 12
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Z9 7
U1 1
U2 10
PU AMER INST PHYSICS
PI MELVILLE
PA CIRCULATION & FULFILLMENT DIV, 2 HUNTINGTON QUADRANGLE, STE 1 N O 1,
MELVILLE, NY 11747-4501 USA
SN 0003-6951
EI 1077-3118
J9 APPL PHYS LETT
JI Appl. Phys. Lett.
PD NOV 1
PY 2010
VL 97
IS 18
AR 182108
DI 10.1063/1.3511681
PG 3
WC Physics, Applied
SC Physics
GA 676RK
UT WOS:000283934100041
ER
PT J
AU Li, L
Yang, S
Wang, ZY
Zhu, XD
Tang, HY
AF Li, Lin
Yang, Song
Wang, Zhenyu
Zhu, Xide
Tang, Hongyu
TI Evidence of Warming and Wetting Climate over the Qinghai-Tibet Plateau
SO ARCTIC ANTARCTIC AND ALPINE RESEARCH
LA English
DT Article
ID ASIAN SUMMER MONSOON; LONG-TERM CHANGES; CHINA; CIRCULATION; OROGRAPHY;
RAINFALL; DECADES; WAVES; ONSET; SHIFT
AB In this study, we apply temperature, precipitation, and other data from 66 Chinese meteorological stations including Xining and Lhasa to analyze the extreme climate events and their impacting factors over the Qinghai-Tibet Plateau during the period 1961-2007 We focus on the spatial and temporal features of extreme climate events and their long-term changes over five climate zones of alpine grassland meadow and desert areas
Results show that, during the past decades, the changes in climate over the Qinghai-Tibet Plateau present trends towards warm and wet conditions These changes in temperature and precipitation are evident in both seasonal means and extreme events, and the changes in precipitation are apparent in both precipitation amount and number of precipitation days Clearly, warm and wet events Increase, but cold and dry events decrease over the plateau region Features of the warming climate are relatively consistent in spatial and seasonal distributions, with the most significant changes in winter and autumn and at nighttime Northern Qinghai exhibits the greatest and most significant decrease in the frequency of extremely low-temperature events However, the wetting trend shows more distinctive spatial features and is more seasonally dependent While the trends in both precipitation amount and the number of precipitation days are positive in all climate zones for winter and spring, both positive and insignificant negative trends appear in summer and autumn The largest decrease in the frequency of severely dry events is found over southeastern Tibet and western Sichuan
C1 [Yang, Song] NOAA, Climate Predict Ctr, Camp Springs, MD 20746 USA.
[Li, Lin; Wang, Zhenyu; Zhu, Xide; Tang, Hongyu] Qinghai Climate Ctr, Xining 810001, Qinghai, Peoples R China.
[Li, Lin; Wang, Zhenyu; Zhu, Xide; Tang, Hongyu] Qinghai Ctr Climate Change Monitoring & Evaluat, Xining 810001, Qinghai, Peoples R China.
RP Yang, S (reprint author), NOAA, Climate Predict Ctr, 5200 Auth Rd,Room 605, Camp Springs, MD 20746 USA.
RI Yang, Song/B-4952-2009
FU China Meteorological Administration [GYHY200906019]
FX The authors are thankful for the comments by two anonymous reviewers
that are helpful for improving the overall quality of the paper This
study was supported by a meteorological research project of the China
Meteorological Administration (Grant GYHY200906019)
NR 47
TC 29
Z9 32
U1 2
U2 31
PU INST ARCTIC ALPINE RES
PI BOULDER
PA UNIV COLORADO, BOULDER, CO 80309 USA
SN 1523-0430
EI 1938-4246
J9 ARCT ANTARCT ALP RES
JI Arct. Antarct. Alp. Res.
PD NOV
PY 2010
VL 42
IS 4
BP 449
EP 457
DI 10.1657/1938-4246-42.4.449
PG 9
WC Environmental Sciences; Geography, Physical
SC Environmental Sciences & Ecology; Physical Geography
GA 690EW
UT WOS:000284986300009
ER
PT J
AU Oltmans, SJ
Lefohn, AS
Harris, JM
Tarasick, DW
Thompson, AM
Wernli, H
Johnson, BJ
Novelli, PC
Montzka, SA
Ray, JD
Patrick, LC
Sweeney, C
Jefferson, A
Dann, T
Davies, J
Shapiro, M
Holben, BN
AF Oltmans, S. J.
Lefohn, A. S.
Harris, J. M.
Tarasick, D. W.
Thompson, A. M.
Wernli, H.
Johnson, B. J.
Novelli, P. C.
Montzka, S. A.
Ray, J. D.
Patrick, L. C.
Sweeney, C.
Jefferson, A.
Dann, T.
Davies, J.
Shapiro, M.
Holben, B. N.
TI Enhanced ozone over western North America from biomass burning in
Eurasia during April 2008 as seen in surface and profile observations
SO ATMOSPHERIC ENVIRONMENT
LA English
DT Article
DE Ozone; Biomass burning; Pollution; Arctic; Transport; Trajectories
ID BACKGROUND OZONE; VARIABILITY; MISSION; ARCTAS; TROPOSPHERE; TRANSPORT;
POLLUTION; AIRCRAFT
AB During April 2008, as part of the International Polar Year (IPY), a number of ground-based and aircraft campaigns were carried out in the North American Arctic region (e.g., ARCTAS, ARCPAC). The widespread presence during this period of biomass burning effluent, both gaseous and particulate, has been reported. Unusually high ozone readings for this time of year were recorded at surface ozone monitoring sites from northern Alaska to northern California. At Barrow, Alaska, the northernmost point in the United States, the highest April ozone readings recorded at the surface (hourly average values >55 ppbv) in 37 years of observation were measured on April 19, 2008. At Denali National Park in central Alaska, an hourly average of 79 ppbv was recorded during an 8-h period in which the average was over 75 ppbv, exceeding the ozone ambient air quality standard threshold value in the U.S. Elevated ozone (>60 ppbv) persisted almost continuously from April 19-23 at the monitoring site during this event. At a coastal site in northern California (Trinidad Head), hourly ozone readings were >50 ppbv almost continuously for a 35-h period from April 18-20. At several sites in northern California, located to the east of Trinidad Head, numerous occurrences of ozone readings exceeding 60 ppbv were recorded during April 2008. Ozone profiles from an extensive series of balloon soundings showed lower tropospheric features at similar to 1-6 km with enhanced ozone during the times of elevated ozone amounts at surface sites in western Canada and the U.S. Based on extensive trajectory calculations, biomass burning in regions of southern Russia was identified as the likely source of the observed ozone enhancements. Ancillary measurements of atmospheric constituents and optical properties (aerosol optical thickness) supported the presence of a burning plume at several locations. At two coastal sites (Trinidad Head and Vancouver Island), profiles of a large suite of gases were measured from airborne flask samples taken during probable encounters with burning plumes. These profiles aided in characterizing the vertical thickness of the plumes, as well as confirming that the plumes reaching the west coast of North America were associated with biomass burning events. Published by Elsevier Ltd.
C1 [Oltmans, S. J.; Harris, J. M.; Johnson, B. J.; Novelli, P. C.; Montzka, S. A.; Patrick, L. C.; Sweeney, C.; Jefferson, A.] NOAA Earth Syst Res Lab, Global Monitoring Div, Boulder, CO 80305 USA.
[Lefohn, A. S.] ASL & Associates, Helena, MT USA.
[Tarasick, D. W.; Davies, J.] Environm Canada, Air Qual Res Div, Downsview, ON, Canada.
[Thompson, A. M.] Penn State Univ, Dept Meteorol, University Pk, PA 16802 USA.
[Wernli, H.] ETHZ, Inst Atmospher & Climate Sci, Zurich, Switzerland.
[Ray, J. D.] Natl Pk Serv, Air Resources Div, Denver, CO USA.
[Patrick, L. C.; Sweeney, C.; Jefferson, A.] Univ Colorado, CIRES, Boulder, CO 80309 USA.
[Dann, T.] Environm Canada, Anal & Air Qual Div, Ottawa, ON K1A 0H3, Canada.
[Shapiro, M.] NCAR, Boulder, CO USA.
[Holben, B. N.] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
RP Oltmans, SJ (reprint author), NOAA Earth Syst Res Lab, Global Monitoring Div, 325 Broadway, Boulder, CO 80305 USA.
EM Samuel.J.Oltmans@noaa.gov
RI Jefferson, Anne/K-4793-2012; Thompson, Anne /C-3649-2014;
OI Thompson, Anne /0000-0002-7829-0920; Montzka,
Stephen/0000-0002-9396-0400; Tarasick, David/0000-0001-9869-0692
FU NASA as part of ARCTAS; Environment Canada; NOAA/ESRL/GMD
FX Debbie Miller, U.S. National Park Service, provided the IMPROVE aerosol
data. Funding for the ozonesonde launches was provided by NASA as part
of ARCTAS, Environment Canada, and NOAA/ESRL/GMD.
NR 32
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U1 1
U2 13
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 1352-2310
J9 ATMOS ENVIRON
JI Atmos. Environ.
PD NOV
PY 2010
VL 44
IS 35
BP 4497
EP 4509
DI 10.1016/j.atmosenv.2010.07.004
PG 13
WC Environmental Sciences; Meteorology & Atmospheric Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA 672FL
UT WOS:000283568300021
ER
PT J
AU Saikawa, E
Naik, V
Horowitz, LW
Liu, JF
Mauzerall, DL
AF Saikawa, Eri
Naik, Vaishali
Horowitz, Larry W.
Liu, Junfeng
Mauzerall, Denise L.
TI Present and potential future contributions of sulfate, black and organic
carbon aerosols from China to global air quality, premature mortality
and radiative forcing (vol 43, pg 2814, 2009)
SO ATMOSPHERIC ENVIRONMENT
LA English
DT Correction
C1 [Saikawa, Eri; Naik, Vaishali; Liu, Junfeng; Mauzerall, Denise L.] Princeton Univ, Woodrow Wilson Sch Publ & Int Affairs, Princeton, NJ 08544 USA.
[Horowitz, Larry W.] Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA.
RP Mauzerall, DL (reprint author), Princeton Univ, Woodrow Wilson Sch Publ & Int Affairs, Princeton, NJ 08544 USA.
EM mauzeral@princeton.edu
RI Mauzerall, Denise/I-5977-2013; Horowitz, Larry/D-8048-2014; Naik,
Vaishali/A-4938-2013;
OI Mauzerall, Denise/0000-0003-3479-1798; Horowitz,
Larry/0000-0002-5886-3314; Naik, Vaishali/0000-0002-2254-1700; Saikawa,
Eri/0000-0003-3166-8620
NR 1
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U1 1
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PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 1352-2310
J9 ATMOS ENVIRON
JI Atmos. Environ.
PD NOV
PY 2010
VL 44
IS 35
BP 4528
EP 4528
DI 10.1016/j.atmosenv.2010.07.009
PG 1
WC Environmental Sciences; Meteorology & Atmospheric Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA 672FL
UT WOS:000283568300024
ER
PT J
AU Wang, DH
Li, XF
Tao, WK
AF Wang, Donghai
Li, Xiaofan
Tao, Wei-Kuo
TI Cloud radiative effects on responses of rainfall to large-scale forcing
during a landfall of severe tropical storm Bilis (2006)
SO ATMOSPHERIC RESEARCH
LA English
DT Article
DE Cloud-radiation interaction; Cloud radiative effects; Convective and
stratiform rainfall; Cloud-resolving model simulation
ID SOUTH CHINA SEA; MICROSCALE STRUCTURE; STRATIFORM REGIONS; FRONTAL
RAINBANDS; RESOLVING MODEL; PHASE-III; SYSTEMS; WATER; PRECIPITATION;
CONVECTION
AB The cloud radiative effects on responses of rainfall to the large-scale forcing during a landfall of severe tropical storm Bilis (2006) are investigated by analyzing sensitivity experiments Imposed by large-scale forcing from NCEP/GDAS data in a two-dimensional cloud-resolving model The daily average analysis is conducted on 15 and 16 July 2009 respectively due to dominant stratiform and convective rainfall associated with different large-scale forcing When cloud radiative effects are excluded the increased mean rainfall is associated with the increased mean radiative cooling through the enhanced mean latent heat on 15 July The reduction in mean rain rate is related to the slowdown in the mean net condensation while the enhanced mean radiative cooling from the removal of cloud radiative effects is balanced by the suppressed heat divergence on 16 July The increased mean rainfall on 15 July and decreased mean rainfall on 16 July are mainly from raining stratiform regions The enhanced stratiform rainfall is associated with the weakened local atmospheric moistening and strengthened local hydrometeor loss on 15 July whereas the reduced stratiform rainfall is related to the weakened water vapor convergence on 16 July
When cloud-radiation interaction is excluded the decreases in the mean ram rate are associated with the slowdown in the mean hydrometeor loss on 15 July and the suppression in the net condensation on 16 July The decreased mean rainfall is mainly from convective regions on 15 July and raining stratiform regions on 16 July The reduced convective rainfall is associated with strengthened transport of hydrometeor concentration from convective regions to raining stratiform regions on 15 July whereas the decreased stratiform rainfall is related to the weakened water vapor convergence on 16 July (C) 2010 Elsevier B V All rights reserved
C1 [Wang, Donghai] Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing, Peoples R China.
[Wang, Donghai] Sci Syst & Applicat Inc, Lanham, MD USA.
[Li, Xiaofan] NOAA, NESDIS, Ctr Satellite Applicat & Res, Camp Springs, MD USA.
[Tao, Wei-Kuo] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
RP Wang, DH (reprint author), Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing, Peoples R China.
RI Li, Xiaofan/F-5605-2010; Li, Xiaofan/G-2094-2014
FU State Key Basic Research Development Program [2009CB421504]; National
Natural Science Foundation of China [40633016, 40875022, 40830958]
FX The authors thank two anonymous reviewers for their constructive
comments This research was supported by the State Key Basic Research
Development Program (2009CB421504), and the National Natural Science
Foundation of China under grant No 40633016, 40875022 and 40830958
NR 33
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U1 0
U2 3
PU ELSEVIER SCIENCE INC
PI NEW YORK
PA 360 PARK AVE SOUTH, NEW YORK, NY 10010-1710 USA
SN 0169-8095
J9 ATMOS RES
JI Atmos. Res.
PD NOV-DEC
PY 2010
VL 98
IS 2-4
BP 512
EP 525
DI 10.1016/j.atmosres.2010.08.020
PG 14
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 690DT
UT WOS:000284983400033
ER
PT J
AU Kramida, AE
AF Kramida, A. E.
TI A critical compilation of experimental data on spectral lines and energy
levels of hydrogen, deuterium, and tritium
SO ATOMIC DATA AND NUCLEAR DATA TABLES
LA English
DT Article
ID FUNDAMENTAL PHYSICAL CONSTANTS; OSCILLATORY-FIELD MEASUREMENT; CODATA
RECOMMENDED VALUES; ABSOLUTE FREQUENCY MEASUREMENTS; HIGH-RESOLUTION
SPECTROSCOPY; MICROWAVE-OPTICAL METHOD; FINE-STRUCTURE INTERVAL;
LAMB-SHIFT MEASUREMENT; SOLAR EMISSION-LINES; SHORT-LIVED STATES
AB For more than 50 years, Charlotte Moore's compilation of atomic energy levels and its subsequent revisions have been the standard source of reference data for the spectra of hydrogen and its isotopes. In those publications, theoretical data based on quantum-electrodynamic calculations have been given. This reflects the fact that the theory of the hydrogen spectrum has been perfected to an extent far exceeding the capabilities of the best measurements. However, rapid advances in the techniques of laser spectroscopy and optical frequency metrology have recently put experiments on a par with theory in terms of precision. This calls for construction of new comprehensive data sets for H, D, and T that summarize the latest experimental work and can be directly compared with the modern theoretical reference data. The present work compiles several tens of recent measurements of the hydrogen, deuterium, and tritium fine and hyperfine structure intervals and presents sets of energy levels and Ritz wavelengths derived from those measurements. Data exist for the fine structure of energy levels of hydrogen and deuterium up to principal quantum number n = 12. For higher lying levels, there are many observed lines with unresolved fine structure. From those observations, level centers (centers of the fine structure) are derived by a least-squares optimization, and Ritz wavelengths of series with upper levels up to n = 40 are obtained. For tritium, the n = 2 and 3 energy level intervals are derived from experimental observations. (C) 2010 Elsevier Inc. All rights reserved.
C1 Natl Inst Stand & Technol, Atom Phys Div, Gaithersburg, MD 20899 USA.
RP Kramida, AE (reprint author), Natl Inst Stand & Technol, Atom Phys Div, 100 Bur Dr,MS 8422, Gaithersburg, MD 20899 USA.
EM Alexander.kramida@nist.gov
OI Kramida, Alexander/0000-0002-0788-8087
FU Office of Fusion Energy Sciences of the U.S. Department of Energy;
National Aeronautics and Space Administration
FX The author is grateful to P.J. Mohr for fruitful discussions on various
aspects of the QED theory of fine and hyperfine structure and the
determination of the fundamental constants. The correspondence with S.R.
Lundeen, D.A. Van Baak, F. Nez, F. Biraben, and J.C. Bergquist regarding
the details of their experiments on the fine structure measurements and
hyperfine corrections is gratefully acknowledged. The author also thanks
T.A. Clark for the help with solar observations of high members of the
hydrogen series and for providing his latest data prior to publication.
Fruitful discussions with J. Reader and W.C. Martin, as well as generous
help provided by C.J. Sansonetti on the interpretation of
interferometric measurements, are greatly appreciated. The author
expresses his gratitude to one of the referees for providing multiple
important corrections and stylistic improvements. This work is supported
in part by the Office of Fusion Energy Sciences of the U.S. Department
of Energy and by the National Aeronautics and Space Administration.
NR 231
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U2 25
PU ACADEMIC PRESS INC ELSEVIER SCIENCE
PI SAN DIEGO
PA 525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA
SN 0092-640X
J9 ATOM DATA NUCL DATA
JI Atom. Data Nucl. Data Tables
PD NOV
PY 2010
VL 96
IS 6
BP 586
EP 644
DI 10.1016/j.adt.2010.05.001
PG 59
WC Physics, Atomic, Molecular & Chemical; Physics, Nuclear
SC Physics
GA 657GH
UT WOS:000282400700002
ER
PT J
AU Tang, PB
Huber, D
Akinci, B
Lipman, R
Lytle, A
AF Tang, Pingbo
Huber, Daniel
Akinci, Burcu
Lipman, Robert
Lytle, Alan
TI Automatic reconstruction of as-built building information models from
laser-scanned point clouds: A review of related techniques
SO AUTOMATION IN CONSTRUCTION
LA English
DT Review
DE Building information models; Building reconstruction; Laser scanners;
Object recognition; Geometric modeling; Relationship modeling; Shape
representation
ID 3D OBJECT RECOGNITION; RANGE IMAGES; MOBILE ROBOTS; MAPS;
REPRESENTATION; CONSTRUCTION; ENVIRONMENTS; REGISTRATION; ACQUISITION;
ALGORITHMS
AB Building information models (BIMs) are maturing as a new paradigm for storing and exchanging knowledge about a facility. BIMs constructed from a CAD model do not generally capture details of a facility as it was actually built. Laser scanners can be used to capture dense 3D measurements of a facility's as-built condition and the resulting point cloud can be manually processed to create an as-built BIM - a time-consuming, subjective, and error-prone process that could benefit significantly from automation. This article surveys techniques developed in civil engineering and computer science that can be utilized to automate the process of creating as-built BIMs. We sub-divide the overall process into three core operations: geometric modeling, object recognition, and object relationship modeling. We survey the state-of-the-art methods for each operation and discuss their potential application to automated as-built BIM creation. We also outline the main methods used by these algorithms for representing knowledge about shape, identity, and relationships. In addition, we formalize the possible variations of the overall as-built BIM creation problem and outline performance evaluation measures for comparing as-built BIM creation algorithms and tracking progress of the field. Finally, we identify and discuss technology gaps that need to be addressed in future research. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Huber, Daniel] Carnegie Mellon Univ, Inst Robot, Pittsburgh, PA 15213 USA.
[Tang, Pingbo] Western Michigan Univ, Dept Civil & Construct Engn, Kalamazoo, MI 49008 USA.
[Akinci, Burcu] Carnegie Mellon Univ, Dept Civil & Environm Engn, Pittsburgh, PA 15213 USA.
[Lipman, Robert; Lytle, Alan] Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
RP Huber, D (reprint author), Carnegie Mellon Univ, Inst Robot, 4105 Newell Simon Hall, Pittsburgh, PA 15213 USA.
EM tangpingbo@gmail.com; dhuber@cs.cmu.edu; bakinci@andrew.cmu.edu;
robert.lipman@nist.gov; alan.lytle@nist.gov
RI Tang, Pingbo/I-7649-2012; Tang, Pingbo/I-9534-2012;
OI Tang, Pingbo/0000-0001-9048-1327; Tang, Pingbo/0000-0002-4910-1326
FU National Institute of Standards and Technology (NIST) [60NANB7D6156];
General Services Administration (GSA) [GS00P07CYP0233]; National Science
Foundation [0856558]
FX This research was supported, in part, by the National Institute of
Standards and Technology (NIST) under grant 60NANB7D6156, by the General
Services Administration (GSA) under grant GS00P07CYP0233, and by the
National Science Foundation under Grant No. 0856558. Their support is
gratefully acknowledged. Any opinions, findings and conclusions, or
recommendations expressed in this material are those of the authors and
do not necessarily reflect the views of NIST or the National Science
Foundation. Mention of trade names in this article does not imply
endorsement by Carnegie Mellon University or NIST.
NR 100
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Z9 156
U1 53
U2 265
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0926-5805
EI 1872-7891
J9 AUTOMAT CONSTR
JI Autom. Constr.
PD NOV
PY 2010
VL 19
IS 7
BP 829
EP 843
DI 10.1016/j.autcon.2010.06.007
PG 15
WC Construction & Building Technology; Engineering, Civil
SC Construction & Building Technology; Engineering
GA 669ZJ
UT WOS:000283388600002
ER
PT J
AU Donoso, M
Dutton, PH
AF Donoso, Miguel
Dutton, Peter H.
TI Sea turtle bycatch in the Chilean pelagic longline fishery in the
southeastern Pacific: Opportunities for conservation
SO BIOLOGICAL CONSERVATION
LA English
DT Article
DE Sea turtles; Marine conservation; Bycatch; Longlines; Incidental take;
Fisheries
ID LOGGERHEAD CARETTA-CARETTA; POST-NESTING MIGRATIONS; WESTERN
NORTH-ATLANTIC; DERMOCHELYS-CORIACEA; LEATHERBACK TURTLES; INCIDENTAL
CAPTURE; LEPIDOCHELYS-OLIVACEA; SWORDFISH FISHERY; SPATIAL-PATTERNS;
POPULATION-MODEL
AB Data are presented on sea turtles caught in the Chilean longline fishery targeting swordfish, Xiphias gladius, in international waters off Chile. A total of 10,604,059 hooks from 7976 sets were observed, representing 94% of the total number of hooks fished between 2001 and 2005. Leatherbacks, Dermochelys coriacea, (n = 284) and loggerheads, Caretta caretta, (n = 59) were the most common species captured. Leatherbacks were caught in less than 4% of the sets, with an overall mean of 0.0268 turtles per 1000 hooks. Loggerheads were caught in less than 1% of the sets with a mean catch rate of 0.0056 turtles per 1000 hooks. Most leatherbacks (97.5% of total) were caught between 24 degrees S and 38 degrees S, while loggerheads were caught primarily in the northern portion of the area fished, between 24 degrees 19'S and 25 degrees 31'S. All loggerheads were dehooked where appropriate and released alive. A total of two leatherbacks were found dead. Despite the low catch rate of leatherbacks, the potential impact of this fishery on the severely depleted nesting populations in the eastern Pacific could be significant when combined with other fisheries and threats in the region. The very low mortality of bycaught sea turtles observed in our study is encouraging and suggests that there are opportunities for further reducing harmful effects of swordfish longline fishing on sea turtles. Results of spatial analysis of loggerhead bycatch relative to fishing effort show that closure of the northernmost fishing area would eliminate the majority of the loggerhead bycatch. Published by Elsevier Ltd.
C1 [Dutton, Peter H.] NOAA, Protected Resources Div, SW Fisheries Sci Ctr, Natl Marine Fisheries Serv, La Jolla, CA 92037 USA.
[Donoso, Miguel] Pacifico Laud, Quilpue, Chile.
RP Dutton, PH (reprint author), NOAA, Protected Resources Div, SW Fisheries Sci Ctr, Natl Marine Fisheries Serv, 3333 N Torrey Pines Court, La Jolla, CA 92037 USA.
EM Peter.Dutton@noaa.gov
FU NOAA Fisheries Service; Instituto de Fomento Pesquero (IFOP)
FX This study was carried out as part of the US-Chile Fisheries Cooperation
Agreement between NOAA Fisheries Service and SER-NAPESCA, with funding
from NOAA Fisheries Service and the Instituto de Fomento Pesquero
(IFOP). We thank the IFOP scientific observers, as well as the captains
and crew of the participating fishing vessels. Carlos Montenegro
assisted with statistical analysis. We thank William Perrin, Kelly
Stewart, James Carretta and two anonymous reviewers for helpful comments
and suggestions.
NR 101
TC 23
Z9 23
U1 2
U2 20
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0006-3207
EI 1873-2917
J9 BIOL CONSERV
JI Biol. Conserv.
PD NOV
PY 2010
VL 143
IS 11
BP 2672
EP 2684
DI 10.1016/j.biocon.2010.07.011
PG 13
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 670HR
UT WOS:000283412300030
ER
PT J
AU Allen, SD
Fathi, Y
Gross, K
Mace, M
AF Allen, S. D.
Fathi, Y.
Gross, K.
Mace, M.
TI An optimal and near-optimal strategy to selecting individuals for
transfer in captive breeding programs
SO BIOLOGICAL CONSERVATION
LA English
DT Article
DE Minimum kinship; Maximum genetic diversity; Relocation; Reintroductions
ID POPULATIONS; MANAGEMENT; SCHEMES; SIZE
AB As species extinction rates continue to rise, zoos have adopted a more active role in the conservation of endangered species. A central concern is to preserve genetic diversity of zoological populations. Accordingly, when selecting individuals to transfer to new or existing populations, zoo managers must consider the genetic effects on all populations involved. We propose a quadratic integer programming (IP) model to identify a group of individuals to transfer that maximizes genetic diversity within two subpopulations. We then reduce this model to a linear IP formulation and apply it to the California condor (Gymnogyps californianus) studbook. After simplifying the linear IP model, optimality is achieved within a reasonable time limit when a limited number of individuals are relocated. We also develop a local improvement algorithm (LIA) to efficiently provide near-optimal solutions when we increase the number of transferred individuals. The LIA quickly obtains optimal solutions when few individuals are transferred and in most cases, the LIA outperforms MetaMK, an existing program used to select animals for transfer. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Allen, S. D.; Fathi, Y.] N Carolina State Univ, Dept Operat Res, Coll Engn, Raleigh, NC 27695 USA.
[Gross, K.] N Carolina State Univ, Dept Stat, Coll Phys & Math Sci, Raleigh, NC 27695 USA.
[Mace, M.] San Diego Zoos Wild Anim Pk, Escondido, CA 92027 USA.
RP Allen, SD (reprint author), SW Fisheries Sci Ctr, Fisheries Ecol Div, 110 Shaffer Rd, Santa Cruz, CA 95060 USA.
EM shanae.allen@noaa.gov; fathi@eos.ncsu.edu; gross@stat.ncsu.edu;
mmace@sandiegozoo.org
NR 29
TC 2
Z9 2
U1 3
U2 42
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0006-3207
J9 BIOL CONSERV
JI Biol. Conserv.
PD NOV
PY 2010
VL 143
IS 11
BP 2858
EP 2863
DI 10.1016/j.biocon.2010.08.003
PG 6
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 670HR
UT WOS:000283412300051
ER
PT J
AU Sun, JR
Ding, YF
Lin, NJ
Zhou, J
Ro, H
Soles, CL
Cicerone, MT
Lin-Gibson, S
AF Sun, Jirun
Ding, Yifu
Lin, Nancy J.
Zhou, Jing
Ro, Hyunwook
Soles, Christopher L.
Cicerone, Marcus T.
Lin-Gibson, Sheng
TI Exploring Cellular Contact Guidance Using Gradient Nanogratings
SO BIOMACROMOLECULES
LA English
DT Article
ID MESENCHYMAL STEM-CELLS; NANOIMPRINT LITHOGRAPHY; SUBSTRATE TOPOGRAPHY;
BEHAVIOR; SURFACE; DIFFERENTIATION; NANOSCALE; MICRO; NANOTOPOGRAPHY;
DIMENSIONS
AB Nanoscale surface features that mimic extracellular matrix are critical environmental cues for cell contact guidance and are vital in advanced medical devices in order to manipulate cell behaviors. Among them, nanogratings (line-and-space gratings) are common platforms to study geometric effects on cell contact guidance, especially cell alignment, but generally are one pattern height per platform. In this study, we developed a strategy to fabricate controlled substrates with a wide range of pattern shapes and surface chemistries and to separate surface chemistry and topography effects. As a demonstration of this strategy, six nanograting platforms on three materials were fabricated and applied to examine and differentiate the effects of surface topography and surface chemistry on cell contact guidance of murine preosteoblasts. All of the six platforms contained the same gradient in pattern height (0 to approximate to 350 nm). They were prepared using nanoimprint lithography and annealing for thermoplastic materials (low molecular weight polystyrene (PS) and polymethylmethacrylate (PMMA)) and photoimprint for a thermoset material (a cross-linked dimethacrylate (DMA)). Each material contains two platforms that are only different in line-and-space pitch (420 or 800 nm). The DMA nanogratings had a reverse line-and-space profile to those of the PS and PMMA nanogratings. Using these platforms, a full range of cell alignment, from randomly orientated to completely parallel to the grating direction was achieved, Results from focal adhesion assays and scanning electronic microscopy indicated a change in cell substrate contact from a noncomposite state (full contact) to a composite state (partial contact between cell and substrate) as pattern height increased. These gradient platforms allowed for the separation of surface chemistry and surface topography to provide insight into the mechanisms responsible for cell contact guidance on nanopatterned surfaces.
C1 [Sun, Jirun] Amer Dent Assoc Fdn, Paffenbarger Res Ctr, Gaithersburg, MD 20899 USA.
[Ding, Yifu] Univ Colorado, Dept Mech Engn, Boulder, CO 80309 USA.
[Lin, Nancy J.; Zhou, Jing; Ro, Hyunwook; Soles, Christopher L.; Cicerone, Marcus T.; Lin-Gibson, Sheng] NIST, Div Polymers, Gaithersburg, MD 20899 USA.
RP Sun, JR (reprint author), Amer Dent Assoc Fdn, Paffenbarger Res Ctr, 100 Bur Dr, Gaithersburg, MD 20899 USA.
EM jsun@nist.gov; slgibson@nist.gov
FU National Institute of Denial and Craniofacial Research (NIDCR)
[Y1-DE-7005-01]; NIST; NIST Office of Microelectronic Programs; National
Science Foundation [CMMI-0928067]
FX This work is partially funded by the National Institute of Denial and
Craniofacial Research (NIDCR) through an Interagency Agreement
(Y1-DE-7005-01) with NIST and by the NIST Office of Microelectronic
Programs. Y.D. acknowledges partial funding support from the National
Science Foundation under Grant No. CMMI-0928067. We acknowledge the
nanofabrication laboratory of the Center for Nanoscale Science and
Technology (CNST) at NIST for providing facilities for the nanoimprint
process, and acknowledge the use of the NIST Combinatorial Methods
Center equipment. The authors would like to thank Drs. Nathan Gallant,
Xiaohua Zhang, and Carl Simon for their advice and technical
recommendations. Certain equipment, instruments, or materials are
identified in this paper to adequately specify the experimental details.
Such identification does not imply recommendation by the National
Institute of Standards and Technology, nor does it imply the materials
are necessary the best available for the purpose.
NR 34
TC 18
Z9 18
U1 2
U2 24
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 1525-7797
J9 BIOMACROMOLECULES
JI Biomacromolecules
PD NOV
PY 2010
VL 11
IS 11
BP 3067
EP 3072
DI 10.1021/bm100883m
PG 6
WC Biochemistry & Molecular Biology; Chemistry, Organic; Polymer Science
SC Biochemistry & Molecular Biology; Chemistry; Polymer Science
GA 675FD
UT WOS:000283810900032
PM 20954734
ER
PT J
AU Liebmann, B
Dole, RM
Jones, C
Blade, I
Allured, D
AF Liebmann, Brant
Dole, Randall M.
Jones, Charles
Blade, Ileana
Allured, Dave
TI INFLUENCE OF CHOICE OF TIME PERIOD ON GLOBAL SURFACE TEMPERATURE TREND
ESTIMATES
SO BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY
LA English
DT Article
ID AIR-TEMPERATURE; UPDATE; SERIES; LAND
AB Annual global surface temperature and global land surface temperature trends are calculated for all possible periods of the historical record between 1850 and 2009. Two-dimensional parameter diagrams show the critical influence of the choice of start and end years on the calculated trend and associated temperature changes and suggest time scales required to establish robust trends.
The largest trends and associated temperature changes are all positive and have occurred over periods ending in recent years. Substantial positive changes also occurred from the early twentieth century until the mid-1940s. The continents exhibit greater long-term warming than the global average overall, but less warming in the early part of the century (segments ending in the 1940s). The recent period of short-term cooling beginning in the late 1990s is neither statistically significant nor unusual in the context of trend variability in the full historical record.
Global-mean and land surface temperature changes for periods ending in recent years and longer than about 90 years are extremely unlikely to have occurred by chance. In contrast, short-term trends over less than a few decades are generally not statistically significant. This implies significant contributions of decadal variability to trends estimated over such short time periods.
C1 [Liebmann, Brant] NOAA, ESRL, PSD Climate Diagnost Branch, Boulder, CO 80305 USA.
[Liebmann, Brant; Allured, Dave] Univ Colorado, Boulder, CO 80309 USA.
[Jones, Charles] Univ Calif Santa Barbara, Inst Computat Earth Syst Sci, Santa Barbara, CA 93106 USA.
[Blade, Ileana] Univ Barcelona, Dept Astron & Meteorol, Barcelona, Spain.
RP Liebmann, B (reprint author), NOAA, ESRL, PSD Climate Diagnost Branch, R PSD1,325 Broadway, Boulder, CO 80305 USA.
EM brant.liebmann@noaa.gov
RI Jones, Charles/I-4574-2012
OI Jones, Charles/0000-0003-4808-6977
NR 24
TC 40
Z9 41
U1 0
U2 15
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0003-0007
EI 1520-0477
J9 B AM METEOROL SOC
JI Bull. Amer. Meteorol. Soc.
PD NOV
PY 2010
VL 91
IS 11
BP 1485
EP U71
DI 10.1175/2010BAMS3030.1
PG 9
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 695YP
UT WOS:000285409200002
ER
PT J
AU McClatchie, S
Goericke, R
Auad, G
Hill, K
AF McClatchie, Sam
Goericke, Ralf
Auad, Guillermo
Hill, Kevin
TI Re-assessment of the stock-recruit and temperature-recruit relationships
for Pacific sardine (Sardinops sagax)
SO CANADIAN JOURNAL OF FISHERIES AND AQUATIC SCIENCES
LA English
DT Article
ID SANTA-BARBARA CHANNEL; ANCHOVY POPULATIONS; CALIFORNIA CURRENT; FISH;
MELANOSTICTUS; FLUCTUATIONS; SABLEFISH
AB The harvest guideline for Pacific sardine (Sardinops sagax) incorporates an environmental parameter based on averaged surface temperatures at the Scripps Institution of Oceanography pier (SIO pier) in La Jolla, California, USA, which would be invoked after a series of cool years to reduce commercial catches using a precautionary decision rule. We revisit the stock-recruit and temperature-recruit relationships underpinning the currently used environmental parameter for sardine assessment and found that the temperature-recruit relationship no longer holds for the SIO pier when time series are updated with data from more recent years. The significance of the correlation between temperature and recruitment was also artificially increased by autocorrelation in the time series. In contrast, the stock-recruit relationship was still valid when recent data were added. SIO pier surface temperatures are warmer than 10 m-depth Southern California Bight (SCB) temperatures where the sardine spawn, and the difference has increased since the late 1970s. Sardine recruitment was also not related to offshore temperatures in the SCB. We demonstrate that the environmental proxy derived from SIO pier temperature, which has never affected the harvest guideline since its implementation, no longer predicts recruitment of Pacific sardine, and should be removed from sardine management.
C1 [McClatchie, Sam; Hill, Kevin] NOAA Fisheries Serv, SW Fisheries Sci Ctr, La Jolla, CA 92037 USA.
[Goericke, Ralf] Scripps Inst Oceanog, Integrat Oceanog Div, La Jolla, CA 92093 USA.
[Auad, Guillermo] Scripps Inst Oceanog, Div Climate Res, La Jolla, CA 92093 USA.
RP McClatchie, S (reprint author), NOAA Fisheries Serv, SW Fisheries Sci Ctr, 8604 La Jolla Shores Dr, La Jolla, CA 92037 USA.
EM Sam.McClatchie@noaa.gov
FU NOAA Fisheries; National Science Foundation [OCE-0417616]
FX NOAA_ERSST_V3 data provided by the National Oceanic and Atmospheric
Administration Office of Oceanic and Atmospheric Research Earth System
Research Laboratory Physical Sciences Division, Boulder, Colorado, USA,
from their web site at www.cdc.noaa.gov. S. M. was supported by NOAA
Fisheries through the Fisheries And The Environment program (FATE); R.
G. was supported by the National Science Foundation grant OCE-0417616 to
the CCE-LTER. We appreciate the reviews provided by Ed Weber, Christian
Reiss, Alec MacCall, and Nancy Lo, prior to submission.
NR 28
TC 29
Z9 30
U1 0
U2 13
PU CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS
PI OTTAWA
PA 1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA
SN 0706-652X
EI 1205-7533
J9 CAN J FISH AQUAT SCI
JI Can. J. Fish. Aquat. Sci.
PD NOV
PY 2010
VL 67
IS 11
BP 1782
EP 1790
DI 10.1139/F10-101
PG 9
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 676OG
UT WOS:000283921200007
ER
PT J
AU Williamson, KS
Murdoch, AR
Pearsons, TN
Ward, EJ
Ford, MJ
AF Williamson, Kevin S.
Murdoch, Andrew R.
Pearsons, Todd N.
Ward, Eric J.
Ford, Michael J.
TI Factors influencing the relative fitness of hatchery and wild spring
Chinook salmon (Oncorhynchus tshawytscha) in the Wenatchee River,
Washington, USA
SO CANADIAN JOURNAL OF FISHERIES AND AQUATIC SCIENCES
LA English
DT Article
ID CROSS-SPECIES AMPLIFICATION; STEELHEAD TROUT; REPRODUCTIVE SUCCESS;
MICROSATELLITE LOCI; COLUMBIA-RIVER; PACIFIC SALMON; LIFE-HISTORY;
1ST-GENERATION HATCHERY; PARENTAGE ANALYSIS; SMOLT PRODUCTION
AB Understanding the relative fitness of naturally spawning hatchery fish compared with wild fish has become an important issue in the management and conservation of salmonids. We used a DNA-based parentage analysis to measure the relative reproductive success of hatchery- and natural-origin spring Chinook salmon (Oncorhynchus tshawytscha) in the natural environment. Size and age had a large influence on male fitness, with larger and older males producing more offspring than smaller or younger individuals. Size had a significant effect on female fitness, but the effect was smaller than on male fitness. For both sexes, run time had a smaller but still significant effect on fitness, with earlier returning fish favored. Spawning location within the river had a significant effect on fitness for both sexes. Hatchery-origin fish produced about half the juvenile progeny per parent when spawning naturally than did natural-origin fish. Hatchery fish tended to be younger and return to lower areas of the watershed than wild fish, which explained some of their lower fitness.
C1 [Williamson, Kevin S.; Ward, Eric J.; Ford, Michael J.] NW Fisheries Sci Ctr, Conservat Biol Div, Seattle, WA 98112 USA.
[Murdoch, Andrew R.; Pearsons, Todd N.] Washington Dept Fish & Wildlife, N Olympia, WA 98501 USA.
RP Ford, MJ (reprint author), NW Fisheries Sci Ctr, Conservat Biol Div, 2725 Montlake Blvd E, Seattle, WA 98112 USA.
EM mike.ford@noaa.gov
RI Ford, Michael/K-3147-2012
FU Bonneville Power Administration
FX Linda Park, Eric Iwamoto, and several anonymous reviewers provided
useful comments on earlier drafts of this manuscript, and Ewann Berntson
assisted with data collection. This research was funded by contracts to
M.J.F. and A. R. M from the Bonneville Power Administration.
NR 60
TC 38
Z9 38
U1 2
U2 28
PU CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS
PI OTTAWA
PA 1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA
SN 0706-652X
J9 CAN J FISH AQUAT SCI
JI Can. J. Fish. Aquat. Sci.
PD NOV
PY 2010
VL 67
IS 11
BP 1840
EP 1851
DI 10.1139/F10-099
PG 12
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 676OG
UT WOS:000283921200012
ER
PT J
AU Li, Y
Morrill, C
AF Li, Yu
Morrill, Carrie
TI Multiple factors causing Holocene lake-level change in monsoonal and
arid central Asia as identified by model experiments
SO CLIMATE DYNAMICS
LA English
DT Article
DE Lake level; Holocene; Asian monsoon; CCSM3; Lake evaporation
ID EASTERN INNER-MONGOLIA; NORTH CENTRAL MONGOLIA; CLIMATE SYSTEM MODEL;
HIGH-RESOLUTION; TIBETAN PLATEAU; MOISTURE EVOLUTION; ALASHAN PLATEAU;
TENGGER DESERT; QINGHAI LAKE; BOSTEN LAKE
AB Lake-level records provide a rich resource of information about past changes in effective moisture, but water-balance fluctuations can be driven by a number of different climate variables and it is often difficult to pinpoint their exact cause. This understanding is essential, however, for reconciling divergent paleo-records or for making predictions about future lake-level variations. This research uses a series of models, the NCAR CCSM3, a lake energy-balance and a lake water-balance model, to examine the reasons for lake-level changes in monsoonal Asia and arid central Asia between the early (8.5 ka), middle (6.0 ka) and late (ca. 1800 AD) Holocene. Our results indicate that the components of the lake water balance responsible for lake-level changes varied by region and through time. High lake levels at 8.5 and 6.0 ka in the monsoon region were caused by the combined effects of low lake evaporation and high precipitation. The low lake evaporation resulted from low winter solar radiation and high summer cloud cover. Precipitation associated with the mid-latitude westerlies increased from the early to middle Holocene and maintained high lake levels throughout most of arid central Asia ca. 6 ka. The modeled evolution of lake level in arid central Asia from the mid to late Holocene was spatially heterogeneous, due to different sensitivities of the northern and southern parts of the region to seasonally-changing insolation, particularly regarding the duration of lake ice cover. The model results do not suggest that precipitation and lake evaporation changes compete with one another in forcing lake-level change, as has been hypothesized.
C1 [Li, Yu] Lanzhou Univ, Coll Earth & Environm Sci, Ctr Hydrol Cycle & Water Resources Arid Reg, Lanzhou 730000, Peoples R China.
[Li, Yu; Morrill, Carrie] Univ Colorado, CIRES, Boulder, CO 80309 USA.
[Li, Yu; Morrill, Carrie] NOAA, Paleoclimatol Branch, Natl Climat Data Ctr, Boulder, CO 80305 USA.
RP Li, Y (reprint author), Lanzhou Univ, Coll Earth & Environm Sci, Ctr Hydrol Cycle & Water Resources Arid Reg, Lanzhou 730000, Peoples R China.
EM liyu@lzu.edu.cn
OI Morrill, Carrie/0000-0002-1635-5469
FU China Scholarship Council; National Science Foundation [ARC 0713951]
FX We thank the China Scholarship Council for support (to YL), N.
Rosenbloom for assistance with the 8.5 ka simulation, D. Anderson for
helpful discussions, and two anonymous reviewers for insightful
comments. The simulations were completed at the National Center for
Atmospheric Research, which is supported by the National Science
Foundation. The 8.5 ka simulation was funded in part by NSF grant ARC
0713951 (to CM).
NR 64
TC 30
Z9 38
U1 3
U2 23
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0930-7575
J9 CLIM DYNAM
JI Clim. Dyn.
PD NOV
PY 2010
VL 35
IS 6
BP 1115
EP 1128
DI 10.1007/s00382-010-0861-8
PG 14
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 668VE
UT WOS:000283298900014
ER
PT J
AU Noble, JE
Bunk, DM
Christenson, RH
Cole, KD
He, HJ
Katrukha, AG
Panteghini, M
Porter, RA
Schimmel, H
Tate, JR
Wang, LL
AF Noble, James E.
Bunk, David M.
Christenson, Robert H.
Cole, Kenneth D.
He, Hua-Jun
Katrukha, Alexei G.
Panteghini, Mauro
Porter, Robert A.
Schimmel, Heinz
Tate, Jillian R.
Wang, Lili
CA IFCC Working Grp Standardization T
TI Development of a candidate secondary reference procedure (immunoassay
based measurement procedure of higher metrological order) for cardiac
troponin I: I. Antibody characterization and preliminary validation
SO CLINICAL CHEMISTRY AND LABORATORY MEDICINE
LA English
DT Article
DE antibody specificity; antigen-antibody reactions; candidate reference
procedure; ELISA; reference standards; troponin I
ID ACUTE MYOCARDIAL-INFARCTION; LABORATORY MEDICINE; ASSAYS;
STANDARDIZATION; PERFORMANCE; SYSTEMS; SERUM
AB In this study, the first steps in the development of a secondary reference measurement procedure (RMP) 'higher metrological order measurement procedure' to support the cardiac troponin I (cTnI) standardization initiative is described. The RMP should be used to assign values to serum-based secondary reference materials (RMs) without analytical artifacts causing bias. A multiplexed bead-based assay and sodium dodecyl sulfate polyacrylamide gel electrophoresis (SDS-PAGE) were used to identify the optimum monoclonal antibody pair (clones 560 and 19C7) for the RMP. Using these antibodies, an ELISA-based procedure was developed to accurately measure the main cTnI forms present in blood. The proposed RMP appears to show no bias when tested on samples containing various troponin complexes, phosphorylated and dephosphorylated forms, and heparin. The candidate assay displayed suitable linearity and sensitivity (limit of detection, 0.052 mu g/L) for the measurement of the proposed cTnI secondary RMs. Preliminary comparison data on patient samples with a commercial cTnI assay are also provided to support the suitability of RMP for value assignment to RMs. Full validation and final assessment of the RMP will be performed through transferability and inter-comparison studies. Clin Chem Lab Med 2010;48:1603-10.
C1 [Noble, James E.; Porter, Robert A.] Natl Phys Lab, Analyt Sci Grp, Teddington TW11 0LW, Middx, England.
[Bunk, David M.] Natl Inst Stand & Technol, Chem Sci & Technol Lab, Gaithersburg, MD 20899 USA.
[Christenson, Robert H.] Univ Maryland, Sch Med, Dept Pathol, Baltimore, MD 21201 USA.
[Cole, Kenneth D.; He, Hua-Jun; Wang, Lili] Natl Inst Stand & Technol, Div Biochem Sci, Gaithersburg, MD 20899 USA.
[Katrukha, Alexei G.] HyTest Ltd, Turku, Finland.
[Panteghini, Mauro] Univ Milan, Ctr Metrol Traceabil, Lab Med CIRME, Milan, Italy.
[Schimmel, Heinz] Commiss European Communities, Joint Res Ctr, Inst Reference Mat & Measurements, Geel, Belgium.
[Tate, Jillian R.] Royal Brisbane & Womens Hosp, Dept Chem Pathol, Herston, Qld, Australia.
RP Noble, JE (reprint author), Natl Phys Lab, Analyt Sci Grp, Teddington TW11 0LW, Middx, England.
EM james.noble@npl.co.uk; lili.wang@nist.gov
FU DIUS, UK
FX Research funding: We wish to acknowledge DIUS, UK for funding this
research through the ChemBio Programme (JEN).
NR 18
TC 9
Z9 9
U1 2
U2 5
PU WALTER DE GRUYTER & CO
PI BERLIN
PA GENTHINER STRASSE 13, D-10785 BERLIN, GERMANY
SN 1434-6621
J9 CLIN CHEM LAB MED
JI Clin. Chem. Lab. Med.
PD NOV
PY 2010
VL 48
IS 11
BP 1603
EP 1610
DI 10.1515/CCLM.2010.316
PG 8
WC Medical Laboratory Technology
SC Medical Laboratory Technology
GA 678SP
UT WOS:000284101000009
PM 21062228
ER
PT J
AU Miller, AK
Kappes, MA
Trivelpiece, SG
Trivelpiece, WZ
AF Miller, Aileen K.
Kappes, Michelle A.
Trivelpiece, Susan G.
Trivelpiece, Wayne Z.
TI FORAGING-NICHE SEPARATION OF BREEDING GENTOO AND CHINSTRAP PENGUINS,
SOUTH SHETLAND ISLANDS, ANTARCTICA
SO CONDOR
LA English
DT Article
DE Gentoo Penguin; Chinstrap Penguin; Pygoscelis papua; Pygoscelis
antarctica; niche; foraging ecology
ID KING-GEORGE-ISLAND; PYGOSCELIS-PAPUA; PROVISIONING STRATEGIES; DIVING
BEHAVIOR; ADELIE PENGUINS; ORKNEY ISLANDS; SIGNY ISLAND; URIA-AALGE;
DIET; KRILL
AB The realized niches of closely related species must differ if these species are to co-exist stably. The Gentoo (Pygoscelis papua) and Chinstrap Penguins (P. antarctica) breed concurrently in the Scotia Sea and Antarctic Peninsula regions. To identify species- and site-specific foraging niches, we compared the two species' foraging niches, including diet and foraging locations, at two sites in the South Shetland Islands with contrasting marine habitats. Both species fed primarily on Antarctic krill (Euphausia superba), though fish was also a component of the Gentoo Penguin's diet. Gentoo Penguins foraged closer to shore than did Chinstrap Penguins. Gentoo Penguins foraged during the day, while Chinstrap Penguins foraged throughout the diet cycle, sometimes traveling farther from shore on overnight foraging trips. In most cases, these species-specific foraging patterns were consistent with trends seen elsewhere in the region. However, within each species, site-specific differences in foraging niches were still evident. Overall, we observed that Gentoo Penguins traveled within consistent and limited distances from their colonies, but their diets varied by site in both meal mass and content. Chinstrap Penguins, in contrast, had a uniform diet of krill at both sites but varied the distance from shore and times at which they foraged.
C1 [Miller, Aileen K.; Kappes, Michelle A.; Trivelpiece, Susan G.; Trivelpiece, Wayne Z.] SW Fisheries Sci Ctr, Antarctic Ecosyst Res Div, La Jolla, CA 92037 USA.
RP Miller, AK (reprint author), SW Fisheries Sci Ctr, Antarctic Ecosyst Res Div, 8604 La Jolla Shores Dr, La Jolla, CA 92037 USA.
EM aileenkmiller@yahoo.com
FU U.S. AMLR; NSF's Office of Polar Programs; Pew Charitable Trusts;
Oceanites Foundation
FX We thank all those who assisted in the collection of the diet data over
the 7 years of our study at Cape Shirreff and Admiralty Bay. In
particular, we are grateful to Steve Agius, Matt Becker, Stacey
Buckelew, Terry Carten, Sarah Chisholm, Elaine Leung, Stephan
Kropidlowski, Dave Loomis, Rachael Orben, Mike Polito, Ladi Rektoris,
Iris Saxer, Laina Shill, and Michael Taft, each of whom supervised
portions of the field work for this study. We thank our Chilean
colleagues who assisted us at Cape Shirreff and personnel at the Polish
Academy of Sciences' Arctowski Station for their hospitality and
logistical support during this period. We are grateful to the many
people that assisted us from the Antarctic logistical-support groups of
the U.S. AMLR program and National Science Foundation (NSF). Helpful
comments on earlier drafts of this paper were provided by P. Kappes, A.
Takahashi, and an anonymous reviewer. J. Hinke assisted with figure
preparation. This research was supported by the U.S. AMLR Program,
grants from the NSF's Office of Polar Programs, the Lenfest Ocean
Program of the Pew Charitable Trusts, and the Oceanites Foundation.
NR 47
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PU COOPER ORNITHOLOGICAL SOC
PI LAWRENCE
PA ORNITHOLOGICAL SOC NORTH AMER PO BOX 1897, LAWRENCE, KS 66044-8897 USA
SN 0010-5422
J9 CONDOR
JI Condor
PD NOV
PY 2010
VL 112
IS 4
BP 683
EP 695
DI 10.1525/cond.2010.090221
PG 13
WC Ornithology
SC Zoology
GA 700HD
UT WOS:000285727700007
ER
PT J
AU Gu, LS
Kim, J
Kim, YK
Liu, Y
Dickens, SH
Pashley, DH
Ling, JQ
Tay, FR
AF Gu, Li-sha
Kim, Jongryul
Kim, Young Kyung
Liu, Yan
Dickens, Sabine H.
Pashley, David H.
Ling, Jun-qi
Tay, Franklin R.
TI A chemical phosphorylation-inspired design for Type I collagen
biomimetic remineralization
SO DENTAL MATERIALS
LA English
DT Article
DE Adsorption; Sodium trimetaphosphate; Collagen; Dentin; Intrafibrillar
remineralization
ID DENTIN MATRIX PROTEIN-1; CALCIUM-PHOSPHATE; ELECTRON-MICROSCOPY; MINERAL
INDUCTION; APATITE FORMATION; DEGRADATION; FIBRILS; VITRO; BONE;
COMPONENTS
AB Objectives. Type I collagen alone cannot initiate tissue mineralization. Sodium trimetaphosphate (STMP) is frequently employed as a chemical phosphorylating reagent in the food industry. This study examined the feasibility of using STMP as a functional analog of matrix phosphoproteins for biomimetic remineralization of resin-bonded dentin.
Methods. Equilibrium adsorption and desorption studies of STMP were performed using demineralized dentin powder (DDP). Interaction between STMP and DDP was examined using Fourier transform-infrared spectroscopy. Based on those results, a bio-inspired mineralization scheme was developed for chemical phosphorylation of acid-etched dentin with STMP, followed by infiltration of the STMP-treated collagen matrix with two etch-and-rinse adhesives. Resin-dentin interfaces were remineralized in a Portland cement-simulated body fluid system, with or without the use of polyacrylic acid (PAA) as a dual biomimetic analog. Remineralized resin-dentin interfaces were examined unstained using transmission electron microscopy.
Results. Analysis of saturation binding curves revealed the presence of irreversible phosphate group binding sites on the surface of the DDP. FT-IR provided additional evidence of chemical interaction between STMP and DDP, with increased in the peak intensities of the P=O and P-O-C stretching modes. Those peaks returned to their original intensities after alkaline phosphatase treatment. Evidence of intrafibrillar apatite formation could be seen in incompletely resin-infiltrated, STMP-phosphorylated collagen matrices only when PAA was present in the SBF.
These results reinforce the importance of PAA for sequestration of amorphous calcium phosphate nanoprecursors in the biomimetic remineralization scheme. They also highlight the role of STMP as a templating analog of dentin matrix phosphoproteins for inducing intrafibrillar remineralization of apatite nanocrystals within the collagen matrix of incompletely resin-infiltrated dentin. (c) 2010 Academy of Dental Materials. Published by Elsevier Ltd. All rights reserved.
C1 [Pashley, David H.; Tay, Franklin R.] Med Coll Georgia, Sch Dent, Dept Oral Biol, Augusta, GA 30912 USA.
[Tay, Franklin R.] Med Coll Georgia, Sch Dent, Dept Endodont, Augusta, GA 30912 USA.
[Gu, Li-sha; Ling, Jun-qi] Sun Yat Sen Univ, Dept Operat Dent & Endodont, Guanghua Sch Stomatol, Guangzhou 510080, Guangdong, Peoples R China.
[Kim, Jongryul] Kyung Hee Univ, Sch Dent, Dept Conservat Dent, Seoul, South Korea.
[Kim, Young Kyung] Kyungpook Natl Univ, Sch Dent, Dept Conservat Dent, Taegu, South Korea.
[Liu, Yan] Huazhong Univ Sci & Technol, Tongji Hosp, Tongji Med Coll, Dept Stomatol, Wuhan 430074, Peoples R China.
[Dickens, Sabine H.] NIST, Amer Dent Assoc Hlth Fdn, Paffenbarger Res Ctr, Gaithersburg, MD 20899 USA.
RP Tay, FR (reprint author), Med Coll Georgia, Sch Dent, Dept Oral Biol, Augusta, GA 30912 USA.
EM lingjq@mail.sysu.edu.cn; ftay@mcg.edu
FU National Institute of Dental and Craniofacial Research [R21 DE019213-01]
FX This study was supported by Grant R21 DE019213-01 from the National
Institute of Dental and Craniofacial Research (PI. Franklin R. Tay). We
thank Michelle Barnes for secretarial support.
NR 71
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PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0109-5641
J9 DENT MATER
JI Dent. Mater.
PD NOV
PY 2010
VL 26
IS 11
BP 1077
EP 1089
DI 10.1016/j.dental.2010.07.008
PG 13
WC Dentistry, Oral Surgery & Medicine; Materials Science, Biomaterials
SC Dentistry, Oral Surgery & Medicine; Materials Science
GA 656UX
UT WOS:000282367200007
PM 20688381
ER
PT J
AU Ross, D
AF Ross, David
TI Step width, spacing, and resolution in gradient elution moving boundary
electrophoresis. Part 1. Theory and comparison with zone electrophoresis
SO ELECTROPHORESIS
LA English
DT Article
DE Gradient elution moving boundary electrophoresis; Resolution; Theory
ID CONTACTLESS CONDUCTIVITY-DETECTION; MICROCHIP CAPILLARY-ELECTROPHORESIS;
CHANNEL CURRENT DETECTION; INORGANIC-IONS; DISPERSION; FLOW;
SEPARATIONS; PROTEINS; DEVICES; ANIONS
AB Gradient elution moving boundary electrophoresis (GEMBE) is a recently described technique for electrophoretic separations in short capillaries or microchannels. With GEMBE, the electrophoretic migration of analytes is opposed by a bulk counterflow of separation buffer. The counterflow velocity is varied over the course of a separation so that analytes with different mobilities enter the separation channel at different times and are detected as moving boundary, step-wise increases in the detector response. The resolution of a GEMBE separation is thus dependent on the rate at which the counterflow velocity is varied, and relatively high-resolution separations can be performed with short microfluidic channels or capillaries. In this paper, a theoretical description of GEMBE is presented that can be used for calculation of expected resolution and for optimization of GEMBE separations. A comparison is made with CZE, a conventional electrophoretic separation technique for which the theoretical understanding is mature. The results indicate that the electric field strength and separation channel length are important parameters for both CZE and GEMBE. However, with GEMBE, the counterflow acceleration is also available as a parameter that can be easily adjusted for optimization of the trade-off between resolution and separation time. This allows for optimization of GEMBE separations by making changes only to the software controlling the apparatus rather than to the hardware of the apparatus itself. Further comparison of the theoretical descriptions of GEMBE and CZE indicates that the time required to achieve a desired resolution is equivalent for the two techniques.
C1 Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
RP Ross, D (reprint author), Natl Inst Stand & Technol, 100 Bur Dr, Gaithersburg, MD 20899 USA.
EM david.ross@nist.gov
NR 44
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U1 0
U2 27
PU WILEY-V C H VERLAG GMBH
PI WEINHEIM
PA PO BOX 10 11 61, D-69451 WEINHEIM, GERMANY
SN 0173-0835
J9 ELECTROPHORESIS
JI Electrophoresis
PD NOV
PY 2010
VL 31
IS 22
SI SI
BP 3650
EP 3657
DI 10.1002/elps.201000334
PG 8
WC Biochemical Research Methods; Chemistry, Analytical
SC Biochemistry & Molecular Biology; Chemistry
GA 693LO
UT WOS:000285225800005
PM 21077236
ER
PT J
AU Ross, D
AF Ross, David
TI Step width, spacing, and resolution in gradient elution moving boundary
electrophoresis. Part 2. Results from experiment
SO ELECTROPHORESIS
LA English
DT Article
DE Gradient elution moving boundary electrophoresis; Resolution
ID CHANNEL CURRENT DETECTION
AB In Part 1 of this work, a theoretical description of gradient elution moving boundary electrophoresis (GEMBE) is presented along with a comparison between GEMBE and the more conventional technique of CZE. In this second part, experimental results are presented for comparison with the theoretical predictions of Part 1. Results for the step width, spacing, and resolution are examined as a function of the salient parameters affecting the results of a GEMBE separation (starting pressure, counterflow acceleration, and electric field strength).
C1 Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
RP Ross, D (reprint author), Natl Inst Stand & Technol, 100 Bur Dr, Gaithersburg, MD 20899 USA.
EM david.ross@nist.gov
NR 7
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U1 0
U2 16
PU WILEY-V C H VERLAG GMBH
PI WEINHEIM
PA PO BOX 10 11 61, D-69451 WEINHEIM, GERMANY
SN 0173-0835
J9 ELECTROPHORESIS
JI Electrophoresis
PD NOV
PY 2010
VL 31
IS 22
SI SI
BP 3658
EP 3664
DI 10.1002/elps.201000335
PG 7
WC Biochemical Research Methods; Chemistry, Analytical
SC Biochemistry & Molecular Biology; Chemistry
GA 693LO
UT WOS:000285225800006
PM 21077237
ER
PT J
AU Singer, SF
AF Singer, S. Fred
TI A RESPONSE TO "THE CLIMATE CHANGE DEBATES"
SO ENERGY & ENVIRONMENT
LA English
DT Editorial Material
C1 [Singer, S. Fred] Univ Virginia, Charlottesville, VA 22903 USA.
[Singer, S. Fred] NESDIS NOAA, Camp Springs, MD USA.
[Singer, S. Fred] NIPCC, Chicago, IL USA.
RP Singer, SF (reprint author), Univ Virginia, Charlottesville, VA 22903 USA.
NR 0
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U1 1
U2 3
PU MULTI-SCIENCE PUBL CO LTD
PI BRENTWOOD
PA 5 WATES WAY, BRENTWOOD CM15 9TB, ESSEX, ENGLAND
SN 0958-305X
J9 ENERG ENVIRON-UK
JI Energy Environ.
PD NOV
PY 2010
VL 21
IS 7
BP 847
EP 851
DI 10.1260/0958-305X.21.7.847
PG 5
WC Environmental Studies
SC Environmental Sciences & Ecology
GA 760EK
UT WOS:000290306700008
ER
PT J
AU Baustian, J
Mendelssohn, I
Lin, QX
Rapp, J
AF Baustian, Joseph
Mendelssohn, Irving
Lin, Qianxin
Rapp, John
TI In Situ Burning Restores the Ecological Function and Structure of an
Oil-Impacted Coastal Marsh
SO ENVIRONMENTAL MANAGEMENT
LA English
DT Article
DE In situ burn; Oil spill; Coastal marsh; Louisiana; Functional recovery;
Resilience
ID ALTERNIFLORA SALT-MARSH; CRUDE-OIL; SPARTINA-ALTERNIFLORA; CELLULOSE
DECOMPOSITION; PLANT COMMUNITY; WATER DEPTH; SPILL; VEGETATION;
LOUISIANA; RECOVERY
AB As the use of in situ burning for oil spill remediation in coastal wetlands accelerates, the capacity of this procedure to restore the ecological structure and function of oil-impacted wetlands becomes increasingly important. Thus, our research focused on evaluating the functional and structural recovery of a coastal marsh in South Louisiana to an in situ burn following a Hurricane Katrina-induced oil spill. Permanent sampling plots were set up to monitor marsh recovery in the oiled and burned areas as well as non-oiled and non-burned (reference) marshes. Plots were monitored for species composition, stem density, above- and belowground productivity, marsh resiliency, soil chemistry, soil residual oil, and organic matter decomposition. The burn removed the majority of the oil from the marsh, and structurally the marsh recovered rapidly. Plant biomass and species composition returned to control levels within 9 months; however, species richness remained somewhat lower in the oiled and burned areas compared to the reference areas. Recovery of ecological function was also rapid following the in situ burn. Aboveground and belowground plant productivity recovered within one growing season, and although decomposition rates were initially higher in the oiled areas, over time they became equivalent to those in reference sites. Also, marsh resiliency, i.e., the rate of recovery from our applied disturbances, was not affected by the in situ burn. We conclude that in situ burning is an effective way to remove oil and allow ecosystem recovery in coastal marshes.
C1 [Baustian, Joseph; Mendelssohn, Irving; Lin, Qianxin] Louisiana State Univ, Dept Oceanog & Coastal Sci, Baton Rouge, LA 70803 USA.
[Rapp, John] NOAA, Off Habitat Conservat, Restorat Ctr, Silver Spring, MD USA.
RP Baustian, J (reprint author), Louisiana State Univ, Dept Oceanog & Coastal Sci, Baton Rouge, LA 70803 USA.
EM baustian@lsu.edu
FU Louisiana Sea Grant; Chevron
FX Louisiana Sea Grant, a part of the National Sea Grant College Program,
and the Louisiana Oil Spill Research and Development Program, via a
grant from Chevron, provided funding for this project. Don Davis of the
Louisiana Oil Spill Research & Development Program and Jim Meyers of
Chevron were instrumental in initiating the research following the in
situ burn. Sean Graham, Camille Stagg, Carey Perry, Jane Buck, Will
Estis, and Allison Music aided in sample collection and processing, and
Brandon Edwards performed the elevation survey. Arthur Dillon and Ernie
Petrovich of Chevron Pipe Line Company provided logistical support
throughout the project.
NR 45
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U1 3
U2 37
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0364-152X
J9 ENVIRON MANAGE
JI Environ. Manage.
PD NOV
PY 2010
VL 46
IS 5
BP 781
EP 789
DI 10.1007/s00267-010-9549-4
PG 9
WC Environmental Sciences
SC Environmental Sciences & Ecology
GA 669OO
UT WOS:000283360300011
PM 20821009
ER
PT J
AU Hutchings, JW
Ervens, B
Straub, D
Herckes, P
AF Hutchings, James W.
Ervens, Barbara
Straub, Derek
Herckes, Pierre
TI N-Nitrosodimethylamine Occurrence, Formation and Cycling in Clouds and
Fogs
SO ENVIRONMENTAL SCIENCE & TECHNOLOGY
LA English
DT Article
ID THERMAL-ENERGY ANALYSIS; NITROUS-ACID; AQUEOUS SURFACES; DRINKING-WATER;
AMBIENT AIR; NITROSAMINES; CHEMISTRY; NDMA; DIMETHYLNITROSAMINE;
ATMOSPHERE
AB The occurrence, source, and sink processes of N-nitrosodimethylamine (NDMA) have been explored by means of combined laboratory, field, and model studies. Observations have shown the occurrence of NDMA in fogs and clouds at substantial concentrations (7.5-397 ng L(-1)). Laboratory studies were conducted to investigate the formation of NDMA from nitrous acid and dimethylamine in the homogeneous aqueous phase. While NDMA was produced in the aqueous phase, the low yields (<1%) observed could not explain observational concentrations. Therefore gaseous formation of NDMA with partitioning to droplets likely dominates aqueous NDMA formation. Box-model calculations confirmed the predominant contributions from gas phase formation followed by partitioning into the cloud droplets. Measurements and model calculations showed that while NDMA is eventually photolyzed, it might persist in the atmosphere for hours after sunrise and before sunset since the photolysis in the aqueous phase might be much less efficient than in the gas phase.
C1 [Hutchings, James W.; Herckes, Pierre] Arizona State Univ, Dept Chem & Biochem, Tempe, AZ 85287 USA.
[Ervens, Barbara] Univ Colorado, CIRES, Boulder, CO 80309 USA.
[Ervens, Barbara] NOAA Earth Syst Res Lab, Div Chem Sci, Boulder, CO USA.
[Straub, Derek] Susquehanna Univ, Dept Earth & Environm Sci, Selinsgrove, PA USA.
RP Herckes, P (reprint author), Arizona State Univ, Dept Chem & Biochem, Tempe, AZ 85287 USA.
EM pierre.herckes@asu.edu
RI Herckes, Pierre/E-6824-2011; Ervens, Barbara/D-5495-2013; Manager, CSD
Publications/B-2789-2015
OI Herckes, Pierre/0000-0002-0205-3187; Ervens,
Barbara/0000-0002-6223-1635;
FU NSF [AGS0530718, AGS0847710, AGS0907261]; United States Department of
Energy (BER) [DE-FG02-08ER64539]
FX We are grateful to Youliang Wang and Shawn Ashkan for help during the
Fresno 2010 campaign, to Mann Robinson for her help sampling at Mt.
Elden in Flagstaff, Arizona, and to Jeff Collett and Lynn Mazzoleni for
their help in the Fresno 2006 campaign. We thank Sasha Madronich (NCAR,
Boulder) for help with estimating the NDMA photolysis rate. Funding was
provided to J.W.H. and P.H. by NSF AGS0530718, AGS0847710, and
AGS0907261. BE acknowledges funding from the United States Department of
Energy (BER, ASP Program), Grant DE-FG02-08ER64539.
NR 33
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U1 1
U2 19
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0013-936X
J9 ENVIRON SCI TECHNOL
JI Environ. Sci. Technol.
PD NOV 1
PY 2010
VL 44
IS 21
BP 8128
EP 8133
DI 10.1021/es101698q
PG 6
WC Engineering, Environmental; Environmental Sciences
SC Engineering; Environmental Sciences & Ecology
GA 671EV
UT WOS:000283484000027
PM 20932002
ER
PT J
AU Shibata, T
Solo-Gabriele, HM
Sinigalliano, CD
Gidley, ML
Plano, LRW
Fleisher, JM
Wang, JD
Elmir, SM
He, GQ
Wright, ME
Abdelzaher, AM
Ortega, C
Wanless, D
Garza, AC
Kish, J
Scott, T
Hollenbeck, J
Backer, LC
Fleming, LE
AF Shibata, Tomoyuki
Solo-Gabriele, Helena M.
Sinigalliano, Christopher D.
Gidley, Maribeth L.
Plano, Lisa R. W.
Fleisher, Jay M.
Wang, John D.
Elmir, Samir M.
He, Guoqing
Wright, Mary E.
Abdelzaher, Amir M.
Ortega, Cristina
Wanless, David
Garza, Anna C.
Kish, Jonathan
Scott, Troy
Hollenbeck, Julie
Backer, Lorraine C.
Fleming, Lora E.
TI Evaluation of Conventional and Alternative Monitoring Methods for a
Recreational Marine Beach with Nonpoint Source of Fecal Contamination
SO ENVIRONMENTAL SCIENCE & TECHNOLOGY
LA English
DT Article
ID ESCHERICHIA-COLI CONCENTRATIONS; SOUTHERN LAKE-MICHIGAN; 16S
RIBOSOMAL-RNA; WATER-QUALITY; SOURCE IDENTIFICATION; MICROBIAL
INDICATORS; BACTERIA; URBAN; BACTEROIDALES; ENTEROCOCCI
AB The objectives of this work were to compare enterococci (ENT) measurements based on the membrane filter, ENT(MF) with alternatives that can provide faster results including alternative enterococci methods (e.g., chromogenic substrate (CS), and quantitative polymerase chain reaction (qPCR)), and results from regression models based upon environmental parameters that can be measured in real-time. ENT(MF) were also compared to source tracking markers (Staphylococcus aureus, Bacteroidales human and dog markers, and Catellicoccus gull marker) in an effort to interpret the variability of the signal. Results showed that concentrations of enterococci based upon MF (<2 to 3320 CFU/100 mL) were significantly different from the CS and qPCR methods (p < 0.01). The correlations between MF and CS (r = 0.58, p < 0.01) were stronger than between MF and qPCR (r <= 0.36, p < 0.01). Enterococci levels by MF, CS, and qPCR methods were positively correlated with turbidity and tidal height Enterococci by MF and CS were also inversely correlated with solar radiation but enterococci by qPCR was not. The regression model based on environmental variables provided fair qualitative predictions of enterococci by ME in real-time, for daily geometric mean levels, but not for individual samples. Overall, ENT(ME) was not significantly correlated with source tracking markers with the exception of samples collected during one storm event. The inability of the regression model to predict ENT(MF) levels for individual samples is likely due to the different sources of ENT impacting the beach at any given time, making it particularly difficult to to predict short-term variability of ENT(MF) for environmental parameters.
C1 [Shibata, Tomoyuki] No Illinois Univ, Sch Nursing & Hlth Studies, De Kalb, IL 60115 USA.
[Shibata, Tomoyuki; Solo-Gabriele, Helena M.; Sinigalliano, Christopher D.; Gidley, Maribeth L.; Plano, Lisa R. W.; Fleisher, Jay M.; Wang, John D.; Elmir, Samir M.; He, Guoqing; Wright, Mary E.; Abdelzaher, Amir M.; Ortega, Cristina; Wanless, David; Garza, Anna C.; Kish, Jonathan; Hollenbeck, Julie; Fleming, Lora E.] Univ Miami, NSF, NIEHS, Oceans & Human Hlth Ctr,Rosenstiel Sch, Miami, FL USA.
[Shibata, Tomoyuki; Sinigalliano, Christopher D.; Gidley, Maribeth L.] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
[Fleisher, Jay M.] Nova SE Univ, Ft Lauderdale, FL 33314 USA.
[Solo-Gabriele, Helena M.; Wright, Mary E.; Abdelzaher, Amir M.; Ortega, Cristina] Univ Miami, Coll Engn, Coral Gables, FL 33124 USA.
[Plano, Lisa R. W.; Garza, Anna C.; Kish, Jonathan; Fleming, Lora E.] Univ Miami, Miller Sch Med, Miami, FL 33136 USA.
[Elmir, Samir M.] Miami Dade Cty Publ Hlth Dept, Miami, FL USA.
[Scott, Troy] BCS Labs, Miami, FL USA.
[Gidley, Maribeth L.; Wanless, David] Univ Miami, Cooperat Inst Marine & Atmospher Studies, Miami, FL USA.
[Backer, Lorraine C.] Ctr Dis Control & Prevent, Natl Ctr Environm Hlth, Chamblee, GA USA.
RP Shibata, T (reprint author), No Illinois Univ, Sch Nursing & Hlth Studies, Wirtz Hall 2091, De Kalb, IL 60115 USA.
EM tshibata@niu.edu
RI Sinigalliano, Christopher/A-8760-2014; gidley, maribeth/B-8335-2014;
OI Sinigalliano, Christopher/0000-0002-9942-238X; gidley,
maribeth/0000-0001-9583-8073; Fleisher, Jay/0000-0002-2553-2201
FU Centers for Disease Control and Prevention; Florida Department of Health
through Florida Department of Environmental Protection; Environmental
Protection Agency Internship Program; National Science Foundation (NSF);
National Institute of Environmental Health Sciences (NIEHS) Oceans and
Human Health Center at the University of Miami [NSF 0CE0432368/0911373,
NIEHS P50 ES12736]; NSF REU in Oceans and Human Health; NSF SGER [NSF
SGER 0743987]; Northern Gulf Institute, a NOAA Cooperative Institute
[NA06OAR4320264]
FX Funding was received from the Centers for Disease Control and
Prevention; Florida Department of Health through monies from the Florida
Department of Environmental Protection; the Environmental Protection
Agency Internship Program; the National Science Foundation (NSF) and the
National Institute of Environmental Health Sciences (NIEHS) Oceans and
Human Health Center at the University of Miami [NSF 0CE0432368/0911373]
and [NIEHS P50 ES12736] and NSF REU in Oceans and Human Health, and the
NSF SGER (NSF SGER 0743987) in Oceans and Human Health. Development of
the dog-host-specific Bacteroides and gull-host-specific Catellicoccus
qPCR assays were funded in part by the Northern Gulf Institute, a NOAA
Cooperative Institute (U.S. Department of Commerce award
NA06OAR4320264). We would also like to thank IDEXX Corporation for the
provision of supplies for the CS method. This study is dedicated to the
memory of Ms. Seana Campbell, a very talented, hardworking and creative
young researcher who died too young.
NR 36
TC 29
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U1 3
U2 28
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0013-936X
J9 ENVIRON SCI TECHNOL
JI Environ. Sci. Technol.
PD NOV 1
PY 2010
VL 44
IS 21
BP 8175
EP 8181
DI 10.1021/es100884w
PG 7
WC Engineering, Environmental; Environmental Sciences
SC Engineering; Environmental Sciences & Ecology
GA 671EV
UT WOS:000283484000035
PM 20925349
ER
PT J
AU Dillon, T
Beckvar, N
Kern, J
AF Dillon, Tom
Beckvar, Nancy
Kern, John
TI RESIDUE-BASED MERCURY DOSE-RESPONSE IN FISH: AN ANALYSIS USING
LETHALITY-EQUIVALENT TEST ENDPOINTS
SO ENVIRONMENTAL TOXICOLOGY AND CHEMISTRY
LA English
DT Article
DE Fish; Mercury; Injury; Dose-response; Residue-effects
ID WALLEYE STIZOSTEDION-VITREUM; MINNOWS PIMEPHALES-PROMELAS; DIETARY
METHYLMERCURY; FATHEAD MINNOWS; FUNDULUS-HETEROCLITUS; FRESH-WATER;
TOXICITY; BEHAVIOR; BIOACCUMULATION; SENSITIVITY
AB Dose-response relationships for aquatic organisms have been developed for numerous contaminants using external media exposures (water and sediment). Dose-response relationships based on internal concentrations (tissue residues) are limited The present study reports Hg dose response curves for early life stage and juvenile or adult fish based on published tissue-residue toxicity studies These curves rely primarily on endpoints that can be directly related to mortality, such as survival, reproductive success. and lethal developmental abnormalities These lethality-equivalent-endpoints were linked using the common metric of injury. Uncertainties and potential applications of this mercury close response curve are discussed Major uncertainties include lab to field extrapolations. biological endpoints selected by investigators. Iraqi-specific extrapolations, and the paucity of published early life stage residue (close) response information To the extent this curve is based exclusively on laboratory toxicity tests and does not consider other potentially sensitive and ecologically important biological endpoints (e.g., growth and behavior), the magnitude of the adverse effects predicted by the curve may be underestimated Environ Toxicol, Chem, 2010,29 2559-2565. (C) 2010 SETAC
C1 [Dillon, Tom] US EPA Superfund, Off Response & Restorat, NOAA, Atlanta, GA 30303 USA.
[Beckvar, Nancy] NOAA, Off Response & Restorat, Seattle, WA 98115 USA.
[Kern, John] Kern Stat Serv, Sauk Rapids, MN 56379 USA.
RP Dillon, T (reprint author), US EPA Superfund, Off Response & Restorat, NOAA, 61 Forsyth St, Atlanta, GA 30303 USA.
EM dillon@noaa.gov
FU National Oceanic and Atmospheric Administration; University of New
Hampshire's Coastal Response Research Center
FX This work was funded by National Oceanic and Atmospheric Administration
and the University of New Hampshire's Coastal Response Research Center
We thank Jay Field and Greg Baker for their review and insightful
comments on the manuscript We also thank two anonymous reviewers who
provided valuable and constructive feedback that improved the quality of
this article
NR 40
TC 19
Z9 19
U1 1
U2 25
PU SETAC PRESS
PI PENSACOLA
PA 1010 N 12TH AVE, PENSACOLA, FL 32501-3367 USA
SN 0730-7268
J9 ENVIRON TOXICOL CHEM
JI Environ. Toxicol. Chem.
PD NOV
PY 2010
VL 29
IS 11
BP 2559
EP 2565
DI 10.1002/etc.314
PG 7
WC Environmental Sciences; Toxicology
SC Environmental Sciences & Ecology; Toxicology
GA 673DP
UT WOS:000283639500022
PM 20886502
ER
PT J
AU Beyer, J
Jonsson, G
Porte, C
Krahn, MM
Ariese, F
AF Beyer, Jonny
Jonsson, Grete
Porte, Cinta
Krahn, Margaret M.
Ariese, Freek
TI Analytical methods for determining metabolites of polycyclic aromatic
hydrocarbon (PAH) pollutants in fish bile: A review
SO ENVIRONMENTAL TOXICOLOGY AND PHARMACOLOGY
LA English
DT Review
DE PAH pollution; Fish; Environmental monitoring; Bile metabolites;
Biomarkers of exposure
ID FIXED-WAVELENGTH FLUORESCENCE; FLOUNDER PLATICHTHYS-FLESUS;
CHROMATOGRAPHY-MASS-SPECTROMETRY; PERFORMANCE LIQUID-CHROMATOGRAPHY;
TROUT ONCORHYNCHUS-MYKISS; COD GADUS-MORHUA; SOLE PAROPHRYS-VETULUS;
PRESSURE CHEMICAL-IONIZATION; TURBOT SCOPHTHALMUS-MAXIMUS;
GLUTATHIONE-S-TRANSFERASE
AB The determination of polycyclic aromatic hydrocarbon (PAH) metabolites in bile can serve as a tool for assessing environmental PAH exposure in fish. Biliary PAH metabolite levels can be measured using several analytical methods, including simple fluorescence assays (fixed fluorescence detection or synchronous fluorescence spectrometry); high-performance liquid chromatography with fluorescence detection (HPLC-F); gas chromatography-mass spectrometry (GC-MS) after deconjugation, extraction and derivatization of the bile sample, and finally by advanced liquid chromatography-tandem mass spectrometry (LC-MS/MS) and gas chromatography-tandem mass spectrometry (GC-MS/MS) methods. The method alternatives are highly different both with regard to their analytical performance towards different PAH metabolite structures as well as in general technical demands and their suitability for different monitoring strategies. In the present review, the state-of-the-art for these different analytical methods is presented and the advantages and limitations of each approach as well as aspects related to analytical quality control and inter-laboratory comparability of data and availability of certified reference materials are discussed. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Beyer, Jonny] IRIS, N-4068 Stavanger, Norway.
[Beyer, Jonny] Univ Stavanger, N-4036 Stavanger, Norway.
[Jonsson, Grete] Stavanger Univ Hosp, N-4068 Stavanger, Norway.
[Porte, Cinta] CSIC, Environm Chem Dept IDAEA, ES-08034 Barcelona, Spain.
[Krahn, Margaret M.] NOAA Fisheries, NW Fisheries Sci Ctr, Natori, Miyagi 98112, Japan.
[Ariese, Freek] Vrije Univ Amsterdam, NL-1081 HV Amsterdam, Netherlands.
RP Beyer, J (reprint author), IRIS, N-4068 Stavanger, Norway.
EM jb@iris.no; gina.ylitalo@noaa.gov
RI Beyer, Jonny/E-8001-2011; Porte, Cinta/L-3191-2014;
OI Porte, Cinta/0000-0002-3940-6409; Ariese, Freek/0000-0002-8756-7223
FU EU [SMT4-CT98-2250]; Norwegian Research Council [653879, 152449/720,
153898/S40]; Total E&P Norge AS (TCP project)
FX Financial support for different parts of the current work was provided
by the EU - Standards, Measurements and Testing program (contract
SMT4-CT98-2250), the Norwegian Research Council (projects 653879,
152449/720 and 153898/S40) and Total E&P Norge AS (TCP project). M.O.
Sydnes (IRIS), G. Ylitalo and J. Stein (NOAA) are acknowledged for their
valuable critical comments on the manuscript.
NR 207
TC 90
Z9 98
U1 8
U2 132
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1382-6689
J9 ENVIRON TOXICOL PHAR
JI Environ. Toxicol. Pharmacol.
PD NOV
PY 2010
VL 30
IS 3
BP 224
EP 244
DI 10.1016/j.etap.2010.08.004
PG 21
WC Environmental Sciences; Pharmacology & Pharmacy; Toxicology
SC Environmental Sciences & Ecology; Pharmacology & Pharmacy; Toxicology
GA 677AJ
UT WOS:000283961200002
PM 21787655
ER
PT J
AU Williams, MR
Filoso, S
Longstaff, BJ
Dennison, WC
AF Williams, Michael R.
Filoso, Solange
Longstaff, Benjamin J.
Dennison, William C.
TI Long-Term Trends of Water Quality and Biotic Metrics in Chesapeake Bay:
1986 to 2008
SO ESTUARIES AND COASTS
LA English
DT Article
DE Biotic; Chesapeake Bay; Eutrophication; Health indices; Water quality
ID PATUXENT RIVER ESTUARY; COASTAL EUTROPHICATION; AQUATIC VEGETATION;
CONSTITUENT LOADS; TIDAL TRIBUTARIES; BENTHIC INDEX; HUDSON RIVER; TAMPA
BAY; PHYTOPLANKTON; INTEGRITY
AB We analyzed trends in a 23-year period of water quality and biotic data for Chesapeake Bay. Indicators were used to detect trends of improving and worsening environmental health in 15 regions and 70 segments of the bay and to assess the estuarine ecosystem's responses to reduced nutrient loading from point (i.e., sewage treatment facilities) and non-point (e.g., agricultural and urban land use) sources. Despite extensive restoration efforts, ecological health-related water quality (chlorophyll-a, dissolved oxygen, Secchi depth) and biotic (phytoplankton and benthic indices) metrics evaluated herein have generally shown little improvement (submerged aquatic vegetation was an exception), and water clarity and chlorophyll-a have considerably worsened since 1986. Nutrient and sediment inputs from higher-than-average annual flows after 1992 combined with those from highly developed Coastal Plain areas and compromised ecosystem resiliency are important factors responsible for worsening chlorophyll-a and Secchi depth trends in mesohaline and polyhaline zones from 1986 to 2008.
C1 [Williams, Michael R.; Dennison, William C.] Univ Maryland, Annapolis Synth Ctr, Ctr Environm Sci, Annapolis, MD 21401 USA.
[Filoso, Solange] Univ Maryland, Ctr Environm Sci, Chesapeake Biol Lab, Solomons, MD 20688 USA.
[Longstaff, Benjamin J.] NOAA UMCES Partnership, Cooperat Oxford Lab, Oxford, MD 21654 USA.
RP Williams, MR (reprint author), Univ Maryland, Annapolis Synth Ctr, Ctr Environm Sci, Suite 301, Annapolis, MD 21401 USA.
EM mwilliams@umces.edu; filoso@cbl.umces.edu
RI Dennison, William/D-7739-2012; Filoso, Solange/G-4461-2015; feng,
yongzhong/F-5090-2012
OI feng, yongzhong/0000-0002-5202-4368
NR 57
TC 24
Z9 24
U1 2
U2 37
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1559-2723
J9 ESTUAR COAST
JI Estuaries Coasts
PD NOV
PY 2010
VL 33
IS 6
BP 1279
EP 1299
DI 10.1007/s12237-010-9333-y
PG 21
WC Environmental Sciences; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 658SZ
UT WOS:000282511000003
ER
PT J
AU McKinney, RA
Oczkowski, AJ
Prezioso, J
Hyde, KJW
AF McKinney, R. A.
Oczkowski, A. J.
Prezioso, J.
Hyde, K. J. W.
TI Spatial variability of nitrogen isotope ratios of particulate material
from Northwest Atlantic continental shelf waters
SO ESTUARINE COASTAL AND SHELF SCIENCE
LA English
DT Article
DE nitrogen; stable isotope; continental shelf; particulate material;
estuary; chlorophyll-a
ID STABLE-ISOTOPE; COASTAL WATERS; ATMOSPHERIC NITROGEN; ORGANIC-MATTER;
UNITED-STATES; FOOD-WEB; NITRATE; OCEAN; PHYTOPLANKTON; ECOSYSTEMS
AB Human encroachment on the coastal zone has led to concern about the impact of anthropogenic nitrogen (N) on estuarine and continental shelf waters. Western North Atlantic watershed budgets suggest that the export of human-derived N from estuaries to shelf waters off the east coast of the US may be significant: however, models based on water inputs and estimates of upwelling of deepwater nutrients to surface waters of the mid-Atlantic bight indicate that estuarine N may be a relatively minor component of the overall shelf N budget. Stable N isotope ratios could provide a means to assess the relative input of anthropogenic N to shelf waters, particularly since dissolved N from human sources has elevated delta(15)N values (range: 7-30 parts per thousand). We collected particulate material from surface shelf waters off the US east coast from 2000 to 2005 at near-shore sample sites proximal to the mouth of six estuaries and corresponding sites farther offshore. Near-shore (mean 33.7 km from estuary mouth) delta(15)N values ranged from 5.5 to 7.7 parts per thousand, Offshore values (mean 92.4 km from estuary mouth) were consistently lower than near-shore sites (average 4.7 +/- 1.0 parts per thousand versus 6.8 +/- 1.1 parts per thousand)(,) suggesting different N sources to near and offshore stations. Near-shore regions are often more productive, as mean monthly chlorophyll-a concentrations from the sea-viewing wide field-of-view sensor (SeaWiFS) were significantly higher at near-shore sites near the mouth of three of the six estuaries. A mass balance using a concentration-dependent mixing model with chlorophyll-a concentrations as a surrogate for dissolved inorganic nitrogen can account for all of the nitrogen at near-shore sites south of Cape Cod with estuarine nitrogen estimated to contribute 45-85% of the nitrogen to the near-shore surface particulate material. Our results support the hypothesis that estuarine nitrogen is influencing continental shelf ecosystems, and also provide preliminary evidence of the spatial extent of its influence on shelf waters in the mid-Atlantic bight. Published by Elsevier Ltd.
C1 [McKinney, R. A.; Oczkowski, A. J.] USA, US EPA, Off Res & Dev, Natl Hlth & Environm Effects Res Lab,Atlantic Eco, Narragansett, RI 02882 USA.
[Prezioso, J.; Hyde, K. J. W.] NOAA, Natl Marine Fisheries Serv, NE Fisheries Sci Ctr, Narragansett Lab, Narragansett, RI 02882 USA.
RP McKinney, RA (reprint author), USA, US EPA, Off Res & Dev, Natl Hlth & Environm Effects Res Lab,Atlantic Eco, 27 Tarzwell Dr, Narragansett, RI 02882 USA.
EM mckinney.rick@epa.gov
OI Oczkowski, Autumn/0000-0002-2421-0956
FU U.S. Environmental Protection Agency
FX We thank Joe Kane for assistance with sample collection and data
analysis. Also many thanks to John O'Reilly for providing chlorophyll-a
data and Teresa Ducas for help with data processing. We are grateful to
Scott Nixon, Richard Pruell and Mark Cantwell for their critical review
and helpful comments that greatly improved the manuscript. Mention of
trade names or commercial products does not constitute endorsement or
recommendation. Although the research described in this article has been
funded wholly by the U.S. Environmental Protection Agency, it has not
been subjected to Agency-level review. Therefore, it does not
necessarily reflect the views of the Agency. This is the Office of
Research and Development, National Health and Environmental Effects
Research Laboratory, Atlantic Ecology Division contribution number
AED-08-083.
NR 57
TC 9
Z9 9
U1 3
U2 16
PU ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
PI LONDON
PA 24-28 OVAL RD, LONDON NW1 7DX, ENGLAND
SN 0272-7714
J9 ESTUAR COAST SHELF S
JI Estuar. Coast. Shelf Sci.
PD NOV 1
PY 2010
VL 89
IS 4
BP 287
EP 293
DI 10.1016/j.ecss.2010.08.004
PG 7
WC Marine & Freshwater Biology; Oceanography
SC Marine & Freshwater Biology; Oceanography
GA 664ZF
UT WOS:000283002100005
ER
PT J
AU Fullerton, AH
Burnett, KM
Steel, EA
Flitcroft, RL
Pess, GR
Feist, BE
Torgersen, CE
Miller, DJ
Sanderson, BL
AF Fullerton, A. H.
Burnett, K. M.
Steel, E. A.
Flitcroft, R. L.
Pess, G. R.
Feist, B. E.
Torgersen, C. E.
Miller, D. J.
Sanderson, B. L.
TI Hydrological connectivity for riverine fish: measurement challenges and
research opportunities
SO FRESHWATER BIOLOGY
LA English
DT Review
DE migratory fish; movement barriers; river network; spatial structure
ID PSEUDOMUGIL-SIGNIFER PSEUDOMUGILIDAE; COASTAL CUTTHROAT TROUT; 2 LOWLAND
RIVERS; LANDSCAPE ECOLOGY; POPULATION-DYNAMICS; SPATIAL VARIATION;
SPECIES RICHNESS; EXTINCTION RISK; BULL TROUT; HABITAT FRAGMENTATION
AB P>1. In this review, we first summarize how hydrologic connectivity has been studied for riverine fish capable of moving long distances, and then identify research opportunities that have clear conservation significance. Migratory species, such as anadromous salmonids, are good model organisms for understanding ecological connectivity in rivers because the spatial scale over which movements occur among freshwater habitats is large enough to be easily observed with available techniques; they are often economically or culturally valuable with habitats that can be easily fragmented by human activities; and they integrate landscape conditions from multiple surrounding catchment(s) with in-river conditions. Studies have focussed on three themes: (i) relatively stable connections (connections controlled by processes that act over broad spatio-temporal scales > 1000 km2 and > 100 years); (ii) dynamic connections (connections controlled by processes acting over fine to moderate spatio-temporal scales similar to 1-1000 km2 and < 1-100 years); and (iii) anthropogenic influences on hydrologic connectivity, including actions that disrupt or enhance natural connections experienced by fish.
2. We outline eight challenges to understanding the role of connectivity in riverine fish ecology, organized under three foci: (i) addressing the constraints of river structure; (ii) embracing temporal complexity in hydrologic connectivity; and (iii) managing connectivity for riverine fishes. Challenges include the spatial structure of stream networks, the force and direction of flow, scale-dependence of connectivity, shifting boundaries, complexity of behaviour and life histories and quantifying anthropogenic influence on connectivity and aligning management goals. As we discuss each challenge, we summarize relevant approaches in the literature and provide additional suggestions for improving research and management of connectivity for riverine fishes.
3. Specifically, we suggest that rapid advances are possible in the following arenas: (i) incorporating network structure and river discharge into analyses; (ii) increasing explicit consideration of temporal complexity and fish behaviour in the scope of analyses; and (iii) parsing degrees of human and natural influences on connectivity and defining acceptable alterations. Multiscale analyses are most likely to identify dominant patterns of connections and disconnections, and the appropriate scale at which to focus conservation activities.
C1 [Fullerton, A. H.; Pess, G. R.; Feist, B. E.; Sanderson, B. L.] NOAA NW Fisheries Sci Ctr, Seattle, WA USA.
[Burnett, K. M.; Flitcroft, R. L.] USDA Forest Serv, Corvallis, OR USA.
[Burnett, K. M.; Flitcroft, R. L.] Oregon State Univ, Corvallis, OR 97331 USA.
[Steel, E. A.] USDA Forest Serv, Pacific NW Res Stn, Olympia, WA USA.
[Torgersen, C. E.] USGS Forest & Rangeland Ecosyst Sci Ctr, Cascadia Field Stn, Seattle, WA USA.
[Miller, D. J.] Earth Syst Inst, Seattle, WA USA.
RP Fullerton, AH (reprint author), NOAA NW Fisheries Sci Ctr, 2725 Montlake Blvd E, Seattle, WA USA.
EM aimee.fullerton@noaa.gov
OI Feist, Blake/0000-0001-5215-4878
FU Northwest Fisheries Science Center
FX We thank Peter Kiffney, Belinda Robson, Phil Roni and two anonymous
referees for critical reviews of the manuscript, and Kathryn Ronnenberg
for help with Fig. 2 and technical review. Funding for this work was
provided to AHF by the Northwest Fisheries Science Center's Internal
Grants Program. Any use of trade, product, or firm names is for
descriptive purposes only and does not imply endorsement by the U.S.
Government.
NR 212
TC 91
Z9 94
U1 11
U2 138
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0046-5070
J9 FRESHWATER BIOL
JI Freshw. Biol.
PD NOV
PY 2010
VL 55
IS 11
BP 2215
EP 2237
DI 10.1111/j.1365-2427.2010.02448.x
PG 23
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA 661BU
UT WOS:000282698800001
ER
PT J
AU Macneale, KH
Kiffney, PM
Scholz, NL
AF Macneale, Kate H.
Kiffney, Peter M.
Scholz, Nathaniel L.
TI Pesticides, aquatic food webs, and the conservation of Pacific salmon
SO FRONTIERS IN ECOLOGY AND THE ENVIRONMENT
LA English
DT Review
ID RISK-ASSESSMENT; CHINOOK SALMON; ONCORHYNCHUS-TSHAWYTSCHA; HABITAT
RESTORATION; CLIMATE-CHANGE; FISH-HABITAT; STREAMS; INSECTICIDE;
CHALLENGES; TOXICITY
AB Pesticides pose complex threats to the biological integrity of aquatic ecosystems. In the western US, pesticides have contaminated many surface waters that provide habitat for endangered salmon. These iconic species depend on the productivity of rivers, lakes, and estuaries to provide food for juvenile growth, a key determinant of subsequent marine survival. Despite extensive societal investments in salmon habitat restoration in recent years, the role of pesticides as a limiting factor for salmon recovery has received little attention. Pesticides can be toxic to primary producers and macroinvertebrates, thereby limiting salmon population recovery through adverse, bottom-up impacts on aquatic food webs. The integration of toxicology, environmental chemistry, population biology, community ecology, landscape ecology, conservation biology, and environmental policy is needed to better understand these indirect effects of pesticides on endangered species. We highlight key information gaps and discuss how future research on pesticides and food webs can most effectively guide the long-term conservation of imperiled fish species.
C1 [Macneale, Kate H.; Kiffney, Peter M.; Scholz, Nathaniel L.] NOAA Fisheries, NW Fisheries Sci Ctr, Ecotoxicol & Environm Fish Hlth Program, Seattle, WA USA.
RP Scholz, NL (reprint author), NOAA Fisheries, NW Fisheries Sci Ctr, Ecotoxicol & Environm Fish Hlth Program, Seattle, WA USA.
EM Nathaniel.Scholz@noaa.gov
RI Scholz, Nathaniel/L-1642-2013
OI Scholz, Nathaniel/0000-0001-6207-0272
NR 50
TC 27
Z9 29
U1 4
U2 70
PU ECOLOGICAL SOC AMER
PI WASHINGTON
PA 1990 M STREET NW, STE 700, WASHINGTON, DC 20036 USA
SN 1540-9295
J9 FRONT ECOL ENVIRON
JI Front. Ecol. Environ.
PD NOV
PY 2010
VL 8
IS 9
BP 475
EP 482
DI 10.1890/090142
PG 8
WC Ecology; Environmental Sciences
SC Environmental Sciences & Ecology
GA 679KG
UT WOS:000284159700018
ER
PT J
AU Schiel, J
Au, J
Phinney, K
AF Schiel, John
Au, Jennifer
Phinney, Karen
TI Pronase Digestion and Mass Spectrometry-Based Characterization of
Biopharmaceutical Glycosylation
SO GLYCOBIOLOGY
LA English
DT Meeting Abstract
CT Annual Conference of the Society-for-Glycobiology
CY NOV 07-10, 2010
CL St. Pete Beach, FL
SP Soc Glycobiol
C1 [Schiel, John; Au, Jennifer; Phinney, Karen] NIST, Gaithersburg, MD 20899 USA.
NR 0
TC 0
Z9 0
U1 0
U2 2
PU OXFORD UNIV PRESS INC
PI CARY
PA JOURNALS DEPT, 2001 EVANS RD, CARY, NC 27513 USA
SN 0959-6658
J9 GLYCOBIOLOGY
JI Glycobiology
PD NOV
PY 2010
VL 20
IS 11
MA 106
BP 1482
EP 1483
PG 2
WC Biochemistry & Molecular Biology
SC Biochemistry & Molecular Biology
GA 661TF
UT WOS:000282750300116
ER
PT J
AU Del Rio, R
Bargu, S
Baltz, D
Fire, S
Peterson, G
Wang, ZH
AF Del Rio, Ross
Bargu, Sibel
Baltz, Donald
Fire, Spencer
Peterson, Gary
Wang, Zhihong
TI Gulf menhaden (Brevoortia patronus): A potential vector of domoic acid
in coastal Louisiana food webs
SO HARMFUL ALGAE
LA English
DT Article
DE Pseudo-nitzschia; Domoic acid; Gulf menhaden; Brevoortia patronus;
Louisiana; Gulf of Mexico
ID DOLPHINS TURSIOPS-TRUNCATUS; DIATOM PSEUDO-NITZSCHIA;
PRINCE-EDWARD-ISLAND; OF-MEXICO; TYRANNUS PISCES; SEA LIONS; SHARK;
BACILLARIOPHYCEAE; BAY; PSEUDODELICATISSIMA
AB Harmful algal blooms are an increasing problem for coastal waters world-wide. The presence of the toxigenic diatom genus Pseudo-nitzschia is of concern in the Gulf of Mexico, due to the potential for several species in this genus to produce the neurotoxin domoic acid (DA). Louisiana coastal waters are of particular interest due to the presence of both toxin-producing species of Pseudo-nitzschia and abundant potential vectors. While trophic transfer of DA to consumers has repeatedly occurred along the California coast, little is known about trophic transfer of recently detected DA in the Gulf of Mexico. In this study, the presence of DA was investigated in filter-feeding gulf menhaden (Brevoortia patronus) and in seawater where high abundances of these fish reside. Pseudo-nitzschia presence and enumeration was determined using light microscopy, species identification in seawater and gulf menhaden gut contents was conducted with transmission electron microscopy (TEM), and DA quantification in corresponding seawater and tissue samples was determined by competitive enzyme-linked immunosorbent assay (cELISA). Examination of the phytoplankton revealed the presence of four species of Pseudo-nitzschia: P. calliantha for the first time, P. pseudodelicatissima, P. pungens, and P. americana, with P. calliantha as the dominant Pseudo-nitzschia species. Low levels of DA were detected in both seawater and fish samples, with a significant correlation between the two (n = 22, p = 0.043). Thus, for the first time in the Gulf of Mexico, a potential vector of DA has been identified, revealing the possibility of DA contamination in coastal Louisiana food webs. Published by Elsevier B.V.
C1 [Del Rio, Ross; Bargu, Sibel; Baltz, Donald; Peterson, Gary] Louisiana State Univ, Dept Oceanog & Coastal Sci, Sch Coast & Environm, Baton Rouge, LA 70803 USA.
[Fire, Spencer; Wang, Zhihong] NOAA NOS Ctr Coastal Environm Hlth & Biomol Res, Marine Biotoxins Program, Charleston, SC 29412 USA.
RP Bargu, S (reprint author), Louisiana State Univ, Dept Oceanog & Coastal Sci, Sch Coast & Environm, 1235 Energy,Coast & Environm Bldg, Baton Rouge, LA 70803 USA.
EM sbargu@lsu.edu
RI Baltz, Donald/A-9374-2009; Fire, Spencer/P-6040-2014
OI Fire, Spencer/0000-0002-1657-790X
FU Louisiana Board of Regents [LEQSF (2007-10)-RD-A-02]; Louisiana State
University Department of Oceanography and Coastal Sciences
FX This study was funded by the Louisiana Board of Regents under award
number LEQSF (2007-10)-RD-A-02 to Sibel Bargu and the Louisiana State
University Department of Oceanography and Coastal Sciences. We would
like to thank Dr. Cindy Henk for her help with the TEM, and Dr. Gregory
Stone for granting access to WAVCIS data and its interpretation.
Finally, we would also like to thank Brian Milan, Elin Sandy, Jessica
Czubakowski, Dr. Kari Galvan, Ana Cristina Garcia, and Benjamin Von
Korff for their assistance either in the field or lab.[SS]
NR 51
TC 17
Z9 17
U1 2
U2 10
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1568-9883
J9 HARMFUL ALGAE
JI Harmful Algae
PD NOV
PY 2010
VL 10
IS 1
BP 19
EP 29
DI 10.1016/j.hal.2010.05.006
PG 11
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA 677CC
UT WOS:000283965700003
ER
PT J
AU Rensel, JEJ
Haigh, N
Tynan, TJ
AF Rensel, J. E. Jack
Haigh, Nicola
Tynan, Tim J.
TI Fraser river sockeye salmon marine survival decline and harmful blooms
of Heterosigrna akashiwo
SO HARMFUL ALGAE
LA English
DT Article
DE British Columbia; Fish mortality; Fraser River; Heterosigma akashiwo;
Puget Sound; Sockeye salmon; Strait of Georgia
ID ONCORHYNCHUS-NERKA SMOLTS; DE-FUCA STRAIT; BRITISH-COLUMBIA; RED-TIDE;
ALGAL BLOOMS; PACIFIC SALMON; CLIMATE-CHANGE; HETEROTROPHIC
DINOFLAGELLATE; LABORATORY CULTURES; VERTICAL MIGRATION
AB A two-decade decline of Fraser River sockeye salmon, historically the most valuable west coast Canadian and United States salmon fishery, was linked with blooms of the harmful raphidophyte flagellate Heterosigma akashiwo in the Strait of Georgia ("Strait"), British Columbia. This region has the most intense and prolonged Heterosigma blooms of all B.C. regions analyzed. Marine survival of Chilko stock averaged 2.7% in years when juvenile sockeye salmon seawater migration in the Strait coincided with major Heterosigma blooms versus 10.9% in no or minor bloom index years. Since the mid 1990s, September young-of-the-year ("YOY") herring abundance was strongly correlated with marine survival rates of Chilko stock Fraser River sockeye salmon and Heterosigma bloom timing in the Strait. Juvenile sockeye salmon and YOY herring co-occur for only six weeks in mid-May through June during initial salmon migration in the Strait. Sockeye salmon marine survival rates were therefore determined in that early period. Fraser River discharge was a bloom-controlling factor with earlier and larger spring and early summer flows linked to major blooms in that period. Heterosignia is a most versatile and allelopathic harmful algal bloom species and may adversely affect sockeye salmon through acute and chronic toxicity or food web impoverishment. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Rensel, J. E. Jack] Rensel Associates Aquat Sci, Arlington, WA 98223 USA.
[Haigh, Nicola] British Columbia Harmful Algae Monitoring Program, Nanaimo, BC V9R 5S5, Canada.
[Tynan, Tim J.] US Natl Marine Fisheries Serv, Salmon Recovery Div, Lacey, WA 98503 USA.
RP Rensel, JEJ (reprint author), Rensel Associates Aquat Sci, Arlington, WA 98223 USA.
EM jackrensel@att.net
FU Marine Harvest Canada; Mainstream Canada; Grieg Seafoods BC; Creative
Salmon; North Pacific Marine Science Organization (PICES); National
Science Foundation
FX The authors thank the following organizations and individuals for
providing data, manuscript review, or illustration drafting: James
Irvine and Dario Stucchi (Dept. of Fisheries and Oceans), Rita Homer
(University of Washington), Michael Lapointe (Pacific Salmon
Commission), Brian Riddell (Pacific Salmon Foundation), Randall Peterman
(Simon Fraser University), Ruth Milner (Washington Dept. of Fish and
Wildlife) and anonymous reviewers. Peter Chandler (Dept. of Fisheries
and Oceans) formatted draft and final figures. HAMP sample analysis was
funded by Marine Harvest Canada, Mainstream Canada, Grieg Seafoods BC
and Creative Salmon. This paper was prepared without any external
funding or compensation of any type. A travel grant from the North
Pacific Marine Science Organization (PICES) and the National Science
Foundation allowed the primary author to present initial findings at the
2009 annual PICES meeting.[SS]
NR 130
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Z9 33
U1 3
U2 31
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1568-9883
J9 HARMFUL ALGAE
JI Harmful Algae
PD NOV
PY 2010
VL 10
IS 1
BP 98
EP 115
DI 10.1016/j.hal.2010.07.005
PG 18
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA 677CC
UT WOS:000283965700012
ER
PT J
AU Costa, PR
Botelho, MJ
Lefebvre, KA
AF Costa, Pedro Reis
Botelho, Maria Joao
Lefebvre, Kathi A.
TI Characterization of paralytic shellfish toxins in seawater and sardines
(Sardina pilchardus) during blooms of Gymnodinium catenatum
SO HYDROBIOLOGIA
LA English
DT Article
DE Gymnodinium catenatum; Vector; Sardines; Saxitoxins; Paralytic shellfish
poisoning; Dissolved and particulate; Planktivorous fish
ID HARMFUL ALGAL BLOOMS; ALEXANDRIUM-FUNDYENSE; DISSOLVED SAXITOXIN; LARVAL
FISH; DINOFLAGELLATE; ACCUMULATION; EXPOSURE; FINFISH; RISK; PSP
AB The re-emergence of Gymnodinum catenatum blooms after a 10 year hiatus of absence initiated the present investigation. This study aims to evaluate the exposure of small pelagic fishes to paralytic shellfish toxins (PST) during blooms of G. catenatum. Sardines (Sardina pilchardus) were selected as a representative fish species. In order to assess toxin availability to fish, both intracellular PSTs (toxin retained within the algal cells) and extracellular PSTs (toxin found in seawater outside algal cells) were quantified, as well as toxin levels within three fish tissue matrices (viscera, muscle and brain). During the study period, the highest cell densities of G. catenatum reached 2.5 x 10(4) cells l(-1) and intracellular PST levels ranged from 3.4 to 398 ng STXeq l(-1) as detected via an enzyme linked immunosorbent assay (ELISA). Measurable extracellular PSTs were also detected in seawater (0.2-1.1 mu g STXeq l(-1)) for the first time in Atlantic waters. The PST profile in G. catenatum was determined via high performance liquid chromatography with fluorescence detection (HPLC-FLD) and consisted mostly of sulfocarbamoyl (C1+2, B1) and decarbamoyl (dcSTX, dcGTX2+3, dcNEO) toxins. The observed profile was similar to that reported previously in G. catenatum blooms in this region before the 10-year hiatus. Sardines, planktivorous fish that ingest a large number of phytoplankton cells, were found to contain PSTs in the viscera, reaching a maximum of 531 mu g STXeq kg(-1). PSTs were not detected in corresponding muscle or brain tissues. The PST profile characterized in sardine samples consisted of the same sulfocarbamoyl and decarbamoyl toxins found in the algal prey with minor differences in relative abundance of each toxin. Overall, the data suggest that significant biotransformation of PSTs does not occur in sardines. Therefore, planktivorous fish may be a good tracer for the occurrence of offshore G. catenatum blooms and the associated PSTs produced by these algae.
C1 [Costa, Pedro Reis; Botelho, Maria Joao] IPIMAR, Natl Inst Biol Resources, P-1449006 Lisbon, Portugal.
[Lefebvre, Kathi A.] NOAA Fisheries, NW Fisheries Sci Ctr, Marine Biotoxins Program, Seattle, WA 98112 USA.
RP Costa, PR (reprint author), IPIMAR, Natl Inst Biol Resources, Ave Brasilia S-N, P-1449006 Lisbon, Portugal.
EM prcosta@ipimar.pt
RI Costa, Pedro/F-2192-2011;
OI Costa, Pedro/0000-0001-6083-470X; Henriques, Maria Joao
Botelho/0000-0001-9330-9979
FU The Portuguese Foundation for Science and Technology
[PTDC/MAR/78997/2006, SFRH/BPD/27002/2006]
FX Authors greatly appreciated the helpful assistance of Ms Bich-Thuy
Eberhart (Seattle-NOAA) in ELISA determinations, and Ms Lourdes Dias
(Lisbon-IPIMAR) for seawater sampling. The Portuguese Foundation for
Science and Technology supported this study through the research grant
PTDC/MAR/78997/2006 and post-doctoral grant to P.R. Costa, grant number:
SFRH/BPD/27002/2006.
NR 49
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U1 1
U2 17
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0018-8158
J9 HYDROBIOLOGIA
JI Hydrobiologia
PD NOV
PY 2010
VL 655
IS 1
BP 89
EP 97
DI 10.1007/s10750-010-0406-5
PG 9
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA 654PG
UT WOS:000282179900008
ER
PT J
AU Arthaud, DL
Greene, CM
Guilbault, K
Morrow, JV
AF Arthaud, David L.
Greene, Correigh M.
Guilbault, Kimberly
Morrow, James V., Jr.
TI Contrasting life-cycle impacts of stream flow on two Chinook salmon
populations
SO HYDROBIOLOGIA
LA English
DT Article
DE Stream flow; Snake River; Chinook salmon; Survival
ID ONCORHYNCHUS-MYKISS ABUNDANCE; ATLANTIC SALMON; JUVENILE SALMONIDS;
COLUMBIA RIVER; RAINBOW-TROUT; SNAKE RIVER; PACIFIC-NORTHWEST; TRUTTA
POPULATION; SMOLT PRODUCTION; CLIMATE-CHANGE
AB Stream flow affects many aspects of freshwater fish biology, but the extent to which variation in stream flow influences productivity of anadromous salmonid populations across their entire life cycle is not well known. We compared relationships of stream flow and productivity for Chinook salmon (Oncorhynchus tshawytscha) from two systems in the Salmon River basin in Idaho: the Lemhi River, a watershed subjected to intensive water use for irrigation, and Marsh Creek, a drainage with a natural hydrograph. We estimated rates of productivity based on monitoring at four life stages: the number of eggs initiating each cohort, juveniles migrating from the natal tributary past an outmigrant trap, smolts surviving to the Snake River, and adults returning to spawn. Using model selection techniques, we examined whether river flow experienced during these life stages explained variation above and beyond predictors of climate associated with each stage. In the Lemhi River, tributary stream flow during early residence exhibited strong correlations with egg-trap, egg-smolt, and egg-adult return rates, and was consistently a better predictor of productivity than stream flow occurring during late summer. Model selection indicated that early rearing flow was the single best predictor of both egg-trap and trap-smolt transition rates in the Lemhi River, and path analysis revealed a strong set of pathways linking rearing flow to adult return rate primarily through egg-trap productivity. These patterns were much less strongly exhibited or nonexistent in Marsh Creek. However, for both populations, migration flow in the Columbia River was the best predictor of smolt-adult return rates. Potentially confounding climatic variables exhibited relatively weak effects upon both early life histories and tributary flow, but were included in the best models of migration flows and smolt-adult return rate. These results suggest that effects of stream flow on juvenile salmonids in flow-altered systems can have substantial impacts on returning adults.
C1 [Arthaud, David L.; Morrow, James V., Jr.] Natl Marine Fisheries Serv, 10095 W Emerald St,Room 180, Boise, ID 83704 USA.
[Greene, Correigh M.; Guilbault, Kimberly] NOAA, Natl Marine Fisheries Serv, NW Fisheries Sci Ctr, Environm Conservat Div, Seattle, WA 98112 USA.
RP Morrow, JV (reprint author), Natl Marine Fisheries Serv, 10095 W Emerald St,Room 180, Boise, ID 83704 USA.
EM Jim.morrow@noaa.gov
NR 75
TC 7
Z9 7
U1 3
U2 44
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0018-8158
EI 1573-5117
J9 HYDROBIOLOGIA
JI Hydrobiologia
PD NOV
PY 2010
VL 655
IS 1
BP 171
EP 188
DI 10.1007/s10750-010-0419-0
PG 18
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA 654PG
UT WOS:000282179900015
ER
PT J
AU Cadrin, SX
Bernreuther, M
Danielsdottir, AK
Hjorleifsson, E
Johansen, T
Kerr, L
Kristinsson, K
Mariani, S
Nedreaas, K
Pampoulie, C
Planque, B
Reinert, J
Saborido-Rey, F
Sigurosson, T
Stransky, C
AF Cadrin, Steven X.
Bernreuther, Matthias
Danielsdottir, Anna Kristin
Hjorleifsson, Einar
Johansen, Torild
Kerr, Lisa
Kristinsson, Kristjan
Mariani, Stefano
Nedreaas, Kjell
Pampoulie, Christophe
Planque, Benjamin
Reinert, Jakup
Saborido-Rey, Fran
Sigurosson, Thorsteinn
Stransky, Christoph
TI Population structure of beaked redfish, Sebastes mentella: evidence of
divergence associated with different habitats
SO ICES JOURNAL OF MARINE SCIENCE
LA English
DT Article
DE adaptation; depth; fisheries management; habitat; molecular genetics;
multidisciplinary approach; North Atlantic; stock structure
ID DEEP-WATER REDFISH; ANCIENT SPECIES FLOCKS; OTOLITH SHAPE-ANALYSIS;
NORTH-ATLANTIC; IRMINGER-SEA; GEOGRAPHIC-VARIATION; ADJACENT WATERS;
GENUS SEBASTES; GENETIC-STRUCTURE; S.-MENTELLA
AB Throughout their range, Sebastes spp. are adapted to a diversity of ecological niches, with overlapping spatial distributions of different species that have little or no morphological differences. Divergence of behavioural groups into depth-defined adult habitats has led to reproductive isolation, adaptive radiation, and speciation in the genus Sebastes. Recent genetic research, supported by life-history information, indicates four biological stocks of Sebastes mentella in the Irminger Sea and adjacent waters: a western stock, a deep-pelagic stock, a shallow-pelagic stock, and an Iceland slope stock. Congruent differences in fatty acids and parasites suggest that these genetically distinct populations are adapted to disparate trophic habitats in pelagic waters (shallower and deeper than the deep-scattering layer) and in demersal habitats on the continental slope. Morphology of pelagic forms is also more streamlined than demersal forms. Although genetic differences and evidence for reproductive isolation are clear, these populations appear to share common nursery habitats on the Greenland shelf. We propose a redefinition of practical management units near the Irminger Sea based on geographic proxies for biological stocks and minimizing mixed-stock catches according to the spatial patterns of the recent fishery.
C1 [Cadrin, Steven X.] NOAA, Sch Marine Sci & Technol, UMass CMER Program, Fairhaven, MA 02719 USA.
[Bernreuther, Matthias; Stransky, Christoph] Johann Heinrich von Thunen Inst, Inst Sea Fisheries, D-38116 Braunschweig, Germany.
[Hjorleifsson, Einar; Kristinsson, Kristjan; Pampoulie, Christophe; Sigurosson, Thorsteinn] Marine Res Inst, IS-121 Reykjavik, Iceland.
[Johansen, Torild; Planque, Benjamin] Inst Marine Res, N-9294 Tromso, Norway.
[Kerr, Lisa] Univ Massachusetts, Sch Marine Sci & Technol, Fairhaven, MA 02719 USA.
[Mariani, Stefano] Univ Coll Dublin, Sch Biol & Environm Sci, Dublin 4, Ireland.
[Nedreaas, Kjell] Inst Marine Res, N-5817 Bergen, Norway.
[Reinert, Jakup] Faroe Marine Res Inst, Torshavn, Faroe Islands, Denmark.
[Saborido-Rey, Fran] Inst Marine Res CSIC, E-36208 Vigo, Spain.
RP Cadrin, SX (reprint author), NOAA, Sch Marine Sci & Technol, UMass CMER Program, 200 Mill Rd, Fairhaven, MA 02719 USA.
EM steven.cadrin@noaa.gov
RI Mariani, Stefano/A-2964-2012; Planque, Benjamin/D-2729-2013;
Saborido-Rey, Fran/A-8440-2008
OI Mariani, Stefano/0000-0002-5329-0553; Planque,
Benjamin/0000-0002-0557-7410; Saborido-Rey, Fran/0000-0002-2760-8169
NR 90
TC 21
Z9 23
U1 1
U2 21
PU OXFORD UNIV PRESS
PI OXFORD
PA GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND
SN 1054-3139
J9 ICES J MAR SCI
JI ICES J. Mar. Sci.
PD NOV
PY 2010
VL 67
IS 8
BP 1617
EP 1630
DI 10.1093/icesjms/fsq046
PG 14
WC Fisheries; Marine & Freshwater Biology; Oceanography
SC Fisheries; Marine & Freshwater Biology; Oceanography
GA 666NK
UT WOS:000283121900009
ER
PT J
AU Kerr, LA
Cadrin, SX
Secor, DH
AF Kerr, Lisa A.
Cadrin, Steven X.
Secor, Dave H.
TI Simulation modelling as a tool for examining the consequences of spatial
structure and connectivity on local and regional population dynamics
SO ICES JOURNAL OF MARINE SCIENCE
LA English
DT Article
DE connectivity; metapopulation; persistence; population; spatial structure
ID COD GADUS-MORHUA; ATLANTIC COD; MANAGEMENT; METAPOPULATIONS;
BIOCOMPLEXITY; PRODUCTIVITY; STABILITY; ECOLOGY; FISHES; MAINE
AB Kerr, L. A., Cadrin, S. X., and Secor, D. H. 2010. Simulation modelling as a tool for examining the consequences of spatial structure and connectivity on local and regional population dynamics. - ICES Journal of Marine Science, 67: 1631-1639.
C1 [Kerr, Lisa A.] Univ Massachusetts Dartmouth, Sch Marine Sci & Technol, Fairhaven, MA 02719 USA.
[Cadrin, Steven X.] NOAA, UMass Cooperat Marine Educ & Res Program, Fairhaven, MA 02719 USA.
[Secor, Dave H.] Univ Maryland, Chesapeake Biol Lab, Ctr Environm Sci, Solomons, MD 20688 USA.
RP Kerr, LA (reprint author), Univ Massachusetts Dartmouth, Sch Marine Sci & Technol, 200 Mill Rd,Suite 325, Fairhaven, MA 02719 USA.
EM lkerr@umassd.edu
RI Secor, D/D-4367-2012
OI Secor, D/0000-0001-6007-4827
FU National Science Foundation [OCE-032485]; Massachusetts Marine Fisheries
Institute
FX The white perch and herring work described was supported by the National
Science Foundation under Grant No. OCE-032485. Deirdre Brophy was
helpful in specifying the herring model. Support for the Atlantic cod
research described was provided by the Massachusetts Marine Fisheries
Institute. We acknowledge the contribution of research by SMAST cod
tagging/genetic collaborators (including D. Martins, J. Loehrke, S.
Tallack, I. Wirgin, D. L. Berlinsky, and A. I. Kovach).
NR 37
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U1 0
U2 24
PU OXFORD UNIV PRESS
PI OXFORD
PA GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND
SN 1054-3139
J9 ICES J MAR SCI
JI ICES J. Mar. Sci.
PD NOV
PY 2010
VL 67
IS 8
BP 1631
EP 1639
DI 10.1093/icesjms/fsq053
PG 9
WC Fisheries; Marine & Freshwater Biology; Oceanography
SC Fisheries; Marine & Freshwater Biology; Oceanography
GA 666NK
UT WOS:000283121900010
ER
PT J
AU Grant, WS
Spies, I
Canino, MF
AF Grant, W. Stewart
Spies, Ingrid
Canino, Michael F.
TI Shifting-balance stock structure in North Pacific walleye pollock (Gadus
chalcogrammus)
SO ICES JOURNAL OF MARINE SCIENCE
LA English
DT Article
DE Bering Sea; cytochrome oxidase I; Gulf of Alaska; isolation by distance;
marine fish; mitochondrial DNA
ID EASTERN BERING-SEA; HERRING CLUPEA-PALLASI; PAN-I LOCUS;
THERAGRA-CHALCOGRAMMA; MITOCHONDRIAL-DNA; MARINE FISH;
GENETIC-STRUCTURE; ATLANTIC COD; POPULATION-STRUCTURE;
GEOGRAPHIC-VARIATION
AB Grant, W. S., Spies, I., and Canino, M. F. 2010. Shifting-balance stock structure in North Pacific walleye pollock (Gadus chalcogrammus). - ICES Journal of Marine Science, 67: 1687-1696.
C1 [Grant, W. Stewart] Alaska Dept Fish & Game, Genet Lab, Anchorage, AK 99518 USA.
[Grant, W. Stewart] Univ Alaska, Dept Biol Sci, Anchorage, AK 99508 USA.
[Spies, Ingrid; Canino, Michael F.] Alaska Fisheries Sci Ctr, Seattle, WA 98115 USA.
RP Grant, WS (reprint author), Alaska Dept Fish & Game, Genet Lab, 333 Raspberry Rd, Anchorage, AK 99518 USA.
EM william.grant@alaska.gov
NR 78
TC 7
Z9 7
U1 0
U2 8
PU OXFORD UNIV PRESS
PI OXFORD
PA GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND
SN 1054-3139
J9 ICES J MAR SCI
JI ICES J. Mar. Sci.
PD NOV
PY 2010
VL 67
IS 8
BP 1687
EP 1696
DI 10.1093/icesjms/fsq079
PG 10
WC Fisheries; Marine & Freshwater Biology; Oceanography
SC Fisheries; Marine & Freshwater Biology; Oceanography
GA 666NK
UT WOS:000283121900016
ER
PT J
AU Kang, MG
Park, HJ
Ahn, SH
Xu, T
Guo, LJ
AF Kang, Myung-Gyu
Park, Hui Joon
Ahn, Se Hyun
Xu, Ting
Guo, L. Jay
TI Toward Low-Cost, High-Efficiency, and Scalable Organic Solar Cells with
Transparent Metal Electrode and Improved Domain Morphology
SO IEEE JOURNAL OF SELECTED TOPICS IN QUANTUM ELECTRONICS
LA English
DT Article
DE Bulk heterojunction (BHJ); nanoimprint lithography (NIL); organic solar
cell (OSC); roll-to-roll (R2R); surface plasmons (SPs); transparent and
conductive electrode (TCE)
ID INDIUM-TIN-OXIDE; LIGHT-EMITTING-DIODES; POLYMER PHOTOVOLTAIC CELLS;
ROLL-TO-ROLL; NANOIMPRINT LITHOGRAPHY; SELF-ORGANIZATION; EXCITON
DIFFUSION; PHASE-SEPARATION; THIN-FILMS; HETEROJUNCTION
AB We review our recent progress toward realizing future low-cost, high-efficiency, and scalable organic solar cells (OSCs). First, we show that the transparent electrodes based on metallic nanostructure is a strong candidate as a replacement of conventional indium tin oxide (ITO) electrode due to their superior properties, such as high optical transparency, good electrical conductivity, and mechanical flexibility, and the versatility that these properties can be adjusted independently by changing the linewidth and thickness of the metal grid structure. Furthermore, we exploited the unique optical properties due to the excitation of surface plasmon resonance by the metallic nanogratings to enhance the light absorption of organic semiconductors, and demonstrated enhanced power conversion efficiency than devices made using ITO electrode. In addition, we also investigated a new device fabrication process with a focus on the photoactive layer formation, which produces the most optimum bulk-heterojunction morphology compared with conventional annealing-based methods. Finally, we successfully demonstrated that these approaches are scalable to large-area and high-speed roll-to-roll processes. We believe that the works highlighted in this paper represent one step forward to realizing low-cost, high-efficiency, and large-area OSCs.
C1 [Kang, Myung-Gyu; Park, Hui Joon; Ahn, Se Hyun; Xu, Ting; Guo, L. Jay] Univ Michigan, Dept Elect Engn & Comp Sci, Solid State Elect Lab, Ann Arbor, MI 48109 USA.
[Ahn, Se Hyun] Univ Michigan, Dept Mech Engn, Ann Arbor, MI 48109 USA.
[Park, Hui Joon] Univ Michigan, Ctr Macromol Sci & Engn, Ann Arbor, MI 48109 USA.
RP Kang, MG (reprint author), NIST, Gaithersburg, MD 20899 USA.
EM myung-gyu.kang@nist.gov; huijoon@umich.edu; happyash@umich.edu;
xuting@umich.edu; guo@umich.edu
RI Xu, Ting/D-3921-2013
OI Xu, Ting/0000-0002-2008-7049
FU National Science Foundation; National Institute of Standards and
Technology; King Abdulaziz City for Science and Technology; Department
of Energy; Rackham Predoctoral Fellowship; Rackham International Student
Fellowship; China Scholarship Council
FX This work was supported in part by the National Science Foundation, in
part by the National Institute of Standards and Technology, in part by
the King Abdulaziz City for Science and Technology, and in part by the
Department of Energy. The work of M.-G. Kang was supported by a Rackham
Predoctoral Fellowship. The work of H. J. Park was supported by a
Rackham International Student Fellowship. The work of T. Xu was
supported by a China Scholarship Council Scholarship. The first two
authors (M.-G. Kang and H. J. Park) contributed equally to this study.
Correspondence should be addressed to L. J. Guo.
NR 91
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U1 10
U2 49
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 1077-260X
EI 1558-4542
J9 IEEE J SEL TOP QUANT
JI IEEE J. Sel. Top. Quantum Electron.
PD NOV-DEC
PY 2010
VL 16
IS 6
BP 1807
EP 1820
DI 10.1109/JSTQE.2010.2044634
PG 14
WC Engineering, Electrical & Electronic; Optics; Physics, Applied
SC Engineering; Optics; Physics
GA 736IY
UT WOS:000288488400039
ER
PT J
AU Genender, E
Holloway, CL
Remley, KA
Ladbury, JM
Koepke, G
Garbe, H
AF Genender, Evgeni
Holloway, Christopher L.
Remley, Kate A.
Ladbury, John M.
Koepke, Galen
Garbe, Heyno
TI Simulating the Multipath Channel With a Reverberation Chamber:
Application to Bit Error Rate Measurements
SO IEEE TRANSACTIONS ON ELECTROMAGNETIC COMPATIBILITY
LA English
DT Article
DE Bit error rate (BER); digital modulation; multipath; reverberation
chamber; wireless propagation; wireless system
ID SHIELDING EFFECTIVENESS; ELECTRICALLY LARGE; DIVERSITY GAIN;
ENVIRONMENT; PROPAGATION; CAVITIES; ANTENNAS; ARRAY
AB We illustrate the use of the reverberation chamber to simulate fixed wireless propagation environments including effects such as narrowband fading and Doppler spread. These effects have a strong impact on the quality of the wireless channel and the ability of a receiver to decode a digitally modulated signal. Different channel characteristics such as power delay profile and RMS delay spread are varied inside the chamber by incorporating various amounts of absorbing material. In order to illustrate the impact of the chamber configuration on the quality of a wireless communication channel, bit error rate measurements are performed inside the reverberation chamber for different loadings, symbol rates, and paddle speeds; the results are discussed. Measured results acquired inside a chamber are compared with those obtained both in an actual industrial environment and in an office.
C1 [Genender, Evgeni; Holloway, Christopher L.; Remley, Kate A.; Ladbury, John M.; Koepke, Galen] NIST, Electromagnet Div, Boulder Labs, US Dept Commerce, Boulder, CO 80305 USA.
[Genender, Evgeni; Garbe, Heyno] Leibniz Univ Hannover, Inst Grundlagen Elektrotech & Messtech, D-30167 Hannover, Germany.
RP Genender, E (reprint author), Leibniz Univ Hannover, Inst Grundlagen Elektrotech & Messtech, D-30167 Hannover, Germany.
EM holloway@boulder.nist.gov
OI Garbe, Heyno/0000-0003-1601-1321
FU Public Safety Communications Research Laboratory of the Office of Law
Enforcement Standards at NIST
FX The field tests at the oil refinery and the 60-storied office building
for this work were supported by the Public Safety Communications
Research Laboratory of the Office of Law Enforcement Standards at NIST.
NR 35
TC 68
Z9 69
U1 0
U2 4
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 0018-9375
J9 IEEE T ELECTROMAGN C
JI IEEE Trans. Electromagn. Compat.
PD NOV
PY 2010
VL 52
IS 4
BP 766
EP 777
DI 10.1109/TEMC.2010.2044578
PG 12
WC Engineering, Electrical & Electronic; Telecommunications
SC Engineering; Telecommunications
GA 681YT
UT WOS:000284361300001
ER
PT J
AU Moore, N
Torbick, N
Lofgren, B
Wang, J
Pijanowski, B
Andresen, J
Kim, DY
Olson, J
AF Moore, Nathan
Torbick, Nathan
Lofgren, Brent
Wang, Jing
Pijanowski, Bryan
Andresen, Jeffrey
Kim, Dong-Yun
Olson, Jennifer
TI Adapting MODIS-derived LAI and fractional cover into the RAMS in East
Africa
SO INTERNATIONAL JOURNAL OF CLIMATOLOGY
LA English
DT Article
DE climate modelling; MODIS; LAI; fractional cover; RAMS
ID LAND-SURFACE TEMPERATURE; REGIONAL CLIMATE MODEL; LEAF-AREA INDEX; SHORT
RAINS; INTERANNUAL VARIABILITY; RAINFALL PRODUCTS; VALIDATION;
VEGETATION; SATELLITE; IMPACT
AB Land cover and its associated biophysical parameters govern many land-atmosphere interactions. Several previous studies have demonstrated the utility of incorporating satellite-derived observations of land cover into climate models to improve prediction accuracy. In the developing world where agriculture is a primary livelihood, a better understanding of seasonal variability in precipitation and near-surface temperature is critical to constructing more effective coping strategies for climate changes and food security. However, relatively few studies have been able to assess the impacts of improved surface parameterisation on these variables and their seasonality. Using moderate resolution imaging spectroradiometer (MODIS)-derived products, we sought to address this shortcoming by adapting leaf area index (LAI) and vegetative fractional cover (FC) products, along with an improved representation of the land surface (i.e. land use land cover) into the Regional Atmospheric Modelling System in East Africa to evaluate the effect improved representations would have on simulated precipitation and land surface temperature (LST). In particular, we tested the hypothesis that improved phenological parameterisations could reduce error in precipitation and LST under dramatically different atmospheric conditions. The model was used to simulate dry/normal/wet rainfall years of 2000, 2001, and 2002 (respectively) in order to understand biases in this parameterisation under different boundary conditions. Our results show a dramatic improvement in LST simulation due to the use of the improved representations (spline functions) during most of the year, both spatially and temporally. Annual precipitation, which is dependent upon a much greater variety of surface and atmospheric characteristics, did not improve as much by adopting the spline representations of LAI and FC; the results were more equivocal. However, seasonal timing of precipitation improved in some areas, and this improvement has important consequences for integrated climate-agriculture assessments. Copyright (C) 2009 Royal Meteorological Society
C1 [Moore, Nathan; Andresen, Jeffrey; Olson, Jennifer] Michigan State Univ, Dept Geog, E Lansing, MI 48824 USA.
[Torbick, Nathan] Appl GeoSolut LLC, Durham, NH 03824 USA.
[Lofgren, Brent] NOAA GLERL, Ann Arbor, MI 48108 USA.
[Wang, Jing] Univ Illinois, Dept Math Stat & Comp Sci, Chicago, IL 60680 USA.
[Pijanowski, Bryan] Purdue Univ, Dept Forestry & Nat Resources, W Lafayette, IN 47907 USA.
[Kim, Dong-Yun] Virginia Tech, Dept Stat, Blacksburg, VA 24061 USA.
RP Moore, N (reprint author), Michigan State Univ, Dept Geog, E Lansing, MI 48824 USA.
EM moorena@msu.edu
OI Lofgren, Brent/0000-0003-2189-0914
FU NSF [0308420]
FX The images and data used in this study were acquired using the GES-DISC
Interactive Online Visualization ANd aNalysis Infrastructure (Giovanni)
as part of the NASA's Goddard Earth Sciences (GES) Data and Information
Services Center (DISC). This research was supported by NSF Grant
0308420, Biocomplexity/CNH. NCEP reanalysis data were provided by the
NOAA/OAR/ESRL PSD, Boulder, Colorado, USA, from their website
http://www.cdc.noaa.gov/. We are also grateful to Richard Anyah for
advice in adapting a lake model for RAMS.
NR 77
TC 14
Z9 15
U1 0
U2 6
PU JOHN WILEY & SONS LTD
PI CHICHESTER
PA THE ATRIUM, SOUTHERN GATE, CHICHESTER PO19 8SQ, W SUSSEX, ENGLAND
SN 0899-8418
J9 INT J CLIMATOL
JI Int. J. Climatol.
PD NOV
PY 2010
VL 30
IS 13
BP 1954
EP 1969
DI 10.1002/joc.2011
PG 16
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 680CZ
UT WOS:000284211300006
ER
PT J
AU Wang, JH
Hong, Y
Gourley, J
Adhikari, P
Li, L
Su, FG
AF Wang, Jiahu
Hong, Yang
Gourley, Jonathan
Adhikari, Pradeep
Li, Li
Su, Fengge
TI Quantitative assessment of climate change and human impacts on long-term
hydrologic response: a case study in a sub-basin of the Yellow River,
China
SO INTERNATIONAL JOURNAL OF CLIMATOLOGY
LA English
DT Article
DE climate change; hydrology; human impact; impact factor formula; run-off
ID LAST 50 YEARS; WATER-RESOURCES; BASIN; MODEL; VARIABILITY; PREDICTION;
STREAMFLOW; RUNOFF; TRENDS
AB In this study we developed an impact factor formula (IFF) to quantitatively attribute separately the impacts of climate change and local human activities on hydrological response (i.e. run-off) in a sub-basin of Yellow River for the period 1950-2000.Using the daily climatic data, we first calibrated and verified the variable infiltration capacity (VIC) hydrological model to the baseline period 1955-1970. Then we developed the basin's natural run-off for the following three decades (1971-2000) using the VIC model without considering local human impacts, as the VIC model is benchmarked by the 1960's hydrological regime.
On the basis of observed precipitation, run-off and reconstructed natural run-off data from 1971 to 2000, we quantified their long-term trend, decadal and annual variations. Using daily climatic observations, we showed that the precipitation and run-off have decreased from the baseline decade, the 1960s, indicating a drier hydrological regime for recent decades. We further applied the IFF to quantitatively attribute separately the impacts of reduced precipitation and increased temperatures from climate change and then of local human activities on hydrological run-off response. It was found that climate change has a greater impact than human activities on the basin's run-off for the three consecutive decades. The pCC (percentage change of run-off due to climate change impact) is found to be 89% followed by 66% and 56% in 1970s, 1980s and 1990s, respectively. Over the decades, pHA (percentage change of run-off due to human activities) has continuously increased from 11% to 44%. If the trend continues, in future, the pHA is going to outweigh pCC in this basin. This study provides a quantitative assessment methodology for water resources managers to understand the changing process of the hydrological cycle and attribute its causative factors in a sub-basin of the Yellow River. Copyright (C) 2009 Royal Meteorological Society
C1 [Wang, Jiahu; Hong, Yang; Adhikari, Pradeep; Li, Li] Univ Oklahoma, Sch Civil Engn & Environm Sci, Natl Weather Ctr, Norman, OK 73019 USA.
[Wang, Jiahu; Li, Li] Hohai Univ, State Key Lab Hydrol Water Resources & Hydraul En, Nanjing 210098, Peoples R China.
[Gourley, Jonathan] NOAA, Natl Severe Storms Lab, Norman, OK 73072 USA.
[Su, Fengge] Univ Washington, Dept Civil & Environm Engn, Seattle, WA 98195 USA.
RP Hong, Y (reprint author), Univ Oklahoma, Sch Civil Engn & Environm Sci, Natl Weather Ctr, Norman, OK 73019 USA.
EM yanghong@ou.edu
RI Hong, Yang/D-5132-2009; Gourley, Jonathan/C-7929-2016;
OI Hong, Yang/0000-0001-8720-242X; Gourley, Jonathan/0000-0001-7363-3755;
Adhikari, Pradeep/0000-0003-2218-4376
FU Remote Sensing Hydrology Research Group at the University of Oklahoma;
NSFC (National Natural Science Foundation of China) [40801012]
FX This study is supported by Remote Sensing Hydrology Research Group at
the University of Oklahoma (http://hydro.ou.edu). The authors would like
to extend their appreciation to Project 40801012 supported by NSFC
(National Natural Science Foundation of China) for providing data used
in the study. The field data were gratefully shared by Hydrological
Bureau, YRCC (Yellow River Conservancy Commission, P.R. China).
NR 28
TC 38
Z9 43
U1 7
U2 49
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0899-8418
J9 INT J CLIMATOL
JI Int. J. Climatol.
PD NOV
PY 2010
VL 30
IS 14
BP 2130
EP 2137
DI 10.1002/joc.2023
PG 8
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 680DB
UT WOS:000284211500002
ER
PT J
AU Bogoutdinov, SR
Gvishiani, AD
Agayan, SM
Solovyev, AA
Kin, E
AF Bogoutdinov, Sh. R.
Gvishiani, A. D.
Agayan, S. M.
Solovyev, A. A.
Kin, E.
TI Time Series. Part 1: Spikes on Magnetograms of the Worldwide INTERMAGNET
Network
SO IZVESTIYA-PHYSICS OF THE SOLID EARTH
LA English
DT Article
AB The International Real-time Magnetic Observatory Network (INTERMAGNET) is the world's biggest international network of ground-based observatories, providing geomagnetic data almost in real time (within 72 hours of collection) [Kerridge, 2001]. The observation data are rapidly transferred by the observatories participating in the program to regional Geomagnetic Information Nodes (GINs), which carry out a global exchange of data and process the results. The observations of the main (core) magnetic field of the Earth and its study are one of the key problems of geophysics. The INTERMAGNET system is the basis of monitoring the state of the Earth's magnetic field; therefore, the information provided by the system is required to be very reliable. Despite the rigid high-quality standard of the recording devices, they are subject to external effects that affect the quality of the records. Therefore, an objective and formalized recognition with the subsequent remedy of the anomalies (artifacts) that occur on the records is an important task. Expanding on the ideas of Agayan [Agayan et al., 2005] and Gvishiani [Gvishiani et al., 2008a; 2008b], this paper suggests a new algorithm of automatic recognition of anomalies with specified morphology, capable of identifying both physically-and anthropogenically-derived spikes on the magnetograms. The algorithm is constructed using fuzzy logic and, as such, is highly adaptive and universal. The developed algorithmic system formalizes the work of the expert-interpreter in terms of artificial intelligence. This ensures identical processing of large data arrays, almost unattainable manually. Besides the algorithm, the paper also reports on the application of the developed algorithmic system for identifying spikes at the INTERMAGNET observatories. The main achievement of the work is the creation of an algorithm permitting the almost unmanned extraction of spike-free (definitive) magnetograms from preliminary records. This automated system is developed for the first time with the application of fuzzy logic system for geomagnetic measurements. It is important to note that the recognition of time disturbances is formalized and identical. The algorithm presented here appreciably increases the reliability of spike-free INTERMAGNET magnetograms, thus increasing the objectivity of our knowledge of the Earth's magnetic field. At the same time, the created system can accomplish identical, formalized, and retrospective analysis of large archives of digital and digitized magnetograms, accumulated in the system of Worldwide Data Centers. The relevant project has already been initiated as a collaborative initiative of the Worldwide Data Center at Geophysical Center (Russian Academy of Sciences) and the NOAA National Geophysical Data Center (Unite States). Thus, by improving and adding objectivity to both new and historical initial data, the developed algorithmic system may contribute appreciably to improving our understanding of the Earth's magnetic field.
C1 [Bogoutdinov, Sh. R.; Gvishiani, A. D.; Agayan, S. M.; Solovyev, A. A.] Russian Acad Sci, Geophys Ctr, Moscow, Russia.
[Kin, E.] NOAA, Natl Geophys Data Ctr, Boulder, CO 80303 USA.
RP Bogoutdinov, SR (reprint author), Russian Acad Sci, Geophys Ctr, Moscow, Russia.
RI Gvishiani, Alexei/F-8289-2014
FU Russian Foundation for Basic Research [09-05-00789-a]
FX This work was supported by the Russian Foundation for Basic Research
(grant no. 09-05-00789-a).
NR 11
TC 12
Z9 13
U1 0
U2 7
PU MAIK NAUKA/INTERPERIODICA/SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013-1578 USA
SN 1069-3513
J9 IZV-PHYS SOLID EART+
JI Izv.-Phys. Solid Earth
PD NOV
PY 2010
VL 46
IS 11
BP 1004
EP 1016
DI 10.1134/S1069351310110091
PG 13
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 691XM
UT WOS:000285114100009
ER
PT J
AU Yang, P
Feng, QA
Hong, G
Kattawar, GW
Wiscombe, WJ
Mishchenko, MI
Dubovik, O
Laszlo, I
Sokolik, IN
AF Yang, Ping
Feng, Qian
Hong, Gang
Kattawar, George W.
Wiscombe, Warren J.
Mishchenko, Michael I.
Dubovik, Oleg
Laszlo, Istvan
Sokolik, Irina N.
TI Modeling of the scattering and radiative properties of nonspherical
dust-like aerosols (vol 38, pg 995, 2007)
SO JOURNAL OF AEROSOL SCIENCE
LA English
DT Correction
C1 [Yang, Ping; Feng, Qian; Hong, Gang] Texas A&M Univ, Dept Atmospher Sci, College Stn, TX 77843 USA.
[Kattawar, George W.] Texas A&M Univ, Dept Phys, College Stn, TX 77843 USA.
[Wiscombe, Warren J.] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
[Mishchenko, Michael I.] NASA, Goddard Inst Space Studies, New York, NY 10025 USA.
[Dubovik, Oleg] Univ Lille 1, Opt Atmospher Lab, CNRS, F-59655 Villeneuve Daascq, France.
[Laszlo, Istvan] NOAA, NESDIS, Off Res & Applicat, Camp Springs, MD 20746 USA.
[Sokolik, Irina N.] Georgia Inst Technol, Sch Earth & Atmospher Sci, Atlanta, GA 30332 USA.
RP Yang, P (reprint author), Texas A&M Univ, Dept Atmospher Sci, College Stn, TX 77843 USA.
EM pyang@csrp.tamu.edu
RI Yang, Ping/B-4590-2011; Hong, Gang/A-2323-2012; Wiscombe,
Warren/D-4665-2012; Laszlo, Istvan/F-5603-2010; Dubovik,
Oleg/A-8235-2009; Mishchenko, Michael/D-4426-2012
OI Wiscombe, Warren/0000-0001-6844-9849; Laszlo,
Istvan/0000-0002-5747-9708; Dubovik, Oleg/0000-0003-3482-6460;
NR 1
TC 0
Z9 0
U1 0
U2 7
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0021-8502
J9 J AEROSOL SCI
JI J. Aerosol. Sci.
PD NOV
PY 2010
VL 41
IS 11
BP 1052
EP 1053
DI 10.1016/j.jaerosci.2010.07.006
PG 2
WC Engineering, Chemical; Engineering, Mechanical; Environmental Sciences;
Meteorology & Atmospheric Sciences
SC Engineering; Environmental Sciences & Ecology; Meteorology & Atmospheric
Sciences
GA 676HO
UT WOS:000283901800008
ER
PT J
AU Michelson, SA
Djalalova, IV
Bao, JW
AF Michelson, Sara A.
Djalalova, Irina V.
Bao, Jian-Wen
TI Evaluation of the Summertime Low-Level Winds Simulated by MM5 in the
Central Valley of California
SO JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY
LA English
DT Article
ID NUMERICAL WEATHER PREDICTION; BOUNDARY-LAYER DEPTH; PACIFIC-NORTHWEST;
PROFILER; DESIGN
AB A season-long set of 5-day simulations between 1200 UTC 1 June and 1200 UTC 30 September 2000 are evaluated using the observations taken during the Central California Ozone Study (CCOS) 2000 experiment. The simulations are carried out using the fifth-generation Pennsylvania State University-NCAR Mesoscale Model (MM5), which is widely used for air-quality simulations and control planning. The evaluation results strongly indicate that themodel-simulated low-level winds in California's Central Valley are biased in speed and direction: the simulated winds tend to have a stronger northwesterly component than observed. This bias is related to the difference in the observed and simulated large-scale, upper-level flows. The model simulations also show a bias in the height of the daytime atmospheric boundary layer (ABL), particularly in the northern and southern Central Valley. There is evidence to suggest that this bias in the daytime ABL height is not only associated with the large-scale, upper-level bias but also linked to apparent differences in the surface forcing.
C1 [Michelson, Sara A.; Djalalova, Irina V.; Bao, Jian-Wen] Univ Colorado, NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA.
[Michelson, Sara A.; Djalalova, Irina V.] Univ Boulder, Cooperat Inst Res Environm Sci, Boulder, CO USA.
RP Michelson, SA (reprint author), Univ Colorado, NOAA, Earth Syst Res Lab, Mail Stop PSD3,325 Broadway, Boulder, CO 80305 USA.
EM sara.a.michelson@noaa.gov
NR 19
TC 7
Z9 7
U1 1
U2 2
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 1558-8424
EI 1558-8432
J9 J APPL METEOROL CLIM
JI J. Appl. Meteorol. Climatol.
PD NOV
PY 2010
VL 49
IS 11
BP 2230
EP 2245
DI 10.1175/2010JAMC2295.1
PG 16
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 675NT
UT WOS:000283838100004
ER
PT J
AU Wind, G
Platnick, S
King, MD
Hubanks, PA
Pavolonis, MJ
Heidinger, AK
Yang, P
Baum, BA
AF Wind, Galina
Platnick, Steven
King, Michael D.
Hubanks, Paul A.
Pavolonis, Michael J.
Heidinger, Andrew K.
Yang, Ping
Baum, Bryan A.
TI Multilayer Cloud Detection with the MODIS Near-Infrared Water Vapor
Absorption Band
SO JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY
LA English
DT Article
ID BULK SCATTERING PROPERTIES; MULTIPLE-SCATTERING; OPTICAL-PROPERTIES;
LAND PRODUCTS; TOP PRESSURE; CIRRUS CLOUD; ICE CLOUDS; PART I;
ALGORITHM; PHASE
AB Data Collection 5 processing for the Moderate Resolution Imaging Spectroradiometer (MODIS) on board the NASA Earth Observing System (EOS) Terra and Aqua spacecraft includes an algorithm for detecting multilayered clouds in daytime. The main objective of this algorithm is to detect multilayered cloud scenes, specifically optically thin ice cloud overlying a lower-level water cloud, that present difficulties for retrieving cloud effective radius using single-layer plane-parallel cloud models. The algorithm uses the MODIS 0.94-mu m water vapor band along with CO(2) bands to obtain two above-cloud precipitable water retrievals, the difference of which, in conjunction with additional tests, provides a map of where multilayered clouds might potentially exist. The presence of a multilayered cloud results in a large difference in retrievals of above-cloud properties between the CO(2) and the 0.94-mu m methods. In this paper the MODIS multilayered cloud algorithm is described, results of using the algorithm over example scenes are shown, and global statistics for multilayered clouds as observed by MODIS are discussed. A theoretical study of the algorithm behavior for simulated multilayered clouds is also given. Results are compared to two other comparable passive imager methods. A set of standard cloudy atmospheric profiles developed during the course of this investigation is also presented. The results lead to the conclusion that the MODIS multilayer cloud detection algorithm has some skill in identifying multilayered clouds with different thermodynamic phases.
C1 [Wind, Galina] NASA, Goddard Space Flight Ctr, Code 613 2, Greenbelt, MD 20771 USA.
[Wind, Galina] SSAI Inc, Lanham, MD USA.
[King, Michael D.] Univ Colorado, Lab Atmospher & Space Phys, Boulder, CO 80309 USA.
[Hubanks, Paul A.] Wyle Inc, Silver Spring, MD USA.
[Hubanks, Paul A.] NOAA, NESDIS, Ctr Satellite Applicat & Res, Madison, WI USA.
[Pavolonis, Michael J.; Heidinger, Andrew K.; Yang, Ping] Texas A&M Univ, Dept Atmospher Sci, College Stn, TX USA.
[Baum, Bryan A.] Univ Wisconsin, Ctr Space Sci & Engn, Madison, WI 53706 USA.
RP Wind, G (reprint author), NASA, Goddard Space Flight Ctr, Code 613 2, Greenbelt, MD 20771 USA.
EM gala.wind@nasa.gov
RI Yang, Ping/B-4590-2011; King, Michael/C-7153-2011; Pavolonis,
Mike/F-5618-2010; Baum, Bryan/B-7670-2011; Platnick, Steven/J-9982-2014;
Heidinger, Andrew/F-5591-2010
OI King, Michael/0000-0003-2645-7298; Pavolonis, Mike/0000-0001-5822-219X;
Baum, Bryan/0000-0002-7193-2767; Platnick, Steven/0000-0003-3964-3567;
Heidinger, Andrew/0000-0001-7631-109X
FU MODIS Science Team; NASA
FX The authors thank Brad Wind for developing the groundwork for
simplifying the modifications to the operational MODIS code that made
most of these studies possible. This work was funded by the MODIS
Science Team and NASA's Radiation Sciences Program.
NR 32
TC 27
Z9 27
U1 0
U2 11
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 1558-8424
J9 J APPL METEOROL CLIM
JI J. Appl. Meteorol. Climatol.
PD NOV
PY 2010
VL 49
IS 11
BP 2315
EP 2333
DI 10.1175/2010JAMC2364.1
PG 19
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 675NT
UT WOS:000283838100009
ER
PT J
AU Shaw, JM
Nembach, HT
Silva, TJ
AF Shaw, Justin M.
Nembach, Hans T.
Silva, T. J.
TI Roughness induced magnetic inhomogeneity in Co/Ni multilayers:
Ferromagnetic resonance and switching properties in nanostructures
SO JOURNAL OF APPLIED PHYSICS
LA English
DT Article
ID ULTRATHIN FILMS; THIN-FILMS; ANISOTROPY; LINEWIDTH; MEDIA; FIELD
AB We report on the effect roughness has on the magnetic properties of Co/Ni multilayers with perpendicular anisotropy. We can systematically vary the surface roughness and grain size by the variation in the Cu seed layer thickness. The roughness has a significant effect on the lateral anisotropy variation across the material, which was studied through the size dependence of the switching field and switching field distribution in nanostructures. Ferromagnetic resonance measurements show a large dependence of the linewidth on the topography. However, only the inhomogeneous linewidth broadening varied significantly with roughness with little to no effect on the intrinsic damping parameter of alpha=0.015-0.018. (C) 2010 American Institute of Physics. [doi:10.1063/1.3506688]
C1 [Shaw, Justin M.; Nembach, Hans T.; Silva, T. J.] Natl Inst Stand & Technol, Electromagnet Div, Boulder, CO 80305 USA.
RP Shaw, JM (reprint author), Natl Inst Stand & Technol, Electromagnet Div, Boulder, CO 80305 USA.
EM justin.shaw@nist.gov
RI Shaw, Justin/C-1845-2008; Gastelois, Pedro/F-3891-2012; Silva,
Thomas/C-7605-2013
OI Shaw, Justin/0000-0003-2027-1521; Silva, Thomas/0000-0001-8164-9642
NR 28
TC 22
Z9 22
U1 0
U2 22
PU AMER INST PHYSICS
PI MELVILLE
PA CIRCULATION & FULFILLMENT DIV, 2 HUNTINGTON QUADRANGLE, STE 1 N O 1,
MELVILLE, NY 11747-4501 USA
SN 0021-8979
J9 J APPL PHYS
JI J. Appl. Phys.
PD NOV 1
PY 2010
VL 108
IS 9
AR 093922
DI 10.1063/1.3506688
PG 5
WC Physics, Applied
SC Physics
GA 680XN
UT WOS:000284270900095
ER
PT J
AU Wisbey, DS
Gao, JS
Vissers, MR
da Silva, FCS
Kline, JS
Vale, L
Pappas, DP
AF Wisbey, David S.
Gao, Jiansong
Vissers, Michael R.
da Silva, Fabio C. S.
Kline, Jeffrey S.
Vale, Leila
Pappas, David P.
TI Effect of metal/substrate interfaces on radio-frequency loss in
superconducting coplanar waveguides
SO JOURNAL OF APPLIED PHYSICS
LA English
DT Article
ID CAVITY; QUBITS
AB Microscopic two-level systems (TLSs) are known to contribute to loss in resonant superconducting microwave circuits. This loss increases at low power and temperatures as the TLSs become unsaturated. We find that the loss is dependent on both the substrate-superconductor interface and the roughness of the surfaces. A native, oxide-free interface reduced the loss due to TLSs. However, a rough surface in the CPW gap did not cause more TLS loss, but the overall loss was significantly increased for the roughest surfaces. [doi:10.1063/1.3499608]
C1 [Wisbey, David S.; Gao, Jiansong; Vissers, Michael R.; da Silva, Fabio C. S.; Kline, Jeffrey S.; Vale, Leila; Pappas, David P.] Natl Inst Stand & Technol, Boulder, CO 80305 USA.
RP Wisbey, DS (reprint author), Natl Inst Stand & Technol, 325 Broadway, Boulder, CO 80305 USA.
EM david.pappas@boulder.nist.gov
FU Office of the Director of National Intelligence (ODNI), Intelligence
Advanced Research Projects Activity (IARPA)
FX We acknowledge important discussions with Kevin Osborn, John Martinis,
and Ben Mazin. This research was funded in part by the Office of the
Director of National Intelligence (ODNI), Intelligence Advanced Research
Projects Activity (IARPA). All statements of fact, opinion or
conclusions contained herein are those of the authors and should not be
construed as representing the official views or policies of IARPA, the
ODNI, or the U.S. Government. This work is a contribution of the U.S.
Government, not subject to copyright in the U.S.
NR 18
TC 24
Z9 24
U1 1
U2 11
PU AMER INST PHYSICS
PI MELVILLE
PA CIRCULATION & FULFILLMENT DIV, 2 HUNTINGTON QUADRANGLE, STE 1 N O 1,
MELVILLE, NY 11747-4501 USA
SN 0021-8979
J9 J APPL PHYS
JI J. Appl. Phys.
PD NOV 1
PY 2010
VL 108
IS 9
AR 093918
DI 10.1063/1.3499608
PG 4
WC Physics, Applied
SC Physics
GA 680XN
UT WOS:000284270900091
ER
PT J
AU Xu, D
Sriram, V
Ozolins, V
Yang, JM
Tu, KN
Stafford, GR
Beauchamp, C
AF Xu, Di
Sriram, Vinay
Ozolins, Vidvuds
Yang, Jenn-Ming
Tu, K. N.
Stafford, Gery R.
Beauchamp, Carlos
TI In situ measurements of stress evolution for nanotwin formation during
pulse electrodeposition of copper (vol 105, 023521, 2009)
SO JOURNAL OF APPLIED PHYSICS
LA English
DT Correction
C1 [Xu, Di; Sriram, Vinay; Ozolins, Vidvuds; Yang, Jenn-Ming; Tu, K. N.] Univ Calif Los Angeles, Dept Mat Sci & Engn, Los Angeles, CA 90095 USA.
[Stafford, Gery R.; Beauchamp, Carlos] Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
RP Xu, D (reprint author), Univ Calif Los Angeles, Dept Mat Sci & Engn, Los Angeles, CA 90095 USA.
EM dixu@ucla.edu
RI Ozolins, Vidvuds/D-4578-2009
NR 1
TC 1
Z9 1
U1 0
U2 18
PU AMER INST PHYSICS
PI MELVILLE
PA CIRCULATION & FULFILLMENT DIV, 2 HUNTINGTON QUADRANGLE, STE 1 N O 1,
MELVILLE, NY 11747-4501 USA
SN 0021-8979
J9 J APPL PHYS
JI J. Appl. Phys.
PD NOV 1
PY 2010
VL 108
IS 9
AR 099901
DI 10.1063/1.3503174
PG 1
WC Physics, Applied
SC Physics
GA 680XN
UT WOS:000284270900164
ER
PT J
AU Karion, A
Sweeney, C
Tans, P
Newberger, T
AF Karion, Anna
Sweeney, Colm
Tans, Pieter
Newberger, Timothy
TI AirCore: An Innovative Atmospheric Sampling System
SO JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY
LA English
DT Article
ID IN-SITU OBSERVATIONS; CARBON-DIOXIDE; CO2; AIRCRAFT; CH4; N2O; AIR;
STRATOSPHERE; VARIABILITY; TRANSPORT
AB This work describes the Air Core, a simple and innovative atmospheric sampling system. The AirCore used in this study is a 150-m-long stainless steel tube, open at one end and closed at the other, that relies on positive changes in ambient pressure for passive sampling of the atmosphere. The Air Core evacuates while ascending to a high altitude and collects a sample of the ambient air as it descends. It is sealed upon recovery and measured with a continuous analyzer for trace gas mole fraction. The Air Core tubing can be shaped into a variety of configurations to accommodate any sampling platform; for the testing done in this work it was shaped into a 0,75-m-diameter coil. Measurements of CO(2) and CH(4) mole fractions in laboratory tests indicate a repeatability and lack of bias to better than 0.07 ppm (one sigma) for CO, and 0.4 ppb for CH(4) under various conditions. Comparisons of AirCore data with flask data from aircraft flights indicate a standard deviation of differences of 0.3 ppm and 5 ppb for CO(2) and CH(4), respectively, with no apparent bias. Accounting for longitudinal mixing, the expected measurement resolution for CO2 is 110 m at sea level, 260 m at 8000 m. and 1500 m at 20 000 m ASL after 3 h of storage, decreasing to 170, 390, and 2300 m, after 12 h. Validation tests confirm that the AirCore is a robust sampling device for many species on a variety of platforms, including balloons, unmanned aerial vehicles (UAVs), and aircraft.
C1 [Karion, Anna; Sweeney, Colm; Tans, Pieter] NOAA, ESRL, Boulder, CO 80305 USA.
[Karion, Anna; Sweeney, Colm] Univ Colorado, CIRES, Boulder, CO 80309 USA.
[Newberger, Timothy] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY USA.
RP Karion, A (reprint author), NOAA, ESRL, 325 Broadway, Boulder, CO 80305 USA.
EM anna.karion@noaa.gov
FU NASA through KalScott Engineering [NNX09CC18P]
FX We thank Kelly Loving for her assistance in performing laboratory tests.
This work was partially funded by NASA Contract NNX09CC18P through a
subcontract from KalScott Engineering.
NR 33
TC 34
Z9 34
U1 4
U2 28
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0739-0572
J9 J ATMOS OCEAN TECH
JI J. Atmos. Ocean. Technol.
PD NOV
PY 2010
VL 27
IS 11
BP 1839
EP 1853
DI 10.1175/2010JTECHA1448.1
PG 15
WC Engineering, Ocean; Meteorology & Atmospheric Sciences
SC Engineering; Meteorology & Atmospheric Sciences
GA 680PX
UT WOS:000284248000004
ER
PT J
AU Reinoso-Rondinel, R
Yu, TY
Torres, S
AF Reinoso-Rondinel, Ricardo
Yu, Tian-You
Torres, Sebastian
TI Multifunction Phased-Array Radar: Time Balance Scheduler for Adaptive
Weather Sensing
SO JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY
LA English
DT Article
ID SPECTRAL MOMENT; WSR-88D; PRIORITIZATION; TRACKING; SIGNAL
AB Phased-array radars (PARs) have the capability of instantaneously and dynamically controlling beam position on a pulse-by-pulse basis, which allows a single radar to perform multiple functions, such as tracking multiple storms or weather and aviation surveillance. Moreover, these tasks can be carried out with different update times to achieve the goal of better characterizing and forecasting the storms of interest. However, these tasks usually compete for finite radar resources, and scheduling algorithms are often needed to address resource contention. To capitalize on the PAR capabilities, an algorithm based on the concept of time balance (TB) is developed for adaptive weather sensing. Two quality measures are introduced to quantify the gain of adaptive sensing relative to standard scanning patterns used by the Weather Surveillance Radar-1988 Doppler (WSR-88D). A simulation experiment is performed to demonstrate the advantages of adaptive sensing and to test and verify the performance of the TB scheduling algorithm. It is shown that the gain of adaptive sensing can be realized by the TB scheduler: that is, storms of interest can be revisited more frequently within a relatively short period time compared to conventional scanning.
C1 [Reinoso-Rondinel, Ricardo; Yu, Tian-You; Torres, Sebastian] Univ Oklahoma, Atmospher Radar Res Ctr, Norman, OK 73072 USA.
[Reinoso-Rondinel, Ricardo; Yu, Tian-You; Torres, Sebastian] Univ Oklahoma, Sch Elect & Comp Engn, Norman, OK 73072 USA.
[Torres, Sebastian] Univ Oklahoma, Cooperat Inst Mesoscale Meteorol Studies, Norman, OK 73072 USA.
[Torres, Sebastian] NOAA, OAR, Natl Severe Storms Lab, Norman, OK USA.
RP Reinoso-Rondinel, R (reprint author), Univ Oklahoma, Atmospher Radar Res Ctr, Room 5900,120 David L Boren Blvd, Norman, OK 73072 USA.
EM rein3@ou.edu
FU NOAA/NSSL [NA17RJ1227]; DOD, EPSCoR [N00014-06-1-0590]
FX This work was primarily supported by NOAA/NSSL under Cooperative
Agreement NA17RJ1227. Part of this work was supported by DOD, EPSCoR
Grant N00014-06-1-0590.
NR 38
TC 7
Z9 7
U1 0
U2 2
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0739-0572
EI 1520-0426
J9 J ATMOS OCEAN TECH
JI J. Atmos. Ocean. Technol.
PD NOV
PY 2010
VL 27
IS 11
BP 1854
EP 1867
DI 10.1175/2010JTECHA1420.1
PG 14
WC Engineering, Ocean; Meteorology & Atmospheric Sciences
SC Engineering; Meteorology & Atmospheric Sciences
GA 680PX
UT WOS:000284248000005
ER
PT J
AU Hood, K
Torres, S
Palmer, R
AF Hood, Kenta
Torres, Sebastian
Palmer, Robert
TI Automatic Detection of Wind Turbine Clutter for Weather Radars
SO JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY
LA English
DT Article
ID CLASSIFICATION; SPECTRA
AB Wind turbines cause contamination of weather radar signals that is often detrimental and difficult to distinguish from cloud returns. Because the turbines are always at the same location, it would seem simple to identify where wind turbine clutter (WTC) contaminates the weather radar data. However, under certain atmospheric conditions, anomalous propagation of the radar beam can occur such that WTC corrupts weather data on constantly evolving locations, or WTC can be relatively weak such that contamination on predetermined locations does not occur. Because of the deficiency of using turbine locations as a proxy for WTC, an effective detection algorithm is proposed to perform automatic flagging of contaminated weather radar data, which can then be censored or filtered. Thus, harmful effects can be reduced that may propagate to automatic algorithms or may hamper the forecaster's ability to issue timely warnings. In this work, temporal and spectral features related to WTC signatures are combined in a fuzzy logic algorithm to classify the radar return as being contaminated by WTC or not. The performance of the algorithm is quantified using simulations and the algorithm is applied to a real data case from the radar facility in Dodge City, Kansas (KDDC). The results illustrate that WTC contamination can be detected automatically, thereby improving the quality control of weather radar data.
C1 [Hood, Kenta] Univ Oklahoma, Sch Elect & Comp Engn, Norman, OK 73019 USA.
[Hood, Kenta; Torres, Sebastian; Palmer, Robert] Univ Oklahoma, Atmospher Radar Res Ctr, Norman, OK 73019 USA.
[Torres, Sebastian] Univ Oklahoma, Cooperat Inst Mesoscale Meteorol Studies, Norman, OK 73019 USA.
[Torres, Sebastian] NOAA, OAR, Natl Severe Storms Lab, Norman, OK USA.
[Palmer, Robert] Univ Oklahoma, Sch Meteorol, Norman, OK 73019 USA.
RP Torres, S (reprint author), Natl Weather Ctr, 120 David L Boren Blvd, Norman, OK 73072 USA.
EM sebastian.torres@noaa.gov
FU NOAA/Office of Oceanic and Atmospheric Research under NOAA-University of
Oklahoma [NA17RJ1227]; U.S. Department of Commerce
FX The authors thank the three anonymous reviewers for their useful
suggestions and the Radar Operations Center of the National Weather
Service for their work in studying the impacts of WTC and their
assistance in carrying out experiments to collect WTC data. Additional
thanks go to Khoi Le and Boon Leng Cheong for their work in simulating
WTC; Brad Isom, who prepared and provided the Dodge City, Kansas, radar
data; and Feng Nai for his comments regarding the analysis of the
results. Funding was provided by the NOAA/Office of Oceanic and
Atmospheric Research under NOAA-University of Oklahoma Cooperative
Agreement NA17RJ1227, U.S. Department of Commerce.
NR 24
TC 17
Z9 18
U1 1
U2 13
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0739-0572
J9 J ATMOS OCEAN TECH
JI J. Atmos. Ocean. Technol.
PD NOV
PY 2010
VL 27
IS 11
BP 1868
EP 1880
DI 10.1175/2010JTECHA1437.1
PG 13
WC Engineering, Ocean; Meteorology & Atmospheric Sciences
SC Engineering; Meteorology & Atmospheric Sciences
GA 680PX
UT WOS:000284248000006
ER
PT J
AU Dash, P
Ignatov, A
Kihai, Y
Sapper, J
AF Dash, Prasanjit
Ignatov, Alexander
Kihai, Yury
Sapper, John
TI The SST Quality Monitor (SQUAM)
SO JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY
LA English
DT Article
ID SEA-SURFACE TEMPERATURE; EMITTED RADIANCE INTERFEROMETER;
HIGH-RESOLUTION; IN-SITU; MATCHUP DATABASE; SKIN TEMPERATURE;
CALIBRATION DATA; REAL-TIME; SATELLITE; ACCURACY
AB The National Environmental Satellite, Data, and Information Service (NESDIS) has been operationally generating sea surface temperature (SST) products (T(S)) from the Advanced Very High Resolution Radiometers (AVHRR) onboard NOAA and MetOp-A satellites since the early 1980s. Customarily, T(S) are validated against in situ SSTs. However, in situ data are sparse and are not available globally in near real time (NRT). This study describes a complementary SST Quality Monitor (SQUAM), which employs global level 4 (L4) SST fields as a reference standard (T(R)) and performs statistical analyses of the differences Delta T(S) = T(S) - T(R). The results are posted online in NRT. The T(S) data that are analyzed are the heritage National Environmental Satellite, Data. and Information Service (NESDIS) SST products from NOAA-16, -17, -18, and -19 and MetOp-A from 2001 to the present. The T(R) fields include daily Reynolds, real-time global (RTG), Operational Sea Surface Temperature and Sea Ice Analysis (OSTIA), and Ocean Data Analysis System for Marine Environment and Security for the European Area (MERSEA) (ODYSSEA) analyses. Using multiple fields facilitates the distinguishing of artifacts in satellite SSTs from those in the L4 products. Global distributions of Delta T(S) are mapped and their histograms are analyzed for proximity to Gaussian shape. Outliers are handled using robust statistics, and the Gaussian parameters are trended in time to monitor SST products for stability and consistency. Additional T(S) checks are performed to identify retrieval artifacts by plotting Delta T(S) versus observational parameters. Cross-platform T(S) biases are evaluated using double differences, and cross-L4 T(R) differences are assessed using Hovmoller diagrams. SQUAM results compare well with the customary in situ validation. All satellite products show a high degree of self- and cross-platform consistency, except for NOAA-16, which has flown close to the terminator in recent years and whose AVHRR is unstable.
C1 [Dash, Prasanjit] NOAA, CSU, CIRA Res Scientist 2, NESDIS,STAR,WWB,Ctr Satellite Applicat & Res, Camp Springs, MD 20746 USA.
[Dash, Prasanjit] Colorado State Univ, Cooperat Inst Res Atmospheres, Ft Collins, CO 80523 USA.
[Kihai, Yury] Perot Syst Govt Serv, Fairfax, VA USA.
[Sapper, John] NOAA, NESDIS, Off Satellite Data Proc & Distribut, Camp Springs, MD USA.
RP Dash, P (reprint author), NOAA, CSU, CIRA Res Scientist 2, NESDIS,STAR,WWB,Ctr Satellite Applicat & Res, Room 601-1,5200 Auth Rd, Camp Springs, MD 20746 USA.
EM prasanjit.dash@noaa.gov
RI Dash, Prasanjit/F-5582-2010; Ignatov, Alexander/F-5594-2010
OI Ignatov, Alexander/0000-0002-7463-5944
FU Product System Development and Implementation program; Internal
Government Studies; GOES-R Algorithm Working Group
FX This work was supported by the Product System Development and
Implementation program managed by the NESDIS Office of Systems
Development, by the Internal Government Studies managed by the NPOESS
Integrated Program Office, and by the GOES-R Algorithm Working Group. We
thank members of the SST Team (F. Xu, X. Liang, B. Petrenko, N.
Shabanov, J. Stroup, and D. Frey) for helpful discussions and
constructive feedback. P. Dash acknowledges the CIRA visiting scientist
fellowship. We would also like to thank the anonymous reviewers for
their comments. The views, opinions, and findings contained in this
report are those of the authors and should not be construed as an
official NOAA or U.S. Government position, policy, or decision.
NR 47
TC 21
Z9 23
U1 0
U2 4
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0739-0572
J9 J ATMOS OCEAN TECH
JI J. Atmos. Ocean. Technol.
PD NOV
PY 2010
VL 27
IS 11
BP 1899
EP 1917
DI 10.1175/2010JTECHO756.1
PG 19
WC Engineering, Ocean; Meteorology & Atmospheric Sciences
SC Engineering; Meteorology & Atmospheric Sciences
GA 680PX
UT WOS:000284248000009
ER
PT J
AU Zou, CZ
Wang, WH
AF Zou, Cheng-Zhi
Wang, Wenhui
TI Stability of the MSU-Derived Atmospheric Temperature Trend
SO JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY
LA English
DT Article
ID MICROWAVE SOUNDING UNIT; TROPOSPHERIC TEMPERATURE; SATELLITE;
CONSTRUCTION; CALIBRATION; VALIDATION; CHANNEL-2
AB Warm target effect and diurnal drift errors are the main sources of uncertainties in the trend determination from the NOAA Microwave Sounding Unit (MSU) observations. Currently, there are two methods to correct the warm target effect: 1) finding a best root-level (level-1c) calibration nonlinearity using simultaneous nadir overpass (SNO) matchups to minimize this effect for each scene radiance, and 2) finding a best-fit empirical relationship between the correction term of the end-level gridded brightness temperature and warm target temperature and then removing the best fit from the unadjusted time series. The former corrects the warm target effect before the diurnal drift adjustment and provides more accurate, warm target effect-minimized, level-1c scene radiances for reanalysis applications. The latter corrects the warm target effect at the end-level merging step, which depend on the diurnal drift correction that occurred at a previous step. Although minimized, the first method still leaves small residual warm target-related errors due to imperfect calibrations. This study demonstrates that when the diurnal drift effect is negligible, a combination of the two methods completely removes warm target effect and produces an invariant trend that is independent of the level-1c calibration in the SNO framework. The conclusion is directly applicable to the MSU channel-2 oceanic midtropospheric temperature (T-2) and global channel-3 upper-tropospheric temperature (T-3) and channel-4 lower-stratospheric temperature (T-4), which satisfy the condition of negligible diurnal drift effect. On the basis of these results, version 1.2 of the National Environmental Satellite, Data, and Information Service (NESDIS)-Center for Satellite Applications and Research (STAR) multisatellite MSU time series was constructed, including all T-2, T-3, and T-4 products. In addition, a diurnal drift correction based on the Remote Sensing Systems diurnal anomalies was applied to the T-2 product, which produces consistent climate trends between land and ocean. The global long-term climate trends for T-2 and T-4 derived from the STAR V1.2 dataset are, respectively, 0.18 +/- 0.05 and -0.39 +/- 0.36 K decade(-1) during 1979-2006; the T-3 trend is 0.11 +/- 0.08 K decade(-1) for 1981-2006.
C1 [Zou, Cheng-Zhi] NOAA, Ctr Satellite Applicat & Res, NESDIS, NOAA Sci Ctr, Camp Springs, MD 20746 USA.
[Wang, Wenhui] NOAA, IMSG, NESDIS, Camp Springs, MD 20746 USA.
RP Zou, CZ (reprint author), NOAA, Ctr Satellite Applicat & Res, NESDIS, NOAA Sci Ctr, Room 712,5200 Auth Rd, Camp Springs, MD 20746 USA.
EM cheng-zhi.zou@noaa.gov
RI Wang, Wenhui/D-3240-2012; Zou, Cheng-Zhi/E-3085-2010
NR 26
TC 23
Z9 24
U1 1
U2 4
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0739-0572
J9 J ATMOS OCEAN TECH
JI J. Atmos. Ocean. Technol.
PD NOV
PY 2010
VL 27
IS 11
BP 1960
EP 1971
DI 10.1175/2009JTECHA1333.1
PG 12
WC Engineering, Ocean; Meteorology & Atmospheric Sciences
SC Engineering; Meteorology & Atmospheric Sciences
GA 680PX
UT WOS:000284248000013
ER
PT J
AU Kang, JW
Diky, V
Chirico, RD
Magee, JW
Muzny, CD
Abdulagatov, I
Kazakov, AF
Frenkel, M
AF Kang, Jeong Won
Diky, Vladimir
Chirico, Robert D.
Magee, Joseph W.
Muzny, Chris D.
Abdulagatov, Ilmutdin
Kazakov, Andrei F.
Frenkel, Michael
TI Comment on "Quality Assessment Algorithm for Vapor-Liquid Equilibrium
Data" (Kang, J. W.; Diky, V.; Chirico, R. D.; Magee, J. W.; Muzny, C.
D.; Abdulagatov, I.; Kazakov, AF; Frenkel, M. J. Chem. Eng. Data 2010,
55, 3631-3640) Reply
SO JOURNAL OF CHEMICAL AND ENGINEERING DATA
LA English
DT Editorial Material
C1 [Diky, Vladimir; Chirico, Robert D.; Magee, Joseph W.; Muzny, Chris D.; Abdulagatov, Ilmutdin; Kazakov, Andrei F.; Frenkel, Michael] Natl Inst Stand & Technol, Thermophys Properties Div, Boulder, CO 80305 USA.
[Kang, Jeong Won] Korea Univ, Dept Chem & Biol Engn, Seoul 136701, South Korea.
RP Chirico, RD (reprint author), Natl Inst Stand & Technol, Thermophys Properties Div, Boulder, CO 80305 USA.
EM chirico@jced.acs.org
RI Magee, Joseph/A-8496-2009; Kang, Jeongwon/F-7010-2013
OI Magee, Joseph/0000-0002-9312-8593; Kang, Jeongwon/0000-0002-5161-1122
NR 0
TC 1
Z9 1
U1 0
U2 3
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0021-9568
J9 J CHEM ENG DATA
JI J. Chem. Eng. Data
PD NOV
PY 2010
VL 55
IS 11
BP 5395
EP 5395
DI 10.1021/je100942r
PG 1
WC Thermodynamics; Chemistry, Multidisciplinary; Engineering, Chemical
SC Thermodynamics; Chemistry; Engineering
GA 677UP
UT WOS:000284017600141
ER
PT J
AU Kelly, KA
Small, RJ
Samelson, RM
Qiu, B
Joyce, TM
Kwon, YO
Cronin, MF
AF Kelly, Kathryn A.
Small, R. Justin
Samelson, R. M.
Qiu, Bo
Joyce, Terrence M.
Kwon, Young-Oh
Cronin, Meghan F.
TI Western Boundary Currents and Frontal Air-Sea Interaction: Gulf Stream
and Kuroshio Extension
SO JOURNAL OF CLIMATE
LA English
DT Article
ID SUBTROPICAL MODE WATER; OCEAN-ATMOSPHERE INTERACTION; NORTHERN
RECIRCULATION GYRE; SURFACE TEMPERATURE; STORM-TRACKS; INTERANNUAL
VARIABILITY; DECADAL VARIABILITY; HEAT-TRANSPORT;
SATELLITE-OBSERVATIONS; STRATIFORM CLOUDINESS
AB In the Northern Hemisphere midlatitude western boundary current (WBC) systems there is a complex interaction between dynamics and thermodynamics and between atmosphere and ocean. Their potential contribution to the climate system motivated major parallel field programs in both the North Pacific [Kuroshio Extension System Study (KESS)] and the North Atlantic [ Climate Variability and Predictability (CLIVAR) Mode Water Dynamics Experiment (CLIMODE)], and preliminary observations and analyses from these programs highlight that complexity. The Gulf Stream (GS) in the North Atlantic and the Kuroshio Extension (KE) in the North Pacific have broad similarities, as subtropical gyre WBCs, but they also have significant differences, which affect the regional air-sea exchange processes and their larger-scale interactions. The 15-yr satellite altimeter data record, which provides a rich source of information, is combined here with the longer historical record from in situ data to describe and compare the current systems. While many important similarities have been noted on the dynamic and thermodynamic aspects of the time-varyingGS and KE, some not-so-subtle differences exist in current variability, mode water properties, and recirculation gyre structure. This paper provides a comprehensive comparison of these two current systems from both dynamical and thermodynamical perspectives with the goal of developing and evaluating hypotheses about the physics underlying the observed differences, and exploring the WBC's potential to influence midlatitude sea-air interaction. Differences between the GS and KE systems offer opportunities to compare the dominant processes and thereby to advance understanding of their role in the climate system.
C1 [Kelly, Kathryn A.] Univ Washington, Appl Phys Lab, Seattle, WA 98195 USA.
[Small, R. Justin] USN, Jacobs Technol, Res Lab, Stennis Space Ctr, MS 39529 USA.
[Samelson, R. M.] Oregon State Univ, COAS, Corvallis, OR 97331 USA.
[Qiu, Bo] Univ Hawaii Manoa, Honolulu, HI 96822 USA.
[Joyce, Terrence M.; Kwon, Young-Oh] WHOI, Woods Hole, MA USA.
[Cronin, Meghan F.] NOAA, PMEL, Seattle, WA USA.
RP Kelly, KA (reprint author), Univ Washington, Appl Phys Lab, POB 355640, Seattle, WA 98195 USA.
EM kkelly@apl.washington.edu
RI Kwon, Young-Oh/C-2190-2008; Qiu, Bo/D-9569-2017
OI Kwon, Young-Oh/0000-0002-1241-2817;
FU NASA [1267196, NNX08AR30G, 1207881]; NSF [OCE-0424912, OCE-0424516,
OCE-0220680, OCE-0424865]; WHOI Ocean Climate Change Institute
FX KAK was supported by NASA Contracts 1267196 and NNX08AR30G and by NSF
Grant OCE-0424912 (CLIMODE). RMS was supported by NSF Grant OCE-0424516.
BQ was supported by NSF Grant OCE-0220680 and by NASA Contract 1207881.
TJ was supported by NSF Grant OCE-0424865. Y-OK was supported by the
Claudia Heyman Fellowship of the WHOI Ocean Climate Change Institute.
NR 100
TC 82
Z9 85
U1 3
U2 21
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0894-8755
J9 J CLIMATE
JI J. Clim.
PD NOV
PY 2010
VL 23
IS 21
BP 5644
EP 5667
DI 10.1175/2010JCLI3346.1
PG 24
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 683HG
UT WOS:000284463700006
ER
PT J
AU Kanzow, T
Cunningham, SA
Johns, WE
Hirschi, JJM
Marotzke, J
Baringer, MO
Meinen, CS
Chidichimo, MP
Atkinson, C
Beal, LM
Bryden, HL
Collins, J
AF Kanzow, T.
Cunningham, S. A.
Johns, W. E.
Hirschi, J. J. -M.
Marotzke, J.
Baringer, M. O.
Meinen, C. S.
Chidichimo, M. P.
Atkinson, C.
Beal, L. M.
Bryden, H. L.
Collins, J.
TI Seasonal Variability of the Atlantic Meridional Overturning Circulation
at 26.5 degrees N
SO JOURNAL OF CLIMATE
LA English
DT Article
ID WESTERN BOUNDARY CURRENT; TROPICAL NORTH-ATLANTIC; OCEAN HEAT-TRANSPORT;
THERMOHALINE CIRCULATION; ROSSBY WAVES; HYDROGRAPHIC DATA; SUBTROPICAL
GYRE; MASS TRANSPORTS; FLORIDA CURRENT; BOTTOM WATER
AB The Atlantic meridional overturning circulation (AMOC) makes the strongest oceanic contribution to the meridional redistribution of heat. Here, an observation-based, 48-month-long time series of the vertical structure and strength of the AMOC at 26.5 degrees N is presented. From April 2004 to April 2008, the AMOC had a mean strength of 18.7 +/- 2.1 Sv (1 Sv equivalent to 10(6) m(3) s(-1)) with fluctuations of 4.8 Sv rms. The best guess of the peak-to-peak amplitude of the AMOC seasonal cycle is 6.7 Sv, with a maximum strength in autumn and a minimum in spring. While seasonality in the AMOC was commonly thought to be dominated by the northward Ekman transport, this study reveals that fluctuations of the geostrophic midocean and Gulf Stream transports of 2.2 and 1.7 Sv rms, respectively, are substantially larger than those of the Ekman component (1.2 Sv rms). A simple model based on linear dynamics suggests that the seasonal cycle is dominated by wind stress curl forcing at the eastern boundary of the Atlantic. Seasonal geostrophic AMOC anomalies might represent an important and previously underestimated component of meridional transport and storage of heat in the subtropical North Atlantic. There is evidence that the seasonal cycle observed here is representative of much longer intervals. Previously, hydrographic snapshot estimates between 1957 and 2004 had suggested a long-term decline of the AMOC by 8 Sv. This study suggests that aliasing of seasonal AMOC anomalies might have accounted for a large part of the inferred slowdown.
C1 [Kanzow, T.] Univ Kiel, Leibniz Inst Meereswissensch, D-24105 Kiel, Germany.
[Kanzow, T.; Cunningham, S. A.; Hirschi, J. J. -M.; Atkinson, C.; Bryden, H. L.] Natl Oceanog Ctr Southampton, Ocean Observat & Climate Grp, Southampton, Hants, England.
[Johns, W. E.; Beal, L. M.] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Div Meteorol & Phys Oceanog, Miami, FL 33149 USA.
[Marotzke, J.; Chidichimo, M. P.] Max Planck Inst Meteorol, Hamburg, Germany.
[Baringer, M. O.; Meinen, C. S.] NOAA, Atlantic Oceanog & Meteorol Lab, Phys Oceanog Div, Miami, FL 33149 USA.
[Collins, J.] British Oceanog Data Ctr, Liverpool, Merseyside, England.
RP Kanzow, T (reprint author), Univ Kiel, Leibniz Inst Meereswissensch, Dusternbrooker Weg 20, D-24105 Kiel, Germany.
EM tkanzow@ifm-geomar.de
RI Meinen, Christopher/G-1902-2012; Hirschi, Joel/F-5631-2013; Baringer,
Molly/D-2277-2012;
OI Meinen, Christopher/0000-0002-8846-6002; Hirschi,
Joel/0000-0003-1481-3697; Baringer, Molly/0000-0002-8503-5194;
Chidichimo, Maria Paz/0000-0002-4745-9017
FU Natural Environment Research Council (NERC) [880 NER/T/S/2002/00481];
U.S. National Science Foundation (NSF) [0728108]; U.S. National Oceanic
and Atmospheric Administration; NOAA Office of Climate Observation
FX The authors thank the captains and crews of the R/Vs Charles Darwin,
Discovery, Ronald H. Brown, Knorr, Poseidon, and Seward Johnson; and the
UKORS, RSMAS, and AOML mooring and hydrography teams. The mooring
operations have been supported by the Natural Environment Research
Council (NERC) RAPID program, the U.S. National Science Foundation (NSF)
under Grant 0728108, and the U.S. National Oceanic and Atmospheric
Administration Western Boundary Time Series program. The Florida Current
cable data are made freely available by the Atlantic Oceanographic and
Meteorological Laboratory (available online at
www.aoml.noaa.gov/phod/floridacurrent/) and are funded by the NOAA
Office of Climate Observation. The wind stress data were obtained from
CERSAT at IFREMER, Plouzane (France). We thank Darren Rayner (NOCS) for
coordinating the U.K. seagoing activities and for leading the mooring
data recovery. Two of the authors (TK and JJMH) were supported in the
framework of the NERC-funded Rapid Climate Change Program (Grant 880
NER/T/S/2002/00481). We thank the two anonymous reviewers for their
detailed criticism, which led to significant improvement of the
manuscript.
NR 69
TC 132
Z9 132
U1 5
U2 40
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0894-8755
J9 J CLIMATE
JI J. Clim.
PD NOV
PY 2010
VL 23
IS 21
BP 5678
EP 5698
DI 10.1175/2010JCLI3389.1
PG 21
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 683HG
UT WOS:000284463700008
ER
PT J
AU Rawlins, MA
Steele, M
Holland, MM
Adam, JC
Cherry, JE
Francis, JA
Groisman, PY
Hinzman, LD
Huntington, TG
Kane, DL
Kimball, JS
Kwok, R
Lammers, RB
Lee, CM
Lettenmaier, DP
McDonald, KC
Podest, E
Pundsack, JW
Rudels, B
Serreze, MC
Shiklomanov, A
Skagseth, O
Troy, TJ
Vorosmarty, CJ
Wensnahan, M
Wood, EF
Woodgate, R
Yang, DQ
Zhang, K
Zhang, TJ
AF Rawlins, Michael A.
Steele, Michael
Holland, Marika M.
Adam, Jennifer C.
Cherry, Jessica E.
Francis, Jennifer A.
Groisman, Pavel Ya.
Hinzman, Larry D.
Huntington, Thomas G.
Kane, Douglas L.
Kimball, John S.
Kwok, Ron
Lammers, Richard B.
Lee, Craig M.
Lettenmaier, Dennis P.
McDonald, Kyle C.
Podest, Erika
Pundsack, Jonathan W.
Rudels, Bert
Serreze, Mark C.
Shiklomanov, Alexander
Skagseth, Oystein
Troy, Tara J.
Voeroesmarty, Charles J.
Wensnahan, Mark
Wood, Eric F.
Woodgate, Rebecca
Yang, Daqing
Zhang, Ke
Zhang, Tingjun
TI Analysis of the Arctic System for Freshwater Cycle Intensification:
Observations and Expectations
SO JOURNAL OF CLIMATE
LA English
DT Article
ID MACKENZIE RIVER-BASIN; MOORED CURRENT METERS; PAST 4 DECADES;
NORTHERN-HEMISPHERE; HYDROLOGIC-CYCLE; CLIMATE-CHANGE; SEA-ICE; ATLANTIC
INFLOW; BEAUFORT GYRE; HEAT FLUXES
AB Hydrologic cycle intensification is an expected manifestation of a warming climate. Although positive trends in several global average quantities have been reported, no previous studies have documented broad intensification across elements of the Arctic freshwater cycle (FWC). In this study, the authors examine the character and quantitative significance of changes in annual precipitation, evapotranspiration, and river discharge across the terrestrial pan-Arctic over the past several decades from observations and a suite of coupled general circulation models (GCMs). Trends in freshwater flux and storage derived from observations across the Arctic Ocean and surrounding seas are also described.
With few exceptions, precipitation, evapotranspiration, and river discharge fluxes from observations and the GCMs exhibit positive trends. Significant positive trends above the 90% confidence level, however, are not present for all of the observations. Greater confidence in the GCM trends arises through lower interannual variability relative to trend magnitude. Put another way, intrinsic variability in the observations tends to limit confidence in trend robustness. Ocean fluxes are less certain, primarily because of the lack of long-term observations. Where available, salinity and volume flux data suggest some decrease in saltwater inflow to the Barents Sea (i.e., a decrease in freshwater outflow) in recent decades. A decline in freshwater storage across the central Arctic Ocean and suggestions that large-scale circulation plays a dominant role in freshwater trends raise questions as to whether Arctic Ocean freshwater flows are intensifying. Although oceanic fluxes of freshwater are highly variable and consistent trends are difficult to verify, the other components of the Arctic FWC do show consistent positive trends over recent decades. The broad-scale increases provide evidence that the Arctic FWCis experiencing intensification. Efforts that aim to develop an adequate observation system are needed to reduce uncertainties and to detect and document ongoing changes in all system components for further evidence of Arctic FWC intensification.
C1 [Rawlins, Michael A.] Dartmouth Coll, Dept Earth Sci, Hanover, NH 03755 USA.
[Steele, Michael; Wensnahan, Mark; Woodgate, Rebecca] Univ Washington, Appl Phys Lab, Polar Sci Ctr, Seattle, WA 98105 USA.
[Holland, Marika M.] Natl Ctr Atmospher Res, Boulder, CO 80307 USA.
[Adam, Jennifer C.] Washington State Univ, Dept Civil & Environm Engn, Pullman, WA 99164 USA.
[Cherry, Jessica E.; Hinzman, Larry D.] Univ Alaska Fairbanks, Int Arctic Res Ctr, Fairbanks, AK USA.
[Francis, Jennifer A.] Rutgers State Univ, Inst Marine & Coastal Sci, Highlands, NJ USA.
[Groisman, Pavel Ya.] UCAR, Natl Climat Data Ctr, Asheville, NC USA.
[Huntington, Thomas G.] US Geol Survey, Augusta, ME USA.
[Kane, Douglas L.; Yang, Daqing] Univ Alaska Fairbanks, Inst No Engn, Water & Environm Res Ctr, Fairbanks, AK USA.
[Kimball, John S.; Zhang, Ke] Univ Montana, Numer Terradynam Simulat Grp, Missoula, MT 59812 USA.
[Kwok, Ron; McDonald, Kyle C.; Podest, Erika] CALTECH, Jet Prop Lab, Pasadena, CA USA.
[Lammers, Richard B.; Pundsack, Jonathan W.; Shiklomanov, Alexander] Univ New Hampshire, Inst Study Earth Oceans & Space, Water Syst Anal Grp, Durham, NH 03824 USA.
[Lee, Craig M.] Univ Washington, Appl Phys Lab, Ocean Phys Dept, Seattle, WA 98105 USA.
[Lettenmaier, Dennis P.] Univ Washington, Dept Civil & Environm Engn, Seattle, WA 98105 USA.
[Rudels, Bert] Univ Helsinki, Dept Phys Sci, Helsinki, Finland.
[Rudels, Bert] Finnish Meteorol Inst, FIN-00101 Helsinki, Finland.
[Serreze, Mark C.; Zhang, Tingjun] Univ Colorado, Cooperat Inst Res Environm Sci, Natl Snow & Ice Data Ctr, Boulder, CO 80309 USA.
[Skagseth, Oystein] Inst Marine Res, N-5024 Bergen, Norway.
[Skagseth, Oystein] Bjerknes Ctr Climate Res, Bergen, Norway.
[Troy, Tara J.; Wood, Eric F.] Princeton Univ, Dept Civil & Environm Engn, Princeton, NJ 08544 USA.
[Voeroesmarty, Charles J.] CUNY, Dept Civil Engn, New York, NY 10021 USA.
RP Rawlins, MA (reprint author), Univ Massachusetts, Dept Geosci, Amherst, MA 01003 USA.
EM rawlins@geo.umass.edu
RI Kwok, Ron/A-9762-2008; Zhang, Ke/B-3227-2012; Hinzman,
Larry/B-3309-2013; lettenmaier, dennis/F-8780-2011; Shiklomanov,
Alexander/C-5521-2014;
OI Kwok, Ron/0000-0003-4051-5896; Zhang, Ke/0000-0001-5288-9372; Hinzman,
Larry/0000-0002-5878-6814; lettenmaier, dennis/0000-0003-3317-1327;
Troy, Tara/0000-0001-5366-0633; Huntington, Thomas/0000-0002-9427-3530
FU National Science Foundation's Office of Polar Programs; NASA
[NNG06GE43G, NNH04AA66I, NNH08AI57I, NNX08AN58G]; NSF [ARC-0531040,
ARC-0531302, ARC-0612062, ARC-0629471, ARC-0632154, ARC-0632231,
ARC-0633885, ARC-0652838, ARC-0805789, OPP-0229705, OPP-0230083,
OPP-0230211, OPP-0230381, OPP-0328686, OPP-0335941, OPP-0352754]; New
Hampshire Space Grant Consortium
FX We acknowledge the modeling groups, the Program for Climate Model
Diagnosis and Intercomparison (PCMDI) and the WCRP's Working Group on
Coupled Modeling (WGCM) for their roles in making available the WCRP
CMIP3 multimodel dataset. Support of this dataset is provided by the
Office of Science, U.S. Department of Energy. We gratefully acknowledge
funding from the National Science Foundation's Office of Polar Programs
through the Freshwater Integration Project and from NASA's Cryosphere
Program. Funding was provided through NSF Grants ARC-0531040,
ARC-0531302, ARC-0612062, ARC-0629471, ARC-0632154, ARC-0632231,
ARC-0633885, ARC-0652838, ARC-0805789, OPP-0229705, OPP-0230083,
OPP-0230211, OPP-0230381, OPP-0328686, OPP-0335941, and OPP-0352754 and
NASA Grants NNG06GE43G, NNH04AA66I, NNH08AI57I, and NNX08AN58G. The lead
author was supported by fellowships from the NASA Postdoctoral Program
and the New Hampshire Space Grant Consortium. Portions of this work were
carried out at the Jet Propulsion Laboratory, California Institute of
Technology, under contract with the National Aeronautics and Space
Administration. Any use of trade, product, or firm names in this
publication is for descriptive purposes only and does not imply
endorsement by the U.S. Government.
NR 154
TC 99
Z9 99
U1 5
U2 50
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0894-8755
EI 1520-0442
J9 J CLIMATE
JI J. Clim.
PD NOV
PY 2010
VL 23
IS 21
BP 5715
EP 5737
DI 10.1175/2010JCLI3421.1
PG 23
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 683HG
UT WOS:000284463700010
ER
PT J
AU Smith, TM
Arkin, PA
Sapiano, MRP
Chang, CY
AF Smith, Thomas M.
Arkin, Phillip A.
Sapiano, Mathew R. P.
Chang, Ching-Yee
TI Merged Statistical Analyses of Historical Monthly Precipitation
Anomalies Beginning 1900
SO JOURNAL OF CLIMATE
LA English
DT Article
ID GLOBAL PRECIPITATION; DATASET; CYCLE
AB A monthly reconstruction of precipitation beginning in 1900 is presented. The reconstruction resolves interannual and longer time scales and spatial scales larger than 58 over both land and oceans. Because of different land and ocean data availability, the reconstruction combines two separate historical reconstructions. One analyzes interannual variations directly by fitting gauge-based anomalies to large-scale spatial modes. This direct reconstruction is used for land anomalies and interannual oceanic anomalies. The other analyzes annual and longer variations indirectly from correlations with analyzed sea surface temperature and sea level pressure. This indirect reconstruction is used for oceanic variations with time scales longer than interannual. In addition, a method of estimating reconstruction errors is also presented.
Over land the reconstruction is a filtered representation of the gauge data with data gaps filled. Over oceans the reconstruction gives an estimate of the atmospheric response to changing temperature and pressure, combined with interannual variations. The reconstruction makes it possible to evaluate global precipitation variations for periods much longer than the satellite period, which begins in 1979. Evaluations show some large-scale similarities with coupled model precipitation variations over the twentieth century, including an increasing tendency over the century. The reconstructed land and sea trends tend to be out of phase at low latitudes, similar to the out-of-phase relationship for interannual variations. This reconstruction may be used for climate monitoring, for statistical climate studies of the twentieth century, and for helping to evaluate dynamic climate models. In the future the possibility of improving the reconstruction will be explored by further improving the analysis methods and including additional data.
C1 [Smith, Thomas M.] NOAA, NESDIS, STAR, SCSB, College Pk, MD 20740 USA.
[Smith, Thomas M.; Arkin, Phillip A.; Sapiano, Mathew R. P.] Univ Maryland, CICS ESSIC, College Pk, MD 20742 USA.
[Chang, Ching-Yee] Univ Calif Berkeley, Dept Geog, Berkeley, CA 94720 USA.
RP Smith, TM (reprint author), NOAA, NESDIS, STAR, SCSB, 5825 Univ Res Ct,Suite 4001, College Pk, MD 20740 USA.
EM tom.smith@noaa.gov
RI Smith, Thomas M./F-5626-2010
OI Smith, Thomas M./0000-0001-7469-7849
FU NOAA Climate Program Office; Cooperative Institute for Climate Studies
(NOAA) [NA17EC1483]
FX We thank several centers for making their data easily available for this
study, including the National Climatic Data Center for the GHCN and SST
data, NASA for the GPCP, the Deutscher Wetterdienst for the GPCC, the
University of East Anglia for the CRU, and the Met Office Hadley Centre
for the SLP data (available online at www.metoffice.gov.uk/hadobs). We
also thank R. Vose and two anonymous reviewers for their useful
comments. This project is supported in part by the Climate Change Data
and Diagnostic program element of the NOAA Climate Program Office and
the Cooperative Institute for Climate Studies (NOAA Grant NA17EC1483).
The contents of this paper are solely the opinions of the authors and do
not constitute a statement of policy, decision, or position on behalf of
NOAA or the U.S. Government.
NR 30
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Z9 15
U1 0
U2 5
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0894-8755
J9 J CLIMATE
JI J. Clim.
PD NOV
PY 2010
VL 23
IS 21
BP 5755
EP 5770
DI 10.1175/2010JCLI3530.1
PG 16
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 683HG
UT WOS:000284463700012
ER
PT J
AU Powell, CJ
AF Powell, C. J.
TI Recommended Auger-electron kinetic energies for 42 elemental solids
SO JOURNAL OF ELECTRON SPECTROSCOPY AND RELATED PHENOMENA
LA English
DT Article
DE Auger electron spectroscopy; Auger energies; Elemental solids
ID RAY PHOTOELECTRON SPECTROMETERS; SURFACE CHEMICAL-ANALYSIS; ISO/TC-201
STANDARD; CALIBRATION; SPECTRA; AES; REEVALUATION; SELENIUM
AB An analysis is presented of Auger-electron kinetic energies (KEs) from four data sources for 65 Auger transitions in 45 elemental solids For each data source a single instrument had been used to measure KEs for many elements In order to compare KEs from two sources it was necessary to recalibrate the energy scales of each instrument using recommended reference data Mean KEs are given for most of the Auger transitions for which there were at least two independent measurements and for which differences from the mean KEs were considered acceptably small In several cases comparisons were made to published KE data to resolve discrepancies We are able to recommend mean KEs for 59 Auger transitions from 42 elemental solids and to provide estimates of the uncertainties of these KEs This compilation should be useful for the determination of chemical shifts of Auger peaks in Auger electron spectroscopy and X-ray photoelectron spectroscopy (C) 2010 Elsevier B V All rights reserved
C1 Natl Inst Stand & Technol, Surface & Microanal Sci Div, Gaithersburg, MD 20899 USA.
RP Powell, CJ (reprint author), Natl Inst Stand & Technol, Surface & Microanal Sci Div, 100 Bur Dr,Stop 8370, Gaithersburg, MD 20899 USA.
NR 29
TC 7
Z9 7
U1 3
U2 15
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0368-2048
J9 J ELECTRON SPECTROSC
JI J. Electron Spectrosc. Relat. Phenom.
PD NOV
PY 2010
VL 182
IS 1-2
BP 11
EP 18
DI 10.1016/j.elspec.2010.05.012
PG 8
WC Spectroscopy
SC Spectroscopy
GA 687BU
UT WOS:000284749600003
ER
PT J
AU Morrow, JB
Arango, C
Holbrook, RD
AF Morrow, Jayne B.
Arango P, Catalina
Holbrook, R. David
TI Association of Quantum Dot Nanoparticles with Pseudomonas aeruginosa
Biofilm
SO JOURNAL OF ENVIRONMENTAL QUALITY
LA English
DT Article
ID MICROBIAL BIOFILMS; POROUS-MEDIA; BACTERIAL BIOFILMS; FOOD-WEB;
ENVIRONMENT; DEFORMATION; MECHANISMS; DIFFUSION; TRANSPORT; PROTEINS
AB Quantum dots (QDs) of two different surface chemistries (carboxyl [COOH] and polyethylene glycol [PEG] modified) were utilized to determine the impact of surface functionality on QD mobility and distribution in Pseudomonas aeruginosa PAO1 biofilms. Confocal laser scanning microscopy was utilized to evaluate QD association with biofilm components (proteins, cells, and polysaccharides). Quantum dots did not preferentially associate with cell surfaces compared but did colocalize with extracellular proteins in the biofilm matrix. Neither PEG nor COOH QDs were found to be internalized by individual bacterial cells. Neither QD functionality nor flow rate of QD application (0.3 mL min(-1) or 3.0 mL min(-1)) resulted in a marked difference in QD association with I? aeruginosa biofilms. However, center of density determinations indicated COOH QDs could more easily penetrate the biofilm matrix by diffusion than PEG QDs. Biofilms with PEG QDs associated had rougher polysaccharide layers and rougher cell distribution than biofilms with COOH QDs. This work suggests natural biofilms may serve as deposition locations in natural and engineered environmental systems, and biofilm structural parameters may change based on exposure to nanomaterials of varied physical characteristics.
C1 [Morrow, Jayne B.] NIST, Div Biochem Sci, Gaithersburg, MD 20878 USA.
[Arango P, Catalina] Univ Connecticut, Dep Mol & Cell Biol, Storrs, CT 06269 USA.
[Holbrook, R. David] NIST, Surface & Microanal Div, Gaithersburg, MD 20878 USA.
RP Morrow, JB (reprint author), NIST, Div Biochem Sci, 100 Bur Dr,MS 8312, Gaithersburg, MD 20878 USA.
EM jmorrow@nist.gov
NR 37
TC 16
Z9 16
U1 0
U2 23
PU AMER SOC AGRONOMY
PI MADISON
PA 677 S SEGOE RD, MADISON, WI 53711 USA
SN 0047-2425
J9 J ENVIRON QUAL
JI J. Environ. Qual.
PD NOV-DEC
PY 2010
VL 39
IS 6
BP 1934
EP 1941
DI 10.2134/jeq2009.0455
PG 8
WC Environmental Sciences
SC Environmental Sciences & Ecology
GA 676FU
UT WOS:000283897200007
PM 21284290
ER
PT J
AU Sharma, R
Liermann, M
AF Sharma, R.
Liermann, M.
TI Using hierarchical models to estimate effects of ocean anomalies on
north-west Pacific Chinook salmon Oncorhynchus tshawytscha recruitment
SO JOURNAL OF FISH BIOLOGY
LA English
DT Article
DE Bayesian; climate change; meta-analysis; productivity; Ricker; sea
surface temperature
ID SOCKEYE-SALMON; SURVIVAL; CLIMATE; KISUTCH; RIVER; RATES
AB The high variability in survival over the past three decades of north-west Pacific Chinook salmon Oncorhynchus tshawytscha is summarized for 24 stocks and analysed using hierarchical Bayesian models. Results from a simple model indicate that recruitment anomalies appear to be correlated in time and space. A simple model with a covariate based on basin-scale effects (Pacific Decadal Oscillation and El Nino Southern Oscillation) and local-scale effects (sea surface temperature, SST anomaly) was introduced to explain this variability. The model still exhibited residual patterns that were removed when a random-walk component was added to the model. The analysis indicates that recruitment is negatively related to SST anomaly for all stocks and the effect of basin-scale variables is negligible. The effect of climate over the next century is expected to result in estimated recruitment declining by an average of 13% for O. tshawytscha stocks coastwide.
C1 [Sharma, R.] Columbia River Intertribal Fish Commiss, Portland, OR 97232 USA.
[Liermann, M.] NOAA, Fish Ecol Div, NW Fisheries Sci Ctr, Natl Marine Fisheries Serv, Seattle, WA 98112 USA.
RP Sharma, R (reprint author), Columbia River Intertribal Fish Commiss, 729 NE Oregon St,Suite 200, Portland, OR 97232 USA.
EM shar@critfc.org
FU Bonneville Power Administration (BPA)
FX The authors would like to thank D. Graves [Columbia River Inter-Tribal
Fish Commision (CRITFC), Portland, OR] for generating the map in Fig. 1.
In addition, the authors would like to acknowledge C. Parken (Department
of Fisheries and Oceans Canada) for sharing the spawner-recruitment data
with us, P. Roni (National Oceanic and Atmospheric Administration) for
reviewing this and two anonymous reviewers for very helpful reviews in
improving the manuscript, as well as the Guest Editor, I. Winfield for
making substantial effort in improving the clarity of this manuscript.
Finally, the authors would like to thank Bonneville Power Administration
(BPA) for providing partial funding for this work.
NR 47
TC 3
Z9 3
U1 0
U2 9
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0022-1112
J9 J FISH BIOL
JI J. Fish Biol.
PD NOV
PY 2010
VL 77
IS 8
BP 1948
EP 1963
DI 10.1111/j.1095-8649.2010.02779.x
PG 16
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 681NC
UT WOS:000284321600014
PM 21078100
ER
PT J
AU Atha, DH
Manne, U
Grizzle, WE
Wagner, PD
Srivastava, S
Reipa, V
AF Atha, Donald H.
Manne, Upender
Grizzle, William E.
Wagner, Paul D.
Srivastava, Sudhir
Reipa, Vytas
TI Standards for Immunohistochemical Imaging: A Protein Reference Device
for Biomarker Quantitation
SO JOURNAL OF HISTOCHEMISTRY & CYTOCHEMISTRY
LA English
DT Article
DE p53; immunohistochemistry; standards; cancer biomarker quantitation;
molecular imaging; protein immobilization; spectroscopy; microscopy
ID STORED PARAFFIN SLIDES; STRAND CONFORMATION POLYMORPHISM;
MARKER-IMMUNOSTAINING INTENSITY; P53 POINT MUTATIONS;
CAPILLARY-ELECTROPHORESIS; NUCLEAR ACCUMULATION; COLORECTAL
ADENOCARCINOMA; PROGNOSTIC-SIGNIFICANCE; SILICON NANOPARTICLES;
TELOMERASE ACTIVITY
AB We are developing a reference device to be used in the validation of immunohistochemical imaging of biomarkers by microscopy. The prototype device consists of p53 protein immobilized at various concentrations on a glass slide. The device is designed as a reference control to be used with assays that incorporate commercially available anti-p53 antibodies. p53 protein was characterized by mass spectrometry and covalently immobilized through amide linkage to the (3-aminopropyl)trietoxysilane-modified glass surface. This procedure is reproducible and provides a chemically stable product in high yield. The surface-bound protein was shown to be immunoreactive by its specific interaction with anti-p53 antibody (Ab) and detection by absorbance and fluorescence spectroscopy. Also, comparison was made with microscopic images of Ab-stained tissue samples, known to stain positive for p53. Further development will be required to establish accurate surface protein concentrations in the range required for specific clinical applications. (J Histochem Cytochem 58:1005-1014, 2010)
C1 [Atha, Donald H.; Reipa, Vytas] Natl Inst Stand & Technol, Div Biochem Sci, Gaithersburg, MD 20899 USA.
[Manne, Upender; Grizzle, William E.] Univ Alabama, Dept Pathol, Birmingham, AL 35294 USA.
[Wagner, Paul D.; Srivastava, Sudhir] NCI, Canc Prevent Div, Rockville, MD USA.
RP Atha, DH (reprint author), Natl Inst Stand & Technol, Div Biochem Sci, Bldg 227,Room A243,Mail Stop 8311,100 Bur Dr, Gaithersburg, MD 20899 USA.
EM donald.atha@nist.gov
FU National Cancer Institute-Early Detection Research Network (EDRN);
National Institute of Standards and Technology (NIST)-Biochemical
Science Division [YI-CN5001]; EDRN Reference Laboratory at UAB
[5U24CA086359-10]
FX This work was funded in part by National Cancer Institute-Early
Detection Research Network (EDRN) and National Institute of Standards
and Technology (NIST)-Biochemical Science Division jointly under
interagency agreement no. YI-CN5001 and by the EDRN Reference Laboratory
at UAB (5U24CA086359-10).
NR 46
TC 0
Z9 0
U1 0
U2 6
PU SAGE PUBLICATIONS LTD
PI LONDON
PA 1 OLIVERS YARD, 55 CITY ROAD, LONDON EC1Y 1SP, ENGLAND
SN 0022-1554
J9 J HISTOCHEM CYTOCHEM
JI J. Histochem. Cytochem.
PD NOV
PY 2010
VL 58
IS 11
BP 1005
EP 1014
DI 10.1369/jhc.2010.956342
PG 10
WC Cell Biology
SC Cell Biology
GA 666JV
UT WOS:000283111900006
PM 20805583
ER
PT J
AU Altman, WR
Moreland, J
Russek, SE
Bright, VM
AF Altman, Wendy R.
Moreland, John
Russek, Stephen E.
Bright, Victor M.
TI Optimization of spin-valve parameters for magnetic bead trapping and
manipulation
SO JOURNAL OF MAGNETISM AND MAGNETIC MATERIALS
LA English
DT Article
DE Spin-valve; Magnetic bead; Microfluidic; Magnetic manipulation;
Switchable magnetic trap
ID DETECTION SYSTEM; NANOPARTICLES; SEPARATOR; SENSORS; DEVICES
AB Magneto-optic Kerr effect (MOKE) and magnetoresistance (MR) measurements were used to measure the switching characteristics of spin-valve (SV) arrays currently being developed to trap and release superparamagnetic beads within a fluid medium. The effect of SV size on switching observed by MOKE showed that a 1 mu mx8 mu m SV element was found to have optimal switching characteristics. MR measurements on a single 1 mu mx8 mu m SV switched with either an external applied magnetic field or a local magnetic field generated by an integrated write wire (current density ranging from 10(6) to 10(7) A/cm(2)) confirmed the MOKE findings. The 1 mu mx8 mu m SV low field switching was observed to be +8 and -2 mT with two stable states at zero field; the high field switching was observed to be -18 mT. The low switching fields and the large magnetic moment of the SV trap along with our observation of minimal magnetostatic effects for dense arrays are necessary design characteristics for high-force, switchable-magnet, microfluidic bead trap applications (C) 2010 Elsevier B.V. All rights reserved.
C1 [Altman, Wendy R.; Moreland, John; Russek, Stephen E.] NIST, Boulder, CO 80305 USA.
[Altman, Wendy R.; Bright, Victor M.] Univ Colorado, Boulder, CO 80309 USA.
RP Altman, WR (reprint author), NIST, MS 818-03,325 Broadway, Boulder, CO 80305 USA.
EM wendy.krauser@colorado.edu
NR 16
TC 6
Z9 6
U1 0
U2 7
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0304-8853
J9 J MAGN MAGN MATER
JI J. Magn. Magn. Mater.
PD NOV
PY 2010
VL 322
IS 21
BP 3236
EP 3239
DI 10.1016/j.jmmm.2010.05.043
PG 4
WC Materials Science, Multidisciplinary; Physics, Condensed Matter
SC Materials Science; Physics
GA 640OR
UT WOS:000281061400003
ER
PT J
AU Anderson, CR
Sapiano, MRP
Prasad, MBK
Long, W
Tango, PJ
Brown, CW
Murtugudde, R
AF Anderson, Clarissa R.
Sapiano, Mathew R. P.
Prasad, M. Bala Krishna
Long, Wen
Tango, Peter J.
Brown, Christopher W.
Murtugudde, Raghu
TI Predicting potentially toxigenic Pseudo-nitzschia blooms in the
Chesapeake Bay
SO JOURNAL OF MARINE SYSTEMS
LA English
DT Article
DE Algal blooms; Domoic acid; Amnesic shellfish poisoning; Diatoms;
Prediction; Regression analysis; Chesapeake Bay
ID HARMFUL ALGAL BLOOMS; GULF-OF-MEXICO; DOMOIC ACID PRODUCTION;
PHYSICAL-BIOLOGICAL MODEL; NORTH PACIFIC-OCEAN; KARENIA-BREVIS;
AUSTRALIS BACILLARIOPHYCEAE; ENVIRONMENTAL-CONDITIONS; SILICATE
LIMITATION; ECOSYSTEM MODEL
AB Harmful algal blooms are now recognized as a significant threat to the Chesapeake Bay as they can severely compromise the economic viability of important recreational and commercial fisheries in the largest estuary of the United States This study describes the development of empirical models for the potentially domoic acid producing Pseudo-nitzschia species complex present in the Bay developed from a 22-year time series of cell abundance and concurrent measurements of hydrographic and chemical properties Using a logistic Generalized Linear Model (GLM) approach model parameters and performance were compared over a range of Pseudo nitzschia bloom thresholds relevant to toxin production by different species Small threshold blooms (>= 10cells mL(-1)) are explained by time of year location and variability in surface values of phosphate temperature nitrate plus nitrite and freshwater discharge Medium (100 cells mL(-1)) to large-threshold (1000 cells mL(-1)) blooms are further explained by salinity silicic acid dissolved organic carbon and light attenuation (Secchi) depth These predictors are similar to other models for Pseudo nitzschia blooms on the west coast suggesting commonalities across ecosystems Hindcasts of bloom probabilities at a 19% bloom prediction point yield a Heidke Skill Score of similar to 53% a Probability of Detection similar to 75% a False Alarm Ratio of similar to 52% and a Probability of False Detection similar to 9% The implication of possible future changes in Baywide nutrient stoichiometry on Pseudo-nitzschia blooms is discussed (C) 2010 Elsevier BV All rights reserved
C1 [Anderson, Clarissa R.] Univ Calif Santa Cruz, Ocean Sci Dept, Santa Cruz, CA 95064 USA.
[Anderson, Clarissa R.] Univ S Carolina, Dept Earth & Ocean Sci, Columbia, SC 29208 USA.
[Sapiano, Mathew R. P.] Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA.
[Sapiano, Mathew R. P.] Univ Maryland, ESSIC, CICS, College Pk, MD 20742 USA.
[Long, Wen] Univ Maryland, Ctr Environm Sci, Horn Point Lab, Cambridge, MD 21613 USA.
[Tango, Peter J.] US Environm Protect Agcy, US Geol Survey, Chesapeake Bay Program Off, Annapolis, MD 21403 USA.
[Brown, Christopher W.] Natl Ocean & Atmospher Adm, CICS, College Pk, MD 20740 USA.
RP Anderson, CR (reprint author), Univ Calif Santa Cruz, Ocean Sci Dept, 1156 High St, Santa Cruz, CA 95064 USA.
RI Brown, Christopher/B-8213-2008
OI Brown, Christopher/0000-0002-9905-6391
FU National Research Council; NOAA National Environmental Satellite Data
and Information Service (NESDIS)
FX This study was funded by a National Research Council postdoctoral
fellowship to C R.A. sponsored by the NOAA National Environmental
Satellite Data and Information Service (NESDIS) with additional support
from NOAA MERHAB Award (PI CW B) and the Chesapeake Bay Forecasting
System project (PI It M) The authors gratefully acknowledge the Maryland
Department of Natural Resources and USEPA Chesapeake Bay Program for
contributing monitoring data and we are especially appreciative of the
technical assistance provided by J Johnson B Cole M Naylor W Butler B
Wind M Baith and J Beauchamps J lane D McGillicuddy and several
anonymous reviewers provided comments which greatly improved the paper
We give special thanks to A. Thessen for her innovative work on
Pseudo-nitzschia ecophysiology in the Chesapeake Bay and for significant
input to this manuscript
NR 108
TC 27
Z9 28
U1 8
U2 35
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0924-7963
J9 J MARINE SYST
JI J. Mar. Syst.
PD NOV
PY 2010
VL 83
IS 3-4
SI SI
BP 127
EP 140
DI 10.1016/j.jmarsys.2010.04.003
PG 14
WC Geosciences, Multidisciplinary; Marine & Freshwater Biology;
Oceanography
SC Geology; Marine & Freshwater Biology; Oceanography
GA 679SF
UT WOS:000284180400004
ER
PT J
AU Glibert, PM
Allen, JI
Bouwman, AF
Brown, CW
Flynn, KJ
Lewitus, AJ
Madden, CJ
AF Glibert, Patricia M.
Allen, J. Icarus
Bouwman, A. F.
Brown, Christopher W.
Flynn, Kevin J.
Lewitus, Alan J.
Madden, Christopher J.
TI Modeling of HABs and eutrophication Status, advances, challenges
SO JOURNAL OF MARINE SYSTEMS
LA English
DT Article
DE Algal blooms; Land use; Algal physiology; Nutrient cycling; Forecasts
ID HARMFUL ALGAL BLOOMS; DISSOLVED ORGANIC NITROGEN; COASTAL MARINE
ECOSYSTEMS; SPATIALLY EXPLICIT; GLOBAL-MODEL; FLORIDA BAY; REACTIVE
NITROGEN; NARRAGANSETT-BAY; SKILL ASSESSMENT; NUTRIENT EXPORT
AB Harmful algal blooms (HABs) are often associated with eutrophication of coastal waters and estuaries However identifying quantitative relationships between nutrient Input and proliferation of specific algal species is very challenging and complex The complexity arises from the diversity of sources forms and fluxes of nutrients both exported into and cycled within the system the diversity of algal mechanisms for acquiring nutrients and the interaction of the target harmful species with other members of the food web Even more challenging is the development of forecasts and predictions both on the short term and on the long term Short term scales (days to weeks) are necessary for managers to prepare for and respond to events longer scales are needed to enable strategic planning to prevent HAB events mitigate their impacts or estimate the interactive effects of anthropogenic activities and climate change To address these needs the HAB modeling community will need to engage with climate scientists (assess climate change scenarios) marine ecologists (describe organism ecophysiology) invasive species experts watershed modelers and hydrologists (estimate future changes in the land derived inputs) and socio economists managers and policy makers (define future land use scenarios and to interpret results in a policy context) (C) 2010 Elsevier BV All rights reserved
C1 [Glibert, Patricia M.] Univ Maryland, Ctr Environm Sci, Horn Point Lab, Cambridge, MD 21613 USA.
[Allen, J. Icarus] Plymouth Marine Lab, Plymouth PL1 5LT 3DH, Devon, England.
[Bouwman, A. F.] Netherlands Environm Assessment Agcy, NL-3720 AH Bilthoven, Netherlands.
[Bouwman, A. F.] Univ Utrecht, Geochem Fac Geosci, NL-3508 TA Utrecht, Netherlands.
[Brown, Christopher W.] Natl Ocean & Atmospher Adm, College Pk, MD 20742 USA.
[Flynn, Kevin J.] Swansea Univ, Dept Pure & Appl Ecol, Inst Environm Sustainabil, Swansea SA2 8PP, W Glam, Wales.
[Lewitus, Alan J.] Natl Ocean & Atmospher Adm, Silver Spring, MD 20910 USA.
[Madden, Christopher J.] S Florida Water Management Dist Everglades Div, W Palm Beach, FL 33411 USA.
RP Glibert, PM (reprint author), Univ Maryland, Ctr Environm Sci, Horn Point Lab, POB 775, Cambridge, MD 21613 USA.
RI Brown, Christopher/B-8213-2008; Bouwman, Lex/B-7053-2012; glibert,
patricia/G-1026-2013; Bouwman, Lex/F-1444-2015;
OI Brown, Christopher/0000-0002-9905-6391; glibert,
patricia/0000-0001-5690-1674; Bouwman, Lex/0000-0002-2045-1859; Flynn,
Kevin/0000-0001-6913-5884
FU Center for Satellite Applications and Research of the National Oceanic
and Atmospheric Administration (NOAA); NOAA [NA06NOS4780039]
FX This is a contribution of SCOR/LOICZ Working Group 132 and the GEOHAB
Core Research Project on HABs and Eutrophication PMG and CJM were funded
by the NOAA South Florida Program grant NA06NOS4780039 CWB was supported
by the Center for Satellite Applications and Research of the National
Oceanic and Atmospheric Administration (NOAA) The views opinions and
findings contained in this report are those of the author(s) and should
not be construed as an official NOM or U S Government position policy or
decision This is contribution number 4374 from the University of
Maryland Center for Environmental Science
NR 121
TC 56
Z9 58
U1 4
U2 58
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0924-7963
J9 J MARINE SYST
JI J. Mar. Syst.
PD NOV
PY 2010
VL 83
IS 3-4
SI SI
BP 262
EP 275
DI 10.1016/j.jmarsys.2010.05.004
PG 14
WC Geosciences, Multidisciplinary; Marine & Freshwater Biology;
Oceanography
SC Geology; Marine & Freshwater Biology; Oceanography
GA 679SF
UT WOS:000284180400015
ER
PT J
AU Haynes, RJ
Holden, MJ
Kline, MC
Butler, JM
Mackay, W
Wallace, P
AF Haynes, R. J.
Holden, M. J.
Kline, M. C.
Butler, J. M.
Mackay, W.
Wallace, P.
TI NIST Standard Reference Material (SRM)2366 Cytomegalovirus DNA
SO JOURNAL OF MOLECULAR DIAGNOSTICS
LA English
DT Meeting Abstract
CT Annual Meeting of the Association-for-Molecular-Pathology
CY NOV 18-20, 2010
CL San Jose, CA
SP Assoc Mol Pathol
C1 [Haynes, R. J.; Holden, M. J.; Kline, M. C.; Butler, J. M.] Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
[Mackay, W.; Wallace, P.] Qual Control Mol Diagnost, Glasgow, Lanark, Scotland.
RI Butler, John/C-7812-2011
NR 0
TC 0
Z9 0
U1 0
U2 0
PU AMER SOC INVESTIGATIVE PATHOLOGY, INC
PI BETHESDA
PA 9650 ROCKVILLE PIKE, BETHESDA, MD 20814-3993 USA
SN 1525-1578
J9 J MOL DIAGN
JI J. Mol. Diagn.
PD NOV
PY 2010
VL 12
IS 6
BP 878
EP 878
PG 1
WC Pathology
SC Pathology
GA 677FE
UT WOS:000283973700110
ER
PT J
AU Kline, MC
Butler, JM
AF Kline, M. C.
Butler, J. M.
TI Cautionary Considerations when Exploring Cell Lines as Potential
Reference Materials
SO JOURNAL OF MOLECULAR DIAGNOSTICS
LA English
DT Meeting Abstract
CT Annual Meeting of the Association-for-Molecular-Pathology
CY NOV 18-20, 2010
CL San Jose, CA
SP Assoc Mol Pathol
C1 [Kline, M. C.; Butler, J. M.] NIST, Gaithersburg, MD 20899 USA.
NR 0
TC 0
Z9 0
U1 0
U2 0
PU AMER SOC INVESTIGATIVE PATHOLOGY, INC
PI BETHESDA
PA 9650 ROCKVILLE PIKE, BETHESDA, MD 20814-3993 USA
SN 1525-1578
J9 J MOL DIAGN
JI J. Mol. Diagn.
PD NOV
PY 2010
VL 12
IS 6
BP 895
EP 895
PG 1
WC Pathology
SC Pathology
GA 677FE
UT WOS:000283973700183
ER
PT J
AU Yetley, EA
Pfeiffer, CM
Schleicher, RL
Phinney, KW
Lacher, DA
Christakos, S
Eckfeldt, JH
Fleet, JC
Howard, G
Hoofnagle, AN
Hui, SL
Lensmeyer, GL
Massaro, J
Peacock, M
Rosner, B
Wiebe, D
Bailey, RL
Coates, PM
Looker, AC
Sempos, C
Johnson, CL
Picciano, MF
AF Yetley, Elizabeth A.
Pfeiffer, Christine M.
Schleicher, Rosemary L.
Phinney, Karen W.
Lacher, David A.
Christakos, Sylvia
Eckfeldt, John H.
Fleet, James C.
Howard, George
Hoofnagle, Andrew N.
Hui, Siu L.
Lensmeyer, Gary L.
Massaro, Joseph
Peacock, Munro
Rosner, Bernard
Wiebe, Donald
Bailey, Regan L.
Coates, Paul M.
Looker, Anne C.
Sempos, Christopher
Johnson, Clifford L.
Picciano, Mary Frances
CA Vitamin D Roundtable NHANES
TI NHANES Monitoring of Serum 25-Hydroxyvitamin D: A Roundtable Summary
SO JOURNAL OF NUTRITION
LA English
DT Article; Proceedings Paper
CT Conference on NHANES Monitoring of Serum 25(OH)D - Assay Challenges and
Options for Resolving Them
CY JUL 27-28, 2009
CL Rockville, MD
ID TANDEM MASS-SPECTROMETRY; CIRCULATING 25-HYDROXYVITAMIN-D; ASSAYS;
ACCURACY; STANDARDIZATION; DISEASE; D-3
AB A roundtable to discuss monitoring of serum 25-hydroxyvitamin D [25(OH)D] in the NHANES was held in late July 2009. Topics included the following: 1) options for dealing with assay fluctuations in serum 25(OH)D in the NHANES conducted between 1988 and 2006; 2) approaches for transitioning between the RIA used in the NHANES between 1988 and 2006 to the liquid chromatography tandem MS (LC-MS/MS) measurement procedure to be used in NHANES 2007 and later; 31 approaches for integrating the recently available standard reference material for vitamin D in human serum (SAM 972) from the National Institute of Standards and Technology (NIST) into the NHANES; 41 questions regarding whether the C-3 epimer of 25-hydroxyvitamin D3 [3-epi-25(OH)D3] should be measured in NHANES 2007 and later; and 5) identification of research and educational needs. The roundtable experts agreed that the NHANES data needed to be adjusted to control for assay fluctuations and offered several options for addressing this issue. The experts suggested that the LC-MS/MS measurement procedure developed by NIST could serve as a higher order reference measurement procedure. They noted the need for a commutability study for the recently released NIST SRM 972 across a range of measurement procedures. They suggested that federal agencies and professional organizations work with manufacturers to improve the quality and comparability of measurement procedures across all laboratories. The experts noted the preliminary nature of the evidence of the 3-epi-25(OH)D3 but felt that it should be measured in 2007 NHANES and later. J. Nutr. 140: 2030S-2045S, 2010.
C1 [Yetley, Elizabeth A.; Bailey, Regan L.; Coates, Paul M.; Sempos, Christopher; Picciano, Mary Frances] NIH, Off Dietary Supplements, Bethesda, MD 20892 USA.
[Pfeiffer, Christine M.; Schleicher, Rosemary L.] Ctr Dis Control & Prevent, Div Sci Lab, Natl Ctr Environm Hlth, Atlanta, GA 30341 USA.
[Phinney, Karen W.] NIST, Div Analyt Chem, Gaithersburg, MD 20899 USA.
[Lacher, David A.; Looker, Anne C.; Johnson, Clifford L.] Ctr Dis Control & Prevent, Div Hlth & Nutr Examinat Surveys, Natl Ctr Hlth Stat, Hyattsville, MD 20782 USA.
[Christakos, Sylvia] Univ Med & Dent New Jersey, Dept Biochem & Mol Biol, Newark, NJ 07103 USA.
[Eckfeldt, John H.] Univ Minnesota, Dept Lab Med & Pathol, Minneapolis, MN 55455 USA.
[Fleet, James C.] Purdue Univ, Dept Foods & Nutr, W Lafayette, IN 47906 USA.
[Howard, George] Univ Alabama, Dept Biostat, Birmingham, AL 35294 USA.
[Hoofnagle, Andrew N.] Univ Washington, Dept Lab Med, Seattle, WA 98195 USA.
[Hui, Siu L.; Peacock, Munro] Indiana Univ Sch Med, Dept Med, Indianapolis, IN 46202 USA.
[Lensmeyer, Gary L.] Univ Wisconsin Hosp & Clin, Clin Toxicol Lab, Madison, WI 53792 USA.
[Massaro, Joseph] Boston Univ, Sch Publ Hlth, Dept Biostat, Boston, MA 02118 USA.
[Rosner, Bernard] Harvard Univ, Channing Lab, Harvard Med Sch, Boston, MA 02155 USA.
[Wiebe, Donald] Univ Wisconsin, Sch Med & Publ Hlth, Dept Pathol & Lab Med, Madison, WI 53792 USA.
RP Yetley, EA (reprint author), NIH, Off Dietary Supplements, Bldg 10, Bethesda, MD 20892 USA.
EM beth@yetley.com
OI Fleet, James/0000-0002-0142-9517
FU NIDDK NIH HHS [R01 DK038961, R01 DK038961-22]
NR 40
TC 62
Z9 64
U1 1
U2 6
PU AMER SOC NUTRITIONAL SCIENCE
PI BETHESDA
PA 9650 ROCKVILLE PIKE, RM L-2407A, BETHESDA, MD 20814 USA
SN 0022-3166
J9 J NUTR
JI J. Nutr.
PD NOV
PY 2010
VL 140
IS 11
BP 2030S
EP 2045S
DI 10.3945/jn.110.121483
PG 16
WC Nutrition & Dietetics
SC Nutrition & Dietetics
GA 671RD
UT WOS:000283525700020
PM 20881084
ER
PT J
AU Beron-Vera, FJ
Olascoaga, MJ
Goni, GJ
AF Beron-Vera, Francisco J.
Olascoaga, Maria J.
Goni, Gustavo J.
TI Surface Ocean Mixing Inferred from Different Multisatellite Altimetry
Measurements
SO JOURNAL OF PHYSICAL OCEANOGRAPHY
LA English
DT Article
ID LAGRANGIAN COHERENT STRUCTURES; TIME LYAPUNOV EXPONENTS; CHAOTIC FLOWS;
3-DIMENSIONAL TURBULENCE; 2-DIMENSIONAL TURBULENCE; VELOCITY DATA;
TRANSPORT; TOPEX/POSEIDON; CIRCULATION; MESOSCALE
AB Two sea surface height (SSH) anomaly fields distributed by Archiving, Validation, and Interpretation of Satellite Oceanographic (AVISO) Altimetry are evaluated in terms of the effects that they produce on mixing. One SSH anomaly field, tagged REF, is constructed using measurements made by two satellite altimeters; the other SSH anomaly field, tagged UPD, is constructed using measurements made by up to four satellite altimeters. Advection is supplied by surface geostrophic currents derived from the total SSH fields resulting from the addition of these SSH anomaly fields to a mean SSH field. Emphasis is placed on the extraction from the currents of Lagrangian coherent structures (LCSs), which, acting as skeletons for patterns formed by passively advected tracers, entirely control mixing. The diagnostic tool employed to detect LCSs is provided by the computation of finite-time Lyapunov exponents. It is found that currents inferred using UPD SSH anomalies support mixing with characteristics similar to those of mixing produced by currents inferred using REF SSH anomalies. This result mainly follows from the fact that, being more easily characterized as chaotic than turbulent, mixing as sustained by currents derived using UPD SSH anomalies is quite insensitive to spatiotemporal truncations of the advection field.
C1 [Beron-Vera, Francisco J.] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, AMP, Miami, FL 33149 USA.
[Goni, Gustavo J.] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
RP Beron-Vera, FJ (reprint author), Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, AMP, 4600 Rickenbacker Cswy, Miami, FL 33149 USA.
EM fberon@rsmas.miami.edu
RI Goni, Gustavo/D-2017-2012
OI Goni, Gustavo/0000-0001-7093-3170
FU NSF [CMG0825547]; NASA [NNX09AD82G, NNX10AE99G]; CNES
FX Technical assistance by P. DiNezio is sincerely appreciated. The
comments made by two anonymous reviewers contributed to improve the
manuscript. The altimeter products used in this work are produced by
SSALTO/DUCAS and distributed by AVISO, with support from CNES (available
online at http://www.aviso.oceanobs.com/duacs). The Rio05 product is
produced by CLS Space Oceanography Division and is distributed by AVISO,
with support from CNES (available online at
http://www.aviso.oceanobs.com). The drifter trajectory data are
distributed by the NOAA/AOML Drifter Data Assembly Center (available
online at http://www.aoml.noaa.gov/phod/dac). FJBV and MJO were
supported by NSF Grant CMG0825547 and NASA Grants NNX09AD82G and
NNX10AE99G. GJG was supported by NASA Grants NNX09AD82G and NNX10AE99G
and the NOAA/CPO.
NR 63
TC 14
Z9 15
U1 0
U2 7
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0022-3670
EI 1520-0485
J9 J PHYS OCEANOGR
JI J. Phys. Oceanogr.
PD NOV
PY 2010
VL 40
IS 11
BP 2466
EP 2480
DI 10.1175/2010JPO4458.1
PG 15
WC Oceanography
SC Oceanography
GA 690AR
UT WOS:000284972900007
ER
PT J
AU Song, HJ
Ji, RB
Stock, C
Wang, ZL
AF Song, Hongjun
Ji, Rubao
Stock, Charles
Wang, Zongling
TI Phenology of phytoplankton blooms in the Nova Scotian Shelf-Gulf of
Maine region: remote sensing and modeling analysis
SO JOURNAL OF PLANKTON RESEARCH
LA English
DT Article
DE Phytoplankton bloom; Phenology; Remote sensing; Environmental
conditions; Nova Scotian Shelf; Gulf of Maine
ID SURFACE HEAT-FLUX; INTERANNUAL VARIABILITY; GEORGES-BANK; MARINE
PLANKTON; MATCH-MISMATCH; CLIMATE-CHANGE; LIFE-HISTORY; SPRING BLOOM;
NORTH-SEA; WATER
AB Remotely sensed ocean color data and numerical modeling have been used to study the phenology of both spring and fall phytoplankton blooms (FPBs) in the Nova Scotian Shelf (NSS)-Gulf of Maine (GoM) region. The ocean color data reveal a general pattern of westward progression of the spring phytoplankton bloom (SPB), and an eastward progression of the FPB in the NSS-GoM region. The spatial pattern of mean chlorophyll concentration in spring is similar to that in fall, with a lower concentration in the NSS and higher in the GoM. Interannually, there is a weak but significant tendency for years with earlier (delayed) SPBs to be followed by delayed (earlier) FPBs, but the mean chlorophyll concentrations during SPBs are not correlated with those during FPBs. The interannual variability of SPB timing is significantly correlated with sea surface salinity (SSS), but the FPB timing is correlated with both SSS and sea surface temperature. The process-oriented numerical modeling experiments suggest that (i) salinity is the main factor influencing the bloom timing and magnitude in the NSS-GoM region, especially for the timing of SPBs; (ii) compared to buoyancy forcing induced by vertical salinity gradients, the impact of surface heating and surface wind stress on the blooms variability is much weaker; and (iii) the nutrient level controls the bloom magnitude, but only has a minor effect on bloom timing. This study provides a quantitative estimation of relationship between changes in local/remote environmental forcing and phytoplankton phenological shifts, thus improving our understanding on the possible impact of climate change on coastal/shelf ecosystems.
C1 [Song, Hongjun; Ji, Rubao] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA.
[Song, Hongjun] Ocean Univ China, Coll Environm Sci & Engn, Qingdao 266100, Peoples R China.
[Song, Hongjun; Wang, Zongling] First Inst Oceanog, Key Lab Sci & Engn Marine Ecol Environm, Qingdao 266061, Peoples R China.
[Stock, Charles] Princeton Univ, NOAA Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA.
[Ji, Rubao] Shanghai Ocean Univ, Marine Ecosyst & Environm Lab, Shanghai 201306, Peoples R China.
RP Ji, RB (reprint author), Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA.
EM songhongjun@fio.org.cn; rji@whoi.edu
RI Stock, Charles/H-1281-2012; Ji, Rubao/I-1970-2015;
OI Ji, Rubao/0000-0002-8839-5427; Stock, Charles/0000-0001-9549-8013
FU NSF [OCE-0727033, 0815838]; National Key Basic Research Program of China
(973 Program) [2010CB428703]; China Scholarship Council (CSC)
FX This study was supported by the NSF grants OCE-0727033 and 0815838
provided to R. J., National Key Basic Research Program of China (973
Program) grant 2010CB428703 provided to Z. W. and a China Scholarship
Council (CSC) government-sponsored graduate scholarship provided to H.
S.
NR 50
TC 20
Z9 22
U1 4
U2 22
PU OXFORD UNIV PRESS
PI OXFORD
PA GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND
SN 0142-7873
J9 J PLANKTON RES
JI J. Plankton Res.
PD NOV
PY 2010
VL 32
IS 11
BP 1485
EP 1499
DI 10.1093/plankt/fbq086
PG 15
WC Marine & Freshwater Biology; Oceanography
SC Marine & Freshwater Biology; Oceanography
GA 661TK
UT WOS:000282750800001
ER
PT J
AU Martin, WE
Hesse, E
Hough, JH
Sparks, WB
Cockell, CS
Ulanowski, Z
Germer, TA
Kaye, PH
AF Martin, W. E.
Hesse, E.
Hough, J. H.
Sparks, W. B.
Cockell, C. S.
Ulanowski, Z.
Germer, T. A.
Kaye, P. H.
TI Polarized optical scattering signatures from biological materials
SO JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER
LA English
DT Article
DE Circular polarization; Chlorophyll red-edge; Remote sensing; Biomarkers;
Astrobiology
ID ULTRAVIOLET-RADIATION; SPECTRAL SIGNATURES; CIRCULAR-DICHROISM; MUELLER
MATRICES; RED EDGE; LIGHT; PHOTOSYNTHESIS; EARTHSHINE; LEAF;
COLONIZATION
AB The polarization of laser light backscattered from biological samples has been measured over the wavelength range 350-850 nm. Incident circular, linearly polarized, and unpolarized light produces significant spectral features in the case of samples containing chlorophyll such as leaves and cyanobacteria. Polarization scattering signatures are observed around the chlorophyll 'red edge' that may have diagnostic value in the search for life signatures from extrasolar planets. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Martin, W. E.; Hough, J. H.] Univ Hertfordshire, Ctr Astrophys Res, Hatfield AL10 9AB, Herts, England.
[Hesse, E.; Ulanowski, Z.; Kaye, P. H.] Univ Hertfordshire, Sci & Technol Res Inst, Hatfield AL10 9AB, Herts, England.
[Sparks, W. B.] Space Telescope Sci Inst, Baltimore, MD 21218 USA.
[Cockell, C. S.] Open Univ, Geomicrobiol Res Grp, St Andrews, Fife, Scotland.
[Germer, T. A.] Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
RP Martin, WE (reprint author), Univ Hertfordshire, Ctr Astrophys Res, Hatfield AL10 9AB, Herts, England.
EM w.e.martin@herts.ac.uk
OI Hesse, Evelyn/0000-0002-2721-7600
FU Leverhulme Trust [F/00 281/F]; University of Hertfordshire Science
Research Infrastructure Fund (SRIF)
FX This work has been supported by a grant from the Leverhulme Trust (Grant
number: F/00 281/F) and by funding from the University of Hertfordshire
Science Research Infrastructure Fund (SRIF).
NR 42
TC 7
Z9 7
U1 3
U2 24
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0022-4073
J9 J QUANT SPECTROSC RA
JI J. Quant. Spectrosc. Radiat. Transf.
PD NOV
PY 2010
VL 111
IS 16
BP 2444
EP 2459
DI 10.1016/j.jqsrt.2010.07.001
PG 16
WC Optics; Spectroscopy
SC Optics; Spectroscopy
GA 655LW
UT WOS:000282252500008
ER
PT J
AU Olson, DA
Driver, RG
Bowers, WJ
AF Olson, Douglas A.
Driver, R. Greg
Bowers, Walter J.
TI A Gas Pressure Scale Based on Primary Standard Piston Gauges
SO JOURNAL OF RESEARCH OF THE NATIONAL INSTITUTE OF STANDARDS AND
TECHNOLOGY
LA English
DT Article
DE gas pressure scale; piston gauge; primary standard piston gauge;
pressure measurement; secondary standard piston gauge
ID MANOMETER
AB The National Institute of Standards and Technology (NIST) has redefined its gas pressure scale, up to 17 MPa, based on two primary standard piston gauges. The primary standard piston gauges are 35.8 mm in diameter and operate from 20 kPa to 1 MPa. Ten secondary standard piston gauges, two each of five series of the Ruska 2465 type, with successively smaller diameters form the scale extending up to 17 MPa. Six of the piston gauges were directly compared to the primary standards to determine their effective area and expanded (k = 2) uncertainty. Two piston gauges operating to 7 MPa were compared to the 1.4 MPa gauges, and two piston gauges operating to 17 MPa were compared to the 7 MPa gauges. Distortion in the 7 MPa piston gauges was determined by comparing those gauges to a DH Instruments PG7601 type piston gauge, whose distortion was calculated using elasticity theory. The relative standard uncertainties achieved by the primary standards range from 3.0 x 10(-6) to 3.2 x 10(-6). The relative standard uncertainty of the secondary standards is as low as 4.2 x 10(-6) at 300 kPa. The effective areas and uncertainties were validated by comparison to standards of other National Metrology Institutes (NMIs). Results show agreement in all cases to better than the expanded (k = 2) uncertainty of the difference between NIST and the other NMIs, and in most cases to better than the standard (k = 1) uncertainty of the difference.
C1 [Olson, Douglas A.; Driver, R. Greg; Bowers, Walter J.] Natl Inst Stand & Technol, Temp Pressure & Flow Metrol Div, NIST Phys Measurement Lab, Gaithersburg, MD 20899 USA.
RP Olson, DA (reprint author), Natl Inst Stand & Technol, Temp Pressure & Flow Metrol Div, NIST Phys Measurement Lab, Gaithersburg, MD 20899 USA.
EM douglas.olson@nist.gov; robert.driver@nist.gov
NR 16
TC 1
Z9 1
U1 0
U2 5
PU US GOVERNMENT PRINTING OFFICE
PI WASHINGTON
PA SUPERINTENDENT DOCUMENTS,, WASHINGTON, DC 20402-9325 USA
SN 1044-677X
J9 J RES NATL INST STAN
JI J. Res. Natl. Inst. Stand. Technol.
PD NOV-DEC
PY 2010
VL 115
IS 6
BP 393
EP 412
DI 10.6028/jres.115.027
PG 20
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA 699FW
UT WOS:000285650300001
PM 27134793
ER
PT J
AU Stone, JA
Egan, P
AF Stone, Jack A.
Egan, Patrick
TI An Optical Frequency Comb Tied to GPS for Laser Frequency/Wavelength
Calibration
SO JOURNAL OF RESEARCH OF THE NATIONAL INSTITUTE OF STANDARDS AND
TECHNOLOGY
LA English
DT Article
DE global positioning system; GPSDO; laser frequency calibration; laser
wavelength calibration; optical frequency comb
ID HE-NE-LASER; MODE NUMBER; OSCILLATORS
AB Optical frequency combs can be employed over a broad spectral range to calibrate laser frequency or vacuum wavelength. This article describes procedures and techniques utilized in the Precision Engineering Division of NIST ( National Institute of Standards and Technology) for comb-based calibration of laser wavelength, including a discussion of ancillary measurements such as determining the mode order. The underlying purpose of these calibrations is to provide traceable standards in support of length measurement. The relative uncertainty needed to fulfill this goal is typically 10(-8) and never below 10(-12), very modest requirements compared to the capabilities of comb-based frequency metrology. In this accuracy range the Global Positioning System (GPS) serves as an excellent frequency reference that can provide the traceable underpinning of the measurement. This article describes techniques that can be used to completely characterize measurement errors in a GPS-based comb system and thus achieve full confidence in measurement results.
C1 [Stone, Jack A.; Egan, Patrick] Natl Inst Stand & Technol, Mech Metrol Div, NIST Phys Measurement Lab, Gaithersburg, MD 20899 USA.
RP Stone, JA (reprint author), Natl Inst Stand & Technol, Mech Metrol Div, NIST Phys Measurement Lab, Gaithersburg, MD 20899 USA.
EM jack.stone@nist.gov; patrick.egan@nist.gov
NR 20
TC 3
Z9 3
U1 1
U2 4
PU US GOVERNMENT PRINTING OFFICE
PI WASHINGTON
PA SUPERINTENDENT DOCUMENTS,, WASHINGTON, DC 20402-9325 USA
SN 1044-677X
J9 J RES NATL INST STAN
JI J. Res. Natl. Inst. Stand. Technol.
PD NOV-DEC
PY 2010
VL 115
IS 6
BP 413
EP 431
DI 10.6028/jres.115.028
PG 19
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA 699FW
UT WOS:000285650300002
PM 27134794
ER
PT J
AU Vayshenker, I
Livigni, DJ
Li, X
Lehman, JH
Li, J
Xiong, LM
Zhang, ZX
AF Vayshenker, I.
Livigni, D. J.
Li, X.
Lehman, J. H.
Li, J.
Xiong, L. M.
Zhang, Z. X.
TI Optical Fiber Power Meter Comparison Between NIST and NIM
SO JOURNAL OF RESEARCH OF THE NATIONAL INSTITUTE OF STANDARDS AND
TECHNOLOGY
LA English
DT Article
DE international comparison; optical fiber; optical power
ID PTB
AB We describe the results of a comparison of reference standards between the National Institute of Standards and Technology (NIST-USA) and National Institute of Metrology (NIM-China). We report optical fiber-based power measurements at nominal wavelengths of 1310 nm and 1550 nm. We compare the laboratories' reference standards by means of a commercial optical power meter. Measurement results showed the largest difference of less than 2.6 parts in 10(3), which is within the combined standard (k = 1) uncertainty for the laboratories' reference standards.
C1 [Vayshenker, I.; Livigni, D. J.; Li, X.; Lehman, J. H.] Natl Inst Stand & Technol, Div Optoelect, NIST Elect & Elect Engn Lab, Boulder, CO 80305 USA.
[Li, J.; Xiong, L. M.; Zhang, Z. X.] Natl Inst Metrol, Div Metrol Opt & Laser Technol, Beijing 100013, Peoples R China.
RP Vayshenker, I (reprint author), Natl Inst Stand & Technol, Div Optoelect, NIST Elect & Elect Engn Lab, Boulder, CO 80305 USA.
EM igor.vayshenker@boulder.nist.gov; david.livigni@boulder.nist.gov;
xiaoyu.li@boulder.nist.gov; john.lehman@boulder.nist.gov;
jianl@nim.ac.cn; xlmin@nim.ac.cn; zhixinzhang@nim.ac.cn
RI Vayshenker, Igor/H-9793-2013
OI Vayshenker, Igor/0000-0002-7098-3781
NR 13
TC 2
Z9 2
U1 0
U2 3
PU US GOVERNMENT PRINTING OFFICE
PI WASHINGTON
PA SUPERINTENDENT DOCUMENTS,, WASHINGTON, DC 20402-9325 USA
SN 1044-677X
J9 J RES NATL INST STAN
JI J. Res. Natl. Inst. Stand. Technol.
PD NOV-DEC
PY 2010
VL 115
IS 6
BP 433
EP 436
DI 10.6028/jres.115.029
PG 4
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA 699FW
UT WOS:000285650300003
PM 27134795
ER
PT J
AU Nanninga, N
Slifka, A
Levy, Y
White, C
AF Nanninga, N.
Slifka, A.
Levy, Y.
White, C.
TI A Review of Fatigue Crack Growth for Pipeline Steels Exposed to Hydrogen
SO JOURNAL OF RESEARCH OF THE NATIONAL INSTITUTE OF STANDARDS AND
TECHNOLOGY
LA English
DT Review
DE fatigue crack growth; hydrogen; pipelines; steel; review
ID AQUEOUS-SOLUTIONS; EMBRITTLEMENT; PROPAGATION; MECHANISMS; DUCTILE;
MODEL
AB Hydrogen pipeline systems offer an economical means of storing and transporting energy in the form of hydrogen gas. Pipelines can be used to transport hydrogen that has been generated at solar and wind farms to and from salt cavern storage locations. In addition, pipeline transportation systems will be essential before widespread hydrogen fuel cell vehicle technology becomes a reality. Since hydrogen pipeline use is expected to grow, the mechanical integrity of these pipelines will need to be validated under the presence of pressurized hydrogen. This paper focuses on a review of the fatigue crack growth response of pipeline steels when exposed to gaseous hydrogen environments. Because of defect-tolerant design principles in pipeline structures, it is essential that designers consider hydrogen-assisted fatigue crack growth behavior in these applications.
C1 [Nanninga, N.; Slifka, A.; Levy, Y.] Natl Inst Stand & Technol, Div Mat Reliabil, Boulder, CO 80305 USA.
[White, C.] Michigan Technol Univ, Dept Mat Sci & Engn, Houghton, MI 49931 USA.
RP Nanninga, N (reprint author), Natl Inst Stand & Technol, Div Mat Reliabil, Boulder, CO 80305 USA.
EM nanninga@boulder.nist.gov; slifka@boulder.nist.gov;
ylevy@boulder.nist.gov; cwhite@mtu.edu
RI White, Calvin/F-7981-2011
OI White, Calvin/0000-0003-1299-4375
NR 56
TC 15
Z9 15
U1 3
U2 30
PU US GOVERNMENT PRINTING OFFICE
PI WASHINGTON
PA SUPERINTENDENT DOCUMENTS,, WASHINGTON, DC 20402-9325 USA
SN 1044-677X
J9 J RES NATL INST STAN
JI J. Res. Natl. Inst. Stand. Technol.
PD NOV-DEC
PY 2010
VL 115
IS 6
BP 437
EP 452
DI 10.6028/jres.115.030
PG 16
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA 699FW
UT WOS:000285650300004
PM 27134796
ER
PT J
AU Kacker, RN
Kessel, R
Sommer, KD
AF Kacker, Raghu N.
Kessel, Ruediger
Sommer, Klaus-Dieter
TI Assessing Differences Between Results Determined According to the Guide
to the Expression of Uncertainty in Measurement
SO JOURNAL OF RESEARCH OF THE NATIONAL INSTITUTE OF STANDARDS AND
TECHNOLOGY
LA English
DT Article
DE Birge test; interlaboratory evaluations; predictive p-value; uncertainty
ID FUNDAMENTAL PHYSICAL CONSTANTS; INTERLABORATORY EVALUATIONS; CONSISTENCY
AB In some metrology applications multiple results of measurement for a common measurand are obtained and it is necessary to determine whether the results agree with each other. A result of measurement based on the Guide to the Expression of Uncertainty in Measurement (GUM) consists of a measured value together with its associated standard uncertainty. In the GUM, the measured value is regarded as the expected value and the standard uncertainty is regarded as the standard deviation, both known values, of a state-of-knowledge probability distribution. A state-of-knowledge distribution represented by a result need not be completely known. Then how can one assess the differences between the results based on the GUM? Metrologists have for many years used the Birge chisquare test as 'a rule of thumb' to assess the differences between two or more measured values for the same measurand by pretending that the standard uncertainties were the standard deviations of the presumed sampling probability distributions from random variation of the measured values. We point out that this is misuse of the standard uncertainties; the Birge test and the concept of statistical consistency motivated by it do not apply to the results of measurement based on the GUM. In 2008, the International Vocabulary of Metrology, third edition (VIM3) introduced the concept of metrological compatibility. We propose that the concept of metrological compatibility be used to assess the differences between results based on the GUM for the same measurand. A test of the metrological compatibility of two results of measurement does not conflict with a pairwise Birge test of the statistical consistency of the corresponding measured values.
C1 [Kacker, Raghu N.; Kessel, Ruediger] Natl Inst Stand & Technol, Informat Technol Lab, Gaithersburg, MD 20899 USA.
[Sommer, Klaus-Dieter] Phys Tech Bundesanstalt, Chem Phys & Explos Protect Div, Natl Metrol Inst Germany, D-38116 Braunschweig, Germany.
RP Kacker, RN (reprint author), Natl Inst Stand & Technol, Informat Technol Lab, Gaithersburg, MD 20899 USA.
EM raghu.kacker@nist.gov; ruediger.kessel@nist.gov;
klaus-dieter.sommer@ptb.de
NR 13
TC 8
Z9 8
U1 0
U2 8
PU US GOVERNMENT PRINTING OFFICE
PI WASHINGTON
PA SUPERINTENDENT DOCUMENTS,, WASHINGTON, DC 20402-9325 USA
SN 1044-677X
J9 J RES NATL INST STAN
JI J. Res. Natl. Inst. Stand. Technol.
PD NOV-DEC
PY 2010
VL 115
IS 6
BP 453
EP 459
DI 10.6028/jres.115.031
PG 7
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA 699FW
UT WOS:000285650300005
PM 27134797
ER
PT J
AU Franaszek, M
AF Franaszek, Marek
TI Variances of Plane Parameters Fitted to Range Data
SO JOURNAL OF RESEARCH OF THE NATIONAL INSTITUTE OF STANDARDS AND
TECHNOLOGY
LA English
DT Article
DE LADAR; nonlinear least squares; variances of fitted parameters
AB Formulas for variances of plane parameters fitted with Nonlinear Least Squares to point clouds acquired by 3D imaging systems (e.g., LADAR) are derived. Two different error objective functions used in minimization are discussed: the orthogonal and the directional functions. Comparisons of corresponding formulas suggest the two functions can yield different results when applied to the same dataset.
C1 Natl Inst Stand & Technol, Engn Lab, Gaithersburg, MD 20899 USA.
RP Franaszek, M (reprint author), Natl Inst Stand & Technol, Engn Lab, Gaithersburg, MD 20899 USA.
EM marek.franaszek@nist.gov
NR 9
TC 1
Z9 1
U1 0
U2 3
PU US GOVERNMENT PRINTING OFFICE
PI WASHINGTON
PA SUPERINTENDENT DOCUMENTS,, WASHINGTON, DC 20402-9325 USA
SN 1044-677X
J9 J RES NATL INST STAN
JI J. Res. Natl. Inst. Stand. Technol.
PD NOV-DEC
PY 2010
VL 115
IS 6
BP 461
EP 470
DI 10.6028/jres.115.032
PG 10
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA 699FW
UT WOS:000285650300006
PM 27134798
ER
PT J
AU Cherng, AM
Takagi, S
Chow, LC
AF Cherng, A. Maria
Takagi, Shozo
Chow, Laurence C.
TI Acid Neutralization Capacity of a Tricalcium Silicate-Containing Calcium
Phosphate Cement as an Endodontic Material
SO JOURNAL OF RESEARCH OF THE NATIONAL INSTITUTE OF STANDARDS AND
TECHNOLOGY
LA English
DT Article
DE acid neutralization; basicity; calcium phosphate cement; endo-materials;
mineral trioxide aggregate; setting time; tricalcium silicate
ID CANAL SEALER-FILLER; IN-VITRO; APICAL BARRIER; THERAPY
AB A calcium phosphate cement (CPC) was shown to have the necessary attributes for endodontic materials except adequate basicity needed for antimicrobial properties. To enhance its basicity, tricalcium silicate (Ca3SiO5), a highly alkaline compound, was added to CPC at a mass fraction of 0.25, 0.5 or 0.75. The basicity, acid neutralization and physical properties of the CPC-Ca3SiO5 composites were investigated. Mineral trioxide aggregate (MTA) was used as the control. The acid neutralizing capacity of the CPC-Ca3SiO5 composites and MTA were measured by titrating the suspensions of ground set samples with a 0.2 mol/L HCl at predetermined pH levels, i.e., 11, 9.0, and 7.4. The setting time of CPC-Ca3SiO5 composites determined by the Gilmore needle method was 40 + 10 min. Acid neutralizing capacity of CPC depended (p < 0.05) on Ca3SiO5 content. CPC containing 75 % Ca3SiO5 could neutralize slightly less acid than MTA (p < 0.05), but it had a shorter setting time than that of MTA(> 4 h) and excellent handling properties.
C1 [Cherng, A. Maria; Takagi, Shozo; Chow, Laurence C.] Natl Inst Stand & Technol, Amer Dent Assoc Fdn, Paffenbarger Res Ctr, MML, Gaithersburg, MD 20899 USA.
RP Cherng, AM (reprint author), Natl Inst Stand & Technol, Amer Dent Assoc Fdn, Paffenbarger Res Ctr, MML, Gaithersburg, MD 20899 USA.
EM maria.cherng@nist.gov; shozo.takagi@nist.gov; laurence.chow@nist.gov
FU American Dental Association Foundation; National Institute of Standards
and Technology; National Institute of Dental and Craniofacial Research
[DE11789]
FX Tricalcium silicate was prepared by Stan Frukhtbeyn in the laboratory.
This work has been supported by the American Dental Association
Foundation, the National Institute of Standards and Technology, and the
National Institute of Dental and Craniofacial Research (DE11789).
NR 17
TC 3
Z9 4
U1 0
U2 8
PU US GOVERNMENT PRINTING OFFICE
PI WASHINGTON
PA SUPERINTENDENT DOCUMENTS,, WASHINGTON, DC 20402-9325 USA
SN 1044-677X
J9 J RES NATL INST STAN
JI J. Res. Natl. Inst. Stand. Technol.
PD NOV-DEC
PY 2010
VL 115
IS 6
BP 471
EP 476
DI 10.6028/jres.115.033
PG 6
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA 699FW
UT WOS:000285650300007
PM 27134799
ER
PT J
AU Chalfoun, J
Cardone, A
Dima, AA
Allen, DP
Halter, MW
AF Chalfoun, Joe
Cardone, Antonio
Dima, Alden A.
Allen, Daniel P.
Halter, Michael W.
TI Overlap-Based Cell Tracker
SO JOURNAL OF RESEARCH OF THE NATIONAL INSTITUTE OF STANDARDS AND
TECHNOLOGY
LA English
DT Article
DE cell motility; live-cell imaging; overlap-based cell tracking;
time-lapse cell imaging
ID ACTIVE CONTOURS; MIGRATING CELLS; QUANTIFICATION; MICROSCOPY; MOTILITY
AB In order to facilitate the extraction of quantitative data from live cell image sets, automated image analysis methods are needed. This paper presents an introduction to the general principle of an overlap cell tracking software developed by the National Institute of Standards and Technology (NIST). This cell tracker has the ability to track cells across a set of time lapse images acquired at high rates based on the amount of overlap between cellular regions in consecutive frames. It is designed to be highly flexible, requires little user parameterization, and has a fast execution time.
C1 [Chalfoun, Joe; Cardone, Antonio; Dima, Alden A.; Allen, Daniel P.] Natl Inst Stand & Technol, Software & Syst Div, Informat Technol Lab, Gaithersburg, MD 20899 USA.
[Halter, Michael W.] Natl Inst Stand & Technol, Div Biochem Sci, Mat Measurement Lab, Gaithersburg, MD 20899 USA.
RP Chalfoun, J (reprint author), Natl Inst Stand & Technol, Software & Syst Div, Informat Technol Lab, Gaithersburg, MD 20899 USA.
EM joe.chalfoun@nist.gov; antonio.cardone@nist.gov; alden.dima@nist.gov;
oldhokie@verizon.net; michael.halter@nist.gov
NR 20
TC 3
Z9 3
U1 0
U2 2
PU US GOVERNMENT PRINTING OFFICE
PI WASHINGTON
PA SUPERINTENDENT DOCUMENTS,, WASHINGTON, DC 20402-9325 USA
SN 1044-677X
J9 J RES NATL INST STAN
JI J. Res. Natl. Inst. Stand. Technol.
PD NOV-DEC
PY 2010
VL 115
IS 6
BP 477
EP 486
DI 10.6028/jres.115.034
PG 10
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA 699FW
UT WOS:000285650300008
PM 27134800
ER
PT J
AU Neuman, M
Tissot, B
Vanblaricom, G
AF Neuman, Melissa
Tissot, Brian
Vanblaricom, Glenn
TI OVERALL STATUS AND THREATS ASSESSMENT OF BLACK ABALONE (HALIOTIS
CRACHERODII LEACH, 1814) POPULATIONS IN CALIFORNIA
SO JOURNAL OF SHELLFISH RESEARCH
LA English
DT Article; Proceedings Paper
CT 7th International Symposium on Abalone Biology, Fisheries and Culture
CY JUL 19-24, 2009
CL Pattaya, THAILAND
SP Int Abalone Soc, Marine Sci Assoc Thailand, Aquat Resources Res Inst, Fac Sci Chulalongkorn Univ
DE Allee effect; black abalone; depensation; Haliotis cracherodii;
endangered species; long-term trends in abundance; threats assessment;
withering syndrome
ID WITHERING SYNDROME; GENETIC-STRUCTURE; MASS MORTALITY; COAST;
RECRUITMENT; DECLINES; RECOVERY; ISLANDS; CO2
AB The black abalone (Haliolitis cracherodii Leach, 1814) is a relatively large prosobranch gastropod mollusc ranging from approximately Point Arena in northern California to Bahia Tortugas and Isla Guadalupe, Mexico. In the United States, populations of black abalone on offshore islands, especially those of southern California, were particularly large prior to the mid 1980s. Analysis of long-term fishery-dependent and -independent data revealed that fishing pressure in combination with a lethal disease, withering syndrome, has resulted in mass mortalities of 95% or greater in black abalone populations south of Monterey County, CA. Reduction in local densities below the threshold necessary for successful fertilization (0.34/m(2)) has been a widespread and pervasive consequence of population reductions by withering syndrome and other factors. The most significant current and future threat that the black abalone faces is that imposed by the spread of withering syndrome, known to be enhanced by periods of ocean warming. Other factors, such as illegal take, ocean pollution, and natural predation, also pose risks to remaining populations and those that may be restored via active management in the future. Without identification, development, and implementation of effective measures to counter the population-level effects of withering syndrome, remaining black abalone populations may experience further declines.
C1 [Neuman, Melissa] NOAA, Natl Marine Fisheries Serv, Long Beach, CA 90802 USA.
[Tissot, Brian] Washington State Univ, Sch Earth & Environm Sci, Vancouver, WA 98686 USA.
[Vanblaricom, Glenn] Univ Washington, Sch Aquat & Fishery Sci, Washington Cooperat Fish & Wildlife Res Unit, Seattle, WA 98195 USA.
RP Neuman, M (reprint author), NOAA, Natl Marine Fisheries Serv, 501 W Ocean Blvd,Suite 4200, Long Beach, CA 90802 USA.
EM Melissa.Neuman@noaa.gov
NR 48
TC 15
Z9 15
U1 2
U2 37
PU NATL SHELLFISHERIES ASSOC
PI GROTON
PA C/O DR. SANDRA E. SHUMWAY, UNIV CONNECTICUT, 1080 SHENNECOSSETT RD,
GROTON, CT 06340 USA
SN 0730-8000
J9 J SHELLFISH RES
JI J. Shellfish Res.
PD NOV
PY 2010
VL 29
IS 3
BP 577
EP 586
DI 10.2983/035.029.0305
PG 10
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 679BU
UT WOS:000284135200004
ER
PT J
AU Smith, JN
Ressler, PH
Warren, JD
AF Smith, Joy N.
Ressler, Patrick H.
Warren, Joseph D.
TI Material properties of euphausiids and other zooplankton from the Bering
Sea
SO JOURNAL OF THE ACOUSTICAL SOCIETY OF AMERICA
LA English
DT Article
ID POLLOCK THERAGRA-CHALCOGRAMMA; SOUND-SPEED; ACOUSTIC SCATTERING;
PRIBILOF ISLANDS; ANTARCTIC KRILL; BACKSCATTERING; DENSITY; VARIABILITY;
CONTRASTS; ABUNDANCE
AB Acoustic assessment of Bering Sea euphausiids and their predators can provide useful data for ecosystem studies if the acoustic scattering characteristics of these animals are known. The amount of acoustic energy that is scattered by different marine zooplankton taxa is strongly affected by the contrast of the animal's density (g) and sound speed (h) with the surrounding seawater. Density and sound speed contrast were measured in the Bering Sea during the summer of 2008 for several different zooplankton and nekton taxa including: euphausiids (Thysanoessa inermis, Thysanoessa raschii, and Thysanoessa spinifera), copepods, amphipods, chaetognaths, gastropods, fish larvae, jellyfish, and squid. Density contrast values varied between different taxa as well as between individual animals within the same species. Sound speed contrast was measured for monospecific groups of animals and differences were found among taxa. The range, mean, and standard deviation of g and h for all euphausiid species were: g=1.001-1.041; 1.018 +/- 0.009 and h=0.990-1.017; 1.006 +/- 0.008. Changes in the relationship between euphausiid material properties and animal length, seawater temperature, seawater density, and geographic location were also evaluated. Results suggest that environmental conditions at different sample locations led to significant differences in animal density and material properties. (C) 2010 Acoustical Society of America. [DOI: 10.1121/1.3488673]
C1 [Smith, Joy N.; Warren, Joseph D.] SUNY Stony Brook, Sch Marine & Atmospher Sci, Southampton, NY 11968 USA.
[Ressler, Patrick H.] NOAA, Natl Marine Fisheries Serv, Alaska Fisheries Sci Ctr, Resource Assessment & Conservat Engn Div, Seattle, WA 98115 USA.
RP Warren, JD (reprint author), SUNY Stony Brook, Sch Marine & Atmospher Sci, 239 Montauk Highway, Southampton, NY 11968 USA.
EM joe.warren@stonybrook.edu
FU Alaska Fisheries Science Center; National Marine Fisheries Service;
NOAA; North Pacific Research Board
FX This project was supported by the Alaska Fisheries Science Center,
National Marine Fisheries Service, NOAA, and the North Pacific Research
Board's Bering Sea Integrated Ecosystem Research Program. The captain,
crew, and scientists aboard the NOAA ship Oscar Dyson provided excellent
logistical support and sampling assistance. Abigail McCarthy helped us
greatly with the set up and maintenance of the on board aquaria as well
as with the trawl sampling operations. We acknowledge the taxonomic
advice of Elaina Jorgensen (squid) and Claudia Mills (hydromedusae). We
would like to thank Alex De Robertis and Neal Williamson for their
comments and suggestions on this manuscript.
NR 44
TC 15
Z9 15
U1 0
U2 15
PU ACOUSTICAL SOC AMER AMER INST PHYSICS
PI MELVILLE
PA STE 1 NO 1, 2 HUNTINGTON QUADRANGLE, MELVILLE, NY 11747-4502 USA
SN 0001-4966
J9 J ACOUST SOC AM
JI J. Acoust. Soc. Am.
PD NOV
PY 2010
VL 128
IS 5
BP 2664
EP 2680
DI 10.1121/1.3488673
PG 17
WC Acoustics; Audiology & Speech-Language Pathology
SC Acoustics; Audiology & Speech-Language Pathology
GA 685GT
UT WOS:000284617900037
PM 21110563
ER
PT J
AU Shapiro, A
Willingham, KM
Potvin, CK
AF Shapiro, Alan
Willingham, Katherine M.
Potvin, Corey K.
TI Spatially Variable Advection Correction of Radar Data. Part I.
Theoretical Considerations
SO JOURNAL OF THE ATMOSPHERIC SCIENCES
LA English
DT Article
ID SINGLE-DOPPLER RADAR; NUMERICAL VARIATIONAL ANALYSIS; 3-DIMENSIONAL
WIND-FIELD; SEVERE FRONTAL RAINBAND; WEATHER RADAR; MOVING-FRAME;
THERMODYNAMIC RETRIEVAL; VELOCITY RETRIEVALS; BOUNDARY-LAYER; PHOENIX-II
AB Radar data based analysis products such as accumulated rainfall maps dual Doppler wind syntheses and the) modynamic retrievals are prone to substantial error it the temporal sampling interval is too coarse Techniques to mitigate these errors typically make use of advection correction procedures (since to time conversions) in which the analyzed radial velocity or reflectivity field is idealized as a pattern of unchanging form that translates horizontally at constant speed The present study is concerned with in advection correction procedure for the reflectivity field in which the pattern advection component vary spatially The analysis is phrased as a variational problem in which errors in the frozen turbulence constraint are minimized subject to smoothness constraints The Euler-Lagrange equations for this problem are derived and a solution is proposed in which the trajectories pattern advection fields and reflectivity field are analyzed simultaneouslv using a combined analytical and numerical procedure The potential for solution nonuniqueness is explored
C1 [Shapiro, Alan; Potvin, Corey K.] Univ Oklahoma, Sch Meteorol, Norman, OK 73072 USA.
[Shapiro, Alan; Potvin, Corey K.] Univ Oklahoma, Ctr Anal & Predict Storms, Norman, OK 73072 USA.
[Willingham, Katherine M.; Potvin, Corey K.] Univ Oklahoma, Cooperat Inst Mesoscale Meteorol Studies, Norman, OK 73072 USA.
[Willingham, Katherine M.] NOAA, OAR, Natl Severe Storms Lab, Norman, OK USA.
RP Shapiro, A (reprint author), Univ Oklahoma, Sch Meteorol, 120 David L Boren Blvd,Room 5900, Norman, OK 73072 USA.
RI Shapiro, Alan/G-6116-2011
FU National Science Foundation (NSF) [ATM-0532107, EEC-0313747]; NOAA/NWS
[NA17RJ1227]
FX The authors thank the anonymous reviewers for their helpful comments
This research was supported by the National Science Foundation (NSF)
under Grant ATM-0532107, by the Engineering Research Centers Program of
the NSF under Cooperative Agreement EEC-0313747, and by the NOAA/NWS
Collaborative Science, Technology, and Applied Research (CSTAR) Program
through Grant NA17RJ1227
NR 72
TC 8
Z9 8
U1 0
U2 1
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0022-4928
J9 J ATMOS SCI
JI J. Atmos. Sci.
PD NOV
PY 2010
VL 67
IS 11
BP 3445
EP 3456
DI 10.1175/2010JAS3465.1
PG 12
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 686ZI
UT WOS:000284740600001
ER
PT J
AU Shapiro, A
Willingham, KM
Potvin, CK
AF Shapiro, Alan
Willingham, Katherine M.
Potvin, Corey K.
TI Spatially Variable Advection Correction of Radar Data. Part II Test
Results
SO JOURNAL OF THE ATMOSPHERIC SCIENCES
LA English
DT Article
ID DOPPLER WEATHER RADAR; TORNADO DETECTION; ASSIMILATION; WSR-88D;
SIGNATURES; SUPERCELL; SYSTEM; DETECT
AB The spatially variable advection correction/analysis procedure introduced in Part I is tested using analytical reflectivity blobs embedded in a solid body vortex and Terminal Doppler Weather Radar (TDWR) and Weather Surveillance Radar 1988 Doppler (WSR 88D) data of a tornadic supercell thunderstorm that passed over central Oklahoma on 8 May 2003 In the TDWR tests plan position indicator (PPI) data at two volume scan times are input to the advection correction procedure with PPI data from a third scan time intermediate between the two input times that is used to validate the results The procedure yields analyzed reflectivity fields with lower root mean square errors and higher correlation coefficients than those reflectivity fields that were advection corrected with any constant advection speed
C1 [Shapiro, Alan; Potvin, Corey K.] Univ Oklahoma, Sch Meteorol, Norman, OK 73072 USA.
[Shapiro, Alan; Potvin, Corey K.] Univ Oklahoma, Ctr Anal & Predict Storms, Norman, OK 73072 USA.
[Willingham, Katherine M.; Potvin, Corey K.] Univ Oklahoma, Cooperat Inst Mesoscale Meteorol Studies, Norman, OK 73072 USA.
[Willingham, Katherine M.] NOAA, OAR, Natl Severe Storms Lab, Norman, OK USA.
RP Shapiro, A (reprint author), Univ Oklahoma, Sch Meteorol, 120 David L Boren Blvd,Room 5900, Norman, OK 73072 USA.
RI Shapiro, Alan/G-6116-2011
FU National Science Foundation (NSF) [ATM-0532107, EEC-0313747]; NOAA/NWS
[NA17RJ1227]
FX The authors thank the anonymous reviewers for their helpful comments
This research was supported by the National Science Foundation (NSF)
under Grant ATM-0532107, by the Engineering Research Centers Program of
the NSF under Cooperative Agreement EEC-0313747, and by the NOAA/NWS
Collaborative Science, Technology, and Applied Research (CSTAR) Program
through Grant NA17RJ1227 Solo II and REORDER software developed at the
National Center for Atmospheric Research (NCAR) were used in the
processing of the radar data
NR 24
TC 6
Z9 6
U1 0
U2 1
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0022-4928
J9 J ATMOS SCI
JI J. Atmos. Sci.
PD NOV
PY 2010
VL 67
IS 11
BP 3457
EP 3470
DI 10.1175/2010JAS3466.1
PG 14
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 686ZI
UT WOS:000284740600002
ER
PT J
AU Kulie, MS
Bennartz, R
Greenwald, TJ
Chen, Y
Weng, FZ
AF Kulie, Mark S.
Bennartz, Ralf
Greenwald, Thomas J.
Chen, Yong
Weng, Fuzhong
TI Uncertainties in Microwave Properties of Frozen Precipitation
Implications for Remote Sensing and Data Assimilation
SO JOURNAL OF THE ATMOSPHERIC SCIENCES
LA English
DT Article
ID RADIATIVE-TRANSFER MODEL; PARTICLE-SIZE DISTRIBUTIONS; WEATHER
PREDICTION MODELS; SUCCESSIVE-ORDER; 1D+4D-VAR ASSIMILATION; RETRIEVAL
ALGORITHM; SOUNDING UNIT; ICE PARTICLES; AMSR-E; CLOUD
AB A combined active/passive modeling system that converts CloudSat observations to simulated microwave brightness temperatures (T-B) is used to assess different ice particle models under precipitating conditions Simulation results indicate that certain ice models (e g low density spheres) produce excessive scattering and implausibly low simulated T(B)s for stratiform precipitation events owing to excessive derived ice water paths (IWPs) while other ice models produce unphysical T-B depressions due to the combined effects of elevated derived IWP and excessive particle size distribution-averaged extinction An ensemble of nonspherical ice particle models however consistently produces realistic results under most circumstances and adequately captures the radiative properties of frozen hydrometeors associated with precipitation-with the possible exception of very high IWP events Large derived IWP uncertainties exceeding 60% are also noted and may indicate IWP retrieval accuracy deficiencies using high frequency passive microwave observations Simulated T-B uncertainties due to the ice particle model ensemble members approach 9 (5) K at 89 (157) GHz for high ice water path conditions associated with snowfall and similar to 2-3 (similar to 1-2) K under typical stratiform rain conditions These uncertainties however display considerable variability owing to ice water path precipitation type, satellite zenith angle and frequency Comparisons between 157 GHz simulations and observations under precipitating conditions produce low biases (<1 5 K) and high correlations but lower frequency channels display consistent negative biases of 3-4 K in precipitating regions Sample en or correlations and covariance matrices for select microwave frequencies also show strong functional relationships with ice water pat h and variability depending on precipitation type
C1 [Kulie, Mark S.; Bennartz, Ralf] Univ Wisconsin, Dept Atmospher & Ocean Sci, Madison, WI 53706 USA.
[Greenwald, Thomas J.] Univ Wisconsin, Cooperat Inst Meteorol Satellite Studies, Madison, WI 53706 USA.
[Chen, Yong; Weng, Fuzhong] Joint Ctr Satellite Data Assimilat, Camp Springs, MD USA.
[Weng, Fuzhong] NOAA, NESDIS, Off Res & Applicat, Camp Springs, MD USA.
RP Kulie, MS (reprint author), Univ Wisconsin, Dept Atmospher & Ocean Sci, 1225 W Dayton St, Madison, WI 53706 USA.
RI Kulie, Mark/C-3289-2011; Bennartz, Ralf/F-3760-2010; Chen,
Yong/E-4321-2010; Weng, Fuzhong/F-5633-2010
OI Kulie, Mark/0000-0003-1400-1007; Chen, Yong/0000-0002-0279-9405; Weng,
Fuzhong/0000-0003-0150-2179
FU Joint Center for Satellite Data Assimilation through NOAA
[NA06NES4400002]; NASA [NNX07AE29G]
FX The authors would like to acknowledge the CloudSat project and its Data
Processing Center, as well as the National Snow and Ice Data Center and
NOAA's Comprehensive Large Array Data Stewardship System, for products
used in this study Dr Gang Hong is thanked for supplying microwave
properties for some of the ice particle models used in this study Dr
Guosheng Liu is gratefully acknowledged for making his database publicly
available and easily accessible Mr Michael Hiley provided extensive and
invaluable data processing assistance for this study The authors would
also like to thank three anonymous reviewers for their constructive
comments This work was partially funded by the Joint Center for
Satellite Data Assimilation through NOAA Cooperative Agreement
NA06NES4400002 and NASA Grant NNX07AE29G
NR 54
TC 40
Z9 40
U1 2
U2 16
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0022-4928
EI 1520-0469
J9 J ATMOS SCI
JI J. Atmos. Sci.
PD NOV
PY 2010
VL 67
IS 11
BP 3471
EP 3487
DI 10.1175/2010JAS3520.1
PG 17
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 686ZI
UT WOS:000284740600003
ER
PT J
AU Jiang, HL
Feingold, G
Sorooshian, A
AF Jiang, Hongli
Feingold, Graham
Sorooshian, Armin
TI Effect of Aerosol on the Susceptibility and Efficiency of Precipitation
in Warm Trade Cumulus Clouds
SO JOURNAL OF THE ATMOSPHERIC SCIENCES
LA English
DT Article
ID LARGE-EDDY SIMULATIONS; SHALLOW CUMULUS; STRATOCUMULUS CLOUDS; DRIZZLE;
MODEL; CONVECTION; RAIN; SENSITIVITY; STATISTICS; EVOLUTION
AB Large eddy simulations of warm trade wind cumulus clouds are conducted for a range of aerosol conditions with a focus on precipitating clouds Individual clouds are tracked over the course of their lifetimes Precipitation rate decreases progressively as aerosol Increases For larger precipitating clouds the polluted clouds have longer lifetimes because of precipitation suppression For clean aerosol conditions there is good agreement between the average model precipitation rate and that calculated based on observed radar reflectivity Z and precipitation rate R relationships Precipitation rate can be expressed as a power law function of liquid water path (LWP) and N-d to reasonable accuracy The respective powers for LWP and N-d are of similar magnitude compared to those based on observational studies of stratocumulus clouds The time integrated precipitation rate represented by a power law function of LWP N-d and cloud lifetime is much more reliably predicted than is R expressed in terms of LWP and N-d alone The precipitation susceptibility (So = dInR/dInN(d)) that quantifies the sensitivity of precipitation to changes in N-d depends strongly on LWP and exhibits nonmonotonic behavior with a maximum at intermediate LWP values The relationship between So and precipitation efficiency is explored and the Importance of including dependence on N-d in the latter is highlighted The results provide trade cumulus cloud population statistics as well as relationships between (memicrophysical/macrophysical properties and precipitation that are amenable for use in larger scale models
C1 [Jiang, Hongli; Feingold, Graham] NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA.
[Jiang, Hongli] Colorado State Univ, Cooperat Inst Res Atmosphere, Ft Collins, CO 80523 USA.
[Sorooshian, Armin] Univ Arizona, Dept Chem & Environm Engn, Tucson, AZ USA.
RP Jiang, HL (reprint author), NOAA, Earth Syst Res Lab, 325 Broadway, Boulder, CO 80305 USA.
RI Feingold, Graham/B-6152-2009; Jiang, Hongli/N-3281-2014; Manager, CSD
Publications/B-2789-2015;
OI Sorooshian, Armin/0000-0002-2243-2264
FU NOAA's Climate Goal; ONR; NOAA's High Performance Computing Center at
the Earth System Research Laboratory
FX HJ and GF were funded by NOAA's Climate Goal AS acknowledges support
from an ONR YIP award The authors acknowledge the excellent support of
NOAA's High Performance Computing Center at the Earth System Research
Laboratory and comments and suggestions by the anonymous reviewers
NR 43
TC 27
Z9 27
U1 0
U2 13
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0022-4928
EI 1520-0469
J9 J ATMOS SCI
JI J. Atmos. Sci.
PD NOV
PY 2010
VL 67
IS 11
BP 3525
EP 3540
DI 10.1175/2010JAS3484.1
PG 16
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 686ZI
UT WOS:000284740600006
ER
PT J
AU Dong, MY
Chen, LS
Li, Y
Lu, CG
AF Dong, Meiying
Chen, Lianshou
Li, Ying
Lu, Chungu
TI Rainfall Reinforcement Associated with Landfalling Tropical Cyclones
SO JOURNAL OF THE ATMOSPHERIC SCIENCES
LA English
DT Article
ID EXTRATROPICAL CYCLONE; STORM AGNES; JUNE 1972; PRECIPITATION;
TRANSFORMATION; SIMULATION; TAIWAN; IMPACT; MOTION; SHEAR
AB Landfalling tropical cyclones (TCs) often bring about heavy rainfall which typically decreases with the weakening of the TCs However, some TCs may suddenly be reinvigorated after they become remnants over land Such TCs may produce even stronger rains than those at the time of their landfall This reinvigorating phenomenon is known as rainfall reinforcement associated with landfalling tropical cyclones (RRLTC) The TCs triggering rainfall reinforcement account for 9 7% of the total number of TCs that make landfall on mainland China and often cause problems and surprises for forecasters The TCs with rainfall reinforcement mostly make landfall in the area of the southeastern coast of China and move primarily along two tracks spreading northward or westward RRLTC often occurs in the remnant of a tropical depression that has already been downgraded from typhoon intensity particularly in a period when the remnant Iris slowed down or even stagnated The highest frequency of RRLTC occurrence is during the third day after landfall and in the northeast quadrant of a TC moving northward and the southwest quadrants of a TC moving westward
Diagnostic analysis shows that an RRLTC with a northward track can be mainly attributed to the in teraction between westerly troughs and the tropical cyclone In this way a remnant gains baroclinic energy from the midlatitude trough Such an interaction does not appear for northward track TCs without rainfall reinforcement Rainfall reinforcement for TCs with a westward track is mainly due to the interaction between monsoon surge cloud clusters and tropical cyclones which is favorable for moisture and latent he'd gain Analyses show that the westward TCs would not have, rainfall reinforcement without such an Interaction RRLTC requires new energy transport into TCs The results of the present study indicate that baroclinic potential energy and latent heat are the two major energy sources that will trigger the remnant revival and rainfall reinforcement Land surface topography also plays an important role in increasing the rainfall of TCs
C1 [Dong, Meiying; Chen, Lianshou; Li, Ying] Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Nanjing, Peoples R China.
[Dong, Meiying] Nanjing Univ Informat Sci & Technol, Nanjing, Peoples R China.
[Dong, Meiying] Zhejiang Prov Meteorol Observ, Hangzhou, Zhejiang, Peoples R China.
[Lu, Chungu] NOAA, Earth Syst Res Lab, Boulder, CO USA.
RP Lu, CG (reprint author), DSRC, 325 S Broadway, Boulder, CO 80305 USA.
FU China National Key Basic Research and Development Project [2009CB421504,
2004CB418301]; China National Science Foundation [40730948, 40675033];
Chinese Academy of Meteorological Sciences [2007Y006]; Zhejiang Science
Project for Social Development [2007C13G1610002]
FX The research is supported by the China National Key Basic Research and
Development Project (Grants 2009CB421504 and 2004CB418301), China
National Science Foundation (Grants 40730948 and 40675033), Special
Project of Chinese Academy of Meteorological Sciences (2007Y006), and
Zhejiang Science Project for Social Development (Grant 2007C13G1610002)
The authors are grateful for the constructive comments from three
anonymous reviewers and excellent editorship by Dr Shigeo Yoden Helpful
comments and discussions from Dr Taoyong Peng are appreciated We are
also grateful to Annie Reiser for providing typographical, grammar, and
style edits for this paper
NR 40
TC 19
Z9 24
U1 0
U2 7
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0022-4928
J9 J ATMOS SCI
JI J. Atmos. Sci.
PD NOV
PY 2010
VL 67
IS 11
BP 3541
EP 3558
DI 10.1175/2010JAS3268.1
PG 18
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 686ZI
UT WOS:000284740600007
ER
PT J
AU Lohbauer, U
Amberger, G
Quinn, GD
Scherrer, SS
AF Lohbauer, Ulrich
Amberger, Gudrun
Quinn, George D.
Scherrer, Susanne S.
TI Fractographic analysis of a dental zirconia framework: A case study on
design issues
SO JOURNAL OF THE MECHANICAL BEHAVIOR OF BIOMEDICAL MATERIALS
LA English
DT Article
DE Fractography; Failure analysis; Ceramic restoration; Zirconia; Fixed
partial denture; Dental ceramic
ID FIXED PARTIAL DENTURES; FINITE-ELEMENT-ANALYSIS; OF-THE-LITERATURE;
IN-VITRO; FAILURE ANALYSIS; CERAMIC CROWNS; FRACTURE-RESISTANCE; LUTING
AGENTS; STRENGTH; RESIN
AB Fractographic analysis of clinically failed dental ceramics can provide insights as to the failure origin and related mechanisms. One anterior 6-unit all-ceramic zirconia fixed partial denture (FPD) (Cercon (R)) has been clinically recovered and examined using qualitative fractography. The purpose was to identify the fracture origin and to state the reasons for failure. The recovered parts of the zirconia FPD were microscopically examined to identify classic fractographic patterns such as arrest lines, hackle, twist hackle and wake hackle. The direction of crack propagation was mapped and interpreted back to the origin of failure at the interface of the occlusal-palatal tip of the core and the veneering ceramic. An inappropriate core drop design favoring localized stress concentration combined with a pore cluster in the veneering ceramic at the core tip interface were the reasons for this premature through-the-core thickness failure. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Quinn, George D.] Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
[Scherrer, Susanne S.] Univ Geneva, Sch Dent Med, Geneva, Switzerland.
[Lohbauer, Ulrich; Amberger, Gudrun] Univ Erlangen Nuernberg, Erlangen, Germany.
RP Lohbauer, U (reprint author), Dent Clin 1 Operat Dent & Periodontol, Glueckstr 11, D-91054 Erlangen, Germany.
EM lohbauer@dent.uni-erlangen.de; amberger@dent.uni-erlangen.de;
George.quinn@nist.gov; Susanne.Scherrer@unige.ch
FU National Institute for Standards and Technology; American Dental
Association Foundation; National Institute of Health [NIH R01-DE17983]
FX This work was partially supported by National Institute for Standards
and Technology, American Dental Association Foundation and National
Institute of Health with grant NIH R01-DE17983.
NR 36
TC 21
Z9 21
U1 2
U2 9
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1751-6161
J9 J MECH BEHAV BIOMED
JI J. Mech. Behav. Biomed. Mater.
PD NOV
PY 2010
VL 3
IS 8
BP 623
EP 629
DI 10.1016/j.jmbbm.2010.07.004
PG 7
WC Engineering, Biomedical; Materials Science, Biomaterials
SC Engineering; Materials Science
GA 665AZ
UT WOS:000283007800010
PM 20826369
ER
PT J
AU Diddams, SA
AF Diddams, Scott A.
TI The evolving optical frequency comb
SO JOURNAL OF THE OPTICAL SOCIETY OF AMERICA B-OPTICAL PHYSICS
LA English
DT Article
ID FEMTOSECOND LASER FREQUENCY; MODE-LOCKED LASER; TI-SAPPHIRE LASER; LOW
PHASE-NOISE; 2-PHOTON SPECTROSCOPY; MICROWAVE SIGNALS; NOBEL LECTURE;
LIGHT-PULSES; GENERATION; PRECISION
AB In the past decade we have witnessed remarkable advances associated with the frequency stabilization of the comb present in the output of a mode-locked femtosecond laser. While proving itself to be fantastically successful in its role as the "gears" of optical atomic clocks, the optical frequency comb has further evolved into a valuable tool for a wide range of applications, including ultraviolet and infrared spectroscopy, frequency synthesis, optical and microwave waveform generation, astronomical spectrograph calibration, and attosecond pulse generation, to name a few. In this review, I will trace several of these developments while attempting to offer perspective on the challenges and opportunities for frequency combs that might lie ahead in the next decade.
C1 Natl Inst Stand & Technol, Div Time & Frequency, Boulder, CO 80305 USA.
RP Diddams, SA (reprint author), Natl Inst Stand & Technol, Div Time & Frequency, 325 Broadway, Boulder, CO 80305 USA.
EM sdiddams@boulder.nist.gov
RI Diddams, Scott/L-2819-2013
NR 101
TC 171
Z9 173
U1 10
U2 63
PU OPTICAL SOC AMER
PI WASHINGTON
PA 2010 MASSACHUSETTS AVE NW, WASHINGTON, DC 20036 USA
SN 0740-3224
J9 J OPT SOC AM B
JI J. Opt. Soc. Am. B-Opt. Phys.
PD NOV
PY 2010
VL 27
IS 11
BP B51
EP B62
PG 12
WC Optics
SC Optics
GA 674VS
UT WOS:000283778900007
ER
PT J
AU Katayama, N
Ji, SD
Louca, D
Lee, S
Fujita, M
Sato, TJ
Wen, JS
Xu, ZJ
Gu, GD
Xu, GY
Lin, ZW
Enoki, M
Chang, S
Yamada, K
Tranquada, JM
AF Katayama, Naoyuki
Ji, Sungdae
Louca, Despina
Lee, Seunghun
Fujita, Masaki
Sato, Taku J.
Wen, Jinsheng
Xu, Zhijun
Gu, Genda
Xu, Guangyong
Lin, Ziwei
Enoki, Masanori
Chang, Sung
Yamada, Kazuyoshi
Tranquada, John M.
TI Investigation of the Spin-Glass Regime between the Antiferromagnetic and
Superconducting Phases in Fe1+ySexTe1-x
SO JOURNAL OF THE PHYSICAL SOCIETY OF JAPAN
LA English
DT Article
DE Fe based superconductivity; neutron scattering; spin glass; phase
diagram; Fe(Se,Te)
ID SMFEASO1-XFX; MAGNETISM; ORDER; STATE
AB Using bulk magnetization along with elastic and inelastic neutron scattering techniques, we have investigated the phase diagram of Fe1+ySexTe1-x and the nature of magnetic correlations in three nonsuperconducting samples of Fe1.01Se0.1Te0.9, Fe1.01Se0.15Te0.85, and Fe1.02Se0.3Te0.7. A cusp and hysteresis in the temperature dependence of the magnetization for the x = 0.15 and 0.3 samples indicates spin-glass (SG) ordering below T-sg = 23 K. Neutron scattering measurements indicate that the spin-glass behavior is associated with short-range spin density wave (SDW) ordering characterized by a static component and a low-energy dynamic component with a characteristic incommensurate wave vector of Q(m) = (0.46, 0, 0.50) and an anisotropy gap of similar to 2.5 meV. Our high Q-resolution data also show that the systems undergo a glassy structural distortion that coincides with the short-range SDW order.
C1 [Katayama, Naoyuki; Ji, Sungdae; Louca, Despina; Lee, Seunghun] Univ Virginia, Dept Phys, Charlottesville, VA 22904 USA.
[Fujita, Masaki; Enoki, Masanori; Yamada, Kazuyoshi] Tohoku Univ, Inst Mat Res, Sendai, Miyagi 9808577, Japan.
[Sato, Taku J.; Tranquada, John M.] Univ Tokyo, Inst Solid State Phys, Chiba 2778581, Japan.
[Wen, Jinsheng; Xu, Zhijun; Gu, Genda; Xu, Guangyong; Lin, Ziwei] Brookhaven Natl Lab, Condensed Matter Phys & Mat Sci Dept, Upton, NY 11973 USA.
[Chang, Sung] Natl Inst Stand & Technol, NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA.
RP Katayama, N (reprint author), Univ Virginia, Dept Phys, Charlottesville, VA 22904 USA.
RI Wen, Jinsheng/F-4209-2010; Yamada, Kazuyoshi/C-2728-2009; Tranquada,
John/A-9832-2009; Xu, Guangyong/A-8707-2010; xu, zhijun/A-3264-2013;
Fujita, Masaki/D-8430-2013; Sato, Taku/I-7664-2015; Ji,
Sungdae/G-3808-2010
OI Wen, Jinsheng/0000-0001-5864-1466; Tranquada, John/0000-0003-4984-8857;
Xu, Guangyong/0000-0003-1441-8275; xu, zhijun/0000-0001-7486-2015; Sato,
Taku/0000-0003-2511-4998; Ji, Sungdae/0000-0001-6736-3103
FU U.S. Department of Energy, Office of Basic Energy Sciences, Division of
Materials Sciences and Engineering [DE-FG02-07ER45384,
DE-FG02-01ER45927, DE-AC02-98CH110886]; National Science Foundation
[DMR-0454672]
FX Work at the University of Virginia (Brookhaven) is supported by the U.S.
Department of Energy, Office of Basic Energy Sciences, Division of
Materials Sciences and Engineering, under Contract Nos.
DE-FG02-07ER45384 and DE-FG02-01ER45927 (DE-AC02-98CH110886). This work
utilized facilities supported in part by the National Science Foundation
under Agreement No. DMR-0454672.
NR 30
TC 53
Z9 54
U1 2
U2 28
PU PHYSICAL SOC JAPAN
PI TOKYO
PA YUSHIMA URBAN BUILDING 5F, 2-31-22 YUSHIMA, BUNKYO-KU, TOKYO, 113-0034,
JAPAN
SN 0031-9015
J9 J PHYS SOC JPN
JI J. Phys. Soc. Jpn.
PD NOV
PY 2010
VL 79
IS 11
AR 113702
DI 10.1143/JPSJ.79.113702
PG 4
WC Physics, Multidisciplinary
SC Physics
GA 671OE
UT WOS:000283514600004
ER
PT J
AU Naulleau, PP
Gallatin, GM
AF Naulleau, Patrick P.
Gallatin, Gregg M.
TI Effect of resist on the transfer of line-edge roughness spatial metrics
from mask to wafer
SO JOURNAL OF VACUUM SCIENCE & TECHNOLOGY B
LA English
DT Article
ID EXTREME-ULTRAVIOLET LITHOGRAPHY; CHEMICALLY AMPLIFIED PHOTORESIST;
EFFICIENCY; RESOLUTION; ALIGNMENT; SYSTEMS; IMPACT; MODEL
AB Mask contributors to line-edge roughness (LER) have recently been shown to be an issue of concern for extreme ultraviolet lithography both in terms of the accuracy of current resist evaluation tests and in terms of the ultimate LER requirements for the 22 nm production node and beyond. More recently, it has been shown that the power spectral density of the mask-induced roughness is markedly different from that of intrinsic resist roughness and thus potentially serves as a mechanism for distinguishing mask effects from resist effects in experimental results. However, the evaluation of stochastic effects in the resist itself demonstrates that such a test would only be viable in cases where the resist effects are negligible in terms of their contribution to the total LER compared with the mask effects. Moreover, the results presented here lead the authors to the surprising conclusion that it is indeed possible for mask contributors to be the dominant source of LER while the spatial characteristics of the LER remain indistinguishable from the fractal characteristics of resist-induced LER. (C) 2010 American Vacuum Society. [DOI: 10.1116/1.3509437]
C1 [Naulleau, Patrick P.] Univ Calif Berkeley, Lawrence Berkeley Lab, Ctr Xray Opt, Berkeley, CA 94720 USA.
[Gallatin, Gregg M.] NIST, Ctr Nanoscale Sci & Technol, Gaithersburg, MD 20899 USA.
RP Naulleau, PP (reprint author), Univ Calif Berkeley, Lawrence Berkeley Lab, Ctr Xray Opt, Berkeley, CA 94720 USA.
EM pnaulleau@lbl.gov
RI Gallatin, Gregg/H-1998-2012
FU SEMATECH; Director, Office of Science, Office of Basic Energy Sciences,
of the U. S. Department of Energy [DE-AC02-05CH11231]
FX This work was funded in part by SEMATECH; the authors are grateful to
Warren Montgomery for program support. This work was partially carried
out at Lawrence Berkeley National Laboratory, which is supported by the
Director, Office of Science, Office of Basic Energy Sciences, of the U.
S. Department of Energy under Contract No. DE-AC02-05CH11231.
NR 30
TC 11
Z9 11
U1 0
U2 2
PU A V S AMER INST PHYSICS
PI MELVILLE
PA STE 1 NO 1, 2 HUNTINGTON QUADRANGLE, MELVILLE, NY 11747-4502 USA
SN 1071-1023
J9 J VAC SCI TECHNOL B
JI J. Vac. Sci. Technol. B
PD NOV
PY 2010
VL 28
IS 6
BP 1259
EP 1266
DI 10.1116/1.3509437
PG 8
WC Engineering, Electrical & Electronic; Nanoscience & Nanotechnology;
Physics, Applied
SC Engineering; Science & Technology - Other Topics; Physics
GA 690OX
UT WOS:000285015200159
ER
PT J
AU Steele, AV
Knuffman, B
McClelland, JJ
Orloff, J
AF Steele, A. V.
Knuffman, B.
McClelland, J. J.
Orloff, J.
TI Focused chromium ion beam
SO JOURNAL OF VACUUM SCIENCE & TECHNOLOGY B
LA English
DT Article
ID ATOMS; NANOTECHNOLOGY; PROBE
AB With the goal of expanding the capabilities of focused ion beam microscopy and milling systems, the authors have demonstrated nanoscale focusing of chromium ions produced in a magneto-optical trap ion source. Neutral chromium atoms are captured into a magneto-optical trap and cooled to 100 mu K with laser light at 425 nm. The atoms are subsequently photoionized and accelerated to energies between 0.5 and 3 keV. The accelerated ion beam is scanned with a dipolar deflector and focused onto a sample by an einzel lens. Secondary electron images are collected and analyzed, and from these, a beam diameter is inferred. The result is a focused probe with a 1 standard-deviation radius as small as 205 +/- 10 nm. While this probe size is in the useful range for nanoscale applications, it is almost three times larger than is predicted by ray-tracing simulations. Possible explanations for this discrepancy are discussed. (C) 2010 American Vacuum Society. [DOI: 10.1116/1.3502668]
C1 [Steele, A. V.; Knuffman, B.; McClelland, J. J.] NIST, Ctr Nanoscale Sci & Technol, Gaithersburg, MD 20899 USA.
[Orloff, J.] FEI Co, Hillsboro, OR 97124 USA.
RP Steele, AV (reprint author), NIST, Ctr Nanoscale Sci & Technol, Gaithersburg, MD 20899 USA.
EM adam.steele@nist.gov
RI McClelland, Jabez/A-2358-2015
OI McClelland, Jabez/0000-0001-5672-5965
NR 23
TC 10
Z9 10
U1 0
U2 7
PU A V S AMER INST PHYSICS
PI MELVILLE
PA STE 1 NO 1, 2 HUNTINGTON QUADRANGLE, MELVILLE, NY 11747-4502 USA
SN 1071-1023
J9 J VAC SCI TECHNOL B
JI J. Vac. Sci. Technol. B
PD NOV
PY 2010
VL 28
IS 6
BP C6F1
EP C6F5
DI 10.1116/1.3502668
PG 5
WC Engineering, Electrical & Electronic; Nanoscience & Nanotechnology;
Physics, Applied
SC Engineering; Science & Technology - Other Topics; Physics
GA 690OX
UT WOS:000285015200030
ER
PT J
AU Meegan, J
Field, C
Sidor, I
Romano, T
Casinghino, S
Smith, CR
Kashinsky, L
Fair, PA
Bossart, G
Wells, R
Dunn, JL
AF Meegan, Jenny
Field, Cara
Sidor, Inga
Romano, Tracy
Casinghino, Sandra
Smith, Cynthia R.
Kashinsky, Lizabeth
Fair, Patricia A.
Bossart, Gregory
Wells, Randall
Dunn, J. Lawrence
TI Development, validation, and utilization of a competitive enzyme-linked
immunosorbent assay for the detection of antibodies against Brucella
species in marine mammals
SO JOURNAL OF VETERINARY DIAGNOSTIC INVESTIGATION
LA English
DT Article
DE Brucella; competitive enzyme-linked; immunosorbent; assay; marine;
mammals; validation
ID BOTTLE-NOSED DOLPHINS; NORTH-ATLANTIC OCEAN; SEALS PHOCA-HISPIDA; BOVINE
BRUCELLOSIS; RINGED SEALS; MOLECULAR CHARACTERIZATION;
TURSIOPS-TRUNCATUS; DNA POLYMORPHISM; SP INFECTION; STRAINS
AB A competitive enzyme-linked immunosorbent assay (cELISA) was developed by using a whole-cell antigen from a marine Brucella sp isolated from a harbor seal (Phoca vitulina) The assay was designed to screen sera from multiple marine mammal species for the presence of antibodies against marine-origin Brucella Based on comparisons with culture confirmed cases specificity and sensitivity for cetacean samples tested were 73% and 100%, respectively For pinniped samples, specificity and sensitivity values were 77% and 67%, respectively Hawaiian monk seal (Monachus schauinslandi, n = 28) and bottlenose dolphin (Turstops truncatus, n = 48) serum samples were tested, and the results were compared with several other assays designed to detect Brucella abortus antibodies The comparison testing revealed the marine-origin cELISA to be more sensitive than the B abortus tests by the detection of additional positive serum samples The newly developed cELISA is an effective serologic method for detection of the presence of antibodies against marine-origin Brucella sp in marine mammals
C1 [Meegan, Jenny; Field, Cara; Sidor, Inga; Romano, Tracy; Casinghino, Sandra; Dunn, J. Lawrence] Mystic Aquarium & Inst Explorat, Mystic, CT USA.
[Kashinsky, Lizabeth] Univ Hawaii, Joint Inst Marine & Atmospher Res, Honolulu, HI 96822 USA.
[Smith, Cynthia R.] USN, Marine Mammal Program, Space & Naval Warfare Syst Ctr, San Diego, CA 92152 USA.
[Fair, Patricia A.] NOAA, Natl Ocean Serv Ctr Coastal Environm Hlth & Biomo, Charleston, SC USA.
[Wells, Randall] Mote Marine Lab, Chicago Zool Soc, Sarasota, FL 34236 USA.
[Bossart, Gregory] Harbor Branch Oceanog Inst Inc, Ft Pierce, FL 34946 USA.
RP Meegan, J (reprint author), Univ Florida, Coll Vet Med, Aquat Anim Hlth Dept, Gainesville, FL 32610 USA.
FU National Oceanic and Atmospheric Association (NOAA) [NA04OAR4600209,
NA03NMF4390408]; Harbor Branch Oceanographic Institution's; Wild
Dolphins license tag; NOAA National Marine Fisheries Service; Dolphin
Quest; Disney's Animal Programs
FX The Brucella Project is funded by National Oceanic and Atmospheric
Association (NOAA) Oceans and Human Health Initiative Grant
NA04OAR4600209 and has received previous support from the NOAA Fisheries
Prescott Grant Award NA03NMF4390408 The wild Hawaiian monk seal blood
samples were collected under Scientific Research and Enhancement Permit
to Take Marine Mammals 848-1335 The wild bottlenose dolphin blood
samples were collected under the National Marine Fisheries Service
Scientific Research permit 522 1569 and 522-1785 issued to Dr Randall
Wells of the Sarasota Dolphin Research Program (SDRP) in Sarasota Bay,
Florida and 998 1678 issued to Dr Greg Bossart as part of the Bottlenose
Dolphin Health and Risk Assessment Project conducted in the Indian River
Lagoon, Florida, and the estuarine waters of Charleston South Carolina
Funding was partially provided by the Harbor Branch Oceanographic
Institution's Project Wild Dolphins license tag, NOAA National Marine
Fisheries Service, Dolphin Quest, and Disney's Animal Programs Brian
Balmer's expertise in preparing and processing samples for the SDRP is
much appreciated The authors also thank John McGiven of the Veterinary
Laboratory Agency (Surrey UK) for supplying the terrestrial Brucella and
Yersinia serum samples This work constitutes scientific contribution 181
from the Sea Research Foundation
NR 39
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PU SAGE PUBLICATIONS INC
PI THOUSAND OAKS
PA 2455 TELLER RD, THOUSAND OAKS, CA 91320 USA
SN 1040-6387
J9 J VET DIAGN INVEST
JI J. Vet. Diagn. Invest.
PD NOV
PY 2010
VL 22
IS 6
BP 856
EP 862
PG 7
WC Veterinary Sciences
SC Veterinary Sciences
GA 685ZL
UT WOS:000284666500003
PM 21088168
ER
PT J
AU Singhal, G
Panchang, VG
Lillibridge, JL
AF Singhal, Gaurav
Panchang, Vijay G.
Lillibridge, John L.
TI Reliability Assessment for Operational Wave Forecasting System in Prince
William Sound, Alaska
SO JOURNAL OF WATERWAY PORT COASTAL AND OCEAN ENGINEERING-ASCE
LA English
DT Article
DE Prince William Sound; Wave forecast reliability; Likelihood of
occurrence
ID 2 NUMERICAL-MODELS; COASTAL REGIONS; SWAN MODEL; WIND-WAVES; WRF MODEL;
PREDICTION; CLIMATOLOGY; WEATHER; ESTUARY; BUOY
AB To ensure the safety of a variety of marine operations, ocean weather monitoring and prediction in many coastal regions have gained prominence over the last couple of decades. To support ongoing forecasting efforts in Prince William Sound, the site of the worst oil spill disaster in U.S. history, a three-way coupled wave forecasting system is developed. The issue of wave forecast reliability is addressed in the context of the associated uncertainty that confronts the manager of engineering operations or other planners. This issue has generally not been systematically addressed in literature. High-resolution 36-h daily forecasts of significant wave heights (SWHs) are compared with measurements from buoys and satellites for about I year. The results show that 70% of the peak SWHs (in the range 5-8 m) were predicted with an accuracy of 15% or less for a forecast lead time of 9 h. The errors are larger for smaller SWHs. Correlation coefficients (R(2)) and indices of agreement (D) between predicted and measured SWHs were reasonable and generally more than 0.78 for all lead times. On average, our analysis showed 70% or greater likelihood of the prediction falling within a tolerance of +/-(1 X RMSE) for all lead times. Barring changes in model physics, resolution, etc., similar acceptance levels could be expected from comparable systems.
C1 [Singhal, Gaurav; Panchang, Vijay G.] Texas A&M Univ, Galveston, TX 77553 USA.
[Lillibridge, John L.] NOAA Lab Satellite Altimetry, Silver Spring, MD 20910 USA.
RP Singhal, G (reprint author), Texas A&M Univ, 200 Seawolf Pkwy,POB 1675, Galveston, TX 77553 USA.
EM singhalg@tamug.edu; panchanv@tamug.edu; John.Lillibridge@noaa.gov
RI Lillibridge, John/F-5606-2010
OI Lillibridge, John/0000-0001-9102-171X
FU PWS OSRI through NOAA; Maine Sea Grant College Program; NASA; PWS
Regional Citizens' Advisory Council
FX This work was possible due to funding received from PWS OSRI (through a
NOAA grant), Maine Sea Grant College Program, NASA, and the PWS Regional
Citizens' Advisory Council. ENVISAT altimetry data were provided by the
European Space Agency. NOAA/NESDIS staff assisted with the satellite
data. The writers acknowledge Dr. Remko Scharroo for his continuing
support, maintenance, and development of the Radar Altimeter Database
system. The efforts of the NCEP, which make local predictions possible,
are invaluable. Dr. Yi Chao of JPL provided access to forecasts of
surface currents in PWS. Dr. Scott Pegau and his team helped in the
installation and provision of gauge data. All of the above contributions
are gratefully acknowledged. Dr. Khalid Zubier and Mr. Dongcheng Li made
technical contributions.
NR 32
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U2 10
PU ASCE-AMER SOC CIVIL ENGINEERS
PI RESTON
PA 1801 ALEXANDER BELL DR, RESTON, VA 20191-4400 USA
SN 0733-950X
J9 J WATERW PORT C-ASCE
JI J. Waterw. Port Coast. Ocean Eng.-ASCE
PD NOV-DEC
PY 2010
VL 136
IS 6
BP 337
EP 349
DI 10.1061/(ASCE)WW.1943-5460.0000056
PG 13
WC Engineering, Civil; Engineering, Ocean; Water Resources
SC Engineering; Water Resources
GA 670HL
UT WOS:000283411700005
ER
PT J
AU Gardner, CL
Lawler, JP
Hoef, JMV
Magoun, AJ
Kellie, KA
AF Gardner, Craig L.
Lawler, James P.
Hoef, Jay M. Ver
Magoun, Audrey J.
Kellie, Kalin A.
TI Coarse-Scale Distribution Surveys and Occurrence Probability Modeling
for Wolverine in Interior Alaska
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE detection probability; distribution mapping; Gulo gulo; hierarchical
spatial modeling; Interior Alaska; occurrence probability; track survey;
wolverine
ID CHAIN MONTE-CARLO; GULO-GULO; BRITISH-COLUMBIA; HABITAT USE; MORTALITY;
CANADA; TRACKS; SNOW
AB We determined wolverine (Gulo gulo) distribution and occurrence probabilities using aerial surveys and hierarchical spatial modeling in a 180,000-km(2) portion of Interior Alaska, USA. During 8 February-12 March 2006, we surveyed 149 of 180 1,000-km(2) sample units for wolverine tracks. We observed wolverine tracks in 99 (66.4%) sample units. Wolverine detection probability was >= 69% throughout the survey period. Posterior occurrence probabilities of whether a wolverine track occurred in a sample unit was dependent on survey timing, number of transects flown, number of neighboring sample units with detected tracks, percentage of the sample unit with elevation >= 305 m, and human influences. Our model indicated strong evidence of occurrence (>0.80) in 72% of the 180 survey units, strong evidence of absence (<0.20) in 12%, and weak evidence of occurrence or absence (0.20-0.80) in 16%. Wolverine area of occupancy made up 83% of the study area. Simulations illustrated that 2-4 survey routes were necessary for the survey technique to provide strong evidence of wolverine presence or absence in Interior Alaska if a track was not identified along the first route. The necessary number of survey routes depends on the occurrence probability in a sample unit. We provided managers with a map of wolverine distribution in Interior Alaska and an efficient and lower-cost method to detect coarse-scale changes in wolverine distribution. Our technique was effective in both Interior Alaska and Ontario, Canada, suggesting it would be effective throughout most of the boreal forest range of wolverines where tracks can be readily observed from the air. The technique requires a certain skill level in recognizing tracks; it is essential that tracks are identified correctly and training may be necessary depending on surveyor experience.
C1 [Gardner, Craig L.; Kellie, Kalin A.] Alaska Dept Fish & Game, Fairbanks, AK 99701 USA.
[Lawler, James P.] Natl Pk Serv, Fairbanks, AK 99709 USA.
[Hoef, Jay M. Ver] Natl Marine Fisheries Serv, Natl Ocean & Atmospher Adm, Natl Marine Mammal Lab, Alaska Fisheries Sci Ctr, Seattle, WA 98115 USA.
RP Gardner, CL (reprint author), Alaska Dept Fish & Game, 1300 Coll Rd, Fairbanks, AK 99701 USA.
EM craig.gardner@alaska.gov
OI Ver Hoef, Jay/0000-0003-4302-6895
FU National Park Service; [W-33-3]
FX The National Park Service and Federal Aid in Wildlife Restoration
Project 7.21 under grant W-33-3 provided financial support. We thank B.
Taras, S. Brainerd, L. McCarthy, G. Roloff, and 2 anonymous referees for
their editorial comments to this manuscript. N. Pamperin assisted
constructing the figures. We particularly want to thank M. Webb, P.
Valkenburg, and P. Zaczkowski for many hours of safe flying and
discussions on wolverine movements.
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PU WILDLIFE SOC
PI BETHESDA
PA 5410 GROSVENOR LANE, BETHESDA, MD 20814-2197 USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD NOV
PY 2010
VL 74
IS 8
BP 1894
EP 1903
DI 10.2193/2009-386
PG 10
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 678UN
UT WOS:000284107000031
ER
PT J
AU Montgomery, RA
Roloff, GJ
Hoef, JMV
Millspaugh, JJ
AF Montgomery, Robert A.
Roloff, Gary J.
Hoef, Jay M. Ver
Millspaugh, Joshua J.
TI Can We Accurately Characterize Wildlife Resource Use When Telemetry Data
Are Imprecise?
SO JOURNAL OF WILDLIFE MANAGEMENT
LA English
DT Article
DE Geographic Information Systems (GIS); habitat patches; positional error;
resource use; telemetry
ID ROCKY-MOUNTAIN ELK; HABITAT-SELECTION; GPS TELEMETRY; HOME-RANGE;
RADIOTELEMETRY SYSTEM; TRIANGULATION ERROR; COLLAR PERFORMANCE; WOODLAND
CARIBOU; ANIMAL MOVEMENT; RADIO-LOCATION
AB Telemetry data have been widely used to quantify wildlife habitat relationships despite the fact that these data are inherently imprecise. All telemetry data have positional error, and failure to account for that error can lead to incorrect predictions of wildlife resource use. Several techniques have been used to account for positional error in wildlife studies. These techniques have been described in the literature, but their ability to accurately characterize wildlife resource use has never been tested. We evaluated the performance of techniques commonly used for incorporating telemetry error into studies of wildlife resource use. Our evaluation was based on imprecise telemetry data (mean telemetry error = 174 m, SD = 130 m) typical of field-based studies. We tested 5 techniques in 10 virtual environments and in one real-world environment for categorical (i.e., habitat types) and continuous (i.e., distances or elevations) rasters. Technique accuracy varied by patch size for the categorical rasters, with higher accuracy as patch size increased. At the smallest patch size (1 ha), the technique that ignores error performed best on categorical data (0.31 and 0.30 accuracy for virtual and real data, respectively); however, as patch size increased the bivariate-weighted technique performed better (0.56 accuracy at patch sizes >31 ha) and achieved complete accuracy (i.e., 1.00 accuracy) at smaller patch sizes (472 ha and 1,522 ha for virtual and real data, respectively) than any other technique. We quantified the accuracy of the continuous covariates using the mean absolute difference (MAD) in covariate value between true and estimated locations. We found that average MAD varied between 104 m (ignore telemetry error) and 140 m (rescale the covariate data) for our continuous covariate surfaces across virtual and real data sets. Techniques that rescale continuous covariate data or use a zonal mean on values within a telemetry error polygon were significantly less accurate than other techniques. Although the technique that ignored telemetry error performed best on categorical rasters with smaller average patch sizes (i.e., <= 31 ha) and on continuous rasters in our study, accuracy was so low that the utility of using point-based approaches for quantifying resource use is questionable when telemetry data are imprecise, particularly for small-patch habitat relationships.
C1 [Montgomery, Robert A.; Roloff, Gary J.] Michigan State Univ, Dept Fisheries & Wildlife, E Lansing, MI 48824 USA.
[Hoef, Jay M. Ver] Natl Marine Fisheries Serv, Natl Ocean & Atmospher Adm, Natl Marine Mammal Lab, Alaska Fisheries Sci Ctr, Fairbanks, AK 99775 USA.
[Millspaugh, Joshua J.] Univ Missouri, Dept Fisheries & Wildlife Sci, Columbia, MO 65211 USA.
RP Montgomery, RA (reprint author), Michigan State Univ, Dept Fisheries & Wildlife, 13 Nat Resources Bldg, E Lansing, MI 48824 USA.
EM montg164@msu.edu
OI Ver Hoef, Jay/0000-0003-4302-6895
FU Lyman Briggs College; Department of Fisheries and Wildlife at Michigan
State University; Rocky Mountain Elk Foundation; University of
Washington; South Dakota State University; University of Missouri;
Custer State Park; [W-75-R]
FX We thank Lyman Briggs College and the Department of Fisheries and
Wildlife at Michigan State University for supporting this research.
Thanks are also due to C. Y. Lim for statistical guidance. Funding and
logistical support for collection of the elk data were provided by Rocky
Mountain Elk Foundation, University of Washington, South Dakota State
University, University of Missouri, Custer State Park, and Federal Aid
to Wildlife Restoration Act W-75-R; Study No. 7559 administered through
the South Dakota Department of Game, Fish, and Parks. We thank J.
Baldwin, B. Mueller, D. Welch, C. Willmott, and R. Woods for help with
fieldwork.
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PU WILDLIFE SOC
PI BETHESDA
PA 5410 GROSVENOR LANE, BETHESDA, MD 20814-2197 USA
SN 0022-541X
J9 J WILDLIFE MANAGE
JI J. Wildl. Manage.
PD NOV
PY 2010
VL 74
IS 8
BP 1917
EP 1925
DI 10.2193/2010-019
PG 9
WC Ecology; Zoology
SC Environmental Sciences & Ecology; Zoology
GA 678UN
UT WOS:000284107000034
ER
PT J
AU Moore, SK
Mantua, NJ
Hickey, BM
Trainer, VL
AF Moore, Stephanie K.
Mantua, Nathan J.
Hickey, Barbara M.
Trainer, Vera L.
TI The relative influences of El Nino-Southern Oscillation and Pacific
Decadal Oscillation on paralytic shellfish toxin accumulation in Pacific
northwest shellfish
SO LIMNOLOGY AND OCEANOGRAPHY
LA English
DT Article
ID PUGET-SOUND; ALEXANDRIUM-CATENELLA; TEMPERATURE; VARIABILITY; ANOMALIES;
SELECTION; IMPACTS; SHIFTS; STATE; COAST
AB Historical records of paralytic shellfish toxins (PSTs) in shellfish from a coastal embayment in the Pacific Northwest of the United States are used to examine the influence of large-scale climate variations on aspects of Alexandrium catenella bloom dynamics on interannual and interdecadal timescales. An annual index of shellfish toxicity covaries with the number of days annually that sea surface temperature (SST) exceeds 13 degrees C-a known temperature threshold for increased shellfish toxicity in this region-and with an index of the Pacific Decadal Oscillation (PDO). In contrast, no robust relationship exists between our shellfish toxicity index and an index of the El Nino Southern Oscillation (ENSO). We hypothesize that this is because anomalously warm water temperatures created during El Nino winters do not generally persist into the seasonal time period that shellfish in this region accumulate PSTs, which is typically in the summer and fall. In contrast, anomalously warm water temperatures created during warm-phase PDO winters and springs typically persist into the summer and fall, thereby increasing the number of days annually that SST exceeds 13 degrees C, and increasing the window of opportunity for Alexandrium blooms that ultimately lead to shellfish acquiring higher concentrations of PSTs.
C1 [Moore, Stephanie K.; Trainer, Vera L.] NOAA, NW Fisheries Sci Ctr, W Coast Ctr Oceans & Human Hlth, Seattle, WA USA.
[Mantua, Nathan J.] Univ Washington, Sch Aquat & Fishery Sci, Seattle, WA 98195 USA.
[Mantua, Nathan J.] Univ Washington, Climate Impacts Grp, Seattle, WA 98195 USA.
[Hickey, Barbara M.] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA.
RP Moore, SK (reprint author), NOAA, NW Fisheries Sci Ctr, W Coast Ctr Oceans & Human Hlth, Seattle, WA USA.
EM stephanie.moore@noaa.gov
FU West Coast Center for Oceans and Human Health (WCCOHH); NOAA Oceans and
Human Health Initiative; West Coast Center for Oceans and Human Health
[31]; NOAA Climate Program Office through the Joint Institute for the
Study of the Atmosphere and Ocean under NOAA [NA17RJ1232]
FX Shellfish toxicity data are used courtesy of the Washington State
Department of Health. Sea surface temperature data from Sequim Bay were
collected by N. Adams, B. Bill, and K. Baugh from National Oceanic and
Atmospheric Administration's (NOAA) Northwest Fisheries Science Center.
We thank B. Peterson, F. Cox, J. Borchert, R. Horner, J. Postel, C.
Greengrove, and two anonymous reviewers for providing highly valued
comments. This publication was supported by the West Coast Center for
Oceans and Human Health (WCCOHH) as part of the NOAA Oceans and Human
Health Initiative, West Coast Center for Oceans and Human Health
Publication No. 31. The WCCOHH is part of the National Marine Fisheries
Service's Northwest Fisheries Science Center, Seattle, Washington. This
work was also supported by a grant from the NOAA Climate Program Office
to the Center for Science in the Earth System through the Joint
Institute for the Study of the Atmosphere and Ocean under NOAA
Cooperative Agreement NA17RJ1232. This is Joint Institute for the Study
of the Atmosphere and Ocean Contribution No. 1425.
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PU AMER SOC LIMNOLOGY OCEANOGRAPHY
PI WACO
PA 5400 BOSQUE BLVD, STE 680, WACO, TX 76710-4446 USA
SN 0024-3590
J9 LIMNOL OCEANOGR
JI Limnol. Oceanogr.
PD NOV
PY 2010
VL 55
IS 6
BP 2262
EP 2274
DI 10.4319/lo.2010.55.6.2262
PG 13
WC Limnology; Oceanography
SC Marine & Freshwater Biology; Oceanography
GA 728AE
UT WOS:000287844700003
ER
PT J
AU Jiang, LQ
Cai, WJ
Feely, RA
Wang, YC
Guo, XH
Gledhill, DK
Hu, XP
Arzayus, F
Chen, FZ
Hartmann, J
Zhang, LJ
AF Jiang, Li-Qing
Cai, Wei-Jun
Feely, Richard A.
Wang, Yongchen
Guo, Xianghui
Gledhill, Dwight K.
Hu, Xinping
Arzayus, Felipe
Chen, Feizhou
Hartmann, Justin
Zhang, Longjun
TI Carbonate mineral saturation states along the US East Coast
SO LIMNOLOGY AND OCEANOGRAPHY
LA English
DT Article
ID OCEAN ACIDIFICATION; CONTINENTAL-SHELF; ATMOSPHERIC CO2; DIOXIDE;
SEAWATER; PH; WATERS; DISSOCIATION; CHEMISTRY; CONSTANTS
AB To assess the impact of ocean acidification on the carbonate chemistry of the shelf waters off the southeastern United States (South Atlantic Bight [SAB]), we measured carbonate mineral saturation states from January 2005 to May 2006. The findings reveal that aragonite (Omega(arag): 2.6-4.0) and calcite (Omega(cal): 4.1-6.0) saturation states were considerably higher than those recently reported along the West Coast of North America. Different water mass age between the Atlantic and Pacific Oceans during global ocean circulation is the primary reason for the higher carbonate mineral saturation states in the SAB than along the West Coast. The contrasting water temperatures in the two coasts contribute to such differences. Both upwelling and freshwater discharge also play important roles in controlling saturation state. Carbonate mineral saturation in the surface water of the West Coast is strongly controlled by the upwelling of high-salinity, low-temperature, low-oxygen, and low-pH deep water. In comparison, saturation states in the surface water of the SAB coast are rarely affected by upwelling. Instead, they are strongly influenced by the input of low-saturation-state water from rivers. Continued increases of atmospheric CO2 under the Intergovernmental Panel on Climate Change B1 emission scenario will decrease the carbonate mineral saturation states by up to 40% by the end of this century, and aragonite will approach undersaturation near the coast.
C1 [Jiang, Li-Qing; Cai, Wei-Jun; Wang, Yongchen; Guo, Xianghui; Hu, Xinping; Chen, Feizhou; Hartmann, Justin] Univ Georgia, Dept Marine Sci, Athens, GA 30602 USA.
[Feely, Richard A.] NOAA, Pacific Marine Environm Lab, Seattle, WA 98115 USA.
[Zhang, Longjun] Ocean Univ China, Coll Environm Sci & Engn, Qingdao, Shandong, Peoples R China.
[Arzayus, Felipe] NOAA, Off Ocean Explorat & Res, Silver Spring, MD USA.
[Gledhill, Dwight K.] Univ Miami, Rosenstiel Sch, Cooperat Inst Marine & Atmospher Studies, Miami, FL USA.
[Gledhill, Dwight K.] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
RP Jiang, LQ (reprint author), Yale Univ, Yale Sch Forestry & Environm Studies, New Haven, CT 06520 USA.
EM Liqing.Jiang@yale.edu
RI Hu, Xinping/F-6282-2011; Jiang, Li-Qing/G-5228-2014; Cai,
Wei-Jun/C-1361-2013
OI Hu, Xinping/0000-0002-0613-6545; Jiang, Li-Qing/0000-0003-3311-1658;
Cai, Wei-Jun/0000-0003-3606-8325
FU National Science Foundation (Division of Ocean Science) [OCE-0425153];
National Oceanic & Atmospheric Administration [NA050AR4311161]
FX Support for this work is from a National Science Foundation grant
(Division of Ocean Science: OCE-0425153) and a National Oceanic &
Atmospheric Administration grant (NA050AR4311161) awarded to W.-J.C.
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PU AMER SOC LIMNOLOGY OCEANOGRAPHY
PI WACO
PA 5400 BOSQUE BLVD, STE 680, WACO, TX 76710-4446 USA
SN 0024-3590
EI 1939-5590
J9 LIMNOL OCEANOGR
JI Limnol. Oceanogr.
PD NOV
PY 2010
VL 55
IS 6
BP 2424
EP 2432
DI 10.4319/lo.2010.55.6.2424
PG 9
WC Limnology; Oceanography
SC Marine & Freshwater Biology; Oceanography
GA 728AE
UT WOS:000287844700016
ER
PT J
AU Herndon, A
Gallucci, VF
DeMaster, D
Burke, W
AF Herndon, Andrew
Gallucci, Vincent F.
DeMaster, Douglas
Burke, William
TI The case for an international commission for the conservation and
management of sharks (ICCMS)
SO MARINE POLICY
LA English
DT Article
DE Shark conservation; International fisheries management; IWC; Shark
finning
ID SQUALUS-ACANTHIAS; PRIONACE-GLAUCA; UNITED-STATES; WHITE SHARKS;
ATLANTIC; OCEAN; POPULATION; EXTINCTION; MIGRATION; DOGFISH
AB The current rate of shark global exploitation and mortality is arguably so high under current management regimes that unless a renewed initiative is undertaken some species of shark will become effectively extinct. Current efforts to sustainably manage shark mortality are driven primarily by domestic laws in a few countries, big international non-governmental organizations (BINGOs) promoting environmental laws in the countries or regions where they exist, a handful of regional fisheries management organizations (e.g., IATTC and ICCAT), and inter-governmental organizations such as CITES. The absence of enforcement capability is often argued as the critical component in the failure to protect sharks from overexploitation. The remedy advanced here goes far beyond the need for stepped up enforcement, and calls for the creation of an entirely new international management regime, the International Commission for the Conservation and Management of Sharks (ICCMS). Such an agency could learn from the experiences of management bodies tasked with conservation of species biologically similar to sharks, such as the International Whaling Commission (IWC), to improve its efficacy. Critics have identified many organizational flaws that reduced the IWC's effectiveness during its earliest years. Some of those flaws are examined here and remedies are suggested that an ICCMS could use to create a more effective management regime. The life histories of elasmobranches and large whales are compared to illustrate their similarities as a biological foundation for the selection of the IWC as a model. Published by Elsevier Ltd.
C1 [Herndon, Andrew; Gallucci, Vincent F.; Burke, William] Univ Washington, Seattle, WA 98105 USA.
[DeMaster, Douglas] Alaska Fisheries Sci Ctr, Juneau, AK 99801 USA.
[Herndon, Andrew] Natl Marine Fisheries Serv, SE Reg Off, Protected Species Div, St Petersburg, FL 33701 USA.
RP Herndon, A (reprint author), Univ Washington, 3707 Brooklyn Ave NE, Seattle, WA 98105 USA.
EM Andrew.Herndon@noaa.gov
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PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0308-597X
J9 MAR POLICY
JI Mar. Pol.
PD NOV
PY 2010
VL 34
IS 6
BP 1239
EP 1248
DI 10.1016/j.marpol.2010.05.001
PG 10
WC Environmental Studies; International Relations
SC Environmental Sciences & Ecology; International Relations
GA 641ZY
UT WOS:000281173600015
ER
PT J
AU Jacob, S
Weeks, P
Blount, BG
Jepson, M
AF Jacob, Steve
Weeks, Priscilla
Blount, Benjamin G.
Jepson, Michael
TI Exploring fishing dependence in gulf coast communities
SO MARINE POLICY
LA English
DT Article
DE Fishing dependence; Social indicators; Ethnography; Evaluation
AB Two unrelated data sources (quantitative secondary data and qualitative primary data) and mixed methodologies (statistical analysis and ethnography) are used to define the concept of, and develop indicators for, fishing dependence. Techniques for integrating differing data sources are developed. Comparisons of the qualitative rankings with the quantitative rankings were, overall, positive and statistically significant. The process used thus confirmed that the indicators were reliable measures for fishing dependence. In terms of external validity and triangulation, the process used was more rigorous than using ethnography "after-the-fact" to ground-truth the quantitative indicators. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Weeks, Priscilla] Houston Adv Res Ctr, The Woodlands, TX 77381 USA.
[Jacob, Steve] York Coll Penn, York, PA 17405 USA.
[Blount, Benjamin G.] SocioEcol Informat, Helotes, TX 78023 USA.
[Jepson, Michael] NOAA, Natl Marine Fisheries Serv, SE Reg Off, Social Sci Branch, St Petersburg, FL 33701 USA.
RP Weeks, P (reprint author), Houston Adv Res Ctr, 4800 Res Forest Dr, The Woodlands, TX 77381 USA.
EM sjacob@ycp.edu; pweeks@harc.edu; bblount13239@sbcglobal.net;
michael.jepson@noaa.gov
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U2 9
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0308-597X
J9 MAR POLICY
JI Mar. Pol.
PD NOV
PY 2010
VL 34
IS 6
BP 1307
EP 1314
DI 10.1016/j.marpol.2010.06.003
PG 8
WC Environmental Studies; International Relations
SC Environmental Sciences & Ecology; International Relations
GA 641ZY
UT WOS:000281173600023
ER
PT J
AU Tissot, BN
Best, BA
Borneman, EH
Bruckner, AW
Cooper, CH
D'Agnes, H
Fitzgerald, TP
Leland, A
Lieberman, S
Amos, AM
Sumaila, R
Telecky, TM
McGilvray, F
Plankis, BJ
Rhyne, AL
Roberts, GG
Starkhouse, B
Stevenson, TC
AF Tissot, Brian N.
Best, Barbara A.
Borneman, Eric H.
Bruckner, Andrew W.
Cooper, Cara H.
D'Agnes, Heather
Fitzgerald, Timothy P.
Leland, Amanda
Lieberman, Susan
Amos, Amy Mathews
Sumaila, Rashid
Telecky, Teresa M.
McGilvray, Frazer
Plankis, Brian J.
Rhyne, Andrew L.
Roberts, Glynnis G.
Starkhouse, Benjamin
Stevenson, Todd C.
TI How US ocean policy and market power can reform the coral reef wildlife
trade
SO MARINE POLICY
LA English
DT Article
DE Coral reef; Marine ornamental trade; CITES; Lacey Act; Destructive
fishing; Aquarium
ID LIONFISH PTEROIS-VOLITANS; AQUARIUM TRADE; FISHES; INVASION
AB As the world's largest importer of marine ornamental species for the aquaria, curio, home decor, and jewelry industries, the United States has an opportunity to leverage its considerable market power to promote more sustainable trade and reduce the effects of ornamental trade stress on coral reefs worldwide. Evidence indicates that collection of some coral reef animals for these trades has caused virtual elimination of local populations, major changes in age structure, and promotion of collection practices that destroy reef habitats. Management and enforcement of collection activities in major source countries such as Indonesia and the Philippines remain weak. Strengthening US trade laws and enforcement capabilities combined with increasing consumer and industry demand for responsible conservation can create strong incentives for improving management in source countries. This is particularly important in light of the March 2010 failure of the parties to the Convention on International Trade in Endangered Species (CITES) to take action on key groups of corals. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Tissot, Brian N.; Stevenson, Todd C.] Washington State Univ, Sch Earth & Environm Sci, Vancouver, WA 98686 USA.
[Best, Barbara A.] US Agcy Int Dev, Off Nat Resources, Washington, DC 20523 USA.
[Borneman, Eric H.] Univ Houston, Dept Biol & Biochem, Houston, TX 77004 USA.
[Bruckner, Andrew W.] NOAA, Natl Marine Fisheries Serv, Silver Spring, MD 20910 USA.
[Cooper, Cara H.; Fitzgerald, Timothy P.; Leland, Amanda] Environm Def Fund, Washington, DC 20009 USA.
[D'Agnes, Heather] US Agcy Int Dev, Inst Publ Hlth, Washington, DC 20523 USA.
[Lieberman, Susan] Pew Charitable Trusts, Pew Environm Grp, Washington, DC 20004 USA.
[Amos, Amy Mathews] Turnstone Consulting, Shepherdstown, WV 25443 USA.
[Sumaila, Rashid; Starkhouse, Benjamin] Univ British Columbia, Fisheries Ctr, Aquat Ecosyst Res Lab, Vancouver, BC V6T 1Z4, Canada.
[Telecky, Teresa M.] Humane Soc Int, Washington, DC 20037 USA.
[McGilvray, Frazer] Conservat Int, Arlington, VA 22202 USA.
[Plankis, Brian J.] Reef Stewardship Fdn, Pearland, TX 77584 USA.
[Rhyne, Andrew L.] Roger Williams Univ & New England Aquarium, RWU Dept Biol & Marine Biol, Bristol, RI 02809 USA.
[Roberts, Glynnis G.] IM Syst Grp Inc, Natl Ocean & Atmospher Adm, Coral Reef Conservat Program, Silver Spring, MD 20910 USA.
RP Tissot, BN (reprint author), Washington State Univ, Sch Earth & Environm Sci, 14204 NE Salmon Creek Ave, Vancouver, WA 98686 USA.
EM tissot@vancouver.wsu.edu
OI Rhyne, Andrew/0000-0001-7252-3431
NR 24
TC 24
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U1 7
U2 51
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0308-597X
J9 MAR POLICY
JI Mar. Pol.
PD NOV
PY 2010
VL 34
IS 6
BP 1385
EP 1388
DI 10.1016/j.marpol.2010.06.002
PG 4
WC Environmental Studies; International Relations
SC Environmental Sciences & Ecology; International Relations
GA 641ZY
UT WOS:000281173600033
ER
PT J
AU Willis, Z
Manley, J
AF Willis, Zdenka
Manley, Justin
TI Ocean Observing: Delivering the Benefits INTRODUCTION
SO MARINE TECHNOLOGY SOCIETY JOURNAL
LA English
DT Editorial Material
C1 [Willis, Zdenka] NOAA, Integrated Ocean Observing Syst Program, Silver Spring, MD USA.
RP Willis, Z (reprint author), NOAA, Integrated Ocean Observing Syst Program, Silver Spring, MD USA.
NR 0
TC 0
Z9 0
U1 0
U2 0
PU MARINE TECHNOLOGY SOC INC
PI COLUMBIA
PA 5565 STERRETT PLACE, STE 108, COLUMBIA, MD 21044 USA
SN 0025-3324
J9 MAR TECHNOL SOC J
JI Mar. Technol. Soc. J.
PD NOV-DEC
PY 2010
VL 44
IS 6
BP 4
EP 5
PG 2
WC Engineering, Ocean; Oceanography
SC Engineering; Oceanography
GA 712FG
UT WOS:000286649500001
ER
PT J
AU Lubchenco, J
AF Lubchenco, Jane
TI Ocean Observations: Essential for Good Stewardship
SO MARINE TECHNOLOGY SOCIETY JOURNAL
LA English
DT Editorial Material
C1 NOAA, Silver Spring, MD USA.
RP Lubchenco, J (reprint author), NOAA, Silver Spring, MD USA.
NR 0
TC 5
Z9 5
U1 0
U2 3
PU MARINE TECHNOLOGY SOC INC
PI COLUMBIA
PA 5565 STERRETT PLACE, STE 108, COLUMBIA, MD 21044 USA
SN 0025-3324
J9 MAR TECHNOL SOC J
JI Mar. Technol. Soc. J.
PD NOV-DEC
PY 2010
VL 44
IS 6
BP 6
EP 9
PG 4
WC Engineering, Ocean; Oceanography
SC Engineering; Oceanography
GA 712FG
UT WOS:000286649500002
ER
PT J
AU Bassett, R
Beard, R
Burnett, W
Crout, R
Griffith, B
Jensen, R
Signell, R
AF Bassett, Robert
Beard, Russ
Burnett, William
Crout, Richard
Griffith, Bryon
Jensen, Robert
Signell, Richard
TI Implementing the National Integrated Ocean From the Observing System
(IOOS (R))-Federal Agency Perspective
SO MARINE TECHNOLOGY SOCIETY JOURNAL
LA English
DT Article
AB The national Integrated Ocean Observing System (IOOS (R)) is responsible for coordinating a network of people, resources, and technology to disseminate continuous data, information, models, products, and services made throughout our coastal waters, Great Lakes, and the oceans. There are many components of the IOOS-including government academic, and private entities. This article will focus on some of the federal contributions to IOOS and describe the capabilities of several agency partners.
C1 [Bassett, Robert] NOAA NOS, Ctr Operat Oceanog Prod & Serv, Silver Spring, MD 20910 USA.
[Burnett, William] NOAA NWS, Natl Data Buoy Ctr, Stennis Space Ctr, MS 39529 USA.
[Beard, Russ] NOAA NESDIS, Natl Coastal Data Dev Ctr, Silver Spring, MD USA.
[Crout, Richard] NOAA NDBC, Natl Data Buoy Ctr, Silver Spring, MD USA.
[Signell, Richard] US Geol Survey, Reston, VA USA.
RP Bassett, R (reprint author), NOAA NOS, Ctr Operat Oceanog Prod & Serv, 1305 East West Highway,Bldg SSMC4, Silver Spring, MD 20910 USA.
EM Robert.bassett@noaa.gov; Bill.burnett@noaa.gov
NR 3
TC 1
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U1 0
U2 2
PU MARINE TECHNOLOGY SOC INC
PI COLUMBIA
PA 5565 STERRETT PLACE, STE 108, COLUMBIA, MD 21044 USA
SN 0025-3324
J9 MAR TECHNOL SOC J
JI Mar. Technol. Soc. J.
PD NOV-DEC
PY 2010
VL 44
IS 6
BP 32
EP 41
PG 10
WC Engineering, Ocean; Oceanography
SC Engineering; Oceanography
GA 712FG
UT WOS:000286649500010
ER
PT J
AU de la Beaujardiere, J
Mendelssohn, R
Ortiz, C
Signell, R
AF de la Beaujardiere, Jeff
Mendelssohn, Roy
Ortiz, Carmel
Signell, Richard
TI Building the IOOS (R) Data Management Subsystem
SO MARINE TECHNOLOGY SOCIETY JOURNAL
LA English
DT Article
AB We discuss progress to date and plans for the Integrated Ocean Observing System (IOOS (R)). Data Management and Communications (DMAC) subsystem. We begin by presenting a conceptual architecture of IOOS DMAC. We describe work done as part of a 3-year pilot project known as the Data Integration Framework and the subsequent assessment of lessons learned. We present work that has been accomplished as part of the initial version of the IOOS Data Catalog. Finally, we discuss near-term plans for augmenting IOOS DMAC capabilities.
C1 [de la Beaujardiere, Jeff] NOAA, US IOOS Program Off, Silver Spring, MD 20910 USA.
[Mendelssohn, Roy] NOAA NMFS, Div Environm Res, SW Fisheries Sci Ctr, Silver Spring, MD USA.
[Ortiz, Carmel] Skjei Telecom, US IOOS Program Off, Falls Church, VA USA.
[Signell, Richard] US Geol Survey, Reston, VA USA.
RP de la Beaujardiere, J (reprint author), NOAA, US IOOS Program Off, Silver Spring, MD 20910 USA.
EM jeff.deLaBeaujardiere@noaa.gov
RI de La Beaujardiere, Jeff/D-9579-2012
OI de La Beaujardiere, Jeff/0000-0002-1001-9210
NR 26
TC 1
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U1 0
U2 2
PU MARINE TECHNOLOGY SOC INC
PI COLUMBIA
PA 5565 STERRETT PLACE, STE 108, COLUMBIA, MD 21044 USA
SN 0025-3324
J9 MAR TECHNOL SOC J
JI Mar. Technol. Soc. J.
PD NOV-DEC
PY 2010
VL 44
IS 6
BP 73
EP 83
PG 11
WC Engineering, Ocean; Oceanography
SC Engineering; Oceanography
GA 712FG
UT WOS:000286649500014
ER
PT J
AU Read, J
Klump, V
Johengen, T
Schwab, D
Paige, K
Eddy, S
Anderson, E
Manninen, C
AF Read, Jennifer
Klump, Val
Johengen, Tom
Schwab, David
Paige, Kelli
Eddy, Stuart
Anderson, Eric
Manninen, Christine
TI Working in Freshwater: The Great Lakes Observing System Contributions to
Regional and National Observations, Data Infrastructure, and Decision
Support
SO MARINE TECHNOLOGY SOCIETY JOURNAL
LA English
DT Article
DE Great Lakes; Observation; Decision support; Drinking water; Modeling;
Spill response
ID QUALITY; NETWORK
AB The Laurentian Great Lakes is the world's largest freshwater ecosystem. A charge of the Great Lakes Observing System (GLOS) Regional Association is to help coordinate and integrate data and information relative to the needs of multiple user communities decision makers with responsibility for coastal resources, maritime operations, human health and water security data, and issues associated with adapting to climate change and weather-related hazards. This article outlines the process GLOS has developed for determining regional data and information needs, how GLOS outreach activities inform data management functions and the development of decision support tools, and how the nearshore network of multiple observation platform types was conceived and is being implemented. The article finishes with a case study of this approach as it is being applied to source water protection, spill response, and search and rescue in the St. Clair River, Lake St. Clair, and Detroit River, the connecting channels that link Lake Huron to Lake Erie.
C1 [Klump, Val] Univ Wisconsin Milwaukee, WATER Inst, Milwaukee, WI USA.
[Johengen, Tom; Anderson, Eric] Univ Michigan, Cooperat Inst Limnol & Ecosyst Res, Ann Arbor, MI 48109 USA.
[Schwab, David] NOAA, Great Lakes Environm Res Lab, Silver Spring, MD USA.
EM jread@glos.us
RI Schwab, David/B-7498-2012;
OI Anderson, Eric/0000-0001-5342-8383
NR 33
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U1 1
U2 10
PU MARINE TECHNOLOGY SOC INC
PI COLUMBIA
PA 5565 STERRETT PLACE, STE 108, COLUMBIA, MD 21044 USA
SN 0025-3324
J9 MAR TECHNOL SOC J
JI Mar. Technol. Soc. J.
PD NOV-DEC
PY 2010
VL 44
IS 6
BP 84
EP 98
PG 15
WC Engineering, Ocean; Oceanography
SC Engineering; Oceanography
GA 712FG
UT WOS:000286649500015
ER
PT J
AU Jochens, AE
Malone, TC
Stumpf, RP
Hickey, BM
Carter, M
Morrison, R
Dyble, J
Jones, B
Trainer, VL
AF Jochens, Ann E.
Malone, Thomas C.
Stumpf, Richard P.
Hickey, Barbara M.
Carter, Melissa
Morrison, Ru
Dyble, Juli
Jones, Burt
Trainer, Vera L.
TI Integrated Ocean Observing System in Support of Forecasting Harmful
Algal Blooms
SO MARINE TECHNOLOGY SOCIETY JOURNAL
LA English
DT Article
DE Integrated Ocean Observing System; harmful algal bloom; HAS forecasting;
Karenia brevis; Alexandrium spp.; Dinophysis spp.; Pseudo-nitzschia
spp.; Microcystis spp.; Heterosigma akashiwo
ID ALEXANDRIUM-FUNDYENSE BLOOMS; PHYSICAL-BIOLOGICAL MODEL; FUCA EDDY
REGION; FLORIDA RED TIDE; DOMOIC ACID; LAKE-ERIE; WASHINGTON COAST;
PSEUDO-NITZSCHIA; KARENIA-BREVIS; GREAT-LAKES
AB Harmful algal bloom (HAS) events threaten human health, living marine resources, and ecosystem health. Their occurrence has increased in frequency, duration, and severity over the last several decades. Preventing, controlling, or mitigating the impacts of HABs requires the development of permanent, operational ocean observing systems that continuously provide the data and information necessary for rapid detection and timely forecasts of changes in ecosystem states. Key elements of such observing systems are observations and modeling that must be efficiently linked via data management and communication networks. Building the observing system begins by integrating existing assets, is followed by incorporation of new technologies and knowledge, and is guided by the data and information needs of decision makers. User needs are particularly important for development of operational forecast models and new sensors for measuring required biological (e.g., HAB species abundance) and chemical (e.g., concentrations of HAB toxins) variables in near real time. This article describes operational observing system requirements for a HAB forecasting system and current efforts by Regional Associations to develop these observing systems for targeted species in their respective regions.
C1 [Jochens, Ann E.] Texas A&M Univ, Gulf Mexico Coastal Ocean Observing Syst Reg Asso, College Stn, TX 77843 USA.
[Malone, Thomas C.] Univ Maryland, Horn Point Lab, Ctr Environm Sci, College Pk, MD 20742 USA.
[Stumpf, Richard P.] NOAA, Natl Ocean Serv, Silver Spring, MD USA.
[Hickey, Barbara M.] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA.
[Carter, Melissa] Univ Calif San Diego, Scripps Inst Oceanog, San Diego, CA 92103 USA.
[Dyble, Juli] NOAA, Great Lakes Environm Res Lab, Silver Spring, MD USA.
[Jones, Burt] Univ So Calif, Los Angeles, CA 90089 USA.
[Trainer, Vera L.] NOAA, NW Fisheries Sci Ctr, Silver Spring, MD USA.
RP Jochens, AE (reprint author), Texas A&M Univ, GCOOS Reg Assoc, College Stn, TX 77843 USA.
EM ajochens@tamu.edu
FU National Oceanic and Atmospheric Administration [NA09NOS4780180];
National Science Foundation [OCE0942675]
FX The authors thank the executive directors and regional coordinators of
the 11 IOOS RAs for assisting with identification of information to be
included and, in some cases, for arranging for someone from the region
to provide input. They also thank Don Anderson, Gary Kirkpatrick, Worth
Nowlin, Josie Quintrell, Zdenka Willis, and three anonymous reviewers
for their excellent suggestions and comments that improved the article.
The work of Dr. Hickey was supported by the Coastal Ocean Program of the
National Oceanic and Atmospheric Administration (NA09NOS4780180) and the
National Science Foundation (OCE0942675); this is contribution # 633 and
3 of the ECOHAB and PNWTOX programs, respectively. The contents are
solely the responsibility of the authors and do not necessarily
represent the official views of the supporting agencies.
NR 79
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U1 4
U2 25
PU MARINE TECHNOLOGY SOC INC
PI COLUMBIA
PA 5565 STERRETT PLACE, STE 108, COLUMBIA, MD 21044 USA
SN 0025-3324
EI 1948-1209
J9 MAR TECHNOL SOC J
JI Mar. Technol. Soc. J.
PD NOV-DEC
PY 2010
VL 44
IS 6
BP 99
EP 121
PG 23
WC Engineering, Ocean; Oceanography
SC Engineering; Oceanography
GA 712FG
UT WOS:000286649500016
ER
PT J
AU Harlan, J
Terrill, E
Hazard, L
Keen, C
Barrick, D
Whelan, C
Howden, S
Kohut, J
AF Harlan, Jack
Terrill, Eric
Hazard, Lisa
Keen, Carolyn
Barrick, Donald
Whelan, Chad
Howden, Stephan
Kohut, Josh
TI The Integrated Ocean Observing System High-Frequency Radar Network:
Status and Local, Regional, and National Applications
SO MARINE TECHNOLOGY SOCIETY JOURNAL
LA English
DT Article
ID SURFACE CURRENT MEASUREMENTS; HF RADAR; SEA
AB A national high-frequency radar network has been created over the past 20 years or so that provides hourly 2-D ocean surface current velocity fields in near real time from a few kilometers offshore out to approximately 200 km. This preoperational network is made up of more than 100 radars from 30 different institutions. The Integrated Ocean Observing System efforts have supported the standards-based ingest and delivery of these velocity fields to a number of applications such as coastal search and rescue, oil spill response, water quality monitoring, and safe and efficient 1 marine navigation. Thus, regardless of the operating institution or location of the radar systems, emergency response managers, and other users, can rely on a common source and means of obtaining and using the data. Details of the history, the physics, and the application of high-frequency radar are discussed with successes of the integrated network highlighted.
C1 [Harlan, Jack] NOAA, IOOS Program, Silver Spring, MD USA.
[Terrill, Eric; Hazard, Lisa] Scripps Inst Oceanog, Coastal Observing R&D Ctr, La Jolla, CA USA.
[Keen, Carolyn] Scripps Inst Oceanog, Inst Geophys & Planetary Phys, La Jolla, CA USA.
[Howden, Stephan] Univ So Mississippi, Stennis Space Ctr, Hattiesburg, MS 39406 USA.
[Kohut, Josh] Rutgers State Univ, Piscataway, NJ 08855 USA.
RP Harlan, J (reprint author), NOAA, IOOS Program, Silver Spring, MD USA.
EM jack.harlan@noaa.gov
NR 17
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U1 0
U2 8
PU MARINE TECHNOLOGY SOC INC
PI COLUMBIA
PA 5565 STERRETT PLACE, STE 108, COLUMBIA, MD 21044 USA
SN 0025-3324
J9 MAR TECHNOL SOC J
JI Mar. Technol. Soc. J.
PD NOV-DEC
PY 2010
VL 44
IS 6
BP 122
EP 132
PG 11
WC Engineering, Ocean; Oceanography
SC Engineering; Oceanography
GA 712FG
UT WOS:000286649500017
ER
PT J
AU Gu, DZ
Walter, DK
Randa, J
AF Gu, Dazhen
Walter, David K.
Randa, James
TI NOISE-PARAMETER MEASUREMENTS WITH A REFLECTION TYPE PHASE SHIFTER
SO MICROWAVE AND OPTICAL TECHNOLOGY LETTERS
LA English
DT Article
DE amplifier noise parameters; noise measurement; phase shifter; source
pull technique; uncertainty analysis
AB We report a miniaturized phase shifter operating in the frequency range from 5 to 7 GHz for noise-parameter extraction. Such a tunable solid-state unit represents a significant reduction in the size and mass as a source-pull component, compared to its mechanical counterparts. It provides adequate impedance coverage, ultra-fast response, as well as high repeatability, across the designed region. A packaged low-noise amplifier was measured at integer frequencies by use of the phase shifter on the NIST NFRad system. The measured results exhibited good accuracy. The combined uncertainties (Type-A and Type-B) are below 6% for both the minimum noise temperature and the magnitude of the optimum input reflection coefficient. (C) 2010 Wiley Periodicals, Inc. Microwave Opt Technol Lett 52:2600-2603, 2010; View this article online at wileyonlinelibrary.com. DOI 10.1002/mop.25532
C1 [Gu, Dazhen; Walter, David K.; Randa, James] NIST, Electromagnet Div, Boulder, CO 80305 USA.
[Randa, James] Univ Colorado, Dept Phys, Boulder, CO 80309 USA.
RP Gu, DZ (reprint author), NIST, Electromagnet Div, 325 Broadway, Boulder, CO 80305 USA.
EM dazhen.gu@boulder.nist.gov
RI Gu, Dazhen/B-4854-2012
NR 8
TC 1
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U1 0
U2 0
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0895-2477
EI 1098-2760
J9 MICROW OPT TECHN LET
JI Microw. Opt. Technol. Lett.
PD NOV
PY 2010
VL 52
IS 11
BP 2600
EP 2603
DI 10.1002/mop.25532
PG 4
WC Engineering, Electrical & Electronic; Optics
SC Engineering; Optics
GA 650EH
UT WOS:000281831500056
ER
PT J
AU Salinas, K
Hemmer, MJ
Serrano, J
Higgins, L
Anderson, LB
Benninghoff, AD
Williams, DE
Walker, C
AF Salinas, K.
Hemmer, M. J.
Serrano, J.
Higgins, L.
Anderson, L. B.
Benninghoff, A. D.
Williams, D. E.
Walker, C.
TI Identification of Estrogen-Responsive Vitelline Envelope Protein
Fragments From Rainbow Trout (Oncorhynchus mykiss) Plasma Using Mass
Spectrometry
SO MOLECULAR REPRODUCTION AND DEVELOPMENT
LA English
DT Article
ID MOLECULAR-CLONING; GENE-EXPRESSION; MESSENGER-RNA; EGG; FISH; LIVER;
17-BETA-ESTRADIOL; BIOMARKERS; PROTEOMICS; ORGANISMS
AB Plasma peptides previously associated with exposure of juvenile male rainbow trout (Oncorhynchus rnykiss) to the hormone 17 beta-estradiol (E2) were identified using matrix-assisted laser desorption ionization time of flight mass spectrometry (MALDI-TOF-MS). Specifically, plasma peptides of interest were fractionated and subsequently identified via spectra obtained by MALDI QqTOF MS/MS and LC-MALDI TOFTOF MS/MS analysis, de novo sequencing and database matching. The two peptide masses were identified as significant matches for fragments of the C-terminal propeptides from rainbow trout vitelline envelope protein (VEP)alpha and VEP gamma isoforms. Our findings document the presence of the C-terminal propeptides from rainbow trout VEP alpha and VEP gamma proteins in the bloodstream of juvenile male rainbow trout exposed to E2 via MALDI-TOF-MS detection. We provide three possible explanations for the presence of C-terminal propeptides in the bloodstream, as well as compare previously obtained hepatic transcriptomic results with the plasma proteomic results obtained in the present study.
C1 [Salinas, K.; Hemmer, M. J.] US EPA, Natl Hlth & Environm Effects Res Lab, Gulf Ecol Div, Gulf Breeze, FL USA.
[Serrano, J.] US EPA, Natl Hlth & Environm Effects Res Lab, Midcontinent Ecol Div, Duluth, MN USA.
[Higgins, L.; Anderson, L. B.] Univ Minnesota, Dept Biochem Mol Biol & Biophys, Minneapolis, MN USA.
[Benninghoff, A. D.] Utah State Univ, Grad Program Toxicol, Logan, UT 84322 USA.
[Williams, D. E.] Oregon State Univ, Dept Environm & Mol Toxicol, Corvallis, OR 97331 USA.
[Williams, D. E.] Oregon State Univ, Linus Pauling Inst, Corvallis, OR 97331 USA.
[Walker, C.] Natl Marine Fisheries Serv, NOAA, Natl Seafood Inspect Lab, Pascagoula, MS USA.
RP Salinas, K (reprint author), 1 Sabine Isl Dr, Gulf Breeze, FL 32514 USA.
EM salinas.kimberly@epa.gov
FU Marine and Freshwater Biomedical Sciences Center at Oregon State
University; Environmental Health Sciences Center at Oregon State
University; U. S. Environmental Protection Agency; NIH [ES013534,
ES00210, ES003850]; Gulf Ecology Division Marine and Freshwater
Biomedical Sciences Center at Oregon State University
FX The information in this document has been subjected to review by the U.
S. Environmental Protection Agency National Health and Environmental
Effects Research Laboratory and approved for publication. Approval does
not signify that the contents reflect the views of the Agency, nor does
mention of trade names or commercial products constitute endorsement or
recommendation for use. This is contribution number 1360 from the Gulf
Ecology Division. Dr. Benninghoff and Dr. Williams wish to acknowledge
support of the Marine and Freshwater Biomedical Sciences Center and the
Environmental Health Sciences Center at Oregon State University. The
information in this document has been funded wholly (or in part) by the
U. S. Environmental Protection Agency. Dr. Benninghoff and Dr. Williams
wish to acknowledge financial support from NIH grants ES013534, ES00210,
and ES003850.; Supported by the Gulf Ecology Division Marine and
Freshwater Biomedical Sciences Center, the Environmental Health Sciences
Center at Oregon State University and the NIH (grants ES013534, ES00210,
ES003850).
NR 38
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U1 1
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PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 1040-452X
J9 MOL REPROD DEV
JI Mol. Reprod. Dev.
PD NOV
PY 2010
VL 77
IS 11
BP 963
EP 970
DI 10.1002/mrd.21244
PG 8
WC Biochemistry & Molecular Biology; Cell Biology; Developmental Biology;
Reproductive Biology
SC Biochemistry & Molecular Biology; Cell Biology; Developmental Biology;
Reproductive Biology
GA 692PQ
UT WOS:000285165400005
PM 20939045
ER
PT J
AU Jeglum, ME
Steenburgh, WJ
Lee, TP
Bosart, LF
AF Jeglum, Matthew E.
Steenburgh, W. James
Lee, Tiros P.
Bosart, Lance F.
TI Multi-Reanalysis Climatology of Intermountain Cyclones
SO MONTHLY WEATHER REVIEW
LA English
DT Article
ID SURROUNDING OCEAN ENVIRONS; MOUNTAIN LEE CYCLOGENESIS; WESTERN
UNITED-STATES; SSI ANALYSIS SYSTEM; NORTH-AMERICA; SYNOPTIC CLIMATOLOGY;
BAROCLINIC WAVES; SURFACE-ANALYSES; ANTI-CYCLONES; HEMISPHERE
AB The topography in and around the Intermountain West strongly affects the genesis, migration, and lysis of extratropical cyclones Here intermountain (i e Nevada or Great Basin) cyclone (IC) activity and evolution are examined using the ECMWF Re-Analysis Interim (ERA-Interim) the North American Regional Reanalysis (NARR) and the NCEP-NCAR reanalysis from 1989 to 2008, the period during which all three arc available The Is are defined and tracked objectively as 850-hPa geopotential height depressions of >= 40 m that persist for >= 12 h
The monthly distribution of IC center and genesis frequency in all three reanalyses is bimodal with spring (absolute) and fall (secondary) maxima Although the results arc sensitive to differences in resolution, topographic representation, and reanalysis methodology, both the ERA Interim and NARR produce frequent IC centers and genesis in the Great Basin cyclone region, which extends from the southern "high" Sierra to northwest Utah. and the Canyonlands cyclone region, which lies over the upper Colorado River basin of southeast Utah The NCEP-NCAR reanalysis fails to resolve these two distinct cyclone regions and produces less frequent IC centers and genesis than the ERA-Interim and NARR
An ERA-Interim-based composite of strong ICs generated in cross-Sierra (210 degrees-300 degrees) 500-hPa flow shows that cyclogenesis is preceded by the development of the Great Basin confluence zone (GBCZ), a regional airstream boundary that extends downstream from the Sierra Nevada across the Intermountain West Cyclogenesis occurs along the GBCZ as large-scale ascent develops over the Intermountain West in advance of an approaching upper level trough Flow splitting around the high Sierra and the presence of low-level baroclinicity along the GBCZ suggest that IC evolution may be better conceptualized from a potential vorticity perspective than from traditional quasigeostrophic models of lee cyclogenesis Although these results provide new insights into IC activity and evolution, analysis uncertainty and the cyclone identification criteria are important sources of ambiguity that cannot be fully eliminated
C1 [Jeglum, Matthew E.; Steenburgh, W. James] Univ Utah, Dept Atmospher Sci, Salt Lake City, UT 84112 USA.
[Lee, Tiros P.] NOAA NWS NCEP NCO, Camp Springs, MD USA.
[Bosart, Lance F.] SUNY Albany, Albany, NY USA.
RP Steenburgh, WJ (reprint author), Univ Utah, Dept Atmospher Sci, 135 South,1460 East,Room 819, Salt Lake City, UT 84112 USA.
EM jim.steenburgh@utah.edu
FU National Science Foundation [ATM-0627937]; National Weather Service
FX We thank Court Strong, Larry Dunn, and John Horel for their suggestions
and comments and gratefully acknowledge the provision of datasets,
software, or computer time and services by the ECMWF, NCEP, NCAR,
Unidata Program Center, Center for Ocean Land Atmosphere Studies, and
University of Utah Center for High Performance Computing This research
was supported by National Science Foundation Grant ATM-0627937 and the
National Weather Service C-STAR program Any opinions, findings, and
conclusions or recommendations expressed in this material are those of
the authors and do not necessarily reflect the views of the National
Science Foundation or the National Weather Service
NR 46
TC 11
Z9 11
U1 0
U2 7
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0027-0644
J9 MON WEATHER REV
JI Mon. Weather Rev.
PD NOV
PY 2010
VL 138
IS 11
BP 4035
EP 4053
DI 10.1175/2010MWR3432.1
PG 19
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 690WG
UT WOS:000285039700003
ER
PT J
AU Adhikari, P
Hong, Y
Douglas, KR
Kirschbaum, DB
Gourley, J
Adler, R
Brakenridge, GR
AF Adhikari, Pradeep
Hong, Yang
Douglas, Kimberly R.
Kirschbaum, Dalia Bach
Gourley, Jonathan
Adler, Robert
Brakenridge, G. Robert
TI A digitized global flood inventory (1998-2008): compilation and
preliminary results
SO NATURAL HAZARDS
LA English
DT Article
DE Flood database; Global hazard assessment; Spatiotemporal analysis;
Fatality, impact assessment; Hydrological modeling
AB Floods have profound impacts on populations worldwide in terms of both loss of life and property. A global inventory of floods is an important tool for quantifying the spatial and temporal distribution of floods and for evaluating global flood prediction models. Several global hazard inventories currently exist; however, their utility for spatiotemporal analysis of global floods is limited. The existing flood catalogs either fail to record the geospatial area over which the flood impacted or restrict the types of flood events included in the database according to a set of criteria, limiting the scope of the inventory. To improve upon existing databases, and make it more comprehensive, we have compiled a digitized Global Flood Inventory (GFI) for the period 1998-2008 which also geo-references each flood event by latitude and longitude. This technical report presents the methodology used to compile the GFI and preliminary findings on the spatial and temporal distributions of the flooding events that are contained in the inventory.
C1 [Adhikari, Pradeep; Hong, Yang; Douglas, Kimberly R.] Univ Oklahoma, Sch Civil Engn & Environm Sci, Ctr Nat Hazard & Disaster Res, Norman, OK 73019 USA.
[Kirschbaum, Dalia Bach; Adler, Robert] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
[Gourley, Jonathan] NOAA, Natl Severe Storm Lab, Norman, OK 73072 USA.
[Brakenridge, G. Robert] Dartmouth Coll, Dept Geog, Dartmouth Flood Observ, Hanover, NH 03755 USA.
RP Hong, Y (reprint author), Univ Oklahoma, Sch Civil Engn & Environm Sci, Ctr Nat Hazard & Disaster Res, Natl Weather Ctr Suite 3630, Norman, OK 73019 USA.
EM yanghong@ou.edu
RI Hong, Yang/D-5132-2009; Kirschbaum, Dalia/F-9596-2012; Gourley,
Jonathan/C-7929-2016;
OI Hong, Yang/0000-0001-8720-242X; Gourley, Jonathan/0000-0001-7363-3755;
Adhikari, Pradeep/0000-0003-2218-4376
FU NASA; National Science Foundation
FX This study is supported by NASA Applied Science Global Flood and
Landslide Project, NASA SERVIR-Africa Project, and National Science
Foundation's REU award to School of Civil Engineering and Environmental
Sciences at the University of Oklahoma. The authors would like to extend
their appreciation to many institutions, particularly the EM-DAT and DFO
for sharing the flood hazard data for the current study. Similarly, the
authors would like to thank two anonymous reviewers for thoughtful
comments and suggestion which helped to improve the earlier manuscript.
NR 13
TC 37
Z9 37
U1 0
U2 8
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0921-030X
J9 NAT HAZARDS
JI Nat. Hazards
PD NOV
PY 2010
VL 55
IS 2
BP 405
EP 422
DI 10.1007/s11069-010-9537-2
PG 18
WC Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences;
Water Resources
SC Geology; Meteorology & Atmospheric Sciences; Water Resources
GA 671MJ
UT WOS:000283509900017
ER
PT J
AU Ham, MH
Choi, JH
Boghossian, AA
Jeng, ES
Graff, RA
Heller, DA
Chang, AC
Mattis, A
Bayburt, TH
Grinkova, YV
Zeiger, AS
Van Vliet, KJ
Hobbie, EK
Sligar, SG
Wraight, CA
Strano, MS
AF Ham, Moon-Ho
Choi, Jong Hyun
Boghossian, Ardemis A.
Jeng, Esther S.
Graff, Rachel A.
Heller, Daniel A.
Chang, Alice C.
Mattis, Aidas
Bayburt, Timothy H.
Grinkova, Yelena V.
Zeiger, Adam S.
Van Vliet, Krystyn J.
Hobbie, Erik K.
Sligar, Stephen G.
Wraight, Colin A.
Strano, Michael S.
TI Photoelectrochemical complexes for solar energy conversion that
chemically and autonomously regenerate
SO NATURE CHEMISTRY
LA English
DT Article
ID PHOTOSYNTHETIC REACTION CENTERS; ELECTRON-TRANSFER; CARBON NANOTUBES;
CELLS; BIOSYNTHESIS; SPHAEROIDES; PROTEINS; BINDING; FILMS; GEL
AB Naturally occurring photosynthetic systems use elaborate pathways of self-repair to limit the impact of photo-damage. Here, we demonstrate a complex consisting of two recombinant proteins, phospholipids and a carbon nanotube that mimics this process. The components self-assemble into a configuration in which an array of lipid bilayers aggregate on the surface of the carbon nanotube, creating a platform for the attachment of light-converting proteins. The system can disassemble upon the addition of a surfactant and reassemble upon its removal over an indefinite number of cycles. The assembly is thermodynamically metastable and can only transition reversibly if the rate of surfactant removal exceeds a threshold value. Only in the assembled state do the complexes exhibit photoelectrochemical activity. We demonstrate a regeneration cycle that uses surfactant to switch between assembled and disassembled states, resulting in an increased photoconversion efficiency of more than 300% over 168 hours and an indefinite extension of the system lifetime.
C1 [Ham, Moon-Ho; Boghossian, Ardemis A.; Jeng, Esther S.; Graff, Rachel A.; Heller, Daniel A.; Chang, Alice C.; Strano, Michael S.] MIT, Dept Chem Engn, Cambridge, MA 02139 USA.
[Choi, Jong Hyun] Purdue Univ, Sch Mech Engn, Birck Nanotechnol Ctr, Bindley Biosci Ctr, W Lafayette, IN 47907 USA.
[Mattis, Aidas; Bayburt, Timothy H.; Grinkova, Yelena V.; Sligar, Stephen G.; Wraight, Colin A.] Univ Illinois, Dept Biochem, Urbana, IL 61801 USA.
[Zeiger, Adam S.; Van Vliet, Krystyn J.] MIT, Dept Mat Sci & Engn, Cambridge, MA 02139 USA.
[Hobbie, Erik K.] NIST, Div Polymers, Gaithersburg, MD 20899 USA.
RP Ham, MH (reprint author), MIT, Dept Chem Engn, Cambridge, MA 02139 USA.
EM strano@mit.edu
RI Heller, Daniel/A-4283-2008; Ham, Moon-Ho/K-1305-2012; Hobbie,
Erik/C-8269-2013; Zhou, Charlie/N-5376-2015
OI Heller, Daniel/0000-0002-6866-0000;
FU ENI Petroleum Co. Inc.; MIT Energy Initiative (MITEI); U.S. Department
of Energy [ER46488]; Korean Government (MOEHRD) [KRF-2007-357-D00133];
Purdue University; NIH [GM33775]
FX This work was financially supported by a grant from ENI Petroleum Co.
Inc. Eni S.p.A. under the Eni-MIT Alliance Solar Frontiers Program, seed
funding from the MIT Energy Initiative (MITEI) and the U.S. Department
of Energy (grant no. ER46488). M.H.H. is grateful for support from the
Korea Research Foundation Grant funded by the Korean Government (MOEHRD)
(KRF-2007-357-D00133). J.H.C. acknowledges financial support from Purdue
University. Membrane scaffold proteins were produced and initial PSII
reconstitution experiments were supported by NIH GM33775.
NR 29
TC 72
Z9 74
U1 3
U2 100
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 1755-4330
J9 NAT CHEM
JI Nat. Chem.
PD NOV
PY 2010
VL 2
IS 11
BP 929
EP 936
DI 10.1038/NCHEM.822
PG 8
WC Chemistry, Multidisciplinary
SC Chemistry
GA 669MG
UT WOS:000283354300011
PM 20966948
ER
PT J
AU Di Lorenzo, E
Cobb, KM
Furtado, JC
Schneider, N
Anderson, BT
Bracco, A
Alexander, MA
Vimont, DJ
AF Di Lorenzo, E
Cobb, KM
Furtado, JC
Schneider, N
Anderson, BT
Bracco, A
Alexander, MA
Vimont, DJ
TI Central Pacific El Nino and decadal climate change in the North Pacific
Ocean
SO NATURE GEOSCIENCE
LA English
DT Article
ID VARIABILITY; WINTER; PHYTOPLANKTON; OSCILLATION; TEMPERATURE; ANOMALIES;
PATTERNS; TROPICS; EVENTS; IMPACT
AB Decadal fluctuations of the ocean and atmosphere over the North Pacific Ocean significantly affect the weather and
climate of North America and Eurasia. They also cause transitions between different states of marine ecosystems
across the Pacific Ocean(1-3). An important fraction of North Pacific low-frequency variability is linked to the North Pacific Gyre Oscillation(4), a climate pattern associated with decadal
fluctuations of the ocean circulation. Decadal variations in the North Pacific Gyre Oscillation are characterized by a pattern of sea surface temperature anomalies that resemble the central
Pacific El Nino, a dominant mode of interannual variability with far-reaching effects on global climate patterns(5-7). Here we use an ensemble of simulations with a coupled ocean-atmosphere model to show that the sea surface temperature anomalies associated with central Pacific El Nino force changes in the extra-tropical atmospheric circulation. These changes in turn drive the decadal fluctuations of the North Pacific Gyre Oscillation. Given that central Pacific El Nino events could become more frequent with increasing levels of greenhouse gases in the atmosphere(8), we infer that the North Pacific Gyre Oscillation may play an increasingly important role
in shaping Pacific climate and marine ecosystems in the twenty-first century.
C1 [Di Lorenzo, E; Cobb, KM; Furtado, JC] Georgia Inst Technol, Sch Earth & Atmospher Sci, Atlanta, GA 30332 USA.
[Schneider, N] Univ Hawaii Manoa, Int Pacific Res Ctr, Honolulu, HI 96822 USA.
[Schneider, N] Univ Hawaii Manoa, Dept Oceanog, Honolulu, HI 96822 USA.
[Alexander, MA] NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA.
[Alexander, MA; Vimont, DJ] Univ Wisconsin, Dept Atmospher & Ocean Sci, Madison, WI 53706 USA.
[Anderson, BT] Boston Univ, Dept Geog & Environm, Boston, MA 02215 USA.
RP Di Lorenzo, E (reprint author), Georgia Inst Technol, Sch Earth & Atmospher Sci, 311 Ferst Dr, Atlanta, GA 30332 USA.
EM edl@gatech.edu
RI Alexander, Michael/A-7097-2013; Furtado, Jason/A-3459-2015; Di Lorenzo,
Emanuele/E-9107-2012
OI Alexander, Michael/0000-0001-9646-6427; Furtado,
Jason/0000-0001-6580-2109; Di Lorenzo, Emanuele/0000-0002-1935-7363
NR 29
TC 94
Z9 95
U1 6
U2 67
PU NATURE PUBLISHING GROUP
PI NEW YORK
PA 75 VARICK ST, 9TH FLR, NEW YORK, NY 10013-1917 USA
SN 1752-0894
J9 NAT GEOSCI
JI Nat. Geosci.
PD NOV
PY 2010
VL 3
IS 11
BP 762
EP 765
DI 10.1038/NGEO984
PG 4
WC Geosciences, Multidisciplinary
SC Geology
GA 673GZ
UT WOS:000283648800018
ER
PT J
AU Cundiff, ST
Weiner, AM
AF Cundiff, Steven T.
Weiner, Andrew M.
TI Optical arbitrary waveform generation
SO NATURE PHOTONICS
LA English
DT Article
ID TI-SAPPHIRE LASER; FREQUENCY COMB GENERATOR; MODE-LOCKED LASERS;
REPETITION-RATE; WAVELENGTH DEMULTIPLEXER; SPECTRAL INTERFEROMETRY;
PULSE GENERATION; PHASE-CONTROL; SPECTROSCOPY; DISPERSION
AB Optical arbitrary waveform generation will allow waveforms to be synthesized at optical frequencies but with the flexibility currently available at radiofrequencies. This technique is enabled by combining frequency comb technology, which produces trains of optical pulses with a well-defined frequency spectrum, with pulse shaping methods, which are used to transform a train of ultrashort pulses into an arbitrary waveform. To produce a waveform that fills time, the resolution of the shaper must match the repetition rate of the original pulse train, which in turn must have a comb spectrum that is locked to the shaper. Here, we review the current efforts towards achieving optical arbitrary waveform generation and discuss the possible applications of this technology.
C1 [Cundiff, Steven T.] NIST, JILA, Boulder, CO 80309 USA.
[Cundiff, Steven T.] Univ Colorado, Boulder, CO 80309 USA.
[Weiner, Andrew M.] Purdue Univ, Dept Elect & Comp Engn, W Lafayette, IN 47907 USA.
RP Cundiff, ST (reprint author), NIST, JILA, Boulder, CO 80309 USA.
EM cundiff@jila.colorado.edu
RI Cundiff, Steven/B-4974-2009
OI Cundiff, Steven/0000-0002-7119-5197
FU NIST; Naval Postgraduate School [N00244-09-1-0068]
FX S.T.C. was supported by NIST. A.M.W. was supported in part by the Naval
Postgraduate School under grant N00244-09-1-0068 through the National
Security Science and Engineering Faculty Fellowship programme. Any
opinions, findings, conclusions or recommendations expressed in this
publication are those of the authors and do not necessarily reflect the
views of the sponsors.
NR 61
TC 159
Z9 164
U1 12
U2 61
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 1749-4885
J9 NAT PHOTONICS
JI Nat. Photonics
PD NOV
PY 2010
VL 4
IS 11
BP 760
EP 766
DI 10.1038/NPHOTON.2010.196
PG 7
WC Optics; Physics, Applied
SC Optics; Physics
GA 672MP
UT WOS:000283589200015
ER
PT J
AU Rakher, MT
Ma, LJ
Slattery, O
Tang, XA
Srinivasan, K
AF Rakher, Matthew T.
Ma, Lijun
Slattery, Oliver
Tang, Xiao
Srinivasan, Kartik
TI Quantum transduction of telecommunications-band single photons from a
quantum dot by frequency upconversion
SO NATURE PHOTONICS
LA English
DT Article
ID PERIODICALLY POLED LINBO3; WAVE-GUIDE; INFRARED SPECTROMETER; LINEAR
OPTICS; FIBER TAPER; TELEPORTATION; WAVELENGTHS; GENERATION; QUBITS;
COMMUNICATION
AB Transducing non-classical states of light from one wavelength to another is required for integrating disparate quantum systems that take advantage of telecommunications-band photons for optical-fibre transmission of quantum information and near-visible, stationary systems for manipulation and storage. In addition, transducing a single-photon source at 1.3 mu m to visible wavelengths would be integral to linear optical quantum computation because of near-infrared detection challenges. Recently, transduction at single-photon power levels has been accomplished through frequency upconversion, but it has yet to be demonstrated for a true single-photon source. Here, we transduce triggered single photons from a semiconductor quantum dot at 1.3 mu m to 710 nm with 21% (75%) total detection (internal conversion) efficiency. We demonstrate that the upconverted signal maintains the quantum character of the original light, yielding a second-order intensity correlation, g((2))(tau), that shows that the optical field is composed of single photons with g((2))(0) = 0.165 < 0.5.
C1 [Rakher, Matthew T.; Srinivasan, Kartik] NIST, Ctr Nanoscale Sci & Technol, Gaithersburg, MD 20899 USA.
[Ma, Lijun; Slattery, Oliver; Tang, Xiao] NIST, Informat Technol Lab, Gaithersburg, MD 20899 USA.
RP Srinivasan, K (reprint author), NIST, Ctr Nanoscale Sci & Technol, Gaithersburg, MD 20899 USA.
EM xiao.tang@nist.gov; kartik.srinivasan@nist.gov
RI Srinivasan, Kartik/D-6369-2010; Rakher, Matthew/C-2287-2011
OI Rakher, Matthew/0000-0002-4490-4197
NR 42
TC 122
Z9 125
U1 10
U2 39
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 1749-4885
J9 NAT PHOTONICS
JI Nat. Photonics
PD NOV
PY 2010
VL 4
IS 11
BP 786
EP 791
DI 10.1038/NPHOTON.2010.221
PG 6
WC Optics; Physics, Applied
SC Optics; Physics
GA 672MP
UT WOS:000283589200020
ER
PT J
AU Shoemaker, RC
House, D
Ryan, JC
AF Shoemaker, Ritchie C.
House, Dennis
Ryan, James C.
TI Defining the neurotoxin derived illness chronic ciguatera using markers
of chronic systemic inflammatory disturbances: A case/control study
SO NEUROTOXICOLOGY AND TERATOLOGY
LA English
DT Article
DE Ciguatera fish poisoning; Ciguatoxin; Inflammation; Immune; Biotoxin;
Chronic inflammatory response syndrome
ID MELANOCYTE-STIMULATING HORMONE; COMPLEMENT ACTIVATION; CONTRAST
SENSITIVITY; HLA-DR; EXPRESSION; PEPTIDE; DISEASE; SUSCEPTIBILITY;
NEUROPEPTIDES; INTOXICATION
AB Background: Ciguatoxins are extremely potent neurotoxins, produced by tropical marine dinoflagellates, that persistently enter into our food web. Over 100,000 people annually experience acute ciguatera poisoning from consuming toxic fish. Roughly 5% of these victims will develop chronic ciguatera (CC), a widespread, multisymptom, multisystem, chronic illness that can last tens of years. CC is marked by disproportionate disability and non-specific refractory symptoms such as fatigue, cognitive deficits and pain, and is suggestive of other illnesses. Its unknown pathophysiology makes both diagnosis and treatment difficult.
Objectives: We wanted to compare objective parameters of visual contrast sensitivity testing, measures of innate immune response and genetic markers in cases to controls to assess the potential for the presence of persistent inflammatory parameters that are demonstrated in other biotoxin associated illnesses at a single specialty clinic.
Methods: Using 59 CC cases and 59 controls we present in retrospective review, in all cases, abnormalities in immune responses paralleling the chronic systemic inflammatory response syndrome seen in several other chronic diseases.
Results: This study defines a preliminary case definition using medical history, total symptoms, visual contrast sensitivity, HLA DR genotype analysis, reduction of regulatory neuropeptides VIP and MSH, and multiple measures of inflammatory immune response, especially C4a and TGF beta 1, thereby providing a basis for identification and targeted therapy.
Conclusions: CC provides a model for chronic human illness associated with initiation of inflammatory responses by biologically produced neurotoxins. (C) 2010 Elsevier Inc. All rights reserved.
C1 [Shoemaker, Ritchie C.; House, Dennis] Ctr Res Biotoxin Associated Illnesses, Pocomoke City, MD USA.
[Ryan, James C.] NOAA, Natl Ocean Serv, Marine Biotoxins Program, Charleston, SC USA.
RP Shoemaker, RC (reprint author), 500 Market St, Pocomoke City, MD 21851 USA.
EM ritchieshoemaker@msn.com
OI Ryan, James/0000-0002-1101-3785
FU Center for Research on Biotoxin Associated Illnesses; Center for
Research on Biotoxin Associated Illnesses, Pocomoke, MD [501-c-3]
FX Ritchie C. Shoemaker MD is medical director of the Center for Research
on Biotoxin Associated Illnesses, which is a not-for-profit institution
in the United States. The Center for Research on Biotoxin Associated
Illnesses funded the work carried out in this research paper.; Grant
information: Funding for this study was provided by the Center for
Research on Biotoxin Associated Illnesses, a private, non-profit 501-c-3
organization, Pocomoke, MD 21851.
NR 55
TC 11
Z9 11
U1 1
U2 5
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0892-0362
J9 NEUROTOXICOL TERATOL
JI Neurotoxicol. Teratol.
PD NOV-DEC
PY 2010
VL 32
IS 6
BP 633
EP 639
DI 10.1016/j.ntt.2010.05.007
PG 7
WC Neurosciences; Toxicology
SC Neurosciences & Neurology; Toxicology
GA 692BY
UT WOS:000285127700008
PM 20685390
ER
PT J
AU Guan, ZL
Kim, JB
Wang, H
Jaye, C
Fischer, DA
Loo, YL
Kahn, A
AF Guan, Ze-Lei
Kim, Jong Bok
Wang, He
Jaye, Cherno
Fischer, Daniel A.
Loo, Yueh-Lin
Kahn, Antoine
TI Direct determination of the electronic structure of the
poly(3-hexylthiophene):phenyl-[6,6]-C61 butyric acid methyl ester blend
SO ORGANIC ELECTRONICS
LA English
DT Article
DE Electronic structure; Bulk heterojunction; Blend; P3HT; PCBM; Interface
dipole
ID ENERGY-LEVEL ALIGNMENT; OPEN-CIRCUIT VOLTAGE; PLASTIC SOLAR-CELLS;
ORGANIC INTERFACES; GALLIUM-ARSENIDE; HETEROJUNCTIONS; ORIENTATION;
MORPHOLOGY; EFFICIENCY; DIPOLE
AB This article focuses on the electronic structure of the poly(3-hexylthiophene):phenyl-[6,6]-C61 butyric acid methyl ester (P3HT:PCBM) blend, widely used in bulk heterojunction (BHJ) solar cells. Given the fact that the surface of the blend film is a nearly pure P3HT wetting layer, we use a lift-off method to access the originally buried surface, which is rich in both P3HT and PCBM and thus representative of the BHJ. The combination of direct and inverse photoemission spectroscopy on this surface leads to a determination of the energy gap between the lowest unoccupied molecular orbital (LUMO) of the acceptor and the highest occupied molecular orbital (HOMO) of the donor. The gap is similar to 1.4 eV, which implies a 0.5-0.6 eV interface dipole barrier between the two materials. The energy gap is found to be stable versus in situ annealing up to 100 degrees C. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Guan, Ze-Lei; Wang, He; Kahn, Antoine] Princeton Univ, Dept Elect Engn, Princeton, NJ 08544 USA.
[Kim, Jong Bok; Wang, He; Loo, Yueh-Lin] Princeton Univ, Dept Chem Engn, Princeton, NJ 08544 USA.
[Jaye, Cherno; Fischer, Daniel A.] Natl Inst Stand & Technol, Mat Sci & Engn Lab, Gaithersburg, MD 20899 USA.
RP Guan, ZL (reprint author), Princeton Univ, Dept Elect Engn, Princeton, NJ 08544 USA.
EM zeleig@princeton.edu
RI Loo, Yueh-Lin/C-6607-2011; Guan, Zelei/E-1241-2011; Wang, He/C-3202-2012
FU Department of Energy [DE-FG02-04ER46165]; Office of Science DOE Energy
Frontier Research Center for Interface Science: Solar Electric Materials
[DE-S0001084]; Princeton MRSEC [DMR-0819860]; ONR [N000140811175]
FX Support of this work by the Department of Energy (DE-FG02-04ER46165),
the Office of Science DOE Energy Frontier Research Center for Interface
Science: Solar Electric Materials (DE-S0001084), the Princeton MRSEC
(DMR-0819860) and the Organic Photovoltaic Program at ONR
(N000140811175) is gratefully acknowledged.
NR 32
TC 145
Z9 145
U1 6
U2 85
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1566-1199
J9 ORG ELECTRON
JI Org. Electron.
PD NOV
PY 2010
VL 11
IS 11
BP 1779
EP 1785
DI 10.1016/j.orgel.2010.07.023
PG 7
WC Materials Science, Multidisciplinary; Physics, Applied
SC Materials Science; Physics
GA 656WB
UT WOS:000282370700012
ER
PT J
AU Tribollet, AD
Schils, T
Vroom, PS
AF Tribollet, Aline D.
Schils, Toni
Vroom, Peter S.
TI Spatio-temporal variability in macroalgal assemblages of American Samoa
SO PHYCOLOGIA
LA English
DT Article
DE American Samoa; Coral reefs; Macroalgal abundance; Spatio-temporal
variability
ID NORTHWESTERN HAWAIIAN-ISLANDS; CORAL-REEF COMMUNITIES; FISH ASSEMBLAGES;
PHASE-SHIFTS; ROSE-ATOLL; ALGAE; PATTERNS; ARCHIPELAGO; NITROGEN;
BIODIVERSITY
AB Spatial and temporal variability of relative abundance of macroalgae at the genus and functional group levels was examined at 14 m depth across the six islands of American Samoa between 2004 and 2006. Diversity of common macroalgae was high with 54 taxa (50 genera and four algal functional groups) identified from sampled quadrats. The highest taxon richness (33) was found at the largest island, Tutuila. Crustose coralline algae, mixed turf algal assemblages, and the chlorophyte Halimeda were ubiquitous across all islands. Other algal genera or functional groups were, however, representative of specific areas. For instance, the chlorophyte Microdictyon was only found at Rose Atoll and Swains Island (the only low open-ocean atoll systems examined). Similarly, the siphonous green alga Rhipilia only occurred at Swains Island, where it was very abundant. Multivariate analyses revealed that macroalgal assemblages differed significantly among sites around a single island and among islands. All islands were significantly different from each other with Swains Islands having the most important dissimilarity with other islands. We hypothesize that Swains Island differs from the other islands because of its geographic isolation. Statistical analyses also highlighted significant differences in the relative abundance of macroalgae between years. The interaction between spatial and temporal variability was also significant, indicating that temporal changes in algal assemblages are island dependant, and spatial differences among islands are a function of the year in which surveys were conducted. Changes in algal assemblages between the 2004 and 2006 surveys were apparent for all islands except Swains Island and Tutuila, probably because of intense cyclone activity in the region during 2005 (Cyclone Olaf). This study contributes to the overall understanding of coral reef diversity and function in American Samoa and forms a baseline for future algal monitoring surveys.
C1 [Tribollet, Aline D.; Vroom, Peter S.] NOAA Fisheries, Joint Inst Marine & Atmospher Res, Pacific Isl Fisheries Sci Ctr, Coral Reef Ecosyst Div, Honolulu, HI 96814 USA.
[Schils, Toni] Univ Guam, Marine Lab, Mangilao, GU 96923 USA.
RP Tribollet, AD (reprint author), IRD, BP A5, Noumea 98848, New Caledonia.
EM aline.tribollet@ird.fr
RI Schils, Tom/A-7087-2008
OI Schils, Tom/0000-0002-1516-9082
FU NOAA Fisheries Office of Habitat Conservation
FX We would like to thank Kimberly Page (CRED), Bonnie DeJoseph (CRED), and
Meghan Dailer (UH Botany) for their help in collecting algal field data.
Special thanks to Captains Ken Barton and Scott Kuester and the crews of
the NOAA ships Oscar Elton Sette and Hi'ialakai. Funding to PIFSC-CRED
for scientific expeditions to American Samoa was provided through the
NOAA Fisheries Office of Habitat Conservation, as part of the NOAA Coral
Reef Conservation Program. The observations and collections of algae
carried out in American Samoa complied with the current laws of the
country.
NR 63
TC 4
Z9 4
U1 3
U2 13
PU INT PHYCOLOGICAL SOC
PI LAWRENCE
PA NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA
SN 0031-8884
J9 PHYCOLOGIA
JI Phycologia
PD NOV
PY 2010
VL 49
IS 6
BP 574
EP 591
DI 10.2216/09-63.1
PG 18
WC Plant Sciences; Marine & Freshwater Biology
SC Plant Sciences; Marine & Freshwater Biology
GA 676JN
UT WOS:000283907300006
ER
PT J
AU Pitman, RL
Durban, JW
AF Pitman, Robert L.
Durban, John W.
TI Killer whale predation on penguins in Antarctica
SO POLAR BIOLOGY
LA English
DT Article
DE Antarctic Peninsula; Chinstrap Penguin; Gentoo Penguin; Killer whale;
Orcinus orca; Predation
ID ORCINUS-ORCA; BEHAVIOR; POPULATIONS; ADELIE; ISLAND
AB We report here the first published observations of killer whales (Orcinus orca) feeding on penguins in Antarctica. The sightings took place in the Gerlache Strait off the western Antarctic Peninsula during February 2010. Two species of pygoscelid penguins were taken-gentoo (Pygoscelis papua, at least four individuals) and chinstrap (P. antarctica, 2). From remains left at the surface, it was clear that the killer whales fed mainly on the breast muscles, although some penguins may have been swallowed whole. The killer whales were ecotype B, which are purported seal specialists, but we also saw ecotype A, prey specialists on Antarctic minke whales Balaenoptera bonaerensis, chase, but not catch penguins. Because of their small relative size, if penguins are regularly targeted by killer whales in Antarctica, the impact on their populations could be significant.
C1 [Pitman, Robert L.; Durban, John W.] Natl Ocean & Atmospher Adm, Protected Resources Div, SW Fisheries Sci Ctr, Natl Marine Fisheries Serv, La Jolla, CA 92037 USA.
RP Pitman, RL (reprint author), Natl Ocean & Atmospher Adm, Protected Resources Div, SW Fisheries Sci Ctr, Natl Marine Fisheries Serv, 8604 La Jolla Shores Dr, La Jolla, CA 92037 USA.
EM robert.pitman@noaa.gov
FU US National Oceanographic and Atmospheric Administration (NOAA)
Fisheries; British Broadcasting Corporation (BBC) Natural History Film
Unit
FX This work was supported by US National Oceanographic and Atmospheric
Administration (NOAA) Fisheries and the British Broadcasting Corporation
(BBC) Natural History Film Unit. We would like to thank Jerome and Dion
Poncet of the Golden Fleece for their capable boat handling, and a
special thanks to the BBC Frozen Planet film crew-E. White, D. Anderson
and T. Fitz-for their enthusiastic support and assistance with our
research efforts. D. Ainley improved our manuscript with his comments.
NR 27
TC 25
Z9 25
U1 5
U2 33
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0722-4060
J9 POLAR BIOL
JI Polar Biol.
PD NOV
PY 2010
VL 33
IS 11
BP 1589
EP 1594
DI 10.1007/s00300-010-0853-5
PG 6
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 684JH
UT WOS:000284545700012
ER
PT J
AU Lewin, M
Zhang, J
Pearce, E
Zammarano, M
AF Lewin, Menachem
Zhang, Jin
Pearce, Eli
Zammarano, Mauro
TI Polyamide 6 treated with pentabromobenzyl acrylate and layered silicates
SO POLYMERS FOR ADVANCED TECHNOLOGIES
LA English
DT Article
DE polyamide; clay; flame retardancy; migration; pentabromobenzyl acrylate
ID FIBER-REINFORCED POLYPROPYLENE; FLAME RETARDANCY; STRUCTURAL-CHANGES;
NANOCOMPOSITES; MIGRATION; POLYMERS; SURFACE; BLENDS; MORPHOLOGY; SYSTEM
AB A study of the simultaneous application of a brominated flame retardant and an organically layered silicate (OLS) for the flame retarding of polyamide 6 (PA6) is presented. Upon treating PA6 with at least 7 wt% monomeric pentabromobenzyl acrylate (PMA), a UL-94 V-0 rating and an oxygen index (OI) value of 29.7 were obtained. By adding 1 wt% organically layered montorillonite (OMMT) and 10 wt% PMA, the V-0 rating remained, indicating cooperation between PMA and OMMT. Higher concentrations of OMMT result in a decreased UL-94 rating showing an antagonism. The size and mass of drops formed in the UL-94 test increased with increasing OMMT, suggesting an increase in the viscosity and density of the pyrolyzing matrix. The effect of the Br additive on the peak heat release rate (PHRR) measured in the cone calorimeter is similar, but smaller, than that of clay. A calculation of the synergistic effectivity related to PHRR enabling a numerical estimate of the extent of synergism or antagonism is presented. When the ill-dispersed pristine clay (Na(+)MMT) is used, the viscosity does not increase, the PHRR decreases slightly, but the mass loss rate (MLR) is close to that of the matrix. The time of ignition (TOI) decreases upon the addition of PMA, similarly to the addition of OMMT. This is explained by migration of the Br additive to the surface barrier similar to that of clay so that the low thermal conductivity (TC) barrier is formed before the ignition. Accumulation of heat in the barrier decreases the TOI. Copyright (C) 2010 John Wiley & Sons, Ltd.
C1 [Lewin, Menachem; Zhang, Jin; Pearce, Eli] NYU, Polytech Inst, MetroTech Ctr 6, Brooklyn, NY 11201 USA.
[Zammarano, Mauro] NIST, Bldg & Fire Res Lab, Gaithersburg, MD 20899 USA.
RP Lewin, M (reprint author), NYU, Polytech Inst, MetroTech Ctr 6, Brooklyn, NY 11201 USA.
EM mlewin@duke.poly.edu
OI Zammarano, Mauro/0000-0002-5145-7110
FU NSF [DMR 0352558]; National Institute of Standards and Technology [NIST
4H1129]
FX Contract/grant sponsor: NSF; contract/grant number: DMR 0352558.;
Contract/grant sponsor: National Institute of Standards and Technology;
contract/grant number: NIST 4H1129.
NR 34
TC 14
Z9 14
U1 2
U2 27
PU JOHN WILEY & SONS LTD
PI CHICHESTER
PA THE ATRIUM, SOUTHERN GATE, CHICHESTER PO19 8SQ, W SUSSEX, ENGLAND
SN 1042-7147
J9 POLYM ADVAN TECHNOL
JI Polym. Adv. Technol.
PD NOV
PY 2010
VL 21
IS 11
BP 825
EP 834
DI 10.1002/pat.1719
PG 10
WC Polymer Science
SC Polymer Science
GA 677WF
UT WOS:000284024000011
ER
PT J
AU Neta, P
Godugu, B
Liang, YX
Simon-Manso, Y
Yang, XY
Stein, SE
AF Neta, Pedatsur
Godugu, Bhaskar
Liang, Yuxue
Simon-Manso, Yamil
Yang, Xiaoyu
Stein, Stephen E.
TI Electrospray tandem quadrupole fragmentation of quinolone drugs and
related ions. On the reversibility of water loss from protonated
molecules
SO RAPID COMMUNICATIONS IN MASS SPECTROMETRY
LA English
DT Article
ID MULTIPLE LINEAR-REGRESSION; IONIZATION-CONSTANTS; MOBILITY CONSTANTS;
AQUEOUS-SOLUTION; GAS; COMPLEXATION; SPECTROMETRY; ANTIBIOTICS;
EQUILIBRIA; PREDICTION
AB Selected reaction monitoring (SRM) of quinolone drugs showed different sensitivities in aqueous solution vs. biological extract. The authors suggested formation of two singly protonated molecules with different behavior, one undergoing loss of H(2)O and the other loss of CO(2), so that SRM transitions might depend on the ratios of these forms generated by the electrospray. These surprising results prompted us to re-examine several quinolone drugs and some simpler compounds to further elucidate the mechanisms. We find that the relative contributions of loss of H(2)O vs. loss of CO(2) in tandem mass spectrometric (MS/MS) experiments depend not only on molecular structure and collision energy, but also, in certain cases, on the cone voltage. We further find that many product ions formed by loss of H(2)O can reattach a water molecule in the collision cell, whereas ions formed by loss of CO(2) do not. Since reattachment of H(2)O can occur after water loss in the cone region and prior to selection of the precursor ion, this effect leads to the dependence of MS/MS spectra on the cone voltage used in creating the precursor ion, which explains the formerly observed effect on SRM ratios. Our results support the earlier conclusion that varying amounts of two ions of the same m/z value are responsible for problems in the analysis of these drugs, but the origin is in dehydration/rehydration reactions. Thus, SRM transitions for certain complex compounds may be comparable only when monitored under equivalent ion-forming conditions, including the voltage used in the production of the protonated molecules in the electrospray ionization (ESI) source. Published in 2010 by John Wiley & Sons, Ltd.
C1 [Neta, Pedatsur; Godugu, Bhaskar; Liang, Yuxue; Simon-Manso, Yamil; Yang, Xiaoyu; Stein, Stephen E.] NIST, Chem & Biochem Reference Data Div, Gaithersburg, MD 20899 USA.
RP Neta, P (reprint author), NIST, Chem & Biochem Reference Data Div, Gaithersburg, MD 20899 USA.
EM pedi@nist.gov
NR 19
TC 14
Z9 14
U1 2
U2 11
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0951-4198
J9 RAPID COMMUN MASS SP
JI Rapid Commun. Mass Spectrom.
PD NOV
PY 2010
VL 24
IS 22
BP 3271
EP 3278
DI 10.1002/rcm.4769
PG 8
WC Biochemical Research Methods; Chemistry, Analytical; Spectroscopy
SC Biochemistry & Molecular Biology; Chemistry; Spectroscopy
GA 677VZ
UT WOS:000284023400007
PM 20973001
ER
PT J
AU Xiong, XZ
Barnet, C
Maddy, E
Wei, J
Liu, XP
Pagano, TS
AF Xiong, Xiaozhen
Barnet, Chris
Maddy, Eric
Wei, Jennifer
Liu, Xingpin
Pagano, Thomas S.
TI Seven Years' Observation of Mid-Upper Tropospheric Methane from
Atmospheric Infrared Sounder
SO REMOTE SENSING
LA English
DT Article
DE methane; mid-upper troposphere; satellite; AIRS; trend; seasonal cycle
ID GROWTH-RATE; RETRIEVALS; TRANSPORT; PLUME; MODEL
AB The Atmospheric Infrared Sounder (AIRS) on EOS/Aqua platform provides a measurement of global methane (CH4) in the mid-upper troposphere since September, 2002. As a thermal infrared sounder, the most sensitivity of AIRS to atmospheric CH4 is in the mid-upper troposphere with the degree of freedom of similar to 1.0. Validation of AIRS CH4 product versus thousands of aircraft profiles (convolved using the AIRS averaging kernels) demonstrates that its RMS error (RMSE) is mostly less than 1.5%, and its quality is pretty stable from 2003 to 2009. For scientific analysis of the spatial and temporal variation of mid-upper tropospheric CH4 (MUT-CH4) in the High Northern Hemisphere (HNH), it is more valuable to use the AIRS retrieved CH4 in a layer of about 100 hPa below tropopause ("Representative Layer") than in a fixed pressure layer. Further analysis of deseasonalized time-series of AIRS CH4 in both a fixed pressure layer and the "Representative Layer" of AIRS (only for the HNH) from 2003 to 2009 indicates that, similar to the CH4 in the marine boundary layer (MBL) that was found to increase in 2007-2008, MUT-CH4 was also observed to have a recent increase but the most significant increase occurred in 2008. MUT-CH4 continued to increase in 2009, especially in the HNH. Moreover, the trend of MUT-CH4 from 2006 to 2008 is lower than the trend of CH4 in the MBL by 30-40% in both the southern hemisphere and HNH. This delay for the MUT-CH4 increase of about one year than CH4 in the MBL as well as the smaller increase trend for MUT-CH4 suggest that surface emission is likely a major driver for the recent CH4 increase. It is also found that the seasonal cycle of MUT-CH4 is different from CH4 in the MBL due to the impact of transport, in addition to the surface emission and the photochemical loss.
C1 [Xiong, Xiaozhen; Maddy, Eric; Wei, Jennifer; Liu, Xingpin] Dell Perot Syst Govt Serv, Fairfax, VA 22031 USA.
[Xiong, Xiaozhen; Barnet, Chris; Maddy, Eric; Wei, Jennifer; Liu, Xingpin] NOAA, Ctr Satellite Applicat & Res STAR, Natl Environm Satellite Data & Informat Serv NESD, Camp Springs, MD 20746 USA.
[Pagano, Thomas S.] NASA, Jet Prop Lab, Pasadena, CA USA.
RP Xiong, XZ (reprint author), Dell Perot Syst Govt Serv, Fairfax, VA 22031 USA.
EM Xiaozhen.xiong@noaa.gov; Chris.barnet@noaa.gov; Eric.maddy@noaa.gov;
Jennifer.wei@noaa.gov; Xingpin.liu@noaa.gov;
Thomas.s.pagano@jpl.nasa.gov
RI Maddy, Eric/G-3683-2010; Xiong, Xiaozhen/F-6591-2010
OI Maddy, Eric/0000-0003-1151-339X;
FU NOAA Office of Application Research
FX This research was supported by funding from NOAA Office of Application &
Research. The views, opinions, and findings contained in this paper are
those of the authors and should not be construed as an official National
Oceanic and Atmospheric Administration or U.S. Government position,
policy, or decision. The data of INTEX-A and B used in this publication
was obtained from Aura Validation Data Center (AVDC)
(http://avdc.gsfc.nasa.gov/index.php) and the aircraft measurements of
INTEX-NA were carried out by Donald R. Blake of Department of Chemistry,
University of California, Irvine; and airborne CH4 data from
INTEX-B and ARCTAS were provided by Glen Sachse and Glenn Diskin of NASA
Langley. ARCTAS data were downloaded from
(ftp://ftp-air.larc.nasa.gov/pub/ARCTAS/). The CH4 data of
START08 aircraft measurements were carried out by Dale Hurst and Jim
Elkins of NOAA/ESRL/GMD. We appreciate Colm Sweeney at NOAA/ESRL/GMD for
providing the aircraft measurements data.
NR 32
TC 19
Z9 23
U1 0
U2 12
PU MDPI AG
PI BASEL
PA ST ALBAN-ANLAGE 66, CH-4052 BASEL, SWITZERLAND
SN 2072-4292
J9 REMOTE SENS-BASEL
JI Remote Sens.
PD NOV
PY 2010
VL 2
IS 11
BP 2509
EP 2530
DI 10.3390/rs2112509
PG 22
WC Remote Sensing
SC Remote Sensing
GA V24HS
UT WOS:000208402100003
ER
PT J
AU Fullerton, AH
Steel, EA
Lange, I
Caras, Y
AF Fullerton, Aimee H.
Steel, E. Ashley
Lange, Ian
Caras, Yuko
TI Effects of Spatial Pattern and Economic Uncertainties on Freshwater
Habitat Restoration Planning: A Simulation Exercise
SO RESTORATION ECOLOGY
LA English
DT Article
DE decision analysis; land management; land use; landscape ecology; Pacific
salmon; watershed
ID RIVER-BASIN; POPULATION VIABILITY; SENSITIVITY ANALYSIS; ALTERNATIVE
FUTURES; CONSERVATION STATUS; UNITED-STATES; MODELS; SALMON; VALUATION;
RECOVERY
AB Evaluating alternative future scenarios using simulation models is an emerging approach to conservation planning over large spatial and temporal extents. Such an approach is useful when predictions cannot be validated empirically; however, evaluating the sensitivity of scenario-based approaches to key uncertainties is necessary so that managers understand how real-world constraints might impact results. We used a simulation approach to investigate the sensitivity of freshwater habitat restoration plans to spatial pattern (e.g., project locations) and economic uncertainties (e.g., budget level and project costs) in a case study on Pacific salmon in the Lewis River Basin (WA, U.S.A.). We found that some evaluation metrics performed better when restoration was distributed randomly, whereas others improved more when restoration occurred on contiguous stretches of river. Subwatersheds responded differently to restoration, suggesting that intrinsic characteristics limit restoration potential. Changes in budget usually caused proportionate improvements in habitat but disproportionate fish responses, suggesting a cumulative benefit for fish. Most per-dollar benefits increased as project cost decreased; therefore, model predictions are sensitive to project cost. Simulation analyses provided increased information about how economics and spatial pattern might affect habitats and salmon; these insights can help policymakers identify an appropriate restoration strategy.
C1 [Fullerton, Aimee H.; Steel, E. Ashley] NOAA Fisheries, NW Fisheries Sci Ctr, Seattle, WA 98112 USA.
[Lange, Ian] Univ Stirling, Dept Econ, Stirling FK9 4LA, Scotland.
[Caras, Yuko] King Cty Dept Nat Resources & Pk, Seattle, WA 98104 USA.
RP Fullerton, AH (reprint author), NOAA Fisheries, NW Fisheries Sci Ctr, 2725 Montlake Blvd E, Seattle, WA 98112 USA.
EM Aimee.Fullerton@noaa.gov
FU NOAA Fisheries Service; Northwest Fisheries Science Center
FX We thank J. Davies, M. Plummer, and P. Roni for comments on earlier
versions of this article. Funding was provided by NOAA Fisheries
Service, and by an internal grant from the Northwest Fisheries Science
Center to AHF.
NR 49
TC 2
Z9 2
U1 2
U2 6
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 1061-2971
J9 RESTOR ECOL
JI Restor. Ecol.
PD NOV
PY 2010
VL 18
SU 2
BP 354
EP 369
DI 10.1111/j.1526-100X.2009.00620.x
PG 16
WC Ecology
SC Environmental Sciences & Ecology
GA 679OX
UT WOS:000284171800013
ER
PT J
AU Williams, DE
Miller, MW
AF Williams, Dana E.
Miller, Margaret W.
TI Stabilization of Fragments to Enhance Asexual Recruitment in Acropora
Palmata, a Threatened Caribbean Coral
SO RESTORATION ECOLOGY
LA English
DT Article
DE acroporid; Biscayne National Park; Florida; restoration; reef
ID REEF REHABILITATION; GROWTH; TRANSPLANTATION; SURVIVAL; REGENERATION;
SURVIVORSHIP; REPRODUCTION; RESTORATION
AB Historically, fragmentation has been a successful life history strategy in Acropora palmata. However, in areas where the population is sparse and degraded, the survivorship of fragments is now compromised. This study aimed to determine whether stabilization of A. palmata fragments could increase their overall performance. Naturally occurring fragments were found and assigned to one of three treatments: stabilized to the natural substrate (1) using cable ties, (2) using epoxy or (3) tethered to the substrate as an unstabilized control. After 44 weeks, the general "performance" of the fragments was ranked based on their change in live tissue cover and formation of tissue connections with the substrate. Stabilized fragments lost less tissue cover and ranked higher in performance than the unstabilized control fragments. Stabilization using cable ties and epoxy were similarly effective. The results indicate that stabilizing fragments will preserve live tissue and enhance growth of fragments and can thus improve the survivorship of fragments.
C1 [Williams, Dana E.] Univ Miami, Cooperat Inst Marine & Atmospher Studies, RSMAS, Miami, FL 33149 USA.
[Williams, Dana E.; Miller, Margaret W.] NOAA Fisheries, SEFSC, Miami, FL 33149 USA.
RP Williams, DE (reprint author), Univ Miami, Cooperat Inst Marine & Atmospher Studies, RSMAS, 4600 Rickenbacker Causeway, Miami, FL 33149 USA.
EM dana.williams@noaa.gov
OI Williams, Dana/0000-0002-9660-5359
FU Biscayne National Park; NOAA
FX This study was supported by Biscayne National Park and the NOAA Coral
Reef Conservation Program and conducted with express permission from
park managers. Field assistance was provided by Lindsey Kramer, Rebecca
Cassotis, and Chris Tilghman. Consultation by Amanda Bourque is greatly
appreciated.
NR 38
TC 14
Z9 14
U1 1
U2 23
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 1061-2971
J9 RESTOR ECOL
JI Restor. Ecol.
PD NOV
PY 2010
VL 18
SU 2
BP 446
EP 451
DI 10.1111/j.1526-100X.2009.00579.x
PG 6
WC Ecology
SC Environmental Sciences & Ecology
GA 679OX
UT WOS:000284171800022
ER
PT J
AU Huber, HP
Moertelmaier, M
Wallis, TM
Chiang, CJ
Hochleitner, M
Imtiaz, A
Oh, YJ
Schilcher, K
Dieudonne, M
Smoliner, J
Hinterdorfer, P
Rosner, SJ
Tanbakuchi, H
Kabos, P
Kienberger, F
AF Huber, H. P.
Moertelmaier, M.
Wallis, T. M.
Chiang, C. J.
Hochleitner, M.
Imtiaz, A.
Oh, Y. J.
Schilcher, K.
Dieudonne, M.
Smoliner, J.
Hinterdorfer, P.
Rosner, S. J.
Tanbakuchi, H.
Kabos, P.
Kienberger, F.
TI Calibrated nanoscale capacitance measurements using a scanning microwave
microscope
SO REVIEW OF SCIENTIFIC INSTRUMENTS
LA English
DT Article
ID NEAR-FIELD MICROSCOPY; SILICON; PROBE
AB A scanning microwave microscope (SMM) for spatially resolved capacitance measurements in the attofarad-to-femtofarad regime is presented. The system is based on the combination of an atomic force microscope (AFM) and a performance network analyzer (PNA). For the determination of absolute capacitance values from PNA reflection amplitudes, a calibration sample of conductive gold pads of various sizes on a SiO(2) staircase structure was used. The thickness of the dielectric SiO(2) staircase ranged from 10 to 200 nm. The quantitative capacitance values determined from the PNA reflection amplitude were compared to control measurements using an external capacitance bridge. Depending on the area of the gold top electrode and the SiO(2) step height, the corresponding capacitance values, as measured with the SMM, ranged from 0.1 to 22 fF at a noise level of similar to 2 aF and a relative accuracy of 20%. The sample capacitance could be modeled to a good degree as idealized parallel plates with the SiO(2) dielectric sandwiched in between. The cantilever/sample stray capacitance was measured by lifting the tip away from the surface. By bringing the AFM tip into direct contact with the SiO(2) staircase structure, the electrical footprint of the tip was determined, resulting in an effective tip radius of similar to 60 nm and a tip-sample capacitance of similar to 20 aF at the smallest dielectric thickness. (C) 2010 American Institute of Physics. [doi:10.1063/1.3491926]
C1 [Moertelmaier, M.; Dieudonne, M.; Rosner, S. J.; Tanbakuchi, H.; Kienberger, F.] Agilent Technol, Santa Clara, CA 95051 USA.
[Huber, H. P.; Hochleitner, M.; Oh, Y. J.; Hinterdorfer, P.] Univ Linz, Christian Doppler Lab Nanoscop Methods Biophys, A-4040 Linz, Austria.
[Wallis, T. M.; Chiang, C. J.; Imtiaz, A.; Kabos, P.] Natl Inst Stand & Technol, Electromagnet Div, Boulder, CO 80305 USA.
[Chiang, C. J.] Natl Changhua Univ Educ, Dept Elect Engn, Changhua 500, Taiwan.
[Schilcher, K.] Upper Austria Univ Appl Sci, A-4020 Linz, Austria.
[Smoliner, J.] Vienna Univ Technol, Inst Solid State Elect, A-1040 Vienna, Austria.
RP Kienberger, F (reprint author), Agilent Technol Osterreich GmbH, Aubrunnerweg 11, A-4040 Linz, Austria.
EM ferry_kienberger@agilent.com
RI Hinterdorfer, Peter/C-4235-2013; OH, YOO JIN/M-7109-2014;
OI Oh, Yoo Jin/0000-0002-9636-3329
FU Austrian Christian Doppler Society
FX We thank Gerald Kada, Matthias Fenner, Dirk Orgassa, and Shijie Wu from
Agilent Technologies and Fritz Mayr from the Upper Austria University of
Applied Sciences for helpful technical discussions. This work was
financially supported by the Austrian Christian Doppler Society.
NR 24
TC 59
Z9 60
U1 5
U2 38
PU AMER INST PHYSICS
PI MELVILLE
PA CIRCULATION & FULFILLMENT DIV, 2 HUNTINGTON QUADRANGLE, STE 1 N O 1,
MELVILLE, NY 11747-4501 USA
SN 0034-6748
J9 REV SCI INSTRUM
JI Rev. Sci. Instrum.
PD NOV
PY 2010
VL 81
IS 11
AR 113701
DI 10.1063/1.3491926
PG 9
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA 690LO
UT WOS:000285006500019
PM 21133472
ER
PT J
AU Park, GH
Wanninkhof, R
Doney, SC
Takahashi, T
Lee, K
Feely, RA
Sabine, CL
Trinanes, J
Lima, ID
AF Park, Geun-Ha
Wanninkhof, Rik
Doney, Scott C.
Takahashi, Taro
Lee, Kitack
Feely, Richard A.
Sabine, Christopher L.
Trinanes, Joaquin
Lima, Ivan D.
TI Variability of global net sea-air CO2 fluxes over the last three decades
using empirical relationships
SO TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY
LA English
DT Article
ID ATMOSPHERIC CARBON-DIOXIDE; INTERANNUAL VARIABILITY; SUBTROPICAL GYRE;
GAS-EXCHANGE; OCEAN; SINK; CLIMATE; PACIFIC; TRENDS; PCO(2)
AB The interannual variability of net sea-air CO2 flux for the period 1982-2007 is obtained from a diagnostic model using empirical subannual relationships between climatological CO2 partial pressure in surface seawater (pCO(2SW)) and sea surface temperature (SST), along with interannual changes in SST and wind speed. These optimum subannual relationships show significantly better correlation between pCO(2SW) and SST than the previous relationships using fixed monthly boundaries. Our diagnostic model yields an interannual variability of +/- 0.14 PgC yr-1 (1 Sigma) with a 26-year mean of -1.48 PgC yr-1. The greatest interannual variability is found in the Equatorial Pacific, and significant variability is also found at northern and southern high-latitudes, depending in part, on which wind product is used. We provide an assessment of our approach by applying it to pCO(2SW) and SST output from a prognostic global biogeochemical ocean model. Our diagnostic approach applied to this model output shows reasonable agreement with the prognostic model net sea-air CO2 fluxes in terms of magnitude and phase of variability, suggesting that our diagnostic approach can capture much of the observed variability on regional to global scale. A notable exception is that our approach shows significantly less variability than the prognostic model in the Southern Ocean.
C1 [Park, Geun-Ha] Univ Miami, Cooperat Inst Marine & Atmospher Studies, Miami, FL 33149 USA.
[Park, Geun-Ha; Wanninkhof, Rik] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
[Doney, Scott C.; Lima, Ivan D.] Woods Hole Oceanog Inst, Marine Chem & Geochem Dept, Woods Hole, MA 02543 USA.
[Takahashi, Taro] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA.
[Lee, Kitack] Pohang Univ Sci & Technol, Sch Environm Sci & Engn, Pohang 790784, South Korea.
[Feely, Richard A.; Sabine, Christopher L.] NOAA, Pacific Marine Environm Lab, Seattle, WA 98115 USA.
[Trinanes, Joaquin] Univ Santiago de Compostela, Technol Res Inst, Santiago De Compostela 15782, Spain.
RP Park, GH (reprint author), Univ Miami, Cooperat Inst Marine & Atmospher Studies, Miami, FL 33149 USA.
EM Geun-Ha.Park@noaa.gov
RI Park, Geun-Ha/A-5705-2011; Doney, Scott/F-9247-2010; Lee,
Kitack/G-7184-2015; Lima, Ivan/A-6823-2016
OI Doney, Scott/0000-0002-3683-2437; Lima, Ivan/0000-0001-5345-0652
FU Korean Government [KRF-2008-357-C00167]; NOAA [GC07-193,
NA07OAR4310098]; NOAA Climate Observations Division
FX This work was supported by the Korea Research Foundation Grant funded by
the Korean Government (KRF-2008-357-C00167), the NOAA Global Carbon
Cycle Program (GC07-193 and NA07OAR4310098) and the NOAA Climate
Observations Division. This research was carried out, in part, under the
auspices of the Cooperative Institute for Marine and Atmospheric Studies
(CIMAS), a Joint Institute of the University of Miami and the National
Oceanic and Atmospheric Administration (cooperative agreement No.
NA17RJ1226). We are grateful to Nick Bates, John Dore and other
scientists at the BATS and HOT sites for contributing their time-series
data.
NR 58
TC 43
Z9 44
U1 2
U2 44
PU CO-ACTION PUBLISHING
PI JARFALLA
PA RIPVAGEN 7, JARFALLA, SE-175 64, SWEDEN
SN 0280-6509
EI 1600-0889
J9 TELLUS B
JI Tellus Ser. B-Chem. Phys. Meteorol.
PD NOV
PY 2010
VL 62
IS 5
SI SI
BP 352
EP 368
DI 10.1111/j.1600-0889.2010.00498.x
PG 17
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 667BJ
UT WOS:000283167300005
ER
PT J
AU Alden, CB
Miller, JB
White, JWC
AF Alden, Caroline B.
Miller, John B.
White, James W. C.
TI Can bottom-up ocean CO2 fluxes be reconciled with atmospheric 13C
observations?
SO TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY
LA English
DT Article
ID CARBON-ISOTOPE DISCRIMINATION; AIR-SAMPLING-NETWORK; NINO-SOUTHERN
OSCILLATION; GAS TRANSFER VELOCITY; INTERANNUAL VARIABILITY; WIND-SPEED;
EL-NINO; LATITUDINAL DISTRIBUTION; DELTA-C-13 MEASUREMENTS; TERRESTRIAL
BIOSPHERE
AB The rare stable carbon isotope, 13C, has been used previously to partition CO2 fluxes into land and ocean components. Net ocean and land fluxes impose distinctive and predictable fractionation patterns upon the stable isotope ratio, making it an excellent tool for distinguishing between them. Historically, isotope constrained inverse methods for calculating CO2 surface fluxes-the 'double deconvolution'-have disagreed with bottom-up ocean flux estimates. In this study, we use the double deconvolution framework, but add, as a constraint, independent estimates of time histories of ocean fluxes to the atmospheric observations of CO2 and 13CO(2). We calculate timeseries of net land flux, total disequilibrium flux and terrestrial disequilibrium flux from 1991 to 2008 that are consistent with bottom-up net ocean fluxes. We investigate possible drivers of interannual variability in terrestrial disequilibrium flux, including terrestrial discrimination, and test the sensitivity of our results to those mechanisms. We find that C-3 plant discrimination and shifts in the global composition of C-3 and C-4 vegetation are likely drivers of interannual variability in terrestrial disequilibrium flux, while contributions from heterotrophic respiration and disturbance anomalies are also possible.
C1 [Miller, John B.] NOAA ESRL, Boulder, CO 80305 USA.
[Alden, Caroline B.; White, James W. C.] Univ Colorado, Inst Arctic & Alpine Res, Boulder, CO 80309 USA.
[Miller, John B.] Univ Colorado, CIRES, Boulder, CO 80309 USA.
RP Miller, JB (reprint author), NOAA ESRL, 325 Broadway, Boulder, CO 80305 USA.
EM john.b.miller@noaa.gov
RI White, James/A-7845-2009;
OI White, James/0000-0001-6041-4684; ALDEN, CAROLINE/0000-0002-5249-7800
FU NOAA Climate Program Office
FX The authors first thank all of the sample collectors at all of the
NOAA/ESRL sampling sites for their dedication and hard work. The authors
thank Bruce Vaughn, Sylvia Michel, Amy Steiker and Jason Winokur for the
preparation and analysis of delta13C data, and Patricia Lang,
Kelly Sours and Thomas Conway for CO2 analysis and data; Ken
Masarie for creating global means and help with figures; Pieter Tans for
ocean disequilibrium calculation algorithms; Neil Suits for SiB2
terrestrial fractionation model output; Jim Randerson for providing CASA
impulse-response functions; Nikki Lovenduski for discussion regarding
ocean CO2 flux variability; and the valuable input of those
who contributed to the review process of this paper. This work was
funded in part by the NOAA Climate Program Office.
NR 88
TC 13
Z9 13
U1 1
U2 22
PU CO-ACTION PUBLISHING
PI JARFALLA
PA RIPVAGEN 7, JARFALLA, SE-175 64, SWEDEN
SN 0280-6509
EI 1600-0889
J9 TELLUS B
JI Tellus Ser. B-Chem. Phys. Meteorol.
PD NOV
PY 2010
VL 62
IS 5
SI SI
BP 369
EP 388
DI 10.1111/j.1600-0889.2010.00481.x
PG 20
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 667BJ
UT WOS:000283167300006
ER
PT J
AU Gatti, LV
Miller, JB
D'Amelio, MTS
Martinewski, A
Basso, LS
Gloor, ME
Wofsy, S
Tans, P
AF Gatti, L. V.
Miller, J. B.
D'Amelio, M. T. S.
Martinewski, A.
Basso, L. S.
Gloor, M. E.
Wofsy, S.
Tans, P.
TI Vertical profiles of CO2 above eastern Amazonia suggest a net carbon
flux to the atmosphere and balanced biosphere between 2000 and 2009
SO TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY
LA English
DT Article
ID AIRBORNE MEASUREMENTS; RAIN-FOREST; CYCLE; DIOXIDE; EMISSIONS; FEEDBACK;
MODEL
AB From 2000 until January 2010 vertical profiles were collected above eastern Amazonia to help determine regional-scale (similar to 105-106 km2) fluxes of carbon cycle-related greenhouse gases. Samples were collected aboard light aircraft between the surface and 4.3 km and a column integration technique was used to determine the CO2 flux. Measured CO2 profiles were differenced from the CO2 background determined from measurements in the tropical Atlantic. The observed annual flux between the coast and measurement sites was 0.40 +/- 0.27 gC m-2 d-1 (90% confidence interval using a bootstrap analysis). The wet season (January-June) mean flux was 0.44 +/- 0.38 gC m-2 d-1 (positive fluxes defined as a source to the atmosphere) and the dry season mean flux was 0.35 +/- 0.17 gC m-2 d-1 (July-December). The observed flux variability is high, principally in the wet season. The influence of biomass burning has been removed using co-measured CO, and revealed the presence of a significant dry season sink. The annual mean vegetation flux, after the biomass burning correction, was 0.02 +/- 0.27 gC m-2 d-1, and a clear sink was observed between August and November of -0.70 +/- 0.21 gC m-2 d-1 where for all of the dry season it was -0.24 +/- 0.17 gC m-2 d-1.
C1 [Gatti, L. V.; D'Amelio, M. T. S.; Martinewski, A.; Basso, L. S.] IPEN, Atmospher Chem Lab, BR-05508000 Sao Paulo, Brazil.
[Miller, J. B.; Tans, P.] NOAA, Earth Syst Res Lab, Boulder, CO USA.
[Miller, J. B.] Univ Colorado, CIRES, Boulder, CO 80309 USA.
[Gloor, M. E.] Univ Leeds, Leeds LS2 9JT, W Yorkshire, England.
[Wofsy, S.] Harvard Univ, Cambridge, MA 02138 USA.
RP Gatti, LV (reprint author), IPEN, Atmospher Chem Lab, BR-05508000 Sao Paulo, Brazil.
EM lvgatti@ipen.br
RI Basso, Luana/E-3290-2014; Artaxo, Paulo/E-8874-2010; Gatti,
Luciana/J-8569-2012
OI Artaxo, Paulo/0000-0001-7754-3036;
FU NASA [S-10137, S-71307, NNG06GE14A]
FX We wish to thank Andrew Crotwell and Ed Dlugokencky for extensive
support with instrumentation and analysis; Doug Guenther for support
with sampling technology; Kirk Thoning for assistance with raw data
processing; Thomas Conway, Ken Masarie andDuane Kitzis for assistance
with CO2 data, data processing and reference gases,
respectively and Amelia Yamazaki for help with analysis; Aquila Taxi
Aereo for sampling at SAN, and the sample takers at RPB and ASC. We also
wish to thank Peter Bakwin and Paulo Artaxo for their efforts to start
the sampling program. This project is part of the Brazilian led
Large-scale Biosphere-atmosphere experiment in Amazonia (LBA), and was
funded by NASA inter-agency agreements S-10137 and S-71307 and grant
NNG06GE14A to JBM.
NR 40
TC 27
Z9 28
U1 0
U2 19
PU CO-ACTION PUBLISHING
PI JARFALLA
PA RIPVAGEN 7, JARFALLA, SE-175 64, SWEDEN
SN 0280-6509
EI 1600-0889
J9 TELLUS B
JI Tellus Ser. B-Chem. Phys. Meteorol.
PD NOV
PY 2010
VL 62
IS 5
SI SI
BP 581
EP 594
DI 10.1111/j.1600-0889.2010.00484.x
PG 14
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 667BJ
UT WOS:000283167300021
ER
PT J
AU Seitzinger, SP
Bouwman, AF
Kroeze, C
AF Seitzinger, S. P.
Bouwman, A. F.
Kroeze, C.
TI Preface to special section on Past and Future Trends in Nutrient Export
From Global Watersheds and Impacts on Water Quality and Eutrophication
SO GLOBAL BIOGEOCHEMICAL CYCLES
LA English
DT Editorial Material
ID COASTAL ZONE; SPATIALLY EXPLICIT; PHOSPHORUS; NITROGEN; MODEL
C1 [Seitzinger, S. P.] Rutgers State Univ, Inst Marine & Coastal Sci, NOAA CMER Program, New Brunswick, NJ 08903 USA.
[Bouwman, A. F.] Netherlands Environm Assessment Agcy, Bilthoven, Netherlands.
[Kroeze, C.] Wageningen Univ, Environm Syst Anal Grp, Wageningen, Netherlands.
[Kroeze, C.] Open Univ Netherlands, Sch Sci, Heerlen, Netherlands.
RP Seitzinger, SP (reprint author), Rutgers State Univ, Inst Marine & Coastal Sci, NOAA CMER Program, New Brunswick, NJ 08903 USA.
RI Bouwman, Lex/B-7053-2012; Bouwman, Lex/F-1444-2015
OI Bouwman, Lex/0000-0002-2045-1859
NR 20
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Z9 7
U1 1
U2 15
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0886-6236
J9 GLOBAL BIOGEOCHEM CY
JI Glob. Biogeochem. Cycle
PD OCT 30
PY 2010
VL 24
AR GB0A01
DI 10.1029/2010GB003851
PG 2
WC Environmental Sciences; Geosciences, Multidisciplinary; Meteorology &
Atmospheric Sciences
SC Environmental Sciences & Ecology; Geology; Meteorology & Atmospheric
Sciences
GA 674MF
UT WOS:000283748300001
ER
PT J
AU Warren, MA
Gregory, RS
Laurel, BJ
Snelgrove, PVR
AF Warren, M. A.
Gregory, R. S.
Laurel, B. J.
Snelgrove, P. V. R.
TI Increasing density of juvenile Atlantic (Gadus morhua) and Greenland cod
(G. ogac) in association with spatial expansion and recovery of eelgrass
(Zostera marina) in a coastal nursery habitat
SO JOURNAL OF EXPERIMENTAL MARINE BIOLOGY AND ECOLOGY
LA English
DT Article
DE Cod; Disturbance; Recruitment; Seagrass; Vegetation
ID SUBMERGED AQUATIC VEGETATION; WASTING DISEASE; NEWFOUNDLAND; SEAGRASS;
SETTLEMENT; PREDATION; WATERS; EUTROPHICATION; RECRUITMENT; SELECTION
AB Global declines of eelgrass (Zostera marina) have major ramifications for the juvenile fishes for which this plant can provide nursery habitat. However, it is less clear how rapidly fishes can recover when habitat loss is reversed, either through natural growth or through habitat enhancement efforts. We investigated the consequences of natural expansion and recovery of eelgrass following disturbance, on the densities of juveniles of two cod species - Atlantic (Gadus morhua) and Greenland (Gadus ogac) cod - in a coastal nursery area in Newfoundland, Canada. Eelgrass has been expanding at this location, likely as a result of reduced disturbance from winter pack-ice in the past decade. We conducted bi-weekly sampling of juvenile fish densities at 12 sites from July to November annually, 1995-2006, by seine netting. Each site was designated as either 'natural', 'expansion', 'removal-recovery' or 'unvegetated' dependent on their recent eelgrass coverage and involvement in a manipulation study (1999-2000; Laurel et al. 2003b). We measured eelgrass percentage cover at each site by analysis of aerial photographs. Eelgrass cover had noticeably increased in the 1999-2000 'removal-recovery' sites and at the 'expansion' sites following 2000. Using randomized intervention analysis (RIA) we detected positive relationships between eelgrass cover and relative fish density during 2001-2006. These results suggested a significant and rapid increase in age-0 cod density associated with eelgrass habitat expansion. We suggest that juvenile cod density responds to annual expansion and contraction of eelgrass cover, illustrating the potential cascading effects of eelgrass loss associated with climate change, human disturbance, and disease and the potential benefits of eelgrass conservation and enhancement. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Warren, M. A.] Mem Univ Newfoundland, Dept Biol, St John, NF A1C 5S7, Canada.
[Gregory, R. S.] Fisheries & Oceans Canada, Div Environm Sci, St John, NF A1C 5X1, Canada.
[Laurel, B. J.] Natl Marine Fisheries Serv, Fisheries Behav Ecol Program, Alaska Fisheries Sci Ctr, NOAA,Hatfield Marine Sci Ctr, Newport, OR 97365 USA.
[Snelgrove, P. V. R.] Mem Univ Newfoundland, Ctr Ocean Sci, Canada Res Chair Boreal & Cold Ocean Syst, St John, NF A1C 5S7, Canada.
[Snelgrove, P. V. R.] Mem Univ Newfoundland, Dept Biol, St John, NF A1C 5S7, Canada.
RP Warren, MA (reprint author), Univ Western Ontario, Dept Biol, 1151 Richmond St, London, ON N6A 5B7, Canada.
EM mwarren4@uwo.ca
FU Fisheries and Oceans Canada (DFO); National Sciences and Engineering
Research Council; Parks Canada (Terra Nova National Park - TNNP);
Environment Canada
FX Our research was funded in various years by Fisheries and Oceans Canada
(DFO) programs led by RSG, two NSERC Strategic Grants from the National
Sciences and Engineering Research Council led by David C. Schneider and
PVRS, respectively, Parks Canada (Terra Nova National Park - TNNP) led
by RSG, and an Environment Canada grant led by John T. Anderson.
Accommodations, boats, vehicles, were variously provided through the
period by DFO, TNNP, and Memorial University of Newfoundland (MUN). We
appreciate the dozens of MUN, DFO, and TNNP students, technicians, and
volunteers who assisted us with field sampling throughout our study.
Drs. Steven Carr and Evan Edinger also made helpful suggestions on
earlier versions of the manuscript. This paper formed part of the BSc
Honours Thesis research of the senior author, MAW. [SS]
NR 48
TC 11
Z9 12
U1 1
U2 37
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0022-0981
J9 J EXP MAR BIOL ECOL
JI J. Exp. Mar. Biol. Ecol.
PD OCT 30
PY 2010
VL 394
IS 1-2
BP 154
EP 160
DI 10.1016/j.jembe.2010.08.011
PG 7
WC Ecology; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA 665IB
UT WOS:000283027500014
ER
PT J
AU Hong, G
Yang, P
Heidinger, AK
Pavolonis, MJ
Baum, BA
Platnick, SE
AF Hong, Gang
Yang, Ping
Heidinger, Andrew K.
Pavolonis, Michael J.
Baum, Bryan A.
Platnick, Steven E.
TI Detecting opaque and nonopaque tropical upper tropospheric ice clouds: A
trispectral technique based on the MODIS 8-12 mu m window bands
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID ATMOSPHERE RADIATIVE FLUXES; ISCCP DATA SETS; CIRRUS CLOUDS;
SPLIT-WINDOW; ALGORITHM DESCRIPTION; TOP; TROPOPAUSE; SURFACE;
CLASSIFICATION; SENSITIVITY
AB A trispectral technique is developed for detecting tropical upper tropospheric opaque (tau > 6) and nonopaque (tau < 6) ice clouds over ocean based on the brightness temperature differences between the MODIS 8.5 and 11 mu m bands and between the 11 and 12 mu m bands together with the MODIS detected cloud thermodynamic phase. The brightness temperature differences provide robust information for classifying ice clouds, as illustrated by the observations made by a lidar, a radar, and the MODIS Airborne Simulator over tropical ice anvil systems during the Cirrus Regional Study of Tropical Anvils and Cirrus Layers-Florida Area Cirrus Experiment. The trispectral technique for detecting tropical upper tropospheric opaque and nonopaque ice clouds is developed based on the analysis of 1 year of data, including MODIS infrared brightness temperatures at 8.5, 11, and 12 mm bands, MODIS-derived ice cloud optical thicknesses, and cloud top heights from CALIPSO and CloudSat over a region (140 degrees E-180 degrees E, 0 degrees N-20 degrees N) in the Western Pacific Warm Pool. The accuracy of the present trispectral technique is above 80%. A 27 July 2007 MODIS granule over the chosen region is used to verify the trispectral technique. It is found that the classification from the trispectral technique is consistent with a classification based directly on the MODIS ice cloud optical thicknesses. The effects of the variations in the MODIS viewing zenith angle on the detection are found to be negligible. The CALIPSO and CloudSat observations used to develop the classification are more sensitive than MODIS to the height and presence of optically thin cirrus. These differences in cloud heights were found to have a negligible impact on the final detection results.
C1 [Hong, Gang; Yang, Ping] Texas A&M Univ, Dept Atmospher Sci, College Stn, TX 77843 USA.
[Heidinger, Andrew K.; Pavolonis, Michael J.] NOAA NESDIS Ctr Satellite Applicat & Res, Madison, WI USA.
[Baum, Bryan A.] Univ Wisconsin, Ctr Space Sci & Engn, Madison, WI 53706 USA.
[Platnick, Steven E.] NASA, Goddard Space Flight Ctr, Atmospheres Lab, Greenbelt, MD 20771 USA.
RP Hong, G (reprint author), Texas A&M Univ, Dept Atmospher Sci, College Stn, TX 77843 USA.
EM hong@ariel.met.tamu.edu
RI Yang, Ping/B-4590-2011; Pavolonis, Mike/F-5618-2010; Hong,
Gang/A-2323-2012; Baum, Bryan/B-7670-2011; Platnick, Steven/J-9982-2014;
Heidinger, Andrew/F-5591-2010
OI Pavolonis, Mike/0000-0001-5822-219X; Baum, Bryan/0000-0002-7193-2767;
Platnick, Steven/0000-0003-3964-3567; Heidinger,
Andrew/0000-0001-7631-109X
FU NASA [NNX08AP57G, NN08AF68G, NNX08AF78A]
FX We thank the NASA CloudSat project for providing the 2B-GEOPROF-LIDAR
and ECMWF-AUX data used in this study, which are taken from the CloudSat
Data Processing Center at Colorado State University. The MODIS data are
archived at NASA's Goddard Earth Sciences Data and Information Services
Center (GES-DISC). We gratefully thank Drs. Lihua Li and Lin Tian for
providing the CRS data used in this study. We would also like to
acknowledge Dr. Zhibo Zhang for useful comments and suggestions. We
acknowledge the three anonymous reviewers for their constructive
comments and suggestions. This study is supported by NASA grants
NNX08AP57G and NN08AF68G. Support for Bryan Baum is provided through
NASA grant NNX08AF78A.
NR 62
TC 7
Z9 7
U1 0
U2 7
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-897X
EI 2169-8996
J9 J GEOPHYS RES-ATMOS
JI J. Geophys. Res.-Atmos.
PD OCT 30
PY 2010
VL 115
AR D20214
DI 10.1029/2010JD014004
PG 11
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 674MT
UT WOS:000283751000004
ER
PT J
AU Jeerage, KM
LaNasa, SM
Hughes, HA
Lauria, DS
Bryant, SJ
Slifka, AJ
AF Jeerage, Kavita M.
LaNasa, Stephanie M.
Hughes, Holly A.
Lauria, Damian S.
Bryant, Stephanie J.
Slifka, Andrew J.
TI Scanning electrochemical microscopy measurements of poly(ethylene
glycol) hydrogels
SO POLYMER
LA English
DT Article
DE Diffusivity; Hydrogel; Scanning electrochemical microscopy
ID CONTACT-LENSES; LIVING CELLS; TISSUE; OXYGEN; SCAFFOLDS; GELS;
CHONDROCYTES; PRINCIPLES; VIABILITY; TRANSPORT
AB Scanning electrochemical microscopy has been used to examine the molecular transport properties of photopolymerized poly(ethylene glycol) (PEG) hydrogels having different mesh sizes. Both the molecular weight (508 Da or 3000 Da) of the PEG diacrylate macromer and its weight percent (20 wt%, 40 wt%, or 60 wt%) in solution prior to photopolymerization were varied. Mesh size was estimated from equilibrium swelling measurements and a thermodynamic model. Estimated mesh sizes ranged from ca. 10 A for 60 wt% PEG 508 gels to ca. 100 A for 20 wt% PEG 3000 gels. The electrochemically active diffusing species, ferrocenemethanol, was detected via oxidation at a platinum microelectrode. For a given hydrogel, multiple approach curves showed a consistent relationship between current and distance. Electrochemically estimated diffusivities followed the same trend as predictions based on mesh size and ranged from 25% to 80% of the diffusivity in aqueous solution. As a proof of concept, scanning electrochemical microscopy was successfully used to map the topography of hydrogels with complex architecture, which are being designed as cell scaffolds. Published by Elsevier Ltd.
C1 [Jeerage, Kavita M.; Lauria, Damian S.; Slifka, Andrew J.] Natl Inst Stand & Technol, Div Mat Reliabil, Boulder, CO 80305 USA.
[LaNasa, Stephanie M.; Hughes, Holly A.; Bryant, Stephanie J.] Univ Colorado, Dept Chem & Biol Engn, Boulder, CO 80309 USA.
RP Jeerage, KM (reprint author), Natl Inst Stand & Technol, Div Mat Reliabil, 325 Broadway, Boulder, CO 80305 USA.
EM jeerage@boulder.nist.gov
RI Hume, Stephanie/C-5220-2012
FU University of Colorado - National Institute of Standards & Technology
(CU-NIST); National Research Council (NRC); National Science Foundation
(NSF)
FX Financial support for this work was provided by a University of Colorado
- National Institute of Standards & Technology (CU-NIST) Seed Grant.
This research was performed while K.M.J. held a National Research
Council (NRC) Postdoctoral Fellowship and S.M.L. held a National Science
Foundation (NSF) Graduate Research Fellowship.
NR 42
TC 4
Z9 5
U1 2
U2 12
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0032-3861
J9 POLYMER
JI Polymer
PD OCT 29
PY 2010
VL 51
IS 23
BP 5456
EP 5461
DI 10.1016/j.polymer.2010.09.028
PG 6
WC Polymer Science
SC Polymer Science
GA 677XN
UT WOS:000284029200023
ER
PT J
AU Vukicevic, T
Coddington, O
Pilewskie, P
AF Vukicevic, Tomislava
Coddington, Odele
Pilewskie, Peter
TI Characterizing the retrieval of cloud properties from optical remote
sensing
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID RADIUS
AB This paper presents a new approach to the formal characterization of the optical retrieval of cloud optical thickness and effective droplet radius based on a nonlinear methodology that is derived from a general stochastic inverse problem formulation similar to standard Bayesian estimation theory. The methodology includes efficient use of the precomputed radiative transfer model simulations which are already available in standard retrieval algorithms. Another important property of the methodology is that it does not require performing the retrieval with actual measurements in order to characterize the retrieval results. One utility of this analysis is the quantification of information content in the standard retrieval problem, and the increase of information through adding channels (radiances at different wavelengths) to the inversion. This was demonstrated for the five-wavelength retrieval using airborne hyperspectral shortwave irradiance measurements. The ability of the method to evaluate the impact of observation and radiative transfer model uncertainties on the retrieved cloud properties is also demonstrated. Further benefits from this study will be in its application to the cloud retrieval algorithms to be developed for future space-and airborne instruments. The present study puts forth the framework necessary to quantify that increase in information and to optimize new retrieval algorithms that efficiently accommodate the enhanced measurement space.
C1 [Vukicevic, Tomislava] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
[Coddington, Odele; Pilewskie, Peter] Univ Colorado, ATOC, Boulder, CO 80309 USA.
RP Vukicevic, T (reprint author), NOAA, Atlantic Oceanog & Meteorol Lab, 4301 Rickenbacker Causeway, Miami, FL 33149 USA.
EM tomislava.vukicevic@noaa.gov
RI Coddington, Odele/F-6342-2012; Vukicevic, Tomislava/B-1386-2014
OI Coddington, Odele/0000-0002-4338-7028;
FU NSF [ATM 0754998]; NASA [NNX08AI83G]; NOAA [NA06OAR4310085]
FX This study was supported by NSF award ATM 0754998 while the first author
was at University of Colorado, Boulder. Contributions by the second and
third author were supported by NASA grant NNX08AI83G and NOAA grant
NA06OAR4310085.
NR 20
TC 9
Z9 9
U1 0
U2 6
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-897X
J9 J GEOPHYS RES-ATMOS
JI J. Geophys. Res.-Atmos.
PD OCT 29
PY 2010
VL 115
AR D20211
DI 10.1029/2009JD012830
PG 14
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 674MP
UT WOS:000283750600001
ER
PT J
AU Buijsman, MC
McWilliams, JC
Jackson, CR
AF Buijsman, M. C.
McWilliams, J. C.
Jackson, C. R.
TI East-west asymmetry in nonlinear internal waves from Luzon Strait
SO JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
LA English
DT Article
ID SOUTH CHINA SEA; OCEANIC MODELING SYSTEM; PART I; TIDES; GENERATION;
TOPOGRAPHY; CONVERSION; SURFACE; WATER
AB The nonhydrostatic Regional Ocean Modeling System is applied to study the effects of thermocline shoaling/deepening, bathymetry, and asymmetric modulated tides on the soliton growth to the west and east of Luzon Strait in the South China Sea and western Pacific Ocean. Luzon Strait comprises a shallow east ridge and a deep west ridge, and its interaction with barotropic tidal currents yields strong westward internal tides that disperse into solitons. Satellite imagery indicates that the westward solitons are more numerous and better defined than the eastward solitons. The model results show that the eastward solitons are 45%, 39%, 28%, and 23% smaller than the westward solitons due to asymmetric modulated barotropic tides at the east ridge, a deeper Pacific Ocean, westward thermocline shoaling related to the Kuroshio current, and internal tide resonance in a double ridge configuration, respectively. Due to the westward location of the Kuroshio, little thermocline deepening occurs east of the east ridge. Hence, the influence of thermocline deepening on counteracting eastward soliton growth is small. The Kuroshio mainly enhances westward soliton growth. The dispersion of internal tides into solitons is governed by the balance between the nonlinearity parameter on the one hand and the nonhydrostatic and Coriolis dispersions on the other. It is shown that this balance favors soliton growth for thermocline shoaling, while it counters it for a deeper ocean. A series of double ridge experiments is performed, in which the distance between the ridges and the height of the west ridge are varied. For a semidiurnal tidal forcing and two Gaussian ridges separated by 100 km, barotropic to baroclinic energy conversion is enhanced at both ridges, causing larger westward internal tides and solitons. The combination of Coriolis forcing, thermocline shoaling, and a double ridge configuration enhances the distinctiveness of the so-called type a and b solitons when a modulated tide occurs.
C1 [Buijsman, M. C.; McWilliams, J. C.] Univ Calif Los Angeles, Dept Atmospher & Ocean Sci, Los Angeles, CA 90095 USA.
[Jackson, C. R.] Global Ocean Associates, Alexandria, VA 22310 USA.
[Buijsman, M. C.] Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA.
RP Buijsman, MC (reprint author), Univ Calif Los Angeles, Dept Atmospher & Ocean Sci, 405 Hilgard Ave, Los Angeles, CA 90095 USA.
EM maarten.buijsman@noaa.gov
FU Office of Naval Research [N00014-05-10293, N00014-08-10597]
FX The Office of Naval Research is acknowledged for supporting this
research with grants N00014-05-10293 and N00014-08-10597. We thank
Alexander Shchepetkin for assistance with the modeling and Jaison Kurian
for helping with the SODA data analysis.
NR 27
TC 35
Z9 37
U1 2
U2 22
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0148-0227
J9 J GEOPHYS RES-OCEANS
JI J. Geophys. Res.-Oceans
PD OCT 29
PY 2010
VL 115
AR C10057
DI 10.1029/2009JC006004
PG 14
WC Oceanography
SC Oceanography
GA 674SB
UT WOS:000283768900001
ER
PT J
AU Mao, HK
Shirley, EL
Ding, Y
Eng, P
Cai, YQ
Chow, P
Xiao, YM
Shu, JF
Hemley, RJ
Kao, CC
Mao, WL
AF Mao, Ho Kwang
Shirley, Eric L.
Ding, Yang
Eng, Peter
Cai, Yong Q.
Chow, Paul
Xiao, Yuming
Shu, Jinfu
Hemley, Russell J.
Kao, Chichang
Mao, Wendy L.
TI Electronic Structure of Crystalline He-4 at High Pressures
SO PHYSICAL REVIEW LETTERS
LA English
DT Article
AB Using inelastic x-ray scattering techniques, we have succeeded in probing the high-pressure electronic structure of helium at 300 K. Helium has the widest known valence-conduction band gap of all materials a property whose high-pressure response has been inaccessible to direct measurements. We observed a rich electron excitation spectrum, including a cutoff edge above 23 eV, a sharp exciton peak showing linear volume dependence, and a series of excitations and continuum at 26 to 45 eV. We determined the electronic dispersion along the Gamma-M direction over two Brillouin zones, and provided a quantitative picture of the helium exciton beyond the simplified Wannier-Frenkel description.
C1 [Mao, Ho Kwang; Shu, Jinfu; Hemley, Russell J.] Carnegie Inst Washington, Geophys Lab, Washington, DC 20015 USA.
[Mao, Ho Kwang; Ding, Yang] Carnegie Inst Washington, HPSynC, Argonne, IL 60439 USA.
[Mao, Ho Kwang; Chow, Paul; Xiao, Yuming] Carnegie Inst Washington, HPCAT, Argonne, IL 60439 USA.
[Shirley, Eric L.] NIST, Opt Technol Div, Gaithersburg, MD 20899 USA.
[Eng, Peter] Univ Chicago, Consortium Adv Radiat Sources, Chicago, IL 60637 USA.
[Eng, Peter] Univ Chicago, James Franck Inst, Chicago, IL 60637 USA.
[Cai, Yong Q.] Brookhaven Natl Lab, Natl Synchrotron Light Source 2, Upton, NY 11973 USA.
[Kao, Chichang] SLAC Natl Accelerator Lab, SSRL, Menlo Pk, CA 94025 USA.
[Mao, Wendy L.] SLAC Natl Accelerator Lab, SIMES, Menlo Pk, CA 94025 USA.
[Mao, Wendy L.] Stanford Univ, Stanford, CA 94305 USA.
RP Mao, HK (reprint author), Carnegie Inst Washington, Geophys Lab, 5251 Broad Branch Rd NW, Washington, DC 20015 USA.
RI Mao, Wendy/D-1885-2009; Ding, Yang/K-1995-2014; Cai, Yong/C-5036-2008
OI Ding, Yang/0000-0002-8845-4618; Cai, Yong/0000-0002-9957-6426
FU U.S. Department of Energy (DOE), Office of Science, Office of Basic
Energy Sciences (BES) [DE-SC0001057]; Division of Material Science and
Engineering [DE-AC02-76SF00515]; National Aeronautics and Space
Administration [NNX08AL27G]; NSF [DMR-0805056, EAR-0622171]; DOE-NNSA;
DOE-BES [DE-AC02-06CH11357]; DOE-Geosciences [DE-FG02-94ER14466];
National Synchrotron Radiation Research Center; National Science Center
of Taiwan
FX This research was carried out as part of the EFree, an Energy Frontier
Research Center funded by the U.S. Department of Energy (DOE), Office of
Science, Office of Basic Energy Sciences (BES) under Grant No.
DE-SC0001057, and the Division of Material Science and Engineering under
Contract No. DE-AC02-76SF00515, National Aeronautics and Space
Administration Grant No. NNX08AL27G, and NSF Grant No. DMR-0805056. The
use of HPCAT (Sector 16) is supported by CIW, CDAC, UNLV, and LLNL
through funding from DOE-NNSA, DOE-BES, and NSF; the use of GSECARS is
supported by the NSF EAR-0622171 and DOE-Geosciences DE-FG02-94ER14466;
the use of BL12XU, SPring-8, is supported by the National Synchrotron
Radiation Research Center and National Science Center of Taiwan. APS is
supported by DOE-BES, under Contract No. DE-AC02-06CH11357.
NR 12
TC 10
Z9 10
U1 0
U2 10
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 0031-9007
J9 PHYS REV LETT
JI Phys. Rev. Lett.
PD OCT 29
PY 2010
VL 105
IS 18
AR 186404
DI 10.1103/PhysRevLett.105.186404
PG 4
WC Physics, Multidisciplinary
SC Physics
GA 673IF
UT WOS:000283652100003
PM 21231121
ER
PT J
AU Chai, H
Josell, D
AF Chai, Herzl
Josell, Daniel
TI Fracture behavior of nano-layered coatings under tension
SO THIN SOLID FILMS
LA English
DT Article
DE Thin films; Si/Ag; Multilayers; Fragmentation; Tunnel cracks; Fracture
toughness
ID THIN-FILMS; MULTILAYER COATINGS; STRAIN; CRACKING; MECHANICS; CU;
COMPOSITES; SUBSTRATE; TOUGHNESS; STRENGTH
AB The fracture of brittle/ductile multilayers composed of equal thicknesses of Si and Ag layers evaporated on a thick substrate is studied with the aid of a four-point bending apparatus. The system variables include individual layer thickness (2.5 to 30 nm), total film thickness (0.5 to 3.5 mu m) and substrate material (polycarbonate, aluminum alloy and hard steel). The fracture is characterized by transverse cracks that proliferate with load. The crack initiation strain epsilon(i) is virtually independent of total film thickness and substrate material while increasing with decreasing layer thickness h, to a good approximation as epsilon(i)similar to 1/h(1/2). At higher strains, film debonding and buckling are evident.
The fracture conditions are determined with the aid of a 2D finite element analysis incorporating the inelastic response of the interlayer. A fracture scenario consisting of tunnel cracking in the brittle layers followed by cracking in the interlayers is shown to be capable of predicting the observed increase in crack initiation strain with decreasing layer thickness. To realize this benefit the interlayer must be compliant and tough to force tunnel cracking in the brittle layers. The explicit relation for the crack initiation strain obtained from the analysis can be used to assess fracture toughness and improve damage tolerance in nanoscale layered structures. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Chai, Herzl] Tel Aviv Univ, Fac Engn, Sch Mech Engn, IL-69978 Tel Aviv, Israel.
[Josell, Daniel] NIST, Div Met, MSEL, Gaithersburg, MD 20899 USA.
RP Chai, H (reprint author), Tel Aviv Univ, Fac Engn, Sch Mech Engn, IL-69978 Tel Aviv, Israel.
EM herzl@eng.tau.ac.il
NR 26
TC 3
Z9 3
U1 1
U2 17
PU ELSEVIER SCIENCE SA
PI LAUSANNE
PA PO BOX 564, 1001 LAUSANNE, SWITZERLAND
SN 0040-6090
J9 THIN SOLID FILMS
JI Thin Solid Films
PD OCT 29
PY 2010
VL 519
IS 1
BP 331
EP 336
DI 10.1016/j.tsf.2010.07.086
PG 6
WC Materials Science, Multidisciplinary; Materials Science, Coatings &
Films; Physics, Applied; Physics, Condensed Matter
SC Materials Science; Physics
GA 676YI
UT WOS:000283955200058
ER
PT J
AU Niu, XL
Pinker, RT
Cronin, MF
AF Niu, Xiaolei
Pinker, Rachel T.
Cronin, Meghan F.
TI Radiative fluxes at high latitudes
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID ARCTIC SURFACE; CLOUD; MODIS
AB Newly improved satellite products and surface observations provide an opportunity to revisit remote-sensing capabilities for estimating shortwave (SW) radiative fluxes at high latitudes, location of disagreement among models and observations. Estimates of SW fluxes from the Moderate Resolution Imaging Spectro-radiometer (MODIS) are evaluated against land observations from the Baseline Surface Radiation Network (BSRN), from Greenland, and unique buoy measurements. Results show that the MODIS products are in better agreement with observations than those from numerical models. Therefore, the large scale satellite based estimates should be useful for model evaluation and for providing information in formulating energy budgets at high latitudes. Citation: Niu, X., R. T. Pinker, and M. F. Cronin (2010), Radiative fluxes at high latitudes, Geophys. Res. Lett., 37, L20811, doi:10.1029/2010GL044606.
C1 [Niu, Xiaolei; Pinker, Rachel T.] Univ Maryland, Dept Atmospher & Ocean Sci, College Pk, MD 20742 USA.
[Cronin, Meghan F.] NOAA, Pacific Marine Environm Lab, Seattle, WA 98115 USA.
RP Niu, XL (reprint author), Univ Maryland, Dept Atmospher & Ocean Sci, Space Sci Bldg, College Pk, MD 20742 USA.
EM pinker@atmos.umd.edu
RI Pinker, Rachel/F-6565-2010
FU NSF [ATM0631685]; NASA [NNG05GB35G]
FX This work benefited from support under NSF grant ATM0631685 and NASA
grant NNG05GB35G to the University of Maryland. Thanks are due to the
NASA GES DISC Giovanni for the MODIS data, to the various MODIS teams,
to BSRN for observations, to WHOI for the CLIMODE data, to the Greenland
Climate Network (GC-Net) for data for Summit, and to H. Wang for his
contribution.
NR 17
TC 13
Z9 13
U1 0
U2 8
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
EI 1944-8007
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD OCT 28
PY 2010
VL 37
AR L20811
DI 10.1029/2010GL044606
PG 5
WC Geosciences, Multidisciplinary
SC Geology
GA 674LV
UT WOS:000283747000002
ER
PT J
AU Kramida, AE
AF Kramida, A. E.
TI Revised interpretation of the Na I EUV absorption spectrum
SO JOURNAL OF PHYSICS B-ATOMIC MOLECULAR AND OPTICAL PHYSICS
LA English
DT Article
ID EXCITED QUARTET STATES; ENERGY-LEVELS; SODIUM; PHOTOABSORPTION;
ULTRAVIOLET; LIFETIMES; VUV
AB Spectral data for neutral sodium were recently compiled by Sansonetti (2008 J. Phys. Chem. Ref. Data 37 1659). In that compilation, some of the energy levels of the 2p(5)3snl configurations were quoted from the studies of the absorption spectrum in the extreme ultraviolet (EUV) region, while others were quoted from beam-foil and laser-spectroscopy studies of emission in the visible region. These two sets of data partially overlap. However, in Sansonetti (2008) the energy levels observed in both types of studies were not recognized as being the same entities and were listed as different quantum states, interpreted in different coupling schemes. In addition, the analysis of the absorption spectrum was based on an oversimplified theoretical model and is incomplete. The present work identifies the energy levels commonly observed in absorption and emission studies and provides a consistent description of the 2p(5)3snl energy levels. As a result, about a hundred energy levels are revised. In particular, the connection of the quartet level system with the ground state is firmly established based on absorption studies.
C1 Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
RP Kramida, AE (reprint author), Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
EM Alexander.kramida@nist.gov
OI Kramida, Alexander/0000-0002-0788-8087
NR 14
TC 2
Z9 2
U1 0
U2 7
PU IOP PUBLISHING LTD
PI BRISTOL
PA DIRAC HOUSE, TEMPLE BACK, BRISTOL BS1 6BE, ENGLAND
SN 0953-4075
J9 J PHYS B-AT MOL OPT
JI J. Phys. B-At. Mol. Opt. Phys.
PD OCT 28
PY 2010
VL 43
IS 20
AR 205001
DI 10.1088/0953-4075/43/20/205001
PG 9
WC Optics; Physics, Atomic, Molecular & Chemical
SC Optics; Physics
GA 658VF
UT WOS:000282516800006
ER
PT J
AU Mitroy, J
Safronova, MS
Clark, CW
AF Mitroy, J.
Safronova, M. S.
Clark, Charles W.
TI Theory and applications of atomic and ionic polarizabilities
SO JOURNAL OF PHYSICS B-ATOMIC MOLECULAR AND OPTICAL PHYSICS
LA English
DT Review
ID STATIC DIPOLE POLARIZABILITIES; ALKALI-METAL ATOMS; STARK-EFFECT
INVESTIGATIONS; OPTICAL FREQUENCY STANDARD; DER-WAALS COEFFICIENTS;
PRECISION LIFETIME MEASUREMENTS; CORE POLARIZATION CORRECTIONS;
HIGH-ACCURACY CALCULATION; BODY-PERTURBATION-THEORY; LONG-RANGE
INTERACTIONS
AB Atomic polarization phenomena impinge upon a number of areas and processes in physics. The dielectric constant and refractive index of any gas are examples of macroscopic properties that are largely determined by the dipole polarizability. When it comes to microscopic phenomena, the existence of alkaline-earth anions and the recently discovered ability of positrons to bind to many atoms are predominantly due to the polarization interaction. An imperfect knowledge of atomic polarizabilities is presently looming as the largest source of uncertainty in the new generation of optical frequency standards. Accurate polarizabilities for the group I and II atoms and ions of the periodic table have recently become available by a variety of techniques. These include refined many-body perturbation theory and coupled-cluster calculations sometimes combined with precise experimental data for selected transitions, microwave spectroscopy of Rydberg atoms and ions, refractive index measurements in microwave cavities, ab initio calculations of atomic structures using explicitly correlated wavefunctions, interferometry with atom beams and velocity changes of laser cooled atoms induced by an electric field. This review examines existing theoretical methods of determining atomic and ionic polarizabilities, and discusses their relevance to various applications with particular emphasis on cold-atom physics and the metrology of atomic frequency standards.
C1 [Mitroy, J.] Charles Darwin Univ, Sch Engn, Darwin, NT 0909, Australia.
[Safronova, M. S.] Univ Delaware, Dept Phys & Astron, Newark, DE 19716 USA.
[Clark, Charles W.] Natl Inst Stand & Technol, Joint Quantum Inst, Gaithersburg, MD 20899 USA.
[Clark, Charles W.] Univ Maryland, Gaithersburg, MD 20899 USA.
RP Mitroy, J (reprint author), Charles Darwin Univ, Sch Engn, Darwin, NT 0909, Australia.
EM jxm107@rsphysse.anu.edu.au; msafrono@udel.edu; charles.clark@nist.gov
RI Clark, Charles/A-8594-2009; Mitroy, James/N-2162-2013
OI Clark, Charles/0000-0001-8724-9885; Mitroy, James/0000-0002-2477-1251
FU National Science Foundation under Physics Frontiers Center
[PHY-0822671]; US National Science Foundation [PHY-07-58088]; Australian
Research Council [DP-1092620]; US Department of Commerce, National
Institute of Standards and Technology
FX The authors express their appreciation to Dr U I Safronova for useful
discussions and comments on the manuscript, and in particularly for her
thorough check of most of the tables. This work was partly supported by
the National Science Foundation under Physics Frontiers Center grant
PHY-0822671 to the University of Maryland. This research has made
extensive use of NASA's Astrophysics Data System. The work of MSS was
supported in part by the US National Science Foundation grant no
PHY-07-58088. The work of JM was supported in part by the Australian
Research Council Discovery Project DP-1092620. This research was
performed in part under the sponsorship of the US Department of
Commerce, National Institute of Standards and Technology.
NR 385
TC 174
Z9 177
U1 8
U2 81
PU IOP PUBLISHING LTD
PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0953-4075
EI 1361-6455
J9 J PHYS B-AT MOL OPT
JI J. Phys. B-At. Mol. Opt. Phys.
PD OCT 28
PY 2010
VL 43
IS 20
AR 202001
DI 10.1088/0953-4075/43/20/202001
PG 38
WC Optics; Physics, Atomic, Molecular & Chemical
SC Optics; Physics
GA 658VF
UT WOS:000282516800005
ER
PT J
AU Sansonetti, CJ
Veza, D
AF Sansonetti, Craig J.
Veza, Damir
TI Doppler-free measurement of the 546 nm line of mercury
SO JOURNAL OF PHYSICS B-ATOMIC MOLECULAR AND OPTICAL PHYSICS
LA English
DT Article
ID FOURIER-TRANSFORM SPECTROSCOPY; HYPERFINE-STRUCTURE; WAVELENGTHS; LASER;
STANDARDS; SHIFTS; IODINE
AB We have made Doppler-free observations of the 546 nm line of neutral mercury by using saturated absorption and frequency modulation spectroscopy. Absolute wave numbers were measured for 14 resolved components arising from six mercury isotopes. Combining these measurements with precisely known isotope shifts and hyperfine-structure splittings, we derive a value for the wave number in (198)Hg from each of the measured features. Our final value for the wave number of the (198)Hg line is in good agreement with a recently reported measurement using Fourier transform spectroscopy but has an uncertainty that is smaller by a factor of 12.
C1 [Sansonetti, Craig J.; Veza, Damir] Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
[Veza, Damir] Univ Zagreb, Dept Phys, Zagreb 41000, Croatia.
RP Sansonetti, CJ (reprint author), Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
EM craig.sansonetti@nist.gov
NR 18
TC 3
Z9 3
U1 1
U2 12
PU IOP PUBLISHING LTD
PI BRISTOL
PA DIRAC HOUSE, TEMPLE BACK, BRISTOL BS1 6BE, ENGLAND
SN 0953-4075
J9 J PHYS B-AT MOL OPT
JI J. Phys. B-At. Mol. Opt. Phys.
PD OCT 28
PY 2010
VL 43
IS 20
AR 205003
DI 10.1088/0953-4075/43/20/205003
PG 6
WC Optics; Physics, Atomic, Molecular & Chemical
SC Optics; Physics
GA 658VF
UT WOS:000282516800008
ER
PT J
AU Xu, ZJ
Wen, JS
Xu, GY
Stock, C
Gardner, JS
Gehring, PM
AF Xu, Zhijun
Wen, Jinsheng
Xu, Guangyong
Stock, C.
Gardner, J. S.
Gehring, P. M.
TI Two-component model of the neutron diffuse scattering in the relaxor
ferroelectric PZN-4.5% PT
SO PHYSICAL REVIEW B
LA English
DT Article
ID RAMAN-SCATTERING; SINGLE-CRYSTALS; BEHAVIOR; PB(ZN1/3NB2/3)O-3; SYSTEM
AB We report measurements of the neutron diffuse scattering in a single crystal of the relaxor ferroelectric material 95.5% Pb(Zn1/3Nb2/3)O-3-4.5% PbTiO3. Our results suggest that the nanometer scale structure in this compound exhibits both < 100 > and < 110 > polarizations, which contribute to different portions of the total diffuse scattering intensity. These contributions can be distinguished by the differing responses to an electric field applied along [001]. While diffuse scattering intensities associated with < 110 > (T2-type) polarizations show little to no change in a [001] field, those associated with < 100 > (T1-type) polarizations are partially suppressed by the field at temperatures below the Curie temperature T-C similar to 475 K. Neutron spin-echo measurements show that the diffuse scattering at (0.05,0,1) is largely dynamic at high temperature and gradually freezes on cooling, becoming mostly static at 200 K.
C1 [Xu, Zhijun; Wen, Jinsheng; Xu, Guangyong] Brookhaven Natl Lab, Condensed Matter Phys & Mat Sci Dept, Upton, NY 11973 USA.
[Xu, Zhijun] CUNY City Coll, Dept Phys, New York, NY 10033 USA.
[Wen, Jinsheng] SUNY Stony Brook, Dept Mat Sci & Engn, Stony Brook, NY 11794 USA.
[Stock, C.; Gardner, J. S.] Indiana Univ, Bloomington, IN 47408 USA.
[Gardner, J. S.; Gehring, P. M.] Natl Inst Stand & Technol, NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA.
RP Xu, ZJ (reprint author), Brookhaven Natl Lab, Condensed Matter Phys & Mat Sci Dept, Upton, NY 11973 USA.
RI Wen, Jinsheng/F-4209-2010; Xu, Guangyong/A-8707-2010; Gardner,
Jason/A-1532-2013; xu, zhijun/A-3264-2013;
OI Wen, Jinsheng/0000-0001-5864-1466; Xu, Guangyong/0000-0003-1441-8275;
xu, zhijun/0000-0001-7486-2015; Gehring, Peter/0000-0002-9236-2046
FU U.S. Department of Energy [DE-AC02-98CH10886]; Natural Sciences and
Engineering Research Council of Canada (NSERC)
FX We wish to thank W. Ratcliff, S. M. Shapiro, and S. B. Vakhrushev for
useful discussions. Financial support from the U.S. Department of Energy
under Contract No. DE-AC02-98CH10886 and the Natural Sciences and
Engineering Research Council of Canada (NSERC) is also gratefully
acknowledged.
NR 48
TC 14
Z9 14
U1 0
U2 6
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 1098-0121
J9 PHYS REV B
JI Phys. Rev. B
PD OCT 28
PY 2010
VL 82
IS 13
AR 134124
DI 10.1103/PhysRevB.82.134124
PG 9
WC Physics, Condensed Matter
SC Physics
GA 672HL
UT WOS:000283573500004
ER
PT J
AU Zhou, HD
Barlas, Y
Wiebe, CR
Qiu, Y
Copley, JRD
Gardner, JS
AF Zhou, H. D.
Barlas, Y.
Wiebe, C. R.
Qiu, Y.
Copley, J. R. D.
Gardner, J. S.
TI Inter- and intratrimer excitations in the multiferroic Ba3NbFe3Si2O14
SO PHYSICAL REVIEW B
LA English
DT Article
ID LATTICE; ANTIFERROMAGNET; DISORDER; ORDER
AB Elastic and inelastic neutron-scattering experiments have been performed on single crystals of the multiferroic Ba3NbFe3Si2O14. It is found that the organization of the spin clusters into true long-range ordered states occurs by the following process: (i) by 60 K, there is evidence for short-range ordered triangular Fe clusters of spins, (ii) below 40 K, the clusters begin to form long-range ordered structures as a spin-wave spectrum develops, (iii) at T-N=26 K, the sample exhibits coexisting long-range and short-range ordered structures, and (iv) by T=1.5 K, a long-range ordered structure with a well-defined spin-wave spectrum develops. The spin-wave excitation can be described by a Heisenberg Hamiltonian within a distorted triangular lattice including both the intratrimer and intertrimer interactions. Physical property measurements showing anomalies near T=40 K can now be adequately explained as being due to scattering from low-energy spin fluctuations.
C1 [Zhou, H. D.; Barlas, Y.; Wiebe, C. R.] Florida State Univ, Natl High Magnet Field Lab, Tallahassee, FL 32306 USA.
[Wiebe, C. R.] Univ Winnipeg, Dept Chem, Winnipeg, MB R3B 2E9, Canada.
[Qiu, Y.; Copley, J. R. D.; Gardner, J. S.] NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Qiu, Y.] Univ Maryland, Dept Mat Sci & Engn, College Pk, MD 20742 USA.
[Gardner, J. S.] Indiana Univ, Bloomington, IN 47408 USA.
RP Zhou, HD (reprint author), Florida State Univ, Natl High Magnet Field Lab, Tallahassee, FL 32306 USA.
EM zhou@magnet.fsu.edu
RI Gardner, Jason/A-1532-2013; Zhou, Haidong/O-4373-2016
FU NSF [DMR-0654118, DMR-0454672, DMR-0944772]
FX This work utilized facilities supported in part by the NSF through the
Cooperative Agreements No. DMR-0654118, DMR-0454672, and DMR-0944772.
NR 22
TC 9
Z9 9
U1 1
U2 6
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 1098-0121
J9 PHYS REV B
JI Phys. Rev. B
PD OCT 28
PY 2010
VL 82
IS 13
AR 132408
DI 10.1103/PhysRevB.82.132408
PG 4
WC Physics, Condensed Matter
SC Physics
GA 672HL
UT WOS:000283573500002
ER
PT J
AU Denig, W
Cooke, D
Furgeson, D
AF Denig, William
Cooke, David
Furgeson, Dale
TI Spacecraft Charging and Mitigation
SO SPACE WEATHER-THE INTERNATIONAL JOURNAL OF RESEARCH AND APPLICATIONS
LA English
DT Article
C1 [Denig, William] NOAA, Solar & Terr Phys Div, Natl Geophys Data Ctr, Boulder, CO USA.
[Cooke, David] Hanscom AFB, AFRL Space Weather Ctr Excellence, Bedford, MA USA.
[Furgeson, Dale] AFRL, Battlespace Environm Div, Albuquerque, NM USA.
RP Denig, W (reprint author), NOAA, Solar & Terr Phys Div, Natl Geophys Data Ctr, Boulder, CO USA.
EM william.denig@noaa.gov
NR 0
TC 0
Z9 0
U1 0
U2 1
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 1542-7390
J9 SPACE WEATHER
JI Space Weather
PD OCT 28
PY 2010
VL 8
AR S10007
DI 10.1029/2010SW000632
PG 2
WC Astronomy & Astrophysics; Geochemistry & Geophysics; Meteorology &
Atmospheric Sciences
SC Astronomy & Astrophysics; Geochemistry & Geophysics; Meteorology &
Atmospheric Sciences
GA 674UD
UT WOS:000283774600001
ER
PT J
AU Senff, CJ
Alvarez, RJ
Hardesty, RM
Banta, RM
Langford, AO
AF Senff, C. J.
Alvarez, R. J., II
Hardesty, R. M.
Banta, R. M.
Langford, A. O.
TI Airborne lidar measurements of ozone flux downwind of Houston and Dallas
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID POWER-PLANT PLUMES; 1995 SOUTHERN OXIDANTS; STABLE BOUNDARY-LAYER;
LOW-LEVEL JET; TEXAS; NOX
AB We use airborne lidar measurements of ozone collected during the Texas Air Quality Study (TexAQS) 2000 and TexAQS 2006 field campaigns to compute the horizontal flux of ozone downwind of the Houston and Dallas/Fort Worth metropolitan areas. Fluxes are computed for each aircraft transect by integrating excess ozone (plume ozone minus background ozone) in the urban plumes and multiplying the result by the horizontal wind speed provided by radar wind profilers. In addition, we use the lidar data to estimate ozone production rates and ozone enhancements in the Houston and Dallas/Fort Worth plumes. We found that the average horizontal flux of ozone emanating from the Houston area based on data from six research flights was 3.2 . 10(26) molecules per second. This was significantly higher than the flux measured downwind of Dallas/Fort Worth during a single flight. The Houston fluxes exhibited a strong dependence on wind direction. Under southerly or northerly flow, ozone fluxes were about twice as large as under westerly or easterly flow conditions. We estimate that a day's worth of export of ozone from the Houston area could raise regional background ozone by about 10 ppbv over a 40,000 km(2) area. This has important ramifications for air quality in communities downwind of Houston as it could raise background ozone levels enough that regions with little or no local pollution sources of their own may violate the federally mandated ozone standard.
C1 [Senff, C. J.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Senff, C. J.; Alvarez, R. J., II; Hardesty, R. M.; Banta, R. M.; Langford, A. O.] NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA.
RP Senff, CJ (reprint author), Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
EM christoph.senff@noaa.gov
RI Langford, Andrew/D-2323-2009; Hardesty, Robert/H-9844-2013; Senff,
Christoph/I-2592-2013; Alvarez, Raul/I-4879-2013; Banta,
Robert/B-8361-2008; Manager, CSD Publications/B-2789-2015
OI Langford, Andrew/0000-0002-2932-7061;
FU NOAA Health of the Atmosphere program; Texas Commission on Environmental
Quality [582-8-86246]; Flight crews of the Dynamic Aviation [DC-3]; NOAA
Twin Otter research aircraft
FX We thank Ann Weickmann, Scott Sandberg, Richard Marchbanks, Dan Law,
Alan Brewer, Dave Merritt, and Janet Machol for their help with the
airborne ozone lidar instruments; Lisa Darby, Joanne George, and Brandi
McCarty for assistance with the analysis of data from the TexAQS 2000
and TexAQS 2006 experiments; the staff of the NOAA/ESRL/Physical
Sciences Division and Sonoma Tech, Inc. for providing the radar wind
profiler data; David Sullivan for making available the 5 min CAMS
surface ozone data; and Michael Trainer and Greg Frost for helpful
discussions. We acknowledge support from the NOAA Health of the
Atmosphere program, the Texas Commission on Environmental Quality (grant
582-8-86246), and the flight crews of the Dynamic Aviation DC-3 and NOAA
Twin Otter research aircraft.
NR 33
TC 6
Z9 6
U1 2
U2 17
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-897X
EI 2169-8996
J9 J GEOPHYS RES-ATMOS
JI J. Geophys. Res.-Atmos.
PD OCT 27
PY 2010
VL 115
AR D20307
DI 10.1029/2009JD013689
PG 13
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 674MK
UT WOS:000283749100003
ER
PT J
AU Tyssoy, HN
Stadsnes, J
Sorbo, M
Mertens, CJ
Evans, DS
AF Tyssoy, H. Nesse
Stadsnes, J.
Sorbo, M.
Mertens, C. J.
Evans, D. S.
TI Changes in upper mesospheric and lower thermospheric temperatures caused
by energetic particle precipitation
SO JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
LA English
DT Article
ID SOLAR PROTON EVENTS; ATMOSPHERE; JOULE; BUDGET; OZONE
AB A statistical evaluation on the upper mesospheric and lower thermospheric temperature effects caused by energetic particle precipitation is performed on the basis of data from the Thermosphere Ionosphere Mesosphere Energetics and Dynamics (TIMED) and NOAA 15, 16, and 17 satellites. By combining particle measurement from the medium energy proton and electron detectors (MEPED) on board the NOAA satellites, maps of the global particle precipitation can be obtained close in time to the SABER (Sounding of the Atmosphere using Broadband Emission Radiometry) temperature retrieval. Using large data sets, sorted by season, local time, and geomagnetic latitude, we investigated whether there are significant temperature effects in the upper mesosphere and lower thermosphere associated with the energetic particle precipitation. During both May/June and October/November 2003, we found a temperature increase related to particle precipitation at all heights above 100 km. In general, we did not find a consistent immediate temperature modification below 100 km associated with increased particle flux. Considering the temperatures retrieved during the extraordinary large geomagnetic storms in late October 2003, we found a cooling effect associated with energetic particle precipitation.
C1 [Tyssoy, H. Nesse] Royal Norwegian Naval Acad, N-5886 Bergen, Norway.
[Stadsnes, J.; Sorbo, M.] Univ Bergen, Dept Phys & Technol, N-5007 Bergen, Norway.
[Mertens, C. J.] NASA, Langley Res Ctr, Sci Directorate Chem & Dynam Branch, Hampton, VA 23681 USA.
[Evans, D. S.] NOAA, Space Environm Lab, Boulder, CO 80305 USA.
RP Tyssoy, HN (reprint author), Royal Norwegian Naval Acad, Pb 83 Haakonsvern, N-5886 Bergen, Norway.
EM hilde.nesse@ift.uib.no
FU Research Council of Norway [184701]
FX This research was supported by the Research Council of Norway project
184701.
NR 20
TC 2
Z9 2
U1 0
U2 2
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0148-0227
J9 J GEOPHYS RES-SPACE
JI J. Geophys. Res-Space Phys.
PD OCT 26
PY 2010
VL 115
AR A10323
DI 10.1029/2010JA015427
PG 11
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA 674SY
UT WOS:000283771300004
ER
PT J
AU Hammond, MR
Dietsch, H
Pravaz, O
Schurtenberger, P
AF Hammond, Matthew R.
Dietsch, Herve
Pravaz, Olivier
Schurtenberger, Peter
TI Mutual Alignment of Block Copolymer-Magnetic Nanoparticle Composites in
a Magnetic Field
SO MACROMOLECULES
LA English
DT Article
ID DIBLOCK COPOLYMERS; INDUCED ORIENTATION; PHASE; NANOCOMPOSITES;
NANORODS; NANOSTRUCTURE; NANOCRYSTALS; MORPHOLOGY; PARTICLES; POLYMERS
C1 [Hammond, Matthew R.; Dietsch, Herve; Pravaz, Olivier; Schurtenberger, Peter] Univ Fribourg, Adolphe Merkle Inst, CH-1723 Marly 1, Switzerland.
RP Hammond, MR (reprint author), NIST, 100 Bur Dr,MS 8542, Gaithersburg, MD 20899 USA.
EM matthew.hammond@mailaps.org; peter.schurtenberger@fkem1.lu.se
RI Schurtenberger, Peter/K-1777-2013; Dietsch, Herve/J-4848-2016;
OI Schurtenberger, Peter/0000-0002-2790-8831; Merkle Institute,
Adolphe/0000-0002-6220-424X
FU Adolphe Merkle Foundation; European Project; COST [D43]; Office of
Science, Office of Basic Energy Sciences, of the U.S. Department of
Energy [DE-AC02-05CH11231]
FX Financial support was provided by the Adolphe Merkle Foundation, by the
European Project "Nanomodel" within the frame of the FP7 program, and by
COST D43. Alexander Hexemer and Chem; Wang at the Advanced Light Source
(ALS). Lawrence Berkeley National Laboratories, provided technical
assistance. The ALS is supported by the Director, Office of Science,
Office of Basic Energy Sciences, of the U.S. Department of Energy under
Contract DE-AC02-05CH11231. Raffaele Mezzenga and Ronald L. Jones are
gratefully acknowledged for useful discussions.
NR 26
TC 25
Z9 26
U1 2
U2 24
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0024-9297
J9 MACROMOLECULES
JI Macromolecules
PD OCT 26
PY 2010
VL 43
IS 20
BP 8340
EP 8343
DI 10.1021/ma1012896
PG 4
WC Polymer Science
SC Polymer Science
GA 668SD
UT WOS:000283289100004
ER
PT J
AU Shaw, JM
Olsen, M
Lau, JW
Schneider, ML
Silva, TJ
Hellwig, O
Dobisz, E
Terris, BD
AF Shaw, Justin M.
Olsen, Miles
Lau, June W.
Schneider, Michael L.
Silva, T. J.
Hellwig, Olav
Dobisz, Elizabeth
Terris, Bruce D.
TI Intrinsic defects in perpendicularly magnetized multilayer thin films
and nanostructures
SO PHYSICAL REVIEW B
LA English
DT Article
ID PATTERNED MEDIA; ANISOTROPY; RELAXATION; REVERSAL
AB Intrinsic magnetic defects in perpendicularly magnetized nanostructures reduce the predictability of device and developing recording technologies. In addition to a distribution of local anisotropy fields, we show that such defects also exhibit variations in local anisotropy axes. The magnetic defects are identified by the application of in-plane and out-of-plane magnetic fields and magnetic force microscopy imaging. Those defects that control magnetization reversal in arrays of patterned Co/Pd multilayers are highly dependent on applied field orientation. The symmetry of the defects with respect to the applied field direction indicates that the anisotropy consists of a canted axis, deviating from the surface normal. Micromagnetic simulations confirm that variations in anisotropy axis can cause a significant change in reversal field depending on the location and orientation of the defects, consistent with experimental results.
C1 [Shaw, Justin M.; Olsen, Miles; Silva, T. J.] Natl Inst Stand & Technol, Boulder, CO 80305 USA.
[Olsen, Miles; Schneider, Michael L.] Univ Montana, Missoula, MT 59812 USA.
[Lau, June W.] Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
[Hellwig, Olav; Dobisz, Elizabeth; Terris, Bruce D.] Hitachi Global Storage Technol, San Jose, CA 95135 USA.
RP Shaw, JM (reprint author), Natl Inst Stand & Technol, Boulder, CO 80305 USA.
RI Shaw, Justin/C-1845-2008; Lau, June/C-7509-2013; Silva,
Thomas/C-7605-2013
OI Shaw, Justin/0000-0003-2027-1521; Silva, Thomas/0000-0001-8164-9642
FU National Institute of Standards and Technology
FX The authors are grateful to Hans Nembach, Robert McMichael, Stephen
Russek, and Tom Thomson for valuable discussions. This work was
partially supported by the National Institute of Standards and
Technology's Innovation in Measurement Science program.
NR 25
TC 24
Z9 24
U1 0
U2 20
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 1098-0121
J9 PHYS REV B
JI Phys. Rev. B
PD OCT 26
PY 2010
VL 82
IS 14
AR 144437
DI 10.1103/PhysRevB.82.144437
PG 7
WC Physics, Condensed Matter
SC Physics
GA 671GG
UT WOS:000283487900008
ER
PT J
AU Crevoisier, C
Sweeney, C
Gloor, M
Sarmiento, JL
Tans, PP
AF Crevoisier, Cyril
Sweeney, Colm
Gloor, Manuel
Sarmiento, Jorge L.
Tans, Pieter P.
TI Regional US carbon sinks from three-dimensional atmospheric CO2 sampling
SO PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF
AMERICA
LA English
DT Article
DE atmospheric composition; biogeochemistry; carbon cycle; greenhouse gases
ID DIOXIDE EXCHANGE; UNITED-STATES; LAND; REANALYSIS
AB Studies diverge substantially on the actual magnitude of the North American carbon budget. This is due to the lack of appropriate data and also stems from the difficulty to properly model all the details of the flux distribution and transport inside the region of interest. To sidestep these difficulties, we use here a simple budgeting approach to estimate land-atmosphere fluxes across North America by balancing the inflow and outflow of CO2 from the troposphere. We base our study on the unique sampling strategy of atmospheric CO2 vertical profiles over North America from the National Oceanic and Atmospheric Administration/Earth System Research Laboratory aircraft network, from which we infer the three-dimensional CO2 distribution over the continent. We find a moderate sink of 0.5 +/- 0.4 PgCy(-1) for the period 2004-2006 for the coterminous United States, in good agreement with the forest-inventory-based estimate of the first North American State of the Carbon Cycle Report, and averaged climate conditions. We find that the highest uptake occurs in the Midwest and in the Southeast. This partitioning agrees with independent estimates of crop uptake in the Midwest, which proves to be a significant part of the US atmospheric sink, and of secondary forest regrowth in the Southeast. Provided that vertical profile measurements are continued, our study offers an independent means to link regional carbon uptake to climate drivers.
C1 [Crevoisier, Cyril] Ecole Polytech, Meteorol Dynam Lab, Ctr Natl Rech Sci, Inst Pierre Simon Laplace, F-91128 Palaiseau, France.
[Crevoisier, Cyril; Sarmiento, Jorge L.] Princeton Univ, Atmospher & Ocean Sci Program, Princeton, NJ 08544 USA.
[Sweeney, Colm] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Sweeney, Colm; Tans, Pieter P.] NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA.
[Gloor, Manuel] Univ Leeds, Earth & Biosphere Inst, Leeds, W Yorkshire, England.
[Gloor, Manuel] Univ Leeds, Sch Geog, Leeds LS2 9JT, W Yorkshire, England.
RP Crevoisier, C (reprint author), Ecole Polytech, Meteorol Dynam Lab, Ctr Natl Rech Sci, Inst Pierre Simon Laplace, F-91128 Palaiseau, France.
EM cyril.crevoisier@lmd.polytechnique.fr
FU National Oceanic and Atmospheric Administration [NA17RJ2612]; U.S.
Department of Commerce; Carbon Mitigation Initiative; Ford Motor
Company; U.S. Department of Energy's Office of Science (BER) through the
Northeastern Regional Center of the National Institute for Climatic
Change Research
FX This research was funded by the Cooperative Institute for Climate
Science under award NA17RJ2612 from the National Oceanic and Atmospheric
Administration, U.S. Department of Commerce, by the Carbon Mitigation
Initiative, with support provided by the Ford Motor Company, and by the
U.S. Department of Energy's Office of Science (BER) through the
Northeastern Regional Center of the National Institute for Climatic
Change Research. The statements, findings, conclusions, and
recommendations are those of the authors and do not necessarily reflect
the views of the National Oceanic and Atmospheric Administration, or the
U.S. Department of Commerce.
NR 32
TC 36
Z9 36
U1 0
U2 17
PU NATL ACAD SCIENCES
PI WASHINGTON
PA 2101 CONSTITUTION AVE NW, WASHINGTON, DC 20418 USA
SN 0027-8424
J9 P NATL ACAD SCI USA
JI Proc. Natl. Acad. Sci. U. S. A.
PD OCT 26
PY 2010
VL 107
IS 43
BP 18348
EP 18353
DI 10.1073/pnas.0900062107
PG 6
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 673QG
UT WOS:000283677400025
PM 20937899
ER
PT J
AU Solomon, S
Daniel, JS
Sanford, TJ
Murphy, DM
Plattner, GK
Knutti, R
Friedlingstein, P
AF Solomon, Susan
Daniel, John S.
Sanford, Todd J.
Murphy, Daniel M.
Plattner, Gian-Kasper
Knutti, Reto
Friedlingstein, Pierre
TI Persistence of climate changes due to a range of greenhouse gases
SO PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF
AMERICA
LA English
DT Article
DE atmosphere; dynamics; radiation
ID VOLCANIC-ERUPTIONS; ANTHROPOGENIC CO2; ATMOSPHERIC CO2; TIME SCALES;
CYCLE; EMISSIONS; OCEAN
AB Emissions of a broad range of greenhouse gases of varying lifetimes contribute to global climate change. Carbon dioxide displays exceptional persistence that renders its warming nearly irreversible for more than 1,000 y. Here we show that the warming due to non-CO2 greenhouse gases, although not irreversible, persists notably longer than the anthropogenic changes in the greenhouse gas concentrations themselves. We explore why the persistence of warming depends not just on the decay of a given greenhouse gas concentration but also on climate system behavior, particularly the timescales of heat transfer linked to the ocean. For carbon dioxide and methane, nonlinear optical absorption effects also play a smaller but significant role in prolonging the warming. In effect, dampening factors that slow temperature increase during periods of increasing concentration also slow the loss of energy from the Earth's climate system if radiative forcing is reduced. Approaches to climate change mitigation options through reduction of greenhouse gas or aerosol emissions therefore should not be expected to decrease climate change impacts as rapidly as the gas or aerosol lifetime, even for short-lived species; such actions can have their greatest effect if undertaken soon enough to avoid transfer of heat to the deep ocean.
C1 [Solomon, Susan; Daniel, John S.; Sanford, Todd J.; Murphy, Daniel M.] Natl Ocean & Atmospher Adm, Div Chem Sci, Earth Syst Res Lab, Boulder, CO 80305 USA.
[Sanford, Todd J.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80307 USA.
[Plattner, Gian-Kasper] Univ Bern, Climate & Environm Phys Phys Inst, CH-3012 Bern, Switzerland.
[Knutti, Reto] ETH, Inst Atmospher & Climate Sci, CH-8006 Zurich, Switzerland.
[Friedlingstein, Pierre] Univ Versailles St Quentin, CEA Saclay, CNRS, CEA,UMR 1572,Inst Pierre Simon Laplace,Lab Sci Cl, F-91191 Gif Sur Yvette, France.
[Friedlingstein, Pierre] Univ Bristol, QUEST Dept Earth Sci, Bristol BS8 1RJ, Avon, England.
RP Solomon, S (reprint author), Natl Ocean & Atmospher Adm, Div Chem Sci, Earth Syst Res Lab, Boulder, CO 80305 USA.
EM susan.solomon@noaa.gov
RI Daniel, John/D-9324-2011; Murphy, Daniel/J-4357-2012; Knutti,
Reto/B-8763-2008; Friedlingstein, Pierre/H-2700-2014; Plattner,
Gian-Kasper/A-5245-2016; Manager, CSD Publications/B-2789-2015
OI Murphy, Daniel/0000-0002-8091-7235; Knutti, Reto/0000-0001-8303-6700;
Plattner, Gian-Kasper/0000-0002-3765-0045;
NR 39
TC 44
Z9 44
U1 4
U2 46
PU NATL ACAD SCIENCES
PI WASHINGTON
PA 2101 CONSTITUTION AVE NW, WASHINGTON, DC 20418 USA
SN 0027-8424
J9 P NATL ACAD SCI USA
JI Proc. Natl. Acad. Sci. U. S. A.
PD OCT 26
PY 2010
VL 107
IS 43
BP 18354
EP 18359
DI 10.1073/pnas.1006282107
PG 6
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 673QG
UT WOS:000283677400026
PM 20937898
ER
PT J
AU Struve, J
Lorenzen, K
Blanchard, J
Borger, L
Bunnefeld, N
Edwards, C
Hortal, J
MacCall, A
Matthiopoulos, J
Van Moorter, B
Ozgul, A
Royer, F
Singh, N
Yesson, C
Bernard, R
AF Struve, Juliane
Lorenzen, Kai
Blanchard, Julia
Borger, Luca
Bunnefeld, Nils
Edwards, Charles
Hortal, Joaquin
MacCall, Alec
Matthiopoulos, Jason
Van Moorter, Bram
Ozgul, Arpat
Royer, Francois
Singh, Navinder
Yesson, Chris
Bernard, Rodolphe
TI Lost in space? Searching for directions in the spatial modelling of
individuals, populations and species ranges
SO BIOLOGY LETTERS
LA English
DT Editorial Material
DE spatial modelling; dispersal; movement; population dynamics;
biogeography
ID MOVEMENT; ECOLOGY; NICHE
AB The workshop 'Spatial models in animal ecology, management and conservation' held at Silwood Park (UK), 9-11 March 2010, aimed to synthesize recent progress in modelling the spatial dynamics of individuals, populations and species ranges and to provide directions for research. It brought together marine and terrestrial researchers working on spatial models at different levels of organization, using empirical as well as theory-driven approaches. Different approaches, temporal and spatial scales, and practical constraints predominate at different levels of organization and in different environments. However, there are theoretical concepts and specific methods that can fruitfully be transferred across levels and systems, including: habitat suitability characterization, movement rules, and ways of estimating uncertainty.
C1 [Struve, Juliane; Lorenzen, Kai; Blanchard, Julia; Bunnefeld, Nils; Edwards, Charles; Ozgul, Arpat; Singh, Navinder; Bernard, Rodolphe] Univ London Imperial Coll Sci Technol & Med, Dept Life Sci, Ascot SL5 7PY, Berks, England.
[Borger, Luca] Univ Guelph, Dept Integrat Biol, Guelph, ON N1G 2W1, Canada.
[Bunnefeld, Nils] Swedish Univ Agr Sci, Dept Wildlife Fish & Environm Sci, S-90183 Umea, Sweden.
[Hortal, Joaquin] Univ London Imperial Coll Sci Technol & Med, NERC Ctr Populat Biol, Ascot SL5 7PY, Berks, England.
[MacCall, Alec] NOAA, SW Fisheries Sci Ctr, Santa Cruz, CA 95060 USA.
[Matthiopoulos, Jason] Univ St Andrews, Scottish Oceans Inst, St Andrews KY16 8LB, Fife, Scotland.
[Van Moorter, Bram] Norwegian Inst Technol, Dept Biol, N-7491 Trondheim, Norway.
[Royer, Francois] CLS, F-31520 Ramonville St Agne, France.
[Yesson, Chris] Zool Soc London, London NW1 4RY, England.
RP Struve, J (reprint author), Univ London Imperial Coll Sci Technol & Med, Dept Life Sci, Ascot SL5 7PY, Berks, England.
EM j.struve@imperial.ac.uk
RI Singh, Navinder/E-3914-2010; Bunnefeld, Nils/G-1946-2011; Blanchard,
Julia/E-4919-2010; Ozgul, Arpat/K-2032-2012; Borger, Luca/C-6003-2008;
Hortal, Joaquin/A-1531-2008; Matthiopoulos, Jason/N-9808-2013;
OI Blanchard, Julia/0000-0003-0532-4824; Ozgul, Arpat/0000-0001-7477-2642;
Borger, Luca/0000-0001-8763-5997; Hortal, Joaquin/0000-0002-8370-8877;
Bunnefeld, Nils/0000-0002-1349-4463; Yesson, Chris/0000-0002-6731-4229
NR 17
TC 6
Z9 6
U1 2
U2 28
PU ROYAL SOC
PI LONDON
PA 6-9 CARLTON HOUSE TERRACE, LONDON SW1Y 5AG, ENGLAND
SN 1744-9561
EI 1744-957X
J9 BIOL LETTERS
JI Biol. Lett.
PD OCT 23
PY 2010
VL 6
IS 5
BP 575
EP 578
DI 10.1098/rsbl.2010.0338
PG 4
WC Biology; Ecology; Evolutionary Biology
SC Life Sciences & Biomedicine - Other Topics; Environmental Sciences &
Ecology; Evolutionary Biology
GA 649AW
UT WOS:000281739100001
PM 20484232
ER
PT J
AU Bailey, KM
Ciannelli, L
Hunsicker, M
Rindorf, A
Neuenfeldt, S
Mollmann, C
Guichard, F
Huse, G
AF Bailey, Kevin M.
Ciannelli, Lorenzo
Hunsicker, Mary
Rindorf, Anna
Neuenfeldt, Stefan
Moellmann, Christian
Guichard, Frederic
Huse, Geir
TI Comparative analysis of marine ecosystems: workshop on predator-prey
interactions
SO BIOLOGY LETTERS
LA English
DT Editorial Material
DE predator-prey; food webs; scaling; marine ecosystems
AB Climate and human influences on marine ecosystems are largely manifested by changes in predator-prey interactions. It follows that ecosystem-based management of the world's oceans requires a better understanding of food web relationships. An international workshop on predator-prey interactions in marine ecosystems was held at the Oregon State University, Corvallis, OR, USA on 16-18 March 2010. The meeting brought together scientists from diverse fields of expertise including theoretical ecology, animal behaviour, fish and seabird ecology, statistics, fisheries science and ecosystem modelling. The goals of the workshop were to critically examine the methods of scaling-up predator-prey interactions from local observations to systems, the role of shifting ecological processes with scale changes, and the complexity and organizational structure in trophic interactions.
C1 [Bailey, Kevin M.] NOAA, Alaska Fisheries Sci Ctr, Seattle, WA USA.
[Ciannelli, Lorenzo; Hunsicker, Mary] Oregon State Univ, Coll Ocean & Atmospher Sci, Corvallis, OR 97331 USA.
[Rindorf, Anna; Neuenfeldt, Stefan] Tech Univ Denmark, Natl Inst Aquat Resources, Charlottenlund, Denmark.
[Moellmann, Christian] Univ Hamburg, Inst Hydrobiol & Fisheries Sci, Hamburg, Germany.
[Guichard, Frederic] McGill Univ, Dept Biol, Montreal, PQ H3A 1B1, Canada.
[Huse, Geir] Inst Marine Res, N-5024 Bergen, Norway.
RP Bailey, KM (reprint author), NOAA, Alaska Fisheries Sci Ctr, Seattle, WA USA.
EM kevin.bailey@noaa.gov
RI Guichard, Frederic/B-6188-2015; Mollmann, Christian/C-4788-2011;
OI Guichard, Frederic/0000-0002-7369-482X; Mollmann,
Christian/0000-0001-9161-6342
NR 6
TC 7
Z9 7
U1 2
U2 17
PU ROYAL SOC
PI LONDON
PA 6-9 CARLTON HOUSE TERRACE, LONDON SW1Y 5AG, ENGLAND
SN 1744-9561
J9 BIOL LETTERS
JI Biol. Lett.
PD OCT 23
PY 2010
VL 6
IS 5
BP 579
EP 581
DI 10.1098/rsbl.2010.0326
PG 3
WC Biology; Ecology; Evolutionary Biology
SC Life Sciences & Biomedicine - Other Topics; Environmental Sciences &
Ecology; Evolutionary Biology
GA 649AW
UT WOS:000281739100002
PM 20462888
ER
PT J
AU Baker, CS
Steel, D
Choi, Y
Lee, H
Kim, KS
Choi, SK
Ma, YU
Hambleton, C
Psihoyos, L
Brownell, RL
Funahashi, N
AF Baker, C. Scott
Steel, Debbie
Choi, Yeyong
Lee, Hang
Kim, Kyung Seok
Choi, Sung Kyoung
Ma, Yong-Un
Hambleton, Charles
Psihoyos, Louie
Brownell, R. L.
Funahashi, Naoko
TI Genetic evidence of illegal trade in protected whales links Japan with
the US and South Korea
SO BIOLOGY LETTERS
LA English
DT Article
DE IWC; whaling; CITES; infraction
ID PRODUCTS; WILDLIFE; MARKETS
AB We report on genetic identification of 'whale meat' purchased in sushi restaurants in Los Angeles, CA (USA) in October 2009 and in Seoul, South Korea in June and September 2009. Phylogenetic analyses of mtDNA cytochrome b sequences confirmed that the products included three species of whale currently killed in the controversial scientific whaling programme of Japan, but which are protected from international trade: the fin, sei and Antarctic minke. The DNA profile of the fin whale sold in Seoul established a match to products purchased previously in Japan in September 2007, confirming unauthorized trade between these two countries. Following species identification, these products were handed over to the appropriate national or local authorities for further investigation. The illegal trade of products from protected species of whales, presumably taken under a national permit for scientific research, is a timely reminder of the need for independent, transparent and robust monitoring of any future whaling.
C1 [Baker, C. Scott; Steel, Debbie] Oregon State Univ, Marine Mammal Inst, Newport, OR 97365 USA.
[Baker, C. Scott; Steel, Debbie] Oregon State Univ, Dept Fisheries & Wildlife, Newport, OR 97365 USA.
[Choi, Yeyong] Korean Federat Environm Movements, Ocean Comm, Seoul, South Korea.
[Lee, Hang; Kim, Kyung Seok; Choi, Sung Kyoung] Seoul Natl Univ, Conservat & Genome Resource Bank Korean Wildlife, Seoul, South Korea.
[Ma, Yong-Un] Korean Federat Environm Movements, Nat Conservat Comm, Seoul, South Korea.
[Hambleton, Charles; Psihoyos, Louie] Ocean Preservat Soc, Boulder, CO USA.
[Brownell, R. L.] Natl Marine Fisheries Serv, SW Fisheries Ctr, Pacific Grove, CA USA.
[Funahashi, Naoko] Int Fund Anim Welf, Tokyo, Japan.
RP Baker, CS (reprint author), Oregon State Univ, Marine Mammal Inst, Newport, OR 97365 USA.
EM scott.baker@oregonstate.edu
RI Lee, Hang/A-7516-2011
OI Lee, Hang/0000-0003-0264-6289
FU Pacific Life Foundation; US National Marine Fisheries Service
FX Funding in support of laboratory analyses was provided by the Pacific
Life Foundation and the US National Marine Fisheries Service.
NR 13
TC 14
Z9 14
U1 5
U2 39
PU ROYAL SOC
PI LONDON
PA 6-9 CARLTON HOUSE TERRACE, LONDON SW1Y 5AG, ENGLAND
SN 1744-9561
J9 BIOL LETTERS
JI Biol. Lett.
PD OCT 23
PY 2010
VL 6
IS 5
BP 647
EP 650
DI 10.1098/rsbl.2010.0239
PG 4
WC Biology; Ecology; Evolutionary Biology
SC Life Sciences & Biomedicine - Other Topics; Environmental Sciences &
Ecology; Evolutionary Biology
GA 649AW
UT WOS:000281739100021
PM 20392716
ER
PT J
AU Guan, B
Molotch, NP
Waliser, DE
Fetzer, EJ
Neiman, PJ
AF Guan, Bin
Molotch, Noah P.
Waliser, Duane E.
Fetzer, Eric J.
Neiman, Paul J.
TI Extreme snowfall events linked to atmospheric rivers and surface air
temperature via satellite measurements
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID DISTRIBUTED SNOWMELT MODEL; RIO-GRANDE HEADWATERS; WATER EQUIVALENT;
NORTH-AMERICA; SIERRA-NEVADA; COVER DATA; PRECIPITATION; CALIFORNIA;
MOUNTAINS
AB Narrow bands of strong atmospheric water vapor transport, referred to as "atmospheric rivers" (ARs), are responsible for the majority of wintertime extreme precipitation events with important contributions to the seasonal water balance. We investigate relationships between snow water equivalent (SWE), precipitation, and surface air temperature (SAT) across the Sierra Nevada for 45 wintertime AR events. Analysis of assimilated and in situ data for water years 2004-2010 indicates that ARs on average generate similar to 4 times daily SWE accumulation of non-AR storms. In addition, AR events contributed similar to 30-40% of total seasonal SWE accumulation in most years, with the contribution dominated by just 1-2 extreme events in some cases. In situ and remotely sensed observations show that SWE changes associated with ARs are closely related to SAT. These results reveal the previously unexplored significance of ARs with regard to the snowpack and associated sensitivities of AR precipitation to SAT. Citation: Guan, B., N. P. Molotch, D. E. Waliser, E. J. Fetzer, and P. J. Neiman (2010), Extreme snowfall events linked to atmospheric rivers and surface air temperature via satellite measurements, Geophys. Res. Lett., 37, L20401, doi:10.1029/2010GL044696.
C1 [Guan, Bin; Molotch, Noah P.; Waliser, Duane E.; Fetzer, Eric J.] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA.
[Molotch, Noah P.] Univ Colorado, Dept Geog, Boulder, CO 80309 USA.
[Molotch, Noah P.] Univ Colorado, Inst Arctic & Alpine Res, Boulder, CO 80309 USA.
[Neiman, Paul J.] NOAA, Earth Syst Res Lab, Div Phys Sci, Boulder, CO 80305 USA.
RP Guan, B (reprint author), CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91109 USA.
EM bin.guan@jpl.nasa.gov
RI Guan, Bin/F-6735-2010; Molotch, Noah/C-8576-2009
FU NSF [EAR071160]; NASA [NNX08AH18G]; National Aeronautics and Space
Administration
FX This research was supported by NSF EAR071160 and by NASA grant
NNX08AH18G. B. Tian, M. Ralph, G. Wick, M. Dettinger, K. Weickmann and
J. Kim are acknowledged for useful discussions and technical support.
Data used in this study have been obtained online from NSIDC, CA DWR,
NASA and ECMWF. DEW's and BG's contribution, and part of NPM's
contribution, to this study was carried out on behalf of the Jet
Propulsion Laboratory, California Institute of Technology, under a
contract with the National Aeronautics and Space Administration.
NR 28
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PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
EI 1944-8007
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD OCT 23
PY 2010
VL 37
AR L20401
DI 10.1029/2010GL044696
PG 6
WC Geosciences, Multidisciplinary
SC Geology
GA 704YK
UT WOS:000286091800001
ER
PT J
AU Ray, GC
Overland, JE
Hufford, GL
AF Ray, G. Carleton
Overland, James E.
Hufford, Gary L.
TI Seascape as an organizing principle for evaluating walrus and seal
sea-ice habitat in Beringia
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
AB The term "seascape", as used here, relates the natural history of ice-dependent pinnipeds to their sea-ice environments at different spatial scales, following concepts of landscape ecology. Habitats are characterized by heterogeneous but repeatable structures of sea ice. As an example, multiple mesoscale (3-50 km) seascapes present conditions for different ecological preferences of five Beringian ice-dependent pinnipeds, as observed during 2006-2009 winter-spring icebreaker cruises. Seascape partitioning concepts are important for understanding and projecting species' responses to change under climate-change scenarios. Citation: Ray, G. C., J. E. Overland, and G. L. Hufford (2010), Seascape as an organizing principle for evaluating walrus and seal sea-ice habitat in Beringia, Geophys. Res. Lett., 37, L20504, doi:10.1029/2010GL044452.
C1 [Ray, G. Carleton] Univ Virginia, Dept Environm Sci, Charlottesville, VA 22904 USA.
[Overland, James E.] NOAA, Pacific Marine Environm Lab, Seattle, WA 98115 USA.
[Hufford, Gary L.] Natl Weather Serv, NOAA, Anchorage, AK 99513 USA.
RP Ray, GC (reprint author), Univ Virginia, Dept Environm Sci, 291 McCormick Rd, Charlottesville, VA 22904 USA.
EM cr@vrginia.edu; james.e.overland@noaa.gov; gary.hufford@noaa.gov
FU NOAA's National Weather Service-Alaska Region; U.S. Marine Mammal
Commission; University of Virginia
FX We thank the Captains, Chief Scientists, crews, and technical personnel
for assistance recording pinnipeds from the icebreaker USGC Healy during
2006-2009 winter-spring cruises. Special thanks are due to Kathy Kuletz
and Elizabeth Labunski of the Fish and Wildlife Service, Alaska, for
marine mammal observations and photographs, and also to Michael Cameron
and colleagues of NOAA's National Marine Mammal Laboratory and Chadwick
Jay and Anthony Fischback of the U.S. Geological Survey for their
observations. Thanks also to anonymous reviewers for their constructive
suggestions. Steve Roberts of the National Center for Atmospheric
Research, Boulder, Colorado, provided ship positions and access to
satellite imagery aboard the Healy. Robert L. Smith, Charlottesville,
Virginia, formatted the illustrations. NOAA's National Weather
Service-Alaska Region, the U.S. Marine Mammal Commission, and the Global
Biodiversity Fund of the University of Virginia provided support for
this paper. PMEL contribution no. 3614.
NR 23
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PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD OCT 23
PY 2010
VL 37
AR L20504
DI 10.1029/2010GL044452
PG 6
WC Geosciences, Multidisciplinary
SC Geology
GA 704YK
UT WOS:000286091800004
ER
PT J
AU Gettelman, A
Hegglin, MI
Son, SW
Kim, J
Fujiwara, M
Birner, T
Kremser, S
Rex, M
Anel, JA
Akiyoshi, H
Austin, J
Bekki, S
Braesike, P
Bruhl, C
Butchart, N
Chipperfield, M
Dameris, M
Dhomse, S
Garny, H
Hardiman, SC
Jockel, P
Kinnison, DE
Lamarque, JF
Mancini, E
Marchand, M
Michou, M
Morgenstern, O
Pawson, S
Pitari, G
Plummer, D
Pyle, JA
Rozanov, E
Scinocca, J
Shepherd, TG
Shibata, K
Smale, D
Teyssedre, H
Tian, W
AF Gettelman, A.
Hegglin, M. I.
Son, S. -W.
Kim, J.
Fujiwara, M.
Birner, T.
Kremser, S.
Rex, M.
Anel, J. A.
Akiyoshi, H.
Austin, J.
Bekki, S.
Braesike, P.
Bruehl, C.
Butchart, N.
Chipperfield, M.
Dameris, M.
Dhomse, S.
Garny, H.
Hardiman, S. C.
Joeckel, P.
Kinnison, D. E.
Lamarque, J. F.
Mancini, E.
Marchand, M.
Michou, M.
Morgenstern, O.
Pawson, S.
Pitari, G.
Plummer, D.
Pyle, J. A.
Rozanov, E.
Scinocca, J.
Shepherd, T. G.
Shibata, K.
Smale, D.
Teyssedre, H.
Tian, W.
TI Multimodel assessment of the upper troposphere and lower stratosphere:
Tropics and global trends
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID CHEMISTRY-CLIMATE MODEL; GENERAL-CIRCULATION MODEL; MIDDLE ATMOSPHERE;
TROPOPAUSE LAYER; TECHNICAL NOTE; ERA-40 REANALYSIS; ANNUAL CYCLE;
WATER-VAPOR; OZONE; TRANSPORT
AB The performance of 18 coupled Chemistry Climate Models (CCMs) in the Tropical Tropopause Layer (TTL) is evaluated using qualitative and quantitative diagnostics. Trends in tropopause quantities in the tropics and the extratropical Upper Troposphere and Lower Stratosphere (UTLS) are analyzed. A quantitative grading methodology for evaluating CCMs is extended to include variability and used to develop four different grades for tropical tropopause temperature and pressure, water vapor and ozone. Four of the 18 models and the multi-model mean meet quantitative and qualitative standards for reproducing key processes in the TTL. Several diagnostics are performed on a subset of the models analyzing the Tropopause Inversion Layer (TIL), Lagrangian cold point and TTL transit time. Historical decreases in tropical tropopause pressure and decreases in water vapor are simulated, lending confidence to future projections. The models simulate continued decreases in tropopause pressure in the 21st century, along with similar to 1K increases per century in cold point tropopause temperature and 0.5-1 ppmv per century increases in water vapor above the tropical tropopause. TTL water vapor increases below the cold point. In two models, these trends are associated with 35% increases in TTL cloud fraction. These changes indicate significant perturbations to TTL processes, specifically to deep convective heating and humidity transport. Ozone in the extratropical lowermost stratosphere has significant and hemispheric asymmetric trends. O-3 is projected to increase by nearly 30% due to ozone recovery in the Southern Hemisphere (SH) and due to enhancements in the stratospheric circulation. These UTLS ozone trends may have significant effects in the TTL and the troposphere.
C1 [Gettelman, A.; Kinnison, D. E.; Lamarque, J. F.] Natl Ctr Atmospher Res, Div Atmospher Chem, Boulder, CO 80305 USA.
[Hegglin, M. I.; Shepherd, T. G.] Univ Toronto, Dept Phys, Toronto, ON M5S 1A7, Canada.
[Son, S. -W.; Kim, J.] McGill Univ, Dept Atmospher & Ocean Sci, Montreal, PQ H3A 2T5, Canada.
[Fujiwara, M.] Hokkaido Univ, Fac Environm Earth Sci, Sapporo, Hokkaido 0600809, Japan.
[Birner, T.] Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA.
[Kremser, S.] Free Univ Berlin, Inst Meteorol, D-14195 Berlin, Germany.
[Rex, M.] Alfred Wegener Inst Polar & Marine Res, D-14473 Potsdam, Germany.
[Anel, J. A.] Univ Vigo, Environm Phys Lab, E-32004 Orense, Spain.
[Akiyoshi, H.] Natl Inst Environm Studies, Tsukuba, Ibaraki 3058506, Japan.
[Austin, J.] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA.
[Bekki, S.; Marchand, M.] CNRS INSU, UMPC, UVSQ, Inst Pierre Simone Laplace,LATMOS, F-75252 Paris, France.
[Braesike, P.; Pyle, J. A.] Univ Cambridge, Dept Chem, Cambridge CB2 1TN, England.
[Bruehl, C.; Joeckel, P.] Max Planck Inst Chem, D-55020 Mainz, Germany.
[Butchart, N.; Hardiman, S. C.] Met Off, Exeter EX1 3PB, Devon, England.
[Chipperfield, M.; Dhomse, S.; Tian, W.] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England.
[Dameris, M.; Garny, H.] Deutsch Zentrum Luft & Raumfahrt, Inst Phys Atmosphare, D-82234 Oberpfaffenhofen, Wessling, Germany.
[Mancini, E.; Pitari, G.] Univ Aquila, Dipartimento Fis, I-67100 Laquila, Italy.
[Michou, M.; Teyssedre, H.] Meteo France, CNRS, GAME CNRM, F-31400 Toulouse, France.
[Morgenstern, O.; Smale, D.] Natl Inst Water & Atmosphere, Lauder, New Zealand.
[Pawson, S.] NASA, Goddard Space Flight Ctr, Global Modelling & Assimilat Off, Greenbelt, MD 20771 USA.
[Plummer, D.] Environm Canada, Toronto, ON M3H 5T4, Canada.
[Rozanov, E.] Phys Meteorol Observ Davos, CH-7620 Davos, Switzerland.
[Scinocca, J.] Canadian Ctr Climate Modeling & Anal, Victoria, BC V8P 5C2, Canada.
[Shibata, K.] Meteorol Res Inst, Tsukuba, Ibaraki 3050052, Japan.
RP Gettelman, A (reprint author), Natl Ctr Atmospher Res, Div Atmospher Chem, 1850 Table Mesa Dr, Boulder, CO 80305 USA.
EM andrew@ucar.edu
RI Pitari, Giovanni/O-7458-2016; Birner, Thomas/A-2108-2008; Rex,
Markus/A-6054-2009; Jockel, Patrick/C-3687-2009; Dhomse,
Sandip/C-8198-2011; Rozanov, Eugene/A-9857-2012; Fujiwara,
Masatomo/F-7852-2012; Chipperfield, Martyn/H-6359-2013; Son, Seok-Woo
/A-8797-2013; Lamarque, Jean-Francois/L-2313-2014; bekki,
slimane/J-7221-2015; Nakamura, Tetsu/M-7914-2015; Pawson,
Steven/I-1865-2014; Hegglin, Michaela/D-7528-2017;
OI Pitari, Giovanni/0000-0001-7051-9578; Birner,
Thomas/0000-0002-2966-3428; Rex, Markus/0000-0001-7847-8221; Jockel,
Patrick/0000-0002-8964-1394; Dhomse, Sandip/0000-0003-3854-5383;
Rozanov, Eugene/0000-0003-0479-4488; Chipperfield,
Martyn/0000-0002-6803-4149; Lamarque, Jean-Francois/0000-0002-4225-5074;
bekki, slimane/0000-0002-5538-0800; Nakamura, Tetsu/0000-0002-2056-7392;
Pawson, Steven/0000-0003-0200-717X; Hegglin,
Michaela/0000-0003-2820-9044; Mancini, Eva/0000-0001-7071-0292;
Morgenstern, Olaf/0000-0002-9967-9740; /0000-0002-3573-7083
FU United States National Science Foundation; DECC/Defra [GA01101];
Ministry of the Environment of Japan [A-071]; European Union [SCOUT-O3]
FX The National Center for Atmospheric Research is sponsored by the United
States National Science Foundation. The work of N. Butchart and S.
Hardiman was supported by the Joint DECC and Defra Integrated Climate
Programme - DECC/Defra (GA01101). We acknowledge the modeling groups for
making their simulations available for this analysis, the
Chemistry-Climate Model Validation (CCMVal) Activity for WCRP's (World
Climate Research Programme) SPARC (Stratospheric Processes and their
Role in Climate) project for organizing and coordinating the model data
analysis activity, and the British Atmospheric Data Center (BADC) for
collecting and archiving the CCMVal model output. CCSRNIES research was
supported by the Global Environmental Research Fund of the Ministry of
the Environment of Japan (A-071). CCSRNIES and MRI simulations were made
with the supercomputer at the National Institute for Environmental
Studies, Japan. European contributions were supported by the European
Union Integrated Project SCOUT-O3. WACCM-hires simulations were
performed at the Centro de Supercomputacion de Galicia. Thanks go to
Darryn Waugh for the use of code for producing tables.
NR 76
TC 88
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U1 3
U2 48
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-897X
EI 2169-8996
J9 J GEOPHYS RES-ATMOS
JI J. Geophys. Res.-Atmos.
PD OCT 23
PY 2010
VL 115
AR D00M08
DI 10.1029/2009JD013638
PG 22
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 671XH
UT WOS:000283546600002
ER
PT J
AU Hegglin, MI
Gettelman, A
Hoor, P
Krichevsky, R
Manney, GL
Pan, LL
Son, SW
Stiller, G
Tilmes, S
Walker, KA
Eyring, V
Shepherd, TG
Waugh, D
Akiyoshi, H
Anel, JA
Austin, J
Baumgaertner, A
Bekki, S
Braesicke, P
Bruhl, C
Butchart, N
Chipperfield, M
Dameris, M
Dhomse, S
Frith, S
Garny, H
Hardiman, SC
Jockel, P
Kinnison, DE
Lamarque, JF
Mancini, E
Michou, M
Morgenstern, O
Nakamura, T
Olivie, D
Pawson, S
Pitari, G
Plummer, DA
Pyle, JA
Rozanov, E
Scinocca, JF
Shibata, K
Smale, D
Teyssedre, H
Tian, W
Yamashita, Y
AF Hegglin, M. I.
Gettelman, A.
Hoor, P.
Krichevsky, R.
Manney, G. L.
Pan, L. L.
Son, S. -W.
Stiller, G.
Tilmes, S.
Walker, K. A.
Eyring, V.
Shepherd, T. G.
Waugh, D.
Akiyoshi, H.
Anel, J. A.
Austin, J.
Baumgaertner, A.
Bekki, S.
Braesicke, P.
Bruehl, C.
Butchart, N.
Chipperfield, M.
Dameris, M.
Dhomse, S.
Frith, S.
Garny, H.
Hardiman, S. C.
Joeckel, P.
Kinnison, D. E.
Lamarque, J. F.
Mancini, E.
Michou, M.
Morgenstern, O.
Nakamura, T.
Olivie, D.
Pawson, S.
Pitari, G.
Plummer, D. A.
Pyle, J. A.
Rozanov, E.
Scinocca, J. F.
Shibata, K.
Smale, D.
Teyssedre, H.
Tian, W.
Yamashita, Y.
TI Multimodel assessment of the upper troposphere and lower stratosphere:
Extratropics
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID CHEMISTRY-CLIMATE MODEL; QUANTITATIVE PERFORMANCE METRICS; IN-SITU
MEASUREMENTS; IMK-IAA PROCESSOR; MIDDLE ATMOSPHERE; WATER-VAPOR;
VERTICAL-RESOLUTION; GENERAL-CIRCULATION; TROPOPAUSE REGION; TRANSPORT
MODELS
AB A multimodel assessment of the performance of chemistry-climate models (CCMs) in the extratropical upper troposphere/lower stratosphere (UTLS) is conducted for the first time. Process-oriented diagnostics are used to validate dynamical and transport characteristics of 18 CCMs using meteorological analyses and aircraft and satellite observations. The main dynamical and chemical climatological characteristics of the extratropical UTLS are generally well represented by the models, despite the limited horizontal and vertical resolution. The seasonal cycle of lowermost stratospheric mass is realistic, however with a wide spread in its mean value. A tropopause inversion layer is present in most models, although the maximum in static stability is located too high above the tropopause and is somewhat too weak, as expected from limited model resolution. Similar comments apply to the extratropical tropopause transition layer. The seasonality in lower stratospheric chemical tracers is consistent with the seasonality in the Brewer-Dobson circulation. Both vertical and meridional tracer gradients are of similar strength to those found in observations. Models that perform less well tend to use a semi-Lagrangian transport scheme and/or have a very low resolution. Two models, and the multimodel mean, score consistently well on all diagnostics, while seven other models score well on all diagnostics except the seasonal cycle of water vapor. Only four of the models are consistently below average. The lack of tropospheric chemistry in most models limits their evaluation in the upper troposphere. Finally, the UTLS is relatively sparsely sampled by observations, limiting our ability to quantitatively evaluate many aspects of model performance.
C1 [Hegglin, M. I.; Krichevsky, R.; Walker, K. A.; Shepherd, T. G.] Univ Toronto, Dept Phys, Toronto, ON M5S 1A7, Canada.
[Akiyoshi, H.; Nakamura, T.; Yamashita, Y.] Natl Inst Environm Studies, Tsukuba, Ibaraki 3058506, Japan.
[Anel, J. A.] Univ Vigo, Environm Phys Lab, E-32004 Orense, Spain.
[Austin, J.] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA.
[Hoor, P.; Baumgaertner, A.; Bruehl, C.; Joeckel, P.] Max Planck Inst Chem, D-55020 Mainz, Germany.
[Bekki, S.] CNRS INSU, UMPC, UVSQ, Inst Pierre Simone Laplace,LATMOS, F-75252 Paris, France.
[Braesicke, P.; Morgenstern, O.; Pyle, J. A.] Univ Cambridge, Dept Chem, Cambridge CB2 1TN, England.
[Butchart, N.; Hardiman, S. C.] Met Off, Exeter EX1 3PB, Devon, England.
[Chipperfield, M.; Dhomse, S.; Tian, W.] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England.
[Eyring, V.; Dameris, M.; Garny, H.; Joeckel, P.] Deutsch Zentrum Luft & Raumfahrt, Inst Phys Atmosphare, D-82234 Oberpfaffenhofen, Wessling, Germany.
[Frith, S.; Pawson, S.] NASA, Goddard Space Flight Ctr, Global Modelling & Assimilat Off, Greenbelt, MD 20771 USA.
[Gettelman, A.; Pan, L. L.; Tilmes, S.; Kinnison, D. E.; Lamarque, J. F.] Natl Ctr Atmospher Res, Div Atmospher Chem, Boulder, CO 80305 USA.
[Mancini, E.; Pitari, G.] Univ Aquila, Dipartimento Fis, I-67100 Laquila, Italy.
[Manney, G. L.] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA.
[Michou, M.; Olivie, D.; Teyssedre, H.] Meteo France, CNRS, GAME CNRM, F-31400 Toulouse, France.
[Morgenstern, O.; Smale, D.] Natl Inst Water & Atmospher Res, Lauder, New Zealand.
[Plummer, D. A.] Environm Canada, Toronto, ON M3H 5T4, Canada.
[Rozanov, E.] Phys Meteorol Observ Davos, CH-7260 Davos, Switzerland.
[Scinocca, J. F.] Canadian Ctr Climate Modelling & Anal, Victoria, BC V8P 5C2, Canada.
[Shibata, K.] Meteorol Res Inst, Tsukuba, Ibaraki 3050052, Japan.
[Son, S. -W.] McGill Univ, Dept Atmospher & Ocean Sci, Montreal, PQ H3A 2T5, Canada.
[Stiller, G.] Karlsruhe Inst Technol, Inst Meteorol & Climate Res, D-76021 Karlsruhe, Germany.
[Waugh, D.] Johns Hopkins Univ, Dept Earth & Planetary Sci, Baltimore, MD 21218 USA.
[Manney, G. L.] New Mexico Inst Min & Technol, Socorro, NM 87801 USA.
[Walker, K. A.] Univ Waterloo, Dept Chem, Waterloo, ON N2L 3G1, Canada.
[Rozanov, E.] ETH, Inst Atmospher & Climate Sci, Zurich, Switzerland.
RP Hegglin, MI (reprint author), Univ Toronto, Dept Phys, 60 St George St, Toronto, ON M5S 1A7, Canada.
EM michaela@atmosp.physics.utoronto.ca
RI hoor, peter/G-5421-2010; Jockel, Patrick/C-3687-2009; Dhomse,
Sandip/C-8198-2011; Rozanov, Eugene/A-9857-2012; Stiller,
Gabriele/A-7340-2013; Baumgaertner, Andreas/C-4830-2011; Chipperfield,
Martyn/H-6359-2013; Son, Seok-Woo /A-8797-2013; Lamarque,
Jean-Francois/L-2313-2014; Pan, Laura/A-9296-2008; bekki,
slimane/J-7221-2015; Nakamura, Tetsu/M-7914-2015; Braesicke,
Peter/D-8330-2016; Pawson, Steven/I-1865-2014; Pitari,
Giovanni/O-7458-2016; Eyring, Veronika/O-9999-2016; Hegglin,
Michaela/D-7528-2017;
OI hoor, peter/0000-0001-6582-6864; Jockel, Patrick/0000-0002-8964-1394;
Dhomse, Sandip/0000-0003-3854-5383; Rozanov, Eugene/0000-0003-0479-4488;
Stiller, Gabriele/0000-0003-2883-6873; Baumgaertner,
Andreas/0000-0002-4740-0701; Chipperfield, Martyn/0000-0002-6803-4149;
Lamarque, Jean-Francois/0000-0002-4225-5074; Pan,
Laura/0000-0001-7377-2114; bekki, slimane/0000-0002-5538-0800; Nakamura,
Tetsu/0000-0002-2056-7392; Braesicke, Peter/0000-0003-1423-0619; Pawson,
Steven/0000-0003-0200-717X; Pitari, Giovanni/0000-0001-7051-9578;
Eyring, Veronika/0000-0002-6887-4885; Hegglin,
Michaela/0000-0003-2820-9044; Mancini, Eva/0000-0001-7071-0292;
Morgenstern, Olaf/0000-0002-9967-9740
FU Canadian Foundation for Climate and Atmospheric Sciences (CFCAS);
Canadian Space Agency (CSA) through the C-SPARC network; National
Aeronautics and Space Administration; Ministry of Education, Culture,
Sports, Science, and Technology (MEXT) of Japan [19340138]; Ministry of
the Environment of Japan [A-071, A-0903]; DECC/Defra [GA01101]; European
Commission [SCOUT-O3]
FX Thanks go to Diane Pendlebury and Mike Neish (University of Toronto) for
technical assistance with figures and the CCMVal-2 data. M. I. Hegglin
has been supported by the Canadian Foundation for Climate and
Atmospheric Sciences (CFCAS) and the Canadian Space Agency (CSA) through
the C-SPARC network, which supports CMAM. Research at the Jet Propulsion
Laboratory, California Institute of Technology was done under contract
with the National Aeronautics and Space Administration. CCSRNIES
research was supported by a grant-in-aid for scientific research from
Ministry of Education, Culture, Sports, Science, and Technology (MEXT)
of Japan (19340138) and the Global Environmental Research Fund of the
Ministry of the Environment of Japan (A-071 and A-0903). Both CCSRNIES
and MRI simulations were completed with the supercomputer at the
National Institute for Environmental Studies (NIES), Japan. The
contribution of the Met Office Hadley Centre was supported by the Joint
DECC and Defra Integrated Climate Programme, DECC/Defra (GA01101).
European contributions were supported by the European Commission through
the SCOUT-O3 project under the 6th Framework Programme. WACCM-hires
simulations were performed at the Centro de Supercomputacion de Galicia.
We acknowledge the Chemistry-Climate Model Validation (CCMVal) Activity
of WCRP's (World Climate Research Programme) SPARC (Stratospheric
Processes and their Role in Climate) project for organizing and
coordinating the model data analysis activity, and the British
Atmospheric Data Centre (BADC) for collecting and archiving the CCMVal
model output.
NR 100
TC 38
Z9 38
U1 0
U2 22
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-897X
EI 2169-8996
J9 J GEOPHYS RES-ATMOS
JI J. Geophys. Res.-Atmos.
PD OCT 23
PY 2010
VL 115
AR D00M09
DI 10.1029/2010JD013884
PG 24
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 671XH
UT WOS:000283546600006
ER
PT J
AU Scharroo, R
Smith, WHF
AF Scharroo, Remko
Smith, Walter H. F.
TI A global positioning system-based climatology for the total electron
content in the ionosphere
SO JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
LA English
DT Article
ID INTERNATIONAL REFERENCE IONOSPHERE; SOLAR-ACTIVITY; MODEL;
INTERFEROMETRY; DELAY; IRI; TEC
AB The total electron content (TEC) in the ionosphere is an important factor in the propagation of radio waves. Since 1998 the coverage global positioning system (GPS) observations has been sufficient to monitor the TEC globally. We have used the global ionosphere maps provided by the Jet Propulsion Laboratory to devise a new ionosphere climatology (NIC09). The climatology fits the GPS maps to 4.5 TECU, more than twice as well as the IRI2007 climatology. The use of the global mean TEC as the input parameter reduces scaling errors and long-term mean errors in the model. For climatic studies of sea level measured by satellite radar altimeters, it is necessary to go back before 1998. During the earlier years of radar altimetry, we use TOPEX dual-frequency altimeter data to reconstruct the global mean TEC or use the solar radio flux (F(10.7)) as a proxy. The comparison of dual-frequency altimeter data with the GPS maps demonstrated that about 8% of the TEC extends above 1350 km and about 14% above 800 km. The root mean square error of the NIC09 climatology was found to be approximately 18% of the TEC, compared to 14% for the GPS TEC maps, and 35% for IRI2007.
C1 [Scharroo, Remko] Altimetrics LLC, Cornish, NH 03745 USA.
[Smith, Walter H. F.] NOAA, Lab Satellite Altimetry, ERA31, Silver Spring, MD 20910 USA.
RP Scharroo, R (reprint author), Altimetrics LLC, 330A Parsonage Rd, Cornish, NH 03745 USA.
EM remko@altimetrics.com; walter.hf.smith@noaa.gov
RI Scharroo, Remko/F-5623-2010; Smith, Walter/F-5627-2010
OI Smith, Walter/0000-0002-8814-015X
NR 34
TC 26
Z9 28
U1 0
U2 7
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0148-0227
J9 J GEOPHYS RES-SPACE
JI J. Geophys. Res-Space Phys.
PD OCT 22
PY 2010
VL 115
AR A10318
DI 10.1029/2009JA014719
PG 16
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA 671YJ
UT WOS:000283549900001
ER
PT J
AU Cho, KS
Bong, SC
Moon, YJ
Dryer, M
Lee, SE
Kim, KH
AF Cho, K. -S.
Bong, S. -C.
Moon, Y. -J.
Dryer, M.
Lee, S. -E.
Kim, K. -H.
TI An empirical relationship between coronal mass ejection initial speed
and solar wind dynamic pressure
SO JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
LA English
DT Article
ID INTERPLANETARY MAGNETIC-FIELD; ANGLE
AB Interplanetary shocks that precede coronal mass ejections (CMEs) are mainly responsible for sudden impulses, which are characterized by a simple step-like increase in the horizontal H component. Such a magnetic field change has been explained as a compression of the magnetosphere by the passage of a sudden increase in the solar wind dynamic pressure. Strong compression of the dayside magnetopause could cause geosynchronous satellites to be exposed to solar wind environments where large fluctuations of the interplanetary magnetic field and highly energetic particles are present. In this study, we chose 26 event pairs consisting of a type II burst/CME occurring in conjunction with a sudden commencement/sudden impulse (SC/SI) whose solar wind, and Earth magnetic field data are available. We then investigated relationships among three physical properties (kinetic energy, directional parameter, and speed) of near-Sun CMEs, solar wind dynamic pressure, and SC/SI amplitude. As a result, we found that (1) the CME speed is more highly correlated with SC/SI amplitude than its kinetic energy and direction parameter; (2) by adopting the empirical relationship between solar wind dynamic pressure and amplitude of symmetric H (a steplike increase in the horizontal H component at low latitude), we could derive an empirical formula for the relationship between solar wind dynamic pressure near the Earth and the CME speed; (3) the CME speed has a linear relationship with the difference of magnetopause locations derived by using the model of Shue et al. (1998) at the subsolar point before and after the shock arrivals; (4) a fast CME greater than 1600 km s(-1) could be a driver of the magnetopause crossing of a spacecraft at geosynchronous orbit. Our results show that the CME speed is an important parameter for early prediction of geosynchronous magnetopause crossing.
C1 [Cho, K. -S.; Bong, S. -C.; Lee, S. -E.] Korea Astron & Space Sci Inst, Div Space Sci, Taejon 305348, South Korea.
[Moon, Y. -J.; Kim, K. -H.] Kyung Hee Univ, Dept Astron & Space Sci, Yongin 446701, South Korea.
[Dryer, M.] NOAA, Space Weather Predict Ctr, Boulder, CO 80305 USA.
RP Cho, KS (reprint author), Korea Astron & Space Sci Inst, Div Space Sci, Taejon 305348, South Korea.
EM kscho@kasi.re.kr
RI Moon, Yong-Jae/E-1711-2013; Kim , Khan-Hyuk/E-2361-2013
FU KASI; Korean Ministry of Education, Science, and Technology [R31-10016];
Korean Government (MOEHRD) [KRF-2008-314-C00158]
FX This work has been supported by the "Development of Korean Space Weather
Center" project of KASI, and the KASI basic research fund. Y.J.M. and K.
H. K. have been supported by the WCU grant (R31-10016) funded by the
Korean Ministry of Education, Science, and Technology and by the Korea
Research Foundation Grant funded by the Korean Government (MOEHRD, Basic
Research Promotion Fund) (KRF-2008-314-C00158). M. D. expresses
appreciation for the emeritus hospitality of the NOAA Space Weather
Prediction Center.
NR 21
TC 4
Z9 4
U1 0
U2 3
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-9380
EI 2169-9402
J9 J GEOPHYS RES-SPACE
JI J. Geophys. Res-Space Phys.
PD OCT 21
PY 2010
VL 115
AR A10111
DI 10.1029/2009JA015139
PG 8
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA 671YI
UT WOS:000283549800001
ER
PT J
AU Coskuner, O
AF Coskuner, Orkid
TI Single Ion and Dimerization Studies of the Al(III) Ion in Aqueous
Solution
SO JOURNAL OF PHYSICAL CHEMISTRY A
LA English
DT Article
ID MOLECULAR-DYNAMICS SIMULATION; MONTE-CARLO SIMULATIONS; AB-INITIO;
PROTON-TRANSFER; METAL-IONS; ALUMINUM COMPLEXES; HYDROPHOBIC
INTERACTIONS; ALZHEIMERS-DISEASE; OXYGEN-EXCHANGE; ACUTE TOXICITY
AB Aqueous trivalent aluminum (Al) ions and their oligomers play important roles in diverse areas, such as environmental sciences and medicine. The geometries of octahedral Al(H2O)(6)(3+) and tetrahedral Al(OH)(4)(-) species have been studied extensively. However, structures of intermediate hydrolysis products of the Al(III) ion, such as the penta-coordinated Al(OH)(2+) species, which exists at pH values ranging from 3.0 to 4.3, and their mode of formation have been poorly understood. Here, we present that a trigonal bipyramidal Al(OH)(H2O)(4)(2+) structure is formed in aqueous solution and how this monomeric species dimerizes to dinuclear [(H2O)(4)Al(OH)(2)Al(H2O)(4)](4+) complex in aqueous solution. The Gibbs free energy change calculations indicate that the formation of the dinuclear complex is preferred over the existence of two single trigonal bipyramidal Al(OH)(H2O)(4)(2+) species in aqueous solution. This study captures the solution dynamics and proton transfer in the oligomerization reactions of penta-coordinated Al(OH)(2+) species in aqueous solution.
C1 [Coskuner, Orkid] Univ Texas San Antonio, Dept Chem, San Antonio, TX 78249 USA.
[Coskuner, Orkid] US Natl Inst Stand & Technol, Computat Chem Grp, Gaithersburg, MD 20899 USA.
RP Coskuner, O (reprint author), Univ Texas San Antonio, Dept Chem, 1 UTSA Dr, San Antonio, TX 78249 USA.
EM orkid.coskuner@utsa.edu
RI Coskuner, Orkid/O-5376-2016
OI Coskuner, Orkid/0000-0002-0772-9350
NR 69
TC 5
Z9 5
U1 0
U2 9
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 1089-5639
J9 J PHYS CHEM A
JI J. Phys. Chem. A
PD OCT 21
PY 2010
VL 114
IS 41
BP 10981
EP 10987
DI 10.1021/jp102906c
PG 7
WC Chemistry, Physical; Physics, Atomic, Molecular & Chemical
SC Chemistry; Physics
GA 662XW
UT WOS:000282848600010
PM 20879774
ER
PT J
AU Herzing, AA
Richter, LJ
Anderson, IM
AF Herzing, Andrew A.
Richter, Lee J.
Anderson, Ian M.
TI 3D Nanoscale Characterization of Thin-Film Organic Photovoltaic Device
Structures via Spectroscopic Contrast in the TEM
SO JOURNAL OF PHYSICAL CHEMISTRY C
LA English
DT Article
ID TRANSMISSION ELECTRON-MICROSCOPY; MULTIVARIATE STATISTICAL-ANALYSIS; RAY
SPECTRAL IMAGES; POLYMER SOLAR-CELLS; TOMOGRAPHY; EFTEM; MICROANALYSIS;
MORPHOLOGY; SEM
AB The three-dimensional characterization of third generation photovoltaic device structures at the nanometer scale is essential to the development of efficient, reliable, and inexpensive solar cell technologies. Electron tomography is a powerful method for three-dimensional characterization; however, the application of this method to die organic materials systems that comprise typical high-efficiency devices is complicated by the difficulty in generating contrast from the compositionally similar materials. Herein we report the application of low-loss energy-filtered transmission electron microscopy as a method of generating spectroscopic contrast from a common organic bulk-heterojunction thin film consisting of a polymer donor and a fullerene-derivative acceptor. Spectral imaging methods combined with principal component analysis are used to characterize the contrast generation mechanism and to determine the optimum data acquisition parameters for this particular combination of organic phases. A proof of method for using the low-loss spectral signal as a basis for electron tomography is presented. and the advantages and drawbacks or the technique as applied to multiphase organic systems relative to the more commonly employed bright-field imaging approach are outlined.
C1 [Herzing, Andrew A.; Richter, Lee J.; Anderson, Ian M.] Natl Inst Stand & Technol, Surface & Microanal Sci Div, Gaithersburg, MD 20899 USA.
RP Herzing, AA (reprint author), Natl Inst Stand & Technol, Surface & Microanal Sci Div, Gaithersburg, MD 20899 USA.
EM andrew.herzing@nist.gov; lee.richter@nist.gov; ian.anderson@nist.gov
RI Herzing, Andrew/D-6239-2012; Richter, Lee/N-7730-2016
OI Richter, Lee/0000-0002-9433-3724
FU NRC
FX We would like to thank Drs. XinRan Zhang, Steven Hudson, and Dean
Delongchamp (NIST) for providing the samples and for many helpful
discussions. A.A.H. acknowledges the support of the NRC Postdoctoral
Research Associateship Program
NR 31
TC 76
Z9 76
U1 4
U2 33
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 1932-7447
J9 J PHYS CHEM C
JI J. Phys. Chem. C
PD OCT 21
PY 2010
VL 114
IS 41
BP 17501
EP 17508
DI 10.1021/jp105883p
PG 8
WC Chemistry, Physical; Nanoscience & Nanotechnology; Materials Science,
Multidisciplinary
SC Chemistry; Science & Technology - Other Topics; Materials Science
GA 663AM
UT WOS:000282855400034
ER
PT J
AU Shin, JW
Bertocci, U
Stafford, GR
AF Shin, J. W.
Bertocci, U.
Stafford, G. R.
TI Underpotential Deposition of Tl on (111)-Textured Au: In Situ Stress and
Nanogravimetric Measurements
SO JOURNAL OF PHYSICAL CHEMISTRY C
LA English
DT Article
ID 2ND HARMONIC-GENERATION; SINGLE-CRYSTAL SURFACES; X-RAY-SCATTERING;
ELECTRODE SURFACE; GOLD ELECTRODES; AU(111) ELECTRODE; METAL-ELECTRODES;
SOLID ELECTRODES; STEPPED SURFACES; OXYGEN REDUCTION
AB The surface stress associated with the underpotential deposition (upd) of thallium (Tl) on (111)-textured Au is examined, using the wafer curvature method in acidic perchlorate supporting electrolyte. The process is also examined by independent nanogravimetric measurements using an electrochemical quartz crystal nanobalance (EQCN). We observe a sweep rate dependence for both the individual voltammetric waves and stress response, which we attribute to kinetically controlled surface alloying that occurs only it low coverage. Similar behavior has been reported for Pb upd on (111)-textured Au, hut the kinetics for Tl considerably slower and are very sensitive to the defect density of the Au(111) surface. At high coverage. a full Tl monolayer is formed; however. a dealloying step is required prior to completion of the monolayer. The stress hump that is coincident with the last voltammetric wave appears to he caused by the formation and removal of the surface alloy. This is confirmed by long-term potentiostatic pulsing experiments.
C1 [Shin, J. W.; Bertocci, U.; Stafford, G. R.] Natl Inst Stand & Technol, Mat Sci & Engn Lab, Gaithersburg, MD 20899 USA.
RP Stafford, GR (reprint author), Natl Inst Stand & Technol, Mat Sci & Engn Lab, Gaithersburg, MD 20899 USA.
FU Center for Nanoscale Science and Technology NanoFab at the National
Institute of Standards and Technology
FX The authors gratefully acknowledge Carlos Beauchamp for technical
contributions, Abhishek Motayed or electron beam evaporating the Au
cantilever electrodes, and Liang Yueh Ou Yang For helping prepare and
flame anneal the Au single crystal. This work was performed in part at
the Center for Nanoscale Science and Technology NanoFab at the National
Institute of Standards and Technology.
NR 68
TC 8
Z9 8
U1 0
U2 9
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 1932-7447
J9 J PHYS CHEM C
JI J. Phys. Chem. C
PD OCT 21
PY 2010
VL 114
IS 41
BP 17621
EP 17628
DI 10.1021/jp1034486
PG 8
WC Chemistry, Physical; Nanoscience & Nanotechnology; Materials Science,
Multidisciplinary
SC Chemistry; Science & Technology - Other Topics; Materials Science
GA 663AM
UT WOS:000282855400050
ER
PT J
AU Fowler, JW
Acquaviva, V
Ade, PAR
Aguirre, P
Amiri, M
Appel, JW
Barrientos, LF
Battistelli, ES
Bond, JR
Brown, B
Burger, B
Chervenak, J
Das, S
Devlin, MJ
Dicker, SR
Doriese, WB
Dunkley, J
Dunner, R
Essinger-Hileman, T
Fisher, RP
Hajian, A
Halpern, M
Hasselfield, M
Hernandez-Monteagudo, C
Hilton, GC
Hilton, M
Hincks, AD
Hlozek, R
Huffenberger, KM
Hughes, DH
Hughes, JP
Infante, L
Irwin, KD
Jimenez, R
Juin, JB
Kaul, M
Klein, J
Kosowsky, A
Lau, JM
Limon, M
Lin, YT
Lupton, RH
Marriage, TA
Marsden, D
Martocci, K
Mauskopf, P
Menanteau, F
Moodley, K
Moseley, H
Netterfield, CB
Niemack, MD
Nolta, MR
Page, LA
Parker, L
Partridge, B
Quintana, H
Reid, B
Sehgal, N
Sievers, J
Spergel, DN
Staggs, ST
Swetz, DS
Switzer, ER
Thornton, R
Trac, H
Tucker, C
Verde, L
Warne, R
Wilson, G
Wollack, E
Zhao, Y
AF Fowler, J. W.
Acquaviva, V.
Ade, P. A. R.
Aguirre, P.
Amiri, M.
Appel, J. W.
Barrientos, L. F.
Battistelli, E. S.
Bond, J. R.
Brown, B.
Burger, B.
Chervenak, J.
Das, S.
Devlin, M. J.
Dicker, S. R.
Doriese, W. B.
Dunkley, J.
Duenner, R.
Essinger-Hileman, T.
Fisher, R. P.
Hajian, A.
Halpern, M.
Hasselfield, M.
Hernandez-Monteagudo, C.
Hilton, G. C.
Hilton, M.
Hincks, A. D.
Hlozek, R.
Huffenberger, K. M.
Hughes, D. H.
Hughes, J. P.
Infante, L.
Irwin, K. D.
Jimenez, R.
Juin, J. B.
Kaul, M.
Klein, J.
Kosowsky, A.
Lau, J. M.
Limon, M.
Lin, Y. -T.
Lupton, R. H.
Marriage, T. A.
Marsden, D.
Martocci, K.
Mauskopf, P.
Menanteau, F.
Moodley, K.
Moseley, H.
Netterfield, C. B.
Niemack, M. D.
Nolta, M. R.
Page, L. A.
Parker, L.
Partridge, B.
Quintana, H.
Reid, B.
Sehgal, N.
Sievers, J.
Spergel, D. N.
Staggs, S. T.
Swetz, D. S.
Switzer, E. R.
Thornton, R.
Trac, H.
Tucker, C.
Verde, L.
Warne, R.
Wilson, G.
Wollack, E.
Zhao, Y.
TI THE ATACAMA COSMOLOGY TELESCOPE: A MEASUREMENT OF THE 600 < l < 8000
COSMIC MICROWAVE BACKGROUND POWER SPECTRUM AT 148 GHz
SO ASTROPHYSICAL JOURNAL
LA English
DT Article
DE cosmic background radiation; cosmology: observations
ID 1200-MU-M MAMBO SURVEY; STAR-FORMING GALAXIES; SOUTH-POLE TELESCOPE;
GOODS-N FIELD; SOURCE CATALOG; EXTRAGALACTIC SOURCES; ANISOTROPY POWER;
PLANCK SURVEYOR; DUST EMISSION; PROBE
AB We present a measurement of the angular power spectrum of the cosmic microwave background (CMB) radiation observed at 148 GHz. The measurement uses maps with 1'.4 angular resolution made with data from the Atacama Cosmology Telescope (ACT). The observations cover 228 deg(2) of the southern sky, in a 4 degrees.2 wide strip centered on declination 53 degrees south. The CMB at arcminute angular scales is particularly sensitive to the Silk damping scale, to the Sunyaev-Zel'dovich (SZ) effect from galaxy clusters, and to emission by radio sources and dusty galaxies. After masking the 108 brightest point sources in our maps, we estimate the power spectrum between 600 < l < 8000 using the adaptive multi-taper method to minimize spectral leakage and maximize use of the full data set. Our absolute calibration is based on observations of Uranus. To verify the calibration and test the fidelity of our map at large angular scales, we cross-correlate the ACT map to the WMAP map and recover the WMAP power spectrum from 250 < l < 1150. The power beyond the Silk damping tail of the CMB (l similar to 5000) is consistent with models of the emission from point sources. We quantify the contribution of SZ clusters to the power spectrum by fitting to a model normalized to sigma(8) = 0.8. We constrain the model's amplitude A(SZ) < 1.63 (95% CL). If interpreted as a measurement of sigma(8), this implies sigma(SZ)(8) < 0.86 (95% CL) given our SZ model. A fit of ACT and WMAP five-year data jointly to a six-parameter Lambda CDM model plus point sources and the SZ effect is consistent with these results.
C1 [Fowler, J. W.; Appel, J. W.; Das, S.; Dunkley, J.; Essinger-Hileman, T.; Fisher, R. P.; Hajian, A.; Hincks, A. D.; Lau, J. M.; Limon, M.; Martocci, K.; Niemack, M. D.; Page, L. A.; Parker, L.; Reid, B.; Staggs, S. T.; Switzer, E. R.; Zhao, Y.] Princeton Univ, Joseph Henry Labs Phys, Princeton, NJ 08544 USA.
[Acquaviva, V.; Das, S.; Dunkley, J.; Hajian, A.; Lin, Y. -T.; Lupton, R. H.; Marriage, T. A.; Spergel, D. N.; Trac, H.] Princeton Univ, Dept Astrophys Sci, Princeton, NJ 08544 USA.
[Acquaviva, V.; Hughes, J. P.; Menanteau, F.; Sehgal, N.] Rutgers State Univ, Dept Phys & Astron, Piscataway, NJ 08854 USA.
[Ade, P. A. R.; Mauskopf, P.; Tucker, C.] Cardiff Univ, Sch Phys & Astron, Cardiff CF24 3AA, S Glam, Wales.
[Aguirre, P.; Barrientos, L. F.; Duenner, R.; Infante, L.; Juin, J. B.; Lin, Y. -T.; Quintana, H.] Pontificia Univ Catolica Chile, Fac Fis, Dept Astron & Astrofis, Santiago 22, Chile.
[Amiri, M.; Battistelli, E. S.; Burger, B.; Halpern, M.; Hasselfield, M.] Univ British Columbia, Dept Phys & Astron, Vancouver, BC V6T 1Z4, Canada.
[Battistelli, E. S.] Univ Roma La Sapienza, Dept Phys, I-00185 Rome, Italy.
[Bond, J. R.; Nolta, M. R.; Sievers, J.] Univ Toronto, Canadian Inst Theoret Astrophys, Toronto, ON M5S 3H8, Canada.
[Brown, B.; Kosowsky, A.] Univ Pittsburgh, Dept Phys & Astron, Pittsburgh, PA 15260 USA.
[Chervenak, J.; Moseley, H.; Wollack, E.] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
[Das, S.] Univ Calif Berkeley, Berkeley Ctr Cosmol Phys, LBL, Berkeley, CA 94720 USA.
[Das, S.] Univ Calif Berkeley, Dept Phys, Berkeley, CA 94720 USA.
[Devlin, M. J.; Dicker, S. R.; Kaul, M.; Klein, J.; Limon, M.; Marsden, D.; Swetz, D. S.; Thornton, R.] Univ Penn, Dept Phys & Astron, Philadelphia, PA 19104 USA.
[Doriese, W. B.; Hilton, G. C.; Irwin, K. D.; Niemack, M. D.; Swetz, D. S.] NIST, Quantum Devices Grp, Boulder, CO 80305 USA.
[Dunkley, J.; Hlozek, R.] Univ Oxford, Dept Astrophys, Oxford OX1 3RH, England.
[Hernandez-Monteagudo, C.] Max Planck Inst Astrophys, D-85741 Garching, Germany.
[Hilton, M.; Moodley, K.; Warne, R.] Univ KwaZulu Natal, Astrophys & Cosmol Res Unit, Sch Math Sci, ZA-4041 Durban, South Africa.
[Hilton, M.; Moodley, K.] CSIR Campus, Ctr High Performance Comp, Cape Town, South Africa.
[Huffenberger, K. M.] Univ Miami, Dept Phys, Coral Gables, FL 33124 USA.
[Hughes, D. H.] INAOE, Puebla, Mexico.
[Jimenez, R.; Reid, B.; Verde, L.] Univ Barcelona, ICREA, E-08028 Barcelona, Spain.
[Jimenez, R.; Reid, B.; Verde, L.] Univ Barcelona, ICC, E-08028 Barcelona, Spain.
[Lau, J. M.; Sehgal, N.] Stanford Univ, Kavli Inst Particle Astrophys & Cosmol, Stanford, CA 94305 USA.
[Lau, J. M.] Stanford Univ, Dept Phys, Stanford, CA 94305 USA.
[Limon, M.] Columbia Univ, Columbia Astrophys Lab, New York, NY 10027 USA.
[Lin, Y. -T.] Univ Tokyo, Inst Phys & Math Universe, Chiba 2778568, Japan.
[Martocci, K.; Switzer, E. R.] Kavli Inst Cosmol Phys, Chicago, IL 60637 USA.
[Netterfield, C. B.] Univ Toronto, Dept Phys, Toronto, ON M5S 1A7, Canada.
[Partridge, B.] Haverford Coll, Dept Phys & Astron, Haverford, PA 19041 USA.
[Thornton, R.] W Chester Univ Penn, Dept Phys, W Chester, PA 19383 USA.
[Trac, H.] Harvard Univ, Harvard Smithsonian Ctr Astrophys, Cambridge, MA 02138 USA.
[Wilson, G.] Univ Massachusetts, Dept Astron, Amherst, MA 01003 USA.
RP Fowler, JW (reprint author), Princeton Univ, Joseph Henry Labs Phys, Jadwin Hall, Princeton, NJ 08544 USA.
RI Moseley, Harvey/D-5069-2012; Klein, Jeffrey/E-3295-2013; Spergel,
David/A-4410-2011; Hilton, Matthew James/N-5860-2013; Trac,
Hy/N-8838-2014; Wollack, Edward/D-4467-2012;
OI Trac, Hy/0000-0001-6778-3861; Wollack, Edward/0000-0002-7567-4451;
Sievers, Jonathan/0000-0001-6903-5074; Verde, Licia/0000-0003-2601-8770
FU ACT; NASA [NNX08AH30G]; Natural Science and Engineering Research Council
of Canada (NSERC); NSF [AST-0546035, AST-0606975]; FONDAP Centro de
Astrofisica; CONICYT; MECESUP; Fundacion Andes; NSF Physics Frontier
Center [PHY-0114422]; South African National Research Foundation (NRF);
Meraka Institute via funding for the South African Centre for High
Performance Computing (CHPC); South African Square Kilometer Array (SKA)
Project; RCUK; Rhodes Trust; Berkeley Center for Cosmological Physics;
World Premier International Research Center Initiative, MEXT, Japan
FX The ACT project was proposed in 2000 and funded on 2004 January 1. Many
have contributed to the project since its inception. We especially thank
Asad Aboobaker, Christine Allen, Dominic Benford, Paul Bode, Kristen
Burgess, Angelica de Oliveira-Costa, Peter Hargrave, Norm Jarosik, Amber
Miller, Carl Reintsema, Felipe Rojas, Uros Seljak, Martin Spergel,
Johannes Staghun, Carl Stahle, Max Tegmark, Masao Uehara, Katerina
Visnjic, and Ed Wishnow. It is a pleasure to acknowledge Bob Margolis,
ACT's project manager. Reed Plimpton and David Jacobson worked at the
telescope during the 2008 season. ACT is on the Chajnantor Science
preserve, which was made possible by the Chilean Comision Nacional de
Investigacion Cientifica y Tecnologica. We are grateful for the
assistance we received at various times from the ALMA, APEX, ASTE,
CBI/QUIET, and NANTEN2 groups. The ATCA team kindly provided the
positions of their 20 GHz sources prior to publication. The PWV data
come from the public APEX weather Web site. Field operations were based
at the Don Esteban facility run by Astro-Norte. This research has made
use of the NASA/IPAC Extragalactic Database (NED) which is operated by
the Jet Propulsion Laboratory, California Institute of Technology, under
contract with the National Aeronautics and Space Administration. We
thank the members of our external advisory board-Tom Herbig (chair),
Charles Alcock, Walter Gear, Cliff Jackson, Amy Newbury, and Paul
Steinhardt-who helped guide the project to fruition.; This work was
supported by the U.S. National Science Foundation through awards
AST-0408698 for the ACT project, and PHY-0355328, AST-0707731, and
PIRE-0507768. Funding was also provided by Princeton University and the
University of Pennsylvania. The PIRE program made possible exchanges
between Chile, South Africa, Spain, and the US that enabled this
research program. Computations were performed on the GPC supercomputer
at the SciNet HPC Consortium. SciNet is funded by the Canada Foundation
for Innovation under the auspices of Compute Canada, the Government of
Ontario, Ontario Research Fund-Research Excellence, and the University
of Toronto.; V. A., S. D., A. H., and T. M. were supported through NASA
grant NNX08AH30G. A. D. H. received additional support from a Natural
Science and Engineering Research Council of Canada (NSERC) PGS-D
scholarship. A. K. and B. P. were partially supported through NSF
AST-0546035 and AST-0606975, respectively, for work on ACT. H. Q. and L.
I. acknowledge partial support from FONDAP Centro de Astrofisica. R. D.
was supported by CONICYT, MECESUP, and Fundacion Andes. E. S.
acknowledges support by NSF Physics Frontier Center grant PHY-0114422 to
the Kavli Institute of Cosmological Physics. K. M., M. H., and R. W.
received financial support from the South African National Research
Foundation (NRF), the Meraka Institute via funding for the South African
Centre for High Performance Computing (CHPC), and the South African
Square Kilometer Array (SKA) Project. J.D. received support from an RCUK
Fellowship. R. H. received funding from the Rhodes Trust. S. D.
acknowledges support from the Berkeley Center for Cosmological Physics.
Y.T.L. acknowledges support from the World Premier International
Research Center Initiative, MEXT, Japan. The data will be made public
through LAMBDA (http://lambda.gsfc.nasa.gov/) and the ACTWeb site
(http://www.physics.princeton.edu/act/).
NR 72
TC 86
Z9 86
U1 0
U2 8
PU IOP PUBLISHING LTD
PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0004-637X
J9 ASTROPHYS J
JI Astrophys. J.
PD OCT 20
PY 2010
VL 722
IS 2
BP 1148
EP 1161
DI 10.1088/0004-637X/722/2/1148
PG 14
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA 678LK
UT WOS:000284075400014
ER
PT J
AU Nanda, H
Datta, SAK
Heinrich, F
Losche, M
Rein, A
Krueger, S
Curtis, JE
AF Nanda, Hirsh
Datta, Siddhartha A. K.
Heinrich, Frank
Loesche, Mathias
Rein, Alan
Krueger, Susan
Curtis, Joseph E.
TI Electrostatic Interactions and Binding Orientation of HIV-1 Matrix
Studied by Neutron Reflectivity
SO BIOPHYSICAL JOURNAL
LA English
DT Article
ID HUMAN-IMMUNODEFICIENCY-VIRUS; BILAYER-LIPID MEMBRANES;
ROUS-SARCOMA-VIRUS; VIRAL LIFE-CYCLE; TYPE-1 MATRIX; PLASMA-MEMBRANE;
PROTEIN; GAG; DOMAIN; PHOSPHATIDYLINOSITOL-(4,5)-BISPHOSPHATE
AB The N-terminal matrix (MA) domain of the HIV-1 Gag protein is responsible for binding to the plasma membrane of host cells during viral assembly. The putative membrane-binding interface of MA was previously mapped by means of mutagenesis and analysis of its trimeric crystal structure. However, the orientation of MA on membranes has not been directly determined by experimental measurements. We present neutron reflectivity measurements that resolve the one-dimensional scattering length density profile of MA bound to a biomimetic of the native viral membrane. A molecular refinement procedure was developed using atomic structures of MA to determine the orientation of the protein on the membrane. The orientation defines a lipid-binding interface consistent with previous mutagenesis results. The MA protein maintains this orientation without the presence of a myristate group, driven only by electrostatic interactions. Furthermore, MA is found to penetrate the membrane headgroup region peripherally such that only the side chains of specific Lys and Arg residues interact with the surface. The results suggest that electrostatic interactions are sufficient to favorably orient MA on viral membrane mimics. The spatial determination of the membrane-bound protein demonstrates the ability of neutron reflectivity to discern orientation and penetration under physiologically relevant conditions.
C1 [Nanda, Hirsh; Heinrich, Frank; Loesche, Mathias; Krueger, Susan; Curtis, Joseph E.] NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Datta, Siddhartha A. K.; Rein, Alan] NCI, HIV Drug Resistance Program, Frederick, MD 21701 USA.
[Heinrich, Frank; Loesche, Mathias] Carnegie Mellon Univ, Dept Phys, Biol Phys Grp, Pittsburgh, PA 15213 USA.
RP Nanda, H (reprint author), NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
EM hirsh.nanda@nist.gov
RI Heinrich, Frank/A-5339-2010; Losche, Mathias/J-2986-2013;
OI Heinrich, Frank/0000-0002-8579-553X; Losche,
Mathias/0000-0001-6666-916X; Datta, Siddhartha/0000-0002-4098-7490
FU U.S. Department of Commerce [70NANB8H8009]; National Institutes of
Health [NIH; 1P01 AG032131]; American Health Assistance Foundation
[A2008-307]; Center for Cancer Research, National Cancer Institute, NIH
FX This work was supported by the U.S. Department of Commerce through the
MSE program (70NANB8H8009), the National Institutes of Health (NIH; 1P01
AG032131), and the American Health Assistance Foundation (A2008-307). It
was also supported in part by the Intramural Research Program of the
Center for Cancer Research, National Cancer Institute, NIH. This study
utilized the high-performance computational capabilities of the Biowulf
Linux cluster at the NIH, Bethesda, MD (http://biowulf.nih.gov).
NR 45
TC 22
Z9 22
U1 0
U2 14
PU CELL PRESS
PI CAMBRIDGE
PA 600 TECHNOLOGY SQUARE, 5TH FLOOR, CAMBRIDGE, MA 02139 USA
SN 0006-3495
J9 BIOPHYS J
JI Biophys. J.
PD OCT 20
PY 2010
VL 99
IS 8
BP 2516
EP 2524
DI 10.1016/j.bpj.2010.07.062
PG 9
WC Biophysics
SC Biophysics
GA 670HT
UT WOS:000283412500018
PM 20959092
ER
PT J
AU Parekh, SH
Lee, YJ
Aamer, KA
Cicerone, MT
AF Parekh, Sapun H.
Lee, Young Jong
Aamer, Khaled A.
Cicerone, Marcus T.
TI Label-Free Cellular Imaging by Broadband Coherent Anti-Stokes Raman
Scattering Microscopy
SO BIOPHYSICAL JOURNAL
LA English
DT Article
ID MULTIPLEX CARS MICROSCOPY; PHOTONIC CRYSTAL FIBER; EMBRYONIC STEM-CELLS;
LIPID DROPLETS; IN-VIVO; BACTERIAL ENDOSPORES; PROTEIN DISTRIBUTION;
LIVING CELL; SPECTROSCOPY; TISSUE
AB Raman microspectroscopy can provide the chemical contrast needed to characterize the complex intracellular environment and macromolecular organization in cells without exogenous labels. It has shown a remarkable ability to detect chemical changes underlying cell differentiation and pathology-related chemical changes in tissues but has not been widely adopted for imaging, largely due to low signal levels. Broadband coherent anti-Stokes Raman scattering (B-CARS) offers the same inherent chemical contrast as spontaneous Raman but with increased acquisition rates. To date, however, only spectrally resolved signals from the strong CH-related vibrations have been used for CARS imaging. Here, we obtain Raman spectral images of single cells with a spectral range of 600-3200 cm(-1), including signatures from weakly scattering modes as well as CH vibrations. We also show that B-CARS imaging can be used to measure spectral signatures of individual cells at least fivefold faster than spontaneous Raman microspectroscopy and can be used to generate maps of biochemical species in cells. This improved spectral range and signal intensity opens the door for more widespread use of vibrational spectroscopic imaging in biology and clinical diagnostics.
C1 [Parekh, Sapun H.; Lee, Young Jong; Aamer, Khaled A.; Cicerone, Marcus T.] Natl Inst Stand & Technol, Div Polymers, Gaithersburg, MD 20899 USA.
RP Cicerone, MT (reprint author), Natl Inst Stand & Technol, Div Polymers, Gaithersburg, MD 20899 USA.
EM cicerone@nist.gov
RI Lee, Young Jong/B-7129-2008
OI Lee, Young Jong/0000-0001-7754-3001
FU National Research Council NIST; National Institutes of Health/National
Institute of Biomedical Imaging and Bioengineering [P41EB001046]
FX S.H.P. is supported by a National Research Council NIST Postdoctoral
Fellowship, and K.A.A. is supported by award No. P41EB001046 from the
National Institutes of Health/National Institute of Biomedical Imaging
and Bioengineering.
NR 51
TC 67
Z9 68
U1 3
U2 37
PU CELL PRESS
PI CAMBRIDGE
PA 600 TECHNOLOGY SQUARE, 5TH FLOOR, CAMBRIDGE, MA 02139 USA
SN 0006-3495
J9 BIOPHYS J
JI Biophys. J.
PD OCT 20
PY 2010
VL 99
IS 8
BP 2695
EP 2704
DI 10.1016/j.bpj.2010.08.009
PG 10
WC Biophysics
SC Biophysics
GA 670HT
UT WOS:000283412500037
PM 20959111
ER
PT J
AU Zhou, W
Wu, H
Yildirim, T
AF Zhou, Wei
Wu, Hui
Yildirim, Taner
TI Structural stability and elastic properties of prototypical covalent
organic frameworks
SO CHEMICAL PHYSICS LETTERS
LA English
DT Article
ID HYDROGEN STORAGE; CRYSTALLINE
AB We report the first investigation of the structural stabilities and elastic properties of covalent organic frameworks (COFs), a new class of porous crystalline materials. Representative 2D COFs were found to prefer shifted AA stacking, somewhat similar to graphite. The shear moduli of 2D COFs are exceedingly small, suggesting that the layer-layer coupling in 2D COFs is rather weak, and stacking faults may widely exist. Representative 3D COFs were found to exhibit relatively low elastic stiffness overall. In particular, COF-108, the least dense crystal known, exhibits rather low bulk and shear moduli. Our findings provide important structural and physical details to be considered in the further development of COF materials. (c) 2010 Elsevier B. V. All rights reserved.
C1 [Zhou, Wei; Wu, Hui; Yildirim, Taner] Natl Inst Stand & Technol, NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Zhou, Wei; Wu, Hui] Univ Maryland, Dept Mat Sci & Engn, College Pk, MD 20742 USA.
[Yildirim, Taner] Univ Penn, Dept Mat Sci & Engn, Philadelphia, PA 19104 USA.
RP Zhou, W (reprint author), Natl Inst Stand & Technol, NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA.
EM wzhou@nist.gov
RI Wu, Hui/C-6505-2008; Zhou, Wei/C-6504-2008; yildirim, taner/A-1290-2009
OI Wu, Hui/0000-0003-0296-5204; Zhou, Wei/0000-0002-5461-3617;
FU US Department of Energy through BES
FX This work was partially supported by the US Department of Energy through
BES Grant No. DE-FG02-08ER46522 (T. Y.).
NR 23
TC 22
Z9 22
U1 6
U2 39
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0009-2614
J9 CHEM PHYS LETT
JI Chem. Phys. Lett.
PD OCT 20
PY 2010
VL 499
IS 1-3
BP 103
EP 107
DI 10.1016/j.cplett.2010.09.032
PG 5
WC Chemistry, Physical; Physics, Atomic, Molecular & Chemical
SC Chemistry; Physics
GA 661BT
UT WOS:000282698700021
ER
PT J
AU Becerra, FE
Willis, RT
Rolston, SL
Carmichael, HJ
Orozco, LA
AF Becerra, F. E.
Willis, R. T.
Rolston, S. L.
Carmichael, H. J.
Orozco, L. A.
TI Nondegenerate four-wave mixing in rubidium vapor: Transient regime
SO PHYSICAL REVIEW A
LA English
DT Article
ID QUANTUM COMMUNICATION; ATOMIC ENSEMBLES; OPTICAL CAVITY; SPECTROSCOPY;
SUPERFLUORESCENCE; SEMICONDUCTORS; SYSTEM; STATES
AB We investigate the transient response of the generated light from four-wave mixing (FWM) in the diamond configuration using a step-down field excitation. The transients show fast decay times and oscillations that depend on the detunings and intensities of the fields. A simplified model taking into account the thermal motion of the atoms, propagation, absorption, and dispersion effects shows qualitative agreement with the experimental observations with the energy levels in rubidium (5S(1/2), 5P(1/2), 5P(3/2), and 6S(1/2)). The atomic polarization comes from all the contributions of different velocity classes of atoms in the ensemble modifying dramatically the total transient behavior of the light from FWM.
C1 [Becerra, F. E.; Willis, R. T.; Rolston, S. L.; Carmichael, H. J.; Orozco, L. A.] Univ Maryland, Dept Phys, Joint Quantum Inst, College Pk, MD 20742 USA.
[Becerra, F. E.; Willis, R. T.; Rolston, S. L.; Carmichael, H. J.; Orozco, L. A.] Natl Inst Stand & Technol, College Pk, MD 20742 USA.
[Becerra, F. E.] CINVESTAV, Dept Fis, Mexico City 07000, DF, Mexico.
[Carmichael, H. J.] Univ Auckland, Dept Phys, Auckland, New Zealand.
RP Becerra, FE (reprint author), Univ Maryland, Dept Phys, Joint Quantum Inst, College Pk, MD 20742 USA.
RI Joint Quantum Institute, NIST/UMD/H-4494-2011; rolston,
steven/L-5175-2013
OI rolston, steven/0000-0003-1671-4190
FU National Science Foundation; Consejo Nacional de Ciencia y Tecnologia;
Royal Society of New Zealand
FX This work was supported by the National Science Foundation, Consejo
Nacional de Ciencia y Tecnologia, and the Marsden fund of the Royal
Society of New Zealand.
NR 37
TC 6
Z9 6
U1 1
U2 10
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 1050-2947
J9 PHYS REV A
JI Phys. Rev. A
PD OCT 20
PY 2010
VL 82
IS 4
AR 043833
DI 10.1103/PhysRevA.82.043833
PG 9
WC Optics; Physics, Atomic, Molecular & Chemical
SC Optics; Physics
GA 667TC
UT WOS:000283215600021
ER
PT J
AU Bendersky, LA
Burton, B
Wang, K
AF Bendersky, L. A.
Burton, B.
Wang, K.
TI Transmission electron microscopy and first-principles calculations of
hydrogen ordering in beta-YH2+x
SO PHYSICAL REVIEW B
LA English
DT Article
ID METAL-SEMICONDUCTOR TRANSITIONS; SWITCHABLE OPTICAL-PROPERTIES; INITIO
MOLECULAR-DYNAMICS; TOTAL-ENERGY CALCULATIONS; LANTHANUM HYDRIDE FILMS;
RARE-EARTH HYDRIDES; WAVE BASIS-SET; NEUTRON-DIFFRACTION; YTTRIUM;
SYSTEM
AB In YH2+x hydrides stoichiometric deviations are associated with various interesting phenomena such as magnetic transitions and metal-insulator transitions; ordering of hydrogen on the octahedral sites (O sites) was suggested to be responsible. Long-range order was discovered in hydrogenated Y films by electron diffraction and high-resolution transmission electron microscopy. Ordering on interstitial O sites in the fcc-based YfccH2+x solid solution (0 < x < 1) was investigated with computational tools from the Alloy Theoretic Automated Toolkit. The resulting set of 94 structure energies was fit to a cluster-expansion Hamiltonian that was used to perform a ground-state analysis for the mostly metastable fcc-based solid solution and for the more stable YfccH2+x+YhcpH2+x two-phase mixture. The calculated structures were tested by the observed diffraction conditions and two possible ordered structures were suggested, a ground-state triclinic x=0.0625 and an I-centered cubic x=0.375.
C1 [Bendersky, L. A.; Burton, B.; Wang, K.] Natl Inst Stand & Technol, Mat Sci & Engn Lab, Gaithersburg, MD 20899 USA.
RP Bendersky, LA (reprint author), Natl Inst Stand & Technol, Mat Sci & Engn Lab, Gaithersburg, MD 20899 USA.
RI Wang, Ke/C-8021-2011
NR 44
TC 0
Z9 0
U1 2
U2 8
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 1098-0121
EI 1550-235X
J9 PHYS REV B
JI Phys. Rev. B
PD OCT 20
PY 2010
VL 82
IS 14
AR 144111
DI 10.1103/PhysRevB.82.144111
PG 7
WC Physics, Condensed Matter
SC Physics
GA 667UI
UT WOS:000283220100008
ER
PT J
AU Bogdan, TJ
Onsager, TG
AF Bogdan, Thomas J.
Onsager, Terrance G.
TI New Space Weather Activities in the World Meteorological Organization
SO SPACE WEATHER-THE INTERNATIONAL JOURNAL OF RESEARCH AND APPLICATIONS
LA English
DT Editorial Material
C1 [Bogdan, Thomas J.] NOAA, SWPC, Washington, DC 20230 USA.
RP Bogdan, TJ (reprint author), NOAA, SWPC, Washington, DC 20230 USA.
EM terry.onsager@noaa.gov
NR 0
TC 0
Z9 0
U1 0
U2 3
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 1542-7390
J9 SPACE WEATHER
JI Space Weather
PD OCT 20
PY 2010
VL 8
AR S10004
DI 10.1029/2010SW000626
PG 2
WC Astronomy & Astrophysics; Geochemistry & Geophysics; Meteorology &
Atmospheric Sciences
SC Astronomy & Astrophysics; Geochemistry & Geophysics; Meteorology &
Atmospheric Sciences
GA 671YS
UT WOS:000283550800003
ER
PT J
AU Millan, RM
Yando, KB
Green, JC
Ukhorskiy, AY
AF Millan, R. M.
Yando, K. B.
Green, J. C.
Ukhorskiy, A. Y.
TI Spatial distribution of relativistic electron precipitation during a
radiation belt depletion event
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID LOSSES; ACCELERATION; TRANSPORT
AB We present observations from the NOAA-15 MEPED telescopes during a radiation belt depletion event on January 19-20, 2000 to investigate the spatial extent of electron precipitation during this interval. Precipitation mapped to the equatorial plane was confined to radial distances less than similar to 6.5 Earth radii, indicating that precipitation was not the direct cause of the decrease in trapped flux observed by GOES. We found an enhanced day-night magnetic field asymmetry during the event, suggesting that magnetopause losses may have been responsible. Precipitation at lower L-values was observed by POES on the dusk passes (18:30-21:00 MLT), but not on the dawn passes, and was observed in conjugate hemispheres. These observations suggest that both precipitation and magnetopause losses were acting during this flux depletion event. Citation: Millan, R. M., K. B. Yando, J. C. Green, and A. Y. Ukhorskiy (2010), Spatial distribution of relativistic electron precipitation during a radiation belt depletion event, Geophys. Res. Lett., 37, L20103, doi:10.1029/2010GL044919.
C1 [Millan, R. M.; Yando, K. B.] Dartmouth Coll, Dept Phys & Astron, Wilder Lab 6127, Hanover, NH 03755 USA.
[Green, J. C.] Natl Ocean & Atmospher Adm, Space Weather Predict Ctr, Boulder, CO 80305 USA.
[Ukhorskiy, A. Y.] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD 20723 USA.
RP Millan, RM (reprint author), Dartmouth Coll, Dept Phys & Astron, Wilder Lab 6127, Hanover, NH 03755 USA.
EM robyn.millan@dartmouth.edu; janet.green@noaa.gov; ukhoray@jhuapl.edu
RI Ukhorskiy, Aleksandr/E-6429-2016
OI Ukhorskiy, Aleksandr/0000-0002-3326-4024
FU NSF [ATM-0457561, ATM-0540121]
FX This work was supported by NSF ATM-0457561 and NSF ATM-0540121. POES
data were provided by the NOAA Space Weather Prediction Center.
NR 21
TC 19
Z9 19
U1 0
U2 2
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD OCT 19
PY 2010
VL 37
AR L20103
DI 10.1029/2010GL044919
PG 4
WC Geosciences, Multidisciplinary
SC Geology
GA 671WU
UT WOS:000283545100004
ER
PT J
AU Tarasick, DW
Jin, JJ
Fioletov, VE
Liu, G
Thompson, AM
Oltmans, SJ
Liu, J
Sioris, CE
Liu, X
Cooper, OR
Dann, T
Thouret, V
AF Tarasick, D. W.
Jin, J. J.
Fioletov, V. E.
Liu, G.
Thompson, A. M.
Oltmans, S. J.
Liu, J.
Sioris, C. E.
Liu, X.
Cooper, O. R.
Dann, T.
Thouret, V.
TI High-resolution tropospheric ozone fields for INTEX and ARCTAS from IONS
ozonesondes
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID WATER-VAPOR; TRAJECTORIES; TRANSPORT; MODEL; CLIMATOLOGY; VALIDATION;
ACCURACY; TRENDS; CANADA
AB The IONS-04, IONS-06, and ARC-IONS ozone sounding campaigns over North America in 2004, 2006, and 2008 obtained approximately 1400 profiles, in five series of coordinated and closely spaced (typically daily) launches. Although this coverage is unprecedented, it is still somewhat sparse in its geographical spacing. Here we use forward and back trajectory calculations for each sounding to map ozone measurements to a number of other locations and so to fill in the spatial domain. This is possible because the lifetime of ozone in the troposphere is of the order of weeks. The trajectory-mapped ozone values show reasonable agreement, where they overlap, to the actual soundings, and the patterns produced separately by forward and backward trajectory calculations are similar. Comparisons with MOZAIC profiles and surface station data show generally good agreement. A variable-length smoothing algorithm is used to fill data gaps: for each point on the map, the smoothing radius is such that a minimum of 10 data points are included in the average. The total tropospheric ozone column maps calculated by integrating the smoothed fields agree well with similar maps derived from TOMS and OMI/MLS measurements. The resulting three-dimensional picture of the tropospheric ozone field for the INTEX and ARCTAS periods facilitates visualization and comparison of different years and seasons and will be useful to other researchers.
C1 [Tarasick, D. W.; Fioletov, V. E.; Liu, G.; Liu, J.; Sioris, C. E.] Environm Canada, Air Qual Res Div, Downsview, ON M3H 5T4, Canada.
[Jin, J. J.] York Univ, Dept Earth & Space Sci & Engn, Toronto, ON M3J 2R7, Canada.
[Thompson, A. M.] Penn State Univ, Dept Meteorol, University Pk, PA 16802 USA.
[Oltmans, S. J.] NOAA, Climate Monitoring & Diagnost Lab, Boulder, CO 80305 USA.
[Liu, X.] Univ Maryland, Goddard Earth Sci & Technol Ctr, Baltimore, MD 21228 USA.
[Liu, X.] Harvard Smithsonian Ctr Astrophys, Cambridge, MA 02138 USA.
[Cooper, O. R.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Cooper, O. R.] NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA.
[Dann, T.] Environm Canada, Air Qual Res Div, Ottawa, ON K1V 1C7, Canada.
[Thouret, V.] Observ Midi Pyrenees, CNRS, Lab Aerol, F-31400 Toulouse, France.
RP Tarasick, DW (reprint author), Environm Canada, Air Qual Res Div, Downsview, ON M3H 5T4, Canada.
EM david.tarasick@ec.gc.ca
RI Thompson, Anne /C-3649-2014; Manager, CSD Publications/B-2789-2015; Jin,
Jianjun/G-8357-2012; Cooper, Owen/H-4875-2013; Liu, Xiong/P-7186-2014
OI Thompson, Anne /0000-0002-7829-0920; Fioletov,
Vitali/0000-0002-2731-5956; Sioris, Christopher/0000-0003-1168-8755;
Tarasick, David/0000-0001-9869-0692; Liu, Xiong/0000-0003-2939-574X
FU Environment Canada; NOAA; NASA; U.S. EPA; Max Plank Institute for
Chemistry, Mainz; Los Alamos National Laboratory; Valparaiso University;
University of Rhode Island; California Department of Energy; California
Air Resources Board; ExxonMobil Canada; European Commission; INSU-CNRS
(France); Meteo-France; Forschungszentrum Julich (Germany); ETHER (CNES
and INSU-CNRS); Airbus; Lufthansa airlines; Austrian airlines; Air
France airlines
FX We thank the many observers who obtained the measurements at the sites
used in this study. Their careful work is gratefully acknowledged. We
thank J. Witte, who archived all of the IONS data in near-real time. We
also thank J. Davies, R. Mittermeier, and T. Mathews for assistance with
data processing. Data were obtained from the World Ozone and Ultraviolet
Radiation Data Center (WOUDC) operated by Environment Canada, Toronto,
Ontario, Canada, under the auspices of the World Meteorological
Organization. Funding of the IONS ozonesondes was provided by
Environment Canada; NOAA; NASA; U.S. EPA; Max Plank Institute for
Chemistry, Mainz; Los Alamos National Laboratory; Valparaiso University;
the University of Rhode Island; the California Department of Energy; the
California Air Resources Board; and the Friends of the Green Horse
Society via a grant from ExxonMobil Canada. The authors also acknowledge
the strong support of the European Commission, Airbus, and the airlines
(Lufthansa, Austrian, Air France) who carry and maintain the MOZAIC
equipment free of charge since 1994. MOZAIC is presently funded by
INSU-CNRS (France), Meteo-France, and Forschungszentrum Julich
(Germany). The MOZAIC data base is supported by ETHER (CNES and
INSU-CNRS).
NR 56
TC 17
Z9 17
U1 2
U2 9
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-897X
J9 J GEOPHYS RES-ATMOS
JI J. Geophys. Res.-Atmos.
PD OCT 19
PY 2010
VL 115
AR D20301
DI 10.1029/2009JD012918
PG 12
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 671XA
UT WOS:000283545900001
ER
PT J
AU Lee, YJ
Parekh, SH
Fagan, JA
Cicerone, MT
AF Lee, Young Jong
Parekh, Sapun H.
Fagan, Jeffrey A.
Cicerone, Marcus T.
TI Phonon dephasing and population decay dynamics of the G-band of
semiconducting single-wall carbon nanotubes
SO PHYSICAL REVIEW B
LA English
DT Article
ID STOKES-RAMAN SCATTERING; VIBRATIONAL-MODES; SPECTROSCOPY; MICROSCOPY;
LIQUIDS
AB The dephasing and population decay dynamics of optical phonons are studied for semiconducting single-wall carbon nanotubes (SWCNTs) using broadband time-resolved coherent anti-Stokes Raman scattering and time-resolved incoherent anti-Stokes Raman scattering. By simply adjusting the spectral bandwidth of a continuum pulse, we are able to directly measure both the total dephasing time, T(2), and the population decay time, T(1), of the G-band sequentially in the same sample, which allows for one to exclude artifacts due to comparison of dynamics values measured with different sample conditions and different measurement schemes. The values of T(1) and T(2)/2 are presented for two different SWCNT samples: bundles in a film on glass and a dispersion in water. While the measured T(1) values are similar for the two samples, the pure dephasing times, T*(2)/2, determined from the T(2)/2 and T(1) measurements are faster in bundled SWCNTs than in isolated dispersion. This suggests that neighboring tubes in the film perturbs the vibrational mode more strongly than surrounding surfactants and that the pure dephasing dynamics is more sensitive to the perturbation.
C1 [Lee, Young Jong; Parekh, Sapun H.; Fagan, Jeffrey A.; Cicerone, Marcus T.] NIST, Div Polymers, Gaithersburg, MD 20899 USA.
RP Lee, YJ (reprint author), NIST, Div Polymers, Gaithersburg, MD 20899 USA.
EM yjlee@nist.gov; cicerone@nist.gov
RI Lee, Young Jong/B-7129-2008;
OI Lee, Young Jong/0000-0001-7754-3001; Fagan, Jeffrey/0000-0003-1483-5554
FU National Research Council; National Institute of Standards and
Technology (NRC/NIST)
FX The authors thank Lee Richter and John Stephenson for valuable
discussion. S.H.P. was supported by a National Research Council and
National Institute of Standards and Technology (NRC/NIST).
NR 31
TC 12
Z9 12
U1 1
U2 14
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 1098-0121
J9 PHYS REV B
JI Phys. Rev. B
PD OCT 19
PY 2010
VL 82
IS 16
AR 165432
DI 10.1103/PhysRevB.82.165432
PG 7
WC Physics, Condensed Matter
SC Physics
GA 666ML
UT WOS:000283119400009
ER
PT J
AU Malkova, N
Bryant, GW
AF Malkova, Natalia
Bryant, Garnett W.
TI Negative-band-gap quantum dots: Gap collapse, intrinsic surface states,
excitonic response, and excitonic insulator phase
SO PHYSICAL REVIEW B
LA English
DT Article
ID SEMICONDUCTOR NANOCRYSTALS; EXCHANGE INTERACTION; OPTICAL-PROPERTIES;
INTERFACE STATES; SUPER-LATTICE; HGTE; CDTE; SILICON; HGSE; CONSTANTS
AB The spectrum of quantum dots made from semiconductors such as HgTe and HgS changes from negative gap to positive gap with decreasing size. Furthermore, intrinsic surface states, which are not related to dangling bonds, appear in the negative-gap regime. We investigate theoretically the evolution of the spectrum of HgS quantum dots with decreasing size and show how states evolve from a negative gap to a positive gap as confinement is increased. The lowest confined electron level evolves into an intrinsic surface state with increasing size and, thus, is not derived directly from a bulk HgS band. Due to strong band mixing in narrow-gap semiconductors, spacing between confined levels decreases more slowly with increasing size than for quantum dots made from wide-gap semiconductors. Moreover, dielectric screening becomes nearly metallic as the gap closes. As a consequence, confinement energies dominate exciton binding energies for all dot sizes up to the gap closure. Excitons remain in the strong confinement limit as size increases until the gap closes. Nonetheless, the exciton binding exceeds the single-particle gap for sizes near gap closure, opening up the possibility of an excitonic insulator phase in quantum dots not possible in positive-gap quantum dots. Signatures in the quantum-dot optical response for gap collapse and surface states are identified.
C1 [Malkova, Natalia] NIST, Atom Phys Div, Gaithersburg, MD 20899 USA.
NIST, Joint Quantum Inst, Gaithersburg, MD 20899 USA.
RP Malkova, N (reprint author), NIST, Atom Phys Div, Gaithersburg, MD 20899 USA.
EM nmalkova@nist.gov
NR 52
TC 9
Z9 9
U1 5
U2 15
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 1098-0121
J9 PHYS REV B
JI Phys. Rev. B
PD OCT 18
PY 2010
VL 82
IS 15
AR 155314
DI 10.1103/PhysRevB.82.155314
PG 10
WC Physics, Condensed Matter
SC Physics
GA 665QF
UT WOS:000283049800007
ER
PT J
AU Windsor, E
Najarro, M
Bloom, A
Benner, B
Fletcher, R
Lareau, R
Gillen, G
AF Windsor, Eric
Najarro, Marcela
Bloom, Anna
Benner, Bruce, Jr.
Fletcher, Robert
Lareau, Richard
Gillen, Greg
TI Application of Inkjet Printing Technology to Produce Test Materials of
1,3,5-Trinitro-1,3,5 Triazcyclohexane for Trace Explosive Analysis
SO ANALYTICAL CHEMISTRY
LA English
DT Article
AB The feasibility of the use of piezoelectric drop-on-demand inkjet printing to prepare test materials for trace explosive analysis is demonstrated. RDX (1,3,5-trinitro-1,3,5 triazcyclohexane) was formulated into inkjet printable solutions and jetted onto substrates suitable for calibration of the ion mobility spectrometry (IMS) instruments currently deployed worldwide for contraband screening. Gravimetric analysis, gas chromatography/mass spectrometry (GC/MS), and ultraviolet-visible (UV-vis) absorption spectroscopy were used to verify inkjet printer solution concentrations and the quantity of explosive dispensed onto test materials. Reproducibility of the inkjet printing process for mass deposition of the explosive RDX (1,3,5-trinitro-1,3,5 triazcyclohexane) was determined to be better than 2% for a single day of printing and better than 3% day-to-day.
C1 [Windsor, Eric; Najarro, Marcela; Bloom, Anna; Benner, Bruce, Jr.; Fletcher, Robert; Gillen, Greg] NIST, Chem Sci & Technol Lab, Gaithersburg, MD 20899 USA.
[Lareau, Richard] Dept Homeland Secur, Transportat Secur Lab, Sci & Technol Directorate, Atlantic City, NJ USA.
RP Windsor, E (reprint author), NIST, Chem Sci & Technol Lab, Gaithersburg, MD 20899 USA.
EM eric.windsor@nist.gov
FU Science and Technology Directorate of the United States Department of
Homeland Security (DHS)
FX Funding for this work was supplied by the Science and Technology
Directorate of the United States Department of Homeland Security (DHS)
through an interagency agreement.
NR 11
TC 25
Z9 25
U1 1
U2 22
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0003-2700
J9 ANAL CHEM
JI Anal. Chem.
PD OCT 15
PY 2010
VL 82
IS 20
BP 8519
EP 8524
DI 10.1021/ac101439r
PG 6
WC Chemistry, Analytical
SC Chemistry
GA 663BX
UT WOS:000282859100023
PM 20873797
ER
PT J
AU Huang, XL
Zhang, JZ
AF Huang, Xiao-Lan
Zhang, Jia-Zhong
TI Spatial Variation in Sediment-Water Exchange of Phosphorus in Florida
Bay: AMP As a Model Organic Compound
SO ENVIRONMENTAL SCIENCE & TECHNOLOGY
LA English
DT Article
ID INORGANIC PHOSPHORUS; PHOSPHATE SORPTION; NATURAL-WATERS; SOILS;
EUTROPHICATION; ADSORPTION; CHRONOSEQUENCE; TEMPERATURE; LIMITATION;
ESTUARIES
AB Dissolved organic phosphorus (DOP) has been recognized as dominant components in total dissolved phosphorus (TDP) pools in many coastal waters, and its exchange between sediment and water is an important process in biogeochemical cycle of phosphorus. Adenosine monophosphate (AMP) was employed as a model DOP compound to simulate phosphorus exchange across sediment-water interface in Florida Bay. The sorption data from 40 stations were fitted to a modified Freundlich equation and provided a detailed spatial distribution both of the sediment's zero equilibrium phosphorus concentration (EPC(0-T)) and of the distribution coefficient (K(d-T)) with respect to TDP. The K(d-T) was found to be a function of the index of phosphorus saturation (IPS), a molar ratio of the surface reactive phosphorus to the surface reactive iron oxide content in the sediment, across the entire bay. However, the EPC(0-T) was found to correlate to the contents of phosphorus in the eastern bay only. Sediment in the western bay might act as a source of the phosphorus in the exchange process due to their high EPC(0-T) and low K(d-T), whereas sediments in the eastern bay might act as a sink because of their low EPC(0-T) and high K(d-T). These results strongly support the hypothesis that both phosphorus and iron species in calcareous marine sediments play a critical role in governing the sediment-water exchange of both phosphate and DOP in the coastal and estuarine ecosystems.
C1 [Huang, Xiao-Lan; Zhang, Jia-Zhong] NOAA, Ocean Chem Div, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
[Huang, Xiao-Lan] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, CIMAS, Miami, FL 33149 USA.
RP Huang, XL (reprint author), Pegasus Tech Serv Inc, 46 E Hollister St, Cincinnati, OH 45219 USA.
EM xiaolan.huang@ymail.com
RI Zhang, Jia-Zhong/B-7708-2008; Huang, XiaoLan/G-6306-2012; Huang (黄),
Xiao-Lan (晓澜)/E-9159-2010
OI Zhang, Jia-Zhong/0000-0002-1138-2556; Huang (黄), Xiao-Lan
(晓澜)/0000-0002-3330-4858
FU NOAA's Center for Sponsored Coastal Ocean Research, South Florida;
Cooperative Institute for Marine and Atmospheric Studies (CIMAS);
University of Miami and the National Oceanic and Atmospheric
Administration [NA67RJ0149]
FX Financial support for this study was provided by NOAA's Center for
Sponsored Coastal Ocean Research, South Florida Program to J.Z.Z. This
research was carried out, in part, under the auspices of the Cooperative
Institute for Marine and Atmospheric Studies (CIMAS), a joint institute
of the University of Miami and the National Oceanic and Atmospheric
Administration, cooperative agreement #NA67RJ0149. The statements,
findings, conclusions, and recommendations are those of the authors and
do not necessarily reflect the views of NOAA or the U.S. Department of
Commerce.
NR 45
TC 16
Z9 16
U1 1
U2 7
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0013-936X
J9 ENVIRON SCI TECHNOL
JI Environ. Sci. Technol.
PD OCT 15
PY 2010
VL 44
IS 20
BP 7790
EP 7795
DI 10.1021/es100057r
PG 6
WC Engineering, Environmental; Environmental Sciences
SC Engineering; Environmental Sciences & Ecology
GA 661KP
UT WOS:000282727500012
PM 20866067
ER
PT J
AU Gronewold, AD
Borsuk, ME
AF Gronewold, Andrew D.
Borsuk, Mark E.
TI Improving Water Quality Assessments through a Hierarchical Bayesian
Analysis of Variability
SO ENVIRONMENTAL SCIENCE & TECHNOLOGY
LA English
DT Article
ID ESCHERICHIA-COLI; TMDL DEVELOPMENT; STANDARDS; MODELS; IMPLEMENTATION;
UNCERTAINTY; VIOLATIONS; CONFIDENCE; COLIFORMS; FREQUENCY
AB Water quality measurement error and variability, while well-documented in laboratory-scale studies, is rarely acknowledged or explicitly resolved in most model-based water body assessments, including those conducted in compliance with the United States Environmental Protection Agency (USEPA) Total Maximum Daily Load (TMDL) program. Consequently, proposed pollutant loading reductions in TMDLs and similar water quality management programs may be biased, resulting in either slower-than-expected rates of water quality restoration and designated use reinstatement or, in some cases, overly conservative management decisions. To address this problem, we present a hierarchical Bayesian approach for relating actual in situ or model-predicted pollutant concentrations to multiple sampling and analysis procedures, each with distinct sources of variability. We apply this method to recently approved TMDLs to investigate whether appropriate accounting for measurement error and variability will lead to different management decisions. We find that required pollutant loading reductions may in fact vary depending not only on how measurement variability is addressed but also on which water quality analysis procedure is used to assess standard compliance. As a general strategy, our Bayesian approach to quantifying variability may represent an alternative to the common practice of addressing all forms of uncertainty through an arbitrary margin of safety (MOS).
C1 [Gronewold, Andrew D.] NOAA, Great Lakes Environm Res Lab, Ann Arbor, MI 48108 USA.
[Borsuk, Mark E.] Dartmouth Coll, Thayer Sch Engn, Hanover, NH 03755 USA.
RP Gronewold, AD (reprint author), NOAA, Great Lakes Environm Res Lab, Ann Arbor, MI 48108 USA.
EM drew.gronewold@noaa.gov
RI Guan, Xiaokang/A-6675-2012;
OI Borsuk, Mark/0000-0002-5121-1110; Gronewold, Andrew/0000-0002-3576-2529
FU United States Environmental Protection Agency, through Office of
Research and Development
FX The authors thank Jeffrey Chanat of the Virginia Department of
Environmental Quality (VDEQ) and Daniel Powell of the Virginia
Department of Health (Shellfish Sanitation Division) for providing
valuable guidance on Virginia's water quality monitoring programs and
for sharing their water quality monitoring data. The United States
Environmental Protection Agency, through its Office of Research and
Development, partially funded and collaborated in the research described
here. It has been subjected to Agency review and approved for
publication. This paper is GLERL contribution No. 1575. The comments of
three anonymous reviewers helped improve the technical quality of this
paper.
NR 44
TC 9
Z9 10
U1 1
U2 23
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0013-936X
EI 1520-5851
J9 ENVIRON SCI TECHNOL
JI Environ. Sci. Technol.
PD OCT 15
PY 2010
VL 44
IS 20
BP 7858
EP 7864
DI 10.1021/es100657p
PG 7
WC Engineering, Environmental; Environmental Sciences
SC Engineering; Environmental Sciences & Ecology
GA 661KP
UT WOS:000282727500023
PM 20853866
ER
PT J
AU Christensen, K
Roginsky, A
Jimeno, M
AF Christensen, Ken
Roginsky, Allen
Jimeno, Miguel
TI A new analysis of the false positive rate of a Bloom filter
SO INFORMATION PROCESSING LETTERS
LA English
DT Article
DE Data structures; Analysis of algorithms; Bloom filters
AB A Bloom filter is a space-efficient data structure used for probabilistic set membership testing. When testing an object for set membership, a Bloom filter may give a false positive. The analysis of the false positive rate is a key to understanding the Bloom filter and applications that use it. We show experimentally that the classic analysis for false positive rate is wrong. We formally derive a correct formula using a balls-and-bins model and show how to numerically compute the new, correct formula in a stable manner. We also prove that the new formula always results in a predicted greater false positive rate than the classic formula. This correct formula is numerically compared to the classic formula for relative error - for a small Bloom filter the prediction of false positive rate will be in error when the classic formula is used. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Christensen, Ken; Jimeno, Miguel] Univ S Florida, Dept Comp Sci & Engn, Tampa, FL 33620 USA.
[Roginsky, Allen] Natl Inst Stand & Technol, Comp Secur Div, Gaithersburg, MD 20899 USA.
RP Christensen, K (reprint author), Univ S Florida, Dept Comp Sci & Engn, 4202 E Fowler Ave,ENB 118, Tampa, FL 33620 USA.
EM christen@csee.usf.edu; allen.roginsky@nist.gov; mjimeno@csee.usf.edu
FU National Science Foundation [CNS-0520081]
FX This material is based on work supported by the National Science
Foundation under CNS-0520081.
NR 9
TC 18
Z9 18
U1 0
U2 1
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0020-0190
EI 1872-6119
J9 INFORM PROCESS LETT
JI Inf. Process. Lett.
PD OCT 15
PY 2010
VL 110
IS 21
BP 944
EP 949
DI 10.1016/j.ipl.2010.07.024
PG 6
WC Computer Science, Information Systems
SC Computer Science
GA 651HP
UT WOS:000281918900006
ER
PT J
AU Dessler, AE
Davis, SM
AF Dessler, A. E.
Davis, S. M.
TI Trends in tropospheric humidity from reanalysis systems
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID WATER-VAPOR FEEDBACK; CLIMATE FEEDBACKS; RADIOSONDE; PINATUBO; MODEL
AB A recent paper (Paltridge et al., 2009) found that specific humidity in the National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis declined between 1973 and 2007, particularly in the tropical mid and upper troposphere, the region that plays the key role in the water vapor feedback. If borne out, this result suggests potential problems in the consensus view of a positive water vapor feedback. Here we consider whether this result holds in other reanalyses and what time scale of climate fluctuation is associated with the negative specific humidity trends. The five reanalyses analyzed here (the older NCEP/NCAR and ERA40 reanalyses and the more modern Japanese Reanalysis (JRA), Modern Era Retrospective-Analysis for Research and Applications (MERRA), and European Centre for Medium-Range Weather Forecasts (ECMWF)-interim reanalyses) unanimously agree that specific humidity generally increases in response to short-term climate variations (e. g., El Nino). In response to decadal climate fluctuations, the NCEP/NCAR reanalysis is unique in showing decreases in tropical mid and upper tropospheric specific humidity as the climate warms. All of the other reanalyses show that decadal warming is accompanied by increases in mid and upper tropospheric specific humidity. We conclude from this that it is doubtful that these negative long-term specific humidity trends in the NCEP/NCAR reanalysis are realistic for several reasons. First, the newer reanalyses include improvements specifically designed to increase the fidelity of long-term trends in their parameters, so the positive trends found there should be more reliable than in the older reanalyses. Second, all of the reanalyses except the NCEP/NCAR assimilate satellite radiances rather than being solely dependent on radiosonde humidity measurements to constrain upper tropospheric humidity. Third, the NCEP/NCAR reanalysis exhibits a large bias in tropical upper tropospheric specific humidity. And finally, we point out that there exists no theoretical support for having a positive short-term water vapor feedback and a negative long-term one.
C1 [Dessler, A. E.] Texas A&M Univ, Dept Atmospher Sci, College Stn, TX 77843 USA.
[Davis, S. M.] NOAA, Earth Syst Res Lab, Div Chem Sci, Boulder, CO 80305 USA.
[Davis, S. M.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
RP Dessler, AE (reprint author), Texas A&M Univ, Dept Atmospher Sci, College Stn, TX 77843 USA.
EM adessler@tamu.edu
RI Davis, Sean/C-9570-2011; Dessler, Andrew/G-8852-2012
OI Davis, Sean/0000-0001-9276-6158; Dessler, Andrew/0000-0003-3939-4820
FU NASA [NNX08AR27G]; NOAA; National Science Foundation (NSF)
FX This work was supported by NASA grant NNX08AR27G to Texas A&M
University, as well as the NOAA Atmospheric composition and climate
program. MERRA data were obtained from the NASA GES DISC. NCEP/NCAR
reanalysis data were provided by the NOAA/OAR/ESRL PSD, Boulder,
Colorado, USA, from their Web site at http://www.cdc.noaa.gov. ERA-40
and ECMWF interim reanalysis data were obtained from the ECMWF website
(http://data.ecmwf.int/data). The JRA data are from the Research Data
Archive (RDA), which is maintained by the Computational and Information
Systems Laboratory (CISL) at the National Center for Atmospheric
Research (NCAR). NCAR is sponsored by the National Science Foundation
(NSF). AIRS data in Figure 3 were obtained from the Giovanni online data
system, developed and maintained by the NASA GES DISC.
NR 31
TC 38
Z9 39
U1 1
U2 15
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-897X
J9 J GEOPHYS RES-ATMOS
JI J. Geophys. Res.-Atmos.
PD OCT 15
PY 2010
VL 115
AR D19127
DI 10.1029/2010JD014192
PG 5
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 666BU
UT WOS:000283084800006
ER
PT J
AU Fuller-Rowell, T
Wu, F
Akmaev, R
Fang, TW
Araujo-Pradere, E
AF Fuller-Rowell, Tim
Wu, Fei
Akmaev, Rashid
Fang, Tzu-Wei
Araujo-Pradere, Eduardo
TI A whole atmosphere model simulation of the impact of a sudden
stratospheric warming on thermosphere dynamics and electrodynamics
SO JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
LA English
DT Article
ID QUASI-BIENNIAL OSCILLATION; LATENT-HEAT RELEASE; INTERANNUAL
VARIABILITY; NORTHERN-HEMISPHERE; TIDES; MIDDLE; DRIFTS; WINTER
AB A Whole Atmosphere Model (WAM) has been used to explore the possible physical connection between a sudden stratospheric warming (SSW) and the dynamics and electrodynamics of the lower thermosphere. WAM produces SSWs naturally without the need for external forcing. The classical signatures of an SSW appear in the model with a warming of the winter polar stratosphere, a reversal of the temperature gradient, and a breakdown of the stratospheric polar vortex. Substantial changes in the amplitude of stationary planetary wave numbers 1, 2, and 3 occur as the zonal mean zonal wind evolves. The simulations also show a cooling in the mesosphere and a warming in the lower thermosphere consistent with observations. The magnitude of this particular SSW is modest, belonging to the category of minor warming. In the lower thermosphere the amplitude of diurnal, semidiurnal, and terdiurnal, eastward and westward propagating tidal modes change substantially during the event. Since the magnitude of the warming is minor and the tidal interactions with the mean flow and planetary waves are complex, the one-to-one correspondence between tidal amplitudes in the lower thermosphere and the zonal mean and stationary waves in the stratosphere is not entirely obvious. The increase in the magnitude of the terdiurnal tide (TW3) in the lower thermosphere has the clearest correlation with the SSW, although the timing appears delayed by about three days. The fast group velocity of the long vertical wavelength TW3 tide would suggest a faster onset for the direct propagation of the tide from the lower atmosphere. It is possible that changes in the magnitude of the diurnal and semidiurnal tides, with their slower vertical propagation, may interact in the lower thermosphere to introduce a terdiurnal tide with a longer delay. An increase in TW3 in the lower thermosphere would be expected to alter the local time variation of the electrodynamic response. The day-to-day changes in the lower thermosphere winds from WAM are shown to introduce variability in the magnitude of dayside low latitude electric fields, with a tendency during the warming for the dayside vertical drift to be larger and occur earlier, and for the afternoon minimum to be smaller. The numerical simulations suggest that it is quite feasible that a major SSW, with a magnitude seen in January 2009, could cause large changes in lower thermosphere electrodynamics and hence in total electron content.
C1 [Fuller-Rowell, Tim; Wu, Fei; Fang, Tzu-Wei; Araujo-Pradere, Eduardo] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80303 USA.
[Akmaev, Rashid] NOAA, Space Weather Predict Ctr, Boulder, CO 80305 USA.
RP Fuller-Rowell, T (reprint author), Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80303 USA.
EM tim.fuller-rowell@noaa.gov
RI Fang, Tzu-Wei/I-4882-2013
FU NASA; Air Force Office of Scientific Research (AFOSR) Multidisciplinary
University Research Initiative (MURI)
FX This work has been supported in part by the NASA Heliophysics Theory
programs as well as the Air Force Office of Scientific Research (AFOSR)
Multidisciplinary University Research Initiative (MURI) program.
NR 40
TC 57
Z9 57
U1 0
U2 6
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-9380
EI 2169-9402
J9 J GEOPHYS RES-SPACE
JI J. Geophys. Res-Space Phys.
PD OCT 15
PY 2010
VL 115
AR A00G08
DI 10.1029/2010JA015524
PG 13
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA 666EW
UT WOS:000283097100005
ER
PT J
AU Schmied, R
Leibfried, D
Spreeuw, RJC
Whitlock, S
AF Schmied, Roman
Leibfried, Dietrich
Spreeuw, Robert J. C.
Whitlock, Shannon
TI Optimized magnetic lattices for ultracold atomic ensembles
SO NEW JOURNAL OF PHYSICS
LA English
DT Article
ID BOSE-EINSTEIN CONDENSATE; OPTICAL LATTICES; RYDBERG BLOCKADE; TRAPS;
GASES; PHYSICS; ION
AB We introduce a general method for designing tailored lattices of magnetic microtraps for ultracold atoms on the basis of patterned permanently magnetized films. A fast numerical algorithm is used to automatically generate patterns that provide optimal atom confinement while respecting desired lattice symmetries and trap parameters. The algorithm can produce finite and infinite lattices of any plane symmetry; we focus specifically on square and triangular lattices, which are of interest for future experiments. Typical trap parameters, as well as the impact of realistic imperfections such as finite lithographic resolution and magnetic inhomogeneity, are discussed. The designer lattices presented open new avenues for quantum simulation and quantum information processing with ultracold atoms on atom chips.
C1 [Schmied, Roman] Max Planck Inst Quantum Opt, Garching, Germany.
[Leibfried, Dietrich] Natl Inst Stand & Technol, Boulder, CO USA.
[Spreeuw, Robert J. C.; Whitlock, Shannon] Univ Amsterdam, Van der Waals Zeeman Inst, NL-1012 WX Amsterdam, Netherlands.
RP Schmied, R (reprint author), Univ Basel, Dept Phys, CH-4003 Basel, Switzerland.
EM Roman.Schmied@unibas.ch; whitlock@physi.uni-heidelberg.de
RI Whitlock, Shannon/B-3312-2010; Spreeuw, Robert/B-7571-2008;
OI Spreeuw, Robert/0000-0002-2631-5698; Schmied, Roman/0000-0001-5713-5262
FU Deutsche Forschungsgemeinschaft [Forschungsgruppe 635]; European Union
(ACUTE); DARPA; NSA; ONR; IARPA; Sandia National Labs; NIST; Marie-Curie
fellowship [PIIF-GA-2008-220794]; Stichting voor Fundamenteel Onderzoek
der Materie (FOM); Nederlandse Organisatie voor Wetenschappelijk
Onderzoek (NWO)
FX We thank C F Ockeloen for initiating the calculations about loading the
lattice microtraps. R Schmied was supported by the Deutsche
Forschungsgemeinschaft (Forschungsgruppe 635) and the European Union
(ACUTE). D Leibfried was supported by DARPA, NSA, ONR, IARPA, Sandia
National Labs and the NIST Quantum Information Program. S Whitlock
acknowledges support from a Marie-Curie fellowship
(PIIF-GA-2008-220794). S Whitlock and R J C Spreeuw acknowledge funding
from the Stichting voor Fundamenteel Onderzoek der Materie (FOM), which
is financially supported by the Nederlandse Organisatie voor
Wetenschappelijk Onderzoek (NWO).
NR 53
TC 16
Z9 16
U1 0
U2 1
PU IOP PUBLISHING LTD
PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 1367-2630
J9 NEW J PHYS
JI New J. Phys.
PD OCT 15
PY 2010
VL 12
AR 103029
DI 10.1088/1367-2630/12/10/103029
PG 19
WC Physics, Multidisciplinary
SC Physics
GA 687HE
UT WOS:000284768800004
ER
PT J
AU Msadek, R
Dixon, KW
Delworth, TL
Hurlin, W
AF Msadek, R.
Dixon, K. W.
Delworth, T. L.
Hurlin, W.
TI Assessing the predictability of the Atlantic meridional overturning
circulation and associated fingerprints
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID COUPLED CLIMATE MODELS; NORTH-ATLANTIC; VARIABILITY; ENSEMBLE
AB The North Atlantic is among the few places where decadal climate variations are considered potentially predictable. The physical mechanisms of the decadal variability are hypothesized to be associated with fluctuations of the Atlantic meridional overturning circulation (AMOC). Perfect model predictability experiments using the GFDL CM2.1 climate model are analyzed to investigate the potential predictability of the AMOC. Results indicate that the AMOC is predictable up to 20 years. We further connect AMOC predictability to readily observable fields. We show that modeled surface and subsurface signatures of AMOC variations defined by characteristic patterns of sea surface height, subsurface temperature, and upper ocean heat content anomalies, have a potential predictability similar to the AMOC's. Since we have longer observational records for these quantities than for direct measurements of the AMOC, our study highlights a potentially new promising method for monitoring AMOC variations, and hence assessing the predictability of the real climate system. Citation: Msadek, R., K. W. Dixon, T. L. Delworth, and W. Hurlin (2010), Assessing the predictability of the Atlantic meridional overturning circulation and associated fingerprints, Geophys. Res. Lett., 37, L19608, doi: 10.1029/2010GL044517.
C1 [Msadek, R.] Princeton Univ, NOAA, Geophys Fluid Dynam Lab, Atmospher & Ocean Sci Program, Princeton, NJ 08540 USA.
RP Msadek, R (reprint author), Princeton Univ, NOAA, Geophys Fluid Dynam Lab, Atmospher & Ocean Sci Program, 201 Forrestal Rd, Princeton, NJ 08540 USA.
EM rym.msadek@noaa.gov
RI Delworth, Thomas/C-5191-2014; Msadek, Rym/C-7752-2014; Dixon,
Keith/L-7120-2015
OI Msadek, Rym/0000-0003-0450-4815; Dixon, Keith/0000-0003-3044-326X
FU NOAA Climate Program Office
FX R. Msadek is supported by a grant from the NOAA Climate Program Office
administered by the Visiting Scientist Program of Princeton University
and NOAA/GFDL. We thank Stephen M. Griffies, Rong Zhang and three
anonymous reviewers for thoughtful comments that helped to improve the
manuscript.
NR 15
TC 53
Z9 54
U1 0
U2 6
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
EI 1944-8007
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD OCT 14
PY 2010
VL 37
AR L19608
DI 10.1029/2010GL044517
PG 5
WC Geosciences, Multidisciplinary
SC Geology
GA 666AE
UT WOS:000283078600002
ER
PT J
AU Metzl, N
Corbiere, A
Reverdin, G
Lenton, A
Takahashi, T
Olsen, A
Johannessen, T
Pierrot, D
Wanninkhof, R
Olafsdottir, SR
Olafsson, J
Ramonet, M
AF Metzl, Nicolas
Corbiere, Antoine
Reverdin, Gilles
Lenton, Andrew
Takahashi, Taro
Olsen, Are
Johannessen, Truls
Pierrot, Denis
Wanninkhof, Rik
Olafsdottir, Solveig R.
Olafsson, Jon
Ramonet, Michel
TI Recent acceleration of the sea surface fCO(2) growth rate in the North
Atlantic subpolar gyre (1993-2008) revealed by winter observations
SO GLOBAL BIOGEOCHEMICAL CYCLES
LA English
DT Article
ID ANTHROPOGENIC CO2; DISSOCIATION-CONSTANTS; ATMOSPHERIC CO2;
CARBONIC-ACID; INORGANIC CARBON; OCEAN; SINK; TRENDS; VARIABILITY;
INCREASE
AB Recent studies based on ocean and atmospheric carbon dioxide (CO2) observations, suggesting that the ocean carbon uptake has been reduced, may help explain the increase in the fraction of anthropogenic CO2 emissions that remain in the atmosphere. Is it a response to climate change or a signal of ocean natural variability or both? Regional process analyses are needed to follow the ocean carbon uptake and to enable better attributions of the observed changes. Here, we describe the evolution of the surface ocean CO2 fugacity (fCO(2)(oc)) over the period 1993-2008 in the North Atlantic subpolar gyre (NASPG). This analysis is based primarily on observations of dissolved inorganic carbon (DIC) and total alkalinity (TA) conducted at different seasons in the NASPG between Iceland and Canada. The fCO(2)(oc) trends based on DIC and TA data are also compared with direct fCO(2) measurements obtained between 2003 and 2007 in the same region. During winters 1993-2003, the fCO(2)(oc) growth rate was 3.7 (+/-0.6) mu atm yr(-1), higher than in the atmosphere, 1.8 (+/-0.1) mu atm yr(-1). This translates to a reduction of the ocean carbon uptake primarily explained by sea surface warming, up to 0.24 (+/-0.04) C yr(-1). This warming is a consequence of advection of warm water northward from the North Atlantic into the Irminger basin, which occurred as the North Atlantic Oscillation (NAO) index moved into a negative phase in winter 1995/1996. In winter 2001-2008, the fCO(2)(oc) rise was particularly fast, between 5.8 (+/-1.1) and 7.2 (+/-1.3) mu atm yr(-1) depending on the region, more than twice the atmospheric growth rate of 2.1 (+/-0.2) mu atm yr(-1), and in the winter of 2007-2008 the area was supersaturated with CO2. As opposed to the 1990s, this appears to be almost entirely due to changes in seawater carbonate chemistry, the combination of increasing DIC and decreasing of TA. The rapid fCO(2)(oc) increase was not only driven by regional uptake of anthropogenic CO2 but was also likely controlled by a recent increase in convective processes-vertical mixing in the NASPG and cannot be directly associated with NAO variability. The fCO(2)(oc) increase observed in 2001-2008 leads to a significant drop in pH of -0.069 (+/-0.007) decade(-1).
C1 [Metzl, Nicolas; Corbiere, Antoine; Reverdin, Gilles; Lenton, Andrew] Univ Paris 06, CNRS, IPSL, Lab Oceanog & Climat Expt & Approches Numer, F-75252 Paris, France.
[Takahashi, Taro] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA.
[Olsen, Are] UNI Res, Bjerknes Ctr Climate Res, N-5007 Bergen, Norway.
[Olsen, Are] Univ Gothenburg, Dept Chem, Gothenburg, Sweden.
[Johannessen, Truls] Univ Bergen, Inst Geophys, Bergen, Norway.
[Johannessen, Truls] Univ Bergen, UNIFOB AS, Bjerknes Ctr Climate Res, Bergen, Norway.
[Pierrot, Denis] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Cooperat Inst Marine & Atmospher Studies, Miami, FL 33149 USA.
[Wanninkhof, Rik] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
[Olafsdottir, Solveig R.; Olafsson, Jon] Marine Res Inst, IS-121 Reykjavik, Iceland.
[Olafsson, Jon] Univ Iceland, Inst Earth Sci, Reykjavik, Iceland.
[Ramonet, Michel] UVSQ, CNRS CEA, IPSL, Lab Sci Climat & Environm, F-91191 Gif Sur Yvette, France.
RP Metzl, N (reprint author), Univ Paris 06, CNRS, IPSL, Lab Oceanog & Climat Expt & Approches Numer, Case 100,4 Pl Jussieu, F-75252 Paris, France.
EM nicolas.metzl@locean-ipsl.upmc.fr; antoinecorbiere@aol.fr;
gilles.reverdin@locean-ipsl.upmc.fr; taka@ldeo.columbia.edu;
are.olsen@gfi.uib.no; truls.johannessen@gfi.uib.no;
denis.pierrot@noaa.gov; rik.wanninkhof@noaa.gov; solveig@hafro.is;
jon@hafro.is; michel.ramonet@lsce.ipsl.fr
RI Olsen, Are/A-1511-2011; Lenton, Andrew/D-2077-2012; Pierrot,
Denis/A-7459-2014
OI Olsen, Are/0000-0003-1696-9142; Lenton, Andrew/0000-0001-9437-8896;
Pierrot, Denis/0000-0002-0374-3825
FU Institut National des Sciences de l'Univers (INSU); Institut Paul Emile
Victor (IPEV) in France; French program LEFE/FlamenCO2; Swedish National
Space Board [511176, 96/05]; Norwegian Research Council [185093, 178167]
FX The SURATLANT Project is supported by Institut National des Sciences de
l'Univers (INSU, as contribution of the ORE SSS) and Institut Paul Emile
Victor (IPEV) in France. This work is also supported by French program
LEFE/FlamenCO2, a component of SOLAS-France. We thank the EIMSKIP
Company, the captains and crews of the M/V Skogafoss, M/V Godafoss, M/V
Selfoss and M/V Reykjafoss, all the very helpful embarked observers for
their cooperation in this work, as well as the captains and crew of the
M/V Nuka Arctica of the Royal Arctic Lines. We thank Magnus Danielsen
for salinity analysis done at the Marine Research Institute in
Reykjavik. We also thank the Service National d'Analyze des Parametres
Oceanique du CO2 (SNAPO-CO2) at LOCEAN/IPSL for DIC and TA
analysis. Support from the European Integrated Project CARBOOCEAN
(511176), RESCUE-II (96/05) of the Swedish National Space Board and
CARBON-HEAT (185093) and A-CARB (178167) of the Norwegian Research
Council is also appreciated. Underway pCO2 data was collected
on the Skogafoss as part of the "pCO2 on ships effort" funded
by the Climate Observation Division of the Climate office of NOAA. The
authors would like to thank all people working for the SeaWiFS Project
(NASA Code 970.2). We also express warms thanks to Galen McKinley and an
anonymous reviewer for their positive comments and helpful questions.
NR 66
TC 30
Z9 30
U1 5
U2 26
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0886-6236
J9 GLOBAL BIOGEOCHEM CY
JI Glob. Biogeochem. Cycle
PD OCT 14
PY 2010
VL 24
AR GB4004
DI 10.1029/2009GB003658
PG 13
WC Environmental Sciences; Geosciences, Multidisciplinary; Meteorology &
Atmospheric Sciences
SC Environmental Sciences & Ecology; Geology; Meteorology & Atmospheric
Sciences
GA 666AX
UT WOS:000283080700001
ER
PT J
AU Li, X
Hong, KL
Liu, Y
Shew, CY
Liu, E
Herwig, KW
Smith, GS
Zhao, JP
Zhang, GZ
Pispas, S
Chen, WR
AF Li, Xin
Hong, Kunlun
Liu, Yun
Shew, Chwen-Yang
Liu, Emily
Herwig, Kenneth W.
Smith, Gregory S.
Zhao, Junpeng
Zhang, Guangzhao
Pispas, Stergios
Chen, Wei-Ren
TI Water distributions in polystyrene-block-poly[styrene-g-poly(ethylene
oxide)] block grafted copolymer system in aqueous solutions revealed by
contrast variation small angle neutron scattering study
SO JOURNAL OF CHEMICAL PHYSICS
LA English
DT Article
ID DODECYL-SULFATE MICELLES; TRIBLOCK COPOLYMER; DIBLOCK COPOLYMERS;
POLYSTYRENE; DENDRIMERS; SANS; MICROSTRUCTURE; NANOSTRUCTURES;
CONFORMATION; COUNTERION
AB We develop an experimental approach to analyze the water distribution around a core-shell micelle formed by polystyrene-block-poly[styrene-g-poly(ethylene oxide (PEO)] block copolymers in aqueous media at a fixed polymeric concentration of 10 mg/ml through contrast variation small angle neutron scattering (SANS) study. Through varying the D(2)O/H(2)O ratio, the scattering contributions from the water molecules and the micellar constituent components can be determined. Based on the commonly used core-shell model, a theoretical coherent scattering cross section incorporating the effect of water penetration is developed and used to analyze the SANS I(Q). We have successfully quantified the intramicellar water distribution and found that the overall micellar hydration level increases with the increase in the molecular weight of hydrophilic PEO side chains. Our work presents a practical experimental means for evaluating the intramacromolecular solvent distributions of general soft matter systems. (c) 2010 American Institute of Physics. [doi:10.1063/1.343331]
C1 [Hong, Kunlun] Oak Ridge Natl Lab, Ctr Nanophase Mat Sci, Oak Ridge, TN 37831 USA.
[Li, Xin; Herwig, Kenneth W.; Smith, Gregory S.; Chen, Wei-Ren] Oak Ridge Natl Lab, Neutron Scattering Sci Div, Oak Ridge, TN 37831 USA.
[Li, Xin; Liu, Emily] Rensselaer Polytech Inst, Dept Mech Aerosp & Nucl Engn, Troy, NY 12180 USA.
[Liu, Yun] NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Liu, Yun] Univ Delaware, Dept Chem Engn, Newark, DE 19716 USA.
[Shew, Chwen-Yang] CUNY Coll Staten Isl, Dept Chem, Staten Isl, NY 10314 USA.
[Zhao, Junpeng; Zhang, Guangzhao] Univ Sci & Technol China, Hefei Natl Lab Phys Sci Microscale, Hefei 230026, Anhui, Peoples R China.
[Pispas, Stergios] Natl Hellen Res Fdn, Inst Theoret & Phys Chem, GR-11635 Athens, Greece.
[Chen, Wei-Ren] Oak Ridge Natl Lab, Joint Inst Neutron Sci, Oak Ridge, TN 37831 USA.
[Chen, Wei-Ren] Univ Tennessee, Dept Chem & Biomol Engn, Knoxville, TN 37996 USA.
RP Hong, KL (reprint author), Oak Ridge Natl Lab, Ctr Nanophase Mat Sci, Oak Ridge, TN 37831 USA.
EM hongkq@ornl.gov; liue@rpi.edu; chenw@ornl.gov
RI Herwig, Kenneth/F-4787-2011; Liu, Yun/F-6516-2012; Li, Xin/K-9646-2013;
nhrf, tpci/M-8699-2013; Smith, Gregory/D-1659-2016; Hong,
Kunlun/E-9787-2015
OI Liu, Yun/0000-0002-0944-3153; Li, Xin/0000-0003-0606-434X; Smith,
Gregory/0000-0001-5659-1805; Hong, Kunlun/0000-0002-2852-5111
FU HFIR ORNL [IPTS-2301]; NCNR NIST; U.S. Department of Energy
[DE-FG07-07ID14889]; U.S. Nuclear Regulatory Commission [NRC-38-08-950];
CUNY; Laboratory Directed Research and Development Program [05272];
Scientific User Facilities Division, Office of Basic Energy Sciences,
U.S. Department of Energy
FX The support of HFIR ORNL (Grant No. IPTS-2301) and NCNR NIST is greatly
acknowledged. The research carried out at the Center for Nanophase
Materials Sciences, Oak Ridge National Laboratory, was sponsored by the
Scientific User Facilities Division, Office of Basic Energy Sciences,
U.S. Department of Energy. X.L. and E.L. acknowledge the financial
support by U.S. Department of Energy under NERI-C Award No.
DE-FG07-07ID14889 and U.S. Nuclear Regulatory Commission under Award No.
NRC-38-08-950. C.Y.S. thanks the support from the CUNY PSC grants. We
also thank the support from the Laboratory Directed Research and
Development Program (Project ID No. 05272) of ORNL.
NR 49
TC 9
Z9 9
U1 0
U2 21
PU AMER INST PHYSICS
PI MELVILLE
PA CIRCULATION & FULFILLMENT DIV, 2 HUNTINGTON QUADRANGLE, STE 1 N O 1,
MELVILLE, NY 11747-4501 USA
SN 0021-9606
J9 J CHEM PHYS
JI J. Chem. Phys.
PD OCT 14
PY 2010
VL 133
IS 14
AR 144912
DI 10.1063/1.3493331
PG 8
WC Chemistry, Physical; Physics, Atomic, Molecular & Chemical
SC Chemistry; Physics
GA 667NN
UT WOS:000283200400069
PM 20950046
ER
PT J
AU Seltzer, SJ
Michalak, DJ
Donaldson, MH
Balabas, MV
Barber, SK
Bernasek, SL
Bouchiat, MA
Hexemer, A
Hibberd, AM
Kimball, DFJ
Jaye, C
Karaulanov, T
Narducci, FA
Rangwala, SA
Robinson, HG
Shmakov, AK
Voronov, DL
Yashchuk, VV
Pines, A
Budker, D
AF Seltzer, S. J.
Michalak, D. J.
Donaldson, M. H.
Balabas, M. V.
Barber, S. K.
Bernasek, S. L.
Bouchiat, M. -A.
Hexemer, A.
Hibberd, A. M.
Kimball, D. F. Jackson
Jaye, C.
Karaulanov, T.
Narducci, F. A.
Rangwala, S. A.
Robinson, H. G.
Shmakov, A. K.
Voronov, D. L.
Yashchuk, V. V.
Pines, A.
Budker, D.
TI Investigation of antirelaxation coatings for alkali-metal vapor cells
using surface science techniques
SO JOURNAL OF CHEMICAL PHYSICS
LA English
DT Article
ID ATOMIC FORCE MICROSCOPY; WALL-COATED CELL; PARAFFIN CRYSTALS; POLARIZED
XE-129; NORMAL-ALKANES; MAGNETOMETER; RELAXATION; PHASE; LIGHT;
SPECTROSCOPY
AB Many technologies based on cells containing alkali-metal atomic vapor benefit from the use of antirelaxation surface coatings in order to preserve atomic spin polarization. In particular, paraffin has been used for this purpose for several decades and has been demonstrated to allow an atom to experience up to 10 000 collisions with the walls of its container without depolarizing, but the details of its operation remain poorly understood. We apply modern surface and bulk techniques to the study of paraffin coatings in order to characterize the properties that enable the effective preservation of alkali spin polarization. These methods include Fourier transform infrared spectroscopy, differential scanning calorimetry, atomic force microscopy, near-edge x-ray absorption fine structure spectroscopy, and x-ray photoelectron spectroscopy. We also compare the light-induced atomic desorption yields of several different paraffin materials. Experimental results include the determination that crystallinity of the coating material is unnecessary, and the detection of CvC double bonds present within a particular class of effective paraffin coatings. Further study should lead to the development of more robust paraffin antirelaxation coatings, as well as the design and synthesis of new classes of coating materials. (C) 2010 American Institute of Physics. [doi:10.1063/1.3489922]
C1 [Seltzer, S. J.; Michalak, D. J.; Donaldson, M. H.; Pines, A.] Univ Calif Berkeley, Lawrence Berkeley Lab, Div Mat Sci, Berkeley, CA 94720 USA.
[Seltzer, S. J.; Michalak, D. J.; Donaldson, M. H.; Pines, A.] Univ Calif Berkeley, Dept Chem, Berkeley, CA 94720 USA.
[Balabas, M. V.] SI Vavilov State Opt Inst, St Petersburg 199034, Russia.
[Barber, S. K.; Hexemer, A.; Voronov, D. L.; Yashchuk, V. V.] Univ Calif Berkeley, Lawrence Berkeley Lab, Adv Light Source, Berkeley, CA 94720 USA.
[Bernasek, S. L.; Hibberd, A. M.] Princeton Univ, Dept Chem, Princeton, NJ 08544 USA.
[Bouchiat, M. -A.] Ecole Normale Super, Dept Phys, Lab Kastler Brossel, F-75231 Paris, France.
[Kimball, D. F. Jackson] Calif State Univ E Bay, Dept Phys, Hayward, CA 94542 USA.
[Jaye, C.] NIST, Div Ceram, Mat Sci & Engn Lab, Gaithersburg, MD 20899 USA.
[Karaulanov, T.; Shmakov, A. K.; Budker, D.] Univ Calif Berkeley, Dept Phys, Berkeley, CA 94720 USA.
[Narducci, F. A.] USN, Air Syst Command, EO Sensors Div, Patuxent River, MD 20670 USA.
[Rangwala, S. A.] Raman Res Inst, Bangalore 560080, Karnataka, India.
[Robinson, H. G.] NIST, Div Time & Frequency, Boulder, CO 80305 USA.
[Budker, D.] Univ Calif Berkeley, Lawrence Berkeley Lab, Div Nucl Sci, Berkeley, CA 94720 USA.
RP Seltzer, SJ (reprint author), Univ Calif Berkeley, Lawrence Berkeley Lab, Div Mat Sci, Berkeley, CA 94720 USA.
EM seltzer@berkeley.edu; budker@berkeley.edu
RI Rangwala, Sadiq/E-6899-2012; Balabas, Mikhail/A-5273-2012; Budker,
Dmitry/F-7580-2016
OI Balabas, Mikhail/0000-0002-5383-7897; Budker, Dmitry/0000-0002-7356-4814
FU Office of Science, Office of Basic Energy Sciences, Materials Sciences
Division and Nuclear Science Division, of the U. S. Department of Energy
[DE-AC02-05CH11231]; NSF/DST [PHY-0425916]; Office of Naval Research
(ONR) [N0001409WX21049]
FX The authors thank Daniel Fischer, Kristin Schmidt, and Ed Kramer for
assistance with the NEXAFS measurements, and Joel Ager, Joshua Wnuk,
David Trease, and Gwendal Kervern for helpful discussions and other
assistance. S.J.S., D.J.M., M. H. D., A. P., and D. B., the Advanced
Light Source, and the DSC, FTIR, and AFM studies were supported by the
Director, Office of Science, Office of Basic Energy Sciences, Materials
Sciences Division and Nuclear Science Division, of the U. S. Department
of Energy under Contract No. DE-AC02-05CH11231 at Lawrence Berkeley
National Laboratory. Other parts of this work were funded by the NSF/DST
under Grant No. PHY-0425916 for U.S.-India cooperative research, by an
Office of Naval Research (ONR) MURI grant, and by ONR under Grant No.
N0001409WX21049.
NR 81
TC 20
Z9 20
U1 1
U2 31
PU AMER INST PHYSICS
PI MELVILLE
PA CIRCULATION & FULFILLMENT DIV, 2 HUNTINGTON QUADRANGLE, STE 1 N O 1,
MELVILLE, NY 11747-4501 USA
SN 0021-9606
J9 J CHEM PHYS
JI J. Chem. Phys.
PD OCT 14
PY 2010
VL 133
IS 14
AR 144703
DI 10.1063/1.3489922
PG 11
WC Chemistry, Physical; Physics, Atomic, Molecular & Chemical
SC Chemistry; Physics
GA 667NN
UT WOS:000283200400049
PM 20950026
ER
PT J
AU Meyer, ER
Bohn, JL
AF Meyer, Edmund R.
Bohn, John L.
TI Product-state control of bi-alkali-metal chemical reactions
SO PHYSICAL REVIEW A
LA English
DT Article
ID GROUND ELECTRONIC-STATE; POLAR-MOLECULES; ANGSTROM
AB We consider ultracold, chemically reactive scattering collisions of the diatomic molecules KRb. When two such molecules collide in an ultracold gas, we find that they are energetically forbidden from reacting to form the trimer species K(2)Rb or Rb(2)K, and hence can only react via the bond-swapping reaction 2 KRb -> K(2) + Rb(2). Moreover, the tiny energy released in this reaction can in principle be set to zero by applying electric or microwave fields, implying a means of controlling the available reaction channels in a chemical reaction.
C1 [Meyer, Edmund R.] Natl Inst Stand & Technol, Joint Inst Lab Astrophys, Boulder, CO 80309 USA.
Univ Colorado, Dept Phys, Boulder, CO 80309 USA.
RP Meyer, ER (reprint author), Natl Inst Stand & Technol, Joint Inst Lab Astrophys, Boulder, CO 80309 USA.
EM meyere@murphy.colorado.edu
FU NSF
FX The authors acknowledge useful discussions with G. Quemener and C. H.
Greene, as well as funding from the NSF.
NR 29
TC 18
Z9 18
U1 2
U2 3
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 1050-2947
J9 PHYS REV A
JI Phys. Rev. A
PD OCT 14
PY 2010
VL 82
IS 4
AR 042707
DI 10.1103/PhysRevA.82.042707
PG 6
WC Optics; Physics, Atomic, Molecular & Chemical
SC Optics; Physics
GA 664CP
UT WOS:000282936800004
ER
PT J
AU Tassel, C
Kang, J
Lee, C
Hernandez, O
Qiu, Y
Paulus, W
Collet, E
Lake, B
Guidi, T
Whangbo, MH
Ritter, C
Kageyama, H
Lee, SH
AF Tassel, C.
Kang, J.
Lee, C.
Hernandez, O.
Qiu, Y.
Paulus, W.
Collet, E.
Lake, B.
Guidi, T.
Whangbo, M-H
Ritter, C.
Kageyama, H.
Lee, S-H
TI Ferromagnetically Coupled Shastry-Sutherland Quantum Spin Singlets in
(CuCl)LaNb2O7
SO PHYSICAL REVIEW LETTERS
LA English
DT Article
ID FRUSTRATED SQUARE-LATTICE; AUGMENTED-WAVE METHOD; CL
AB A thorough crystal structure determination at very low temperature of (CuCl)LaNb2O7, originally proposed as a spin-1/2 square-lattice antiferromagnet, is reported thanks to the use of single-crystal x-ray diffraction and powder neutron diffraction. State-of-the-art calculations (maximum entropy method) reveal that (CuCl)LaNb2O7 is orthorhombic with Pbam symmetry. First-principles calculations demonstrate that the dominant magnetic interactions are antiferromagnetic between fourth nearest neighbors with a Cu-Cl-Cl-Cu exchange path, which lead to the formation of spin singlets. The two strongest interactions between the singlets are ferromagnetic, which makes (CuCl)LaNb2O7 the first system of ferromagnetically coupled Shastry-Sutherland quantum spin singlets.
C1 [Tassel, C.; Kageyama, H.] Kyoto Univ, Grad Sch Engn, Dept Energy & Hydrocarbon Chem, Kyoto 6158510, Japan.
[Kang, J.; Lee, C.; Whangbo, M-H] N Carolina State Univ, Dept Chem, Raleigh, NC 27695 USA.
[Hernandez, O.; Paulus, W.] Univ Rennes 1, CNRS, Sci Chim Rennes UMR 6226, F-35042 Rennes, France.
[Qiu, Y.] NIST, NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Collet, E.] Univ Rennes 1, Inst Phys Rennes, CNRS, UMR 6251, F-35042 Rennes, France.
[Lake, B.; Guidi, T.] Helmholtz Zentrum Berlin Mat & Energie, D-14109 Berlin, Germany.
[Lake, B.] Tech Univ Berlin, Inst Festkorperphys, D-10623 Berlin, Germany.
[Guidi, T.] Rutherford Appleton Lab, ISIS Facil, Didcot OX11 0QX, Oxon, England.
[Ritter, C.] Inst Laue Langevin, F-38042 Grenoble, France.
[Lee, S-H] Univ Virginia, Dept Phys, Charlottesville, VA 22904 USA.
RP Tassel, C (reprint author), Kyoto Univ, Grad Sch Engn, Dept Energy & Hydrocarbon Chem, Kyoto 6158510, Japan.
RI Kageyama, Hiroshi/A-4602-2010; Tassel, Cedric/L-5051-2014; Collet,
Eric/N-8816-2013;
OI Collet, Eric/0000-0003-0810-7411; Lake, Bella/0000-0003-0034-0964
FU DOE [DE-FG02-86ER45259]; NERSC and HPC Centers; U.S. NSF [DMR-0454672,
DMR-0903977]
FX Work at NCSU was supported by the DOE (DE-FG02-86ER45259) and by the
resources of the NERSC and HPC Centers. Work at NCNR and UVA were
supported by the U.S. NSF under Agreement No. DMR-0454672 and
DMR-0903977, respectively. C. T. and H. K. acknowledge Science Research
on Priority Area (19052004) from MEXT of Japan.
NR 22
TC 21
Z9 21
U1 0
U2 14
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 0031-9007
J9 PHYS REV LETT
JI Phys. Rev. Lett.
PD OCT 14
PY 2010
VL 105
IS 16
AR 167205
DI 10.1103/PhysRevLett.105.167205
PG 4
WC Physics, Multidisciplinary
SC Physics
GA 664GR
UT WOS:000282948900010
PM 21231006
ER
PT J
AU Kilbourne, KH
Quinn, TM
Webb, R
Guilderson, T
Nyberg, J
Winter, A
AF Kilbourne, K. H.
Quinn, T. M.
Webb, R.
Guilderson, T.
Nyberg, J.
Winter, A.
TI Coral windows onto seasonal climate variability in the northern
Caribbean since 1479
SO GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
LA English
DT Article
DE Little Ice Age; seasonality; coral; Caribbean; Montastrea; paleoclimate
ID SEA-SURFACE TEMPERATURES; INTERTROPICAL CONVERGENCE ZONE; O-18 ISOTOPIC
DISEQUILIBRIUM; HEMISPHERE WARM POOL; ICE-AGE; BIOLOGICAL CARBONATES;
LATE HOLOCENE; SR/CA RATIOS; OXYGEN; WATER
AB Mean surface ocean conditions in the Caribbean were up to similar to 2 degrees C cooler than today at times during the Little Ice Age. The seasonal context for such mean state changes is important for determining the mechanisms involved. We reconstructed surface ocean conditions in southwest Puerto Rico at approximately monthly resolution over eight 4-12 year periods during the last similar to 520 years to test if the seasonal cycles of temperature or salinity varied with mean state. We carried out paired analyses of Sr/Ca and delta O-18 for two coral cores. The delta O-18 data contained clear annual cycles and were significantly correlated to temperature during the 20th century calibration periods (1993-2004 and 1902-1912, r = 0.73). The Sr/Ca data contained high-frequency noise that obscured the seasonal cycles, although the centennial variability matched that of the coral delta O-18, indicating a common forcing that is likely temperature. The seasonal coral delta O-18 amplitude averaged 0.60 +/- 0.17 parts per thousand, with none of the periods significantly different from the most recent. The simplest explanation is that the amplitudes of seasonal seawater delta O-18 and temperature variations were not different from today. Previous work in the southern Caribbean indicates that the Intertropical Convergence Zone was shifted southward or weaker during the Little Ice Age, and we speculate about how this could occur with no apparent affect on seasonality in the northern Caribbean.
C1 [Kilbourne, K. H.; Quinn, T. M.] Univ Maryland, Ctr Environm Sci, Chesapeake Biol Lab, Solomons, MD 20688 USA.
[Kilbourne, K. H.; Quinn, T. M.] Univ S Florida, Coll Marine Sci, St Petersburg, FL 33701 USA.
[Quinn, T. M.] Univ Texas Austin, Jackson Sch Geosci, Dept Geol Sci, Austin, TX 78712 USA.
[Webb, R.] NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA.
[Guilderson, T.] Lawrence Livermore Natl Lab, Ctr Accelerator Mass Spectrometry, Livermore, CA 94550 USA.
[Guilderson, T.] Univ Calif Santa Cruz, Dept Ocean Sci, Santa Cruz, CA 95064 USA.
[Guilderson, T.] Univ Calif Santa Cruz, Inst Marine Sci, Santa Cruz, CA 95064 USA.
[Nyberg, J.] Geol Survey Sweden, SE-75128 Uppsala, Sweden.
[Winter, A.] Univ Puerto Rico, Dept Marine Sci, Mayaguez, PR 00681 USA.
RP Kilbourne, KH (reprint author), Univ Maryland, Ctr Environm Sci, Chesapeake Biol Lab, Solomons, MD 20688 USA.
EM kilbourn@cbl.umces.edu
RI Rinaldi2, Carlos/D-4479-2011; Quinn, Terrence/A-5755-2008; Kilbourne,
Kelly /D-6560-2012
OI Kilbourne, Kelly /0000-0001-7864-8438
FU National Science Foundation [OCE-0327420]; Elsie and William Knight
Oceanographic Fellowship
FX Thank you to Ethan Goddard for analytical support and to Fred Taylor,
Milton Carlo, and Peter Swart for help with coral coring. We also thank
Kevin Helmle for his help cutting and X-raying the cores. Funding for
this project included the National Science Foundation grant OCE-0327420
to T. M. Q., T. P. G., and R. S. W. and the Elsie and William Knight
Oceanographic Fellowship to K. H. K. This manuscript is contribution
4363 of the University of Maryland Center for Environmental Science.
NR 46
TC 6
Z9 6
U1 1
U2 12
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 1525-2027
J9 GEOCHEM GEOPHY GEOSY
JI Geochem. Geophys. Geosyst.
PD OCT 13
PY 2010
VL 11
AR Q10006
DI 10.1029/2010GC003171
PG 11
WC Geochemistry & Geophysics
SC Geochemistry & Geophysics
GA 665YV
UT WOS:000283074900001
ER
PT J
AU Son, SW
Gerber, EP
Perlwitz, J
Polvani, LM
Gillett, NP
Seo, KH
Eyring, V
Shepherd, TG
Waugh, D
Akiyoshi, H
Austin, J
Baumgaertner, A
Bekki, S
Braesicke, P
Bruhl, C
Butchart, N
Chipperfield, MP
Cugnet, D
Dameris, M
Dhomse, S
Frith, S
Garny, H
Garcia, R
Hardiman, SC
Jockel, P
Lamarque, JF
Mancini, E
Marchand, M
Michou, M
Nakamura, T
Morgenstern, O
Pitari, G
Plummer, DA
Pyle, J
Rozanov, E
Scinocca, JF
Shibata, K
Smale, D
Teyssedre, H
Tian, W
Yamashita, Y
AF Son, S. -W.
Gerber, E. P.
Perlwitz, J.
Polvani, L. M.
Gillett, N. P.
Seo, K. -H.
Eyring, V.
Shepherd, T. G.
Waugh, D.
Akiyoshi, H.
Austin, J.
Baumgaertner, A.
Bekki, S.
Braesicke, P.
Bruehl, C.
Butchart, N.
Chipperfield, M. P.
Cugnet, D.
Dameris, M.
Dhomse, S.
Frith, S.
Garny, H.
Garcia, R.
Hardiman, S. C.
Joeckel, P.
Lamarque, J. F.
Mancini, E.
Marchand, M.
Michou, M.
Nakamura, T.
Morgenstern, O.
Pitari, G.
Plummer, D. A.
Pyle, J.
Rozanov, E.
Scinocca, J. F.
Shibata, K.
Smale, D.
Teyssedre, H.
Tian, W.
Yamashita, Y.
TI Impact of stratospheric ozone on Southern Hemisphere circulation change:
A multimodel assessment
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID CHEMISTRY-CLIMATE MODEL; PRIMITIVE EQUATION MODEL; RELATIVELY SIMPLE
AGCM; IPCC AR4 MODELS; TROPOPAUSE HEIGHT; MIDDLE ATMOSPHERE; ANNULAR
MODE; PART II; FLUCTUATION-DISSIPATION; TROPOSPHERIC RESPONSE
AB The impact of stratospheric ozone on the tropospheric general circulation of the Southern Hemisphere (SH) is examined with a set of chemistry-climate models participating in the Stratospheric Processes and their Role in Climate (SPARC)/Chemistry-Climate Model Validation project phase 2 (CCMVal-2). Model integrations of both the past and future climates reveal the crucial role of stratospheric ozone in driving SH circulation change: stronger ozone depletion in late spring generally leads to greater poleward displacement and intensification of the tropospheric midlatitude jet, and greater expansion of the SH Hadley cell in the summer. These circulation changes are systematic as poleward displacement of the jet is typically accompanied by intensification of the jet and expansion of the Hadley cell. Overall results are compared with coupled models participating in the Intergovernmental Panel on Climate Change Fourth Assessment Report (IPCC AR4), and possible mechanisms are discussed. While the tropospheric circulation response appears quasi-linearly related to stratospheric ozone changes, the quantitative response to a given forcing varies considerably from one model to another. This scatter partly results from differences in model climatology. It is shown that poleward intensification of the westerly jet is generally stronger in models whose climatological jet is biased toward lower latitudes. This result is discussed in the context of quasi-geostrophic zonal mean dynamics.
C1 [Son, S. -W.] McGill Univ, Dept Atmospher & Ocean Sci, Montreal, PQ H3A 2K6, Canada.
[Akiyoshi, H.; Nakamura, T.; Yamashita, Y.] Natl Inst Environm Studies, Tsukuba, Ibaraki 3058506, Japan.
[Austin, J.] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA.
[Baumgaertner, A.; Bruehl, C.] Max Planck Inst Chem, D-55020 Mainz, Germany.
[Bekki, S.; Cugnet, D.; Marchand, M.] CNRS INSU, UPMC, UVSQ, Inst Pierre Simone Laplace,LATMOS, F-75252 Paris, France.
[Braesicke, P.; Morgenstern, O.; Pyle, J.] Univ Cambridge, Dept Chem, NCAS Climate Chem, Cambridge CB2 1EW, England.
[Butchart, N.; Hardiman, S. C.] Met Off Hadley Ctr, Exeter EX1 3PB, Devon, England.
[Chipperfield, M. P.; Dhomse, S.; Tian, W.] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England.
[Eyring, V.; Dameris, M.; Garny, H.; Joeckel, P.] Inst Phys Atmosphare, Deutsch Zentrum Luft & Raumfahrt, D-82234 Oberpfaffenhofen, Germany.
[Frith, S.] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
[Garcia, R.; Lamarque, J. F.] Natl Ctr Atmospher Res, Div Atmospher Chem, Boulder, CO 80307 USA.
[Gerber, E. P.] NYU, Courant Inst Math Sci, Ctr Atmosphere Ocean Sci, New York, NY 10012 USA.
[Gillett, N. P.; Scinocca, J. F.] Univ Victoria, Canadian Ctr Climate Modelling & Anal, Environm Canada, Victoria, BC V8W 2Y2, Canada.
[Mancini, E.; Pitari, G.] Univ Aquila, Dipartimento Fis, I-67010 Coppito, Laquila, Italy.
[Michou, M.; Teyssedre, H.] Ctr Natl Rech Meteorol, GAME, CNRM, Meteo France, F-31057 Toulouse, France.
[Perlwitz, J.] NOAA, Earth Syst Res Lab, Div Phys Sci, Boulder, CO 80305 USA.
[Plummer, D. A.] Environm Canada, Canadian Ctr Climate Modelling & Anal, Toronto, ON V8W 3V6, Canada.
[Polvani, L. M.] Columbia Univ, Dept Appl Phys & Appl Math, New York, NY 10027 USA.
[Rozanov, E.] Phys Meteorol Observatorium Davos World Radiat Ct, CH-7260 Davos, Switzerland.
[Seo, K. -H.] Pusan Natl Univ, Dept Atmospher Sci, Pusan 609735, South Korea.
[Shepherd, T. G.] Univ Toronto, Dept Phys, Toronto, ON M5S 1A7, Canada.
[Shibata, K.] Meteorol Res Inst, Tsukuba, Ibaraki 3050052, Japan.
[Smale, D.] Natl Inst Water & Atmospher Res, Lauder 9320, Central Otago, New Zealand.
[Waugh, D.] Johns Hopkins Univ, Dept Earth & Planetary Sci, Baltimore, MD 21218 USA.
[Perlwitz, J.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO USA.
[Polvani, L. M.] Columbia Univ, Dept Earth & Environm Sci, New York, NY USA.
[Rozanov, E.] ETH, Inst Atmospher & Climate Sci, Zurich, Switzerland.
RP Son, SW (reprint author), McGill Univ, Dept Atmospher & Ocean Sci, 805 Sherbrooke St W, Montreal, PQ H3A 2K6, Canada.
EM seok-woo.son@mcgill.ca
RI Pitari, Giovanni/O-7458-2016; Eyring, Veronika/O-9999-2016; Jockel,
Patrick/C-3687-2009; Perlwitz, Judith/B-7201-2008; Dhomse,
Sandip/C-8198-2011; Rozanov, Eugene/A-9857-2012; Baumgaertner,
Andreas/C-4830-2011; Chipperfield, Martyn/H-6359-2013; Son, Seok-Woo
/A-8797-2013; Lamarque, Jean-Francois/L-2313-2014; bekki,
slimane/J-7221-2015; Nakamura, Tetsu/M-7914-2015; Braesicke,
Peter/D-8330-2016
OI Mancini, Eva/0000-0001-7071-0292; Morgenstern, Olaf/0000-0002-9967-9740;
Pitari, Giovanni/0000-0001-7051-9578; Eyring,
Veronika/0000-0002-6887-4885; Jockel, Patrick/0000-0002-8964-1394;
Perlwitz, Judith/0000-0003-4061-2442; Dhomse,
Sandip/0000-0003-3854-5383; Rozanov, Eugene/0000-0003-0479-4488;
Baumgaertner, Andreas/0000-0002-4740-0701; Chipperfield,
Martyn/0000-0002-6803-4149; Lamarque, Jean-Francois/0000-0002-4225-5074;
bekki, slimane/0000-0002-5538-0800; Nakamura, Tetsu/0000-0002-2056-7392;
Braesicke, Peter/0000-0003-1423-0619
FU Office of Sciences, U.S. Department of Energy; NSERC; US NSF; KMA RD
program [RACS 2010-2017]; Joint DECC and Defra Integrated Climate
Programme, DECC/Defra [GA01101]; Ministry of the Environment of Japan
[A-071]; European Commission [SCOUT-O3]
FX Helpful comments by Petra Huck and three anonymous reviewers are
gratefully appreciated. The authors thank the Program for Climate Model
Diagnosis and Intercomparison (PCMDI) for collecting and archiving the
CMIP3 model data, the JSC/CLIVAR Working Groups on Coupled Modeling
(WGCM) and their Coupled Model Intercomparison Project (CMIP) and
Climate Simulation Panel for organizing the model data analysis
activity, and the IPCC WG1 TSU for technical support. The IPCC Data
Archive at Lawrence Livermore National Laboratory is supported by the
Office of Sciences, U.S. Department of Energy. We also thank all of the
modeling groups for making their simulations available for this
analysis, the second round of the Chemistry-Climate Model Validation
(CCMVal-2) Activity for WCRP (World Climate Research Programme) SPARC
(Stratospheric Processes and their Role in Climate) project for
organizing and coordinating the model data analysis activity, and the
British Atmospheric Data Center (BADC) for collecting and archiving the
CCMVal-2 model output. The work of S. W. S. is supported by NSERC
discovery grant. E. P. G. and L. M. P. are supported by grants from the
US NSF to New York University and Columbia University, respectively. K.
H. S. and S. W. S. were funded by the KMA R&D program under grant RACS
2010-2017. D. W. is partly supported by U.S. NSF. N.B. and S. H. are
supported by the Joint DECC and Defra Integrated Climate Programme,
DECC/Defra (GA01101). The CCSRNIES research was supported by the Global
Environmental Research Found of the Ministry of the Environment of Japan
(A-071), and the simulations were completed with the supercomputer at
CGER, NIES, Japan. The MRI simulation was made with the supercomputer at
the NIES, Japan. The scientific work of the European CCM groups was
supported by the European Commission through the project SCOUT-O3 under
the 6th Framework Programme. The National Center for Atmospheric
Research is operated by the University Corporation for Atmospheric
Research under sponsorship of the National Science Foundation. Any
opinions, findings, and conclusions or recommendations expressed in the
publication are those of the authors and do not necessarily reflect the
views of the National Science Foundation.
NR 97
TC 132
Z9 134
U1 2
U2 46
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-897X
EI 2169-8996
J9 J GEOPHYS RES-ATMOS
JI J. Geophys. Res.-Atmos.
PD OCT 13
PY 2010
VL 115
AR D00M07
DI 10.1029/2010JD014271
PG 18
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 666BS
UT WOS:000283084500009
ER
PT J
AU Krayzman, V
Levin, I
AF Krayzman, Victor
Levin, Igor
TI Reverse Monte Carlo refinements of local displacive order in
perovskites: AgNbO3 case study
SO JOURNAL OF PHYSICS-CONDENSED MATTER
LA English
DT Article
ID DIFFUSE-SCATTERING; SOLID-SOLUTIONS; DIFFRACTION; DISORDER
AB Reverse Monte Carlo refinements with combined input from neutron/x-ray total scattering and extended x-ray absorption fine structure (EXAFS) were applied to analyze local atomic displacements in perovskite-related AgNbO3. This compound exhibits complex displacive order-disorder behavior that determines the unique dielectric properties of AgNbO3-based ceramics. Our results revealed that the total scattering and EXAFS data collected from polycrystalline samples were insufficient to reproduce the correlated local Nb displacements which are evident from the diffuse scattering observed in electron diffraction. A credible representation of the AgNbO3 structure was obtained by enforcing these correlations via restraints on the atomic moves, thus ensuring that the refined atomic ensemble not only satisfied the total scattering and EXAFS data (a total of five datasets) but also reproduced the shape of the observed electron diffuse scattering. Such constrained RMC refinements revealed two-site positional disorder for each of the two non-equivalent Ag crystallographic positions. The refinements confirmed that all Ag cations in AgNbO3 exhibit similar local Ag-O coordination environments as opposed to the two distinct Ag coordinations in the average Pbcm structure. These results support the existence of Ag order-disorder behavior similar to that observed for Nb.
C1 [Krayzman, Victor; Levin, Igor] NIST, Div Ceram, Gaithersburg, MD 20899 USA.
RP Krayzman, V (reprint author), NIST, Div Ceram, Gaithersburg, MD 20899 USA.
RI Levin, Igor/F-8588-2010
FU US Department of Energy, Office of Science, Office of Basic Energy
Sciences [DE-AC02-06CH11357]; Science and Technology Facilities Council
FX The authors are grateful to J Woicik (NIST), M Tucker (ISIS), P Chupas
(APS), and K Chapman (APS) for their help with collecting the
experimental data used in this study. Use of the Advanced Photon Source
was supported by the US Department of Energy, Office of Science, Office
of Basic Energy Sciences, under contract No. DE-AC02-06CH11357.
Experiments at the ISIS Pulsed Neutron and Muon Source were supported by
a beam-time allocation from the Science and Technology Facilities
Council. The source code of RMCProfile was kindly provided by M Tucker.
NR 22
TC 4
Z9 4
U1 0
U2 12
PU IOP PUBLISHING LTD
PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0953-8984
J9 J PHYS-CONDENS MAT
JI J. Phys.-Condes. Matter
PD OCT 13
PY 2010
VL 22
IS 40
AR 404201
DI 10.1088/0953-8984/22/40/404201
PG 8
WC Physics, Condensed Matter
SC Physics
GA 653MQ
UT WOS:000282096000004
PM 21386562
ER
PT J
AU Zangmeister, CD
AF Zangmeister, Christopher D.
TI Preparation and Evaluation of Graphite Oxide Reduced at 220 degrees C
SO CHEMISTRY OF MATERIALS
LA English
DT Article
ID GRAPHENE OXIDE; REDUCTION; FILMS; TRANSPARENT; ENVIRONMENT; SERIES
AB The reduction of graphite oxide (GO) thin films was evaluated at 220 degrees C using a combination of infrared (FTIR) and X-ray photoemission spectroscopies (XPS). The results were correlated with electrical resistance measurements. The chemical composition of GO was C-8(OH)(3)O-0.8 and reduced to C-8(OH)(0.5)O-0.3 after nearly 24 h of low-temperature processing, defined as 220 degrees C. The sheet resistance of dropcast GO thin films processed at 220 degrees C in air was 8 k Omega sq(-1), similar to GO reduced at >800 degrees C in an inert atmosphere.
C1 Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
RP Zangmeister, CD (reprint author), Natl Inst Stand & Technol, 100 Bur Dr, Gaithersburg, MD 20899 USA.
EM cdzang@nist.gov
FU NIST Office of Microelectronics
FX The author acknowledges Drs. Christina Hacker, Brent Sperling, Roger van
Zec, Rebecca Zangmeister, and Gery Stafford for assistance in this
investigation. The NIST Office of Microelectronics Programs funded this
work.
NR 34
TC 110
Z9 115
U1 13
U2 78
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0897-4756
EI 1520-5002
J9 CHEM MATER
JI Chem. Mat.
PD OCT 12
PY 2010
VL 22
IS 19
BP 5625
EP 5629
DI 10.1021/cm102005m
PG 5
WC Chemistry, Physical; Materials Science, Multidisciplinary
SC Chemistry; Materials Science
GA 658DS
UT WOS:000282471000027
ER
PT J
AU Chang, YT
Tang, TY
Chao, SY
Chang, MH
Ko, DS
Yang, YJ
Liang, WD
McPhaden, MJ
AF Chang, Ya-Ting
Tang, Tswen Yung
Chao, Shenn-Yu
Chang, Ming-Huei
Ko, Dong S.
Yang, Yiing Jang
Liang, Wen-Der
McPhaden, Michael J.
TI Mooring observations and numerical modeling of thermal structures in the
South China Sea
SO JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
LA English
DT Article
ID TOPEX/POSEIDON ALTIMETRY; DATA ASSIMILATION; MESOSCALE EDDIES;
CIRCULATION; SYSTEM; VARIABILITY; MODULATION; HURRICANE; TIDE
AB Three sets of Autonomous Temperature Line Acquisition Systems were deployed in the South China Sea. Gaps aside, the data covered nearly 3 years at the northern station and about 2 years farther south. Fluctuations ranged from episodic to interannual. Internal tides, more diurnal than semidiurnal, were active basinwide. Twelve typhoons passed during measurement periods. The most severe one, typhoon Babs in 1998, caused a temperature drop of over 7 degrees C at 50 m. Despite strong monsoons, only near-surface temperature showed clear seasonal variations. Intraseasonal variations induced by mesoscale eddy stood out much better at subsurface depths. Propagating eddies aside, some eddies were seasonal and nearly stationary. From daily archives of an eddy-resolving, data-assimilating ocean model ( East Asian Seas Nowcast/Forecast System), we identified two paradigms leading to the generation of a persistent spring-summer warm eddy in the central-western basin. In normal years, a complete cyclonic gyre was driven by a strong winter northeast monsoon. Water piled up along the periphery of the South China Sea. Afterward, a warm eddy could be generated from west of Luzon Island and propagated westward while intensifying. Under a weak northeast monsoon, such as in El Nino years, piled-up water tended to stay in the southern basin. When the wind relaxed in spring, warm water returned northward to form a warm eddy in the central-western basin. Transition from SW to NE monsoon also often led to a warm eddy generation in southern latitudes, when the summer eastward jet departing from central Vietnam broke up.
C1 [Chang, Ya-Ting; Tang, Tswen Yung] Natl Taiwan Univ, Inst Oceanog, Taipei 106, Taiwan.
[Chao, Shenn-Yu] Univ Maryland, Ctr Environm Sci, Horn Point Lab, Cambridge, MD 21613 USA.
[Chang, Ming-Huei] Natl Taiwan Ocean Univ, Dept Marine Environm Informat, Chilung 20224, Taiwan.
[Yang, Yiing Jang; Liang, Wen-Der] Naval Acad, Dept Marine Sci, Kaohsiung 813, Taiwan.
[Ko, Dong S.] USN, Res Lab, Div Oceanog, Ocean Dynam & Predict Branch, Stennis Space Ctr, MS 39529 USA.
[McPhaden, Michael J.] NOAA, Pacific Marine Environm Lab, Seattle, WA 98115 USA.
RP Chang, YT (reprint author), Natl Taiwan Univ, Inst Oceanog, Roosevelt Rd, Taipei 106, Taiwan.
RI McPhaden, Michael/D-9799-2016;
OI CHANG, MING-HUEI/0000-0002-6409-7652
FU Taiwan's National Science Council [95-2611-M-002-016-MY3,
95-2611-M-002-018-MY3, 98-2745-M-002-004]; Office of Naval Research (US)
[N00014-09-0623, N00014-08WX-02-1170]
FX The altimeter products were produced and distributed by Aviso
(http://www.aviso.oceanobs.com/), as part of the Ssalto
ground-processing segment. The work was supported by Taiwan's National
Science Council under grants 95-2611-M-002-016-MY3,
95-2611-M-002-018-MY3, and 98-2745-M-002-004 for T.-Y. Tang, and by the
Office of Naval Research (US) under grants N00014-09-0623 for S.-Y. Chao
and N00014-08WX-02-1170 for D. S. Ko. PMEL publication 3606.
NR 44
TC 7
Z9 7
U1 0
U2 10
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-9275
EI 2169-9291
J9 J GEOPHYS RES-OCEANS
JI J. Geophys. Res.-Oceans
PD OCT 12
PY 2010
VL 115
AR C10022
DI 10.1029/2010JC006293
PG 19
WC Oceanography
SC Oceanography
GA 666DD
UT WOS:000283090900004
ER
PT J
AU Kim, SY
Park, MJ
Balsara, NP
Jackson, A
AF Kim, Sung Yeon
Park, Moon Jeong
Balsara, Nitash P.
Jackson, Andrew
TI Confinement Effects on Watery Domains in Hydrated Block Copolymer
Electrolyte Membranes
SO MACROMOLECULES
LA English
DT Article
ID SMALL-ANGLE SCATTERING; SULFONATED POLYSTYRENE; NEUTRON-SCATTERING;
IONOMER MEMBRANES; NAFION MEMBRANES; PHASE-BEHAVIOR; FUEL-CELLS; X-RAY;
PROTON; CONDUCTIVITY
AB The morphology of a series of diblock copolymers comprising randomly still-ciliated polystyrene (PSS) and polymethylbutylene (PMB) blocks equilibrated with humid air was determined by in situ small-angle neutron scattering (SANS). In-situ SANS data were collected over a wide angular range permitting the determination of the superstructure of the hydrophilic PSS-rich and hydrophobic PMB-rich domains and the substructure within the hydrophilic PSS-rich domains. When the characteristic length oldie superstructure is larger than 10 nm, the hydrophilic PSS domains :ire heterogeneous with periodically arranged watery domains. The scattering signature of the watery domains is very similar to the well-established "ionomer peak". This peak vanishes when the neutron scattering length density or the water (H(2)O/D(2)O mixture) is matched to that of the PSS block. The spacing between watery domains depends only on sulfonation level of the PSS block. When the characteristic length of the superstructure is less than 10 nm, the watery substructure disappears and homogeneous hydrated PSS-rich domains are obtained.
C1 [Park, Moon Jeong] Pohang Univ Sci & Technol, Dept Chem, Pohang 790784, South Korea.
[Kim, Sung Yeon; Park, Moon Jeong] Pohang Univ Sci & Technol, Div Adv Mat Sci, Pohang 790784, South Korea.
[Balsara, Nitash P.] Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Dept Chem Engn, Div Mat Sci, Berkeley, CA 94720 USA.
[Balsara, Nitash P.] Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Environm Energy Technol Div, Berkeley, CA 94720 USA.
[Jackson, Andrew] Natl Inst Stand & Technol, NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Jackson, Andrew] Univ Maryland, Dept Mat Sci & Engn, College Pk, MD 20742 USA.
RP Park, MJ (reprint author), Pohang Univ Sci & Technol, Dept Chem, Pohang 790784, South Korea.
EM moonpark@postech.edu
RI Jackson, Andrew/B-9793-2008; Park, Moon Jeong/F-5752-2013
OI Jackson, Andrew/0000-0002-6296-0336;
FU Ministry or Education, Science and Technology [2010-0007798,
R31-2009-000-10059-0]; National Science Foundation [DMR-0504122]
FX This research was supported by Basic Science Research Program through
the National Research Foundation of Korea (NRF) funded by the Ministry
or Education, Science and Technology (Project No. 2010-0007798) and WCU
(World Class University) program through the Korea Science and
Engineering Foundation funded by the Ministry of Education, Science and
Technology (Project No. R31-2009-000-10059-0). The SANS facilities at
NIST are supported in part by the National Science Foundation under
Agreement DMR-0504122.
NR 35
TC 20
Z9 20
U1 2
U2 40
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0024-9297
J9 MACROMOLECULES
JI Macromolecules
PD OCT 12
PY 2010
VL 43
IS 19
BP 8128
EP 8135
DI 10.1021/ma101620k
PG 8
WC Polymer Science
SC Polymer Science
GA 658GM
UT WOS:000282478500038
ER
PT J
AU Ding, YF
Qi, HJ
Alvine, KJ
Ro, HW
Ahn, DU
Lin-Gibson, S
Douglas, JF
Soles, CL
AF Ding, Yifu
Qi, H. Jerry
Alvine, Kyle J.
Ro, Hyun Wook
Ahn, Dae Up
Lin-Gibson, Sheng
Douglas, Jack F.
Soles, Christopher L.
TI Stability and Surface Topography Evolution in Nanoimprinted Polymer
Patterns under a Thermal Gradient
SO MACROMOLECULES
LA English
DT Article
ID FLASH IMPRINT LITHOGRAPHY; MOLECULAR-WEIGHT; RHEOLOGICAL MEASUREMENTS;
RESIDUAL-STRESS; THIN-FILMS; RELAXATION; VISCOELASTICITY; STEP;
NANOFABRICATION; DEFORMATION
AB Nanostructures created in polymer films by nanoimprint lithography are subject to large stresses, both those from the imprinting processes as well as stresses arising from the intrinsic thermodynamic instabilities. These stresses can induce nanostructure deformations that compromise the intended function of the imprinted pattern. Controlling these stresses, and thus the stability of the imprinted patterns, is a key scientific issue for this technology. The requirement of film stability against dewetting requires the use of entangled polymer films, which necessitates an understanding of complex viscoelastic response of these materials to large stresses. Here we investigate the evolution of the surface topography of nanoimprinted patterns in polystyrene films through a high throughput annealing approach in which the patterns are annealed for a fixed time on a controlled temperature gradient. Using principles of time-temperature superposition we systematically explore the effect of varying basic system variables such as pattern feature size, polymer molecular mass, imprinting temperature. on nanopattern stability, and on the evolution of imprinted patterns driven by surface tension and internal stress. Nanostructure collapse generally occurs through a combination of a "slumping'' instability, where the imprinted film simply relaxes toward it planar film and the pattern height decreases with time, and a lateral "zigzag" instability in the nanoimprinted lines.
C1 [Ding, Yifu; Qi, H. Jerry; Ahn, Dae Up] Univ Colorado, Dept Mech Engn, Boulder, CO 80309 USA.
[Alvine, Kyle J.] Pacific NW Natl Lab, Energy & Environm Directorate, Richland, WA 99352 USA.
[Ro, Hyun Wook; Lin-Gibson, Sheng; Douglas, Jack F.; Soles, Christopher L.] NIST, Div Polymers, Gaithersburg, MD 20899 USA.
RP Ding, YF (reprint author), Univ Colorado, Dept Mech Engn, Boulder, CO 80309 USA.
EM Yifu.Ding@colorado.Edu; Christopher.soles@nist.gov
RI Qi, H. Jerry/C-1588-2009
FU National Science Foundation [CMMI-0928067, CMMI-1031785]
FX We acknowledge the funding support from the National Science Foundation
under Grant Nos. CMMI-0928067 and CMMI-1031785 and the nanofabrication
laboratory of the Center for Nanoscale Science and Technology (CNST) at
NIST for access to their facilities.
NR 52
TC 5
Z9 6
U1 2
U2 27
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0024-9297
J9 MACROMOLECULES
JI Macromolecules
PD OCT 12
PY 2010
VL 43
IS 19
BP 8191
EP 8201
DI 10.1021/ma1018632
PG 11
WC Polymer Science
SC Polymer Science
GA 658GM
UT WOS:000282478500046
ER
PT J
AU Akcora, P
Kumar, SK
Sakai, VG
Li, Y
Benicewicz, BC
Schadler, LS
AF Akcora, Pinar
Kumar, Sanat K.
Sakai, Victoria Garcia
Li, Yu
Benicewicz, Brian C.
Schadler, Linda S.
TI Segmental Dynamics in PMMA-Grafted Nanoparticle Composites
SO MACROMOLECULES
LA English
DT Article
ID NONLINEAR VISCOELASTIC BEHAVIOR; SMALL-ANGLE SCATTERING;
GLASS-TRANSITION TEMPERATURE; FILLED ELASTOMERS; POLYMER MELTS; SILICA
NANOPARTICLES; IMMOBILIZED POLYMER; REINFORCEMENT; NANOCOMPOSITES; MODEL
AB We have recently shown that silica nanopartieles grafted with polystyrene chains behave akin to block copolymers due to the "dislike" between the nanoparticles and the grafts. These decorated nanoparticles, thus, sell-assemble into various morphologies, from well-dispersed nanoparticles to anisotropic superstructures, when they are placed in homopolystyrene matrices of different molecular masses. Here, we consider a slightly different case, where the grafted chains and the matrix (both PM MA) are strongly attracted to the silica nanoparticle surface. We then conjecture that these systems show phase mixing or demixing depending on the miscibility between the brush and matrix chains ("autophobic dewetting"). At 15 mass % particle loading, composites created using the same grafted nanoparticle, hut with two different matrices, yield well dispersed nanoparticles or nanoparticle "agglomerates", respectively. Rheoloey experiments show that the composites display solid-like behavior only when the particles are aggregated. As deduced in previous work, this difference in behavior is attributed to the presence of percolating particle clusters in the agglomerated samples which allows for stress propagation through the system. Going further, we compare the local mobility of matrix and grafted segments of both composites using quasi-elastic neutron scattering experiments. For the liquid-like system, the mean square displacements of the grafted chains and matrix chains, the particle structuring and mechanical response are all unaffected by annealing time. In contrast, in the reinforced case, only the local matrix motion is unaffected by time. Since the particle clustering and solid-like mechanical reinforcement increase with increasing time, we conclude that mechanical reinforcement in polymer nanocomposites is purely based on the nanoparticles, with essentially no "interference" from the matrix. In conjunction with other results in the literature, we then surmise that mechanical reinforcement is caused by the bridging of particles by the grafted polymer layers and not due to the formation of "glassy" polymer layers on the nanoparticles.
C1 [Akcora, Pinar; Kumar, Sanat K.] Columbia Univ, Dept Chem Engn, New York, NY 10027 USA.
[Sakai, Victoria Garcia] NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Li, Yu; Benicewicz, Brian C.] Univ S Carolina, Dept Chem & Biochem, Columbia, SC 29208 USA.
[Schadler, Linda S.] Rensselaer Polytech Inst, Dept Mat Sci & Engn, Troy, NY 12180 USA.
RP Akcora, P (reprint author), Columbia Univ, Dept Chem Engn, New York, NY 10027 USA.
RI Li, Yu/A-3565-2011;
OI Benicewicz, Brian/0000-0003-4130-1232
FU National Science Foundation Division of Materials Research [NSF
DMR-0804647]; Nanoscale Science and Engineering Initiative of the
National Science Foundation [NSF DMR-0642573]; National Science
Foundation [DMR-0454672]; National Institute or Standards and
Technology, U.S. Department of Commerce
FX Partial funding for this research was provided by the National Science
Foundation Division of Materials Research (S.K.K., P.A., NSF
DMR-0804647), and through the Nanoscale Science and Engineering
Initiative of the National Science Foundation under NSF DMR-0642573 at
RPI (S.K.K., B.C.B.). This work utilized facilities supported in part by
the National Science Foundation under Agreement No. DMR-0454672. We
acknowledge the support of the National Institute or Standards and
Technology, U.S. Department of Commerce, in providing the neutron
research facilities used in this work.
NR 39
TC 51
Z9 56
U1 9
U2 92
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0024-9297
J9 MACROMOLECULES
JI Macromolecules
PD OCT 12
PY 2010
VL 43
IS 19
BP 8275
EP 8281
DI 10.1021/ma101240j
PG 7
WC Polymer Science
SC Polymer Science
GA 658GM
UT WOS:000282478500054
ER
PT J
AU Coddington, I
Swann, WC
Newbury, NR
AF Coddington, I.
Swann, W. C.
Newbury, N. R.
TI Coherent dual-comb spectroscopy at high signal-to-noise ratio
SO PHYSICAL REVIEW A
LA English
DT Article
ID FOURIER-TRANSFORM SPECTROSCOPY; LASER FREQUENCY COMBS; FREE-INDUCTION
DECAY; FEMTOSECOND FIBER LASER; MODE-LOCKED LASERS;
ABSORPTION-SPECTROSCOPY; SUPERCONTINUUM GENERATION; SPECTRAL
INTERFEROMETRY; NOBEL LECTURE; RING LASERS
AB Two coherent frequency combs are used to measure the full complex response of a sample in a configuration analogous to a dispersive Fourier transform spectrometer, infrared time domain spectrometer, or a multiheterodyne laser spectrometer. This dual-comb spectrometer retains the frequency accuracy and resolution of the reference underlying the stabilized combs. We discuss the specific design of our coherent dual-comb spectrometer and demonstrate the potential of this technique by measuring the overtone vibration of hydrogen cyanide, centered at 194 THz (1545 nm). We measure the fully normalized, complex response of the gas over a 9 THz bandwidth at 220 MHz frequency resolution yielding 41,000 resolution elements. The average spectral signal-to-noise ratio (SNR) over the 9 THz bandwidth is 2500 for both the magnitude and phase of the measured spectral response and the peak SNR is 4000. This peak SNR corresponds to a fractional absorption sensitivity of 0.05% and a phase sensitivity of 250 microradians. As the spectral coverage of combs expands, coherent dual-comb spectroscopy could provide high-frequency accuracy and resolution measurements of a complex sample response across a range of spectral regions. Work of U. S. government, not subject to copyright.
C1 [Coddington, I.; Swann, W. C.; Newbury, N. R.] NIST, Boulder, CO 80305 USA.
RP Coddington, I (reprint author), NIST, 325 Broadway, Boulder, CO 80305 USA.
FU Department of Homeland Security; NIST
FX We acknowledge useful conversations with Esther Baumann, Fabrizio
Giorgetta, Todd Johnson, and Paul Williams and funding from the
Department of Homeland Security and NIST.
NR 69
TC 84
Z9 84
U1 8
U2 63
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 1050-2947
J9 PHYS REV A
JI Phys. Rev. A
PD OCT 12
PY 2010
VL 82
IS 4
AR 043817
DI 10.1103/PhysRevA.82.043817
PG 13
WC Optics; Physics, Atomic, Molecular & Chemical
SC Optics; Physics
GA 662LI
UT WOS:000282808400009
ER
PT J
AU Li, HF
Broholm, C
Vaknin, D
Fernandes, RM
Abernathy, DL
Stone, MB
Pratt, DK
Tian, W
Qiu, Y
Ni, N
Diallo, SO
Zarestky, JL
Bud'ko, SL
Canfield, PC
McQueeney, RJ
AF Li, H. -F.
Broholm, C.
Vaknin, D.
Fernandes, R. M.
Abernathy, D. L.
Stone, M. B.
Pratt, D. K.
Tian, W.
Qiu, Y.
Ni, N.
Diallo, S. O.
Zarestky, J. L.
Bud'ko, S. L.
Canfield, P. C.
McQueeney, R. J.
TI Anisotropic and quasipropagating spin excitations in superconducting
Ba(Fe0.926Co0.074)(2)As-2
SO PHYSICAL REVIEW B
LA English
DT Article
ID STATE
AB Inelastic neutron scattering from superconducting (SC) Ba (Fe0.926Co0.074)(2)As-2 reveals anisotropic and quasi-two-dimensional (2D) magnetic excitations close to Q(AFM)=(1/21/2) - the 2D antiferromagnetic (AFM) wave vector of the parent BaFe2As2 compound. The correlation length anisotropy of these low-energy fluctuations is consistent with spin nematic correlations in the J(1)-J(2) model with J(1)/J(2)similar to 1. The spin resonance at similar to 8.3 meV in the SC state displays the same anisotropy. The anisotropic fluctuations experimentally evolve into two distinct maxima only along the direction transverse to Q(AFM) above similar to 80 meV indicating unusual quasipropagating excitations.
C1 [Li, H. -F.; Vaknin, D.; Fernandes, R. M.; Pratt, D. K.; Tian, W.; Ni, N.; Diallo, S. O.; Zarestky, J. L.; Bud'ko, S. L.; Canfield, P. C.; McQueeney, R. J.] Iowa State Univ, Ames Lab, Ames, IA 50011 USA.
[Li, H. -F.; Vaknin, D.; Fernandes, R. M.; Pratt, D. K.; Tian, W.; Ni, N.; Diallo, S. O.; Zarestky, J. L.; Bud'ko, S. L.; Canfield, P. C.; McQueeney, R. J.] Iowa State Univ, Dept Phys & Astron, Ames, IA 50011 USA.
[Broholm, C.] Johns Hopkins Univ, Inst Quantum Matter, Baltimore, MD 21218 USA.
[Broholm, C.] Johns Hopkins Univ, Dept Phys & Astron, Baltimore, MD 21218 USA.
[Abernathy, D. L.; Stone, M. B.] Oak Ridge Natl Lab, Oak Ridge, TN 37831 USA.
[Qiu, Y.] Natl Inst Stand & Technol, NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Qiu, Y.] Univ Maryland, Dept Mat Sci & Engn, College Pk, MD 20742 USA.
RP Li, HF (reprint author), Iowa State Univ, Ames Lab, Ames, IA 50011 USA.
RI Broholm, Collin/E-8228-2011; Vaknin, David/B-3302-2009; BL18,
ARCS/A-3000-2012; Stone, Matthew/G-3275-2011; Fernandes,
Rafael/E-9273-2010; Abernathy, Douglas/A-3038-2012; Li,
Haifeng/F-9743-2013; Tian, Wei/C-8604-2013; Canfield, Paul/H-2698-2014;
McQueeney, Robert/A-2864-2016; Diallo, Souleymane/B-3111-2016
OI Broholm, Collin/0000-0002-1569-9892; Vaknin, David/0000-0002-0899-9248;
Stone, Matthew/0000-0001-7884-9715; Abernathy,
Douglas/0000-0002-3533-003X; Tian, Wei/0000-0001-7735-3187; McQueeney,
Robert/0000-0003-0718-5602; Diallo, Souleymane/0000-0002-3369-8391
FU U.S. Department of Energy (U.S. DOE), Office of Basic Energy Sciences,
Division of Materials Sciences and Engineering; U.S. DOE by Iowa State
University [DE-AC02-07CH11358]; U.S. DOE [DE-FG02-08ER46544]; Scientific
User Facilities Division, Office of Basic Energy Sciences, DOE
FX This research is supported by the U.S. Department of Energy (U.S. DOE),
Office of Basic Energy Sciences, Division of Materials Sciences and
Engineering. Ames Laboratory is operated for the U.S. DOE by Iowa State
University under Contract No. DE-AC02-07CH11358. Johns Hopkins Institute
for Quantum Matter is supported by the U.S. DOE under Grant No.
DE-FG02-08ER46544. Research at Oak Ridge National Laboratory's High Flux
Isotope Reactor and Spallation Neutron Source is sponsored by the
Scientific User Facilities Division, Office of Basic Energy Sciences,
DOE. We thank M. J. Loguillo for assistance with the ARCS measurements.
We acknowledge the expert technical assistance of Scott Spangler at JHU
in machining the sample mount for HB-3 measurements.
NR 26
TC 49
Z9 49
U1 1
U2 12
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 1098-0121
J9 PHYS REV B
JI Phys. Rev. B
PD OCT 12
PY 2010
VL 82
IS 14
AR 140503
DI 10.1103/PhysRevB.82.140503
PG 4
WC Physics, Condensed Matter
SC Physics
GA 662LP
UT WOS:000282809100004
ER
PT J
AU O'Neill, BC
Dalton, M
Fuchs, R
Jiang, LW
Pachauri, S
Zigova, K
AF O'Neill, Brian C.
Dalton, Michael
Fuchs, Regina
Jiang, Leiwen
Pachauri, Shonali
Zigova, Katarina
TI Global demographic trends and future carbon emissions
SO PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF
AMERICA
LA English
DT Article
DE climate change; energy; integrated assessment; population; households
ID HOUSEHOLD ENERGY-REQUIREMENTS; CO2 EMISSIONS; POPULATION-GROWTH;
CLIMATE-CHANGE; IMPACT; STABILIZATION; TRANSITIONS; SCENARIOS; INDIA
AB Substantial changes in population size, age structure, and urbanization are expected in many parts of the world this century. Although such changes can affect energy use and greenhouse gas emissions, emissions scenario analyses have either left them out or treated them in a fragmentary or overly simplified manner. We carry out a comprehensive assessment of the implications of demographic change for global emissions of carbon dioxide. Using an energy-economic growth model that accounts for a range of demographic dynamics, we show that slowing population growth could provide 16-29% of the emissions reductions suggested to be necessary by 2050 to avoid dangerous climate change. We also find that aging and urbanization can substantially influence emissions in particular world regions.
C1 [O'Neill, Brian C.; Jiang, Leiwen] Natl Ctr Atmospher Res, Climate & Global Dynam Div, Boulder, CO 80307 USA.
[O'Neill, Brian C.; Jiang, Leiwen] Natl Ctr Atmospher Res, Integrated Sci Program, Boulder, CO 80307 USA.
[Dalton, Michael] NOAA, Alaska Fisheries Sci Ctr, Seattle, WA 98115 USA.
[Fuchs, Regina; Pachauri, Shonali; Zigova, Katarina] Int Inst Appl Syst Anal, A-2361 Laxenburg, Austria.
[Zigova, Katarina] Univ Konstanz, Dept Econ, D-78457 Constance, Germany.
RP O'Neill, BC (reprint author), Natl Ctr Atmospher Res, Climate & Global Dynam Div, POB 3000, Boulder, CO 80307 USA.
EM boneill@ucar.edu
RI O'Neill, Brian/E-6531-2013
FU National Science Foundation; European Young Investigator's award;
Hewlett Foundation; Department of Energy; Environmental Protection
Agency
FX We thank K. Riahi for assistance in interpreting the IIASA A2 and B2
scenario results, R. Sands for advice on alternative energy-balance
techniques, X. Ren for assistance in checking model results, P. Belden,
A. Hayes, W. Lutz, M. Oppenheimer, W. Sanderson, D. Spreng, and E.
Zagheni for helpful comments on this manuscript, and L. Goulder, P.
Ehrlich, S. Schneider, and D. Kennedy for guidance and support during
development of the original version of the PET model. Funding was
provided by the National Science Foundation, a European Young
Investigator's award (to B.C.O.) and the Hewlett Foundation. Funding was
provided for early stages of the analysis by the Department of Energy
and the Environmental Protection Agency.
NR 30
TC 84
Z9 91
U1 5
U2 46
PU NATL ACAD SCIENCES
PI WASHINGTON
PA 2101 CONSTITUTION AVE NW, WASHINGTON, DC 20418 USA
SN 0027-8424
J9 P NATL ACAD SCI USA
JI Proc. Natl. Acad. Sci. U. S. A.
PD OCT 12
PY 2010
VL 107
IS 41
BP 17521
EP 17526
DI 10.1073/pnas.1004581107
PG 6
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 662LV
UT WOS:000282809700017
PM 20937861
ER
PT J
AU Adler, F
Maslowski, P
Foltynowicz, A
Cossel, KC
Briles, TC
Hartl, I
Ye, J
AF Adler, Florian
Maslowski, Piotr
Foltynowicz, Aleksandra
Cossel, Kevin C.
Briles, Travis C.
Hartl, Ingmar
Ye, Jun
TI Mid-infrared Fourier transform spectroscopy with a broadband frequency
comb
SO OPTICS EXPRESS
LA English
DT Article
ID OPTICAL PARAMETRIC OSCILLATOR; ABSORPTION-SPECTROSCOPY; BREATH ANALYSIS;
FEMTOSECOND LASER; NITROUS-OXIDE; MU-M; METHANE; 21ST-CENTURY;
GENERATION; CLIMATE
AB We present a first implementation of optical-frequency-comb-based rapid trace gas detection in the molecular fingerprint region in the mid-infrared. Near-real-time acquisition of broadband absorption spectra with 0.0056 cm(-1) maximum resolution is demonstrated using a frequency comb Fourier transform spectrometer which operates in the 2100-to-3700-cm(-1) spectral region. We achieve part-per-billion detection limits in 30 seconds of integration time for several important molecules including methane, ethane, isoprene, and nitrous oxide. Our system enables precise concentration measurements even in gas mixtures that exhibit continuous absorption bands, and it allows detection of molecules at levels below the noise floor via simultaneous analysis of multiple spectral features. (C) 2010 Optical Society of America
C1 [Adler, Florian; Maslowski, Piotr; Foltynowicz, Aleksandra; Cossel, Kevin C.; Briles, Travis C.; Ye, Jun] Natl Inst Stand & Technol, JILA, Boulder, CO 80309 USA.
[Adler, Florian; Maslowski, Piotr; Foltynowicz, Aleksandra; Cossel, Kevin C.; Briles, Travis C.; Ye, Jun] Univ Colorado, Dept Phys, Boulder, CO 80309 USA.
[Hartl, Ingmar] IMRA Amer Inc, Ann Arbor, MI 48105 USA.
[Maslowski, Piotr] Uniwersytet Mikolaja Kopernika, Inst Fizyki, PL-87100 Torun, Poland.
RP Adler, F (reprint author), Natl Inst Stand & Technol, JILA, Boulder, CO 80309 USA.
EM fadler@jila.colorado.edu
RI Ye, Jun/C-3312-2011; Maslowski, Piotr/H-4476-2014;
OI Maslowski, Piotr/0000-0001-8882-7106; Foltynowicz,
Aleksandra/0000-0002-6191-7926
FU Alexander von Humboldt Foundation; Polish Ministry of Science and Higher
Education; Swedish Research Council; National Science Foundation; Air
Force Office for Scientific Research; Defense Advanced Research Projects
Agency; Agilent Foundation; National Institute for Standards and
Technology
FX We thank R. Fox for the loan of the Herriott cell and D. L. Osborn, M.
J. Thorpe, N. R. Newbury, S. A. Diddams, and R. Ciurylo for valuable
discussions. We further thank Matheson-Trigas for providing certified
sample gas mixtures. F. A. was partially supported by the Alexander von
Humboldt Foundation. P. M. acknowledges a fellowship from the Polish
Ministry of Science and Higher Education. A. F. holds a fellowship from
the Swedish Research Council. K. C. C. is supported by the National
Science Foundation Graduate Fellowship. This project is funded by the
Air Force Office for Scientific Research, the Defense Advanced Research
Projects Agency, the Agilent Foundation, the National Institute for
Standards and Technology, and the National Science Foundation.
NR 44
TC 102
Z9 103
U1 6
U2 72
PU OPTICAL SOC AMER
PI WASHINGTON
PA 2010 MASSACHUSETTS AVE NW, WASHINGTON, DC 20036 USA
SN 1094-4087
J9 OPT EXPRESS
JI Opt. Express
PD OCT 11
PY 2010
VL 18
IS 21
BP 21861
EP 21872
DI 10.1364/OE.18.021861
PG 12
WC Optics
SC Optics
GA 673TR
UT WOS:000283686500039
PM 20941086
ER
PT J
AU Rhoderick, GC
AF Rhoderick, George C.
TI Stability assessment of gas mixtures containing terpenes at nominal 5
nmol/mol contained in treated aluminum gas cylinders
SO ANALYTICAL AND BIOANALYTICAL CHEMISTRY
LA English
DT Article; Proceedings Paper
CT 6th Annual LC/MS/MS Workshop on Environmental Applications and Food
Safety
CY FEB 25-26, 2010
CL Barcelona, SPAIN
DE Terpenes; Internal standard; Growth rate; Isomerization; Degradation;
Gas mixtures in aluminum cylinders; nmol/mol; pmol/mol
ID STANDARD REFERENCE MATERIAL; VOLATILE ORGANIC-COMPOUNDS; MONOTERPENE
EMISSION; NORWAY SPRUCE; VOC EMISSIONS; ALPHA-PINENE; ISOPRENE; L.;
ISOMERIZATION; VEGETATION
AB Studies of climate change increasingly recognize the diverse influences exerted by terpenes in the atmosphere, including roles in particulates, ozone formation, and their oxidizing potential. Measurements of key terpenes suggest atmospheric concentrations ranging from low pmol/mol (parts per trillion) to nmol/mol (parts per billion), depending on location and compound. To accurately establish concentration trends, assess the role of terpenes in atmospheric chemistry, and relate measurement records from many laboratories and researchers, it is essential to have good calibration standards. The feasibility of preparing well-characterized, stable gas cylinder standards for terpenes at the nmol/mol level is not yet well established. Several of the world's National Metrology Institutes (NMIs) are researching the feasibility of developing primary and secondary reference gas standards at the nmol/mol level for terpenes. The US NMI, the National Institute of Standards and Technology, has prepared several nmol/mol mixtures, in treated aluminum gas cylinders, containing terpenes in dry nitrogen at nominal 5 nmol/mol for stability studies. Overall, 11 terpenes were studied for stability. An initial gas mixture containing nine terpenes, one oxygenate, and six aromatic compounds, including benzene as an internal standard, was prepared. Results for four of the nine terpenes in this initial mixture indicate stability in these treated aluminum gas cylinders for over 6 months and project long term (years) stability. Interesting results were seen for beta-pinene, which when using a linear equation rate decline predicts that it will reach a zero concentration level at day 416. At the same time, increases in alpha-pinene, D-limonene (R-(+)-limonene), and p-cymene were observed, including camphene, a terpene not prepared in the gas mixture, indicating a chemical transformation of beta-pinene to these species. Additional mixtures containing combination of either alpha-pinene, camphor, alpha-terpinene, and benzene indicate a second-order quadratic rate decline for the alpha-pinene and alpha-terpinene, a linear rate decline for camphor, and a second-order quadratic rate increase of camphene.
C1 Natl Inst Stand & Technol, Div Analyt Chem, Gaithersburg, MD 20899 USA.
RP Rhoderick, GC (reprint author), Natl Inst Stand & Technol, Div Analyt Chem, 100 Bur Dr,MS 8393, Gaithersburg, MD 20899 USA.
EM george.rhoderick@nist.gov
NR 33
TC 1
Z9 1
U1 0
U2 9
PU SPRINGER HEIDELBERG
PI HEIDELBERG
PA TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY
SN 1618-2642
J9 ANAL BIOANAL CHEM
JI Anal. Bioanal. Chem.
PD OCT 10
PY 2010
VL 398
IS 3
BP 1417
EP 1425
DI 10.1007/s00216-010-4058-0
PG 9
WC Biochemical Research Methods; Chemistry, Analytical
SC Biochemistry & Molecular Biology; Chemistry
GA 648DK
UT WOS:000281670400029
PM 20694720
ER
PT J
AU Xiong, XZ
Barnet, CD
Zhuang, QL
Machida, T
Sweeney, C
Patra, PK
AF Xiong, Xiaozhen
Barnet, Christopher D.
Zhuang, Qianlai
Machida, Toshinobu
Sweeney, Colm
Patra, Prabir K.
TI Mid-upper tropospheric methane in the high Northern Hemisphere:
Spaceborne observations by AIRS, aircraft measurements, and model
simulations
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID TRANS-SIBERIAN RAILROAD; TRACE GAS MEASUREMENTS; ATMOSPHERIC METHANE;
GROWTH-RATE; BUDGET; SATELLITE; MISSION; DESIGN; CYCLE; CH4
AB Spaceborne measurements by the Atmospheric Infrared Sounder (AIRS) on the EOS/Aqua satellite provide a global view of the methane (CH4) distribution in the mid-upper troposphere (MUT-CH4). The focus of this study is to examine the spatiotemporal variation of MUT-CH4 in the high Northern Hemisphere (HNH) using AIRS retrievals, aircraft measurements, and simulations from a forward chemistry-transport model (i.e., ACTM). Data from 2004 and 2005 focusing over two regions (Alaska and Siberia) are analyzed. An important feature in the seasonal variation of CH4 we found is the summer increase of MUT-CH4, which is nearly opposite to the summer minimum of CH4 in the marine boundary layer (MBL). This study also demonstrated an apparent increase of CH4 over Alaska associated with the 2004 Alaska forest fire and a negative bias of the ACTM simulations in the HNH. The larger bias of the model simulations in the late winter to early spring may indicate possible unidentified CH4 emission sources (e. g., the use of energy or gas leakage) during this period, but more studies will be needed due to the retrieval uncertainties in the polar winter season. The summer increase of MUT-CH4 is related to surface emission, but the enhanced convection in summer is likely the most important driver.
C1 [Xiong, Xiaozhen] Dell Perot Syst Govt Serv, Fairfax, VA USA.
[Xiong, Xiaozhen; Barnet, Christopher D.] NOAA, Ctr Satellite Applicat & Res, Natl Environm Satellite Data & Informat Serv, Camp Springs, MD 20746 USA.
[Zhuang, Qianlai] Purdue Univ, Dept Earth & Atmospher Sci, W Lafayette, IN 47906 USA.
[Zhuang, Qianlai] Purdue Univ, Dept Agron, W Lafayette, IN 47906 USA.
[Machida, Toshinobu] Natl Inst Environm Studies, CGER, Tsukuba, Ibaraki 3058506, Japan.
[Sweeney, Colm] NOAA, Global Monitoring Div, ESRL, Boulder, CO 80305 USA.
[Patra, Prabir K.] JAMSTEC, Res Inst Global Change, Yokohama, Kanagawa 236001, Japan.
RP Xiong, XZ (reprint author), Dell Perot Syst Govt Serv, Fairfax, VA USA.
EM xiaozhen.xiong@noaa.gov
RI Patra, Prabir/B-5206-2009; Xiong, Xiaozhen/F-6591-2010; Barnet,
Christopher/F-5573-2010; Ngan, Fong/G-1324-2012
OI Patra, Prabir/0000-0001-5700-9389; Ngan, Fong/0000-0002-7263-7727
FU NOAA Office of Application and Research; National Center of Ecological
Analysis and Synthesis (NCEAS)
FX This research was supported by funding from NOAA Office of Application
and Research. The views, opinions, and findings contained in this paper
are those of the authors and should not be construed as an official
National Oceanic and Atmospheric Administration or U. S. government
position, policy, or decision. This study also benefits from a Methane
Working Group supported by the National Center of Ecological Analysis
and Synthesis (NCEAS). We thank Central Aerological Observatory, Russia,
for conducting Surgut sampling and T. Nakazawa, Tohoku University, for
CH4 analysis before 2005. Also, we thank Nicholas R. Nalli
from NOAA/NESDIS for his kind help in editing the whole manuscript and
providing professional feedback, and we thank three anonymous reviewers
for their comments and constructive suggestions.
NR 58
TC 24
Z9 26
U1 0
U2 0
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-897X
EI 2169-8996
J9 J GEOPHYS RES-ATMOS
JI J. Geophys. Res.-Atmos.
PD OCT 9
PY 2010
VL 115
AR D19309
DI 10.1029/2009JD013796
PG 15
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 690MT
UT WOS:000285009600008
ER
PT J
AU Shindell, D
Schulz, M
Ming, Y
Takemura, T
Faluvegi, G
Ramaswamy, V
AF Shindell, Drew
Schulz, Michael
Ming, Yi
Takemura, Toshihiko
Faluvegi, Greg
Ramaswamy, V.
TI Spatial scales of climate response to inhomogeneous radiative forcing
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID GENERAL-CIRCULATION MODEL; SURFACE-TEMPERATURE; GREENHOUSE GASES;
SENSITIVITY; AEROSOLS; SYSTEM
AB The distances over which localized radiative forcing influences surface temperature have not been well characterized. We present a general methodology to analyze the spatial scales of the forcing/response relationship and apply it to simulations of historical aerosol forcing and response in four climate models. We find that the surface temperature response is not strongly sensitive to the longitude of forcing but is fairly sensitive to latitude. Surface temperature responses in the Arctic and the Southern Hemisphere extratropics, where forcing was small, show little relationship to local forcing. Restricting the analysis to 30 degrees S-60 degrees N, where nearly all the forcing was applied, shows that forcing strongly influences response out to similar to 4500 km away examining all directions. The meridional length of influence is somewhat shorter (similar to 3500 km or 30 degrees), while it extends out to at least 12,000 km in the zonal direction. Substantial divergences between the models are seen over the oceans, whose physical representations differ greatly among the models. Length scales are quite consistent over 30 degrees S-60 degrees N land areas, however, despite differences in both the forcing applied and the physics of the models themselves. The results suggest that better understanding of regionally inhomogeneous radiative forcing would lead to improved projections of regional climate change over land areas. They also provide quantitative estimates of the spatial extent of the climate impacts of pollutants, which can extend thousands of kilometers beyond polluted areas, especially in the zonal direction.
C1 [Shindell, Drew; Faluvegi, Greg] NASA, Goddard Inst Space Studies, New York, NY 10025 USA.
[Ming, Yi; Ramaswamy, V.] NOAA Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA.
[Schulz, Michael] CEA CNRS IPSL, Lab Sci Climat & Environm, F-91191 Gif Sur Yvette, France.
[Takemura, Toshihiko] Kyushu Univ, Appl Mech Res Inst, Fukuoka 8168580, Japan.
RP Shindell, D (reprint author), NASA, Goddard Inst Space Studies, 2880 Broadway, New York, NY 10025 USA.
EM drew.t.shindell@nasa.gov
RI Shindell, Drew/D-4636-2012; Takemura, Toshihiko/C-2822-2009; Ming,
Yi/F-3023-2012; Kyushu, RIAM/F-4018-2015; Schulz, Michael/A-6930-2011;
U-ID, Kyushu/C-5291-2016
OI Takemura, Toshihiko/0000-0002-2859-6067; Schulz,
Michael/0000-0003-4493-4158;
FU NASA; EU-EUCAARI [036833-2]
FX We thank NASA's Modeling and Analysis Program for support and Gavin
Schmidt for helpful discussion. IPSL model simulations could be accessed
thanks to the IPSL infrastructure Pole de modelisation, led by
Jean-Louis Dufresne and Pascale Braconnot. Analysis was also supported
by the (EU-EUCAARI) project (contract 036833-2).
NR 25
TC 44
Z9 46
U1 1
U2 17
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-897X
EI 2169-8996
J9 J GEOPHYS RES-ATMOS
JI J. Geophys. Res.-Atmos.
PD OCT 7
PY 2010
VL 115
AR D19110
DI 10.1029/2010JD014108
PG 10
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 716RG
UT WOS:000286990600015
ER
PT J
AU Wilson, SD
Yamani, Z
Rotundu, CR
Freelon, B
Valdivia, PN
Bourret-Courchesne, E
Lynn, JW
Chi, SX
Hong, T
Birgeneau, RJ
AF Wilson, Stephen D.
Yamani, Z.
Rotundu, C. R.
Freelon, B.
Valdivia, P. N.
Bourret-Courchesne, E.
Lynn, J. W.
Chi, Songxue
Hong, Tao
Birgeneau, R. J.
TI Antiferromagnetic critical fluctuations in BaFe2As2
SO PHYSICAL REVIEW B
LA English
DT Article
ID SPIN DYNAMICS; SUPERCONDUCTIVITY; LA2CUO4; WAVES
AB Magnetic correlations near the magnetostructural phase transition in the bilayer iron-pnictide parent compound, BaFe2As2, are measured. In close proximity to the antiferromagnetic phase transition in BaFe2As2, a crossover to three-dimensional critical behavior is anticipated and has been preliminarily observed. Here we report complementary measurements of two-dimensional magnetic fluctuations over a broad temperature range about T-N. The potential role of two-dimensional critical fluctuations in the magnetic phase behavior of BaFe2As2 and their evolution near the anticipated crossover to three-dimensional critical behavior and long-range order are discussed.
C1 [Wilson, Stephen D.; Rotundu, C. R.; Bourret-Courchesne, E.; Birgeneau, R. J.] Univ Calif Berkeley, Lawrence Berkeley Lab, Div Mat Sci, Berkeley, CA 94720 USA.
[Wilson, Stephen D.] Boston Coll, Dept Phys, Chestnut Hill, MA 02467 USA.
[Yamani, Z.] CNR, Canadian Neutron Beam Ctr, Chalk River Labs, Chalk River, ON K0J 1P0, Canada.
[Freelon, B.; Birgeneau, R. J.] Univ Calif Berkeley, Dept Phys, Berkeley, CA 94720 USA.
[Valdivia, P. N.; Birgeneau, R. J.] Univ Calif Berkeley, Dept Mat Sci, Berkeley, CA 94720 USA.
[Lynn, J. W.; Chi, Songxue] Natl Inst Stand & Technol, NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Chi, Songxue] Univ Maryland, Dept Mat Sci & Engn, College Pk, MD 20742 USA.
[Hong, Tao] Oak Ridge Natl Lab, Neutron Scattering Sci Div, Oak Ridge, TN 37831 USA.
RP Wilson, SD (reprint author), Univ Calif Berkeley, Lawrence Berkeley Lab, Div Mat Sci, Berkeley, CA 94720 USA.
EM stephen.wilson@bc.edu
RI Hong, Tao/F-8166-2010; yamani, zahra/B-7892-2012; Chi,
Songxue/A-6713-2013;
OI Hong, Tao/0000-0002-0161-8588; Chi, Songxue/0000-0002-3851-9153;
Rotundu, Costel/0000-0002-1571-8352
FU Office of Science, Office of Basic Energy Sciences, U.S. Department of
Energy [DE-AC02-05CH11231]; Office of Basic Energy Sciences, U.S. DOE
[DE-AC03-76SF008]; Division of Scientific User Facilities, Office of
Basic Energy Sciences, U.S. DOE
FX This work was supported by the Director, Office of Science, Office of
Basic Energy Sciences, U.S. Department of Energy under Contract No.
DE-AC02-05CH11231 and Office of Basic Energy Sciences, U.S. DOE under
Contract No. DE-AC03-76SF008. Work at ORNL was partially supported by
the Division of Scientific User Facilities, Office of Basic Energy
Sciences, U.S. DOE.
NR 25
TC 5
Z9 5
U1 2
U2 9
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 1098-0121
J9 PHYS REV B
JI Phys. Rev. B
PD OCT 6
PY 2010
VL 82
IS 14
AR 144502
DI 10.1103/PhysRevB.82.144502
PG 6
WC Physics, Condensed Matter
SC Physics
GA 659LS
UT WOS:000282568600006
ER
PT J
AU Hamme, RC
Webley, PW
Crawford, WR
Whitney, FA
DeGrandpre, MD
Emerson, SR
Eriksen, CC
Giesbrecht, KE
Gower, JFR
Kavanaugh, MT
Pena, MA
Sabine, CL
Batten, SD
Coogan, LA
Grundle, DS
Lockwood, D
AF Hamme, Roberta C.
Webley, Peter W.
Crawford, William R.
Whitney, Frank A.
DeGrandpre, Michael D.
Emerson, Steven R.
Eriksen, Charles C.
Giesbrecht, Karina E.
Gower, Jim F. R.
Kavanaugh, Maria T.
Pena, M. Angelica
Sabine, Christopher L.
Batten, Sonia D.
Coogan, Laurence A.
Grundle, Damian S.
Lockwood, Deirdre
TI Volcanic ash fuels anomalous plankton bloom in subarctic northeast
Pacific
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID SURFACE OCEAN; IRON; NE; PHYTOPLANKTON; VARIABILITY; DYNAMICS; NUTRIENT
AB Using multiple lines of evidence, we demonstrate that volcanic ash deposition in August 2008 initiated one of the largest phytoplankton blooms observed in the subarctic North Pacific. Unusually widespread transport from a volcanic eruption in the Aleutian Islands, Alaska deposited ash over much of the subarctic NE Pacific, followed by large increases in satellite chlorophyll. Surface ocean pCO(2), pH, and fluorescence reveal that the bloom started a few days after ashfall. Ship-based measurements showed increased dominance by diatoms. This evidence points toward fertilization of this normally iron-limited region by ash, a relatively new mechanism proposed for iron supply to the ocean. The observations do not support other possible mechanisms. Extrapolation of the pCO2 data to the area of the bloom suggests a modest similar to 0.01 Pg carbon export from this event, implying that even large-scale iron fertilization at an optimum time of year is not very efficient at sequestering atmospheric CO(2). Citation: Hamme, R. C., et al. (2010), Volcanic ash fuels anomalous plankton bloom in subarctic northeast Pacific, Geophys. Res. Lett., 37, L19604, doi:10.1029/2010GL044629.
C1 [Hamme, Roberta C.; Giesbrecht, Karina E.; Coogan, Laurence A.; Grundle, Damian S.] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3V6, Canada.
[Webley, Peter W.] Univ Alaska Fairbanks, Inst Geophys, Alaska Volcano Observ, Fairbanks, AK 99775 USA.
[Crawford, William R.; Whitney, Frank A.; Gower, Jim F. R.; Pena, M. Angelica] Fisheries & Oceans Canada, Inst Ocean Sci, Sidney, BC V8L 4B2, Canada.
[DeGrandpre, Michael D.] Univ Montana, Dept Chem & Biochem, Missoula, MT 59812 USA.
[Emerson, Steven R.; Eriksen, Charles C.; Lockwood, Deirdre] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA.
[Kavanaugh, Maria T.] Oregon State Univ, Coll Ocean & Atmospher Sci, Corvallis, OR 97331 USA.
[Sabine, Christopher L.] NOAA, Pacific Marine Environm Lab, Seattle, WA 98115 USA.
[Batten, Sonia D.] Sir Alister Hardy Fdn Ocean Sci, Nanaimo, BC V9V 1N8, Canada.
RP Hamme, RC (reprint author), Univ Victoria, Sch Earth & Ocean Sci, POB 3065 STN CSC, Victoria, BC V8W 3V6, Canada.
EM rhamme@uvic.ca
RI Giesbrecht, Karina/B-1405-2013; Webley, Peter/F-8238-2015;
OI Webley, Peter/0000-0001-5327-8151; Kavanaugh, Maria/0000-0001-6126-6177
FU NSERC; DFO; NSF; NOAA; SAHFOS
FX We thank M. Robert and Fisheries and Oceans Canada staff for core
measurements and support on Line P cruises, as well as the scientists
and crew on the August 2008 cruises (Tully 2008-27 and Thompson TN224).
Funding support by NSERC, DFO, NSF, NOAA, SAHFOS.
NR 26
TC 81
Z9 84
U1 2
U2 46
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD OCT 5
PY 2010
VL 37
AR L19604
DI 10.1029/2010GL044629
PG 5
WC Geosciences, Multidisciplinary
SC Geology
GA 661XU
UT WOS:000282767500001
ER
PT J
AU Painter, TH
Deems, JS
Belnap, J
Hamlet, AF
Landry, CC
Udall, B
AF Painter, Thomas H.
Deems, Jeffrey S.
Belnap, Jayne
Hamlet, Alan F.
Landry, Christopher C.
Udall, Bradley
TI Response of Colorado River runoff to dust radiative forcing in snow
SO PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF
AMERICA
LA English
DT Article
DE aerosols; land use change; reflectivity; snow melt
ID WESTERN UNITED-STATES; BIOLOGICAL SOIL CRUSTS; WATER AVAILABILITY;
CARBON-DIOXIDE; CLIMATE-CHANGE; CO2; IMPACTS; TRENDS; MODEL; DEPOSITION
AB The waters of the Colorado River serve 27 million people in seven states and two countries but are overallocated by more than 10% of the river's historical mean. Climate models project runoff losses of 7-20% from the basin in this century due to human-induced climate change. Recent work has shown however that by the late 1800s, decades prior to allocation of the river's runoff in the 1920s, a fivefold increase in dust loading from anthropogenically disturbed soils in the southwest United States was already decreasing snow albedo and shortening the duration of snow cover by several weeks. The degree to which this increase in radiative forcing by dust in snow has affected timing and magnitude of runoff from the Upper Colorado River Basin (UCRB) is unknown. Here we use the Variable Infiltration Capacity model with postdisturbance and pre-disturbance impacts of dust on albedo to estimate the impact on runoff from the UCRB across 1916-2003. We find that peak runoff at Lees Ferry, Arizona has occurred on average 3 wk earlier under heavier dust loading and that increases in evapotranspiration from earlier exposure of vegetation and soils decreases annual runoff by more than 1.0 billion cubic meters or similar to 5% of the annual average. The potential to reduce dust loading through surface stabilization in the deserts and restore more persistent snow cover, slow runoff, and increase water resources in the UCRB may represent an important mitigation opportunity to reduce system management tensions and regional impacts of climate change.
C1 [Painter, Thomas H.] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA.
[Painter, Thomas H.] Univ Calif Los Angeles, Joint Inst Reg Earth Syst Sci & Engn, Los Angeles, CA 90095 USA.
[Deems, Jeffrey S.] Natl Snow & Ice Data Ctr, Boulder, CO 80309 USA.
[Deems, Jeffrey S.; Udall, Bradley] Natl Ocean & Atmospher Adm Western Water Assessme, Boulder, CO 80309 USA.
[Belnap, Jayne] US Geol Survey, SW Biol Ctr, Moab, UT 84532 USA.
[Hamlet, Alan F.] Univ Washington, Dept Civil & Environm Engn, Seattle, WA 98195 USA.
[Landry, Christopher C.] Ctr Snow & Avalanche Studies, Silverton, CO 81433 USA.
RP Painter, TH (reprint author), CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91109 USA.
EM Thomas.Painter@jpl.nasa.gov
RI Painter, Thomas/B-7806-2016; Deems, Jeffrey/E-6484-2016
OI Deems, Jeffrey/0000-0002-3265-8670
FU National Science Foundation [ATM0432327]; NASA [NNG04GC52A]
FX We thank J. Sparks, T. Belote, S. Munson, and D. S. Schimel for comments
on the manuscript. We express special thanks to Jeff Dozier for a tough,
thorough, and constructive exchange on the full range of the paper. T.
H. P. was funded by National Science Foundation Grant ATM0432327 and
NASA Cooperative Agreement NNG04GC52A. Part of this work was performed
at the Jet Propulsion Laboratory, California Institute of Technology,
under a contract with the National Aeronautics and Space Administration.
NR 55
TC 112
Z9 113
U1 3
U2 58
PU NATL ACAD SCIENCES
PI WASHINGTON
PA 2101 CONSTITUTION AVE NW, WASHINGTON, DC 20418 USA
SN 0027-8424
J9 P NATL ACAD SCI USA
JI Proc. Natl. Acad. Sci. U. S. A.
PD OCT 5
PY 2010
VL 107
IS 40
BP 17125
EP 17130
DI 10.1073/pnas.0913139107
PG 6
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA 658TJ
UT WOS:000282512000016
PM 20855581
ER
PT J
AU Spietz, L
Irwin, K
Lee, M
Aumentado, J
AF Spietz, Lafe
Irwin, Kent
Lee, Minhyea
Aumentado, Jose
TI Noise performance of lumped element direct current superconducting
quantum interference device amplifiers in the 4-8 GHz range
SO APPLIED PHYSICS LETTERS
LA English
DT Article
ID SQUID
AB We report on the noise of a lumped element direct current superconducting quantum interference device amplifier. We show that the noise temperature in the 4-8 GHz range over ranges of tens of megahertz is below 1 K (three photons of added noise), characterize the overall behavior of the noise as a function of bias parameters, and discuss potential mechanisms which determine the noise performance in this amplifier. We show that this device can provide more than a factor of 10 improvement in practical system noise over existing phase-preserving microwave measurement systems in this frequency band. (C) 2010 American Institute of Physics. [doi:10.1063/1.3497008]
C1 [Spietz, Lafe; Irwin, Kent; Lee, Minhyea; Aumentado, Jose] Natl Inst Stand & Technol, Boulder, CO 80305 USA.
RP Spietz, L (reprint author), Natl Inst Stand & Technol, Boulder, CO 80305 USA.
EM lafe.spietz@boulder.nist.gov
RI Aumentado, Jose/C-2231-2009;
OI Aumentado, Jose/0000-0001-5581-1466; Irwin, Kent/0000-0002-2998-9743
NR 13
TC 11
Z9 11
U1 0
U2 3
PU AMER INST PHYSICS
PI MELVILLE
PA CIRCULATION & FULFILLMENT DIV, 2 HUNTINGTON QUADRANGLE, STE 1 N O 1,
MELVILLE, NY 11747-4501 USA
SN 0003-6951
J9 APPL PHYS LETT
JI Appl. Phys. Lett.
PD OCT 4
PY 2010
VL 97
IS 14
AR 142502
DI 10.1063/1.3497008
PG 3
WC Physics, Applied
SC Physics
GA 661XF
UT WOS:000282765700046
ER
PT J
AU Xu, H
Chen, L
Hu, LB
Zhitenev, N
AF Xu, Hua
Chen, Lei
Hu, Liangbing
Zhitenev, Nikolai
TI Contact resistance of flexible, transparent carbon nanotube films with
metals
SO APPLIED PHYSICS LETTERS
LA English
DT Article
ID ELECTRONICS
AB We studied the contact properties of different metals to optically-transparent single-walled carbon nanotube (SWCNT) films using fabrication processes compatible with flexible electronic applications. The SWCNT films are deposited on flexible polyethylene terephthalate substrate and patterned in test structures optimized for contact resistance measurements for a particular metal contact. Specific contact resistance and current transfer length is determined for Pt, Cr, Cu, and Au contacts. We also evaluate effects of chemical doping and thickness of SWCNT films on the contact resistance. We find that the current transfer length, defining the minimal dimensions of efficient contacts to transparent SWCNT films, ranges from 8 X 10(-6) to 10(-4) m for different metals. (C) 2010 American Institute of Physics. [doi:10.1063/1.3496465]
C1 [Xu, Hua; Chen, Lei; Zhitenev, Nikolai] NIST, Ctr Nanoscale Sci & Technol, Gaithersburg, MD 20899 USA.
[Xu, Hua] Univ Maryland, Maryland NanoCtr, College Pk, MD 20742 USA.
[Hu, Liangbing] Univ Calif Los Angeles, Dept Phys, Los Angeles, CA 90095 USA.
RP Xu, H (reprint author), NIST, Ctr Nanoscale Sci & Technol, Gaithersburg, MD 20899 USA.
EM huxu@nist.gov
RI Hu, Liangbing/C-5589-2011; Xu, Hua/D-5217-2009; Zhitenev,
Nikolai/N-1780-2014; Hu, Liangbing/N-6660-2013
FU NIST-CNST/UMD-Nanocenter Cooperative Agreement
FX The authors would like to thank the staff of the NanoFab at the Center
for Nanoscale Science and Technology for the help with the patterning
process development. This work was supported in part by the
NIST-CNST/UMD-Nanocenter Cooperative Agreement.
NR 23
TC 13
Z9 13
U1 1
U2 24
PU AMER INST PHYSICS
PI MELVILLE
PA CIRCULATION & FULFILLMENT DIV, 2 HUNTINGTON QUADRANGLE, STE 1 N O 1,
MELVILLE, NY 11747-4501 USA
SN 0003-6951
J9 APPL PHYS LETT
JI Appl. Phys. Lett.
PD OCT 4
PY 2010
VL 97
IS 14
AR 143116
DI 10.1063/1.3496465
PG 3
WC Physics, Applied
SC Physics
GA 661XF
UT WOS:000282765700068
ER
PT J
AU Brioude, J
Portmann, RW
Daniel, JS
Cooper, OR
Frost, GJ
Rosenlof, KH
Granier, C
Ravishankara, AR
Montzka, SA
Stohl, A
AF Brioude, J.
Portmann, R. W.
Daniel, J. S.
Cooper, O. R.
Frost, G. J.
Rosenlof, K. H.
Granier, C.
Ravishankara, A. R.
Montzka, S. A.
Stohl, A.
TI Variations in ozone depletion potentials of very short-lived substances
with season and emission region
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID PARTICLE DISPERSION MODEL; STRATOSPHERE; TROPOSPHERE; CLIMATE
AB We present a new approach for calculating the fraction of very-short lived substances (VSLS) emitted at the surface (and their degradation products) that reach the stratosphere (beta) using the FLEXPART Lagrangian model. The values of beta play a key role in determining the efficiency of these compounds for depleting stratospheric ozone, and are used to estimate ozone depletion potentials (ODPs) of several short-lived compounds. Calculated beta and ODPs of VSLSs show large regional and seasonal variability owing to the importance of convective transport. For instance, beta and ODPs associated with emissions from the Indian subcontinent is an order of magnitude larger than that from Europe, mid-latitude North America, or East Asia. The seasonal cycle of beta is mainly driven by transport efficiency from the boundary layer into the tropical stratosphere; beta has a minimum in winter and a maximum in summer. Citation: Brioude, J., R. W. Portmann, J. S. Daniel, O. R. Cooper, G. J. Frost, K. H. Rosenlof, C. Granier, A. R. Ravishankara, S. A. Montzka, and A. Stohl (2010), Variations in ozone depletion potentials of very short-lived substances with season and emission region, Geophys. Res. Lett., 37, L19804, doi: 10.1029/2010GL044856.
C1 [Brioude, J.; Portmann, R. W.; Daniel, J. S.; Cooper, O. R.; Frost, G. J.; Rosenlof, K. H.; Granier, C.; Ravishankara, A. R.] NOAA, Div Chem Sci, Earth Syst Res Lab, Boulder, CO 80305 USA.
[Montzka, S. A.] NOAA, Global Monitoring Div, Earth Syst Res Lab, Boulder, CO 80305 USA.
[Stohl, A.] Norwegian Inst Air Res, N-2027 Kjeller, Norway.
[Brioude, J.; Cooper, O. R.; Frost, G. J.; Granier, C.] Univ Colorado, CIRES, Boulder, CO 80309 USA.
[Granier, C.] Univ Paris 06, LATMOS, IPSL, INSU,CNRS, Paris, France.
RP Brioude, J (reprint author), NOAA, Div Chem Sci, Earth Syst Res Lab, 325 Broadway, Boulder, CO 80305 USA.
EM jerome.brioude@noaa.gov
RI Portmann, Robert/C-4903-2009; Daniel, John/D-9324-2011; Stohl,
Andreas/A-7535-2008; Brioude, Jerome/E-4629-2011; Granier,
Claire/D-5360-2013; Cooper, Owen/H-4875-2013; Frost,
Gregory/I-1958-2013; Ravishankara, Akkihebbal/A-2914-2011; Rosenlof,
Karen/B-5652-2008; Manager, CSD Publications/B-2789-2015;
OI Portmann, Robert/0000-0002-0279-6087; Stohl,
Andreas/0000-0002-2524-5755; Granier, Claire/0000-0001-7344-7995;
Rosenlof, Karen/0000-0002-0903-8270; Montzka,
Stephen/0000-0002-9396-0400
FU European Commission; NOAA
FX We thank Vladimir Orkin for providing some of the loss rates used in the
paper and Chi-Fan Shih for providing ERA-interim data. AS was supported
by the European Commission as part of the SHIVA project. This work was
supported by NOAA Climate Research Program.
NR 14
TC 18
Z9 18
U1 0
U2 17
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD OCT 2
PY 2010
VL 37
AR L19804
DI 10.1029/2010GL044856
PG 5
WC Geosciences, Multidisciplinary
SC Geology
GA 657SQ
UT WOS:000282433000008
ER
PT J
AU Li, XF
Yang, XF
Zheng, QA
Pietrafesa, LJ
Pichel, WG
Li, ZW
Li, XM
AF Li, Xiaofeng
Yang, Xiaofeng
Zheng, Quanan
Pietrafesa, Leonard J.
Pichel, William G.
Li, Ziwei
Li, Xiaoming
TI Deep-water bathymetric features imaged by spaceborne SAR in the Gulf
Stream region
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID SEA BOTTOM TOPOGRAPHY; RADAR IMAGERY; NANTUCKET SHOALS; WAVES
AB Deep-water (>500 m) oceanic bathymetric features are frequently observed in RADARSAT-1 SAR images in the Gulf Stream (GS) region. They are imaged apparently because of the unique environmental conditions in the region, oceanographically characterized by a strong GS current (2 ms(-1)) and favorable ocean stratification. SAR image analysis shows the basic characteristics of these bathymetric features. A coincident sea surface temperature image shows that the bathymetric feature is only "visible" by SAR within the GS pathway. The dominant wavelength of the wave-like feature is about 2.3 km and their crests are perpendicular to the GS axis. Shipboard sounding measurements confirm the SAR observation. A theoretical consideration of the ocean current and corrugated bathymetry interaction in a 3-layer ocean is presented. Using representative ocean density profile data and the GS current data, we analyze the requirements for the generation and upward propagation of the disturbance induced by the current-bathymetry interaction. Citation: Li, X., X. Yang, Q. Zheng, L. J. Pietrafesa, W. G. Pichel, Z. Li, and X. Li (2010), Deep-water bathymetric features imaged by spaceborne SAR in the Gulf Stream region, Geophys. Res. Lett., 37, L19603, doi: 10.1029/2010GL044406.
C1 [Li, Xiaofeng] NOAA, IMSG, NESDIS, Camp Springs, MD 20746 USA.
[Li, Xiaoming] German Aerosp Ctr, Remote Sensing Technol Inst, D-82234 Wessling, Germany.
[Yang, Xiaofeng; Li, Ziwei] Chinese Acad Sci, Inst Remote Sensing Applicat, Beijing 100101, Peoples R China.
[Pichel, William G.] NOAA, Ctr Satellite Applicat & Res, NESDIS, Camp Springs, MD 20746 USA.
[Pietrafesa, Leonard J.] N Carolina State Univ, MEAS, Raleigh, NC 27695 USA.
[Zheng, Quanan] Univ Maryland, Dept Atmospher & Ocean Sci, College Pk, MD 20742 USA.
RP Li, XF (reprint author), NOAA, IMSG, NESDIS, 5200 Auth Rd, Camp Springs, MD 20746 USA.
EM xiaofeng.li@noaa.gov
RI Pichel, William/F-5619-2010; yang, xiaofeng/K-5245-2015; Li,
Xiaofeng/B-6524-2008
OI Pichel, William/0000-0001-6332-0149; yang, xiaofeng/0000-0001-9920-4641;
Li, Xiaofeng/0000-0001-7038-5119
NR 14
TC 13
Z9 13
U1 1
U2 12
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
EI 1944-8007
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD OCT 2
PY 2010
VL 37
AR L19603
DI 10.1029/2010GL044406
PG 6
WC Geosciences, Multidisciplinary
SC Geology
GA 657SQ
UT WOS:000282433000004
ER
PT J
AU McClatchie, S
Goericke, R
Cosgrove, R
Auad, G
Vetter, R
AF McClatchie, S.
Goericke, R.
Cosgrove, R.
Auad, G.
Vetter, R.
TI Oxygen in the Southern California Bight: Multidecadal trends and
implications for demersal fisheries
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID BATHYMETRIC DEMOGRAPHY; SEBASTES; HYPOXIA; ECOSYSTEM; PACIFIC
AB Reports of hypoxic conditions (oxygen <1.5 ml L(-1)) off the U.S. west coast over the last two decades led us to investigate hypoxia in the Southern California Bight (SCB) and its potential impacts on fisheries. The secular trend in hypoxia in the SCB over the last 57 years is not monotonic, and reversed trend in the mid-1980s, bringing oxygen concentrations back to levels measured in the late 1950s to early 1960s. Thirty-seven percent of the rockfish (Sebastes spp.) habitat in the Cowcod Conservation Area at 240-350 m depths suffers exposure to hypoxia in the summer of normal years. If current trends in shoaling of low oxygen water continue for another 20 years, rather than reversing as happened previously, we predict loss of 18% of the habitat with 55% of the total habitat exposed to hypoxia. Citation: McClatchie, S., R. Goericke, R. Cosgrove, G. Auad, and R. Vetter (2010), Oxygen in the Southern California Bight: Multidecadal trends and implications for demersal fisheries, Geophys. Res. Lett., 37, L19602, doi: 10.1029/2010GL044497.
C1 [McClatchie, S.; Cosgrove, R.; Vetter, R.] SW Fisheries Sci Ctr, La Jolla, CA 92037 USA.
[Auad, G.] US Dept Interior, Environm Studies Program, Bur Ocean Energy Management, Herndon, VA 20170 USA.
[Goericke, R.] Univ Calif San Diego, Integrat Oceanog Div, Scripps Inst Oceanog, La Jolla, CA 92093 USA.
RP McClatchie, S (reprint author), SW Fisheries Sci Ctr, 8604 La Jolla Shores Dr, La Jolla, CA 92037 USA.
EM sam.mcclatchie@noaa.gov
FU National Oceanic Atmospheric Administration
FX Ron Lynn, Steven Bograd, Lou Zeidberg, Lisa Levin, Paul Fiedler, Tim
Baumgartner and John Field provided helpful comment on the manuscript.
This research was funded by the Fisheries And The Environment program
(FATE) of the NOAA Fisheries Service of the National Oceanic Atmospheric
Administration.
NR 15
TC 58
Z9 58
U1 1
U2 14
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0094-8276
J9 GEOPHYS RES LETT
JI Geophys. Res. Lett.
PD OCT 2
PY 2010
VL 37
AR L19602
DI 10.1029/2010GL044497
PG 5
WC Geosciences, Multidisciplinary
SC Geology
GA 657SQ
UT WOS:000282433000006
ER
PT J
AU Gann, RG
Averill, JD
Johnsson, EL
Nyden, MR
Peacock, RD
AF Gann, Richard G.
Averill, Jason D.
Johnsson, Erik L.
Nyden, Marc R.
Peacock, Richard D.
TI Fire effluent component yields from room-scale fire tests
SO FIRE AND MATERIALS
LA English
DT Article
DE fire; fire research; smoke; room fire tests; fire toxicity; smoke
toxicity; toxicity
ID TOXIC POTENCY; COMBUSTION; SMOKE
AB Estimation of the time available for escape (ASET) in the event of a fire is a principal component in fire hazard or risk assessment. Valid data on the yields of toxic smoke components from bench-scale apparatus is essential to accurate ASET calculations This paper presents a methodology for obtaining pre-flashover and post-flashover toxicant yields from room-scale fire tests. The data are to be used for comparison with bench-scale data for the same combustibles: a sofa, bookcases, and electric power cable. Each was burned in a room with a long adjacent corridor. The yields of CO(2), CO, HCl, HCN, and soot were determined. Other toxicants (NO(2), formaldehyde, and acrolein), whose concentrations were below the detection limits, were of limited importance relative to the detected toxicants. The uncertainty values were comparable to those estimated for calculations used to determine ASET and were sufficiently small to determine whether a bench-scale apparatus is producing results that are similar to the real-scale results here. The use of Fourier transform infrared spectroscopy was useful for obtaining toxicant concentration data; however, its operation and interpretation are not routine. The losses of CO, HCN, and HCl along the corridor were dependent on the combustible. Copyright (C) 2009 John Wiley & Sons, Ltd.
C1 [Gann, Richard G.; Averill, Jason D.; Johnsson, Erik L.; Nyden, Marc R.; Peacock, Richard D.] Natl Inst Stand & Technol, Bldg & Fire Res Lab, Fire Res Div, Gaithersburg, MD 20899 USA.
RP Gann, RG (reprint author), Natl Inst Stand & Technol, Bldg & Fire Res Lab, Fire Res Div, Gaithersburg, MD 20899 USA.
EM rggann@nist.gov
FU National Institute of Standards and Technology; Alliance for the
Polyurethane Industry; American Plastics Council; DuPont; Lamson &
Sessions; Underwriters Laboratories; Vinyl Institute
FX Contract/grant sponsors: National Institute of Standards and Technology,
the Alliance for the Polyurethane Industry, the American Plastics
Council, DuPont, Lamson & Sessions, Underwriters Laboratories, and the
Vinyl Institute under the aegis of the Fire Protection Research
Foundation; This research was sponsored by the National Institute of
Standards and Technology, the Alliance for the Polyurethane Industry,
the American Plastics Council, DuPont, Lamson & Sessions, Underwriters
Laboratories, and the Vinyl Institute under the aegis of the Fire
Protection Research Foundation and the supervision of Frederick Mulhaupt
and Steven Hanly.
NR 32
TC 2
Z9 2
U1 1
U2 8
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0308-0501
J9 FIRE MATER
JI Fire Mater.
PD OCT
PY 2010
VL 34
IS 6
BP 285
EP 314
DI 10.1002/fam.1024
PG 30
WC Materials Science, Multidisciplinary
SC Materials Science
GA 672TE
UT WOS:000283609000002
ER
PT J
AU Gillaspy, JD
AF Gillaspy, J. D.
TI Testing QED in sodium-like gold and xenon: using atomic spectroscopy and
an EBIT to probe the quantum vacuum
SO JOURNAL OF INSTRUMENTATION
LA English
DT Article; Proceedings Paper
CT International Symposium on Electron Beam Ion Sources and Traps
CY APR 07-10, 2010
CL Stockholm, SWEDEN
DE Ion sources (positive ions, negative ions, electron cyclotron, resonance
(ECR), electron beam (EBIS)); Plasma diagnostics - interferometry,
spectroscopy and imaging
ID FREQUENCY COMB SPECTROSCOPY; CU-LIKE IONS; NA-LIKE; FINE-STRUCTURE;
PRECISION-MEASUREMENT; NOBEL LECTURE; LAMB SHIFTS; H-ALPHA; HELIUM;
ENERGY
AB Electron Beam Ion Traps (EBITs) can strip atoms to their electronic cores, revealing strong perturbations of the quantum vacuum that occur at electric field strengths comparable to those in petawatt lasers focused to their diffraction limit. Wavelengths of the D-lines in sodium-like ions measured previously using the NIST EBIT are discussed in terms of testing quantum electrodynamics in the high-field limit. The accuracy of our measurements in Au(68+) (0.03 eV), together with the estimated accuracy of a corresponding calculation (0.02 eV), provide a 0.6% test of QED, the most precise currently available in any sodium-like ion. This measurement tests the predictions of QED for sodium-like ions to more fractional accuracy than even the best results available in hydrogen-like uranium. For the case of Na-like Xe(43+), where a modest discrepancy exists between theory and measurements from three independent groups, an apparent collision-energy dependence is revealed which may account for the discrepancy.
C1 NIST, Gaithersburg, MD 20899 USA.
RP Gillaspy, JD (reprint author), NIST, 100 Bur Dr, Gaithersburg, MD 20899 USA.
EM john.gillaspy@nist.gov
NR 66
TC 6
Z9 6
U1 1
U2 7
PU IOP PUBLISHING LTD
PI BRISTOL
PA DIRAC HOUSE, TEMPLE BACK, BRISTOL BS1 6BE, ENGLAND
SN 1748-0221
J9 J INSTRUM
JI J. Instrum.
PD OCT
PY 2010
VL 5
AR C10005
DI 10.1088/1748-0221/5/10/C10005
PG 13
WC Instruments & Instrumentation
SC Instruments & Instrumentation
GA 675AZ
UT WOS:000283797200014
ER
PT J
AU Nikoobakht, B
Herzing, A
AF Nikoobakht, Babak
Herzing, Andrew
TI Formation of Planar Arrays of One-Dimensional p-n Heterojunctions Using
Surface-Directed Growth of Nanowires and Nanowalls
SO ACS NANO
LA English
DT Article
DE surface-directed growth; directed assembly; nanowires; nanowalls; zinc
oxide; p-n heterojunction
ID LIGHT-EMITTING-DIODES; ZINC-OXIDE NANOWIRES; SILICON NANOWIRES;
THIN-FILM; SEMICONDUCTOR NANOWIRES; SOLAR-CELLS; ZNO; FABRICATION; GAN;
DEVICES
AB We report a surface-directed vapor-liquid-solid process for planar growth of one-dimensional heterojunctions of zinc oxide on single crystal gallium nitride (GaN) that enables their hierarchical assembly to light emitting diodes. An individual heterojunction is about 10 mu m in length and 80 nm in width and is formed by planar growth of an n-type ZnO nanowire or nanowall on p-type GaN surface using Au catalyst. Our results show that a ZnO nanocrystal at its nucleation site has six possible growth directions that can be engineered and controlled using an intentional blockade of the nanocrystal growth in certain directions owing to similarities in crystal structures of ZnO and GaN. The ZnO nanowalls are formed when nanowires during their planar growth slowly grow in direction normal to the substrate via a self-catalytic process. The crystal structure of these heterojunctions is examined from two different crystallographic perspectives using high resolution transmission electron microscopy. Results indicate abrupt and epitaxial formation of n-p heterojunctions, which are difficult to achieve in thin film growth of these heterojunctions. The collective light emission of micrometer- to millimeter-size arrays of the heterojunctions is demonstrated via a simple design that is scalable to literally any platform size. This technique allows in situ growth and combinations of II-VI and III-V semiconductors and offers their easier integration to photonic and lab-on-chip platforms with applications in energy generation and light detection.
C1 [Nikoobakht, Babak; Herzing, Andrew] NIST, Surface & Microanal Sci Div, Gaithersburg, MD 20899 USA.
RP Nikoobakht, B (reprint author), NIST, Surface & Microanal Sci Div, 100 Bur Dr,Stop 8372, Gaithersburg, MD 20899 USA.
EM babakn@nist.gov
RI Nikoobakht, Babak/D-7562-2011; Herzing, Andrew/D-6239-2012
NR 38
TC 25
Z9 25
U1 3
U2 48
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 1936-0851
J9 ACS NANO
JI ACS Nano
PD OCT
PY 2010
VL 4
IS 10
BP 5877
EP 5886
DI 10.1021/nn1019972
PG 10
WC Chemistry, Multidisciplinary; Chemistry, Physical; Nanoscience &
Nanotechnology; Materials Science, Multidisciplinary
SC Chemistry; Science & Technology - Other Topics; Materials Science
GA 670UV
UT WOS:000283453700054
PM 20843070
ER
PT J
AU Havey, DK
Bueno, PA
Gillis, KA
Hodges, JT
Mulholland, GW
van Zee, RD
Zachariah, MR
AF Havey, Daniel K.
Bueno, Pedro A.
Gillis, Keith A.
Hodges, Joseph T.
Mulholland, George W.
van Zee, Roger D.
Zachariah, Michael R.
TI Photoacoustic Spectrometer with a Calculable Cell Constant for
Measurements of Gases and Aerosols
SO ANALYTICAL CHEMISTRY
LA English
DT Article
ID O-2 A-BAND; LIGHT-ABSORPTION; CAVITY RING; BLACK CARBON; LINE
PARAMETERS; SPECTROSCOPY; CALIBRATION; INSTRUMENTS; UNCERTAINTY;
VALIDATION
AB We benchmark the performance of a photoacoustic spectrometer with a calculable cell constant in applications related to climate change measurements. As presently implemented, this spectrometer has a detection limit of 3.1 x 10(-9) cm(-1) Hz(-1/2) for absorption by a gas and 1.5 x 10(-8) cm(-1) Hz(-1/2) for soot particles. Non-statistical uncertainty limited the accuracy of the instrument to similar to 1%, and measurements of the concentration of CO(2) in laboratory air agreed with measurements made using a cavity ring-down spectrometer, to within 1%. Measurements of the enhanced absorption resulting from ultrathin (<5 nm), nonabsorbing coatings on nanoscale soot particles demonstrate the sensitivity of this instrument. Together, these measurements show the instrument's ability to quantitatively measure the absorption coefficient for species of interest to the climate and atmospheric science communities. Because the system constant is known, in most applications the acoustic response of this instrument need not be calibrated against a sample of known optical density, a decided advantage in field applications. Routine enhancements, such as improved processing of the photoacoustic signal and higher laser beam power, should further increase the instrument's precision and sensitivity.
C1 [Havey, Daniel K.] James Madison Univ, Dept Chem & Biochem, Harrisonburg, VA 22807 USA.
[Havey, Daniel K.; Bueno, Pedro A.; Gillis, Keith A.; Hodges, Joseph T.; Mulholland, George W.; van Zee, Roger D.; Zachariah, Michael R.] Natl Inst Stand & Technol, Chem Sci & Technol Lab, Gaithersburg, MD 20899 USA.
[Bueno, Pedro A.; Mulholland, George W.; Zachariah, Michael R.] Univ Maryland, Dept Mech Engn, College Pk, MD 20742 USA.
[Bueno, Pedro A.; Mulholland, George W.; Zachariah, Michael R.] Univ Maryland, Dept Chem & Biochem, College Pk, MD 20742 USA.
RP Havey, DK (reprint author), James Madison Univ, Dept Chem & Biochem, MSC 4501, Harrisonburg, VA 22807 USA.
FU National Research Council
FX D. K. Havey received support from the National Research Council as a
postdoctoral fellow at NIST. K. L. Plath is thanked for providing
assistance with CRDS measurements of CO2 concentrations in
laboratory air.
NR 53
TC 15
Z9 15
U1 0
U2 32
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0003-2700
J9 ANAL CHEM
JI Anal. Chem.
PD OCT 1
PY 2010
VL 82
IS 19
BP 7935
EP 7942
DI 10.1021/ac101366e
PG 8
WC Chemistry, Analytical
SC Chemistry
GA 655NT
UT WOS:000282257400012
PM 20804170
ER
PT J
AU Restrepo, VR
Diaz, GA
Walter, JF
Neilson, JD
Campana, SE
Secor, D
Wingate, RL
AF Restrepo, Victor R.
Diaz, Guillermo A.
Walter, John F.
Neilson, John D.
Campana, Steven E.
Secor, David
Wingate, Rebecca L.
TI Updated estimate of the growth curve of Western Atlantic bluefin tuna
SO AQUATIC LIVING RESOURCES
LA English
DT Article
DE Atlantic bluefin tuna; Thunnus thynnus; Western stock; Growth; von
Bertalanffy
ID THUNNUS-MACCOYII; AGE
AB The curve used until recently by the International Commission for the Conservation of Atlantic Tunas (ICCAT) to represent the growth of western Atlantic bluefin tuna, Thunnus thynnus, was estimated using tagging information and modal sizes that corresponded primarily to very young fish (ages 1-3, primarily). The estimated maximum average size from this curve is very large (382 cm), which could be a result of the scarcity of large bluefin in the data used. Recently, scientists have developed techniques for reading ages from bluefin ear bones (otoliths); the accuracy of the age readings has been validated with bomb radiocarbon dating. These age readings are primarily for large bluefin (ages 5 and older), and indicate slower growth and older ages than was previously assumed. However, an analysis of these data resulted in growth curves that predicted very small mean sizes for the youngest age group, which could be a result of the lack of small fish in the data used. In this study, we combine the otolith-based age readings with the size frequency distributions of small (ages 1-3) bluefin caught by purse seiners in the 1970s where the age groups are distinctly statistically as well as visible to the eye. We analyzed the two datasets jointly using a maximum likelihood approach and assumed that variability in length-at-age increases with age. The resulting growth curve predicts sizes at young and old ages that are very consistent with observed data such as the maximum sizes observed in the catch and the modal sizes for very young bluefin. The resulting curve is also very similar to the curve used by ICCAT for eastern Atlantic and Mediterranean bluefin.
C1 [Restrepo, Victor R.] Int Seafood Sustainabil Fdn, Mclean, VA 22102 USA.
[Diaz, Guillermo A.] NOAA Fisheries, Off Sci & Technol, Silver Spring, MD 20910 USA.
[Walter, John F.] NOAA Fisheries, SE Fisheries Sci Ctr, Miami, FL 33149 USA.
[Neilson, John D.] Fisheries & Oceans Canada, Biol Stn, St Andrews, NB E5B 2L9, Canada.
[Campana, Steven E.] Fisheries & Oceans Canada, Bedford Inst Oceanog, Dartmouth, NS B2Y 4A2, Canada.
[Secor, David; Wingate, Rebecca L.] Univ Maryland, Ctr Environm Sci, Chesapeake Biol Lab, Solomons, MD 20688 USA.
RP Restrepo, VR (reprint author), Int Seafood Sustainabil Fdn, POB 11110, Mclean, VA 22102 USA.
EM vrestrepo@iss-foundation.org
RI Campana, Steven/C-3420-2013
OI Campana, Steven/0000-0001-8802-3976
NR 15
TC 26
Z9 26
U1 1
U2 26
PU EDP SCIENCES S A
PI LES ULIS CEDEX A
PA 17, AVE DU HOGGAR, PA COURTABOEUF, BP 112, F-91944 LES ULIS CEDEX A,
FRANCE
SN 0990-7440
J9 AQUAT LIVING RESOUR
JI Aquat. Living Resour.
PD OCT-DEC
PY 2010
VL 23
IS 4
BP 335
EP 342
DI 10.1051/alr/2011004
PG 8
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 716MU
UT WOS:000286975000001
ER
PT J
AU Day, BM
Rappengluck, B
Clements, CB
Tucker, SC
Brewer, WA
AF Day, Bridget M.
Rappenglueck, Bernhard
Clements, Craig B.
Tucker, Sara C.
Brewer, W. Alan
TI Nocturnal boundary layer characteristics and land breeze development in
Houston, Texas during TexAQS II
SO ATMOSPHERIC ENVIRONMENT
LA English
DT Article
DE TexAQS II; Tethersonde; Urban nocturnal boundary layer; Inversion
height; Land breeze
ID GREATER ATHENS AREA; MIXING HEIGHT; SEA-BREEZE; AIR-POLLUTION; URBAN;
DISTRIBUTIONS; CIRCULATION; SIMULATIONS; ENVIRONMENT; INVERSION
AB The nocturnal boundary layer in Houston, Texas was studied using a high temporal and vertical resolution tethersonde system on four nights during the Texas Air Quality Study II (TexAQS II) in August and September 2006. The launch site was on the University of Houston campus located approximately 4 km from downtown Houston. Of particular interest was the evolution of the nocturnal surface inversion and the wind flows within the boundary layer. The land-sea breeze oscillation in Houston has important implications for air quality as the cycle can impact ozone concentrations through pollutant advection and recirculation. The results showed that a weakly stable surface inversion averaging in depth between 145 and 200 m AGL formed on each of the experiment nights, typically within 2-3 h after sunset. Tethersonde vertical winds were compared with two other Houston data sets (High Resolution Doppler Lidar and radar wind profiler) from locations near the coastline and good agreement was found, albeit with a temporal lag at the tethersonde site. This comparison revealed development of a land breeze on three nights which began near the coastline and propagated inland both horizontally and vertically with time. The vertical temperature structure was significantly modified on one night at the tethersonde site after the land breeze wind shift, exhibiting near-adiabatic profiles below 100 m AGL. (C) 2009 Elsevier Ltd. All rights reserved.
C1 [Day, Bridget M.; Rappenglueck, Bernhard; Clements, Craig B.] Univ Houston, Dept Earth & Atmospher Sci, Houston, TX 77204 USA.
[Tucker, Sara C.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80305 USA.
[Tucker, Sara C.; Brewer, W. Alan] NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA.
RP Rappengluck, B (reprint author), Univ Houston, Dept Earth & Atmospher Sci, 4800 Calhoun Rd, Houston, TX 77204 USA.
EM brappenglueck@uh.edu
RI Brewer, Wm Alan/I-3920-2013
FU Texas Commission on Environmental Quality (TCEQ); Houston Advanced
Research Center
FX We are grateful for financial support from the Texas Commission on
Environmental Quality (TCEQ) and Houston Advanced Research Center. We
would like to thank Bryan Lambeth (TCEQ) and Wayne Angevine (Cooperative
Institute for Research in Environmental Sciences, University of Colorado
at Boulder and NOAA Earth System Research Laboratory) for providing the
La Porte wind profiler data set. Special thanks go to Ryan Perna, Leo
Pedemonte, Fong Ngan, Soontae Kim, HyunCheol Kim, and Xiangshang Li for
data collection and analysis assistance. Two anonymous reviewers also
provided valuable comments that improved this manuscript.
NR 30
TC 18
Z9 18
U1 4
U2 25
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 1352-2310
J9 ATMOS ENVIRON
JI Atmos. Environ.
PD OCT
PY 2010
VL 44
IS 33
SI SI
BP 4014
EP 4023
DI 10.1016/j.atmosenv.2009.01.031
PG 10
WC Environmental Sciences; Meteorology & Atmospheric Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA 663ER
UT WOS:000282866300003
ER
PT J
AU Wright, ME
Atkinson, DB
Ziemba, L
Griffin, R
Hiranuma, N
Brooks, S
Lefer, B
Flynn, J
Perna, R
Rappengluck, B
Luke, W
Kelley, P
AF Wright, Monica E.
Atkinson, Dean B.
Ziemba, Luke
Griffin, Robert
Hiranuma, Naruki
Brooks, Sarah
Lefer, Barry
Flynn, James
Perna, Ryan
Rappenglueck, Bernhard
Luke, Winston
Kelley, Paul
TI Extensive aerosol optical properties and aerosol mass related
measurements during TRAMP/TexAQS 2006-Implications for PM compliance and
planning
SO ATMOSPHERIC ENVIRONMENT
LA English
DT Article
DE Urban air quality; PM; Aerosol optical properties; AMS; Particle size
distribution
ID SPECTROMETER; PARTICLES
AB Extensive aerosol optical properties, particle size distributions, and Aerodyne quadrupole aerosol mass spectrometer measurements collected during TRAMP/TexAQS 2006 were examined in light of collocated meteorological and chemical measurements. Much of the evident variability in the observed aerosol-related air quality is due to changing synoptic meteorological situations that direct emissions from various sources to the TRAMP site near the center of the Houston-Galveston-Brazoria (HGB) metropolitan area. In this study, five distinct long-term periods have been identified. During each of these periods, observed aerosol properties have implications that are of interest to environmental quality management agencies. During three of the periods, long range transport (LRT), both intra-continental and intercontinental, appears to have played an important role in producing the observed aerosol. During late August 2006, southerly winds brought super-micron Saharan dust and sea salt to the HGB area, adding mass to fine particulate matter (PM(2.5)) measurements, but apparently not affecting secondary particle growth or gas-phase air pollution. A second type of LRT was associated with northerly winds in early September 2006 and with increased ozone and sub-micron particulate matter in the HGB area. Later in the study, LRT of emissions from wildfires appeared to increase the abundance of absorbing aerosols (and carbon monoxide and other chemical tracers) in the HGB area. However, the greatest impacts on Houston PM(2.5) air quality are caused by periods with low-wind-speed sea breeze circulation or winds that directly transport pollutants from major industrial areas, i.e., the Houston Ship Channel, into the city center. (C) 2009 Elsevier Ltd. All rights reserved.
C1 [Wright, Monica E.; Atkinson, Dean B.] Portland State Univ, Dept Chem, Portland, OR 97207 USA.
[Ziemba, Luke; Griffin, Robert] Univ New Hampshire, Climate Change Res Ctr, Durham, NH 03824 USA.
[Hiranuma, Naruki; Brooks, Sarah] Texas A&M Univ, Dept Atmospher Sci, College Stn, TX 77843 USA.
[Lefer, Barry; Flynn, James; Perna, Ryan; Rappenglueck, Bernhard] Univ Houston, Dept Earth & Atmospher Sci, Houston, TX 77004 USA.
[Luke, Winston; Kelley, Paul] NOAA, Air Resources Lab, Silver Spring, MD 20910 USA.
RP Atkinson, DB (reprint author), Portland State Univ, Dept Chem, Portland, OR 97207 USA.
EM AtkinsonD@pdx.edu
RI Brooks, Sarah/H-1176-2012; Hiranuma, Naruki/D-3780-2014; Luke,
Winston/D-1594-2016; Kelley, Paul/C-9155-2016;
OI Hiranuma, Naruki/0000-0001-7790-4807; Luke, Winston/0000-0002-1993-2241;
Lefer, Barry/0000-0001-9520-5495
FU Houston Advanced Research Center (HARC) [H78]; Texas Commission on
Environmental Quality (TCEQ) [582-5-64594]; National Atmospheric and
Oceanic Administration [NA05OAR4310108]
FX The authors would like to express their gratitude to the Houston
Advanced Research Center (HARC) for supporting and funding Projects H78.
In addition we would like to thank the Texas Commission on Environmental
Quality (TCEQ) for supporting and funding this research under grant
582-5-64594. DBA acknowledges support from the Atmospheric Composition
and Climate program at the National Atmospheric and Oceanic
Administration through award number NA05OAR4310108.
NR 26
TC 8
Z9 9
U1 0
U2 24
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 1352-2310
J9 ATMOS ENVIRON
JI Atmos. Environ.
PD OCT
PY 2010
VL 44
IS 33
SI SI
BP 4035
EP 4044
DI 10.1016/j.atmosenv.2008.12.055
PG 10
WC Environmental Sciences; Meteorology & Atmospheric Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA 663ER
UT WOS:000282866300005
ER
PT J
AU Brooks, S
Luke, W
Cohen, M
Kelly, P
Lefer, B
Rappengluck, B
AF Brooks, Steven
Luke, Winston
Cohen, Mark
Kelly, Paul
Lefer, Barry
Rappenglueck, Bernhard
TI Mercury species measured atop the Moody Tower TRAMP site, Houston, Texas
SO ATMOSPHERIC ENVIRONMENT
LA English
DT Article
DE Houston; TexAQS-II; Mercury; GEM; RGM; FPM
ID REACTIVE GASEOUS MERCURY; AMBIENT AIR; PARTICULATE MERCURY
AB Atmospheric mercury speciation was monitored within Houston, Texas, USA, August 6-October 14, 2006 as part of the TexAQS Radical and Aerosol Measurement Program (TRAMP). On average, all mercury levels were significantly elevated compared to a rural Gulf of Mexico coastal site. Concentrations varied from very clean to very dirty. Multi-day periods of stagnant or low-wind conditions brought elevated concentrations of all mercury species, whereas multi-day periods of strong winds, particularly southerly winds off the Gulf of Mexico, brought very low values of mercury species. Over the entire mercury measurement period, the daily averages of mercury species showed distinct and consistent relationships with the average planetary boundary layer dynamics, with gaseous elemental and particulate-bound mercury near-surface concentrations enhanced by a shallow nocturnal boundary layer, and reactive gaseous mercury concentration enhanced by midday convective boundary layer air entrainment transporting air aloft to the surface. Mercury concentrations were not significantly correlated with known products of combustion, likely indicating non-combustion mercury sources from the Houston area petrochemical complexes. On the morning of August 31, 2006 an observed emission event at a refinery complex on the Houston Ship Channel resulted in extremely high concentrations of aerosol mass and particulate-bound mercury at the TRAMP measurement site 20 km downwind. (C) 2009 Elsevier Ltd. All rights reserved.
C1 [Brooks, Steven; Luke, Winston; Cohen, Mark; Kelly, Paul] Natl Ocean & Atmospher Adm, Atmospher Turbulence & Diffus Div, Liaison Canaan Valley Inst, Oak Ridge, TN 37830 USA.
[Lefer, Barry; Rappenglueck, Bernhard] Univ Houston, Dept Earth & Atmospher Sci, Houston, TX USA.
RP Brooks, S (reprint author), Natl Ocean & Atmospher Adm, Atmospher Turbulence & Diffus Div, Liaison Canaan Valley Inst, 456 S Illinois Ave, Oak Ridge, TN 37830 USA.
EM steve.brooks@noaa.gov
RI Cohen, Mark/P-6936-2015; Luke, Winston/D-1594-2016;
OI Cohen, Mark/0000-0003-3183-2558; Luke, Winston/0000-0002-1993-2241;
Lefer, Barry/0000-0001-9520-5495
FU Houston Advanced Research Center (HARC) [H78]; Texas Commission on
Environmental Quality (TCEQ) [582-5-64594-FY07-02]
FX The authors would like to express their gratitude to the Houston
Advanced Research Center (HARC) for supporting and funding Project H78
and the Texas Commission on Environmental Quality (TCEQ) for supporting
and funding this research under grant 582-5-64594-FY07-02.
NR 19
TC 18
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U1 0
U2 12
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 1352-2310
J9 ATMOS ENVIRON
JI Atmos. Environ.
PD OCT
PY 2010
VL 44
IS 33
SI SI
BP 4045
EP 4055
DI 10.1016/j.atmosenv.2009.02.009
PG 11
WC Environmental Sciences; Meteorology & Atmospheric Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA 663ER
UT WOS:000282866300006
ER
PT J
AU Luke, WT
Kelley, P
Lefer, BL
Flynn, J
Rappengluck, B
Leuchner, M
Dibb, JE
Ziemba, LD
Anderson, CH
Buhr, M
AF Luke, Winston T.
Kelley, Paul
Lefer, Barry L.
Flynn, James
Rappenglueck, Bernhard
Leuchner, Michael
Dibb, Jack E.
Ziemba, Luke D.
Anderson, Casey H.
Buhr, Martin
TI Measurements of primary trace gases and NOy composition in Houston,
Texas
SO ATMOSPHERIC ENVIRONMENT
LA English
DT Article
DE NOy budget; Ozone photochemistry; Air quality; Sulfur dioxide; Carbon
monoxide; Houston; TEXAQS-II
ID CARBON-MONOXIDE; OZONE FORMATION; NITROUS-ACID; AIR-QUALITY;
TROPOSPHERE; EMISSIONS; ANALYZERS; COLORADO; DETECTOR; URBAN
AB Concentrations of CO, SO2, NO, NO2, and NOy were measured atop the University of Houston's Moody Tower supersite during the 2006 TexAQS-II Radical and Aerosol Measurement Project (TRAMP). The lowest concentrations of all primary and secondary species were observed in clean marine air in southerly flow. SO2 concentrations were usually low, but increased dramatically in sporadic midday plumes advected from sources in the Houston Ship Channel (HSC), located NE of the site. Concentrations of CO and NO displayed large diurnal variations in keeping with their co-emission by mobile sources in the Houston Metropolitan Area (HMA). CO/NOx emission ratios of 5.81 +/- 0.94 were observed in the morning rush hour. Nighttime concentrations of NOx (NOx = NO + NO2) and NOy (NOy = NO + NO2 + NO3 + HNO3 + HONO + 2*N2O5 + HO2NO2 + PANs + RONO2 + p-NO (3) over bar + ... ) were highest in winds from the NNW-NE due to emission from mobile sources. Median ratios of NOx/NOy were approximately 0.9 overnight, reflecting the persistence and/or generation of NOz (NOz = NOy - NOx) species in the nighttime Houston boundary layer, and approached unity in the morning rush hour. Daytime concentrations of NOx and NOy were highest in winds from the HSC. NO5/NOy ratios reached their minimum values (median ca 0.63) from 1300 to 1500 CST, near local solar noon, and air masses often retained enough NOx to sustain additional O-3 formation farther downwind. HNO3 and PANs comprised the dominant NO2 species in the HMA, and on a median basis represented 17-20% and 12-15% of NOy, respectively, at midday. Concentrations of HNO3, PANs, and NOz, and fractional contributions of these species to NOy, were at a maximum in NE flow, reflecting the source strength and reactivity of precursor emissions in the HSC. As a result, daytime O-3 concentrations were highest in air masses with HSC influence. Overall, our findings confirm the impact of the HSC as a dominant source region within the HMA. A comparison of total NOy measurements with the sum of measured NOy species (NOyi = NOx + HNO3 + PANs + HONO + p-NO (3) over bar) yielded excellent overall agreement during both day ([NOy](ppb) = ([ NOyi](ppb)*1.03 +/- 0.16) - 0.42; r(2) = 0.9933) and night ([NOy](ppb) = (([NOyi](ppb)*1.01 +/- .16) + 0.18: r(2) = 0.9975). A similar comparison between NOy-NOx concentrations and the sum of NOzi (NOzi = HNO3 + PANs + HONO + p-NO (3) over bar) yielded good overall agreement during the day ([NOz](PPb) = (([NOzi](PPb)*1.01 +/- 0.30) + 0.044 ppb; r(2) = 0.8527) and at night (([NOz](ppb) = ([NOzi](ppb)*1.12 +/- 0.69) + 0.16 ppb; r(2) = 0.6899). Median ratios of NOz/NOzi; were near unity during daylight hours but increased to approximately 1.2 overnight, a difference of 0.15-0.50 ppb.
Differences between NO2 and NOzi rarely exceeded combined measurement uncertainties, and variations in NOz/NOzi ratios may have resulted solely from errors in conversion efficiencies of NOy species and changes in NOy comosition. However, nighttime NOz/NOzi ratios and the magnitude of NO2 - NOzi differences were generally consistent with recent observations of ClNO2 in the nocturnal Houston boundary layer. Published by Elsevier Ltd.
C1 [Luke, Winston T.; Kelley, Paul] Natl Ocean & Atmospher Adm, Air Resources Lab, Silver Spring, MD USA.
[Lefer, Barry L.; Flynn, James; Rappenglueck, Bernhard; Leuchner, Michael] Univ Houston, Dept Earth & Atmospher Sci, Houston, TX USA.
[Dibb, Jack E.; Ziemba, Luke D.; Anderson, Casey H.] Univ New Hampshire, Inst Study Earth Oceans & Space, Climate Change Res Ctr, Durham, NH 03824 USA.
[Buhr, Martin] Air Qual Design Inc, Golden, CO USA.
RP Luke, WT (reprint author), Natl Ocean & Atmospher Adm, Air Resources Lab, Silver Spring, MD USA.
EM Winston.Luke@noaa.gov
RI Luke, Winston/D-1594-2016; Kelley, Paul/C-9155-2016;
OI Luke, Winston/0000-0002-1993-2241; Leuchner,
Michael/0000-0002-0927-2622; Lefer, Barry/0000-0001-9520-5495
FU Houston Advanced Research Center (HARC); Texas Commission on
Environmental Quality (TCEQ)
FX The authors would like to express their gratitude to the Houston
Advanced Research Center (HARC) and the Texas Commission on
Environmental Quality (TCEQ) for supporting and funding this research.
We would also like to thank Dr. Jochen Stutz (UCLA) for providing us
with the DOAS data sets. Ms. Marcia Wood (NOAA/ARL) provided extensive
support for travel, logistical, and budget considerations. Mention of
commercial brands, manufacturer, or supplier does not imply or
constitute official endorsement by the National Oceanic and Atmospheric
Administration, Department of Commerce, or United States government.
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PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 1352-2310
J9 ATMOS ENVIRON
JI Atmos. Environ.
PD OCT
PY 2010
VL 44
IS 33
SI SI
BP 4068
EP 4080
DI 10.1016/j.atmosenv.2009.08.014
PG 13
WC Environmental Sciences; Meteorology & Atmospheric Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA 663ER
UT WOS:000282866300008
ER
PT J
AU Flynn, J
Lefer, B
Rappengluck, B
Leuchner, M
Perna, R
Dibb, J
Ziemba, L
Anderson, C
Stutz, J
Brune, W
Ren, XR
Mao, JQ
Luke, W
Olson, J
Chen, G
Crawford, J
AF Flynn, James
Lefer, Barry
Rappenglueck, Bernhard
Leuchner, Michael
Perna, Ryan
Dibb, Jack
Ziemba, Luke
Anderson, Casey
Stutz, Jochen
Brune, William
Ren, Xinrong
Mao, Jingqiu
Luke, Winston
Olson, Jennifer
Chen, Gao
Crawford, James
TI Impact of clouds and aerosols on ozone production in Southeast Texas
SO ATMOSPHERIC ENVIRONMENT
LA English
DT Article
DE TexAQS-II; TRAMP; Photolysis rates; Ozone production; Radiative transfer
model; Photochemical box model
ID PHOTOLYSIS RATE COEFFICIENT; MEXICO-CITY; PHOTOCHEMICAL SMOG;
RADIATIVE-TRANSFER; TRACE-P; RATES; NO2; SENSITIVITY; FREQUENCIES;
PROFILES
AB A radiative transfer model and photochemical box model are used to examine the effects of clouds and aerosols on actinic flux and photolysis rates, and the impacts of changes in photolysis rates on ozone production and destruction rates in a polluted urban environment like Houston, Texas. During the TexAQS-II Radical and Aerosol Measurement Project the combined cloud and aerosol effects reduced j(NO2) photolysis frequencies by nominally 17%, while aerosols reduced j(NO2) by 3% on six clear sky days. Reductions in actinic flux due to attenuation by clouds and aerosols correspond to reduced net ozone formation rates with a nearly one-to-one relationship. The overall reduction in the net ozone production rate due to reductions in photolysis rates by clouds and aerosols was approximately 8 ppbv h(-1). (C) 2009 Elsevier Ltd. All rights reserved,
C1 [Flynn, James; Lefer, Barry; Rappenglueck, Bernhard; Leuchner, Michael; Perna, Ryan] Univ Houston, Dept Earth & Atmospher Sci, Houston, TX 77204 USA.
[Dibb, Jack; Ziemba, Luke; Anderson, Casey] Univ New Hampshire, Dept Earth Sci, Durham, NH 03824 USA.
[Brune, William; Ren, Xinrong; Mao, Jingqiu] Penn State Univ, Dept Meteorol, University Pk, PA 16802 USA.
[Stutz, Jochen] Univ Calif Los Angeles, Dept Atmospher & Ocean Sci, Los Angeles, CA 90095 USA.
[Luke, Winston] NOAA, Air Resources Lab, Silver Spring, MD 20910 USA.
[Olson, Jennifer; Chen, Gao; Crawford, James] NASA, Chem & Dynam Branch, Langley Res Ctr, Hampton, VA 23681 USA.
RP Lefer, B (reprint author), Univ Houston, Dept Earth & Atmospher Sci, 4800 Calhoun Rd, Houston, TX 77204 USA.
EM blefer@uh.edu
RI Mao, Jingqiu/F-2511-2010; Crawford, James/L-6632-2013; Stutz,
Jochen/K-7159-2014; Luke, Winston/D-1594-2016; Ren, Xinrong/E-7838-2015;
OI Mao, Jingqiu/0000-0002-4774-9751; Lefer, Barry/0000-0001-9520-5495;
Crawford, James/0000-0002-6982-0934; Luke, Winston/0000-0002-1993-2241;
Ren, Xinrong/0000-0001-9974-1666; Leuchner, Michael/0000-0002-0927-2622
FU Houston Advanced Research Center; Texas Commission on Environmental
Quality
FX We would like to thank the Houston Advanced Research Center and the
Texas Commission on Environmental Quality for their financial support.
We would also like to thank the USDA-UVB monitoring program, Fong Ngan,
Daewon Byun, and Mark Estes for providing assistance in data analysis
and guidance.
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PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 1352-2310
J9 ATMOS ENVIRON
JI Atmos. Environ.
PD OCT
PY 2010
VL 44
IS 33
SI SI
BP 4126
EP 4133
DI 10.1016/j.atmosenv.2009.09.005
PG 8
WC Environmental Sciences; Meteorology & Atmospheric Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA 663ER
UT WOS:000282866300014
ER
PT J
AU Acharya, AP
Dolgova, NV
Moore, NM
Xia, CQ
Clare-Salzler, MJ
Becker, ML
Gallant, ND
Keselowsky, BG
AF Acharya, Abhinav P.
Dolgova, Natalia V.
Moore, Nicole M.
Xia, Chang-Qing
Clare-Salzler, Michael J.
Becker, Matthew L.
Gallant, Nathan D.
Keselowsky, Benjamin G.
TI The modulation of dendritic cell integrin binding and activation by
RGD-peptide density gradient substrates
SO BIOMATERIALS
LA English
DT Article
DE Dendritic cell; Cell adhesion; Biomimetic; RGD peptide; High-throughput;
Immune response
ID ADAPTIVE IMMUNE-RESPONSES; SELF-ASSEMBLED MONOLAYERS;
EXTRACELLULAR-MATRIX; SURFACE-CHEMISTRY; BIOMIMETIC MATERIALS;
MACROPHAGE BEHAVIOR; ADSORBED PROTEINS; IN-VITRO; T-CELLS; ADHESION
AB Dendritic cells (DCs) are central regulators of the immune system that operate in both innate and adaptive branches of immunity. Activation of DC by numerous factors, such as danger signals, has been well established. However, modulation of DC functions through adhesion-based cues has only begun to be characterized. In this work, DCs were cultured on surfaces presenting a uniform gradient of the integrin-targeting RGD peptide generated using the recently established "universal gradient substrate for click biofunctionalization" methodology. Surface expression of activation markers (costimulatory molecule CD86 and stimulatory molecule MHC-II) and production of cytokines IL-10 and IL-12p40 of adherent DCs was quantified in situ. Additionally, bound alpha(V) integrin was quantified in situ using a biochemical cross-linking/extraction method. Our findings demonstrate that DCs upregulated CD86, MHC-II, IL-10, IL-12p40 and alpha(V) integrin binding as a function of RGD surface density, with production of IL-12p40 being the marker most sensitive to RGD surface density. Surface expression of activation markers demonstrated moderate correlation with alpha(V) integrin binding, while cytokine production was highly correlated with alpha(V) integrin binding. This work demonstrates the utility of the surface density gradient platform as a high-throughput method to investigate RGD density-dependent DC adhesive responses. Furthermore, this quantitative analysis of DC integrin-based activation represents a first of its type, helping to establish the field of adhesion-based modulation of DCs as a general mechanism that has previously not been defined, and informs the rational design of biomimetic biomaterials for immunomodulation. Published by Elsevier Ltd.
C1 [Dolgova, Natalia V.; Keselowsky, Benjamin G.] Univ Florida, J Crayton Pruitt Family Dept Biomed Engn, Gainesville, FL 32611 USA.
[Moore, Nicole M.] Natl Inst Stand & Technol, Div Polymers, Gaithersburg, MD 20899 USA.
[Xia, Chang-Qing; Clare-Salzler, Michael J.] Univ Florida, Coll Med, Dept Pathol Immunol & Lab Med, Gainesville, FL 32611 USA.
[Becker, Matthew L.] Univ Akron, Dept Polymer Sci, Akron, OH 44325 USA.
[Gallant, Nathan D.] Univ S Florida, Dept Mech Engn, Tampa, FL 33620 USA.
RP Keselowsky, BG (reprint author), Univ Florida, J Crayton Pruitt Family Dept Biomed Engn, 130 BME POB 116131, Gainesville, FL 32611 USA.
EM bkeselowsky@bme.ufl.edu
RI Acharya, Abhinav/J-8384-2013;
OI Gallant, Nathan/0000-0001-6454-7660
FU Juvenile Diabetes Research Foundation; NRC/NIST; Innovation in
Measurement Science Award
FX The authors gratefully acknowledge funding from the Juvenile Diabetes
Research Foundation (BGK), an NRC/NIST postdoctoral fellowship (NMM) and
an Innovation in Measurement Science Award (MLB). Note: certain
equipment, instruments or materials are identified in this paper in
order to adequately specify the experimental details. Such
identification does not imply recommendation by the National Institute
of Standards and Technology nor does it imply the materials are
necessarily the best available for the purpose.
NR 70
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PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0142-9612
J9 BIOMATERIALS
JI Biomaterials
PD OCT
PY 2010
VL 31
IS 29
BP 7444
EP 7454
DI 10.1016/j.biomaterials.2010.06.025
PG 11
WC Engineering, Biomedical; Materials Science, Biomaterials
SC Engineering; Materials Science
GA 642DG
UT WOS:000281183200004
PM 20637504
ER
PT J
AU Kadison, E
D'Alessandro, EK
Davis, GO
Hood, PB
AF Kadison, Elizabeth
D'Alessandro, Evan K.
Davis, Gideon O.
Hood, Peter B.
TI AGE, GROWTH, AND REPRODUCTIVE PATTERNS OF THE GREAT BARRACUDA, SPHYRAENA
BARRACUDA, FROM THE FLORIDA KEYS
SO BULLETIN OF MARINE SCIENCE
LA English
DT Article
ID SEAGRASS BEDS; REEF FISHES; CORAL-REEF; MANGROVES; HABITATS; NURSERY
AB Age, growth, and reproductive aspects of the great barracuda, Sphyraena barracuda (Walbaum, 1792), were examined in 467 individuals ranging from 182 to 1348 mm fork length (FL), collected in the vicinity of the Florida Keys from 1996 through 1998. Marginal increment analysis of sectioned sagittal otoliths indicated that a single annulus is formed each year during winter-spring. Male ages ranged from 0.7 to 11.3 yrs old, and female from 0.7 to 18.4 yrs old. The combined-sex von Bertalanffy growth model was L(t) = 1236.4(1-exp[-0.26(t + 0.71)]), and indicated faster growth than previous estimates. Most males matured between 1 and 2 yrs of age (626-806 mm fork length, FL) and females between 2 and 4 yrs of age (710-985 mm FL). Based on gonad analyses and monthly length-frequency histograms of 510 juveniles collected in Florida Bay from 1994 to 1996, spawning and ingress of young-of-the-year into shallow nearshore habitats occurs from spring through fall. These data differ from previous studies, and should be considered in future stock analyses of S. barracuda.
C1 [D'Alessandro, Evan K.] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Div Marine Biol & Fisheries, Miami, FL 33149 USA.
[Kadison, Elizabeth] Fish & Wildlife Res Inst, Florida Fish & Wildlife Conservat Commiss, St Petersburg, FL 33701 USA.
[Davis, Gideon O.] Healthpoint Ltd, Ft Worth, TX 76107 USA.
[Hood, Peter B.] Natl Marine Fisheries Serv, SE Reg Off, St Petersburg, FL 33701 USA.
RP D'Alessandro, EK (reprint author), Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Div Marine Biol & Fisheries, 4600 Rickenbacker Causeway, Miami, FL 33149 USA.
EM edalessa@rsmas.miami.edu
FU Department of the Interior, U.S Fish and Wildlife Service [F-43]
FX We thank P. Barbera, Capt. L. Robinson, Capt. D. DeMaria, T. Dunmire,
and C. Humphrey for providing us with many of the adult barracuda used
in this study; B. Gibbs, L. Anderson and the rest of the staff at Keys
Marine Laboratory for their assistance; J. Colvocoressess, A. Acosta, R.
Bertleson, D. Merryman, C. Bartels and G. Delgado for their guidance and
assistance. J. Serafy, T. MacDonald, D. Adams, and M. Fitchett provided
comments that substantially improved an earlier version of this
manuscript. We also thank J. Quinn and J. Leiby for their valuable
editorial comments. This work was funded in part from the Department of
the Interior, U.S Fish and Wildlife Service, Federal Aid for Sportfish
Restoration, Project F-43, and by funds from the proceeds of the sale of
Florida recreational fishing licenses.
NR 24
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PU ROSENSTIEL SCH MAR ATMOS SCI
PI MIAMI
PA 4600 RICKENBACKER CAUSEWAY, MIAMI, FL 33149 USA
SN 0007-4977
J9 B MAR SCI
JI Bull. Mar. Sci.
PD OCT
PY 2010
VL 86
IS 4
BP 773
EP 784
DI 10.5343/bms.2009.1070
PG 12
WC Marine & Freshwater Biology; Oceanography
SC Marine & Freshwater Biology; Oceanography
GA 668PI
UT WOS:000283281600001
ER
PT J
AU Driggers, WB
Burgess, GH
Hamilton, AN
Hopkins, NM
Schobernd, CM
AF Driggers, William B., III
Burgess, George H.
Hamilton, Alonzo N., Jr.
Hopkins, Nicholas M.
Schobernd, Christina M.
TI SQUALIOLUS LATICAUDUS IN THE WESTERN NORTH ATLANTIC OCEAN:
DISTRIBUTIONAL AND LIFE HISTORY OBSERVATIONS
SO BULLETIN OF MARINE SCIENCE
LA English
DT Article
ID GULF-OF-MEXICO; 1ST RECORD; SHARK
AB The spined pygmy shark (Squaliolus laticaudus Smith and Radcliffe, 1912) is among the smallest known species of sharks and despite its wide distribution, fewer than 100 specimens have been reported globally. On 28 October 2007, 24 spined pygmy sharks, with total lengths ranging from 120 to 210 mm, were collected in a single deepwater trawl in the northern Gulf of Mexico. All specimens, with the exception of two females, were immature. Follicle conditions in the two mature females indicated that vitellogenesis and gestation are consecutive. The stomachs of six specimens contained single cephalopod or teleost prey. Our catch and examinations of museum accessed specimens confirm the questioned presence of spined pygmy sharks in the Gulf of Mexico and demonstrate that it is more widely distributed in the western North Atlantic Ocean than previously known.
C1 [Driggers, William B., III; Hamilton, Alonzo N., Jr.; Hopkins, Nicholas M.; Schobernd, Christina M.] Se Fisheries Sci Ctr, Natl Marine Fisheries Serv, Mississippi Labs, Pascagoula, MS 39567 USA.
[Burgess, George H.] Univ Florida, Florida Museum Nat Hist, Florida Program Shark Res, Gainesville, FL 32611 USA.
RP Driggers, WB (reprint author), Se Fisheries Sci Ctr, Natl Marine Fisheries Serv, Mississippi Labs, 3209 Frederic St, Pascagoula, MS 39567 USA.
EM william.driggers@noaa.gov
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PU ROSENSTIEL SCH MAR ATMOS SCI
PI MIAMI
PA 4600 RICKENBACKER CAUSEWAY, MIAMI, FL 33149 USA
SN 0007-4977
J9 B MAR SCI
JI Bull. Mar. Sci.
PD OCT
PY 2010
VL 86
IS 4
BP 831
EP 838
DI 10.5343/bms.2010.1009
PG 8
WC Marine & Freshwater Biology; Oceanography
SC Marine & Freshwater Biology; Oceanography
GA 668PI
UT WOS:000283281600005
ER
PT J
AU Shapiro, M
Shukla, J
Brunet, G
Nobre, C
Beland, M
Dole, R
Trenberth, K
Anthes, R
Asrar, G
Barrie, L
Bougeault, P
Brasseur, G
Burridge, D
Busalacchi, A
Caughey, J
Chen, DL
Church, J
Enomoto, T
Hoskins, B
Hov, O
Laing, A
Le Treut, H
Marotzke, J
McBean, G
Meehl, G
Miller, M
Mills, B
Mitchell, J
Moncrieff, M
Nakazawa, T
Olafsson, H
Palmer, T
Parsons, D
Rogers, D
Simmons, A
Troccoli, A
Toth, Z
Uccellini, L
Velden, C
Wallace, JM
AF Shapiro, Melvyn
Shukla, Jagadish
Brunet, Gilbert
Nobre, Carlos
Beland, Michel
Dole, Randall
Trenberth, Kevin
Anthes, Richard
Asrar, Ghassem
Barrie, Leonard
Bougeault, Philippe
Brasseur, Guy
Burridge, David
Busalacchi, Antonio
Caughey, Jim
Chen, Deliang
Church, John
Enomoto, Takeshi
Hoskins, Brian
Hov, Oystein
Laing, Arlene
Le Treut, Herve
Marotzke, Jochem
McBean, Gordon
Meehl, Gerald
Miller, Martin
Mills, Brian
Mitchell, John
Moncrieff, Mitchell
Nakazawa, Tetsuo
Olafsson, Haraldur
Palmer, Tim
Parsons, David
Rogers, David
Simmons, Adrian
Troccoli, Alberto
Toth, Zoltan
Uccellini, Louis
Velden, Christopher
Wallace, John M.
TI AN EARTH-SYSTEM PREDICTION INITIATIVE FOR THE TWENTY-FIRST CENTURY
SO BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY
LA English
DT Article
ID ALBEDO ENHANCEMENT; CLIMATE-CHANGE; SIMULATIONS; IMPACT; WORLD; MODEL
C1 [Shapiro, Melvyn; Trenberth, Kevin; Laing, Arlene; Meehl, Gerald; Moncrieff, Mitchell] Natl Ctr Atmospher Res, Boulder, CO 80307 USA.
[Shapiro, Melvyn] Univ Bergen, Inst Geophys, Bergen, Norway.
[Shukla, Jagadish] George Mason Univ, Fairfax, VA 22030 USA.
[Shukla, Jagadish] Inst Global Environm & Soc, Calverton, MD USA.
[Brunet, Gilbert; Beland, Michel] Environm Canada, Atmospher Sci & Technol Directorate, Montreal, PQ, Canada.
[Nobre, Carlos] Natl Inst Space Res, Ctr Earth Syst Sci, Sao Jose Dos Campos, Brazil.
[Dole, Randall; Toth, Zoltan] NOAA, Earth Syst Res Lab, Boulder, CO USA.
[Anthes, Richard] Univ Corp Atmospher Res, Boulder, CO USA.
[Asrar, Ghassem] World Meteorol Org, World Climate Res Programme, Geneva, Switzerland.
[Barrie, Leonard] World Meteorol Org, Atmospher Res & Environm Programme, Geneva, Switzerland.
[Brasseur, Guy] Climate Serv Ctr, Hamburg, Germany.
[Bougeault, Philippe] Meteo France, Toulouse, France.
[Burridge, David; Caughey, Jim] World Meteorol Org, World Weather Res Programme, THORPEX, Geneva, Switzerland.
[Busalacchi, Antonio] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20742 USA.
[Chen, Deliang] Univ Gothenburg, Dept Earth Sci, Gothenburg, Sweden.
[Chen, Deliang] Int Council Sci, Paris, France.
[Church, John] Bur Meteorol, Ctr Australian Weather & Climate Res, Hobart, Tas, Australia.
[Church, John] Commonwealth Sci & Ind Res Org, Hobart, Tas, Australia.
[Enomoto, Takeshi] Japan Agcy Marine Earth Sci & Technol, Earth Simulator Ctr, Yokohama, Kanagawa, Japan.
[Hoskins, Brian] Univ Reading, Dept Meteorol, Reading, Berks, England.
[Hoskins, Brian] Univ London Imperial Coll Sci Technol & Med, Grantham Inst, London, England.
[Hov, Oystein] Norwegian Meteorol Inst, Oslo, Norway.
[Le Treut, Herve] Meteorol Dynam Lab, Palaiseau, France.
[Marotzke, Jochem] Max Planck Inst Meteorol, Hamburg, Germany.
[McBean, Gordon] Univ Western Ontario, Inst Catastroph Loss Reduct, London, ON, Canada.
[Miller, Martin; Palmer, Tim; Simmons, Adrian] European Ctr Medium Range Weather Forecasts, Reading RG2 9AX, Berks, England.
[Mills, Brian] Environm Canada, Adaptat & Impacts Res Div, Waterloo, ON, Canada.
[Mitchell, John] Met Off, Exeter, Devon, England.
[Nakazawa, Tetsuo] Meteorol Res Inst, Tsukuba, Ibaraki 305, Japan.
[Olafsson, Haraldur] Univ Iceland, Reykjavik, Iceland.
[Olafsson, Haraldur] Univ Bergen, Bergen, Norway.
[Palmer, Tim] Univ Oxford, Oxford, England.
[Rogers, David] Hlth & Climate Fdn, Washington, DC USA.
[Troccoli, Alberto] Univ Reading, Environm Syst Sci Ctr, Reading, Berks, England.
[Uccellini, Louis] NOAA, NCEP Environm Modeling Ctr, Camp Springs, MD USA.
[Velden, Christopher] Univ Wisconsin, CIMSS, Madison, WI USA.
[Wallace, John M.] Univ Washington, Dept Meteorol, Seattle, WA 98195 USA.
RP Shapiro, M (reprint author), Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA.
EM mshapiro@ucar.edu
RI Troccoli, Alberto/A-1477-2012; Trenberth, Kevin/A-5683-2012; Church,
John/A-1541-2012; Chen, Deliang/A-5107-2013; nakazawa,
tetsuo/P-9063-2014; Toth, Zoltan/I-6624-2015;
OI Trenberth, Kevin/0000-0002-1445-1000; Church, John/0000-0002-7037-8194;
Chen, Deliang/0000-0003-0288-5618; Toth, Zoltan/0000-0002-9635-9194;
Enomoto, Takeshi/0000-0003-1946-1168; Palmer, Tim/0000-0002-7121-2196
FU National Science Foundation
FX NCAR is sponsored by the National Science Foundation
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PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0003-0007
J9 B AM METEOROL SOC
JI Bull. Amer. Meteorol. Soc.
PD OCT
PY 2010
VL 91
IS 10
BP 1377
EP 1388
DI 10.1175/2010BAMS2944.1
PG 12
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 680BK
UT WOS:000284206300004
ER
PT J
AU Brunet, G
Shapiro, M
Hoskins, B
Moncrieff, M
Dole, R
Kiladis, GN
Kirtman, B
Lorenc, A
Mills, B
Morss, R
Polavarapu, S
Rogers, D
Schaake, J
Shukla, J
AF Brunet, Gilbert
Shapiro, Melvyn
Hoskins, Brian
Moncrieff, Mitch
Dole, Randall
Kiladis, George N.
Kirtman, Ben
Lorenc, Andrew
Mills, Brian
Morss, Rebecca
Polavarapu, Saroja
Rogers, David
Schaake, John
Shukla, Jagadish
TI COLLABORATION OF THE WEATHER AND CLIMATE COMMUNITIES TO ADVANCE
SUBSEASONAL-TO-SEASONAL PREDICTION
SO BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY
LA English
DT Article
ID COUPLED EQUATORIAL WAVES; SOIL-MOISTURE; PART I; FORECASTS; MODEL;
ASSIMILATION
C1 [Brunet, Gilbert] Environm Canada, Meteorol Res Div, Dorval, PQ H9P 1J3, Canada.
[Moncrieff, Mitch; Morss, Rebecca] Univ Corp Atmospher Res, Natl Ctr Atmospher Res, Boulder, CO USA.
[Shapiro, Melvyn] Univ Bergen, Inst Geophys, Bergen, Norway.
[Hoskins, Brian] Univ London Imperial Coll Sci Technol & Med, Grantham Inst Climate Change, London, England.
[Hoskins, Brian] Univ Reading, Reading, Berks, England.
[Dole, Randall; Kiladis, George N.] NOAA, Earth Syst Res Lab, Boulder, CO USA.
[Kirtman, Ben] Ctr Ocean Land Atmosphere Studies, Calverton, MD USA.
[Kirtman, Ben] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Miami, FL 33149 USA.
[Lorenc, Andrew] Met Off, Exeter, Devon, England.
[Mills, Brian] Environm Canada, Adaptat & Impacts Res Div, Waterloo, ON, Canada.
[Polavarapu, Saroja] Environm Canada, Meteorol Res Div, Toronto, ON, Canada.
[Rogers, David] Hlth & Climate Fdn, Washington, DC USA.
[Schaake, John] NOAA, Natl Weather Serv, Off Hydrol Dev, Silver Spring, MD 20910 USA.
[Shukla, Jagadish] George Mason Univ, Fairfax, MD USA.
RP Brunet, G (reprint author), Environm Canada, Meteorol Res Div, 2121 Voie Serv Nord,Route Trans Canadienne, Dorval, PQ H9P 1J3, Canada.
EM gilbert.brunet@ec.gc.ca
NR 28
TC 49
Z9 51
U1 1
U2 19
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0003-0007
J9 B AM METEOROL SOC
JI Bull. Amer. Meteorol. Soc.
PD OCT
PY 2010
VL 91
IS 10
BP 1397
EP 1406
DI 10.1175/2010BAMS3013.1
PG 10
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 680BK
UT WOS:000284206300006
ER
PT J
AU MacFarlane, RB
AF MacFarlane, R. Bruce
TI Energy dynamics and growth of Chinook salmon (Oncorhynchus tshawytscha)
from the Central Valley of California during the estuarine phase and
first ocean year
SO CANADIAN JOURNAL OF FISHERIES AND AQUATIC SCIENCES
LA English
DT Article
ID JUVENILE PACIFIC SALMON; DIEL FEEDING CHRONOLOGY; COHO SALMON;
SOCKEYE-SALMON; CLIMATE-CHANGE; FRASER-RIVER; EL-NINO; BRITISH-COLUMBIA;
MARINE SURVIVAL; TEMPERATURE
AB The greatest rates of energy accumulation and growth in subyearling Chinook salmon (Oncorhynchus tshawytscha) occurred during the first month following ocean entry, supporting the importance of this critical period. Data from an 11-year study in the coastal ocean off California and the San Francisco Estuary revealed that juvenile salmon gained 3.2 kJ.day(-1) and 0.8 g.day(-1), representing 4.3%.day(-1) and 5.2% day(-1), respectively, relative to estuary exit values. Little gain in energy (0.28 kJ.day(-1)) or size (0.07 g.day(-1))occurred in the estuary, indicating that the nursery function typically ascribed to estuaries can be deferred to initial ocean residence. Calculated northern anchovies (Engraulis mordax) equivalents to meet energy gains were one anchovy per day in the estuary (8% body weight.day(-1)) and about three per day immediately following ocean entry (15% body weight.day(-1)). Energy content in the estuary was positively related to higher salinity and lower freshwater outflow, whereas in the ocean, cooler temperatures, lower sea level, and greater upwelling resulted in greater gains. These results suggest that greater freshwater flows, warmer sea temperatures, and reduced or delayed upwelling, all of which are indicated by some (but not all) climate models, will likely decrease growth of juvenile Chinook salmon, leading to reduced survival.
C1 SW Fisheries Sci Ctr, Natl Marine Fisheries Serv, Fisheries Ecol Div, Santa Cruz, CA 95060 USA.
RP MacFarlane, RB (reprint author), SW Fisheries Sci Ctr, Natl Marine Fisheries Serv, Fisheries Ecol Div, 110 Shaffer Rd, Santa Cruz, CA 95060 USA.
EM Bruce.MacFarlane@noaa.gov
NR 78
TC 28
Z9 28
U1 1
U2 27
PU CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS
PI OTTAWA
PA 1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA
SN 0706-652X
J9 CAN J FISH AQUAT SCI
JI Can. J. Fish. Aquat. Sci.
PD OCT
PY 2010
VL 67
IS 10
BP 1549
EP 1565
DI 10.1139/F10-080
PG 17
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 659TG
UT WOS:000282589200002
ER
PT J
AU Forrest, RE
McAllister, MK
Dorn, MW
Martell, SJD
Stanley, RD
AF Forrest, Robyn E.
McAllister, Murdoch K.
Dorn, Martin W.
Martell, Steven J. D.
Stanley, Richard D.
TI Hierarchical Bayesian estimation of recruitment parameters and reference
points for Pacific rockfishes (Sebastes spp.) under alternative
assumptions about the stock-recruit function
SO CANADIAN JOURNAL OF FISHERIES AND AQUATIC SCIENCES
LA English
DT Article
ID BIOLOGICAL REFERENCE POINTS; LIFE-HISTORY PARAMETERS; WEST-COAST
GROUNDFISH; FISHERIES MANAGEMENT; EXPLOITATION RATES; HARVEST RATES;
FISH STOCKS; METAANALYSIS; GROWTH; SELECTIVITY
AB Hierarchical Bayesian meta-analysis can be a useful method for improving estimation of key parameters for harvested fish populations. In hierarchical models, data from multiple populations are used simultaneously to obtain estimates of parameters for individual populations and characterize the variability among populations. Many populations of Pacific rockfishes (Sebastes spp.) have declined off the US West Coast since the 1980s, and there is also concern for their conservation in Canada. We develop a hierarchical Bayesian meta-analysis to improve estimates of stock-recruit parameters, characterize management-related parameters (e.g., optimal harvest rate), and address uncertainties in the structural form of the stock-recruit function for Pacific rockfishes. We estimate steepness and optimal harvest rates for 14 populations of Pacific rockfishes under alternative assumptions about the underlying stock-recruit function (Beverton-Holt and Ricker). We provide a posterior predictive distribution of steepness for rockfishes that can be used as a prior in future assessments for similar populations. We also evaluate whether F(40%) is an appropriate proxy for F(MSY) for Pacific rockfishes and show that uncertainty in the natural mortality rate can have a significant effect on management advice derived from meta-analyses of stock-recruit data.
C1 [Stanley, Richard D.] Fisheries & Oceans Canada, Pacific Biol Stn, Nanaimo, BC V9T 6N7, Canada.
[Forrest, Robyn E.; McAllister, Murdoch K.; Martell, Steven J. D.] Univ British Columbia, Fisheries Ctr, AERL, Vancouver, BC V6T 1Z4, Canada.
[Dorn, Martin W.] NOAA, Natl Marine Fisheries Serv, Alaska Fisheries Sci Ctr, Seattle, WA 98115 USA.
RP Forrest, RE (reprint author), Fisheries & Oceans Canada, Pacific Biol Stn, 3190 Hammond Bay Rd, Nanaimo, BC V9T 6N7, Canada.
EM Robyn.Forrest@dfo-mpo.gc.ca
FU Fisheries and Oceans Canada at the University of British Columbia
Fisheries Centre
FX This study was funded by a sole contract granted to R. F. from Fisheries
and Oceans Canada during R. F.'s term at the University of British
Columbia Fisheries Centre. Data were supplied by the US National Marine
Fisheries Service (Alaska Fisheries Science Center). We are very
grateful to Pamela Mace and one anonymous reviewer for detailed advice
that greatly improved the manuscript. Josh Korman, Paul Starr, Rowan
Haigh, and Andrew Edwards also provided helpful suggestions during the
development of this work.
NR 83
TC 20
Z9 20
U1 1
U2 12
PU CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS
PI OTTAWA
PA 1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA
SN 0706-652X
J9 CAN J FISH AQUAT SCI
JI Can. J. Fish. Aquat. Sci.
PD OCT
PY 2010
VL 67
IS 10
BP 1611
EP 1634
DI 10.1139/F10-077
PG 24
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 659TG
UT WOS:000282589200006
ER
PT J
AU Rooper, CN
Hoff, GR
De Robertis, A
AF Rooper, Christopher N.
Hoff, Gerald R.
De Robertis, Alex
TI Assessing habitat utilization and rockfish (Sebastes spp.) biomass on an
isolated rocky ridge using acoustics and stereo image analysis
SO CANADIAN JOURNAL OF FISHERIES AND AQUATIC SCIENCES
LA English
DT Article
ID PACIFIC-OCEAN PERCH; SITU TARGET STRENGTH; WIDOW ROCKFISH; HECETA BANK;
SEBASTOLOBUS-ALASCANUS; UNTRAWLABLE AREAS; TRAWL SURVEY; DEEP-REEF;
ABUNDANCE; OREGON
AB For those marine fish species with specific habitat preferences, a habitat-based assessment may provide an alternative to traditional surveys. We conducted a habitat-based acoustic and stereo image stock assessment survey for rockfishes (Sebastes spp.) on a rocky ridge habitat in the eastern Bering Sea. Video analysis suggested that juvenile and adult rockfishes were more abundant on the seafloor in the rocky ridge area than on the surrounding sandy flats. Over the ridges, the distribution of rockfishes was uniformly low in the water column during nighttime surveys and higher during daytime surveys. The opposite pattern was observed in the video on the seafloor between night (high density) and day (lower density), indicating that fish in the water column during the day moved to the seafloor at night. Mean biomass of adult rockfishes for the rocky ridges was 1.54 x 10(4) tonnes based on acoustic data. The biomass of juvenile fish was estimated to be 9.2 x 10(2) tonnes. Utilization of similar survey methodologies on a larger scale might improve assessment of rockfishes not only in Alaska, but also throughout their range where fishery-independent biomass estimates have been difficult to obtain.
C1 [Rooper, Christopher N.; Hoff, Gerald R.; De Robertis, Alex] Alaska Fisheries Sci Ctr, Natl Marine Fisheries Serv, Seattle, WA 98115 USA.
RP Rooper, CN (reprint author), Alaska Fisheries Sci Ctr, Natl Marine Fisheries Serv, 7600 Sand Point Way NE, Seattle, WA 98115 USA.
EM Chris.Rooper@noaa.gov
RI Bizzarro, Joseph/A-2988-2012
NR 50
TC 8
Z9 8
U1 1
U2 17
PU CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS
PI OTTAWA
PA 1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA
SN 0706-652X
J9 CAN J FISH AQUAT SCI
JI Can. J. Fish. Aquat. Sci.
PD OCT
PY 2010
VL 67
IS 10
BP 1658
EP 1670
DI 10.1139/F10-088
PG 13
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 659TG
UT WOS:000282589200009
ER
PT J
AU Burla, M
Baptista, AM
Casillas, E
Williams, JG
Marsh, DM
AF Burla, Michela
Baptista, Antonio M.
Casillas, Edmundo
Williams, John G.
Marsh, Douglas M.
TI The influence of the Columbia River plume on the survival of steelhead
(Oncorhynchus mykiss) and Chinook salmon (Oncorhynchus tshawytscha): a
numerical exploration
SO CANADIAN JOURNAL OF FISHERIES AND AQUATIC SCIENCES
LA English
DT Article
ID 3D BAROCLINIC CIRCULATION; CROSS-SCALE MODEL; PACIFIC-SALMON; JUVENILE
SALMON; SHELF SYSTEMS; EL-NINO; OSCILLATION; DISCHARGE; KISUTCH; SUMMER
AB Are smolt-to-adult return rates (SARs) for wild steelhead (i.e., sea-run rainbow trout, Oncorhynchus mykiss) and wild Snake River spring-summer Chinook salmon (Oncorhynchus tshawytscha) related to changes in the Columbia River plume at the time that juvenile migrants enter the ocean? We used three-dimensional (3D) numerical models of the baroclinic circulation in the Columbia River estuary-plume-shelf system to simulate within-season variation in plume size and location, comparing the results with SARs for each day that juvenile salmon entered the ocean for 1999-2003. We found that steelhead benefited from the plume environment at a narrow window of time around their ocean entry. However, when large-scale ocean conditions turned unfavorable, the contribution of local plume conditions to the overall variability in steelhead survival became not significant. A similar evaluation revealed that the plume did not affect survival of Chinook salmon, at least at the fine scale of variability considered. The differential response between the two species is consistent with observed and previously reported behavioral characteristics they exhibit. We speculate that steelhead mainly use the plume to move quickly away from coastal habitats and the predation pressures associated with this environment, for a more direct migration than Chinook salmon to ocean habitats in the Gulf of Alaska.
C1 [Burla, Michela; Baptista, Antonio M.] Oregon Hlth & Sci Univ, Natl Sci Fdn NSF Sci & Technol Ctr Coastal Margin, Beaverton, OR 97006 USA.
[Casillas, Edmundo; Williams, John G.; Marsh, Douglas M.] NOAA Fisheries, NW Fisheries Sci Ctr, Seattle, WA 98112 USA.
RP Burla, M (reprint author), Oregon Hlth & Sci Univ, Natl Sci Fdn NSF Sci & Technol Ctr Coastal Margin, 20000 NW Walker Rd, Beaverton, OR 97006 USA.
EM burla@stccmop.org
OI Baptista, Antonio/0000-0002-7641-5937
FU National Oceanic and Atmospheric Administration [AB133F-04-CN-0033];
National Science Foundation [ACI-0121475, OCE-0424602]
FX Funding for this research was provided in part by the National Oceanic
and Atmospheric Administration (AB133F-04-CN-0033) and the National
Science Foundation (ACI-0121475; OCE-0424602). The study relied on
results of the CORIE modeling system. Within the CORIE team, thanks are
due to Yinglong Zhang, Charles Seaton, and Paul Turner for the
generation of the circulation databases and related information
products. Charles Seaton also drew the map of the study area. We thank
Mark D. Scheuerell and two anonymous reviewers for their useful
comments. We also thank Barbara Hickey (University of Washington) for
the cruise data used in Fig. 2b to assess model simulations. We are
finally grateful to Sandra Oster for editorial advice in the preparation
of the manuscript. Any statements, opinions, findings, conclusions, or
recommendations expressed in this material are those of the authors and
do not necessarily reflect the views or policies of the federal
sponsors, and no official endorsement should be inferred.
NR 37
TC 14
Z9 14
U1 1
U2 12
PU CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS
PI OTTAWA
PA 1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA
SN 0706-652X
EI 1205-7533
J9 CAN J FISH AQUAT SCI
JI Can. J. Fish. Aquat. Sci.
PD OCT
PY 2010
VL 67
IS 10
BP 1671
EP 1684
DI 10.1139/F10-083
PG 14
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA 659TG
UT WOS:000282589200010
ER
PT J
AU Tun, Z
Noel, JJ
Bohdanowicz, T
Cao, LR
Downing, RG
Goncharova, LV
AF Tun, Z.
Noel, J. J.
Bohdanowicz, Th.
Cao, L. R.
Downing, R. G.
Goncharova, L. V.
TI Cold-neutron depth profiling as a research tool for the study of surface
oxides on metals
SO CANADIAN JOURNAL OF PHYSICS
LA English
DT Article
AB A recent experiment at NIST has demonstrated that neutron depth profiling (NDP) based on the (n, alpha) reaction could be developed into a tool that could be routinely used for the study of passive oxides on metals. Whereas most metals are not (n, alpha) active, oxides grown with (17)O, the only (n, alpha) active oxygen isotope, can be observed and tracked by this technique. Problems due to contamination of the samples by boron were encountered, but were shown to be surmountable. For our samples, the NDP facility at NIST, as it exists today, has enough flux and energy resolution to separate the alpha particles emitted by (17)O from those emitted by (10)B. Substantial improvement in the data collection rate, easily achievable with arrays of additional detectors, will make NDP a useful tool in the study of passive oxides.
C1 [Tun, Z.; Bohdanowicz, Th.] Natl Res Council Canada, Canadian Neutron Beam Ctr, Chalk River, ON K0J 1J0, Canada.
[Noel, J. J.] Univ Western Ontario, Dept Chem, London, ON N6A 5B7, Canada.
[Bohdanowicz, Th.] Univ Waterloo, Nanotechnol Engn Undergrad Program, Waterloo, ON N2L 3G1, Canada.
[Cao, L. R.; Downing, R. G.] NIST, Inorgan Chem Metrol Grp, Div Analyt Chem, Gaithersburg, MD 20899 USA.
[Cao, L. R.] Ohio State Univ, Dept Mech Engn, Scott Lab, Columbus, OH 43210 USA.
[Goncharova, L. V.] Univ Western Ontario, Dept Phys & Astron, London, ON N6A 3K7, Canada.
RP Tun, Z (reprint author), Natl Res Council Canada, Canadian Neutron Beam Ctr, Chalk River, ON K0J 1J0, Canada.
EM zin.tun@nrc-cnrc.gc.ca
RI Cao, Lei/B-3254-2012
OI Cao, Lei/0000-0003-4018-9496
NR 6
TC 5
Z9 8
U1 2
U2 12
PU CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS
PI OTTAWA
PA 1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA
SN 0008-4204
J9 CAN J PHYS
JI Can. J. Phys.
PD OCT
PY 2010
VL 88
IS 10
BP 751
EP 758
DI 10.1139/P10-062
PG 8
WC Physics, Multidisciplinary
SC Physics
GA 676OQ
UT WOS:000283922200008
ER
PT J
AU Cao, CY
Uprety, S
Xiong, J
Wu, AS
Jing, P
Smith, D
Chander, G
Fox, N
Ungar, S
AF Cao, Changyong
Uprety, Sirish
Xiong, Jack
Wu, Aisheng
Jing, Ping
Smith, David
Chander, Gyanesh
Fox, Nigel
Ungar, Stephen
TI Establishing the Antarctic Dome C community reference standard site
towards consistent measurements from Earth observation satellites
SO CANADIAN JOURNAL OF REMOTE SENSING
LA English
DT Article
AB Establishing satellite measurement consistency by using common desert sites has become increasingly more important not only for climate change detection but also for quantitative retrievals of geophysical variables in satellite applications. Using the Antarctic Dome C site (75 degrees 06'S, 123 degrees 21'E, elevation 3.2 km) for satellite radiometric calibration and validation (Cal/Val) is of great interest owing to its unique location and characteristics. The site surface is covered with uniformly distributed permanent snow, and the atmospheric effect is small and relatively constant. In this study, the long-term stability and spectral characteristics of this site are evaluated using well-calibrated satellite instruments such as the Moderate Resolution Imaging Spectroradiometer (MODIS) and Sea-viewing Wide Field-of-view Sensor (SeaWiFS). Preliminary results show that despite a few limitations, the site in general is stable in the long term, the bidirectional reflectance distribution function (BRDF) model works well, and the site is most suitable for the Cal/Val of reflective solar bands in the 0.4-1.0 mu m range. It was found that for the past decade, the reflectivity change of the site is within 1.35% at 0.64 mu m, and interannual variability is within 2%. The site is able to resolve calibration biases between instruments at a level of similar to 1%. The usefulness of the site is demonstrated by comparing observations from seven satellite instruments involving four space agencies, including OrbView-2-SeaWiFS, Terra-Aqua MODIS, Earth Observing 1 (EO-1) - Hyperion, Meteorological Operational satellite programme (MetOp) - Advanced Very High Resolution Radiometer (AVHRR), Envisat Medium Resolution Imaging Spectrometer (MERIS) - dvanced Along-Track Scanning Radiometer (AATSR), and Landsat 7 Enhanced Thematic Mapper Plus (ETM+). Dome C is a promising candidate site for climate quality calibration of satellite radiometers towards more consistent satellite measurements, as part of the framework for climate change detection and data quality assurance for the Global Earth Observation System of Systems (GEOSS).
C1 [Cao, Changyong] NOAA, Ctr Satellite Applicat & Res STAR, NESDIS, Camp Springs, MD 20746 USA.
[Uprety, Sirish] Perot Syst Govt Serv Inc PSGS, Fairfax, VA 22031 USA.
[Xiong, Jack; Ungar, Stephen] NASA, Goddard Space Flight Ctr, Greenbelt, MD 21771 USA.
[Wu, Aisheng] Sigma Space Corp, Lanham, MD USA.
[Jing, Ping] IM Syst Grp Inc IMSG, Rockville, MD 20852 USA.
[Smith, David] Rutherford Appleton Lab, Sci & Technol Facil Council, Didcot OX11 0QX, Oxon, England.
[Chander, Gyanesh] US Geol Survey, SGT Inc, Earth Resources Observat & Sci EROS Ctr, Sioux Falls, SD 57198 USA.
[Fox, Nigel] Natl Phys Lab, Teddington TW11 0LW, Middx, England.
RP Cao, CY (reprint author), NOAA, Ctr Satellite Applicat & Res STAR, NESDIS, Camp Springs, MD 20746 USA.
EM changyong.cao@noaa.gov
RI Cao, Changyong/F-5578-2010
FU CEOS-WGCV Dome C project; NOAA NESDIS Center for Satellite Applications
and Research; NPOESS Preparatory Project (NPP) Integrated Program Office
(IPO)
FX This study is part of the CEOS-WGCV Dome C project during 2008-2009 in
support of the CEOS Strategic Implementation Team (SIT) actions and the
World Meteorological Organization - Global Space-based Inter-Calibration
System (WMO-GSICS). The study was partially funded by the NOAA NESDIS
Center for Satellite Applications and Research, the NPOESS Preparatory
Project (NPP) Integrated Program Office (IPO) - Joint Polar Satellite
System (JPSS) Cal/Val program, and the respective space agencies
involved. The authors would like to thank Istvan Laszlo, Pubu Ciren, and
Lawrence Flynn for fruitful discussions on the atmospheric effects at
Dome C. We thank Pascal Lecomte, Philippe Goryl, and Marie-Claire
Greening of ESA; Bruce Guenther, Heather Kilcoyne, and Ray Godin of the
IPO; Greg Stenssas of USGS; Patrice Henry of CNES; Steve Mackin of DMC
International Imaging (DMCII); Stephen Hudson of the University of
Washington; Petya Campbell and Lawrence Ong of GSFC; and all
participating CEOS-WGCV members for their facilitation and contributions
to this study. We also thank Fangfang Yu, Frank Padula, Xiangqian Wu,
and Bob Iacovazzi, and the anonymous reviewers for reviewing the
manuscript and providing valuable comments and suggestions. The
manuscript contents are solely the opinions of the authors and do not
constitute a statement of policy, decision, or position on behalf of
NOAA or the US government.
NR 34
TC 27
Z9 28
U1 1
U2 5
PU CANADIAN AERONAUTICS SPACE INST
PI KANATA
PA 350 TERRY FOX DR, STE 104, KANATA, ON K2K 2W5, CANADA
SN 1712-7971
J9 CAN J REMOTE SENS
JI Can. J. Remote Sens.
PD OCT
PY 2010
VL 36
IS 5
SI SI
BP 498
EP 513
PG 16
WC Remote Sensing
SC Remote Sensing
GA V23QE
UT WOS:000208356500007
ER
PT J
AU Yu, FF
Wu, XQ
AF Yu, Fangfang
Wu, Xiangqian
TI Water vapor correction to improve the operational calibration for NOAA
AVHRR/3 channel 2 (0.85 mu m) over a desert target
SO CANADIAN JOURNAL OF REMOTE SENSING
LA English
DT Article
AB The Advanced Very High Resolution Radiometers (AVHRRs) flown on the National Oceanic and Atmospheric Administration (NOAA) and the European Organisation for the Exploitation of Meteorological Satellites (EUMETSAT) polar satellites have been providing invaluable data for Earth system science and global change studies. However, the use of AVHRR solar reflectance products (e.g., normalized difference vegetation index (NDVI)) is constrained by calibration uncertainty, largely owing to the lack of an on-orbit calibration device for solar reflectance channels. Since the mid-1990s, NOAA has been applying operational calibration to these channels using the time series of top-of-atmosphere (TOA) measurements of the Libyan Desert site. However, the assumed radiometric stability of Libyan Desert TOA measurements can be disrupted by short-term variations in atmospheric components, especially for AVHRR channel 2, which has a spectral response function covering water vapor absorption lines in the near-infrared (NIR) spectra. This study aims to improve the calibration accuracy of AVHRR channel 2 data by applying water vapor correction over the homogeneous desert target surface using the water vapor content (W) derived from the linear relationships between the AVHRR split-window temperature difference (Delta T) and the Moderate Resolution Imaging Spectroradiometer (MODIS) NIR water vapor product. Results show that the linear Delta T-W relationship is affected by the temperature lapse rate at the satellite over-passing time and the spectral response functions of AVHRR split-window channels. Water vapor correction reduces the calibration uncertainty from 2.6%-3.5% to 1.7%-1.8%, and about 1.0% surface-based relative calibration accuracy is independent of the water vapor uncertainty introduced by the Delta T-Wregression. Furthermore, the short-term variations in the channel 2 operational degradation rate are largely reduced after water vapor correction. Thus, implementing water vapor correction can improve the operational calibration accuracy for AVHRR channel 2.
C1 [Yu, Fangfang] Earth Resources Technol Inc ERT, Laurel, MD 20707 USA.
[Wu, Xiangqian] NOAA, Ctr Satellite Applicat & Res STAR, NESDIS, Camp Springs, MD 20746 USA.
RP Yu, FF (reprint author), Earth Resources Technol Inc ERT, 6100 Frost Pl, Laurel, MD 20707 USA.
EM Fangfang.Yu@noaa.gov
RI Yu, Fangfang/E-7942-2011; Wu, Xiangqian/F-5634-2010
OI Yu, Fangfang/0000-0001-8343-0863; Wu, Xiangqian/0000-0002-7804-5650
FU NOAA-NESDIS - Office of Systems Development (OSD)
FX This work is funded by the Product Systems Development and
Implementation (PSDI) program of the NOAA-NESDIS - Office of Systems
Development (OSD). We would like to thank M. K. Rama Varama Raja, Pubu
Ciren, Chenyang Xiao, Frank Padula, and Michael Grotenhuis for their
review comments on this paper. We also appreciate the help from Quanhua
Liu on the discussion of aerosol distribution on the water vapor
absorption in the shortwave spectra. The manuscript contents are solely
the opinions of the authors and do not constitute a statement of policy,
decision, or position on behalf of NOAA or the US government.
NR 39
TC 6
Z9 6
U1 0
U2 3
PU CANADIAN AERONAUTICS SPACE INST
PI KANATA
PA 350 TERRY FOX DR, STE 104, KANATA, ON K2K 2W5, CANADA
SN 1712-7971
J9 CAN J REMOTE SENS
JI Can. J. Remote Sens.
PD OCT
PY 2010
VL 36
IS 5
SI SI
BP 514
EP 526
DI 10.5589/m10-077
PG 13
WC Remote Sensing
SC Remote Sensing
GA V23QE
UT WOS:000208356500008
ER
PT J
AU Wu, XQ
Sullivan, JT
Heidinger, AK
AF Wu, Xiangqian
Sullivan, Jerry T.
Heidinger, Andrew K.
TI Operational calibration of the Advanced Very High Resolution Radiometer
(AVHRR) visible and near-infrared channels
SO CANADIAN JOURNAL OF REMOTE SENSING
LA English
DT Article
AB The Advanced Very High Resolution Radiometer (AVHRR) visible and near-infrared channels must be calibrated after launch to maintain the accuracy of data derived from these channels for quantitative utilizations. The postlaunch calibration of these channels can only be carried out vicariously. The National Oceanic and Atmospheric Administration (NOAA) - National Environmental Satellite, Data, an Information Service (NESDIS) has been using the Libyan Desert as reference for operational calibration of AVHRR visible and near-infrared channels since 1995. A previous algorithm was successful correcting for the long-term instrument degradation in recalibration but had difficulty updating instrument calibration in near-real-time operation. This paper describes the operational calibration algorithm implemented since 2003, which overcomes the existing shortcomings by reducing target contamination and accounting for the effects of target bidirectional reflectance distribution function. Application of the algorithm shortens the latency of postlaunch calibration from 3 to 4 years for NOAA-14 and NOAA-16 to less than 2 years for NOAA-17 and to a few months for later satellites. Compared with the previous algorithm, the current algorithm enhances the calibration precision from 1.7% to 0.9% for channel 1.
C1 [Wu, Xiangqian] NOAA, Sensor Phys Branch, Satellite Meteorol & Climatol Div, Ctr Satellite Applicat & Res STAR,NESDIS, Camp Springs, MD 20746 USA.
[Heidinger, Andrew K.] NOAA, Adv Satellite Prod Team, Ctr Satellite Applicat & Res STAR, NESDIS, Madison, WI 53706 USA.
RP Wu, XQ (reprint author), NOAA, Sensor Phys Branch, Satellite Meteorol & Climatol Div, Ctr Satellite Applicat & Res STAR,NESDIS, 5200 Auth Rd, Camp Springs, MD 20746 USA.
EM Xiangqian.Wu@noaa.gov
RI Heidinger, Andrew/F-5591-2010; Wu, Xiangqian/F-5634-2010
OI Heidinger, Andrew/0000-0001-7631-109X; Wu, Xiangqian/0000-0002-7804-5650
FU NOAA-NESDIS
FX NOAA's AVHRR operational calibration was developed from the early work
of C.R.N. Rao and associates, with contributions from N. Zhang, F. Sun,
and F. Yu. The authors are grateful for the funding support from
NOAA-NESDIS Product System Development and Implementation (PSDI)
program, the moral support from M. Weinreb, and the helpful discussions
with R. Galvin and J. Bobilya of ITT Industries. The contents of this
paper are solely the opinions of the authors and do not constitute a
statement of policy, decision, or position on behalf of NOAA or the US
Government.
NR 41
TC 36
Z9 36
U1 1
U2 6
PU CANADIAN AERONAUTICS SPACE INST
PI KANATA
PA 350 TERRY FOX DR, STE 104, KANATA, ON K2K 2W5, CANADA
SN 1712-7971
J9 CAN J REMOTE SENS
JI Can. J. Remote Sens.
PD OCT
PY 2010
VL 36
IS 5
SI SI
BP 602
EP 616
PG 15
WC Remote Sensing
SC Remote Sensing
GA V23QE
UT WOS:000208356500014
ER
PT J
AU Wetherald, RT
AF Wetherald, Richard T.
TI Changes of time mean state and variability of hydrology in response to a
doubling and quadrupling of CO2
SO CLIMATIC CHANGE
LA English
DT Article
ID GENERAL-CIRCULATION MODELS; ATMOSPHERIC CARBON-DIOXIDE; COUPLED CLIMATE
MODELS; LARGE-SCALE MODELS; WATER AVAILABILITY; SUMMER DRYNESS; PART I;
INCREASE; PRECIPITATION; SENSITIVITY
AB This paper examines the subject of hydrologic variability and its changes in two separate integrations of a coupled ocean-atmosphere general circulation model developed at the Geophysical Fluid Dynamics Laboratory/NOAA assuming a 1% per year increase to a doubling and quadrupling of CO2, respectively. Changes in time mean state and variability of precipitation, runoff and soil moisture are evaluated using monthly and seasonal mean data derived from these integrations. Various statistical tests are then performed on the resulting time mean and variability changes. The patterns of hydrologic change for these three quantities are similar to those obtained from previous studies. In northern middle to higher latitudes for the time means, the changes include increases in monthly mean precipitation, increases in monthly mean runoff during the fall, winter and spring seasons and decreases of monthly mean soil moisture during summer. Many of these changes are found to be statistically significant at the 5% significance level for both the time mean and variability especially for the results where CO2 is quadrupled such as monthly mean precipitation. Significant changes also include increases of runoff variability during spring, winter and spring and increases of soil moisture variability during the summer season. These results support statements made in previous IPCC reports that increasing greenhouse gases can lead to more severe and frequent floods and droughts depending upon season and latitude. This study also indicates that the approaches to equilibrium of these two integrations, and the resulting hydrologic changes, take place over time scales of hundreds of years in agreement with several previous investigations.
C1 NOAA, GFDL, Princeton, NJ 08542 USA.
RP Wetherald, RT (reprint author), NOAA, GFDL, Princeton, NJ 08542 USA.
EM Dick.Wetherald@noaa.gov
NR 42
TC 8
Z9 8
U1 0
U2 4
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0165-0009
J9 CLIMATIC CHANGE
JI Clim. Change
PD OCT
PY 2010
VL 102
IS 3-4
BP 651
EP 670
DI 10.1007/s10584-009-9701-4
PG 20
WC Environmental Sciences; Meteorology & Atmospheric Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA 653WU
UT WOS:000282129400014
ER
PT J
AU Radenac, MH
Plimpton, PE
Lebourges-Dhaussy, A
Commien, L
McPhaden, MJ
AF Radenac, Marie-Helene
Plimpton, Patricia E.
Lebourges-Dhaussy, Anne
Commien, Ludivine
McPhaden, Michael J.
TI Impact of environmental forcing on the acoustic backscattering strength
in the equatorial Pacific: Diurnal, lunar, intraseasonal, and
interannual variability
SO DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
LA English
DT Article
DE Biological-physical interactions; Equatorial Pacific; Sound scattering;
Micronekton; ADCP moorings
ID WESTERN TROPICAL PACIFIC; DOPPLER CURRENT PROFILER; MID-ATLANTIC BIGHT;
1997-1998 EL-NINO; VERTICAL MIGRATION; ZOOPLANKTON BIOMASS; TIME-SERIES;
MEGANYCTIPHANES-NORVEGICA; TAXONOMIC COMPOSITION; PHYTOPLANKTON BLOOMS
AB We analyzed several records of mean volume backscattering strength (S(v)) derived from 150 kHz acoustic doppler current profilers (ADCPs) moored along the equator in upwelling mesotrophic conditions and in the warm pool oligotrophic ecosystem of the Pacific Ocean. The ADCPs allow for gathering long time-series of non-intrusive information about zooplankton and micronekton at the same spatial and temporal scales as physical observations. High S(v) are found from the surface to the middle of the thermocline between dusk and dawn in the mesotrophic regime. Biological and physical influences modified this classical diel cycle. In oligotrophic conditions observed at 170 degrees W and 140 degrees W during El Nino years, a subsurface S(v) maximum characterized nighttime S(v) profiles. Variations of the thermocline depth correlated with variations of the base of the high S(v) layer and the subsurface maximum closely tracked the thermocline depth from intraseasonal to interannual time-scales. A recurring deepening (20-60 m) of the high S(v) layer was observed at a frequency close to the lunar cycle frequency. At 165 degrees E, high day-to-day variations prevailed and our results suggest the influence of moderately mesotrophic waters that would be advected from the western warm pool during westerly wind events. A review of the literature suggests that S(v) variations may result from changes in biomass and species assemblages among which myctophids and euphausiids would be the most likely scatterers. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Radenac, Marie-Helene; Commien, Ludivine] Univ Toulouse 3, Lab Etudes Geophys & Oceanog Spatiales, F-31400 Toulouse, France.
[Plimpton, Patricia E.; McPhaden, Michael J.] NOAA, Pacific Marine Environm Lab, Seattle, WA 98115 USA.
[Lebourges-Dhaussy, Anne] Inst Rech Dev Bretagne, Plouzane, France.
[Radenac, Marie-Helene] Inst Rech Dev, Toulouse, France.
RP Radenac, MH (reprint author), Univ Toulouse 3, Lab Etudes Geophys & Oceanog Spatiales, 14 Av, F-31400 Toulouse, France.
EM marie-helene.radenac@legos.obs-mip.fr
RI McPhaden, Michael/D-9799-2016
FU CNES; NOAA's Climate Program Office
FX We thank Robert Le Borgne for fruitful discussions at different stages
of this study. We also thank reviewers for their incisive and useful
comments that greatly helped to improve this paper. We thank the CNES
for the financial support. PEP and MJM were funded by NOAA's Climate
Program Office. PMEL publication No. 3163.
NR 82
TC 9
Z9 9
U1 0
U2 8
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0967-0637
J9 DEEP-SEA RES PT I
JI Deep-Sea Res. Part I-Oceanogr. Res. Pap.
PD OCT
PY 2010
VL 57
IS 10
BP 1314
EP 1328
DI 10.1016/j.dsr.2010.06.004
PG 15
WC Oceanography
SC Oceanography
GA 667PR
UT WOS:000283206600014
ER
PT J
AU Sheu, WJ
Wu, CR
Oey, LY
AF Sheu, Woei-Jen
Wu, Chau-Ron
Oey, Lie-Yauw
TI Blocking and Westward Passage of Eddies in the Luzon Strait
SO DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
LA English
DT Article
DE Luzon Strait; Kuroshio intrusion; Jet-Eddy interaction
ID SOUTH CHINA SEA; WESTERN BOUNDARY CURRENT; MESOSCALE EDDIES; ZONAL JET;
MODEL; EDDY; PACIFIC; VARIABILITY; TRANSPORT; INTRUSION
AB Satellite observations have shown the abundance of generally westward-propagating eddies in the subtropical regions in the North Pacific Ocean, especially north of 10 degrees N. Eddies transport mass, and can significantly impact the circulation as well as the heat, salt and nutrient balances of the western Pacific marginal seas. This paper uses a numerical model to examine the conditions when eddies can or cannot freely propagate westward through the Luzon Strait into the South China Sea (SCS). Composite analyses on the 10-year model data show that the fates of eddies depend on the strength and path of the Kuroshio. In one path that exists mostly during fall and winter, the Kuroshio loops westward into the SCS, the potential vorticity (PV) across the current is weak, and eddies are likely to propagate freely through the Luzon Strait. In another path, which exists mostly during spring and summer, the Kuroshio tends to leap directly northward bypassing the SCS, the PV across it strengthens, and eddies are then blocked and are constrained to also follow the northward path. Nonlinear eddy-current interaction and the existence of a cyclone north of the Luzon Island during the looping phase explain why eddies of both signs can pass through the strait. It is shown also that the upstream state of the Kuroshio in the western tropical Pacific plays an important role in dictating the different paths of the Kuroshio. The looping (leaping) path is caused by a weakened (stronger) Kuroshio transport related to the northward (southward) shift of the North Equatorial Current in wintertime (summertime). (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Sheu, Woei-Jen; Wu, Chau-Ron] Natl Taiwan Normal Univ, Dept Earth Sci, Taipei 11677, Taiwan.
[Wu, Chau-Ron; Oey, Lie-Yauw] Princeton Univ, Program Atmospher & Ocean Sci, Princeton, NJ 08544 USA.
RP Wu, CR (reprint author), Natl Taiwan Normal Univ, Dept Earth Sci, 88,Sect 4 Ting Chou Rd, Taipei 11677, Taiwan.
EM cwu@ntnu.edu.tw
FU National Science Council, Taiwan, ROC [NSC 97-2621-M-003-006]
FX The authors thank the two anonymous reviewers for their detailed
suggestions to improve the manuscript. Author CRW was supported by the
National Science Council, Taiwan, ROC, under grant NSC
97-2621-M-003-006.
NR 34
TC 44
Z9 48
U1 0
U2 5
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0967-0645
J9 DEEP-SEA RES PT II
JI Deep-Sea Res. Part II-Top. Stud. Oceanogr.
PD OCT
PY 2010
VL 57
IS 19-20
BP 1783
EP 1791
DI 10.1016/j.dsr2.2010.04.004
PG 9
WC Oceanography
SC Oceanography
GA 677GB
UT WOS:000283976000004
ER
PT J
AU Doi, T
Tozuka, T
Yamagata, T
AF Doi, Takeshi
Tozuka, Tomoki
Yamagata, Toshio
TI Equivalent forcing depth in tropical oceans
SO DYNAMICS OF ATMOSPHERES AND OCEANS
LA English
DT Article
DE Equivalent forcing depth; Tropical oceans; Baroclinic mode
ID INDIAN-OCEAN; MODEL; FREQUENCY
AB The forcing efficiency for the first and the second baroclinic modes by the wind stress in tropical oceans has been discussed by calculating equivalent forcing depth from annual mean, seasonal, and pentadal density profiles of the observational data. In the annual mean field, the first mode is forced preferentially in the western Pacific and the Indian Ocean, whereas the second mode is more strongly excited in the Atlantic and the eastern Pacific. This difference is mostly due to the pycnocline depth; the second mode is more dominantly forced where the pycnocline depth is shallower. We also revealed large seasonal variations of the second mode's equivalent forcing depth in the western Indian Ocean. The first mode is more dominantly forced during boreal spring and fall in the western Indian Ocean, while the second mode becomes more dominantly forced during boreal summer and winter. Those are due to seasonal variations of both the zonal wind and the pycnocline depth. Moreover, we show that the excitation of the second mode in the western Pacific increases after the late 1970s, which is associated with the decreasing trend of the zonal pycnocline gradient. Revealing the variation of the equivalent forcing depth will be useful for understanding the oceanic response to winds in tropical oceans and the improvement in the predictability of air-sea coupled climate variability in the tropics. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Doi, Takeshi; Tozuka, Tomoki; Yamagata, Toshio] Univ Tokyo, Grad Sch Sci, Dept Earth & Planetary Sci, Tokyo 113, Japan.
RP Doi, T (reprint author), Princeton Univ, Geophys Fluid Dynam Lab NOAA, US Route 1,Forrestal Campus, Princeton, NJ 08542 USA.
EM Takeshi.Doi@noaa.gov
RI Yamagata, Toshio/A-1807-2009; Tozuka, Tomoki/A-1805-2009; Doi,
Takeshi/C-1989-2013
OI Tozuka, Tomoki/0000-0001-6738-1299;
FU Japan Society for Promotion of Science (JSPS) [50091400, 208479]
FX The present research is supported by the Japan Society for Promotion of
Science (JSPS) through both Grant-in-Aid for Scientific Research B
(50091400). Also, the first author is supported by the Research
Fellowship of the JSPS for Young Scientists (208479).
NR 28
TC 5
Z9 5
U1 0
U2 3
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0377-0265
EI 1872-6879
J9 DYNAM ATMOS OCEANS
JI Dyn. Atmos. Oceans
PD OCT
PY 2010
VL 50
IS 3
BP 415
EP 423
DI 10.1016/j.dynatmoce.2010.03.001
PG 9
WC Geochemistry & Geophysics; Meteorology & Atmospheric Sciences;
Oceanography
SC Geochemistry & Geophysics; Meteorology & Atmospheric Sciences;
Oceanography
GA 676EE
UT WOS:000283892100003
ER
PT J
AU Eldridge, WH
Hard, JJ
Naish, KA
AF Eldridge, William H.
Hard, Jeffrey J.
Naish, Kerry A.
TI Simulating fishery-induced evolution in chinook salmon: the role of
gear, location, and genetic correlation among traits
SO ECOLOGICAL APPLICATIONS
LA English
DT Article
DE chinook salmon; fisheries management; fishing gear selectivity; G
matrix; Oncorhynchus tshawytscha; overlapping generations; Puget Sound;
Washington; USA; simulation modeling; size selection
ID PACIFIC SALMON; QUANTITATIVE GENETICS; DIRECTIONAL SELECTION; PHENOTYPIC
EVOLUTION; POPULATION RECOVERY; SOCKEYE-SALMON; REACTION NORMS; SIZE;
MATURATION; AGE
AB Adaptation to human-modified ecosystems has been implicated in changing the life history of a number of wild animal populations, potentially contributing to their collapse. Fishing may be an important evolutionary force that can change the distribution of fitness-related traits; however, the magnitude and direction of the evolutionary response may be influenced by different management strategies. Most phenotypic traits subject to human-induced selection are simultaneously influenced by the environment and by genetic variation, and many traits are genetically correlated. Here, we evaluated the evolutionary outcomes of harvest activities on mean length and age at maturity in a fish population by coupling a multivariate quantitative genetic model with a Leslie life history matrix model. Lengths-at-ages were treated as genetically correlated characters parameterized from empirical data on chinook salmon (Oncorhynchus tshawytscha) populations. Using simulations, we explored the outcomes of 100 years of harvest using gill nets, which impose disruptive selection, or longlines, which impose minimum size selection, that targeted immature individuals in the high seas or maturing individuals in terminal spawning areas. Response in mean length and age depended on selection differentials imposed by harvest (which depended in turn on fishing location, gear type, and proportion of the population harvested) and on the genetic correlations between traits. Mean length was strongly influenced by the selection differential of the most abundant age class. Large differences in response were observed between the high-seas fishery, where the most abundant age was the youngest age vulnerable to harvest, compared to the terminal area fishery, where an older age class was most abundant. We observed a substantial difference in response between gill nets and longlines in the terminal fishery only. The evolution of mean age of mature individuals was less predictable, but generally increased as length decreased and decreased as length increased. The model presented here has potential for incorporating empirical data into fisheries forecasting and therefore provides a powerful means of integrating evolutionary considerations into harvest management.
C1 [Eldridge, William H.; Naish, Kerry A.] Univ Washington, Sch Aquat & Fishery Sci, Seattle, WA 98105 USA.
[Hard, Jeffrey J.] NOAA, Natl Marine Fisheries Serv, NW Fisheries Sci Ctr, Conservat Biol Div, Seattle, WA 98112 USA.
RP Eldridge, WH (reprint author), Stroud Water Res Ctr, 970 Spencer Rd, Avondale, PA 19311 USA.
EM weldridge@stroudcenter.org
RI Hard, Jeffrey/C-7229-2009; Naish, Kerry/F-5768-2014
OI Naish, Kerry/0000-0002-3275-8778
FU National Sea Grant/National Marine Fisheries Service; National Oceanic
and Atmospheric Administration [NA05OAR41711742, E/I-11]
FX The authors thank Michelle McClure, Fred Utter, and two anonymous
reviewers for providing valuable advice on an earlier version of the
manuscript. Thanks also to Jon Wittouck for providing data from the
University of Washington Hatchery. Funding in support of W. H. Eldridge
came from a National Sea Grant/National Marine Fisheries Service
Fisheries Graduate Fellowship in population dynamics while at the
University of Washington, pursuant to National Oceanic and Atmospheric
Administration award number NA05OAR41711742, project number E/I-11. The
views expressed herein are those of the authors and do not necessarily
reflect the views of NOAA or any of its subagencies.
NR 52
TC 9
Z9 9
U1 3
U2 18
PU ECOLOGICAL SOC AMER
PI WASHINGTON
PA 1990 M STREET NW, STE 700, WASHINGTON, DC 20036 USA
SN 1051-0761
J9 ECOL APPL
JI Ecol. Appl.
PD OCT
PY 2010
VL 20
IS 7
BP 1936
EP 1948
DI 10.1890/09-1186.1
PG 13
WC Ecology; Environmental Sciences
SC Environmental Sciences & Ecology
GA 655UT
UT WOS:000282278200014
PM 21049881
ER
PT J
AU Carey, MP
Wahl, DH
AF Carey, Michael P.
Wahl, David H.
TI Native fish diversity alters the effects of an invasive species on food
webs
SO ECOLOGY
LA English
DT Article
DE biodiversity; common carp; Cyprinus carpio; food webs; Illinois, USA;
invasion; invasive species
ID MULTIPLE TROPHIC LEVELS; CARP CYPRINUS-CARPIO; MICROCOSM EXPERIMENTS;
LIMITED RELEVANCE; ECOSYSTEM ECOLOGY; RECONCILING PATTERN; PREY
AVAILABILITY; MARINE ECOSYSTEM; UNITED-STATES; NORTH-AMERICA
AB Aquatic communities have been altered by invasive species, with impacts on native biodiversity and ecosystem function. At the same time, native biodiversity may mitigate the effects of an invader. Common carp (Cyprinus carpio) is a ubiquitous, invasive fish species that strongly influences community and ecosystem processes. We used common carp to test whether the potential effects of an invasive species are altered across a range of species diversity in native communities. In mesocosms, treatments of zero, one, three, and six native fish species were used to represent the nested subset patterns observed in fish communities of lakes in Illinois, USA. The effect of the invader was tested across fish richness treatments by adding common carp to the native community and substituting native biomass with common carp. Native species and intraspecific effects reduced invader growth. The invader reduced native fish growth; however, the negative effect was minimized with increasing native richness. The zooplankton grazer community was modified by a top-down effect from the invader that increased the amount of phytoplankton. Neither the invader nor richness treatments influenced total phosphorus or community metabolism. Overall, the invader reduced resources for native species, and the effect scaled with how the invader was incorporated into the community. Higher native diversity mitigated the impact of the invader, confirming the need to consider biodiversity when predicting the impacts of invasive species.
C1 Illinois Nat Hist Survey, Champaign, IL 61820 USA.
Univ Illinois, Program Ecol Evolut & Conservat Biol, Champaign, IL 61820 USA.
RP Carey, MP (reprint author), NOAA Fisheries, NW Fisheries Sci Ctr, 2725 Montlake Blvd E, Seattle, WA 98112 USA.
EM Michael.P.Carey@noaa.gov
RI Carey, Michael/G-9516-2012; Gebauer, Radek/G-6749-2015
FU National Science Foundation [DEB-0608256]; Illinois Lake Management
Association
FX We thank the staff at the Kaskaskia Biological Station, Illinois Natural
History Survey, especially K. Schnake, E. Born, K. Maloney, E. Smolik,
and M. Diana, for help in the field and with sample processing. A
National Science Foundation Doctoral Dissertation Improvement Grant
(DEB-0608256) and the Illinois Lake Management Association supported
this work. Experimental and laboratory resources were provided by the
Illinois Natural History Survey. All procedures conformed to the
University of Illinois Institutional Animal Care and Use Committee and
complied with the current laws of the United States. Reviews by J.
Brawn, C. Caceres, and K. Paige substantially improved the manuscript.
NR 83
TC 27
Z9 27
U1 8
U2 95
PU ECOLOGICAL SOC AMER
PI WASHINGTON
PA 1990 M STREET NW, STE 700, WASHINGTON, DC 20036 USA
SN 0012-9658
J9 ECOLOGY
JI Ecology
PD OCT
PY 2010
VL 91
IS 10
BP 2965
EP 2974
DI 10.1890/09-1213.1
PG 10
WC Ecology
SC Environmental Sciences & Ecology
GA 660PE
UT WOS:000282654700015
PM 21058556
ER
PT J
AU Flanigan, PM
Ross, D
Shackman, JG
AF Flanigan, Paul M.
Ross, David
Shackman, Jonathan G.
TI Determination of inorganic ions in mineral water by gradient elution
moving boundary electrophoresis
SO ELECTROPHORESIS
LA English
DT Article
DE Arsenic; Capacitively coupled contactless conductivity detection; CE;
Gradient elution moving boundary electrophoresis; Water analysis
ID CONTACTLESS CONDUCTIVITY DETECTION; CHANNEL CURRENT DETECTION;
CAPILLARY-ELECTROPHORESIS; SIMULTANEOUS SEPARATION; FLUORESCENCE
DETECTION; ZONE-ELECTROPHORESIS; SPECIATION ANALYSIS; CATIONS; ANIONS;
CHROMATOGRAPHY
AB A sensitive method was developed for the determination of the major inorganic ions in commercial mineral waters using gradient elution moving boundary electrophoresis with capacitively coupled contactless conductivity detection. This application was the first to demonstrate the separation of cations and anions simultaneously using gradient elution moving boundary electrophoresis. Seven ionic analytes (calcium, chloride, magnesium, nitrate, potassium, sodium, and sulfate) were separated in less than 7 min with detection values in the low mu mol/L to sub-mu mol/L range. Calculated values of the major ions in three commercial mineral waters were compared to reported values with good correlation. In another application, phosphate and arsenate were separated in less than 2 min with limits of detection of 300 and 140 nmol/L, respectively. For all standard analyses, the RSD for migration times and peak areas were under 3%.
C1 [Flanigan, Paul M.; Shackman, Jonathan G.] Temple Univ, Dept Chem, Philadelphia, PA 19122 USA.
[Ross, David] Natl Inst Stand & Technol, Div Biochem Sci, Gaithersburg, MD 20899 USA.
RP Shackman, JG (reprint author), Temple Univ, Dept Chem, 1901 N 13th St, Philadelphia, PA 19122 USA.
EM jshackman@temple.edu
NR 45
TC 12
Z9 12
U1 1
U2 28
PU WILEY-V C H VERLAG GMBH
PI WEINHEIM
PA PO BOX 10 11 61, D-69451 WEINHEIM, GERMANY
SN 0173-0835
J9 ELECTROPHORESIS
JI Electrophoresis
PD OCT
PY 2010
VL 31
IS 20
BP 3466
EP 3474
DI 10.1002/elps.201000230
PG 9
WC Biochemical Research Methods; Chemistry, Analytical
SC Biochemistry & Molecular Biology; Chemistry
GA 678EG
UT WOS:000284055300013
PM 20922760
ER
PT J
AU Bruno, TJ
Baibourine, E
AF Bruno, Thomas J.
Baibourine, Evgenii
TI Analysis of Organometallic Gasoline Additives with the
Composition-Explicit Distillation Curve Method
SO ENERGY & FUELS
LA English
DT Article
ID SURROGATE MIXTURE MODEL; FUEL JET-A; THERMOPHYSICAL PROPERTIES; AVIATION
FUEL; BIODIESEL FUEL; DIESEL FUEL; PHYSICOCHEMICAL AUTHENTICITY;
IMPROVEMENTS; TEMPERATURE; FLUIDS
AB Problems associated with pre-ignition of fuel in a spark-ignition engine have been documented for many years and include poor performance and structural damage in engines. These problems were addressed in the past by adding organometallic additives, such as tetraethyl lead (TEL), to the fuel. While this additive is banned, others are permitted in some jurisdictions. Two such additives are ferrocene (FC) and methylcyclopentadienyl manganese tricarbonyl (MMT). In this paper, we apply the advanced distillation curve approach to the analysis of these two additives (at concentrations of 20 and 40 mg/L) in a typical gasoline. We observe that neither additive affects the volatility of gasoline until the 55% distillate volume fraction. Subsequent to this fraction, we note temperature departures from the base gasoline that progress from 1 to 7 degrees C for FC and from approximately 1 to 4 degrees C for MMT. We further note, with the composition-explicit data channel Idle advanced distillation curve (ADC), that the additives are not found in the distillate until after the 55% distillate volume fraction and that the concentration in the distillate increases as the distillation proceeds to completion.
C1 [Bruno, Thomas J.; Baibourine, Evgenii] Natl Inst Stand & Technol, Thermophys Properties Div, Boulder, CO 80305 USA.
RP Bruno, TJ (reprint author), Natl Inst Stand & Technol, Thermophys Properties Div, Boulder, CO 80305 USA.
EM bruno@boulder.nist.gov
FU National Institute of Standards and Technology
FX A Professional Research Experience Program Undergraduate Fellowship at
the National Institute of Standards and Technology is gratefully
acknowledged by E.B.
NR 55
TC 6
Z9 6
U1 1
U2 25
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0887-0624
EI 1520-5029
J9 ENERG FUEL
JI Energy Fuels
PD OCT
PY 2010
VL 24
BP 5508
EP 5513
DI 10.1021/ef1006403
PG 6
WC Energy & Fuels; Engineering, Chemical
SC Energy & Fuels; Engineering
GA 666JO
UT WOS:000283111200025
ER
PT J
AU Outcalt, SL
Laesecke, A
Brumback, KJ
AF Outcalt, Stephanie L.
Laesecke, Arno
Brumback, Karin J.
TI Comparison of Jet Fuels by Measurements of Density and Speed of Sound of
a Flightline JP-8
SO ENERGY & FUELS
LA English
DT Article
ID DISTILLATION CURVES; S-8
AB The density of a flightline jet fuel (JP-8) was measured with two vibrating-tube densimeters. The combined range of the data is from 270 to 470 K with pressures of 40 MPa. The speed of sound in the fuel was measured with a propagation time method at ambient pressure from 278.15 to 343.15 K. The density and speed of sound results at ambient pressure were combined to obtain the adiabatic compressibility. A correlation is reported that represents the temperature and pressure dependence of the experimental data within their estimated uncertainties and can be extrapolated meaningfully beyond the pressure range of the data. The data from this jet fuel are compared to those of four previously measured jet fuels to examine the differences in their densities and speeds of sound.
C1 [Outcalt, Stephanie L.; Laesecke, Arno; Brumback, Karin J.] NIST, Expt Properties Fluids Grp, Thermophys Properties Div, Chem Sci & Technol Lab, Boulder, CO 80305 USA.
RP Outcalt, SL (reprint author), NIST, Expt Properties Fluids Grp, Thermophys Properties Div, Chem Sci & Technol Lab, 325 Broadway, Boulder, CO 80305 USA.
EM outcalt@boulder.nist.gov
FU Air Force Office of Scientific Research [MIPR F1ATA060-040004]; NIST
Boulder Summer Undergraduate Research Fellowship (SURF)
FX We acknowledge the financial support of the Air Force Office of
Scientific Research (MIPR F1ATA060-040004). Karin Brumback was supported
by a NIST Boulder Summer Undergraduate Research Fellowship (SURF). Dr.
Stephen Zabarnick, University of Dayton Research Institute, kindly
provided the density data of ref 1.
NR 20
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U1 0
U2 8
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0887-0624
J9 ENERG FUEL
JI Energy Fuels
PD OCT
PY 2010
VL 24
BP 5573
EP 5578
DI 10.1021/ef100863x
PG 6
WC Energy & Fuels; Engineering, Chemical
SC Energy & Fuels; Engineering
GA 666JO
UT WOS:000283111200032
ER
PT J
AU Lovestead, TM
Windom, BC
Riggs, JR
Nickell, C
Bruno, TJ
AF Lovestead, Tara M.
Windom, Bret C.
Riggs, Jennifer R.
Nickell, Christopher
Bruno, Thomas J.
TI Assessment of the Compositional Variability of RP-1 and RP-2 with the
Advanced Distillation Curve Approach
SO ENERGY & FUELS
LA English
DT Article
ID SURROGATE MIXTURE MODEL; FUEL JET-A; THERMOPHYSICAL PROPERTIES; AVIATION
FUEL; PHYSICOCHEMICAL AUTHENTICITY; DIESEL FUEL; IMPROVEMENTS;
TEMPERATURE; GASOLINE; FLUIDS
AB RP-1 is a long-established hydrocarbon fuel that continues to be widely used as the kerosene component in rocket propulsion systems. The desire in recent years to use rocket engines many times, rather than a single time, has led to reformulations of RP-1 and to the formulation of RP-2. In terms of processing, increased hydro-treating or the component feedstock fluids used in the manufacture of RP-1 can lower the sulfur, olefin, and aromatic content significantly. The resulting fuels have demonstrably lower metal corrosion effects and are thus more amenable to multiple use rocket engines. In recent years, the reformulated RP-1 mixtures have been extensively studied in terms of thermophysical properties, combustion processes and kinetics, and performance. Still unknown is how compositional variability resulting from the various blending strategies affects both the properties and our ability to correctly predict the fluid behavior with mathematical models. To address this question, we have obtained 11 batches of RP-1 that were prepared to represent the range of formulation recipes. For each of these representative formulations, we have assessed the compositional variability with the advanced distillation curve (ADC) metrology. This method is an improvement of classical boiling curve techniques. It features (1) a composition explicit data channel for each distillate fraction (for both qualitative and quantitative analysis), (2) temperature measurements that are true thermodynamic state points that can be modeled with an equation of state, (3) temperature, volume, and pressure measurements of low uncertainty suitable for equation of state development, (4) consistency with a century of historical data, (5) an assessment of the energy content of each distillate fraction, (6) trace chemical analysis of each distillate fraction, and (7) corrosivity assessment of each distillate fraction. In this paper, we will employ all applicable data channels of the ADC to show the compositional variability and also discuss how the variability will impact predictive modeling. We use these data to conclude that the variabilities of RP-1 and RP-2 are significant and perhaps higher than expected.
C1 [Lovestead, Tara M.; Windom, Bret C.; Riggs, Jennifer R.; Nickell, Christopher; Bruno, Thomas J.] NIST, Thermophys Properties Div, Boulder, CO USA.
RP Bruno, TJ (reprint author), NIST, Thermophys Properties Div, Boulder, CO USA.
EM bruno@boulder.nist.gov
FU National Academy of Science/National Research Council; Air Force
Research Laboratory [MIPR F4FBEX9205G001]
FX B.C.W. and T.M.L. acknowledge the National Academy of Science/National
Research Council postdoctoral associateship program. J.R.R. and C.N.
acknowledge Summer Undergraduate Research Fellowships at NIST. The
financial support of the Air Force Research Laboratory (Grant MIPR
F4FBEX9205G001) is gratefully acknowledged.
NR 67
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U1 1
U2 13
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0887-0624
EI 1520-5029
J9 ENERG FUEL
JI Energy Fuels
PD OCT
PY 2010
VL 24
BP 5611
EP 5623
DI 10.1021/ef100994w
PG 13
WC Energy & Fuels; Engineering, Chemical
SC Energy & Fuels; Engineering
GA 666JO
UT WOS:000283111200037
ER
PT J
AU Bao, YH
Kunnath, SK
AF Bao, Yihai
Kunnath, Sashi K.
TI Simplified progressive collapse simulation of RC frame-wall structures
SO ENGINEERING STRUCTURES
LA English
DT Article
DE Shear wall; Progressive collapse; Reinforced concrete; Nonlinear
response; Frame and shear wall structures
ID SHEAR PANELS; PREDICTION; FLEXURE; DAMAGE
AB A macromodel-based approach to enable post-event progressive collapse analysis of reinforced concrete (RC) frame-wall structures is investigated. A simplified shear wall model is developed to simulate the inelastic behavior of a multi-story frame-wall system due to the sudden loss of a significant portion of the shear wall at the first story. Detailed finite element analyses are employed not only to provide modeling insights but also as a tool to verify the accuracy of the developed shear wall model. Two perimeter frame-wall systems designed for different seismic zones are modeled using the proposed approach and numerical simulations following the sudden loss of a portion of the shear wall at the lowest story are compared and evaluated. Although no signs of collapse are evident in either system, detailed investigation of force variations in structural members shows that the seismically designed frame-wall system (SDC-D) is a more robust system compared to a system designed for much lower seismic demands due to the effectiveness of its structural layout and seismic detailing. The simplified methodology is a suitable approach for preliminary progressive collapse investigation of RC frame-wall structures. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Bao, Yihai; Kunnath, Sashi K.] Univ Calif Davis, Dept Civil & Environm Engn, Davis, CA 95616 USA.
[Bao, Yihai] NIST, Gaithersburg, MD 20899 USA.
RP Kunnath, SK (reprint author), Univ Calif Davis, Dept Civil & Environm Engn, Davis, CA 95616 USA.
EM skkunnath@ucdavis.edu
FU National Science Foundation [CMMI-0928953]; National Institute of
Standards and Technology [NIST 60NANB8D8139]
FX The presented work was supported by the National Science Foundation
through grant CMMI-0928953 and the National Institute of Standards and
Technology through grant NIST 60NANB8D8139. Any opinions, findings,
conclusions, and recommendations expressed in this paper are those of
the authors and do not necessarily reflect the views of the sponsor.
NR 28
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U1 4
U2 19
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0141-0296
J9 ENG STRUCT
JI Eng. Struct.
PD OCT
PY 2010
VL 32
IS 10
BP 3153
EP 3162
DI 10.1016/j.engstruct.2010.06.003
PG 10
WC Engineering, Civil
SC Engineering
GA 662ZB
UT WOS:000282851700016
ER
PT J
AU Anenberg, SC
West, JJ
Horowitz, LW
Tong, DQ
AF Anenberg, Susan C.
West, J. Jason
Horowitz, Larry W.
Tong, Daniel Q.
TI The Global Burden of Air Pollution on Mortality response
SO ENVIRONMENTAL HEALTH PERSPECTIVES
LA English
DT Letter
C1 [Anenberg, Susan C.; West, J. Jason] Univ N Carolina, Chapel Hill, NC 27515 USA.
[Horowitz, Larry W.] Natl Ocean & Atmospher Adm, Geophys Fluid Dynam Lab, Princeton, NJ USA.
[Tong, Daniel Q.] Sci & Technol Corp, Silver Spring, MD USA.
RP Anenberg, SC (reprint author), Univ N Carolina, Chapel Hill, NC 27515 USA.
EM jjwest@email.unc.edu
RI Tong, Daniel/A-8255-2008; Horowitz, Larry/D-8048-2014; West,
Jason/J-2322-2015
OI Tong, Daniel/0000-0002-4255-4568; Horowitz, Larry/0000-0002-5886-3314;
West, Jason/0000-0001-5652-4987
NR 7
TC 0
Z9 0
U1 0
U2 3
PU US DEPT HEALTH HUMAN SCIENCES PUBLIC HEALTH SCIENCE
PI RES TRIANGLE PK
PA NATL INST HEALTH, NATL INST ENVIRONMENTAL HEALTH SCIENCES, PO BOX 12233,
RES TRIANGLE PK, NC 27709-2233 USA
SN 0091-6765
J9 ENVIRON HEALTH PERSP
JI Environ. Health Perspect.
PD OCT
PY 2010
VL 118
IS 10
BP A424
EP A425
DI 10.1289/ehp.1002397R
PG 2
WC Environmental Sciences; Public, Environmental & Occupational Health;
Toxicology
SC Environmental Sciences & Ecology; Public, Environmental & Occupational
Health; Toxicology
GA 656YL
UT WOS:000282376900004
ER
PT J
AU Conte, D
Miglietta, MM
Moscatello, A
Albers, S
Levizzani, V
AF Conte, Dario
Miglietta, Mario Marcello
Moscatello, Agata
Albers, Steve
Levizzani, Vincenzo
TI A GIS approach to ingest Meteosat Second Generation data into the Local
Analysis and Prediction System
SO ENVIRONMENTAL MODELLING & SOFTWARE
LA English
DT Review
DE Weather forecasting; Mesoscale analyses; Nowcasting; Clouds; Meteosat;
Satellite meteorology; Geographic; Information System; Open source
software
ID MEDITERRANEAN HURRICANE; LAPS
AB The Local Analysis and Prediction System (LAPS) is modified to ingest Meteosat Second Generation (MSG) data for cloud analysis. A first study is conducted to test the actual performance of the weather analysis software after new satellite bands are introduced. Results show that the system provides high quality cloud products such as cloud mask, cloud top height and cloudiness. A comparison with products from EUMETSAT's Nowcasting SAF shows a general underestimation of the LAPS product although the results are not conclusive. The study shows the potential of MSG data in refining the mesoscale analyses produced by LAPS. Moreover the software tools, based on open source codes for geolocation and geographical information systems, written for the transformation of MSG data into input files for LAPS have demonstrated a great flexibility and ease of use. The study opens up an avenue for successive validation and refinement of the analyses together with their improved implementation for operational nowcasting and very short range forecasting applications. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Conte, Dario; Moscatello, Agata] ISAC CNR, I-73100 Lecce, Italy.
[Miglietta, Mario Marcello] ISAC CNR, Padua, Italy.
[Albers, Steve] NOAA ESRL GSD, Boulder, CO USA.
[Albers, Steve] CIRA, Boulder, CO USA.
[Levizzani, Vincenzo] ISAC CNR, Bologna, Italy.
RP Conte, D (reprint author), ISAC CNR, Str Prov Lecce Monteroni Km 1,200, I-73100 Lecce, Italy.
EM d.conte@isac.cnr.it
RI Levizzani, Vincenzo/A-9070-2013; Miglietta, Mario Marcello/C-6416-2013
OI Levizzani, Vincenzo/0000-0002-7620-5235; Miglietta, Mario
Marcello/0000-0003-2898-1595
FU Italian Space Agency (ASI); EUMETSAT; Regione Puglia
FX The authors are grateful to Regione Puglia for support provided under
the Progetto Strategico "Nowcasting avanzato con l'uso di tecnologie
GRID e GIS". VL also wishes to acknowledge partial support from the
Italian Space Agency (ASI) within the project "Prodotti di Osservazione
Satellitare per Allerta Meteorologica" (PROSA) and from EUMETSAT within
the Satellite Application Facility on Support to Operational Hydrology
and Water Management (H-SAF).
NR 29
TC 2
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U1 1
U2 5
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 1364-8152
J9 ENVIRON MODELL SOFTW
JI Environ. Modell. Softw.
PD OCT
PY 2010
VL 25
IS 10
BP 1064
EP 1074
DI 10.1016/j.envsoft.2010.03.023
PG 11
WC Computer Science, Interdisciplinary Applications; Engineering,
Environmental; Environmental Sciences
SC Computer Science; Engineering; Environmental Sciences & Ecology
GA 619DY
UT WOS:000279410600001
ER
PT J
AU Browne, E
Kelley, M
Zhou, GD
He, LY
McDonald, T
Wang, S
Duncan, B
Meador, JP
Donnelly, K
Gallagher, E
AF Browne, Eva
Kelley, Matthew
Zhou, Guo-Dong
He, Ling Yu
McDonald, Thomas
Wang, Shirley
Duncan, Bruce
Meador, James P.
Donnelly, Kirby
Gallagher, Evan
TI In situ biomonitoring of juvenile Chinook salmon (Onchorhynchus
tshawytscha) using biomarkers of chemical exposures and effects in a
partially remediated urbanized waterway of the Puget Sound, WA
SO ENVIRONMENTAL RESEARCH
LA English
DT Article
DE Biomarkers; Chinook salmon; Quantitative RT-PCR; Sediment pollutants;
(32)P-postlabeling
ID SOLE PAROPHRYS-VETULUS; POLYCYCLIC AROMATIC-HYDROCARBONS;
GLUTAMATE-CYSTEINE LIGASE; ONCORHYNCHUS-TSHAWYTSCHA;
POLYCHLORINATED-BIPHENYLS; GENE-EXPRESSION; HEPATIC-LESIONS;
DNA-ADDUCTS; INCREASED SUSCEPTIBILITY; WASHINGTON
AB In situ biomonitoring has been used to assess the effects of pollution on aquatic species in heavily polluted waterways. In the current study, we used in situ biomonitoring in conjunction with molecular biomarker analysis to determine the effects of pollutant exposure in salmon caged in the Duwamish waterway, a Pacific Northwest Superfund site that has been subject to remediation. The Duwamish waterway is an important migratory route for Pacific salmon and has received historic inputs of polycyclic aromatic hydrocarbons (PAHs) and polychlorinated biphenyls (PCBs). juvenile pre-smolt Chinook salmon (Oncorhynchus tshawytscha) caged for 8 days in the three contaminated sites in close proximity within the Duwamish were analyzed for steady state hepatic mRNA expression of 7 exposure biomarker genes encompassing several gene families and known to be responsive to pollutants, including cytochrome P4501A (CYP1A) and CYP2K1, glutathione S-transferase pi class (GST-pi), microsomal GST (mGST), glutamylcysteine ligase catalytic subunit (GCLC), UDP-glucuronyltransferase family 1 (UDPGT), and type 2 deiodinase (type 2 D1, or D2). Quantitation of gene expression was accomplished by quantitative reverse transcriptase polymerase chain reaction (qRT-PCR) in assays developed specifically for Chinook salmon genes. Gill PAH-DNA adducts were assessed as a chemical effects biomarker using (32)P-postlabeling. The biomarkers in the field-caged fish were analyzed with respect to caged animals maintained at the hatchery receiving flow-through water. Chemical analysis of sediment samples from three field sampling sites revealed relatively high concentrations of total PAHs in one site (site B2, 6711 ng/g dry weight) and somewhat lower concentrations of PAHs in two adjacent sites (sites B3 and B4, 1482 and 1987 ng/g, respectively). In contrast, waterborne PAHs at all of the sampling sites were relatively low ( < 1 ng/L). Sediment PCBs at the sites ranged from a low of 421 ng/g at site B3 to 1160 ng/g at site B4, and there were no detectable waterborne PCBs at any of the sites (detection limit= 10 ng/L). There were no significant differences (p < 0.05) in biomarker gene expression in the Duwamish-caged fish relative to controls, although there was a pattern of gene expression suppression at site B3, the most heavily PAH-enriched site. The lack of a marked perturbation of mRNA biomarkers was consistent with relatively low levels of gill PAH-DNA adduct levels that did not differ among caged reference and field fish, and which were also consistent with relatively low waterborne concentrations of chemicals. The results of our study suggest a low bioavailability of sediment pollutants in caged juvenile Chinook potentially reflecting low waterborne exposures occurring at contaminated sites within the Duwamish waterway that have undergone partial remediation. (C) 2010 Elsevier Inc. All rights reserved.
C1 [Browne, Eva; Gallagher, Evan] Univ Washington, Dept Environm & Occupat Hlth Sci, Seattle, WA 98105 USA.
[Kelley, Matthew; Zhou, Guo-Dong; He, Ling Yu; McDonald, Thomas; Wang, Shirley; Donnelly, Kirby] Texas A&M Hlth Sci Ctr, Dept Environm & Occupat Hlth, College Stn, TX 77843 USA.
[Duncan, Bruce] US EPA, Seattle, WA 98101 USA.
[Meador, James P.] Natl Marine Fisheries Serv, Ecotoxicol Div, Seattle, WA 98105 USA.
RP Gallagher, E (reprint author), Univ Washington, Dept Environm & Occupat Hlth Sci, 4225 Roosevelt Way NE,Suite 100, Seattle, WA 98105 USA.
EM evang3@u.washington.edu
FU NIEHS; University of Washington; Texas AM University [P42 ES004696, P42
ES04917]; National Oceanic and Atmospheric Administration, Oceans and
Human Health Program [NA05NS4781253]; USEPA [10]
FX We will miss the friendship, collegiality, and conversations with our
good friend, Dr. K.C. Donnelly, who passed away in July 2009. This work
is a collaboration among two NIEHS Superfund Research Program (SRP)
program project awards to the University of Washington and Texas A&M
University. Accordingly, this work was funded in part by P42 ES004696
and P42 ES04917. Additional funding for the study was provided in part
from the National Oceanic and Atmospheric Administration, Oceans and
Human Health Program (NA05NS4781253), and the Region 10 office of the
USEPA (USEPA Region 10). The technical comments of Dr. Karen Peck at
NOAA fisheries are appreciated.
NR 53
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Z9 7
U1 3
U2 22
PU ACADEMIC PRESS INC ELSEVIER SCIENCE
PI SAN DIEGO
PA 525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA
SN 0013-9351
J9 ENVIRON RES
JI Environ. Res.
PD OCT
PY 2010
VL 110
IS 7
BP 675
EP 683
DI 10.1016/j.envres.2010.06.007
PG 9
WC Environmental Sciences; Public, Environmental & Occupational Health
SC Environmental Sciences & Ecology; Public, Environmental & Occupational
Health
GA 652HV
UT WOS:000281995400005
PM 20619832
ER
PT J
AU Yordy, JE
Mollenhauer, MAM
Wilson, RM
Wells, RS
Hohn, A
Sweeney, J
Schwacke, LH
Rowles, TK
Kucklick, JR
Peden-Adams, MM
AF Yordy, Jennifer E.
Mollenhauer, Meagan A. M.
Wilson, Rachel M.
Wells, Randall S.
Hohn, Aleta
Sweeney, Jay
Schwacke, Lori H.
Rowles, Teri K.
Kucklick, John R.
Peden-Adams, Margie M.
TI COMPLEX CONTAMINANT EXPOSURE IN CETACEANS: A COMPARATIVE E-SCREEN
ANALYSIS OF BOTTLENOSE DOLPHIN BLUBBER AND MIXTURES OF FOUR PERSISTENT
ORGANIC POLLUTANTS
SO ENVIRONMENTAL TOXICOLOGY AND CHEMISTRY
LA English
DT Article
DE Persistent organic pollutants; Contaminant mixtures; Estrogenicity;
Antiestrogenicity; Bottlenose dolphin
ID ENDOCRINE-DISRUPTING CHEMICALS; STEROID-HORMONE ACTION;
POLYCHLORINATED-BIPHENYLS; ESTROGENIC ACTIVITY; TURSIOPS-TRUNCATUS;
GREAT-LAKES; REPRODUCTIVE SUCCESS; POLAR BEARS; HUMAN SERUM; ASSAY
AB Cetaceans are federally protected species that are prone to accumulate complex mixtures of persistent organic pollutants (POPs), which individually may exert estrogenic or antiestrogenic effects. In the present study it was assessed whether contaminant mixtures harbored by cetaceans are estrogenic or antiestrogenic using a comparative approach. Interactions of antiestrogenic and estrogenic compounds were first investigated with the E-Screen assay using a mixture of four POPs (dichlorodiphenyldichloroethylene [4,4'-DDE], trans-nonachlor, and polychlorinated biphenyls [PCBs] 138 180) prevalent in cetacean blubber. Estrogenic/antiestrogenic activity was determined for the individual compounds and their binary, tertiary, and quaternary combinations. Significantly different responses were observed for the various POP mixtures, including enhanced estrogenic and antiestrogenic effects and antagonistic interactions. These results were then compared to the concentrations and estrogenic/antiestrogenic activity of contaminant mixtures isolated directly from the blubber of 15 bottlenose dolphins (Tursiops truncatus) collected from five U.S. Atlantic and Gulf of Mexico locations. The lowest observed effect concentrations (LOECs) determined for 4,4'-DDE (20 mu mol/L), PCB 138 (20 mu mol/L), PCB 180 (21 [anon), and trans-nonachlor (3 mu mol/L) in the E-Screen were greater than estimated dolphin blood concentrations. Although estimated blood concentrations were below the LOECs, significant estrogenic activity was detected in diluted dolphin blubber from Cape May, NJ and Bermuda. Positive correlations between blubber estrogenicity and select POP concentrations (Sigma DDTs, Sigma PBDEs, Sigma HCB, Sigma estrogenic PCBs, Sigma estrogenic POPs) were also observed. Collectively, these results suggest that select bottlenose dolphin populations may be exposed to contaminants that act in concert to exert estrogenic effects at biologically relevant concentrations. These observations do not necessarily provide direct evidence of endocrine disruption; however, they may indicate an environmental source of xenoestrogenic exposure warranting future research. Environ. Toxicol. Chem. 2010;29:2143-2153. (C) 2010 SETAC
C1 [Yordy, Jennifer E.; Peden-Adams, Margie M.] Med Univ S Carolina, Marine Biomed & Environm Sci Ctr, Charleston, SC 29412 USA.
[Yordy, Jennifer E.; Kucklick, John R.] Natl Inst Stand & Technol, Hollings Marine Lab, Charleston, SC 29412 USA.
[Mollenhauer, Meagan A. M.; Peden-Adams, Margie M.] Med Univ S Carolina, Mol & Cell Biol Program, Charleston, SC 29425 USA.
[Mollenhauer, Meagan A. M.; Peden-Adams, Margie M.] Med Univ S Carolina, Dept Pediat, Charleston, SC 29425 USA.
[Wilson, Rachel M.] Florida State Univ, Dept Oceanog, Tallahassee, FL 32306 USA.
[Wells, Randall S.] Mote Marine Lab, Chicago Zool Soc, Sarasota, FL 34236 USA.
[Hohn, Aleta] Natl Marine Fisheries Serv, SE Fisheries Sci Ctr, Beaufort, NC 28516 USA.
[Sweeney, Jay] Dolphin Quest, San Diego, CA 93207 USA.
[Rowles, Teri K.] Natl Marine Fisheries Serv, ff Protected Resources, Silver Spring, MD 20910 USA.
[Schwacke, Lori H.] NOAA, Ctr Human Hlth Risks, Hollings Marine Lab, Charleston, SC USA.
[Peden-Adams, Margie M.] Myst Aquarium, Mystic, CT 06355 USA.
[Peden-Adams, Margie M.] Inst Explorat, Mystic, CT 06355 USA.
RP Yordy, JE (reprint author), Med Univ S Carolina, Marine Biomed & Environm Sci Ctr, Charleston, SC 29412 USA.
EM jennifer.yordy@noaa.gov
RI Hohn, Aleta/G-2888-2011; Wilson, Rachel /F-2723-2013
OI Hohn, Aleta/0000-0002-9992-7062;
FU Sea Research Foundation [185]
FX We thank A. Soto and M. Banica for providing the MCF-7-BOS cells. We
also thank P. Fair for use of her laboratory and instrumentation and A.
Peck, R. Heltsley, S. Tai, and K. Huncik for assistance with LC/MS/MS
method development. This work constitutes Scientific Contribution Number
185 from the Sea Research Foundation. Certain commercial equipment or
instruments are identified in the article to adequately specify the
experimental procedures. Such identification does not imply
recommendations or endorsement by the National Institute of Standards
and Technology, nor does it imply that the equipment or instruments are
the best available for the purpose.
NR 47
TC 6
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U1 1
U2 23
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0730-7268
EI 1552-8618
J9 ENVIRON TOXICOL CHEM
JI Environ. Toxicol. Chem.
PD OCT
PY 2010
VL 29
IS 10
BP 2143
EP 2153
DI 10.1002/etc.279
PG 11
WC Environmental Sciences; Toxicology
SC Environmental Sciences & Ecology; Toxicology
GA 658FV
UT WOS:000282476800004
PM 20872675
ER
PT J
AU Zimmerman, BE
Bergeron, DE
Cessna, JT
AF Zimmerman, B. E.
Bergeron, D. E.
Cessna, J. T.
TI Development of Traceable Phantom Sources for Quantitative PET Imaging
SO EUROPEAN JOURNAL OF NUCLEAR MEDICINE AND MOLECULAR IMAGING
LA English
DT Meeting Abstract
CT 23rd Annual Congress of the European-Association-of-Nuclear-Medicine
(EANM)
CY OCT 09-13, 2010
CL Vienna, AUSTRIA
SP European Assoc Nuclear Med
C1 [Zimmerman, B. E.; Bergeron, D. E.; Cessna, J. T.] NIST, Gaithersburg, MD 20899 USA.
RI Bergeron, Denis/I-4332-2013
OI Bergeron, Denis/0000-0003-1150-7950
NR 0
TC 2
Z9 2
U1 1
U2 1
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1619-7070
J9 EUR J NUCL MED MOL I
JI Eur. J. Nucl. Med. Mol. Imaging
PD OCT
PY 2010
VL 37
SU 2
BP S313
EP S313
PG 1
WC Radiology, Nuclear Medicine & Medical Imaging
SC Radiology, Nuclear Medicine & Medical Imaging
GA 665GQ
UT WOS:000283023800515
ER
PT J
AU Lawson, JR
Mell, WE
Prasad, K
AF Lawson, James R.
Mell, William E.
Prasad, Kuldeep
TI A Heat Transfer Model for Firefighters' Protective Clothing, Continued
Developments in Protective Clothing Modeling
SO FIRE TECHNOLOGY
LA English
DT Article
DE Heat transfer; Computer modeling; Fire; Firefighter safety; Protective
clothing; Thermal insulation; Turnout coats
AB In the year 2000, a paper entitled "A Heat Transfer Model for Firefighters' Protective Clothing" was published in Volume 36, No. 1, of Fire Technology, and it received the 2001 Harry C. Bigglestone Award for Excellence in Written Communication of Fire Protection Concepts from The Fire Protection Research Foundation. Since the publication of this paper, there has been additional development of the heat transfer model. The radiant heat transfer element has been refined, and the model can now address predictions of heat transfer through wet protective clothing materials. Additionally, there has been an extension of the thermal properties database for fabric materials used to manufacture firefighters' protective clothing. These improvements have significantly expanded the capabilities of the model and provide users with a more robust tool for economically predicting thermal protective clothing performance.
C1 [Lawson, James R.] Natl Inst Stand & Technol, Fire Fighting Technol Grp, Fire Res Div, Bldg & Fire Res Lab, Gaithersburg, MD 20899 USA.
RP Lawson, JR (reprint author), Natl Inst Stand & Technol, Fire Fighting Technol Grp, Fire Res Div, Bldg & Fire Res Lab, 100 Bur Dr,Stop 8661, Gaithersburg, MD 20899 USA.
EM james.lawson@nist.gov
NR 10
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U1 2
U2 10
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0015-2684
J9 FIRE TECHNOL
JI Fire Technol.
PD OCT
PY 2010
VL 46
IS 4
SI SI
BP 833
EP 841
DI 10.1007/s10694-010-0139-z
PG 9
WC Engineering, Multidisciplinary; Materials Science, Multidisciplinary
SC Engineering; Materials Science
GA 640XI
UT WOS:000281087000006
ER
PT J
AU Neahr, TA
Stunz, GW
Minello, TJ
AF Neahr, T. A.
Stunz, G. W.
Minello, T. J.
TI Habitat use patterns of newly settled spotted seatrout in estuaries of
the north-western Gulf of Mexico
SO FISHERIES MANAGEMENT AND ECOLOGY
LA English
DT Article
DE hatchery-reared fish; mesocosm; salt marsh; sciaenid; seagrass
ID JUVENILE RED DRUM; SALT-MARSH; STOCK ENHANCEMENT; NURSERY HABITATS;
SEAGRASS MEADOWS; GALVESTON BAY; FISH LARVAE; WILD-CAUGHT; REEF FISHES;
GROWTH
AB P>This study examined habitat use patterns of newly settled spotted seatrout Cynoscion nebulosus (Cuvier) across several Gulf of Mexico estuaries. Intensive sampling using an epibenthic sled was conducted in three Texas bays and among three potential habitat types. A long-term data set (1982 to 1997) from the National Marine Fisheries Service was also used to examine C. nebulosus habitat use patterns in both marsh and seagrass-dominated bay systems for broad regional comparisons along the north-western Gulf of Mexico. Vegetated habitat types such as seagrass and marsh supported the highest densities and use was dependent upon availability of particular vegetated habitat types. In laboratory mesocosm experiments, both wild-caught and hatchery-reared C. nebulosus, showed strong selection for structured and vegetated habitat types. These field and laboratory results suggest that seagrass meadows and marshes may be functioning as important habitat for C. nebulosus in Gulf of Mexico, and other habitat types such as oyster reef need further evaluation.
C1 [Stunz, G. W.] Texas A&M Univ, Harte Res Inst Gulf Mexico Studies, Dept Life Sci, Corpus Christi, TX 78412 USA.
[Neahr, T. A.] Texas Parks & Wildlife Dept, Coastal Fisheries Div, Corpus Christi, TX USA.
[Minello, T. J.] NOAA Fisheries Serv, Fisheries Ecol Branch, SE Fisheries Sci Ctr, Galveston, TX USA.
RP Stunz, GW (reprint author), Texas A&M Univ, Harte Res Inst Gulf Mexico Studies, Dept Life Sci, 6300 Ocean Dr, Corpus Christi, TX 78412 USA.
EM greg.stunz@tamucc.edu
FU Texas Research Development Fund
FX Funding for this study was provided by the Texas Research Development
Fund. We thank the Texas Parks and Wildlife Department, Perry R. Bass
Marine Hatchery for generously supplying us with hatchery-reared fish.
This research was conducted through the Fisheries Ecology Laboratory at
Texas A&M University-Corpus Christi and the Fisheries Ecology Branch at
NOAA Fisheries Galveston Laboratory. Help from many in both laboratories
was essential including Heather Barackman, Sarah Bayer, Amanda Bushon,
Lew Lampton for providing assistance in the field and laboratory.
Special thanks to the contributions and input by Megan Reese Robillard
for helping in many aspects of this project from fieldwork, analysis,
producing Fig. 1 and manuscript review. We would also like to thank two
anonymous reviewers for providing comments and suggestions that greatly
improved this manuscript.
NR 40
TC 13
Z9 14
U1 1
U2 19
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0969-997X
J9 FISHERIES MANAG ECOL
JI Fisheries Manag. Ecol.
PD OCT
PY 2010
VL 17
IS 5
BP 404
EP 413
DI 10.1111/j.1365-2400.2010.00733.x
PG 10
WC Fisheries
SC Fisheries
GA 651AO
UT WOS:000281897200004
ER
PT J
AU Alfaro-Shigueto, J
Mange, JC
Pajuelo, M
Dutton, PH
Seminoff, JA
Godley, BJ
AF Alfaro-Shigueto, Joanna
Mangel, Jeffrey C.
Pajuelo, Mariela
Dutton, Peter H.
Seminoff, Jeffrey A.
Godley, Brendan J.
TI Where small can have a large impact: Structure and characterization of
small-scale fisheries in Peru
SO FISHERIES RESEARCH
LA English
DT Article
DE Small-scale fisheries; Longlines; Gillnets; Peru; Bycatch; Pacific
ID ANCHOVY ENGRAULIS-RINGENS; BYCATCH REDUCTION; SEA-TURTLES; LONGLINE
FISHERIES; SWORDFISH FISHERY; SEABIRD BYCATCH; SOUTH-PACIFIC; MORTALITY;
CATCH; CONSERVATION
AB Small-scale fisheries in Peru constitute an important source of food and employment for coastal communities where fish is the single most important natural resource. Utilizing official statistics and extensive survey data from 30 fishing ports and by onboard observers operating from 11 ports, we review how these fisheries grew from 1995 to 2005, and provide insights into the relative importance of different fishing gears and their modes of operation. Small-scale fisheries operate along the entire Peruvian coast and have continued expanding in number of vessels and fishers in all geopolitical regions except one. Nationwide, the number of fishers grew by 34% from 28 098 to 37727 and the number of vessels increased by 54% from 6268 to 9667. At 30 harbors, the number of vessels increased for purse seiners (17.8%) and longliners (357.4%), while gillnets decreased (similar to 14.5%). These dramatic changes could jeopardize the sustainability of these fisheries and the livelihoods of those who depend upon them, especially considering the limited capacity for management. Despite increase in effort, catch and catch per vessel have decreased, especially in some of the sub-regions that previously constituted the majority of effort and landings, raising concerns regarding their sustainability. Of the fishing gears monitored, gillnets were shown to have the most frequent interactions with threatened taxa such as marine mammals, seabirds and sea turtles. The total length of gillnets set in Peru was estimated at >100000 km of net per year, about 14 times the length used by the Taiwanese high seas driftnet fleet in the Pacific before it was banned. Longlines, although shown to be a more efficient fishing method (economically and in terms of selectivity), still had bycatch of turtles and seabirds, and marine mammals are targeted to be used as bait. We conservatively estimate that longline vessels operating in Peru set an average of 80 million hooks per year; equivalent to one-third of the annual effort of the global industrial swordfish longline fishery. We conclude that, despite their definition as small-scale, the magnitude of these fleets and their fishing effort are vast and are of concern with regard to their long term sustainability and their impacts and interactions with large marine vertebrates. We highlight the need for increased research and management measures to ensure the long term viability of these fisheries. (C) 2010 Elsevier B.V. All rights reserved.
C1 [Alfaro-Shigueto, Joanna; Mangel, Jeffrey C.; Pajuelo, Mariela] Pro Delphinus, Lima 11, Peru.
[Alfaro-Shigueto, Joanna; Mangel, Jeffrey C.; Godley, Brendan J.] Univ Exeter, Marine Turtle Res Grp, Ctr Ecol & Conservat, Sch Biosci, Penryn TR10 9EZ, Cornwall, England.
[Dutton, Peter H.; Seminoff, Jeffrey A.] NOAA Natl Marine Fisheries Serv, SW Fisheries Sci Ctr, La Jolla, CA 92037 USA.
RP Alfaro-Shigueto, J (reprint author), Pro Delphinus, Octavio Bernal 572-5, Lima 11, Peru.
EM jas_26@yahoo.com
RI godley, brendan/A-6139-2009
OI godley, brendan/0000-0003-3845-0034
FU NOAA SWFSC; NFWF; CLP; Idea Wild; IAATO; NOAA PRO in Juneau; ABC; Oak
Foundation through the CMC at Duke University; Darwin Initiative
Sustainable Artisanal Fisheries Initiative in Peru; ORSAS; Exeter
University
FX We would like to thank the members of the fishing communities who
participated in this study, in particular the fishers who were willing
to have an observer on board. We also want to thank Celia Caceres,
Francisco Bernedo and Mateo Mamani for their help in data collection.
The Artisanal Fisheries Office at PRODUCE was most helpful with the
interpretation of the information from PRODUCE landings data. We also
would like to thank the two reviewers and the editor for their useful
comments on this manuscript. This study was conducted with funds and
equipment received from NOAA SWFSC, NFWF, CLP, Idea Wild, IAATO, NOAA
PRO in Juneau, ABC, the Oak Foundation through the CMC at Duke
University and the Darwin Initiative Sustainable Artisanal Fisheries
Initiative in Peru. JCM and JAS are ORSAS and Exeter University
scholarship awardees respectively.
NR 64
TC 43
Z9 48
U1 0
U2 34
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0165-7836
J9 FISH RES
JI Fish Res.
PD OCT
PY 2010
VL 106
IS 1
BP 8
EP 17
DI 10.1016/j.fishres.2010.06.004
PG 10
WC Fisheries
SC Fisheries
GA 670WN
UT WOS:000283458200002
ER
PT J
AU Towler, R
Williams, K
AF Towler, Richard
Williams, Kresimir
TI An inexpensive millimeter-accuracy electronic length measuring board
SO FISHERIES RESEARCH
LA English
DT Article
DE Fish measuring board; Fish length measurement
AB A design is presented for a cost-effective, easy to use, millimeter resolution electronic fish measuring board. The device is easily assembled from commercially available electronic components and a customized electronic control board. The principal component of this design is a magnetostrictive linear distance sensor. This sensor is an alternative to previous approaches in magnetic measuring technology that used magnetoresistive or Hall-effect sensors. The measuring device is connected to a personal computer or personal digital assistant running a data acquisition application. Length measurements are taken by momentarily placing a magnet on the length board sensor at the desired measurement location. The described electronic fish measuring board is a robust, inexpensive and efficient alternative to other methods and devices used to rapidly collect relatively large numbers of high-resolution length measurements. Published by Elsevier B.V.
C1 [Towler, Richard; Williams, Kresimir] NOAA, Natl Marine Fisheries Serv, Alaska Fisheries Sci Ctr, Resource Assessment & Conservat Engn Div, Seattle, WA 98115 USA.
RP Towler, R (reprint author), NOAA, Natl Marine Fisheries Serv, Alaska Fisheries Sci Ctr, Resource Assessment & Conservat Engn Div, 7600 Sand Point Way NE, Seattle, WA 98115 USA.
EM rick.towler@noaa.gov
NR 5
TC 2
Z9 2
U1 0
U2 3
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0165-7836
J9 FISH RES
JI Fish Res.
PD OCT
PY 2010
VL 106
IS 1
BP 107
EP 111
DI 10.1016/j.fishres.2010.06.012
PG 5
WC Fisheries
SC Fisheries
GA 670WN
UT WOS:000283458200016
ER
PT J
AU Hurst, TP
Laurel, BJ
Ciannelli, L
AF Hurst, Thomas P.
Laurel, Benjamin J.
Ciannelli, Lorenzo
TI Ontogenetic patterns and temperature-dependent growth rates in early
life stages of Pacific cod (Gadus macrocephalus)
SO FISHERY BULLETIN
LA English
DT Article
ID NORTHERN ROCK SOLE; PLAICE PLEURONECTES-PLATESSA; SOUTHEASTERN
BERING-SEA; JUVENILE ATLANTIC COD; CLIMATE-CHANGE;
LEPIDOPSETTA-POLYXYSTRA; THERAGRA-CHALCOGRAMMA; FISH POPULATIONS;
LARVAE; MORHUA
AB Pacific cod (Gadus macrocephalus) is an important component of fisheries and food webs in the North Pacific Ocean and Bering Sea. However, vital rates of early life stages of this species have yet to be described in detail. We determined the thermal sensitivity of growth rates of embryos, preflexion and postflexion larvae, and postsettlement juveniles. Growth rates (length and mass) at each ontogenetic stage were measured in three replicate tanks at four to five temperatures. Nonlinear regression was used to obtain parameters for independent stage-specific growth functions and a unified size- and temperature-dependent growth function. Specific growth rates increased with temperature at all stages and generally decreased with increases in body size. However, these analyses revealed a departure from a strict size-based allometry in growth patterns, as reduced growth rates were observed among preflexion larvae: the reduction in specific growth rate between embryos and free-swimming larvae was greater than expected based on body size differences. Growth reductions in the preflexion larvae appear to be associated with increased metabolic rates and the transition from endogenous to exogenous feeding. In future studies, experiments should be integrated across life transitions to more clearly define intrinsic ontogenetic and size-dependent growth patterns because these are critical for evaluations of spatial and temporal variation in habitat quality.
C1 [Hurst, Thomas P.; Laurel, Benjamin J.] Oregon State Univ, Hatfield Marine Sci Ctr, NOAA, Natl Marine Fisheries Serv,Alaska Fisheries Sci C, Newport, OR 97365 USA.
[Ciannelli, Lorenzo] Oregon State Univ, Coll Atmospher & Oceanog Sci, Corvallis, OR 97331 USA.
RP Hurst, TP (reprint author), Oregon State Univ, Hatfield Marine Sci Ctr, NOAA, Natl Marine Fisheries Serv,Alaska Fisheries Sci C, Newport, OR 97365 USA.
EM thomas.hurst@noaa.gov
RI Hurst, Thomas/N-1401-2013
FU North Pacific Research Board [R0605]
FX We thank T. Tripp, M. Spencer, and B. Knoth for assistance with fish
collection and shipping. Staff and students in the Fisheries Behavioral
Ecology Program, including L. Copeman, S. Haines, M. Ottmar, P. Iseri,
A. Colton, L. Logers, E. Seale, and J. Scheingross assisted with various
laboratory experiments. S. Munch, L. Tomaro, A. Stoner, and three
anonymous reviewers provided helpful comments on earlier versions of
this manuscript. This research was supported in part by a grant from the
North Pacific Research Board (no. R0605). This is publication no. 248 of
the North Pacific Research Board.
NR 48
TC 22
Z9 23
U1 1
U2 7
PU NATL MARINE FISHERIES SERVICE SCIENTIFIC PUBL OFFICE
PI SEATTLE
PA 7600 SAND POINT WAY NE BIN C15700, SEATTLE, WA 98115 USA
SN 0090-0656
J9 FISH B-NOAA
JI Fish. Bull.
PD OCT
PY 2010
VL 108
IS 4
BP 382
EP 392
PG 11
WC Fisheries
SC Fisheries
GA 676XS
UT WOS:000283953000002
ER
PT J
AU DeCelles, GR
Cadrin, SX
AF DeCelles, Gregory R.
Cadrin, Steven X.
TI Movement patterns of winter flounder (Pseudopleuronectes americanus) in
the southern Gulf of Maine: observations with the use of passive
acoustic telemetry
SO FISHERY BULLETIN
LA English
DT Article
ID SEASONAL MOVEMENTS; FISH; ESTUARINE; HABITATS; DYNAMICS; LARVAE;
POPULATION; RESPONSES; STORAGE; GROWTH
AB Despite its recreational and commercial importance, the movement patterns and spawning habitats of winter flounder (Pseudopleuronectes americanus) in the Gulf of Maine are poorly understood. To address these uncertainties, 72 adult winter flounder (27-48 cm) were fitted with acoustic transmitters and tracked by passive telemetry in the southern Gulf of Maine between 2007 and 2009. Two sympatric contingents of adult winter flounder were observed, which exhibited divergent spawning migrations. One contingent remained in coastal waters during the spawning season, while a smaller contingent of winter flounder was observed migrating to estuarine habitats. Estuarine residence times were highly variable, and ranged from 2 to 91 days (mean=28 days). Flounder were nearly absent from the estuary during the fall and winter months and were most abundant in the estuary from late spring to early summer. The observed seasonal movements appeared to be strongly related to water temperature. This is the first study to investigate the seasonal distribution, migration, and spawning behavior of adult winter flounder in the Gulf of Maine by using passive acoustic telemetry. This approach offered valuable insight into the life history of this species in nearshore and estuarine habitats and improved the information available for the conservation and management of this species.
C1 [DeCelles, Gregory R.] Natl Ocean & Atmospher Adm, Fairhaven, MA 02719 USA.
Univ Massachusetts, Cooperat Marine Educ & Res Program, Sch Marine Sci & Technol, Fairhaven, MA 02719 USA.
RP DeCelles, GR (reprint author), Natl Ocean & Atmospher Adm, 200 Mill Rd,Suite 325, Fairhaven, MA 02719 USA.
EM gdecelles@umassd.edu
FU Massachusetts Marine Fisheries Institute
FX The Massachusetts Marine Fisheries Institute provided the funding for
this research. T. Grothues and two anonymous reviewers provided valuable
comments on this manuscript. We would also like to thank M. Mather, G.
Skomal, and G. Cowles for their guidance and advice during this
experiment. We thank J. Manderson and M. Armstrong for allowing us to
borrow acoustic receivers. We would also like to thank V. Malkoski, V.
Manfredi, P. Milligan, B. Courchene, H. Bourbon, C. Sarro, and M. Marino
for assistance in the field. Finally, we would like to thank the dozens
of other people whose help at sea made this project possible.
NR 31
TC 22
Z9 22
U1 0
U2 20
PU NATL MARINE FISHERIES SERVICE SCIENTIFIC PUBL OFFICE
PI SEATTLE
PA 7600 SAND POINT WAY NE BIN C15700, SEATTLE, WA 98115 USA
SN 0090-0656
J9 FISH B-NOAA
JI Fish. Bull.
PD OCT
PY 2010
VL 108
IS 4
BP 408
EP 419
PG 12
WC Fisheries
SC Fisheries
GA 676XS
UT WOS:000283953000004
ER
PT J
AU Laidig, TE
AF Laidig, Thomas E.
TI Influence of ocean conditions on the timing of early life history events
for blue rockfish (Sebastes mystinus) off California
SO FISHERY BULLETIN
LA English
DT Article
ID CORAL-REEF FISHES; NORTHERN CALIFORNIA; BLACK ROCKFISH; INTERANNUAL
VARIATION; JUVENILE ROCKFISH; MARINE FISH; RECRUITMENT; GROWTH; SPP.;
VARIABILITY
AB Settled juvenile blue rockfish (Sebastes mystinus) were collected from two kelp beds approximately 335 km apart off Mendocino in northern California and Monterey in central California. A total of 112 rockfish were collected from both sites over 5 years (1993, 1994, 2001, 2002, and 2003). Total age, settlement date, age at settlement, and birth date were determined from otolith microstructure. Fish off Mendocino settled mostly in June and fish off Monterey settled mostly in May (average difference in settlement=23 days). Although the difference in the timing of settlement followed this same pattern for both areas over the five years, settlement occurred later in 2002 and 2003 than in the prior years of sampling. The difference in the timing of settlement was due primarily to differences in birth dates for the two areas. The time of settlement was positively related to upwelling and negatively related to sea level anomaly for most of the months before settlement. Knowledge of the timing of settlement has implications for design and placement of marine protected areas because protection of nursery grounds is frequently a major objective of these protected areas. The timing of settlement is also an important consideration in the planning of surveys of early recruits because mistimed surveys (caused by latitudinal differences in the timing of settlement) could produce biased estimates.
C1 Natl Ocean & Atmospher Adm, Natl Marine Fisheries Serv, SW Fisheries Sci Ctr, Fisheries Ecol Div, Santa Cruz, CA 95060 USA.
RP Laidig, TE (reprint author), Natl Ocean & Atmospher Adm, Natl Marine Fisheries Serv, SW Fisheries Sci Ctr, Fisheries Ecol Div, 110 Shaffer Rd, Santa Cruz, CA 95060 USA.
EM tom.laidig@noaa.gov
NR 34
TC 9
Z9 9
U1 0
U2 8
PU NATL MARINE FISHERIES SERVICE SCIENTIFIC PUBL OFFICE
PI SEATTLE
PA 7600 SAND POINT WAY NE BIN C15700, SEATTLE, WA 98115 USA
SN 0090-0656
J9 FISH B-NOAA
JI Fish. Bull.
PD OCT
PY 2010
VL 108
IS 4
BP 442
EP 449
PG 8
WC Fisheries
SC Fisheries
GA 676XS
UT WOS:000283953000007
ER
PT J
AU Hart, TD
Clemons, JER
Wakefield, WW
Heppell, SS
AF Hart, Ted D.
Clemons, Julia E. R.
Wakefield, W. Waldo
Heppell, Selina S.
TI Day and night abundance, distribution, and activity patterns of demersal
fishes on Heceta Bank, Oregon
SO FISHERY BULLETIN
LA English
DT Article
ID REEF FISHES; HABITAT ASSOCIATIONS; PHOTIC ENVIRONMENT;
CONTINENTAL-SHELF; DIEL VARIATION; SILVER HAKE; DEEP-REEF; SEBASTES;
TRAWL; CATCHABILITY
AB Most shallow-dwelling tropical marine fishes exhibit different activity patterns during the day and night but show similar transition behavior among habitat sites despite the dissimilar assemblages of the species. However, changes in species abundance, distribution, and activity patterns have only rarely been examined in temperate deepwater habitats during the day and night, where day-to-night differences in light intensity are extremely slight. Direct-observation surveys were conducted over several depths and habitat types on Heceta Bank, the largest rocky bank off the Oregon coast. Day and night fish community composition, relative density, and activity levels were compared by using videotape footage from a remotely operated vehicle (ROV) operated along paired transects. Habitat-specific abundance and activity were determined for 31 taxa or groups. General patterns observed were similar to shallow temperate day and night studies, with an overall increase in the abundance and activity of fishes during the day than at night, particularly in shallower cobble, boulder, and rock ridge habitats. Smaller schooling rockfishes (Sebastes spp.) were more abundant and active in day than in night transects, and sharp-chin (S. zacentrus) and harlequin (S. variegatus) rockfish were significantly more abundant in night transects. Most taxa, however, did not exhibit distinct diurnal or nocturnal activity patterns. Rosethorn rockfish (S. helvomaculatus) and hagfishes (Eptatretus spp.) showed the clearest diurnal and nocturnal activity patterns, respectively. Because day and night distributions and activity patterns in demersal fishes are likely to influence both catchability and observability in bottom trawl and direct-count in situ surveys, the patterns observed in the current study should be considered for survey design and interpretation.
C1 [Clemons, Julia E. R.; Wakefield, W. Waldo] Natl Ocean & Atmospher Adm, Natl Marine Fisheries Serv, NW Fisheries Sci Ctr, Fishery Resource Anal & Monitoring Div, Newport, OR 97365 USA.
[Hart, Ted D.; Heppell, Selina S.] Oregon State Univ, Dept Fisheries & Wildlife, Corvallis, OR 97331 USA.
RP Clemons, JER (reprint author), Natl Ocean & Atmospher Adm, Natl Marine Fisheries Serv, NW Fisheries Sci Ctr, Fishery Resource Anal & Monitoring Div, 2032 SE OSU Dr, Newport, OR 97365 USA.
EM Julia.Clemons@noaa.gov
RI Bizzarro, Joseph/A-2988-2012
FU West Coast and Polar Regions Undersea Research Center of the National
Oceanographic and Atmospheric Administration (NOAA); Northwest and
Southwest Fisheries Science Centers; NOAA's Pacific Marine Environmental
Laboratory; Cooperative Institute for Marine Resources Studies at Oregon
State University; Oregon Agricultural Experiment Station [ORE00102]; H.
Richard Carlson Scholarship; Collaborative Marine Fisheries Fellowship;
Oregon State University
FX We would especially like to thank the following colleagues who
contributed to this study: B. Barss, B. Embley, G. Hendler, M. Hixon, D.
Markle, B. McCune, S. Merle, B. Tissot, M. Yoklavich, and K. York. A.
Whitmire and T. Cowles generously contributed information on ambient
light levels. L. Britt, C. Whitmire, and L. Ciannelli provided
constructive reviews of the manuscript. This portion of the Heceta Bank
project was funded by the West Coast and Polar Regions Undersea Research
Center of the National Oceanographic and Atmospheric Administration's
(NOAA) National Undersea Research Program, the Northwest and Southwest
Fisheries Science Centers, NOAA's Pacific Marine Environmental
Laboratory, and the Cooperative Institute for Marine Resources Studies
at Oregon State University. We would like to thank the professional
personnel who operated the ROV ROPOS and the NOAA RV Ronald Brown. T.
Hart was supported through the Oregon Agricultural Experiment Station
project ORE00102, the H. Richard Carlson Scholarship, the Collaborative
Marine Fisheries Fellowship and the Bill Wick Award through Oregon State
University.
NR 41
TC 4
Z9 4
U1 2
U2 12
PU NATL MARINE FISHERIES SERVICE SCIENTIFIC PUBL OFFICE
PI SEATTLE
PA 7600 SAND POINT WAY NE BIN C15700, SEATTLE, WA 98115 USA
SN 0090-0656
J9 FISH B-NOAA
JI Fish. Bull.
PD OCT
PY 2010
VL 108
IS 4
BP 466
EP 477
PG 12
WC Fisheries
SC Fisheries
GA 676XS
UT WOS:000283953000009
ER
PT J
AU Kim, JK
Watson, W
Hyde, J
Lo, N
Kim, JY
Kim, S
Kim, YS
AF Kim, Jin Koo
Watson, William
Hyde, John
Lo, Nancy
Kim, Jin Young
Kim, Sung
Kim, Young Seop
TI Molecular identification of Ammodytes (PISCES, Ammodytidae) larvae, with
ontogenetic evidence on separating populations
SO GENES & GENOMICS
LA English
DT Article
DE Ammodytes personatus; Ammodytes hexapterus; COI; Identification; Larval
development
ID LANCE GENUS AMMODYTES; SAND-LANCE; GEOGRAPHIC POPULATIONS; DNA; JAPAN;
KOREA; REGION; EGGS
AB A total of ten larval Ammodytes were collected from the Yellow (5 specimens) and Bering Seas (5), and a 638 base pair sequence from their mitochondrial DNA COI genes was analyzed for species identification. Sequences were compared with those of adult Ammodytes personatus from the East (4), the Yellow (2) and the East China Seas (2), and Japan (3). Average genetic distance was 0.064 between the Yellow Sea larvae and the Bering Sea larvae, but was 0.0043 between the Yellow Sea larvae and all the adult A. personatus except two individuals from the East Sea. NJ-tree showed that five Yellow Sea larvae were closely clustered with adult A. personatus, except for two individuals. The five Bering Sea larvae were located distantly from adult A. personatus, and are thought to be A. hexapterus. We found morphological differences among two populations of A. personatus larvae and A. hexapterus larvae in morphometric characters and pigmentation. Our results indicated that the East Sea population of A. personatus is closer to A. hexapterus than to the Yellow Sea population of A. personatus, suggesting the East Sea population may be part of separate species.
C1 [Kim, Young Seop] Natl Fisheries Res & Dev Inst, Res & Dev Planning Dept, Pusan 619902, South Korea.
[Kim, Jin Koo] Pukyong Natl Univ, Dept Marine Biol, Pusan 608737, South Korea.
[Watson, William; Hyde, John; Lo, Nancy] NOAA, SW Fisheries Sci Ctr, Natl Marine Fisheries Serv, La Jolla, CA 92037 USA.
[Kim, Jin Young] Natl Fisheries Res & Dev Inst, SW Sea Fisheries Res Inst, Yosu 556823, South Korea.
[Kim, Sung] Korea Ocean Res & Dev Inst, Marine Living Resources Res Div, Ansan 425600, South Korea.
RP Kim, YS (reprint author), Natl Fisheries Res & Dev Inst, Res & Dev Planning Dept, Pusan 619902, South Korea.
EM kys0321@nrfdi.go.kr
FU NFRDI; NOAA; Pukyong National University
FX We sincerely thank Dr. Y Kai (Kyoto University) for loan samples. We are
also grateful to the anonymous reviewers for their valuable comments and
advice. This work was supported by "US-Korea Bilateral Program between
NFRDI and NOAA" and "Pukyong National University". These are
contribution number RP-2010-FR-0117 and PE98474.
NR 41
TC 9
Z9 10
U1 1
U2 6
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1976-9571
EI 2092-9293
J9 GENES GENOM
JI Genes Genom.
PD OCT
PY 2010
VL 32
IS 5
BP 437
EP 445
DI 10.1007/s13258-010-0017-6
PG 9
WC Biochemistry & Molecular Biology; Biotechnology & Applied Microbiology;
Genetics & Heredity
SC Biochemistry & Molecular Biology; Biotechnology & Applied Microbiology;
Genetics & Heredity
GA 694LN
UT WOS:000285299700007
ER
PT J
AU Pendall, E
Schwendenmann, L
Rahn, T
Miller, JB
Tans, PP
White, JWC
AF Pendall, E.
Schwendenmann, L.
Rahn, T.
Miller, J. B.
Tans, P. P.
White, J. W. C.
TI Land use and season affect fluxes of CO2, CH4, CO, N2O, H-2 and isotopic
source signatures in Panama: evidence from nocturnal boundary layer
profiles
SO GLOBAL CHANGE BIOLOGY
LA English
DT Review
DE carbon cycle; C-3; C-4; 13C; greenhouse gas; 18O; Pasture; Plantation;
soil respiration; tropical Rainforest
ID AMAZONIAN RAIN-FOREST; NET ECOSYSTEM EXCHANGE; AIR SAMPLING NETWORK;
SOIL ORGANIC-CARBON; TROPICAL FOREST; MOLECULAR-HYDROGEN; TEMPORAL
VARIATION; EASTERN AMAZONIA; NITROUS-OXIDE; RESPIRED CO2
AB Conversion of tropical rainforests to pastures and plantations is associated with changes in soil properties and biogeochemical cycling, with implications for carbon cycling and trace gas fluxes. The stable isotopic composition of ecosystem respiration (delta 13C(R) and delta 18O(R)) is used in inversion models to quantify regional patterns of CO2 sources and sinks, but models are limited by sparse measurements in tropical regions. We measured soil respiration rates, concentrations of CO2, CH4, CO, N2O and H-2 and the isotopic composition of CO2, CH4 and H-2 at four heights in the nocturnal boundary layer (NBL) above three common land-use types in central Panama, during dry and rainy seasons. Soil respiration rates were lowest in Plantation (average 3.4 mu mol m-2 s-1), highest in Pasture (8.3 mu mol m-2 s-1) and intermediate in Rainforest (5.2 mu mol m-2 s-1). delta 13C(R) closely reflected land use and increased during the dry season where C-3 vegetation was present. delta 18O(R) did not differ by land use but was lower during the rainy than the dry season. CO2 was correlated with other species in approximately half of the NBL profiles, allowing us to estimate trace gas fluxes that were generally within the range of literature values. The Rainforest soil was a sink for CH4 but emissions were observed in Pasture and Plantation, especially during the wet season. N2O emissions were higher in Pasture and Plantation than Rainforest, contrary to expectations. Soil H-2 uptake was highest in Rainforest and was not observable in Pasture and Plantation during the wet season. We observed soil CO uptake during the dry season and emissions during the wet season across land-use types. This study demonstrated that strong impacts of land-use change on soil-atmosphere trace gas exchange can be detected in the NBL, and provides useful observational constraints for top-down and bottom-up biogeochemistry models.
C1 [Pendall, E.] Univ Wyoming, Dept Bot, Laramie, WY 82071 USA.
[Pendall, E.] Univ Wyoming, Program Ecol, Laramie, WY 82071 USA.
[Schwendenmann, L.] Univ Gottingen, Gottingen, Germany.
[Rahn, T.] Los Alamos Natl Lab, Los Alamos, NM USA.
[Miller, J. B.; Tans, P. P.] NOAA, Earth Syst Res Lab, Boulder, CO 80303 USA.
[Miller, J. B.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[White, J. W. C.] Univ Colorado, Dept Geol, Boulder, CO 80309 USA.
[White, J. W. C.] Univ Colorado, Inst Arct & Alpine Ecol, Boulder, CO 80309 USA.
RP Pendall, E (reprint author), Univ Wyoming, Dept Bot, Laramie, WY 82071 USA.
EM Pendall@uwyo.edu
RI White, James/A-7845-2009; Rahn, Thom/C-5211-2012;
OI White, James/0000-0001-6041-4684; Pendall, Elise/0000-0002-1651-8969;
Rahn, Thomas/0000-0001-8634-1348
FU USDA; Smithsonian Tropical Research Institute; Wyoming NASA Space
Consortium (NASA) [NGT-40102]; Wyoming NASA EPSCoR (NASA) [NCC5-578]
FX This project benefited from field assistance from Marco Valdez and
laboratory assistance from P. Lang and V. Moore. We thank C. Potvin, R.
Stallard and STRI for providing access to study sites. Partial funding
for the research was provided by USDA-CSREES Soil Processes Program,
Smithsonian Tropical Research Institute, Wyoming NASA Space Grant
Consortium (NASA Grant #NGT-40102), and Wyoming NASA EPSCoR (NASA Grant
#NCC5-578).
NR 114
TC 11
Z9 12
U1 4
U2 51
PU WILEY-BLACKWELL
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 1354-1013
J9 GLOBAL CHANGE BIOL
JI Glob. Change Biol.
PD OCT
PY 2010
VL 16
IS 10
BP 2721
EP 2736
DI 10.1111/j.1365-2486.2010.02199.x
PG 16
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA 648FV
UT WOS:000281676700008
ER
PT J
AU Hoffman, MJ
Greybush, SJ
Wilson, RJ
Gyarmati, G
Hoffman, RN
Kalnay, E
Ide, K
Kostelich, EJ
Miyoshi, T
Szunyogh, I
AF Hoffman, Matthew J.
Greybush, Steven J.
Wilson, R. John
Gyarmati, Gyorgyi
Hoffman, Ross N.
Kalnay, Eugenia
Ide, Kayo
Kostelich, Eric J.
Miyoshi, Takemasa
Szunyogh, Istvan
TI An ensemble Kalman filter data assimilation system for the martian
atmosphere: Implementation and simulation experiments
SO ICARUS
LA English
DT Article
DE Mars; Mars, Atmosphere; Atmospheres, Dynamics; Meteorology
ID GENERAL-CIRCULATION MODEL; SPECTROMETER TES OBSERVATIONS; METEOROLOGICAL
DATA; GLOBAL-MODEL; MARS; DUST; AEROBRAKING; SCHEME; VARIABILITY; CYCLE
AB The local ensemble transform Kalman filter (LETKF) is applied to the GFDL Mars general circulation model (MGCM) to demonstrate the potential benefit of an advanced data assimilation method. In perfect model (aka identical twin) experiments, simulated observations are used to assess the performance of the LETKF-MGCM system and to determine the dependence of the assimilation on observational data coverage. Temperature retrievals are simulated at locations that mirror the spatial distribution of the Thermal Emission Spectrometer (TES) retrievals from the Mars Global Surveyor (MGS). The LETKF converges quickly and substantially reduces the analysis and subsequent forecast errors in both temperature and velocity fields, even though only temperature observations are assimilated. The LETKF is also found to accurately estimate the magnitude of forecast uncertainties, notably those associated with the phase and amplitude of baroclinic waves along the boundary of the polar ice cap during Northern Hemisphere winter. (C) 2010 Elsevier Inc. All rights reserved.
C1 [Hoffman, Matthew J.] Johns Hopkins Univ, Dept Earth & Planetary Sci, Baltimore, MD 21218 USA.
[Greybush, Steven J.; Miyoshi, Takemasa] Univ Maryland, Dept Atmospher & Ocean Sci, College Pk, MD 20742 USA.
[Wilson, R. John] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08542 USA.
[Gyarmati, Gyorgyi; Szunyogh, Istvan] Texas A&M Univ, Dept Atmospher Sci, College Stn, TX 77843 USA.
[Hoffman, Ross N.] Atmospher & Environm Res Inc, Lexington, MA 02421 USA.
[Kalnay, Eugenia] Univ Maryland, Inst Phys Sci & Technol, Earth Syst Sci Interdisciplinary Ctr, Dept Atmospher & Ocean Sci, College Pk, MD 20742 USA.
[Ide, Kayo] Univ Maryland, Inst Phys Sci & Technol, Earth Syst Sci Interdisciplinary Ctr, Dept Atmospher & Ocean Sci,Ctr Sci Computat & Mat, College Pk, MD 20742 USA.
[Kostelich, Eric J.] Arizona State Univ, Dept Math & Stat, Tempe, AZ 85287 USA.
RP Hoffman, MJ (reprint author), Johns Hopkins Univ, Dept Earth & Planetary Sci, 301 Olin Hall,3400 N Charles St, Baltimore, MD 21218 USA.
EM mjhoffman@jhu.edu
RI Kalnay, Eugenia/F-4393-2010; Ide, Kayo/F-8443-2010; Miyoshi,
Takemasa/C-2768-2009; Szunyogh, Istvan/G-9248-2012;
OI Miyoshi, Takemasa/0000-0003-3160-2525; Kalnay,
Eugenia/0000-0002-9984-9906
FU NASA [NNX07AN97G, NNX07AV45G]
FX This work was supported by the NASA Mars Data Analysis Program (MDAP)
Grant NNX07AN97G and the NASA Mars Fundamental Research Program (MFRP)
Grant NNX07AV45G.
NR 43
TC 12
Z9 12
U1 2
U2 6
PU ACADEMIC PRESS INC ELSEVIER SCIENCE
PI SAN DIEGO
PA 525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA
SN 0019-1035
EI 1090-2643
J9 ICARUS
JI Icarus
PD OCT
PY 2010
VL 209
IS 2
BP 470
EP 481
DI 10.1016/j.icarus.2010.03.034
PG 12
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA 654VL
UT WOS:000282199000015
ER
PT J
AU Judkins, HL
Vecchione, M
Roper, CFE
Torres, J
AF Judkins, Heather L.
Vecchione, Michael
Roper, Clyde F. E.
Torres, Joseph
TI Cephalopod species richness in the wider Caribbean region
SO ICES JOURNAL OF MARINE SCIENCE
LA English
DT Article; Proceedings Paper
CT Symposium of the Cephalopod-International-Advisory-Council
CY SEP, 2009
CL Spanish Natl Res Council, Vigo, SPAIN
SP Cephalopod Int Advisory Council
HO Spanish Natl Res Council
DE cephalopod distribution; species richness; wider Caribbean region
ID LATITUDINAL DIVERSITY GRADIENTS; ATLANTIC-OCEAN; DEEP-SEA; MARINE
MOLLUSKS; RAPOPORTS RULE; NORTH-ATLANTIC; PATTERNS; NEMATODES; RANGE;
SIZE
AB The cephalopods of the wider Caribbean region (western central Atlantic) were examined in terms of distribution and ecological importance. In all, 4190 preserved cephalopod specimens were identified and catalogued to produce regional maps of cephalopod distribution within the wider Caribbean. Regional species richness was examined with respect to Rapoport's rule (RR) and to determine possible cephalopod hotspots in the region. Rarefaction curves were used to normalize the samples of various size collected throughout the wider Caribbean. Cephalopods of the wider Caribbean within latitudinal bands from 8 to 308N do not support RR because they exhibit increasing species richness with increasing latitude. Eight subareas were chosen to compare species richness. Regionally, species richness appears to be patchy, with cephalopods concentrated more off the eastern Florida coast. There is a need for increased sampling throughout the wider Caribbean. Areas were lacking in samples, especially the central and southeastern parts of the region. There is a need to explore the systematics, life histories, and distribution patterns for this group of organisms in future.
C1 [Judkins, Heather L.; Torres, Joseph] Univ S Florida, Coll Marine Sci, St Petersburg, FL 33701 USA.
[Vecchione, Michael] Smithsonian Inst, Natl Museum Nat Hist, NMFS Natl Systemat Lab, Washington, DC 20013 USA.
RP Judkins, HL (reprint author), Univ S Florida, Coll Marine Sci, St Petersburg, FL 33701 USA.
EM judkins@mail.usf.edu
NR 48
TC 0
Z9 0
U1 4
U2 15
PU OXFORD UNIV PRESS
PI OXFORD
PA GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND
SN 1054-3139
J9 ICES J MAR SCI
JI ICES J. Mar. Sci.
PD OCT
PY 2010
VL 67
IS 7
BP 1392
EP 1400
DI 10.1093/icesjms/fsq092
PG 9
WC Fisheries; Marine & Freshwater Biology; Oceanography
SC Fisheries; Marine & Freshwater Biology; Oceanography
GA 648UH
UT WOS:000281719300010
ER
PT J
AU Shea, EK
Vecchione, M
AF Shea, Elizabeth K.
Vecchione, Michael
TI Ontogenic changes in diel vertical migration patterns compared with
known allometric changes in three mesopelagic squid species suggest an
expanded definition of a paralarva
SO ICES JOURNAL OF MARINE SCIENCE
LA English
DT Article
DE allometry; diel vertical migration; oegopsid; paralarva; squid
ID NORTH-ATLANTIC; PELAGIC CEPHALOPODS; DEGREES W; DEGREES N; BIOLOGY; LIFE
AB Planktonic and newly hatched cephalopods are routinely called paralarvae. Currently, the onset of diel vertical migration (DVM) marks the end of the paralarval phase, although changes in ontogenic growth trajectories may also be used. Patterns of DVM are reported for the first time for three poorly understood mesopelagic squid species. Discrete-depth samples taken during the Amsterdam Mid North Atlantic Plankton Expeditions (AMNAPE) of 1980-1983 are used to examine the timing of ecological and morphological changes in Chtenopteryx sicula, Mastigoteuthis magna, and Brachioteuthis sp. 3. DVM patterns are species-specific, and ontogenic changes in DVM coincide with allometric changes in the arm, fin, and funnel characters of C. sicula at 7 mm mantle length. Mastigoteuthis magna is not concentrated in the upper 250 m of the water column during the day, and no clear DVM pattern is found in Brachioteuthis sp. 3, meaning that the endpoint of the paralarval phase cannot be defined ecologically in these species. Other ecological transformations, e. g. changes in prey-capture ability, are therefore explored as alternatives to DVM. The pad-shaped club and long neck are proposed as visual markers of the end of the paralarval phase of C. sicula and Brachioteuthis sp. 3, respectively.
C1 [Shea, Elizabeth K.] Delaware Museum Nat Hist, Wilmington, DE 19807 USA.
[Vecchione, Michael] Natl Museum Nat Hist, Natl Marine Fisheries Serv, Natl Systemat Lab, Washington, DC 20560 USA.
RP Shea, EK (reprint author), Delaware Museum Nat Hist, 4840 Kennett Pike, Wilmington, DE 19807 USA.
EM eshea@delmnh.org
NR 51
TC 9
Z9 9
U1 0
U2 6
PU OXFORD UNIV PRESS
PI OXFORD
PA GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND
SN 1054-3139
J9 ICES J MAR SCI
JI ICES J. Mar. Sci.
PD OCT
PY 2010
VL 67
IS 7
BP 1436
EP 1443
DI 10.1093/icesjms/fsq104
PG 8
WC Fisheries; Marine & Freshwater Biology; Oceanography
SC Fisheries; Marine & Freshwater Biology; Oceanography
GA 648UH
UT WOS:000281719300016
ER
PT J
AU El-Nimri, SF
Jones, WL
Uhlhorn, E
Ruf, C
Johnson, J
Black, P
AF El-Nimri, Salem Fawwaz
Jones, W. Linwood
Uhlhorn, Eric
Ruf, Christopher
Johnson, James
Black, Peter
TI An Improved C-Band Ocean Surface Emissivity Model at Hurricane-Force
Wind Speeds Over a Wide Range of Earth Incidence Angles
SO IEEE GEOSCIENCE AND REMOTE SENSING LETTERS
LA English
DT Article
DE Hurricane Imaging Radiometer (HIRAD); hurricane winds; ocean surface
emissivity; radiometry; Stepped-Frequency Microwave Radiometer (SFMR)
ID TEMPERATURE
AB An improved microwave radiometric ocean surface emissivity model has been developed to support forward radiative transfer modeling of brightness temperature and geophysical retrieval algorithms for the next-generation airborne Hurricane Imaging Radiometer instrument. This physically based C-band emissivity model extends current model capabilities to hurricane-force wind speeds over a wide range of incidence angles. It was primarily developed using brightness temperature observations during hurricanes with coincident high-quality surface-truth wind speeds, which were obtained using the airborne Stepped-Frequency Microwave Radiometer. Also, other ocean emissivity models available through the published literature and the spaceborne WindSat radiometer measurements were used.
C1 [El-Nimri, Salem Fawwaz; Jones, W. Linwood; Johnson, James] Univ Cent Florida, Cent Florida Remote Sensing Lab, Orlando, FL 32816 USA.
[Uhlhorn, Eric] Natl Ocean & Atmospher Adm, Hurricane Res Div, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
[Ruf, Christopher] Univ Michigan, Ann Arbor, MI 48109 USA.
[Black, Peter] SAIC Inc, Monterey, CA 93940 USA.
[Black, Peter] USN, Marine Meteorol Div, Res Lab, Monterey, CA 93940 USA.
RP El-Nimri, SF (reprint author), Univ Cent Florida, Cent Florida Remote Sensing Lab, Orlando, FL 32816 USA.
EM selnimri@mail.ucf.edu; ljones@ucf.edu; eric.uhlhorn@noaa.gov;
cruf@umich.edu; jamesj@mail.ucf.edu; peter.black@nrlmry.navy.mil
RI Ruf, Christopher/I-9463-2012; Uhlhorn, Eric/B-1336-2014
OI Uhlhorn, Eric/0000-0002-4759-5342
FU Von Braun Center for Science and Innovation, Inc., Huntsville, AL
[SUB2006-226]; Marshall Space Flight Center, National Aeronautics and
Space Administration; National Oceanic and Atmospheric Administration in
the development of the Hurricane Imaging Radiometer instrument
FX Manuscript received April 15, 2009; revised July 21, 2009 and November
16, 2009. Date of publication April 12, 2010; date of current version
October 13, 2010. This work was supported in part by the Von Braun
Center for Science and Innovation, Inc., Huntsville, AL, under
Subcontract SUB2006-226, by the Marshall Space Flight Center, National
Aeronautics and Space Administration, and by the National Oceanic and
Atmospheric Administration in the development of the Hurricane Imaging
Radiometer instrument.
NR 15
TC 13
Z9 13
U1 0
U2 5
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 1545-598X
EI 1558-0571
J9 IEEE GEOSCI REMOTE S
JI IEEE Geosci. Remote Sens. Lett.
PD OCT
PY 2010
VL 7
IS 4
BP 641
EP 645
DI 10.1109/LGRS.2010.2043814
PG 5
WC Geochemistry & Geophysics; Engineering, Electrical & Electronic; Remote
Sensing; Imaging Science & Photographic Technology
SC Geochemistry & Geophysics; Engineering; Remote Sensing; Imaging Science
& Photographic Technology
GA 670SD
UT WOS:000283446700005
ER
PT J
AU Lavery, AC
Chu, DZ
Moum, JN
AF Lavery, Andone C.
Chu, Dezhang
Moum, James N.
TI Observations of Broadband Acoustic Backscattering From Nonlinear
Internal Waves: Assessing the Contribution From Microstructure
SO IEEE JOURNAL OF OCEANIC ENGINEERING
LA English
DT Article; Proceedings Paper
CT Shallow Water (SW06) Experiment
CY 2006
CL NJ
DE Acoustic scattering; broadband; nonlinear internal waves; turbulent
oceanic microstructure; zooplankton
ID SOLITARY WAVES; ZOOPLANKTON GROUPS; CONTINENTAL-SHELF; SOUND-SCATTERING;
ECHO-SOUNDER; TURBULENCE; FREQUENCY; ENERGY; DISSIPATION; CALIBRATION
AB In this paper, measurements of high-frequency broadband (160-590 kHz) acoustic backscattering from surface trapped nonlinear internal waves of depression are presented. These waves are ideal for assessing the contribution from oceanic microstructure to scattering as they are intensely turbulent. Almost coincident direct microstructure measurements were performed and zooplankton community structure was characterized using depth-resolved net sampling techniques. The contribution to scattering from microstructure can be difficult to distinguish from the contribution to scattering from zooplankton using a single narrowband frequency as microstructure and zooplankton are often colocated and can have similar scattering levels over a range of frequencies. Yet their spectra are distinct over a sufficiently broad frequency range, allowing broadband backscattering measurements to reduce the ambiguities typically associated with the interpretation of narrowband measurements. In addition, pulse compression signal processing techniques result in very high-resolution images, allowing physical processes that are otherwise hard to resolve to be imaged, such as Kelvin-Helmholtz shear instabilities. In this study, high-resolution acoustic observations of multiple nonlinear internal waves are presented and regions with distinct scattering spectra are identified. Spectra that decrease in level across the available frequency band were highly correlated to regions of intense turbulence and high stratification, and to Kevin-Helmholtz shear instabilities in particular. Spectra that increase in level across the available frequency band were consistent with scattering dominated by small zooplankton. Simple inversions for relevant microstructure parameters are presented. Limitations of, and improvements to, the broadband system and techniques utilized in this study are discussed.
C1 [Lavery, Andone C.] Woods Hole Oceanog Inst, Dept Appl Ocean Phys & Engn, Woods Hole, MA 02543 USA.
[Chu, Dezhang] NW Fisheries Sci Ctr, Seattle, WA 98112 USA.
[Moum, James N.] Oregon State Univ, Coll Ocean & Atmospher Sci, Corvallis, OR 97331 USA.
RP Lavery, AC (reprint author), Woods Hole Oceanog Inst, Dept Appl Ocean Phys & Engn, Woods Hole, MA 02543 USA.
EM alavery@whoi.edu; Dezhang.Chu@noaa.gov; moum@coas.oregonstate.edu
RI Moum, James/A-1880-2012
NR 38
TC 7
Z9 7
U1 0
U2 4
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 0364-9059
J9 IEEE J OCEANIC ENG
JI IEEE J. Ocean. Eng.
PD OCT
PY 2010
VL 35
IS 4
BP 695
EP 709
DI 10.1109/JOE.2010.2047814
PG 15
WC Engineering, Civil; Engineering, Ocean; Engineering, Electrical &
Electronic; Oceanography
SC Engineering; Oceanography
GA 688LP
UT WOS:000284851100004
ER
PT J
AU Schmidt, V
Weber, TC
Wiley, DN
Johnson, MP
AF Schmidt, Val
Weber, Thomas C.
Wiley, David N.
Johnson, Mark P.
TI Underwater Tracking of Humpback Whales (Megaptera Novaeangliae) With
High-Frequency Pingers and Acoustic Recording Tags
SO IEEE JOURNAL OF OCEANIC ENGINEERING
LA English
DT Article
DE acoustic positioning; long-baseline (LBL) positioning; marine mammal;
whale tracking
ID NORTHERN ELEPHANT SEALS; PHYSETER-MACROCEPHALUS; DIVING BEHAVIOR; MARINE
MAMMALS; SOUND; ARRAY; LOCALIZATION; HYDROPHONE; CLICKS; MODEL
AB A long-baseline (LBL) acoustic system has been developed for the tracking of humpback whales (Megaptera novaeangliae) that have been tagged with digital acoustic recording devices (DTAGs), providing quantitative observations of submerged whale behavior during bubble net feeding. The system includes three high-frequency acoustic sources deployed from small boats that follow the whale after the animal has been tagged. Integrated global positioning systems (GPSs) provide positioning and synchronized operation of the sources. Time-encoded acoustic signals from the sources are recorded along with whale vocalizations and ambient noise on the whale tag. Time-of-flight measurements, as measured by the tag acoustic data, are converted to range from the whale to each source with a measured sound-speed profile. A nonlinear least squares solution is then solved for the whale's position with a nominal positional fix rate of once per second. The system is demonstrated with data collected from a tagged animal in summer 2007. Dead-reckoned track generation methods commonly used in previous studies are shown to capture the qualitative nature of the whale track, albeit with poor absolute positional accuracy, and to distort the track when the whale's movement is predominantly vertical. In contrast, the LBL data can provide quantitative measures of whale behavior. Transit speeds between bubble net feeding events for this case study are found to range from 0.7 to 1.9 m . s(-1) (n = 8). The mean diameter of bubble net curtains are measured to range from 9.6 to 10.9 m. Whale speeds during bubble net rotations vary from 1.0 to 1.9 m . s(-1) (n = 6).
C1 [Schmidt, Val; Weber, Thomas C.] Univ New Hampshire, Ctr Coastal & Ocean Mapping, Durham, NH 03820 USA.
[Wiley, David N.] Natl Oceanog & Atmospher Adm, Stellwagen Bank Natl Marine Sanctuary, Situate, MA 02040 USA.
[Johnson, Mark P.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.
RP Schmidt, V (reprint author), Univ New Hampshire, Ctr Coastal & Ocean Mapping, Durham, NH 03820 USA.
EM vschmidt@ccom.unh.edu
RI Weber, Thomas/H-2428-2012
OI Weber, Thomas/0000-0001-8320-361X
FU National Oceanographic and Atmospheric Administration [NA05NOS4001153];
National Oceanographic Partnership Program
FX This work was supported by the National Oceanographic and Atmospheric
Administration under Grant NA05NOS4001153. The work of M. P. Johnson was
supported by the National Oceanographic Partnership Program. Tagging of
whales on Stellwagen Bank was conducted by the staff of the Stellwagen
Bank National Marine Sanctuary under NOAA Permit #775-1600-10.
NR 43
TC 4
Z9 4
U1 2
U2 17
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 0364-9059
J9 IEEE J OCEANIC ENG
JI IEEE J. Ocean. Eng.
PD OCT
PY 2010
VL 35
IS 4
BP 821
EP 836
DI 10.1109/JOE.2010.2068610
PG 16
WC Engineering, Civil; Engineering, Ocean; Engineering, Electrical &
Electronic; Oceanography
SC Engineering; Oceanography
GA 688LP
UT WOS:000284851100015
ER
PT J
AU Kerr, AR
Randa, J
AF Kerr, Anthony R.
Randa, James
TI Thermal Noise and Noise Measurements-A 2010 Update
SO IEEE MICROWAVE MAGAZINE
LA English
DT Article
DE Noise; Fluctuations; Resistors; Temperature measurement; Elementary
particle vacuum; Thermal noise; Hafnium
ID LINEAR-AMPLIFIERS; MIXERS
C1 [Kerr, Anthony R.] Natl Radio Astron Observ, Charlottesville, VA 22903 USA.
[Randa, James] NIST, Electromagnet Div, Boulder, CO 80305 USA.
[Randa, James] Univ Colorado, Dept Phys, Boulder, CO 80309 USA.
RP Kerr, AR (reprint author), Natl Radio Astron Observ, Edgemont Rd, Charlottesville, VA 22903 USA.
NR 22
TC 10
Z9 10
U1 0
U2 1
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 1527-3342
J9 IEEE MICROW MAG
JI IEEE Microw. Mag.
PD OCT
PY 2010
VL 11
IS 6
BP 40
EP 52
DI 10.1109/MMM.2010.937732
PG 13
WC Engineering, Electrical & Electronic; Telecommunications
SC Engineering; Telecommunications
GA 668DG
UT WOS:000283248200004
ER
PT J
AU Sutar, S
Zhang, Q
Seabaugh, A
AF Sutar, Surajit
Zhang, Qin
Seabaugh, Alan
TI InAlAs/InGaAs Interband Tunnel Diodes for SRAM
SO IEEE TRANSACTIONS ON ELECTRON DEVICES
LA English
DT Article
DE Interband tunneling; PVR; PVCR; resonant interband tunnel diode (RITD);
static random access memory (SRAM); tunnel diode (TD); tunnel SRAM;
tunneling-based SRAM (TSRAM)
ID VALLEY CURRENT RATIO; SILICON SUBSTRATE; ROOM-TEMPERATURE; PEAK;
TRANSISTORS; SPEED
AB The dependence of doping and alloy composition in InGaAs/InAlAs double-quantum-well resonant interband tunnel diodes (TDs) for static random access memory (SRAM) applications is explored. The peak current density is shown to vary by 5 orders of magnitude as the effective doping density is varied by a factor of 5. The reasons for this dependence are determined by characterization and analysis of current-voltage-temperature and capacitance-voltage measurements. This paper demonstrates a low-current bistable TD pair for SRAM with peak current density of 4 nA/mu m(2), peak-to-valley current ratio of 14, and peak voltage of 0.05 V enabling static binary storage at a supply voltage as low as 0.25 V.
C1 [Sutar, Surajit] SUNY Albany, Coll Nanoscale Sci & Engn, Albany, NY 12246 USA.
[Zhang, Qin] NIST, Div Semicond Elect, Gaithersburg, MD 20899 USA.
[Seabaugh, Alan] Univ Notre Dame, Dept Elect Engn, Notre Dame, IN 46556 USA.
RP Sutar, S (reprint author), SUNY Albany, Coll Nanoscale Sci & Engn, Albany, NY 12246 USA.
EM seabaugh.l@nd.edu
RI Seabaugh, Alan/I-4473-2012
OI Seabaugh, Alan/0000-0001-6907-4129
FU Intel Corporation
FX The authors would like to thank B. Doyle, D. Somasekhar, and W. Tsai of
Intel for useful discussions and the Intel Corporation for support.
NR 27
TC 2
Z9 2
U1 0
U2 9
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 0018-9383
J9 IEEE T ELECTRON DEV
JI IEEE Trans. Electron Devices
PD OCT
PY 2010
VL 57
IS 10
BP 2587
EP 2593
DI 10.1109/TED.2010.2059611
PG 7
WC Engineering, Electrical & Electronic; Physics, Applied
SC Engineering; Physics
GA 669KH
UT WOS:000283346500029
ER
PT J
AU Boukabara, SA
Garrett, K
Chen, WC
AF Boukabara, Sid-Ahmed
Garrett, Kevin
Chen, Wanchun
TI Global Coverage of Total Precipitable Water Using a Microwave
Variational Algorithm
SO IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING
LA English
DT Article
DE Advanced Microwave Sounding Unit (AMSU); data assimilation; Microwave
Humidity Sounder (MHS); microwave variational retrieval; radiosondes;
SSMIS; total precipitable water (TPW)
ID SOUNDING UNIT; RETRIEVAL; TEMPERATURE; SURFACE; VAPOR; LAND; AMSU
AB This study introduces a variational approach to retrieve total precipitable water (TPW) over all surface backgrounds including ocean, land, snow, sea-ice, and coastal areas, from microwave sensors. The product has been used routinely by forecasters since its recent operational implementation. The emissivity is accounted for by including its spectrum within the retrieved state vector, which allows for a pixel-to-pixel variation of the emissivity, a factor usually preventing the TPW retrieval over land. The algorithm, implemented operationally at the National Atmospheric and Oceanic Administration (NOAA), is called the Microwave Integrated Retrieval System (MiRS). Its main characteristic, besides its applicability over all surfaces, is its validity under all weather conditions. With a generic design, the algorithm is being applied to the following microwave sensors: 1) AMSU and MHS onboard NOAA-18; 2) NOAA-19 and Metop-A; as well as 3) SSMI/S onboard DMSP-F16 platform. The assessment of the MiRS performances is done by undertaking extensive comparisons to the National Center for Environmental Prediction (NCEP) and the European Centre for Medium-Range Weather Forecasts (ECMWF) analyses, to a network of radiosondes and to existing well-established algorithms over ocean, encompassing a wide variety of meteorological situations. The performance of MiRS TPW is shown to depend on the sensor, the reference data source as well as on the surface background considered. It is shown to behave quite well over all surfaces and in all weather conditions, except when there is rain. Although this study focuses on the retrieval of TPW with an emphasis on non-oceanic surfaces, the underlying application of this study is the potential improvement in the variational data assimilation of Numerical Weather Prediction (NWP) models. Indeed, the same dynamic approach could be employed in order to assimilate more surface-sensitive microwave channels, over a multitude of surfaces.
C1 [Boukabara, Sid-Ahmed] NOAA, Ctr Satellite Applicat & Res, Camp Springs, MD 20746 USA.
[Garrett, Kevin] IM Syst Grp IMSG Inc, Camp Springs, MD 20746 USA.
[Chen, Wanchun] Perot Syst Govt Serv, Camp Springs, MD 20746 USA.
RP Boukabara, SA (reprint author), NOAA, Ctr Satellite Applicat & Res, Camp Springs, MD 20746 USA.
EM sid.boukabara@noaa.gov
RI Boukabara, Sid Ahmed/F-5577-2010; Garrett, Kevin/L-7582-2016
OI Boukabara, Sid Ahmed/0000-0002-1857-3806; Garrett,
Kevin/0000-0002-7444-4363
FU U.S. National Oceanic and Atmospheric Administration (NOAA) Office of
Systems Development Product Systems Development Implementation
FX Manuscript received August 14, 2009; revised February 4, 2010. Date of
publication May 27, 2010; date of current version September 24, 2010.
This work was supported by the U.S. National Oceanic and Atmospheric
Administration (NOAA) Office of Systems Development Product Systems
Development Implementation. The views expressed here are those of the
authors and do not necessarily represent those of NOAA or the U.S.
Government.
NR 21
TC 11
Z9 12
U1 0
U2 11
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 0196-2892
J9 IEEE T GEOSCI REMOTE
JI IEEE Trans. Geosci. Remote Sensing
PD OCT
PY 2010
VL 48
IS 10
BP 3608
EP 3621
DI 10.1109/TGRS.2010.2048035
PG 14
WC Geochemistry & Geophysics; Engineering, Electrical & Electronic; Remote
Sensing; Imaging Science & Photographic Technology
SC Geochemistry & Geophysics; Engineering; Remote Sensing; Imaging Science
& Photographic Technology
GA 669KY
UT WOS:000283349400002
ER
PT J
AU Kim, DK
Griffith, D
Golmie, N
AF Kim, Duk Kyung
Griffith, David
Golmie, Nada
TI A New Call Admission Control Scheme for Heterogeneous Wireless Networks
SO IEEE TRANSACTIONS ON WIRELESS COMMUNICATIONS
LA English
DT Article
DE vertical handoffs; heterogeneous networks; ring-based model
ID PERFORMANCE ANALYSIS; SYSTEMS
AB Call Admission Control (CAC) between heterogeneous networks, such as an integrated 3rd Generation Partnership Project (3GPP) Long Term Evolution (LTE) network and a Wireless Local Area Network (WLAN), plays an important role to utilize the system resources in a more efficient way. In this paper, we propose that the preference to the WLAN is determined based on the traffic load in the WLAN and the location of the cellular users. Our analysis relies on a previous study that divides the 3G cellular coverage area into zones based on the amount of resources that are required to support a connection to a mobile user. Using this model, we derive new call blocking and handoff failure probabilities as well as new call and handoff attempt failure probabilities. Through simulations, we investigate proper preference settings by changing the WLAN load in a 3 ring-based sector with a WLAN hotspot.
C1 [Kim, Duk Kyung] Inha Univ, Inchon, South Korea.
[Griffith, David; Golmie, Nada] NIST, Gaithersburg, MD 20899 USA.
RP Kim, DK (reprint author), Inha Univ, Inchon, South Korea.
EM kdk@inha.ac.kr; david.griffith@nist.gov; nada.golmie@nist.gov
FU Ministry of Education, Science and Technology [2010-0022460]
FX This research was in part supported by the Basic Science Research
Program through the National Research Foundation of Korea(NRF) funded by
the Ministry of Education, Science and Technology (No. 2010-0022460).
NR 7
TC 17
Z9 20
U1 0
U2 10
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 1536-1276
J9 IEEE T WIREL COMMUN
JI IEEE Trans. Wirel. Commun.
PD OCT
PY 2010
VL 9
IS 10
BP 3000
EP 3005
DI 10.1109/TWC.2010.090210.100152
PG 6
WC Engineering, Electrical & Electronic; Telecommunications
SC Engineering; Telecommunications
GA 670OP
UT WOS:000283436800005
ER
PT J
AU Barallon, R
Bauer, SR
Butler, J
Capes-Davis, A
Dirks, WG
Elmore, E
Furtado, M
Kline, MC
Kohara, A
Los, GV
MacLeod, RAF
Masters, JRW
Nardone, M
Nardone, RM
Nims, RW
Price, PJ
Reid, YA
Shewale, J
Sykes, G
Steuer, AF
Storts, DR
Thomson, J
Taraporewala, Z
Alston-Roberts, C
Kerrigan, L
AF Barallon, Rita
Bauer, Steven R.
Butler, John
Capes-Davis, Amanda
Dirks, Wilhelm G.
Elmore, Eugene
Furtado, Manohar
Kline, Margaret C.
Kohara, Arihiro
Los, Georgyi V.
MacLeod, Roderick A. F.
Masters, John R. W.
Nardone, Mark
Nardone, Roland M.
Nims, Raymond W.
Price, Paul J.
Reid, Yvonne A.
Shewale, Jaiprakash
Sykes, Gregory
Steuer, Anton F.
Storts, Douglas R.
Thomson, Jim
Taraporewala, Zenobia
Alston-Roberts, Christine
Kerrigan, Liz
TI Recommendation of short tandem repeat profiling for authenticating human
cell lines, stem cells, and tissues
SO IN VITRO CELLULAR & DEVELOPMENTAL BIOLOGY-ANIMAL
LA English
DT Review
DE Cell authentication; STR profiling; Consensus standard; Quality control
ID CONTAMINATION
AB Cell misidentification and cross-contamination have plagued biomedical research for as long as cells have been employed as research tools. Examples of misidentified cell lines continue to surface to this day. Efforts to eradicate the problem by raising awareness of the issue and by asking scientists voluntarily to take appropriate actions have not been successful. Unambiguous cell authentication is an essential step in the scientific process and should be an inherent consideration during peer review of papers submitted for publication or during review of grants submitted for funding. In order to facilitate proper identity testing, accurate, reliable, inexpensive, and standardized methods for authentication of cells and cell lines must be made available. To this end, an international team of scientists is, at this time, preparing a consensus standard on the authentication of human cells using short tandem repeat (STR) profiling. This standard, which will be submitted for review and approval as an American National Standard by the American National Standards Institute, will provide investigators guidance on the use of STR profiling for authenticating human cell lines. Such guidance will include methodological detail on the preparation of the DNA sample, the appropriate numbers and types of loci to be evaluated, and the interpretation and quality control of the results. Associated with the standard itself will be the establishment and maintenance of a public STR profile database under the auspices of the National Center for Biotechnology Information. The consensus standard is anticipated to be adopted by granting agencies and scientific journals as appropriate methodology for authenticating human cell lines, stem cells, and tissues.
C1 [Elmore, Eugene] Univ Calif Irvine, Dept Radiat Oncol, Irvine, CA 92697 USA.
[Barallon, Rita; Thomson, Jim] LGC, Teddington TW11 0LY, Middx, England.
[Bauer, Steven R.] FDA Ctr Biol Evaluat & Res, Div Cellular & Gene Therapies, Off Cellular Tissue & Gene Therapies, Bethesda, MD 20892 USA.
[Butler, John; Kline, Margaret C.] NIST, Biochem Sci Div 831, Adv Chem Sci Lab 227, Gaithersburg, MD 20899 USA.
[Capes-Davis, Amanda] Childrens Med Res Inst, CellBank Australia, Westmead, NSW, Australia.
[Dirks, Wilhelm G.; MacLeod, Roderick A. F.] DSMZ German Collect Microorganisms & Cell Culture, D-38124 Braunschweig, Germany.
[Furtado, Manohar; Shewale, Jaiprakash] Appl Markets Genet Syst Life Technol, Foster City, CA 94404 USA.
[Kohara, Arihiro] Natl Inst Biomed Innovat, Dept Biomed Resources, Lab Cell Cultures, Osaka 5670085, Japan.
[Los, Georgyi V.] Univ Wisconsin, Neurosci Training Program, Madison, WI 53706 USA.
[Masters, John R. W.] UCL, Inst Urol, London W1W 7EJ, England.
[Nardone, Mark] NIH, Biotrac Program, Fdn Adv Educ Sci, Bethesda, MD 20892 USA.
[Nardone, Roland M.] Catholic Univ Amer, Washington, DC 20064 USA.
[Nims, Raymond W.] RMC Pharmaceut Solut Inc, Longmont, CO 80501 USA.
[Price, Paul J.] D Finit Cell Technol, Charleston, SC 29407 USA.
[Steuer, Anton F.] BioReliance, Rockville, MD 20850 USA.
[Storts, Douglas R.] Promega Corp, Nucle Acid Technol, Madison, WI 53711 USA.
[Taraporewala, Zenobia] FDA Ctr Biol Evaluat & Res, Div Cellular & Gene Therapies, Off Cellular Tissue & Gene Therapies, Rockville, MD 20852 USA.
[Reid, Yvonne A.; Sykes, Gregory; Alston-Roberts, Christine; Kerrigan, Liz] Amer Type Culture Collect, Manassas, VA 20110 USA.
RP Elmore, E (reprint author), Univ Calif Irvine, Dept Radiat Oncol, B146D, Irvine, CA 92697 USA.
EM eelmore@uci.edu
RI Butler, John/C-7812-2011; Bauer, Steven/G-5559-2012;
OI Bauer, Steven/0000-0003-2831-846X; Capes-Davis,
Amanda/0000-0003-4184-6339
NR 15
TC 38
Z9 39
U1 2
U2 8
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1071-2690
J9 IN VITRO CELL DEV-AN
JI In Vitro Cell. Dev. Biol.-Anim.
PD OCT
PY 2010
VL 46
IS 9
BP 727
EP 732
DI 10.1007/s11626-010-9333-z
PG 6
WC Cell Biology; Developmental Biology
SC Cell Biology; Developmental Biology
GA 672OC
UT WOS:000283594200001
PM 20614197
ER
PT J
AU Cox, SS
Liu, Z
Little, JC
Howard-Reed, C
Nabinger, SJ
Persily, A
AF Cox, S. S.
Liu, Z.
Little, J. C.
Howard-Reed, C.
Nabinger, S. J.
Persily, A.
TI Diffusion-controlled reference material for VOC emissions testing: proof
of concept
SO INDOOR AIR
LA English
DT Article
DE Diffusion model; Emission testing; Interlaboratory study; Reference
material; Volatile organic compounds
ID VOLATILE ORGANIC-COMPOUNDS; POROUS BUILDING-MATERIALS; ANALYTICAL-MODEL;
SINK BEHAVIOR; AIR-QUALITY; INDOOR AIR; COEFFICIENTS; PARTITION; CANCER;
WATER
AB Because of concerns about indoor air quality, there is growing awareness of the need to reduce the rate at which indoor materials and products emit volatile organic compounds (VOCs). To meet consumer demand for low emitting products, manufacturers are increasingly submitting materials to independent laboratories for emissions testing. However, the same product tested by different laboratories can result in very different emissions profiles because of a general lack of test validation procedures. There is a need for a reference material that can be used as a known emissions source and that will have the same emission rate when tested by different laboratories under the same conditions. A reference material was created by loading toluene into a polymethyl pentene film. A fundamental emissions model was used to predict the toluene emissions profile. Measured VOC emissions profiles using small-chamber emissions tests compared reasonably well to the emissions profile predicted using the emissions model, demonstrating the feasibility of the proposed approach to create a diffusion-controlled reference material.
C1 [Cox, S. S.; Liu, Z.; Little, J. C.] Virginia Tech, Dept Civil & Environm Engn, Blacksburg, VA 24061 USA.
[Howard-Reed, C.; Nabinger, S. J.; Persily, A.] Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
RP Little, JC (reprint author), Virginia Tech, Dept Civil & Environm Engn, 418 Durham Hall, Blacksburg, VA 24061 USA.
EM jcl@vt.edu
RI Little, John/B-4154-2009
FU National Institute of Standards and Testing (NIST) [2006-SGP-01,
60NANB6D6156]
FX Financial support for the contributions of the authors from Virginia
Tech was provided by the National Institute of Standards and Testing
(NIST) through the Small Grants Program No. 2006-SGP-01, Award Number
60NANB6D6156.
NR 29
TC 25
Z9 27
U1 3
U2 15
PU WILEY-BLACKWELL PUBLISHING, INC
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0905-6947
J9 INDOOR AIR
JI Indoor Air
PD OCT
PY 2010
VL 20
IS 5
BP 424
EP 433
DI 10.1111/j.1600-0668.2010.00666.x
PG 10
WC Construction & Building Technology; Engineering, Environmental; Public,
Environmental & Occupational Health
SC Construction & Building Technology; Engineering; Public, Environmental &
Occupational Health
GA 648RZ
UT WOS:000281713000008
PM 20579131
ER
PT J
AU Fleisher, JM
Fleming, LE
Solo-Gabriele, HM
Kish, JK
Sinigalliano, CD
Plano, L
Elmir, SM
Wang, JD
Withum, K
Shibata, T
Gidley, ML
Abdelzaher, A
He, GQ
Ortega, C
Zhu, XF
Wright, M
Hollenbeck, J
Backer, LC
AF Fleisher, Jay M.
Fleming, Lora E.
Solo-Gabriele, Helena M.
Kish, Jonathan K.
Sinigalliano, Christopher D.
Plano, Lisa
Elmir, Samir M.
Wang, John D.
Withum, Kelly
Shibata, Tomoyuki
Gidley, Maribeth L.
Abdelzaher, Amir
He, Guoqing
Ortega, Cristina
Zhu, Xiaofang
Wright, Mary
Hollenbeck, Julie
Backer, Lorraine C.
TI The BEACHES Study: health effects and exposures from non-point source
microbial contaminants in subtropical recreational marine waters
SO INTERNATIONAL JOURNAL OF EPIDEMIOLOGY
LA English
DT Article
DE Gastrointestinal illness; respiratory illness; skin illness; indicator
organisms; enterococci; recreational water quality
ID GASTROINTESTINAL ILLNESS; FECAL CONTAMINATION; DOMESTIC SEWAGE; COASTAL
WATERS; QUALITY; GASTROENTERITIS; ENVIRONMENT; INDICATORS; RISK;
GUIDELINES
AB Methods A total of 1303 adult regular bathers were randomly assigned to bather and non-bather groups, with subsequent follow-up for reported illness, in conjunction with extensive environmental sampling of indicator organisms (enterococci).
Results Bathers were 1.76 times more likely to report gastrointestinal illness [95% confidence interval (CI) 0.94-3.30; P = 0.07]; 4.46 times more likely to report acute febrile respiratory illness (95% CI 0.99-20.90; P = 0.051) and 5.91 times more likely to report a skin illness (95% CI 2.76-12.63; P < 0.0001) relative to non-bathers. Evidence of a dose-response relationship was found between skin illnesses and increasing enterococci exposure among bathers [1.46 times (95% CI 0.97-2.21; P = 0.07) per increasing log(10) unit of enterococci exposure], but not for gastrointestinal or respiratory illnesses.
Conclusions This study indicated that bathers may be at increased risk of several illnesses relative to non-bathers, even in the absence of any known source of domestic sewage impacting the recreational marine waters. There was no dose-response relationship between gastroenteritis and increasing exposure to enterococci, even though many current water-monitoring standards use gastroenteritis as the major outcome illness.
C1 [Fleisher, Jay M.] Nova SE Univ COM MPH, Ft Lauderdale, FL 33328 USA.
[Fleisher, Jay M.; Fleming, Lora E.; Solo-Gabriele, Helena M.; Kish, Jonathan K.; Sinigalliano, Christopher D.; Plano, Lisa; Elmir, Samir M.; Wang, John D.; Withum, Kelly; Shibata, Tomoyuki; Gidley, Maribeth L.; Abdelzaher, Amir; He, Guoqing; Ortega, Cristina; Zhu, Xiaofang; Wright, Mary; Hollenbeck, Julie] Univ Miami, Rosenstiel Sch, Oceans & Human Hlth Ctr, NSF,NIEHS, Miami, FL USA.
[Fleming, Lora E.; Plano, Lisa] Univ Miami, Miller Sch Med, Sch Med, Miami, FL 33136 USA.
[Solo-Gabriele, Helena M.; Shibata, Tomoyuki; Abdelzaher, Amir; He, Guoqing; Ortega, Cristina; Wright, Mary] Univ Miami, Coll Engn, Coral Gables, FL 33124 USA.
[Sinigalliano, Christopher D.; Shibata, Tomoyuki; Gidley, Maribeth L.] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
[Elmir, Samir M.] Miami Dade Cty Publ Hlth Dept, Miami, FL USA.
[Backer, Lorraine C.] Ctr Dis Control & Prevent, Natl Ctr Environm Hlth, Atlanta, GA USA.
RP Fleisher, JM (reprint author), Nova SE Univ COM MPH, 3200 S Univ Dr, Ft Lauderdale, FL 33328 USA.
EM jmfleish@nova.edu
RI Sinigalliano, Christopher/A-8760-2014; gidley, maribeth/B-8335-2014
OI Sinigalliano, Christopher/0000-0002-9942-238X; gidley,
maribeth/0000-0001-9583-8073
FU National Center for Environmental Health (NCEH), Centers for Disease
Control and Prevention (CDC); Florida Dept of Health (FL DOH) through
Florida Dept of Environmental Protection (FL DEP); EPA; National Science
Foundation (NSF); National Institute of Environmental Health Sciences
(NIEHS) Oceans and Human Health Center at the University of Miami
Rosenstiel School [NSF 0CE0432368, NIEHS P50 ES12736]; NSF REU in Oceans
and Human Health; NSF SGER in Oceans and Human Health [NSF SGER 0743987]
FX National Center for Environmental Health (NCEH), Centers for Disease
Control and Prevention (CDC); Florida Dept of Health (FL DOH) through
monies from the Florida Dept of Environmental Protection (FL DEP); the
EPA Internship Program; the National Science Foundation (NSF) and the
National Institute of Environmental Health Sciences (NIEHS) Oceans and
Human Health Center at the University of Miami Rosenstiel School (NSF
0CE0432368) and (NIEHS P50 ES12736) and NSF REU in Oceans and Human
Health and the NSF SGER (NSF SGER 0743987) in Oceans and Human Health.
NR 38
TC 54
Z9 58
U1 2
U2 18
PU OXFORD UNIV PRESS
PI OXFORD
PA GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND
SN 0300-5771
J9 INT J EPIDEMIOL
JI Int. J. Epidemiol.
PD OCT
PY 2010
VL 39
IS 5
BP 1291
EP 1298
DI 10.1093/ije/dyq084
PG 8
WC Public, Environmental & Occupational Health
SC Public, Environmental & Occupational Health
GA 676RA
UT WOS:000283932000025
PM 20522483
ER
PT J
AU Harrower, C
Poirier, E
Fritzsche, H
Kalisvaart, P
Satija, S
Akgun, B
Mitlin, D
AF Harrower, Christopher
Poirier, Eric
Fritzsche, Helmut
Kalisvaart, Peter
Satija, Sushil
Akgun, Bulent
Mitlin, David
TI Early deuteration steps of Pd- and Ta/Pd- catalyzed Mg70Al30 thin films
observed at room temperature
SO INTERNATIONAL JOURNAL OF HYDROGEN ENERGY
LA English
DT Article
DE Hydrogen storage; Metal hydride; Catalyst; Thin film; Neutron
reflectometry
ID HYDROGEN-STORAGE; THERMODYNAMIC PROPERTIES; NEUTRON-REFLECTOMETRY; LAYER
THICKNESS; MG; ABSORPTION; DESORPTION; MAGNESIUM; SURFACE; METALS
AB Deuterium absorption in Mg70Al30 thin films coated with a Pd layer and a Ta/Pd bilayer were investigated using in situ neutron reflectometry at room temperature and deuterium pressures up to 1.3 bar. The approach used provides a detailed profile, at the nanoscale, of the deuterium content inside the specific layers that constitute the films. It is found that Mg70Al30 can store up to 5 wt.% under these mild conditions following a two-step mechanism. The latter involves the deuteration of the top and bottom catalyst layers first, followed by the main Mg70Al30 layer. The presence of deuterium throughout the films in the early absorption stages evidences atomic deuterium spillover from the catalyst layers. The addition of a Ta layer between the Pd and Mg70Al30 was found to allow observable absorption at a pressure 10 times lower than on the Ta-free sample, without affecting the storage capacity. Our measurements imply that this improvement in kinetics is due to a lowering of the nucleation barrier for the formation of the hydride phase in the Mg70Al30 layer. Crown Copyright (C) 2010 Published by Elsevier Ltd on behalf of Professor T. Nejat Veziroglu. All rights reserved.
C1 [Poirier, Eric; Fritzsche, Helmut] Natl Res Council Canada, Canadian Neutron Beam Ctr, SIMS, Chalk River, ON K0J 1J0, Canada.
[Harrower, Christopher; Kalisvaart, Peter; Mitlin, David] Univ Alberta, Edmonton, AB T6G 2V4, Canada.
[Harrower, Christopher; Kalisvaart, Peter; Mitlin, David] Natl Res Council Canada, Natl Inst Nanotechnol, Edmonton, AB T6G 2M9, Canada.
[Satija, Sushil; Akgun, Bulent] Natl Inst Stand & Technol, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Akgun, Bulent] Univ Maryland, Dept Mat Sci & Engn, College Pk, MD 20742 USA.
RP Fritzsche, H (reprint author), Natl Res Council Canada, Canadian Neutron Beam Ctr, SIMS, Chalk River, ON K0J 1J0, Canada.
EM Harrower@ualberta.ca; Helmut.Fritzsche@nrc.gc.ca; dmitlin@ualberta.ca
RI Akgun, Bulent/H-3798-2011; Poirier, Eric/J-2387-2014; Mitlin , David
/M-5328-2016
OI Poirier, Eric/0000-0001-8622-1397; Mitlin , David /0000-0002-7556-3575
NR 31
TC 7
Z9 7
U1 0
U2 2
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0360-3199
J9 INT J HYDROGEN ENERG
JI Int. J. Hydrog. Energy
PD OCT
PY 2010
VL 35
IS 19
BP 10343
EP 10348
DI 10.1016/j.ijhydene.2010.08.001
PG 6
WC Chemistry, Physical; Electrochemistry; Energy & Fuels
SC Chemistry; Electrochemistry; Energy & Fuels
GA 677GM
UT WOS:000283977100037
ER
PT J
AU Hanssen, LM
Mekhontsev, SN
Khromchenko, VB
AF Hanssen, Leonard M.
Mekhontsev, Sergey N.
Khromchenko, Vladimir B.
TI Validation of the Infrared Emittance Characterization of Materials
Through Intercomparison of Direct and Indirect Methods
SO INTERNATIONAL JOURNAL OF THERMOPHYSICS
LA English
DT Article
DE Directional reflectance; Emissivity; Emittance; Fourier spectrometer;
Hemispherical reflectance; Integrating sphere; Radiance; Radiance
temperature
AB A comparison of the spectral directional emittance of samples as a function of wavelength was performed at the Fourier Transform Infrared Spectrophotometry (FTIS) and the Advanced Infrared Radiometry and Imaging (AIRI) facilities at NIST. At the FTIS, the emittance is obtained indirectly through the measurement of near-normal directional-hemispherical reflectance (DHR) using an infrared integrating sphere. At the AIRI, the normal directional emittance is obtained directly through the measurement of the sample spectral radiance referenced to that from blackbody sources, while the sample is located behind a black plate of known temperature and emittance. On the same setup at the AIRI, the normal emittance at near ambient temperatures is also measured indirectly by a "two-temperature" method in which the sample spectral radiance is measured while the background temperature is controlled and varied. The sample emittance measurements on the comparison samples are presented over a wavelength range of 3.4 mu m to 13.5 mu m at several near-ambient temperatures and for near-normal incidence. The results obtained validate the two independent capabilities and demonstrate the potential of the controlled background methods for measurements of the radiative properties of IR materials.
C1 [Hanssen, Leonard M.; Mekhontsev, Sergey N.; Khromchenko, Vladimir B.] NIST, Opt Technol Div, Gaithersburg, MD 20899 USA.
RP Hanssen, LM (reprint author), NIST, Opt Technol Div, Gaithersburg, MD 20899 USA.
EM hanssen@nist.gov
NR 7
TC 4
Z9 4
U1 1
U2 8
PU SPRINGER/PLENUM PUBLISHERS
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0195-928X
J9 INT J THERMOPHYS
JI Int. J. Thermophys.
PD OCT
PY 2010
VL 31
IS 10
BP 1972
EP 1978
DI 10.1007/s10765-008-0507-9
PG 7
WC Thermodynamics; Chemistry, Physical; Mechanics; Physics, Applied
SC Thermodynamics; Chemistry; Mechanics; Physics
GA 683OO
UT WOS:000284485300012
ER
PT J
AU Moffat, TP
Josell, D
AF Moffat, Thomas P.
Josell, Daniel
TI Superconformal Electrodeposition for 3-Dimensional Interconnects
SO ISRAEL JOURNAL OF CHEMISTRY
LA English
DT Review
DE copper; electrochemistry; electrodeposition; electroplating;
microfabrication
ID CHEMICAL-VAPOR-DEPOSITION; SUBMICROMETER TRENCHES; THIN-FILMS; METAL
IONS; COPPER; SILVER; CU; ADSORPTION; CELLS; GOLD
AB Electrodeposition is a key fabrication process used in the state-of-the-art multilevel Cu metallization of microelectronic interconnects, from transistor to circuit board length scale. Recent electrochemical surface science and feature filling studies have provided mechanistic insight into the role of additives in superconformal film growth responsible for void-free filling of recessed surface features. These studies have shown that a physical model based on mass conservation of accelerating surfactant species during area change very effectively describes feature filling of Cu, Ag, and Au from different electrolytes. This paper presents a selective and cursory review of some relevant developments underway in our laboratory.
C1 [Moffat, Thomas P.; Josell, Daniel] Natl Inst Stand & Technol, Mat Sci & Engn Lab, Gaithersburg, MD 20899 USA.
RP Moffat, TP (reprint author), Natl Inst Stand & Technol, Mat Sci & Engn Lab, Gaithersburg, MD 20899 USA.
EM thomas.moffat@nist.gov
NR 38
TC 13
Z9 13
U1 8
U2 47
PU SCIENCE FROM ISRAEL-DIVISION OF LASER PAGES PUBL LTD
PI JERUSALEM
PA PO BOX 34299, JERUSALEM 91341, ISRAEL
SN 0021-2148
J9 ISR J CHEM
JI Isr. J. Chem.
PD OCT
PY 2010
VL 50
IS 3
BP 312
EP 320
DI 10.1002/ijch.201000029
PG 9
WC Chemistry, Multidisciplinary
SC Chemistry
GA 678ME
UT WOS:000284079100008
ER
PT J
AU Petrenko, B
Ignatov, A
Kihai, Y
Heidinger, A
AF Petrenko, B.
Ignatov, A.
Kihai, Y.
Heidinger, A.
TI Clear-Sky Mask for the Advanced Clear-Sky Processor for Oceans
SO JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY
LA English
DT Article
ID SEA-SURFACE TEMPERATURE; CLOUD CONTAMINATION; INFRARED IMAGERY; AVHRR
DATA; RADIANCES; RETRIEVAL; ALGORITHM
AB The Advanced Clear Sky Processor for Oceans (ACSPO) generates clear-sky products, such as SST, clear-sky radiances, and aerosol, from Advanced Very High Resolution Radiometer (AVHRR)-like measurements. The ACSPO clear-sky mask (ACSM) identifies clear-sky pixels within the ACSPO products. This paper describes the ACSM structure and compares the performances of ACSM and its predecessor, Clouds from AVHRR Extended Algorithm (CLAVRx). ACSM essentially employs online clear-sky radiative transfer simulations enabled within ACSPO with the Community Radiative Transfer Model (CRTM) in conjunction with numerical weather prediction atmospheric [Global Forecast System (GFS)] and SST [Reynolds daily high-resolution blended SST (DSST)] fields. The baseline ACSM tests verify the accuracy of fitting observed brightness temperatures with CRTM, check retrieved SST for consistency with Reynolds SST, and identify ambient cloudiness at the boundaries of cloudy systems. Residual cloud effects are screened out with several tests, adopted from CLAVRx, and with the SST spatial uniformity test designed to minimize misclassification of sharp SST gradients as clouds. Cross-platform and temporal consistencies of retrieved SSTs are maintained by accounting for SST and brightness temperature biases, estimated within ACSPO online and independently from ACSM. The performance of ACSM is characterized in terms of statistics of deviations of retrieved SST from the DSST. ACSM increases the amount of "clear'' pixels by 30% to 40% and improves statistics of retrieved SST compared with CLAVRx. ACSM is also shown to be capable of producing satisfactory statistics of SST anomalies if the reference SST field for the exact date of observations is unavailable at the time of processing.
C1 [Petrenko, B.; Ignatov, A.; Kihai, Y.] Natl Environm Satellite Data & Informat Serv, Ctr Satellite Applicat & Res, NOAA, Camp Springs, MD USA.
[Petrenko, B.] IMSG Inc, Kensington, MD USA.
[Kihai, Y.] Dell Perot Syst, Fairfax, VA USA.
[Heidinger, A.] Natl Environm Satellite Data & Informat Serv, NOAA, Madison, WI USA.
RP Petrenko, B (reprint author), Room 601-4,5200 Auth Rd, Camp Springs, MD 20746 USA.
EM boris.petrenko@noaa.gov
RI Heidinger, Andrew/F-5591-2010; Ignatov, Alexander/F-5594-2010
OI Heidinger, Andrew/0000-0001-7631-109X; Ignatov,
Alexander/0000-0002-7463-5944
FU GOES-R Program Office
FX We thank our colleagues John Supper (NESDIS/OSDPD), Xing-Ming Liang,
Feng Xu, and Prasanjit Dash (STAR/CIRA), Nikolay Shabanov (STAR/IMSG),
and Denise Frey (OSDPD/QSS) for valuable assistance, discussions, and
feedback at the different stages of work. Our special thanks go to the
reviewers, whose constructive comments greatly helped us to improve the
manuscript. This work is conducted under the Algorithm Working Group
funded by the GOES-R Program Office. The views, opinions, and findings
contained in this report are those of the authors and should not be
construed as an official NOAA or U.S. Government position, policy, or
decision.
NR 32
TC 26
Z9 27
U1 0
U2 3
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0739-0572
J9 J ATMOS OCEAN TECH
JI J. Atmos. Ocean. Technol.
PD OCT
PY 2010
VL 27
IS 10
BP 1609
EP 1623
DI 10.1175/2010JTECHA1413.1
PG 15
WC Engineering, Ocean; Meteorology & Atmospheric Sciences
SC Engineering; Meteorology & Atmospheric Sciences
GA 665OB
UT WOS:000283044100004
ER
PT J
AU Zrnic, D
Doviak, R
Zhang, GF
Ryzhkov, A
AF Zrnic, Dusan
Doviak, Richard
Zhang, Guifu
Ryzhkov, Alexander
TI Bias in Differential Reflectivity due to Cross Coupling through the
Radiation Patterns of Polarimetric Weather Radars
SO JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY
LA English
DT Article
ID RAINFALL; CLASSIFICATION; CALIBRATION; WSR-88D
AB Examined is bias in differential reflectivity and its effect on estimates of rain rate due to coupling of the vertically and horizontally polarized fields through the radiation patterns. To that end, a brief review of the effects of the bias on quantitative rainfall measurements is given. Suggestions for tolerable values of this bias are made. Of utmost interest is the bias produced by radars simultaneously transmitting horizontally and vertically polarized fields, as this configuration has been chosen for pending upgrades to the U. S. national network of radars (Weather Surveillance Radar-1988 Doppler; WSR-88D). The bias strongly depends on the cross-polar radiation pattern. Two patterns, documented in the literature, are considered.
C1 [Zrnic, Dusan; Doviak, Richard] NOAA, Natl Severe Storms Lab, Norman, OK 73072 USA.
[Zhang, Guifu] Univ Oklahoma, Sch Meteorol, Norman, OK 73019 USA.
[Ryzhkov, Alexander] Univ Oklahoma, Cooperat Inst Mesoscale Meteorol Studies, Norman, OK 73019 USA.
RP Zrnic, D (reprint author), NOAA, Natl Severe Storms Lab, 120 David L Boren Blvd, Norman, OK 73072 USA.
EM dusan.zrnic@noaa.gov
RI Zhang, Guifu/M-3178-2014
OI Zhang, Guifu/0000-0002-0261-2815
FU NOAA/Office of Oceanic and Atmospheric Research under NOAA-University of
Oklahoma [NA17RJ1227]
FX Pattern measurements of the OU PRIME antenna were provided by Enterprise
Electronics Corporation and Dr. Boon Leng Cheong of the Atmospheric
Radar Research Center at the University of Oklahoma. Funding for the
CIMMS author (AR) came from NOAA/Office of Oceanic and Atmospheric
Research under NOAA-University of Oklahoma Cooperative Agreement
NA17RJ1227, U.S. Department of Commerce.
NR 28
TC 41
Z9 41
U1 0
U2 2
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0739-0572
J9 J ATMOS OCEAN TECH
JI J. Atmos. Ocean. Technol.
PD OCT
PY 2010
VL 27
IS 10
BP 1624
EP 1637
DI 10.1175/2010JTECHA1350.1
PG 14
WC Engineering, Ocean; Meteorology & Atmospheric Sciences
SC Engineering; Meteorology & Atmospheric Sciences
GA 665OB
UT WOS:000283044100005
ER
PT J
AU Voss, KJ
McLean, S
Lewis, M
Johnson, C
Flora, S
Feinholz, M
Yarbrough, M
Trees, C
Twardowski, M
Clark, D
AF Voss, Kenneth J.
McLean, Scott
Lewis, Marlon
Johnson, Carol
Flora, Stephanie
Feinholz, Michael
Yarbrough, Mark
Trees, Charles
Twardowski, Mike
Clark, Dennis
TI An Example Crossover Experiment for Testing New Vicarious Calibration
Techniques for Satellite Ocean Color Radiometry
SO JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY
LA English
DT Article
ID PACIFIC; WATERS
AB Vicarious calibration of ocean color satellites involves the use of accurate surface measurements of water-leaving radiance to update and improve the system calibration of ocean color satellite sensors. An experiment was performed to compare a free-fall technique with the established Marine Optical Buoy (MOBY) measurement. It was found in the laboratory that the radiance and irradiance instruments compared well within their estimated uncertainties for various spectral sources. The spectrally averaged differences between the National Institute of Standards and Technology (NIST) values for the sources and the instruments were <2.5% for the radiance sensors and <1.5% for the irradiance sensors. In the field, the sensors measuring the above-surface downwelling irradiance performed nearly as well as they had in the laboratory, with an average difference of <2%. While the water-leaving radiance L(w) calculated from each instrument agreed in almost all cases within the combined instrument uncertainties (approximately 7%), there was a relative bias between the two instrument classes/techniques that varied spectrally. The spectrally averaged (400-600 nm) difference between the two instrument classes/techniques was 3.1%. However, the spectral variation resulted in the free-fall instruments being 0.2% lower at 450 nm and 5.9% higher at 550 nm. Based on the analysis of one matchup, the bias in L(w) was similar to that observed for L(u)(1 m) with both systems, indicating the difference did not come from propagating L(u)(1 m) to L(w).
C1 [Voss, Kenneth J.] Univ Miami, Dept Phys, Coral Gables, FL 33146 USA.
[McLean, Scott; Lewis, Marlon] Dalhousie Univ, Halifax, NS, Canada.
[McLean, Scott; Lewis, Marlon] Satlantic Inc, Halifax, NS, Canada.
[Johnson, Carol] Natl Inst Stand & Technol, Opt Technol Div, Gaithersburg, MD 20899 USA.
[Flora, Stephanie; Feinholz, Michael; Yarbrough, Mark] Moss Landing Marine Labs, Moss Landing, CA 95039 USA.
[Trees, Charles] NATO Undersea Res Ctr, La Spezia, Italy.
[Twardowski, Mike] WET Labs Inc, Narragansett, RI USA.
[Clark, Dennis] DBA Marine Opt Consulting, Arnold, MD USA.
[Clark, Dennis] NIST Utah State Univ Program Opt Sensor Calibrat, Utah State Univ Res Fdn, Logan, UT USA.
RP Voss, KJ (reprint author), Univ Miami, Dept Phys, Room 304,1320 Campo Sano Dr, Coral Gables, FL 33146 USA.
EM voss@physics.miami.edu
RI Voss, Kenneth /A-5328-2013
OI Voss, Kenneth /0000-0002-7860-5080
FU NASA [NNX06AD44G, NNX06AH14G, NNG04HK33I]; NOAA [NA05AANEG0013]; Space
Dynamics Laboratory, Logan, Utah, under a Joint NIST/Utah State
University
FX This work was supported by NASA under Grants NNX06AD44G (KV), NNX06AH14G
(CT), NASA to NOAA NNG04HK33I (BCJ), and NOAA to NIST NA05AANEG0013
(BCJ). Dennis Clark was supported by Space Dynamics Laboratory, Logan,
Utah, under a Joint NIST/Utah State University Program in Optical Sensor
Calibration. We also would like to thank Dr. James Mueller for his help
in interpretation and using his shadowing correction for the MOBY
instrument.
NR 20
TC 13
Z9 13
U1 0
U2 5
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0739-0572
J9 J ATMOS OCEAN TECH
JI J. Atmos. Ocean. Technol.
PD OCT
PY 2010
VL 27
IS 10
BP 1747
EP 1759
DI 10.1175/2010JTECHO737.1
PG 13
WC Engineering, Ocean; Meteorology & Atmospheric Sciences
SC Engineering; Meteorology & Atmospheric Sciences
GA 665OB
UT WOS:000283044100013
ER
PT J
AU Jackson, DL
Wick, GA
AF Jackson, Darren L.
Wick, Gary A.
TI Near-Surface Air Temperature Retrieval Derived from AMSU-A and Sea
Surface Temperature Observations
SO JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY
LA English
DT Article
ID LATENT-HEAT FLUX; SATELLITE DATA
AB A 10-m air temperature (Ta) retrieval using Advanced Microwave Sounding Unit A (AMSU-A) and satellite-derived sea surface temperature (Ts) observations is presented. The multivariable linear regression retrieval uses AMSU-A brightness temperatures from the 52.8- and 53.6-GHz channels and satellite-derived daily sea surface temperatures to determine Ta. A regression error of 0.83 degrees C using 841 matched satellite and ship observations demonstrates a high-quality fit of the satellite observations with in situ Ta. Validation of the retrieval using independent International Comprehensive Ocean-Atmosphere Dataset (ICOADS) ship and buoy observations results in a bias of -0.21 degrees C and root-mean-square (RMS) differences of 1.55 degrees C. A comparison with previous satellite-based Ta retrievals indicates less bias and significantly smaller RMS differences for the new retrieval. Regional biases inherent to previous retrievals are reduced in several oceanic regions using the new Ta retrieval. Satellite-derived Ts-Ta data were found to agree well with ICOADS buoy data and were significantly improved from previous retrievals.
C1 [Jackson, Darren L.] Univ Colorado, Cooperat Inst Res Environm Sci, NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA.
RP Jackson, DL (reprint author), Univ Colorado, Cooperat Inst Res Environm Sci, NOAA, Earth Syst Res Lab, 325 Broadway R-PSD2, Boulder, CO 80305 USA.
EM darren.l.jackson@noaa.gov
RI Jackson, Darren/D-5506-2015
OI Jackson, Darren/0000-0001-5211-7866
FU NASA [NNM04AA67I]; National Science Foundation (NSF)
FX This project supported in part by funding from NASA Grant NNM04AA67I in
collaboration with Dr. Franklin R. Robertson at the Marshall Space
Flight Center. The ICOADS data are from the Research Data Archive (RDA),
which is maintained by the Computational and Information Systems
Laboratory (CISL) at the National Center for Atmospheric Research
(NCAR). NCAR is sponsored by the National Science Foundation (NSF). The
original data are available from the RDA (http://dss.ucar.edu) in
dataset ds540.1.
NR 16
TC 13
Z9 14
U1 0
U2 7
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0739-0572
J9 J ATMOS OCEAN TECH
JI J. Atmos. Ocean. Technol.
PD OCT
PY 2010
VL 27
IS 10
BP 1769
EP 1776
DI 10.1175/2010JTECHA1414.1
PG 8
WC Engineering, Ocean; Meteorology & Atmospheric Sciences
SC Engineering; Meteorology & Atmospheric Sciences
GA 665OB
UT WOS:000283044100015
ER
PT J
AU Moldover, MR
McLinden, MO
AF Moldover, Michael R.
McLinden, Mark O.
TI Using ab initio "data" to accurately determine the fourth density virial
coefficient of helium
SO JOURNAL OF CHEMICAL THERMODYNAMICS
LA English
DT Article
DE Helium; Two-sinker densimeter; Equation of state; Reference data; Gas
metrology; Fourth virial coefficient
ID THERMOPHYSICAL PROPERTIES; STANDARD; TEMPERATURE; PRESSURE; VALUES;
DENSIMETERS; RANGES
AB We combine accurate ab initio calculations of the second and third density virial coefficients. B(T) and C(T), of (4)He with measurements of its (p-rho-T) behavior to determine the fourth density virial coefficient D(7) The measurements were made with a two-sinker, magnetic-suspension densimeter at pressures up to 38 MPa. The measurements on isotherms from T = 223 K to T = 323 K were previously published; new measurements from T = 323 K to T = 500 K are presented here On each isotherm, a regression of the virial expansion was constrained to the ab initio values of B(T) and C(T), the regression determined D(T) as well as two apparatus-dependent parameters that compensated for systematic errors in the measurements. The percentage uncertainties of D(T) ranged from 2.6% at T = 223 K to 95% at T = 400 K to 24 7% at T = 500 K, where these uncertainties are expanded uncertainties with coverage factor of k = 2 corresponding to a 95% confidence interval These uncertainties are 1/6th of the uncertainty obtained without the ab initio values of B(T) and C(T) The apparatus-dependent parameters can be used to calibrate the densimeter, and this will reduce the uncertainty of other measurements made with this two-sinker densimeter The new values of D(T) will find applications in accurate gas metrology, such as a primary pressure standard based on the refractive index of helium (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Moldover, Michael R.] Natl Inst Stand & Technol, Proc Measurements Div, Gaithersburg, MD 20899 USA.
[McLinden, Mark O.] Natl Inst Stand & Technol, Thermophys Properties Div, Boulder, CO 80305 USA.
RP Moldover, MR (reprint author), Natl Inst Stand & Technol, Proc Measurements Div, Gaithersburg, MD 20899 USA.
RI Moldover, Michael/E-6384-2013
NR 22
TC 12
Z9 12
U1 2
U2 10
PU ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
PI LONDON
PA 24-28 OVAL RD, LONDON NW1 7DX, ENGLAND
SN 0021-9614
J9 J CHEM THERMODYN
JI J. Chem. Thermodyn.
PD OCT
PY 2010
VL 42
IS 10
BP 1193
EP 1203
DI 10.1016/j.jct.2010.02.015
PG 11
WC Thermodynamics; Chemistry, Physical
SC Thermodynamics; Chemistry
GA 632BY
UT WOS:000280396300001
ER
PT J
AU Konda, M
Ichikawa, H
Tomita, H
Cronin, MF
AF Konda, Masanori
Ichikawa, Hiroshi
Tomita, Hiroyuki
Cronin, Meghan F.
TI Surface Heat Flux Variations across the Kuroshio Extension as Observed
by Surface Flux Buoys
SO JOURNAL OF CLIMATE
LA English
DT Article
ID PACIFIC INTERMEDIATE WATER; SUBTROPICAL MODE WATER; EXTRATROPICAL SST
ANOMALIES; AIR-SEA FLUXES; NORTH PACIFIC; MIXED-LAYER; ATMOSPHERIC
BRIDGE; TROPICAL PACIFIC; OCEAN; TEMPERATURE
AB Wintertime sea surface heat flux variability across the Kuroshio Extension (KE) front is analyzed using data from the Kuroshio Extension Observatory (KEO) buoy in the Kuroshio recirculation gyre south of the KE front and from the Japan Agency for Marine-Earth Science and Technology KEO (JKEO) buoy in the north of the front. The coincident data used are from periods during two winters (2007 and 2008), when both buoys had a complete suite of meteorological data. In these two winter periods, the focus of this research is on three types of typical weather patterns referred to here as the northerly wind condition, the monsoon wind condition, and the normal condition. During the northerly wind condition, latent and sensible heat fluxes were large and often varied simultaneously at both sites, whereas during the monsoon wind condition the latent heat flux at the KEO site was significantly larger than that at the JKEO site. The difference between these heat flux patterns is attributed to the different airmass transformations that occur when prevailing winds blow across the KE front versus along the front. Reanalysis products appear to reproduce these heat flux spatial patterns at synoptic scales. It is suggested that the relative frequencies of these different types of weather conditions result in anomalous spatial patterns in the heat fluxes on monthly time scales.
C1 [Konda, Masanori] Kyoto Univ, Dept Geophys, Grad Sch Sci, Sakyo Ku, Kyoto 6068502, Japan.
[Konda, Masanori; Ichikawa, Hiroshi; Tomita, Hiroyuki] Japan Agcy Marine Earth Sci & Technol, Res Inst Global Change, Yokosuka, Kanagawa 2370061, Japan.
[Cronin, Meghan F.] NOAA, Pacific Marine Environm Lab, Seattle, WA 98115 USA.
RP Konda, M (reprint author), Kyoto Univ, Dept Geophys, Grad Sch Sci, Sakyo Ku, Kyoto 6068502, Japan.
EM konda@kugi.kyoto-u.ac.jp
RI Ichikawa, Hiroshi/A-9523-2010
OI Ichikawa, Hiroshi/0000-0001-6576-0455
FU Kyoto University; Apan Aerospace Exploration Agency
FX The surface meteorological and oceanic data at KEO used in this study
were provided by NOAA/PMEL. The data of JKEO were obtained from
JAMSTEC/Research Institute for Global Change (RIGC). The observations
from the JKEO buoy were achieved under the collaboration in research
between JAMSTEC/RIGC and NOAA/PMEL. The reanalysis dataset used for this
study was obtained through the cooperative research project of the
JRA-25 long-term reanalysis by the Japan Meteorological Agency (JMA) and
the Central Research Institute of Electric Power Industry (CRIEPI). The
authors appreciate fruitful discussions with Akira Nagano, Hiroki
Tokinaga, and Yasushi Karino. Comments and suggestions from three
anonymous reviewers helped to clarify the focus of this manuscript. We
also appreciate the cooperation of the crew of the R/V Melville for the
deployment and the recovery of the KEO buoy and the R/V Mirai for the
deployment and the recovery of the JKEO1 buoy. This study is partly
supported by the Joint Research Program between Kyoto University and the
Japan Aerospace Exploration Agency (Evaluation of the sea surface flux
through the improvement of the wind speed derived by GCOM-W1 AMSR2).
NR 51
TC 22
Z9 22
U1 1
U2 4
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0894-8755
J9 J CLIMATE
JI J. Clim.
PD OCT
PY 2010
VL 23
IS 19
BP 5206
EP 5221
DI 10.1175/2010JCLI3391.1
PG 16
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 662RY
UT WOS:000282830500010
ER
PT J
AU Zhang, S
Rosati, A
Delworth, T
AF Zhang, S.
Rosati, A.
Delworth, T.
TI The Adequacy of Observing Systems in Monitoring the Atlantic Meridional
Overturning Circulation and North Atlantic Climate
SO JOURNAL OF CLIMATE
LA English
DT Article
ID OCEAN-ATMOSPHERE MODEL; THERMOHALINE CIRCULATION; DATA ASSIMILATION;
PART I; MULTIDECADAL VARIABILITY; SURFACE-TEMPERATURE; SEA; BIAS;
26.5-DEGREES-N; OSCILLATION
AB The Atlantic meridional overturning circulation (AMOC) has an important influence on climate, and yet adequate observations of this circulation are lacking. Here, the authors assess the adequacy of past and current widely deployed routine observing systems for monitoring the AMOC and associated North Atlantic climate. To do so, this study draws on two independent simulations of the twentieth century using an Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4) coupled climate model. One simulation is treated as "truth" and is sampled according to the observing system being evaluated. The authors then assimilate these synthetic "observations" into the second simulation within a fully coupled system that instantaneously exchanges information among all coupled components and produces a nearly balanced and coherent estimate for global climate states including the North Atlantic climate system. The degree to which the assimilation recovers the truth is an assessment of the adequacy of the observing system being evaluated. As the coupled system responds to the constraint of the atmosphere or ocean, the assessment of the recovery for climate quantities such as Labrador Sea Water (LSW) and the North Atlantic Oscillation increases the understanding of the factors that determine AMOC variability. For example, the low-frequency sea surface forcings provided by the atmospheric and sea surface temperature observations are found to excite a LSW variation that governs the long-time-scale variability of the AMOC. When the most complete modern observing system, consisting of atmospheric winds and temperature, is used along with Argo ocean temperature and salinity down to 2000 m, a skill estimate of AMOC reconstruction is 90% (out of 100% maximum). Similarly encouraging results hold for other quantities, such as the LSW. The past XBT observing system, in which deep-ocean temperature and salinity were not available, has a lesser ability to recover the truth AMOC (the skill is reduced to 52%). While these results raise concerns about the ability to properly characterize past variations of the AMOC, they also hold promise for future monitoring of the AMOC and for initializing prediction models.
C1 [Zhang, S.] Princeton Univ, GFDL, NOAA, Princeton, NJ 08542 USA.
RP Zhang, S (reprint author), Princeton Univ, GFDL, NOAA, POB 308, Princeton, NJ 08542 USA.
EM shaoqing.zhang@noaa.gov
RI Delworth, Thomas/C-5191-2014
NR 50
TC 14
Z9 14
U1 0
U2 2
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0894-8755
J9 J CLIMATE
JI J. Clim.
PD OCT
PY 2010
VL 23
IS 19
BP 5311
EP 5324
DI 10.1175/2010JCLI3677.1
PG 14
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 662RY
UT WOS:000282830500018
ER
PT J
AU Butchart, N
Cionni, I
Eyring, V
Shepherd, TG
Waugh, DW
Akiyoshi, H
Austin, J
Bruhl, C
Chipperfield, MP
Cordero, E
Dameris, M
Deckert, R
Dhomse, S
Frith, SM
Garcia, RR
Gettelman, A
Giorgetta, MA
Kinnison, DE
Li, F
Mancini, E
McLandress, C
Pawson, S
Pitari, G
Plummer, DA
Rozanov, E
Sassi, F
Scinocca, JF
Shibata, K
Steil, B
Tian, W
AF Butchart, Neal
Cionni, I.
Eyring, V.
Shepherd, T. G.
Waugh, D. W.
Akiyoshi, H.
Austin, J.
Bruehl, C.
Chipperfield, M. P.
Cordero, E.
Dameris, M.
Deckert, R.
Dhomse, S.
Frith, S. M.
Garcia, R. R.
Gettelman, A.
Giorgetta, M. A.
Kinnison, D. E.
Li, F.
Mancini, E.
McLandress, C.
Pawson, S.
Pitari, G.
Plummer, D. A.
Rozanov, E.
Sassi, F.
Scinocca, J. F.
Shibata, K.
Steil, B.
Tian, W.
TI Chemistry-Climate Model Simulations of Twenty-First Century
Stratospheric Climate and Circulation Changes
SO JOURNAL OF CLIMATE
LA English
DT Article
ID MIDDLE ATMOSPHERE MODEL; GRAVITY-WAVE DRAG; BREWER-DOBSON CIRCULATION;
MIXED GREENHOUSE GASES; ANTARCTIC OZONE HOLE; METEOROLOGICAL ANALYSES;
INTERACTIVE CHEMISTRY; TROPOSPHERE EXCHANGE; CLOUD FORMATION;
WATER-VAPOR
AB The response of stratospheric climate and circulation to increasing amounts of greenhouse gases (GHGs) and ozone recovery in the twenty-first century is analyzed in simulations of 11 chemistry-climate models using near-identical forcings and experimental setup. In addition to an overall global cooling of the stratosphere in the simulations (0.59 +/- 6 0.07 K decade(-1) at 10 hPa), ozone recovery causes a warming of the Southern Hemisphere polar lower stratosphere in summer with enhanced cooling above. The rate of warming correlates with the rate of ozone recovery projected by the models and, on average, changes from 0.8 to 0.48 K decade(-1) at 100 hPa as the rate of recovery declines from the first to the second half of the century. In the winter northern polar lower stratosphere the increased radiative cooling from the growing abundance of GHGs is, in most models, balanced by adiabatic warming from stronger polar downwelling. In the Antarctic lower stratosphere the models simulate an increase in low temperature extremes required for polar stratospheric cloud (PSC) formation, but the positive trend is decreasing over the twenty-first century in all models. In the Arctic, none of the models simulates a statistically significant increase in Arctic PSCs throughout the twenty-first century. The subtropical jets accelerate in response to climate change and the ozone recovery produces a westward acceleration of the lower-stratospheric wind over the Antarctic during summer, though this response is sensitive to the rate of recovery projected by the models. There is a strengthening of the Brewer-Dobson circulation throughout the depth of the stratosphere, which reduces the mean age of air nearly everywhere at a rate of about 0.05 yr decade(-1) in those models with this diagnostic. On average, the annual mean tropical upwelling in the lower stratosphere (similar to 70 hPa) increases by almost 2% decade(-1), with 59% of this trend forced by the parameterized orographic gravity wave drag in the models. This is a consequence of the eastward acceleration of the subtropical jets, which increases the upward flux of (parameterized) momentum reaching the lower stratosphere in these latitudes.
C1 [Butchart, Neal] Hadley Ctr, Met Off, Exeter EX1 3PB, Devon, England.
[Cionni, I.; Eyring, V.; Dameris, M.; Deckert, R.] Deutsch Zentrum Luft & Raumfahrt, Oberpfaffenhofen, Germany.
[Shepherd, T. G.; McLandress, C.] Univ Toronto, Toronto, ON, Canada.
[Waugh, D. W.] Johns Hopkins Univ, Baltimore, MD USA.
[Akiyoshi, H.] Natl Inst Environm Studies, Tsukuba, Ibaraki, Japan.
[Austin, J.] Geophys Fluid Dynam Lab, Princeton, NJ USA.
[Bruehl, C.; Steil, B.] Max Planck Inst Chem, D-55128 Mainz, Germany.
[Chipperfield, M. P.; Dhomse, S.; Tian, W.] Univ Leeds, Leeds, W Yorkshire, England.
[Cordero, E.] San Jose State Univ, San Jose, CA 95192 USA.
[Frith, S. M.] Sci Syst & Applicat Inc, Lanham, MD USA.
[Garcia, R. R.; Gettelman, A.; Kinnison, D. E.] Natl Ctr Atmospher Res, Boulder, CO 80307 USA.
[Giorgetta, M. A.] Max Planck Inst Meteorol, Hamburg, Germany.
[Li, F.] Univ Maryland Baltimore Cty, Baltimore, MD 21228 USA.
[Mancini, E.; Pitari, G.] Univ Aquila, I-67100 Laquila, Italy.
[Pawson, S.] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
[Plummer, D. A.] Environm Canada, Toronto, ON, Canada.
[Rozanov, E.] World Radiat Ctr, Phys Meteorol Observ, Davos, Switzerland.
[Rozanov, E.] Swiss Fed Inst Technol, Zurich, Switzerland.
[Sassi, F.] USN, Res Lab, Washington, DC 20375 USA.
[Scinocca, J. F.] Univ Victoria, Meteorol Serv Canada, Victoria, BC, Canada.
[Shibata, K.] Meteorol Res Inst, Tsukuba, Ibaraki 305, Japan.
RP Butchart, N (reprint author), Hadley Ctr, Met Off, FitzRoy Rd, Exeter EX1 3PB, Devon, England.
EM neal.butchart@metoffice.gov.uk
RI Eyring, Veronika/O-9999-2016; Dhomse, Sandip/C-8198-2011; Rozanov,
Eugene/A-9857-2012; Li, Feng/H-2241-2012; Chipperfield,
Martyn/H-6359-2013; Pawson, Steven/I-1865-2014; Waugh,
Darryn/K-3688-2016; Pitari, Giovanni/O-7458-2016
OI Eyring, Veronika/0000-0002-6887-4885; Mancini, Eva/0000-0001-7071-0292;
Sassi, Fabrizio/0000-0002-9492-7434; Dhomse, Sandip/0000-0003-3854-5383;
Rozanov, Eugene/0000-0003-0479-4488; Chipperfield,
Martyn/0000-0002-6803-4149; Pawson, Steven/0000-0003-0200-717X; Waugh,
Darryn/0000-0001-7692-2798; Pitari, Giovanni/0000-0001-7051-9578
FU European Commission [505390-GOCE-CT-2004]; DECC [GA01101]; Defra
[GA01101]; MoD [CBC/2B/0417_Annex C5]; SCOUT [O3]; Ministry of the
Environment (MOE) of Japan [A-071]; Canadian Foundation for Climate and
Atmospheric Sciences
FX The authors acknowledge the Chemistry-Climate Model Validation Activity
(CCMVal) of the WCRP's (World Climate Research Programme) SPARC
(Stratospheric Processes and their Role in Climate) project for
organizing and coordinating the model data analysis activity, and the
British Atmospheric Data Centre (BADC) for collecting and archiving the
CCMVal model output. The European groups acknowledge support of the EC
Integrated Project SCOUT-O3 (505390-GOCE-CT-2004) funded by the European
Commission. Dr. Butchart's research was supported by the Joint DECC,
Defra, and MoD Integrated Climate Programme-DECC/Defra (GA01101), MoD
(CBC/2B/0417_Annex C5), and SCOUT-O3. CCSR/NIES research was supported
by the Global Environmental Research Fund (GERF) of the Ministry of the
Environment (MOE) of Japan (A-071). The CMAM research was supported by
the Canadian Foundation for Climate and Atmospheric Sciences through the
C-SPARC project. GEOS CCM simulations were conducted on NASA's
High-Performance computing resources at NASA Ames Research Center. The
MRI simulation was made with the supercomputer at the National Institute
for Environmental Studies, Japan.
NR 81
TC 136
Z9 137
U1 4
U2 79
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0894-8755
EI 1520-0442
J9 J CLIMATE
JI J. Clim.
PD OCT
PY 2010
VL 23
IS 20
BP 5349
EP 5374
DI 10.1175/2010JCLI3404.1
PG 26
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 681IW
UT WOS:000284306200001
ER
PT J
AU Cuddalorepatta, G
Williams, M
Dasgupta, A
AF Cuddalorepatta, Gayatri
Williams, Maureen
Dasgupta, Abhijit
TI Viscoplastic Creep Response and Microstructure of As-Fabricated
Microscale Sn-3.0Ag-0.5Cu Solder Interconnects
SO JOURNAL OF ELECTRONIC MATERIALS
LA English
DT Article
DE Lead-free solder; grains; creep; viscoplastic; primary creep; secondary
creep; recrystallization
ID LEAD-FREE SOLDER; SMALL LENGTH SCALES; AG-CU SOLDER;
DEFORMATION-BEHAVIOR; SN-3.5AG SOLDER; THERMOMECHANICAL FATIGUE;
INTERMETALLIC COMPOUNDS; MECHANICAL-PROPERTIES; SOLDER/COPPER JOINTS;
THERMAL FATIGUE
AB The viscoplastic behavior of as-fabricated, undamaged, microscale Sn-3.0 Ag-0.5Cu (SAC305) Pb-free solder is investigated and compared with that of eutectic Sn-37Pb solder and near-eutectic Sn-3.8Ag-0.7Cu (SAC387) solder from prior studies. Creep measurements of microscale SAC305 solder shear specimens show significant piece-to-piece variability under identical loading. Orientation imaging microscopy reveals that these specimens contain only a few, highly anisotropic Sn grains across the entire joint. For the studied loads, the coarse-grained Sn microstructure has a more significant impact on the scatter in primary creep compared to that in the secondary creep. The observed lack of statistical homogeneity (microstructure) and joint-dependent mechanical behavior of microscale SAC305 joints are consistent with those observed for functional microelectronics interconnects. Compared with SAC305 joints, microscale Sn-37Pb shear specimens exhibit more homogenous behavior and microstructure with a large number of small Sn (and Pb) grains. Creep damage in the Pb-free joint is predominantly concentrated at highly misoriented Sn grain boundaries. The coarse-grained Sn microstructure recrystallizes into new grains with high misorientation angles under creep loading. In spite of the observed joint-dependent behavior, as-fabricated SAC305 is significantly more creep resistant than Sn-37Pb solder and slightly less creep resistant than near-eutectic SAC387 solder. Average model constants for primary and secondary creep of SAC305 are presented. Since the viscoplastic measurements are averaged over a wide range of grain configurations, the creep model constants represent the effective continuum behavior in an average sense. The average secondary creep behavior suggests that the dominant creep mechanism is dislocation climb assisted by dislocation pipe diffusion.
C1 [Cuddalorepatta, Gayatri; Dasgupta, Abhijit] Univ Maryland, CALCE Elect Prod & Syst Ctr, Dept Mech Engn, College Pk, MD 20742 USA.
[Williams, Maureen] Natl Inst Stand & Technol, Mat Sci & Engn Lab, Gaithersburg, MD 20899 USA.
RP Cuddalorepatta, G (reprint author), Univ Maryland, CALCE Elect Prod & Syst Ctr, Dept Mech Engn, College Pk, MD 20742 USA.
EM gayatric@umd.edu
RI Cuddalorepatta, Gayatri/A-5536-2011
FU Zonta International and Surface Mount Technology Association (SMTA)
FX This work is sponsored by the members of the CALCE Electronic Products
and Systems Consortium at the University of Maryland, College Park. In
addition, Ms. Cuddalorepatta would like to acknowledge Drs. Kil-Won
Moon, Mark Vaudin, and Adam Creuziger from National Institute of
Standards and Technology for their technical inputs on the OIM
measurements, and the support of Zonta International and Surface Mount
Technology Association (SMTA). The assistance of Roman Kuehner and Ermal
Lamaj for the TMM specimen fabrication is greatly appreciated.
NR 61
TC 17
Z9 17
U1 0
U2 5
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0361-5235
J9 J ELECTRON MATER
JI J. Electron. Mater.
PD OCT
PY 2010
VL 39
IS 10
BP 2292
EP 2309
DI 10.1007/s11664-010-1296-z
PG 18
WC Engineering, Electrical & Electronic; Materials Science,
Multidisciplinary; Physics, Applied
SC Engineering; Materials Science; Physics
GA 662EJ
UT WOS:000282789800018
ER
PT J
AU Quan, P
Lai, MC
Hussey, DS
Jacobson, DL
Kumar, A
Hirano, S
AF Quan, P.
Lai, M. -C.
Hussey, D. S.
Jacobson, D. L.
Kumar, A.
Hirano, S.
TI Time-Resolved Water Measurement in a PEM Fuel Cell Using High-Resolution
Neutron Imaging Technique
SO JOURNAL OF FUEL CELL SCIENCE AND TECHNOLOGY
LA English
DT Article
DE water transport; PEM fuel cell; neutron imaging technique; dynamic
process; time constant
ID 2-PHASE FLOW PHENOMENA; RADIOGRAPHY; PART; QUANTIFICATION; TRANSPORT
AB The dynamic process of water transport along the through-plane direction in the membrane electrode assembly of a proton exchange membrane fuel cell was investigated using the high-resolution neutron imaging. Four different membrane/gas diffusion layer or membrane/gas diffusion electrode assemblies were tested by measuring the through-plane water thickness profiles. The results indicate that proper design and assembly of the test fixture are critical for accurate water measurement; the accumulation speed of liquid water inside an assembly varies with time; the ionomer in catalyst layers could facilitate water management in the membrane; the time constants for wetting and drying processes are functions of gas diffusion layer thickness, inlet flow rate, and gas dew point; and the time constant for the wetting process is about 1.4 times longer than the corresponding drying process. [DOI: 10.1115/1.4001017]
C1 [Quan, P.; Lai, M. -C.] Wayne State Univ, Dept Mech Engn, Detroit, MI 48202 USA.
[Hussey, D. S.; Jacobson, D. L.] Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
[Kumar, A.; Hirano, S.] Ford Motor Co, Dearborn, MI 48121 USA.
RP Quan, P (reprint author), Wayne State Univ, Dept Mech Engn, Detroit, MI 48202 USA.
EM pquan@wayne.edu
FU U.S. Department of Commerce; NIST Ionizing Radiation Division;
Director's office of NIST; NIST Center for Neutron Research; Department
of Energy [DE-AI01-01EE50660]
FX This work was supported by the U.S. Department of Commerce, the NIST
Ionizing Radiation Division, the Director's office of NIST, the NIST
Center for Neutron Research, and the Department of Energy through
interagency Agreement No. DE-AI01-01EE50660. The support of Mr. Shinichi
Hirano of Ford Motor Co., Ford University Research Program is greatly
appreciated as well.
NR 11
TC 5
Z9 5
U1 0
U2 10
PU ASME-AMER SOC MECHANICAL ENG
PI NEW YORK
PA THREE PARK AVE, NEW YORK, NY 10016-5990 USA
SN 1550-624X
J9 J FUEL CELL SCI TECH
JI J. Fuel Cell Sci. Technol.
PD OCT
PY 2010
VL 7
IS 5
AR 051009
DI 10.1115/1.4001017
PG 6
GA 628TH
UT WOS:000280144100009
ER
PT J
AU Luke, EP
Kollias, P
Shupe, MD
AF Luke, Edward P.
Kollias, Pavlos
Shupe, Matthew D.
TI Detection of supercooled liquid in mixed-phase clouds using radar
Doppler spectra
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID RADIATION MEASUREMENT PROGRAM; CLIMATE RESEARCH; ARCTIC SURFACE; LIDAR;
ICE; SHEBA; TURBULENCE; SENSORS; SEA
AB Cloud phase identification from active remote sensors in the temperature range from 0 to 40 degrees C, where both liquid and ice hydrometeor phases are sustainable, is challenging. Millimeter wavelength cloud radars (MMCR) are able to penetrate and detect multiple cloud layers. However, in mixed-phase conditions, ice crystals dominate the radar signal, rendering the detection of liquid droplets from radar observables more difficult. The technique proposed here overcomes this fundamental limitation by using morphological features in MMCR Doppler spectra to detect supercooled liquid droplets in the radar sampling volume in the presence of ice particles. High lidar backscatter and near-zero lidar depolarization measurements (good indicators of the presence of liquid droplets) from the Mixed-Phase Arctic Clouds Experiment (MPACE) conducted in Barrow, Alaska, are used to train the technique and evaluate its potential for detecting mixed-phase conditions. Ceilometer, microwave radiometer, and radiosonde measurements provide additional independent validation. Because of the ability of MMCRs to penetrate multiple liquid layers, this radar-based technique does not suffer from the extinction limitations of lidars and is thus able to expand cloud phase identification methods to cloud regions beyond where lidars can penetrate, providing output at the native radar resolution. The technique is applicable to all profiling radars that have sufficient sensitivity to observe the small amount of liquid in mixed-phase clouds.
C1 [Luke, Edward P.] Brookhaven Natl Lab, Div Atmospher Sci, Upton, NY 11973 USA.
[Kollias, Pavlos] McGill Univ, Dept Atmospher & Ocean Sci, Montreal, PQ H3A 2K6, Canada.
[Shupe, Matthew D.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Shupe, Matthew D.] NOAA, Boulder, CO USA.
RP Luke, EP (reprint author), Brookhaven Natl Lab, Div Atmospher Sci, Bldg 490D,Bell Ave, Upton, NY 11973 USA.
EM eluke@bnl.gov
RI Shupe, Matthew/F-8754-2011
OI Shupe, Matthew/0000-0002-0973-9982
FU Office of Science (BER), U. S. Department of Energy [DE-FG02-05ER63965]
FX This research was supported by the Office of Science (BER), U. S.
Department of Energy, grant DE-FG02-05ER63965. Data were obtained from
the ARM archive and University of Wisconsin.
NR 38
TC 18
Z9 18
U1 2
U2 10
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 2169-897X
J9 J GEOPHYS RES-ATMOS
JI J. Geophys. Res.-Atmos.
PD OCT 1
PY 2010
VL 115
AR D19201
DI 10.1029/2009JD012884
PG 14
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 658RQ
UT WOS:000282507500003
ER
PT J
AU Lundquist, JD
Minder, JR
Neiman, PJ
Sukovich, E
AF Lundquist, Jessica D.
Minder, Justin R.
Neiman, Paul J.
Sukovich, Ellen
TI Relationships between Barrier Jet Heights, Orographic Precipitation
Gradients, and Streamflow in the Northern Sierra Nevada
SO JOURNAL OF HYDROMETEOROLOGY
LA English
DT Article
ID CLIMATOLOGICAL PRECIPITATION; SPATIAL-DISTRIBUTION; MOIST DYNAMICS; WIND
PROFILER; CALIFORNIA; MOUNTAINS; MODEL; FLOW; RAINFALL; STORMS
AB The rate of precipitation increase with elevation, termed the orographic precipitation gradient (OPG), is critically important for hydrologic forecasting in mountain basins that receive both rain and snow. Here, the following are examined to see how well they are able to predict the OPG and how it changes between storms and years: 1) a linear model of orographic precipitation forced by upstream radiosonde data, 2) monthly Parameter-Elevation Regressions on Independent Slopes Model (PRISM) precipitation data, and 3) seven years of hourly wind profiler data used to identify characteristics of the Sierra barrier jet (SBJ). These are compared against 124 daily resolution (four of which also had quality controlled, hourly resolution) precipitation gauge records in the northern Sierra Nevada. All methods represent the OPG well in the mean and during a year when less than 30% of the precipitation occurred on days with SBJs. However, the linear model and PRISM do not adequately capture annual variations in the OPG during years when more than 70% of the precipitation occurred on days with SBJs. Throughout all of the years, wind profiler data indicating the height of the SBJ provided additional, and necessary, information. The OPG is negatively correlated with the height of the SBJ. The SBJ height is lower, and hence, the OPG greater when the westerly winds are stronger, with more vertical wind shear. These westerly storms result in greater increases of precipitation with elevation, which act to increase snow storage in most storms but also to increase storm runoff during warmer-than-average storms.
C1 [Lundquist, Jessica D.] Univ Washington, Dept Civil & Environm Engn, Seattle, WA 98195 USA.
[Minder, Justin R.] Univ Washington, Dept Atmospher Sci, Seattle, WA 98195 USA.
[Neiman, Paul J.; Sukovich, Ellen] NOAA Earth Syst Res Lab, Div Phys Sci, Boulder, CO USA.
[Sukovich, Ellen] Univ Colorado, CIRES, Boulder, CO 80309 USA.
RP Lundquist, JD (reprint author), Univ Washington, Dept Civil & Environm Engn, Seattle, WA 98195 USA.
EM jdlund@u.washington.edu
FU NOAA [NA17RJ1232]; NSF [EAR-0838166, EAR-0642835]
FX This work was primarily supported by the NOAA HMT project. JDL
acknowledges support from NOAA Grant NA17RJ1232 and NSF Grant
EAR-0838166. JRM acknowledges support from NSF Grant EAR-0642835. The
authors thank the dedicated NOAA/ESRL staff who installed the radar
profiler. In addition, we thank the CADWR and cooperators for providing
daily and hourly precipitation records across the region and Noah
Knowles for automating the downloading of CDEC data and making it
available. Finally, thank you to Editor Barros and three anonymous
reviewers for their helpful comments and to Mark Raleigh, Jeff Deems,
Steve Burges, and Andrey Shcherbina for scientific conversations
regarding this material.
NR 69
TC 41
Z9 41
U1 3
U2 18
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 1525-755X
J9 J HYDROMETEOROL
JI J. Hydrometeorol.
PD OCT
PY 2010
VL 11
IS 5
BP 1141
EP 1156
DI 10.1175/2010JHM1264.1
PG 16
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 661DE
UT WOS:000282702400005
ER
PT J
AU Zhang, JA
Qi, YC
AF Zhang, Jian
Qi, Youcun
TI A Real-Time Algorithm for the Correction of Brightband Effects in
Radar-Derived QPE
SO JOURNAL OF HYDROMETEOROLOGY
LA English
DT Article
ID VERTICAL PROFILES; UNITED-STATES; OPERATIONAL RADAR; MELTING-LAYER;
PRECIPITATION MEASUREMENTS; RAINFALL PRODUCT; REFLECTIVITY;
IDENTIFICATION; WSR-88D; RANGE
AB The bright band (BB) is a layer of enhanced reflectivity due to melting of aggregated snow and ice crystals. The locally high reflectivity causes significant overestimation in radar precipitation estimates if an appropriate correction is not applied. The main objective of the current study is to develop a method that automatically corrects for large errors due to BB effects in a real-time national radar quantitative precipitation estimation (QPE) product. An approach that combines the mean apparent vertical profile of reflectivity (VPR) computed from a volume scan of radar reflectivity observations and an idealized linear VPR model was used for computational efficiency. The methodology was tested for eight events from different regions and seasons in the United States. The VPR correction was found to be effective and robust in reducing overestimation errors in radar-derived QPE, and the corrected radar precipitation fields showed physically continuous distributions. The correction worked consistently well for radars in flat land regions because of the relatively uniform spatial distributions of the BB in those areas. For radars in mountainous regions, the performance of the correction is mixed because of limited radar visibility in addition to large spatial variations of the vertical precipitation structure due to underlying topography.
C1 [Zhang, Jian] NOAA OAR Natl Severe Storms Lab, Norman, OK USA.
[Qi, Youcun] Nanjing Univ Informat Sci & Technol, Nanjing, Peoples R China.
[Qi, Youcun] Univ Oklahoma, Cooperat Inst Mesoscale Meteorol Studies, Norman, OK 73019 USA.
RP Zhang, JA (reprint author), NSSL WRDD, 120 David L Boren Blvd, Norman, OK 73072 USA.
EM jian.zhang@noaa.gov
FU NOAA; NOAA-University of Oklahoma [NA17RJ1227]
FX Major funding for this research was provided under NOAA's
Hydro-Meteorological Testbed (HMT) program and partial funding was
provided under NOAA-University of Oklahoma Cooperative Agreement
NA17RJ1227. The authors thank Kenneth Howard for many insightful
discussions during this study. This manuscript has greatly benefited
from the comments of anonymous reviewers, and from the comments of Drs.
David Jorgensen, J. J. Gourley, Alexander Ryzhkov, and David Kingsmill.
NR 35
TC 44
Z9 49
U1 1
U2 4
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 1525-755X
J9 J HYDROMETEOROL
JI J. Hydrometeorol.
PD OCT
PY 2010
VL 11
IS 5
BP 1157
EP 1171
DI 10.1175/2010JHM1201.1
PG 15
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 661DE
UT WOS:000282702400006
ER
PT J
AU Lu, CG
Yuan, HL
Tollerud, EI
Wang, N
AF Lu, Chungu
Yuan, Huiling
Tollerud, Edward I.
Wang, Ning
TI Scale-dependent uncertainties in global QPFs and QPEs from NWP model and
satellite fields (vol 11, pg 139, 2010)
SO JOURNAL OF HYDROMETEOROLOGY
LA English
DT Correction
C1 [Lu, Chungu; Wang, Ning] Colorado State Univ, CIRA, Ft Collins, CO 80523 USA.
[Lu, Chungu; Yuan, Huiling; Tollerud, Edward I.; Wang, Ning] NOAA ESRL Global Syst Div, Boulder, CO USA.
[Yuan, Huiling] Univ Colorado, CIRES, Boulder, CO 80309 USA.
RP Lu, CG (reprint author), Colorado State Univ, CIRA, Ft Collins, CO 80523 USA.
EM huiling.yuan@noaa.gov
RI Yuan, Huiling/G-9795-2013
NR 1
TC 0
Z9 0
U1 0
U2 0
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 1525-755X
J9 J HYDROMETEOROL
JI J. Hydrometeorol.
PD OCT
PY 2010
VL 11
IS 5
BP 1200
EP 1200
DI 10.1175/2010JHM1332.1
PG 1
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA 661DE
UT WOS:000282702400011
ER
PT J
AU Chin, J
Forster, A
Ocel, J
Hartmann, J
Fuchs, P
Hunston, D
AF Chin, Joannie
Forster, Aaron
Ocel, Justin
Hartmann, Joseph
Fuchs, Paul
Hunston, Donald
TI Thermoviscoelastic Analysis and Creep Testing of Ambient Temperature
Cure Epoxies Used in Adhesive Anchor Applications
SO JOURNAL OF MATERIALS IN CIVIL ENGINEERING
LA English
DT Article
DE Epoxy; Adhesives; Dynamic mechanical thermal analysis; Time-temperature
superposition; Creep compliance; Adhesive anchors
ID POLYMERS
AB Thermoviscoelastic properties and creep response of two commercial ambient temperature cure epoxy structural adhesives were analyzed and compared. The adhesives were formulated by the same manufacturer and appeared to be chemically similar; however, one system contained accelerators to shorten its cure time. In the laboratory, dynamic mechanical temperature/frequency sweeps were performed on both systems to generate dynamic mechanical and creep compliance master curves using time-temperature superposition principles. Differences were observed in the dynamic mechanical properties of the two adhesive systems as well as in their calculated creep compliance, which have been attributed to differences in their curing agent(s) and accelerator(s). Full-scale creep tests were carried out on anchors installed in concrete slabs and subjected to sustained loads for 82 days. These results were in good agreement with the creep compliance estimated using time-temperature superposition, suggesting that dynamic mechanical testing can be a useful metrology for characterizing trends in creep behavior.
C1 [Chin, Joannie; Forster, Aaron; Hunston, Donald] NIST, Bldg & Fire Res Lab, Gaithersburg, MD 20899 USA.
[Ocel, Justin; Hartmann, Joseph] Fed Hwy Adm, Turner Fairbank Hwy Res Ctr, Mclean, VA 22101 USA.
[Fuchs, Paul] Fuchs Consulting Inc, Leesburg, VA 20176 USA.
RP Chin, J (reprint author), NIST, Bldg & Fire Res Lab, Gaithersburg, MD 20899 USA.
EM joannie.chin@nist.gov; aaron.forster@nist.gov; justin.ocel@fhwa.dot.gov;
joey.hartmann@fhwa.dot.gov; paul.fuchs@fuchsconsultinginc.com;
donald.hunston@nist.gov
NR 13
TC 5
Z9 5
U1 0
U2 7
PU ASCE-AMER SOC CIVIL ENGINEERS
PI RESTON
PA 1801 ALEXANDER BELL DR, RESTON, VA 20191-4400 USA
SN 0899-1561
J9 J MATER CIVIL ENG
JI J. Mater. Civ. Eng.
PD OCT
PY 2010
VL 22
IS 10
BP 1039
EP 1046
DI 10.1061/(ASCE)MT.1943-5533.0000108
PG 8
WC Construction & Building Technology; Engineering, Civil; Materials
Science, Multidisciplinary
SC Construction & Building Technology; Engineering; Materials Science
GA 650RY
UT WOS:000281870700011
ER
PT J
AU Shah, JJ
Geist, J
Gaitan, M
AF Shah, Jayna J.
Geist, Jon
Gaitan, Michael
TI Microwave-induced adjustable nonlinear temperature gradients in
microfluidic devices
SO JOURNAL OF MICROMECHANICS AND MICROENGINEERING
LA English
DT Article
ID DNA MUTATION DETECTION; CHIP; ELECTROPHORESIS; SYSTEMS; MICROCHIP
AB We describe on-chip microwave generation of spatial temperature gradients in a polymeric microfluidic device that includes an integrated microstrip transmission line. The transmission line was fabricated photolithographically on commercially available adhesive copper tape. The fluid temperature during microwave heating was measured by observing the temperature-dependent fluorescence intensity of a dye solution in the microchannel. Large interference effects, which were produced by superposition of a sinusoidal and two exponential temperature distributions, were measured at 12 GHz and 19 GHz. Temperature extremes of 31 degrees C and 53 degrees C at the minimum and maximum of the sinusoid were established within 1 s. The sinusoid also produced a quasilinear temperature gradient along a 2 mm distance with a slope of 7.3 degrees C mm(-1). This technique has the potential to benefit many biological, chemical and physical applications requiring rapid temperature gradients.
C1 [Shah, Jayna J.; Geist, Jon; Gaitan, Michael] Natl Inst Stand & Technol, Div Semicond Elect, Gaithersburg, MD 20899 USA.
RP Shah, JJ (reprint author), Natl Inst Stand & Technol, Div Semicond Elect, 100 Bur Dr,Stop 8120, Gaithersburg, MD 20899 USA.
EM jjshah@ieee.org; gaitan@nist.gov
OI Geist, Jon/0000-0001-7749-318X
FU Office of Science and Technology of the National Institute of Justice
FX This research was performed while JJS held a National Research Council
(NRC) Research Associateship Award at the Electronics and Electrical
Engineering Laboratory (EEEL) of NIST. We thank J Atencia, S Leigh and B
Nablo for helpful discussions. We also thank the Office of Science and
Technology of the National Institute of Justice for providing part of
the support for this work. Device fabrication was performed in part at
the NIST Center for Nanoscale Science and Technology's Nanofab facility
in Gaithersburg, MD.
NR 50
TC 8
Z9 8
U1 0
U2 14
PU IOP PUBLISHING LTD
PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0960-1317
EI 1361-6439
J9 J MICROMECH MICROENG
JI J. Micromech. Microeng.
PD OCT
PY 2010
VL 20
IS 10
AR 105025
DI 10.1088/0960-1317/20/10/105025
PG 8
WC Engineering, Electrical & Electronic; Nanoscience & Nanotechnology;
Instruments & Instrumentation; Physics, Applied
SC Engineering; Science & Technology - Other Topics; Instruments &
Instrumentation; Physics
GA 655SR
UT WOS:000282270300038
ER
PT J
AU Fan, YL
Ginis, I
Hara, T
AF Fan, Yalin
Ginis, Isaac
Hara, Tetsu
TI Momentum Flux Budget across the Air-Sea Interface under Uniform and
Tropical Cyclone Winds
SO JOURNAL OF PHYSICAL OCEANOGRAPHY
LA English
DT Article
ID SURFACE-WAVE EQUATIONS; 3-DIMENSIONAL CURRENT; DRAG COEFFICIENT;
GENERATED WAVES; PART I; OCEAN; MODEL; SPECTRA; SIMULATIONS; EXCHANGE
AB In coupled ocean-atmosphere models, it is usually assumed that the momentum flux into ocean currents is equal to the flux from air (wind stress). However, when the surface wave field grows (decays) in space or time, it gains (loses) momentum and reduces (increases) the momentum flux into subsurface currents compared to the flux from the wind. In particular, under tropical cyclone (TC) conditions the surface wave field is complex and fast varying in space and time and may significantly affect the momentum flux from wind into ocean. In this paper, numerical experiments are performed to investigate the momentum flux budget across the air-sea interface under both uniform and idealized TC winds. The wave fields are simulated using the WAVEWATCH III model. The difference between the momentum flux from wind and the flux into currents is estimated using an air-sea momentum flux budget model. In many of the experiments, the momentum flux into currents is significantly reduced relative to the flux from the wind. The percentage of this reduction depends on the choice of the drag coefficient parameterization and can be as large as 25%. For the TC cases, the reduction is mainly in the right-rear quadrant of the hurricane, and the percentage of the flux reduction is insensitive to the changes of the storm size and the asymmetry in the wind field but varies with the TC translation speed and the storm intensity. The results of this study suggest that it is important to explicitly resolve the effect of surface waves for accurate estimations of the momentum flux into currents under TCs.
C1 [Fan, Yalin] Princeton Univ, Atmospher & Ocean Sci Program, Princeton, NJ 08540 USA.
[Fan, Yalin] NOAA Geophys Fluid Dynam Lab, Princeton, NJ USA.
[Ginis, Isaac; Hara, Tetsu] Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA.
RP Fan, YL (reprint author), Princeton Univ, Atmospher & Ocean Sci Program, 300 Forrestal Rd, Princeton, NJ 08540 USA.
EM yalinfan@princeton.edu
RI Hara, Tetsu/G-9779-2011
FU U.S. National Science Foundation [ATM 0406895]; WeatherPredict
Consulting Inc.; U.S. Office of Naval Research [N00014-06-10729]; Korea
Research and Development Institute [500-2802-0000-0001377]
FX This work was supported by the U.S. National Science Foundation through
Grants ATM 0406895 and WeatherPredict Consulting Inc. via a grant to the
URI Foundation. TH and IG also thank the U.S. Office of Naval Research
(CBLAST program, Grant N00014-06-10729) and the Korea Research and
Development Institute (Grant 500-2802-0000-0001377) for additional
support.
NR 39
TC 8
Z9 9
U1 0
U2 3
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0022-3670
J9 J PHYS OCEANOGR
JI J. Phys. Oceanogr.
PD OCT
PY 2010
VL 40
IS 10
BP 2221
EP 2242
DI 10.1175/2010JPO4299.1
PG 22
WC Oceanography
SC Oceanography
GA 665RO
UT WOS:000283053400002
ER
PT J
AU Farneti, R
Delworth, TL
AF Farneti, Riccardo
Delworth, Thomas L.
TI The Role of Mesoscale Eddies in the Remote Oceanic Response to Altered
Southern Hemisphere Winds
SO JOURNAL OF PHYSICAL OCEANOGRAPHY
LA English
DT Article
ID ANTARCTIC CIRCUMPOLAR CURRENT; CIRCULATION MODELS; CLIMATE MODELS;
TRANSPORT
AB It has been suggested that a strengthening of the Southern Hemisphere winds would induce a more vigorous overturning through an increased northward Ekman flux, bringing more light waters into the oceanic basins and enhancing the upwelling of North Atlantic Deep Water in the Southern Ocean, thereby increasing ocean ventilation. Simulations from a coarse-and a fine-resolution version of a coupled model, subject to idealized wind stress changes in the Southern Ocean, are presented. In the fine-resolution eddy-permitting model, changes in poleward eddy fluxes largely compensate for the enhanced equatorward Ekman transport in the Southern Ocean. As a consequence, northward transport of light waters, pycnocline depth, Northern Hemisphere overturning, and Southern Ocean upwelling anomalies are much reduced compared with simulations in the coarse-resolution model with parameterized eddies. These results suggest a relatively weak sensitivity of present-day global ocean overturning circulation to the projected strengthening of the Southern Hemisphere winds.
C1 [Farneti, Riccardo] Princeton Univ, Atmospher & Ocean Sci Program, Princeton, NJ 08544 USA.
[Delworth, Thomas L.] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA.
RP Farneti, R (reprint author), ICTP, Earth Syst Phys Sect, Str Costiera 11, I-34151 Trieste, Italy.
EM rfarneti@ictp.it
RI Farneti, Riccardo/B-5183-2011; Delworth, Thomas/C-5191-2014
NR 22
TC 45
Z9 45
U1 0
U2 9
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0022-3670
J9 J PHYS OCEANOGR
JI J. Phys. Oceanogr.
PD OCT
PY 2010
VL 40
IS 10
BP 2348
EP 2354
DI 10.1175/2010JPO4480.1
PG 7
WC Oceanography
SC Oceanography
GA 665RO
UT WOS:000283053400011
ER
PT J
AU Mason, G
Dragovich, J
AF Mason, Greg
Dragovich, Jeff
TI Program Assessment and Evaluation Using Student Grades Obtained on
Outcome-Related Course Learning Objectives
SO JOURNAL OF PROFESSIONAL ISSUES IN ENGINEERING EDUCATION AND PRACTICE
LA English
DT Article
DE Assessment; Education; ABET
AB A methodology was developed for assessing student performance with respect to program outcomes and course objectives using available graded coursework. The methodology uses a matrix formulation to relate individual coursework problems to program outcomes and course objectives. Assessment data and required mapping matrices are collected in spreadsheet form and automatically transferred to a relational database. Student and class performance with respect to program objectives is calculated using Structured Query Language (SQL) queries and data fitting through least-squares. The methodology was used to collect data, assess student performance, and identify necessary program changes over a four-year period in an engineering program.
C1 [Mason, Greg] Seattle Univ, Dept Mech Engn, Seattle, WA 98122 USA.
[Dragovich, Jeff] Seattle Univ, Dept Civil & Environm Engn, Seattle, WA 98122 USA.
[Dragovich, Jeff] NIST, Natl Earthquake Hazards Reduct Program, Bldg & Fire Res Lab MS 8604, Gaithersburg, MD 20899 USA.
RP Mason, G (reprint author), Seattle Univ, Dept Mech Engn, 901 12th Ave, Seattle, WA 98122 USA.
EM mason@seattleu.edu; jeff.dragovich@nist.gov
NR 18
TC 0
Z9 0
U1 3
U2 4
PU ASCE-AMER SOC CIVIL ENGINEERS
PI RESTON
PA 1801 ALEXANDER BELL DR, RESTON, VA 20191-4400 USA
SN 1052-3928
J9 J PROF ISS ENG ED PR
JI J. Prof. Issues Eng. Educ. Pract.
PD OCT
PY 2010
VL 136
IS 4
BP 206
EP 214
DI 10.1061/(ASCE)EI.1943-5541.0000029
PG 9
WC Education, Scientific Disciplines; Engineering, Multidisciplinary
SC Education & Educational Research; Engineering
GA 650OC
UT WOS:000281857900005
ER
PT J
AU Tu, CJ
Rudnick, PA
Martinez, MY
Cheek, KL
Stein, SE
Slebos, RJC
Liebler, DC
AF Tu, Chengjian
Rudnick, Paul A.
Martinez, Misti Y.
Cheek, Kristin L.
Stein, Stephen E.
Slebos, Robbert J. C.
Liebler, Daniel C.
TI Depletion of Abundant Plasma Proteins and Limitations of Plasma
Proteomics
SO JOURNAL OF PROTEOME RESEARCH
LA English
DT Article
DE plasma; high-abundance protein depletion; multiple affinity removal
system; isoelectric focusing; shotgun proteomics
ID TANDEM MASS-SPECTROMETRY; LIQUID-CHROMATOGRAPHY; HUMAN SERUM;
IMMUNOAFFINITY SEPARATION; PEPTIDE IDENTIFICATION; SAMPLE PREPARATION;
STRATEGIES; BINDING; COLUMN
AB Immunoaffinity depletion with antibodies to the top 7 or top 14 high-abundance plasma proteins is used to enhance detection of lower abundance proteins in both shotgun and targeted proteomic analyses. We evaluated the effects of top 7/top 14 immunodepletion on the shotgun proteomic analysis of human plasma. Our goal was to evaluate the impact of immunodepletion on detection of proteins across detectable ranges of abundance. The depletion columns afforded highly repeatable and efficient plasma protein fractionation. Relatively few nontargeted proteins were captured by the depletion columns. Analyses of unfractionated and immunodepleted plasma by peptide isoelectric focusing (IEF), followed by liquid chromatography-tandem mass spectrometry (LC-MS/MS), demonstrated enrichment of nontargeted plasma proteins by an average of 4-fold, as assessed by MS/MS spectral counting. Either top 7 or top 14 immunodepletion resulted in a 25% increase in identified proteins compared to unfractionated plasma. Although 23 low-abundance (<10 ng mL(-1)) plasma proteins were detected, they accounted for only 5-6% of total protein identifications in immunodepleted plasma. In both unfractionated and immunodepleted plasma, the 50 most abundant plasma proteins accounted for 90% of cumulative spectral counts and precursor ion intensities, leaving little capacity to sample lower abundance proteins. Untargeted proteomic analyses using current LC-MS/MS platforms-even with immunodepletion-cannot be expected to efficiently discover low-abundance, disease-specific biomarkers in plasma.
C1 [Tu, Chengjian; Slebos, Robbert J. C.; Liebler, Daniel C.] Vanderbilt Univ, Sch Med, Vanderbilt Ingram Canc Ctr, Jim Ayers Inst Precanc Detect & Diag, Nashville, TN 37232 USA.
[Tu, Chengjian; Martinez, Misti Y.; Cheek, Kristin L.; Liebler, Daniel C.] Vanderbilt Univ, Sch Med, Dept Biochem, Nashville, TN 37232 USA.
[Rudnick, Paul A.; Stein, Stephen E.] Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
[Slebos, Robbert J. C.] Vanderbilt Univ, Sch Med, Dept Canc Biol, Nashville, TN 37232 USA.
RP Liebler, DC (reprint author), Vanderbilt Univ, Sch Med, Vanderbilt Ingram Canc Ctr, Jim Ayers Inst Precanc Detect & Diag, Nashville, TN 37232 USA.
EM daniel.liebler@vanderbilt.edu
OI Liebler, Daniel/0000-0002-7873-3031
FU National Cancer Institute [5U24CA126479]; National Institute of
Standards and Technology; National Cancer Institute
FX This work was supported by a cooperative agreement award 5U24CA126479
from the National Cancer Institute through the Clinical Proteomic
Technology Assessment for Cancer (CPTAC) program and by an interagency
agreement between the National Cancer Institute and the National
Institute of Standards and Technology. Certain commercial equipment,
instruments, or materials are identified in this document. Such
identification does not imply recommendation or endorsement by the
National Institute of Standards and Technology, nor does it imply that
the products identified are necessarily the best available for the
purpose.
NR 32
TC 114
Z9 116
U1 6
U2 49
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 1535-3893
J9 J PROTEOME RES
JI J. Proteome Res.
PD OCT
PY 2010
VL 9
IS 10
BP 4982
EP 4991
DI 10.1021/pr100646w
PG 10
WC Biochemical Research Methods
SC Biochemistry & Molecular Biology
GA 655NX
UT WOS:000282257800011
PM 20677825
ER
PT J
AU Dubernet, ML
Boudon, V
Culhane, JL
Dimitrijevic, MS
Fazliev, AZ
Joblin, C
Kupka, F
Leto, G
Le Sidaner, P
Loboda, PA
Mason, HE
Mason, NJ
Mendoza, C
Mulas, G
Millar, TJ
Nunez, LA
Perevalov, VI
Piskunov, N
Ralchenko, Y
Rixon, G
Rothman, LS
Roueff, E
Ryabchikova, TA
Ryabtsev, A
Sahal-Brechot, S
Schmitt, B
Schlemmer, S
Tennyson, J
Tyuterev, VG
Walton, NA
Wakelam, V
Zeippen, CJ
AF Dubernet, M. L.
Boudon, V.
Culhane, J. L.
Dimitrijevic, M. S.
Fazliev, A. Z.
Joblin, C.
Kupka, F.
Leto, G.
Le Sidaner, P.
Loboda, P. A.
Mason, H. E.
Mason, N. J.
Mendoza, C.
Mulas, G.
Millar, T. J.
Nunez, L. A.
Perevalov, V. I.
Piskunov, N.
Ralchenko, Y.
Rixon, G.
Rothman, L. S.
Roueff, E.
Ryabchikova, T. A.
Ryabtsev, A.
Sahal-Brechot, S.
Schmitt, B.
Schlemmer, S.
Tennyson, J.
Tyuterev, V. G.
Walton, N. A.
Wakelam, V.
Zeippen, C. J.
TI Virtual atomic and molecular data centre
SO JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER
LA English
DT Article
DE Atomic data; Molecular data; Astrophysics; Atmospheric physics; Fusion;
Radiation; Lighting; Space physics; Planetology
ID SPECTROSCOPIC DATABASE; ONLINE DATABASE; ICE; ASTROCHEMISTRY;
ATMOSPHERE; MIXTURES; PROFILE; BAND; CH4
AB The Virtual Atomic and Molecular Data Centre (VAMDC, http://www.vamdc.eu) is a European Union funded collaboration between groups involved in the generation, evaluation, and use of atomic and molecular data. VAMDC aims to build a secure, documented, flexible and interoperable e-science environment-based interface to existing atomic and molecular data. The project will cover establishing the core consortium, the development and deployment of the infrastructure and the development of interfaces to the existing atomic and molecular databases. It will also provide a forum for training potential users and dissemination of expertise worldwide. This review describes the scope of the VAMDC project; it provides a survey of the atomic and molecular data sets that will be included plus a discussion of how they will be integrated. Some applications of these data are also discussed. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Dubernet, M. L.] Univ Paris 06, CNRS INP, UMR 7092, Lab Phys Mol Atmosphere & Astrophys, F-75252 Paris 05, France.
[Dubernet, M. L.; Roueff, E.] Observ Paris, CNRS INSU, UMR 8102, Lab Univers & Theories,Sect Meudon, F-92195 Meudon, France.
[Boudon, V.] Univ Bourgogne, CNRS, UMR 5209, Lab Interdisciplinaire Carnot Bourgogne, F-21078 Dijon, France.
[Culhane, J. L.] Univ Coll London, Mullard Space Sci Lab, Surrey RH5 6NT, England.
[Dimitrijevic, M. S.] Astron Observ, Belgrade 11060, Serbia.
[Fazliev, A. Z.; Perevalov, V. I.] Russian Acad Sci, Siberian Branch, VE Zuev Inst Atmospher Opt, Tomsk 634021, Russia.
[Joblin, C.] Univ Toulouse 3, CNRS INSU, UMR 5187, Ctr Etud Spatiale Rayonnements, F-31028 Toulouse 9, France.
[Kupka, F.] Univ Vienna, Fac Math, A-1090 Vienna, Austria.
[Leto, G.] Osserv Astrofis Catania, Ist Nazl Astrofis, I-95123 Catania, Italy.
[Le Sidaner, P.] Observ Paris, CNRS INSU, UMS 2201, VO Paris Data Ctr,Div Informat Observ, F-92195 Meudon, France.
[Loboda, P. A.] All Russian Inst Tech Phys RFNTC VNIITF, Russian Fed Nucl Ctr, Snezhinsk 456770, Chelyabinsk Reg, Russia.
[Mason, H. E.] Ctr Math Sci, Dept Appl Math & Theoret Phys, Cambridge CB3 0WA, England.
[Mason, N. J.] Open Univ, Fac Sci, Milton Keynes MK7 6AA, Bucks, England.
[Mendoza, C.; Nunez, L. A.] Univ Los Andes, CeCalCULA, Corp Parque Tecnol Merida, Ctr Nacl Calculo Cient, Merida 5101, Venezuela.
[Mendoza, C.] Inst Venezolano Invest Cient, Ctr Fis, Caracas 1020A, Venezuela.
[Nunez, L. A.] Univ Ind Santander, Esc Fis, GIRG, Bucaramanga, Colombia.
[Mulas, G.] Osservatorio Astron Cagliari, Ist Nazl Astrofis, I-09012 Capoterra, CA, Italy.
[Piskunov, N.] Uppsala Univ, Dept Phys & Astron, S-75120 Uppsala, Sweden.
[Ralchenko, Y.] NIST, Atom Phys Div, Gaithersburg, MD 20899 USA.
[Rothman, L. S.] Harvard Smithsonian Ctr Astrophys, Atom & Mol Phys Div, Cambridge, MA 02138 USA.
[Millar, T. J.] Queens Univ Belfast, Sch Math & Phys, Belfast BT7 1NN, Antrim, North Ireland.
[Ryabchikova, T. A.] RAS, Inst Astron, Moscow 119017, Russia.
[Ryabtsev, A.] RAS, Inst Spect, Troitsk 142190, Russia.
[Sahal-Brechot, S.; Zeippen, C. J.] Observ Paris, CNRS INSU, UMR 8112, Lab Etud Rayonnement & Mat Astrophys, F-75014 Paris, France.
[Schmitt, B.] Univ Grenoble 1, CNRS INSU, UMR 5109, Lab Planetol Grenoble, F-38041 Grenoble 9, France.
[Schlemmer, S.] Univ Cologne, Inst Phys 1, D-50937 Cologne, Germany.
[Tennyson, J.] UCL, Dept Phys & Astron, London WC1E 6BT, England.
[Tyuterev, V. G.] Univ Reims, UFR Sci Exactes & Nat, CNRS INP, Grp Spect Mol & Atmospher,UMR 6089, F-51687 Reims 2, France.
[Rixon, G.; Walton, N. A.] Univ Cambridge, Inst Astron, Cambridge CB3 0HA, England.
[Wakelam, V.] Univ Bordeaux, CNRS INSU, UMR 5804, Lab Astrophys Bordeaux, F-33271 Floirac, France.
RP Dubernet, ML (reprint author), Univ Paris 06, CNRS INP, UMR 7092, Lab Phys Mol Atmosphere & Astrophys, Case 76,4 Pl Jussieu, F-75252 Paris 05, France.
EM Marie-Lise.Dubernet-Tuckey@upmc.FR
RI BOUDON, Vincent/A-4504-2010; Ralchenko, Yuri/B-7687-2011; Schmitt,
Bernard/A-1064-2009; Tennyson, Jonathan/I-2222-2012; Mulas,
Giacomo/B-7480-2013; Nunez, Luis/D-3404-2013; Schlemmer,
Stephan/E-2903-2015; Leto, Giuseppe/N-3355-2015; Ralchenko,
Yuri/E-9297-2016;
OI Rothman, Laurence/0000-0002-3837-4847; Millar, Tom/0000-0001-5178-3656;
Schmitt, Bernard/0000-0002-1230-6627; Tennyson,
Jonathan/0000-0002-4994-5238; Mulas, Giacomo/0000-0003-0602-6669; Nunez,
Luis/0000-0003-4575-5899; Schlemmer, Stephan/0000-0002-1421-7281; Leto,
Giuseppe/0000-0002-0040-5011; Ralchenko, Yuri/0000-0003-0083-9554;
Wakelam, Valentine/0000-0001-9676-2605
FU VAMDC [INFRA-2008-1.2.2, 239108]
FX VAMDC is funded under the "Combination of Collaborative Projects and
Coordination and Support Actions" Funding Scheme of The Seventh
Framework Program. Call topic: INFRA-2008-1.2.2 Scientific Data
Infrastructure. Grant Agreement number: 239108.
NR 55
TC 104
Z9 109
U1 1
U2 18
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0022-4073
EI 1879-1352
J9 J QUANT SPECTROSC RA
JI J. Quant. Spectrosc. Radiat. Transf.
PD OCT
PY 2010
VL 111
IS 15
SI SI
BP 2151
EP 2159
DI 10.1016/j.jqsa.2010.05.004
PG 9
WC Optics; Spectroscopy
SC Optics; Spectroscopy
GA 643CE
UT WOS:000281269800003
ER
PT J
AU Tennyson, J
Bernath, PF
Brown, LR
Campargue, A
Csaszar, AG
Daumont, L
Gamache, RR
Hodges, JT
Naumenko, OV
Polyansky, OL
Rothman, LS
Toth, RA
Vandaele, AC
Zobov, NF
Fally, S
Fazliev, AZ
Furtenbacher, T
Gordon, IE
Hu, SM
Mikhailenko, SN
Voronin, BA
AF Tennyson, Jonathan
Bernath, Peter F.
Brown, Linda R.
Campargue, Alain
Csaszar, Attila G.
Daumont, Ludovic
Gamache, Robert R.
Hodges, Joseph T.
Naumenko, Olga V.
Polyansky, Oleg L.
Rothman, Laurence S.
Toth, Robert A.
Vandaele, Ann Carine
Zobov, Nikolai F.
Fally, Sophie
Fazliev, Alexander Z.
Furtenbacher, Tibor
Gordon, Iouli E.
Hu, Shui-Ming
Mikhailenko, Semen N.
Voronin, Boris A.
TI IUPAC critical evaluation of the rotational-vibrational spectra of water
vapor. Part II Energy levels and transition wavenumbers for (HDO)-O-16,
(HDO)-O-17, and (HDO)-O-18
SO JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER
LA English
DT Article
DE Water vapor; Transition wavenumbers; Atmospheric physics; Energy levels;
MARVEL; Information system; Database; W@DIS; Infrared spectra; Microwave
spectra; (HDO)-O-16; (HDO)-O-17; (HDO)-O-18
ID FOURIER-TRANSFORM SPECTROSCOPY; LASER-ABSORPTION SPECTROSCOPY;
BEAM-MASER SPECTROSCOPY; HETERODYNE FREQUENCY MEASUREMENTS;
LORENTZ-BROADENING COEFFICIENTS; LINE-SHIFT COEFFICIENTS;
HIGH-RESOLUTION; CM(-1) REGION; MU-M; HYPERFINE STRUCTURE
AB This is the second of a series of articles reporting critically evaluated rotational-vibrational line positions, transition intensities, pressure dependences, and energy levels, with associated critically reviewed assignments and uncertainties, for all the main isotopologues of water. This article presents energy levels and line positions of the following singly deuterated isotopologues of water: (HDO)-O-16, (HDO)-O-17, and (HDO)-O-18. The MARVEL (measured active rotational-vibrational energy levels) procedure is used to determine the levels, the lines, and their self-consistent uncertainties for the spectral regions 0-22708, 0-1674, and 0-12 105 cm(-1) for (HDO)-O-16, (HDO)-O-17, and (HDO)-O-18, respectively. For (HDO)-O-16, 54 740 transitions were analyzed from 76 sources, the lines come from spectra recorded both at room temperature and from hot samples. These lines correspond to 36 690 distinct assignments and 8818 energy levels. For (HDO)-O-17, only 485 transitions could be analyzed from three sources; the lines correspond to 162 MARVEL energy levels. For (HDO)-O-18, 8729 transitions were analyzed from 11 sources and these lines correspond to 1864 energy levels. The energy levels are checked against ones determined from accurate variational nuclear motion computations employing exact kinetic energy operators. This comparison shows that the measured transitions account for about 86% of the anticipated absorbance of (HDO)-O-16 at 296 K and that the transitions predicted by the MARVEL energy levels account for essentially all the remaining absorbance. The extensive list of MARVEL lines and levels obtained are given in the Supplementary Material of this article, as well as in a distributed information system applied to water, W@DIS, where they can easily be retrieved. In addition, the transition and energy level information for (H2O)-O-17 and (H2O)-O-18, given in the first paper of this series [Tennyson, et al. J Quant Spectr Rad Transfer 2009;110:573-96], has been updated. (C) 2010 Elsevier Ltd. All rights reserved.
C1 [Tennyson, Jonathan; Polyansky, Oleg L.] Univ London Univ Coll, Dept Phys & Astron, London WC1E 6BT, England.
[Bernath, Peter F.] Univ York, York YO10 5DD, N Yorkshire, England.
[Brown, Linda R.; Toth, Robert A.] CALTECH, Jet Prop Lab, Pasadena, CA USA.
[Campargue, Alain] Univ Grenoble 1, Grenoble, France.
[Csaszar, Attila G.; Furtenbacher, Tibor] Eotvos Lorand Univ, Budapest, Hungary.
[Daumont, Ludovic] Univ Reims, Reims, France.
[Gamache, Robert R.] Univ Massachusetts, Lowell, MA USA.
[Hodges, Joseph T.] NIST, Gaithersburg, MD 20899 USA.
[Naumenko, Olga V.; Fazliev, Alexander Z.; Mikhailenko, Semen N.; Voronin, Boris A.] Russian Acad Sci, VE Zuev Inst Atmospher Opt, Tomsk 634021, Russia.
[Polyansky, Oleg L.; Zobov, Nikolai F.] Russian Acad Sci, Inst Appl Phys, Nizhnii Novgorod, Russia.
[Rothman, Laurence S.; Gordon, Iouli E.] Harvard Smithsonian Ctr Astrophys, Cambridge, MA 02138 USA.
[Vandaele, Ann Carine] Inst Aeron Spatiale Belgique, B-1180 Brussels, Belgium.
[Fally, Sophie] Univ Libre Bruxelles, Brussels, Belgium.
[Hu, Shui-Ming] Univ Sci & Technol China, Lab Bond Select Chem, Hefei 230026, Peoples R China.
RP Tennyson, J (reprint author), Univ London Univ Coll, Dept Phys & Astron, Gower St, London WC1E 6BT, England.
EM j.tennyson@ucl.ac.UK
RI Csaszar, Attila/A-5241-2009; Hu, Shuiming/C-4287-2008; Bernath,
Peter/B-6567-2012; Tennyson, Jonathan/I-2222-2012; Voronin,
Boris/A-3444-2014;
OI Hu, Shuiming/0000-0002-1565-8468; Bernath, Peter/0000-0002-1255-396X;
Tennyson, Jonathan/0000-0002-4994-5238; Voronin,
Boris/0000-0002-8743-5554; Gordon, Iouli/0000-0003-4763-2841; Rothman,
Laurence/0000-0002-3837-4847
FU International Union of Pure and Applied Chemistry [2004-035-1-100]; UK
Natural Environment Research Council, the Royal Society
[WWLC-008535-(reintegration) MCA FP6 EC]; Scientific Research Fund. of
Hungary [OTKA K77825]; European Union; Russian Foundation for Basic
Research; Belgian Federal Science Policy Office [EV/35/3A, SD/AT/01A,
PRODEX 1514901NLSFe(IC)]; Communaute de Belgique (Action de Recherche
Concertees); NASA [NNX08AD92G]; National Science Foundation
[ATM-0803135]; CNRS (INSU)
FX We all thank the International Union of Pure and Applied Chemistry for
funding under project 2004-035-1-100 (A database of water transitions
from experiment and theory). In addition, this work has received partial
support from the UK Natural Environment Research Council, the Royal
Society, Grant WWLC-008535-(reintegration) MCA FP6 EC, the Scientific
Research Fund. of Hungary (Grant OTKA K77825), the European Union
QUASAAR Marie Curie research training network, NATO, the Russian
Foundation for Basic Research, the Belgian Federal Science Policy Office
(contracts EV/35/3A, SD/AT/01A, PRODEX 1514901NLSFe(IC)), the Belgian
National Fund for Scientific Research (FRFC contracts), the Communaute
de Belgique (Action de Recherche Concertees), the NASA laboratory
astrophysics program, NASA Earth Observing System (E0S), under Grant
NNX08AD92G, the National Science Foundation, through Grant no.
ATM-0803135, and the Programme National LEFE (CHAT) of CNRS (INSU). Part
of the research described in this paper was performed at the Jet
Propulsion Laboratory, California Institute of Technology, under
contract with the National Aeronautics and Space Administration.
NR 150
TC 82
Z9 89
U1 8
U2 46
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0022-4073
EI 1879-1352
J9 J QUANT SPECTROSC RA
JI J. Quant. Spectrosc. Radiat. Transf.
PD OCT
PY 2010
VL 111
IS 15
SI SI
BP 2160
EP 2184
DI 10.1016/j.jqsrt.2010.06.012
PG 25
WC Optics; Spectroscopy
SC Optics; Spectroscopy
GA 643CE
UT WOS:000281269800004
ER
PT J
AU Kohlmann, H
Skripov, AV
Soloninin, AV
Udovic, TJ
AF Kohlmann, H.
Skripov, A. V.
Soloninin, A. V.
Udovic, T. J.
TI The anti-perovskite type hydride InPd3H0.89
SO JOURNAL OF SOLID STATE CHEMISTRY
LA English
DT Article
DE Metal hydrides; Palladium; Neutron powder diffraction; Inelastic neutron
scattering; Nuclear magnetic resonance spectroscopy
ID INELASTIC NEUTRON-SCATTERING; PALLADIUM-HYDROGEN SYSTEM; INTERMETALLIC
COMPOUNDS; CRYSTAL-STRUCTURE; SINGLE-CRYSTAL; PHASE; DIFFRACTION;
TRANSITIONS; MGPD3
AB Hydrogenation of tetragonal InPd3 in the ZrAl3 type structure (four-fold ccp superstructure) yields a hydride with a cubic AuCu3 type structure (one-fold ccp superstructure). Deuterium can be located by neutron powder diffraction in octahedral voids surrounded exclusively by palladium, [Pd-6], which are 88.5(6)% occupied in a statistical manner. The resulting deuteride InPd3D0.89 thus crystallizes in a cubic anti-perovskite type structure (space group Pm (3) over barm (no. 221), a=402.25(1) pm at 299(2) K). The Pd-D distance of 201.13(1) pm is typical for interstitial hydrides with palladium. Inelastic neutron scattering on the hydride InPd3H0.89, which shows a spectrum similar to that of binary palladium hydride, confirms the cubic site symmetry of hydrogen in [Pd-6] interstices. This is also confirmed by the absence of any quadrupole splitting in the D-2-NMR signal of the deuteride. H-1 NMR spectra of InPd3H0.89 do not show any motional narrowing. Values found for the H jump rate tau(-1) in InPd3H0.89 remain below 10(6) s(-1) in the studied temperature range 28-360K. indicating a small hydrogen mobility in InPd3H0.8 as compared with binary palladium hydride, PdH (<= 1).This can be attributed to the large spatial separation of the [Pd-6] sites. (C) 2010 Elsevier Inc. All rights reserved.
C1 [Kohlmann, H.] Univ Saarland, D-66125 Saarbrucken, Germany.
[Skripov, A. V.; Soloninin, A. V.] Russian Acad Sci, Inst Met Phys, Urals Branch, Ekaterinburg 620041, Russia.
[Udovic, T. J.] Natl Inst Stand & Technol, NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA.
RP Kohlmann, H (reprint author), Univ Saarland, Fachrichtung 8-1 Anorgan Festkorperchem,Markt Zei, D-66125 Saarbrucken, Germany.
EM h.kohlmann@mx.uni-saarland.de
RI Kohlmann, Holger/C-6244-2009; Soloninin, Alexey/J-8580-2013; Skripov,
Alexander/K-4525-2013
OI Soloninin, Alexey/0000-0001-7127-9641; Skripov,
Alexander/0000-0002-0610-5538
FU Deutsche Forschungsgemeinschaft [Ko1803/2-1]
FX This work was supported by the Deutsche Forschungsgemeinschaft
(Ko1803/2-1). We thank H. Recktenwald and S. Beetz (Saarbrucken) for
technical assistance, C. Ritter for assistance with the neutron powder
diffraction experiments, and J.J. Rush for useful discussions. The
Institut Laue-Langevin (Grenoble, France) is gratefully acknowledged for
the allocation of beam time.
NR 35
TC 5
Z9 5
U1 0
U2 14
PU ACADEMIC PRESS INC ELSEVIER SCIENCE
PI SAN DIEGO
PA 525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA
SN 0022-4596
J9 J SOLID STATE CHEM
JI J. Solid State Chem.
PD OCT
PY 2010
VL 183
IS 10
BP 2461
EP 2465
DI 10.1016/j.jssc.2010.08.015
PG 5
WC Chemistry, Inorganic & Nuclear; Chemistry, Physical
SC Chemistry
GA 663FR
UT WOS:000282868900031
ER
PT J
AU Alashker, Y
El-Tawil, S
Sadek, F
AF Alashker, Yasser
El-Tawil, Sherif
Sadek, Fahim
TI Progressive Collapse Resistance of Steel-Concrete Composite Floors
SO JOURNAL OF STRUCTURAL ENGINEERING-ASCE
LA English
DT Article
DE Composite floor systems; Robustness; Disproportionate collapse;
Finite-element analysis; Progressive collapse; Shear connections; Shear
tab; Connection
ID BEHAVIOR
AB This paper discusses the progressive collapse resistance of steel-concrete composite floors in which steel beams are attached to columns through shear tabs. This is a common type of system used for the gravity bay portions of steel buildings. The study is conducted using computational simulation models validated through extensive comparisons to disparate test data. The models are used to investigate key parameters influencing the robustness of generic composite floors subjected to the removal of a center column. In particular, the effects of deck thickness, steel reinforcement, and the numbers of bolts in the shear tab connection on the behavior of the system are studied as a function of the loading scheme. The simulation results show that the majority of collapse resistance comes from the steel deck and that, for the system considered, increasing connection strength by adding more bolts might not be that beneficial in increasing overall collapse strength. The dynamic impact factor, which is widely used to account for dynamic effects within a static design framework, is also computed and the DIF value recommended in existing design guidelines is evaluated.
C1 [Alashker, Yasser; El-Tawil, Sherif] Univ Michigan, Dept Civil & Environm Engn, Ann Arbor, MI 48109 USA.
[Sadek, Fahim] Natl Inst Stand & Technol, Struct Grp, Bldg & Fire Res Lab, Gaithersburg, MD 20899 USA.
RP El-Tawil, S (reprint author), Univ Michigan, Dept Civil & Environm Engn, Ann Arbor, MI 48109 USA.
EM yasserra@umich.edu; eltawil@umich.edu; fahim.sadek@nist.gov
OI El-Tawil, Sherif/0000-0001-6437-5176
FU Department of Civil and Environmental Engineering at the University of
Michigan; National Science Foundation (NSF) [SES-0824737, CMMI-0928193]
FX The presented work was supported in part by the Department of Civil and
Environmental Engineering at the University of Michigan, the National
Science Foundation (NSF) through Grant Nos. SES-0824737 and
CMMI-0928193. Any opinions, findings, conclusions, and recommendations
expressed in this paper are those of the writers and do not necessarily
reflect the views of the sponsors. Certain commercial software or
materials are identified to describe a procedure or concept adequately.
Such identification is not intended to imply recommendation,
endorsement, or implication by NIST that the software or materials are
necessarily the best available for the purpose.
NR 19
TC 34
Z9 35
U1 6
U2 25
PU ASCE-AMER SOC CIVIL ENGINEERS
PI RESTON
PA 1801 ALEXANDER BELL DR, RESTON, VA 20191-4400 USA
SN 0733-9445
J9 J STRUCT ENG-ASCE
JI J. Struct. Eng.-ASCE
PD OCT
PY 2010
VL 136
IS 10
BP 1187
EP 1196
DI 10.1061/(ASCE)ST.1943-541X.0000230
PG 10
WC Construction & Building Technology; Engineering, Civil
SC Construction & Building Technology; Engineering
GA 653DV
UT WOS:000282069000001
ER
PT J
AU Sharif, HO
Hassan, AA
Bin-Shafique, S
Xie, HJ
Zeitler, J
AF Sharif, Hatim O.
Hassan, Almoutaz A.
Bin-Shafique, Sazzad
Xie, Hongjie
Zeitler, Jon
TI HYDROLOGIC MODELING OF AN EXTREME FLOOD IN THE GUADALUPE RIVER IN TEXAS
SO JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION
LA English
DT Article
DE flooding; precipitation; runoff; surface water hydrology; GSSHA
ID FLASH-FLOOD; RAINFALL; BASIN
AB Many of the storms creating the greatest rainfall depths in Texas, measured over durations ranging from one minute to 48 hours, have occurred in the Texas Hill Country area. The upstream portion of the Guadalupe River Basin, located in the Texas Hill Country, is susceptible to flooding and rapid runoff due to thin soils, exposed bedrock, and sparse vegetation, in addition to the Balcones Escarpment uplift contributing to precipitation enhancement. In November 2004, a moist air mass from the Gulf of Mexico combined with moist air from the Pacific Ocean resulted in the wettest November in Texas since 1895. Although the peak discharges were not the highest on record, the U.S. Geological Survey (USGS) stream gauge on the Guadalupe River at Gonzales, Texas reported a daily mean discharge of 2,304 m(3)/s on November 23, 2004 (average discharge is 53 m(3)/s). In this paper, we examine the meteorological conditions that led to this event and apply a two-dimensional, physically based, distributed-parameter hydrologic model to simulate the response of a portion of the basin during this event. The study results clearly demonstrate the ability of physically based, distributed-parameter simulations, driven by operational radar rainfall products, to adequately model the cumulative effect of two rainfall events and route inflows from three upstream watersheds without the need for significant calibration.
C1 [Sharif, Hatim O.; Hassan, Almoutaz A.; Bin-Shafique, Sazzad] Univ Texas San Antonio, Dept Civil & Environm Engn, San Antonio, TX 78249 USA.
[Xie, Hongjie] Univ Texas San Antonio, Dept Earth & Environm Sci, San Antonio, TX 78249 USA.
[Zeitler, Jon] Austin San Antonio Weather Forecast Off, Natl Weather Serv, New Braunfels, TX 78130 USA.
RP Sharif, HO (reprint author), Univ Texas San Antonio, Dept Civil & Environm Engn, 1 UTSA Circle, San Antonio, TX 78249 USA.
EM hatim.sharif@utsa.edu
RI Sharif, Hatim/E-4426-2010; Xie, Hongjie/B-5845-2009
OI Xie, Hongjie/0000-0003-3516-1210
FU NOAA [NA06NWS4680012]
FX This study was supported in part by a NOAA Grant (NA06NWS4680012). Help
from Austin/San Antonio National Weather Service Weather Forecast Office
staff is greatly appreciated. We also acknowledge the assistance of
former UTSA student Terry LeeAnn Lutz who sparked interest in this flood
event.
NR 28
TC 12
Z9 12
U1 2
U2 8
PU WILEY-BLACKWELL PUBLISHING, INC
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 1093-474X
J9 J AM WATER RESOUR AS
JI J. Am. Water Resour. Assoc.
PD OCT
PY 2010
VL 46
IS 5
BP 881
EP 891
DI 10.1111/j.1752-1688.2010.00459.x
PG 11
WC Engineering, Environmental; Geosciences, Multidisciplinary; Water
Resources
SC Engineering; Geology; Water Resources
GA 654MG
UT WOS:000282171800002
ER
PT J
AU Charnotskii, M
AF Charnotskii, Mikhail
TI Beam scintillations for ground-to-space propagation. Part I: Path
integrals and analytic techniques
SO JOURNAL OF THE OPTICAL SOCIETY OF AMERICA A-OPTICS IMAGE SCIENCE AND
VISION
LA English
DT Article
AB We extend our theory of on-axis beam scintillations [Waves Random Media 4, 243 (1994)] for the case of propagation on slant turbulent paths, where turbulence is concentrated in a relatively thin layer near the transmitter. Our technique is based on the parabolic equation for optical wave propagation and the Markov approximation for the calculation of statistical moments of beam intensity. This first of two companion papers presents the details of the path integral formulation of the solution for the fourth-order coherence function. We also discuss in detail two analytic techniques that can be used for the treatment of the path integrals. (C) 2010 Optical Society of America
C1 NOAA, Zel Technol LLC, Earth Syst Res Lab, Boulder, CO 80305 USA.
RP Charnotskii, M (reprint author), NOAA, Zel Technol LLC, Earth Syst Res Lab, 325 Broadway, Boulder, CO 80305 USA.
EM Mikhail.Charnotskii@noaa.gov
RI Charnotskii, Mikhail/A-7193-2013
OI Charnotskii, Mikhail/0000-0002-8315-8254
NR 16
TC 12
Z9 12
U1 0
U2 2
PU OPTICAL SOC AMER
PI WASHINGTON
PA 2010 MASSACHUSETTS AVE NW, WASHINGTON, DC 20036 USA
SN 1084-7529
J9 J OPT SOC AM A
JI J. Opt. Soc. Am. A-Opt. Image Sci. Vis.
PD OCT
PY 2010
VL 27
IS 10
BP 2169
EP 2179
PG 11
WC Optics
SC Optics
GA 658UW
UT WOS:000282515900009
PM 20922007
ER
PT J
AU Charnotskii, M
AF Charnotskii, Mikhail
TI Beam scintillations for ground-to-space propagation. Part 2: Gaussian
beam scintillation
SO JOURNAL OF THE OPTICAL SOCIETY OF AMERICA A-OPTICS IMAGE SCIENCE AND
VISION
LA English
DT Article
ID OPTICAL SCINTILLATION
AB On the basis of the analytic techniques presented in the first of these two companion papers [J. Opt. Soc. Am. A 27, 2169 (2010)] we present the complete asymptotic analysis of the axial beam scintillation index for coherent Gaussian beams on the ground-to-space propagation paths. The ratio of turbulence layer thickness to overall propagation path length contributes an additional small parameter to the analysis. We show that it is possible to use three dimensionless parameters to describe the problem and that the general arrangement of the asymptotic regions established in our earlier work [Waves Random Media 4, 243 (1994)]) is preserved. We find that on a slant propagation path, collimated beams can experience the unusual double-scattering-dominated scintillation found originally for focused beams. (C) 2010 Optical Society of America
C1 NOAA, Zel Technol LLC, Earth Syst Res Lab, Boulder, CO 80305 USA.
RP Charnotskii, M (reprint author), NOAA, Zel Technol LLC, Earth Syst Res Lab, 325 Broadway, Boulder, CO 80305 USA.
EM Mikhail.Charnotskii@noaa.gov
RI Charnotskii, Mikhail/A-7193-2013
OI Charnotskii, Mikhail/0000-0002-8315-8254
NR 10
TC 3
Z9 3
U1 0
U2 1
PU OPTICAL SOC AMER
PI WASHINGTON
PA 2010 MASSACHUSETTS AVE NW, WASHINGTON, DC 20036 USA
SN 1084-7529
J9 J OPT SOC AM A
JI J. Opt. Soc. Am. A-Opt. Image Sci. Vis.
PD OCT
PY 2010
VL 27
IS 10
BP 2180
EP 2187
PG 8
WC Optics
SC Optics
GA 658UW
UT WOS:000282515900010
PM 20922008
ER
PT J
AU Mocklin, JA
Rugh, DJ
Koski, WR
Lawrence-Slavas, N
AF Mocklin, Julie A.
Rugh, David J.
Koski, William R.
Lawrence-Slavas, Noah
TI Comparison of land-based vs. floating calibration targets used in aerial
photogrammetric measurements of whale lengths
SO MARINE MAMMAL SCIENCE
LA English
DT Article
C1 [Mocklin, Julie A.; Rugh, David J.] Alaska Fisheries Sci Ctr, Natl Marine Mammal Lab, Seattle, WA 98115 USA.
[Koski, William R.] LGL Ltd Environm Res Associates, King City, ON L7B 1A6, Canada.
[Lawrence-Slavas, Noah] Pacific Marine Environm Labs, Engn Dev Div, Seattle, WA 98115 USA.
RP Mocklin, JA (reprint author), Alaska Fisheries Sci Ctr, Natl Marine Mammal Lab, 7600 Sand Point Way NE, Seattle, WA 98115 USA.
EM julie.mocklin@noaa.gov
FU MMS
FX We thank MMS for financially supporting the Bowhead Feeding Ecology
Study (BOWFEST). The floating targets were towed by Eugene Brower in
2008 and Fred Brower in 2009 (Barrow Whaling Captains Association), and
J. Craig George (North Slope Borough) and Catherine Berchok (NMFS)
provided logistical support setting out the targets from the vessel. J.
Craig George also provided creative ideas and constructed the land-based
targets. Don LeRoi set up the photogrammetry system in the aircraft
using a radar altimeter supplied by Wayne Perryman (NMFS) and a forward
motion compensation camera mount supplied by Lowell Fritz (NMFS). Kelly
Trask provided most of the photogrammetric measurements made from
digital images. Thanks to Rod Hobbs and Wayne Perryman for suggesting
statistical tests for these data. Pilots Nicholas Toth, Jon French, and
Chris Daniels ably flew our aircraft and mechanic Ron Pauley maintained
it. Kim Goetz did the inflight data collection and provided some of the
figures shown here. Thanks to Kim Shelden, Dave Withrow, Craig George,
Phil Clapham, and three anonymous reviewers for insightful reviews and
helpful comments. Reference to trade names does not imply endorsement by
the National Marine Fisheries Service, NOAA.
NR 12
TC 1
Z9 1
U1 0
U2 1
PU WILEY-BLACKWELL PUBLISHING, INC
PI MALDEN
PA COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA
SN 0824-0469
J9 MAR MAMMAL SCI
JI Mar. Mamm. Sci.
PD OCT
PY 2010
VL 26
IS 4
BP 969
EP 976
DI 10.1111/j.1748-7692.2010.00389.x
PG 8
WC Marine & Freshwater Biology; Zoology
SC Marine & Freshwater Biology; Zoology
GA 660ZQ
UT WOS:000282691000011
ER
PT J
AU Chu, W
Fu, J
Vorburger, TV
AF Chu, Wei
Fu, Joseph
Vorburger, Theodore V.
TI Subpixel image stitching for linewidth measurement based on digital
image correlation
SO MEASUREMENT SCIENCE AND TECHNOLOGY
LA English
DT Article
DE linewidth; atomic force microscopy; carbon nanotube tip; image
registration; image stitching; digital image correlation; nonlinearity;
piezoelectric tube
ID ATOMIC-FORCE MICROSCOPE; AFM IMAGE
AB The inevitable tilt angle resulting from attaching a carbon nanotube to an atomic force microscope (AFM) probe causes probe-related distortion on one sidewall of the linewidth sample during an AFM scan. In order to obtain accurate images at both sidewalls, an image stitching method was proposed in our previous research. An improved digital image correlation technique is outlined here to register two scanned images and detect the relative lateral distortion between them. Then image correction is performed pixel by pixel on both images prior to the stitching. A composite image is formed by stitching these two corrected images, and the linewidth is calculated based on this composite image. Since this method removes a significant portion of in-plane distortion between two images due to the nonlinearity of the AFM piezoelectric tube scanner, uncertainty in the calculation of linewidth due to the image stitching component is estimated to be reduced to the subpixel level from its former estimation of approximately three pixels. The procedure is tested with two standard linewidth features.
C1 [Chu, Wei; Fu, Joseph; Vorburger, Theodore V.] NIST, Gaithersburg, MD 20899 USA.
RP Chu, W (reprint author), NIST, 100 Bur Dr, Gaithersburg, MD 20899 USA.
EM wei.chu@nist.gov
NR 18
TC 2
Z9 2
U1 1
U2 9
PU IOP PUBLISHING LTD
PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0957-0233
EI 1361-6501
J9 MEAS SCI TECHNOL
JI Meas. Sci. Technol.
PD OCT
PY 2010
VL 21
IS 10
AR 105104
DI 10.1088/0957-0233/21/10/105104
PG 5
WC Engineering, Multidisciplinary; Instruments & Instrumentation
SC Engineering; Instruments & Instrumentation
GA 649QG
UT WOS:000281787100007
ER
PT J
AU Panfilo, G
Parker, TE
AF Panfilo, Gianna
Parker, Thomas E.
TI A theoretical and experimental analysis of frequency transfer
uncertainty, including frequency transfer into TAI
SO METROLOGIA
LA English
DT Article
ID MODEL; OSCILLATORS; ALLAN; TIME
AB Results are presented from a theoretical and experimental investigation of the frequency transfer uncertainty (FTU) in long-distance comparisons of frequency standards. The FTU can be an important component of the total uncertainty in such comparisons. The use of the Allan deviation in characterizing the FTU is analysed theoretically and it is shown that for certain noise types the Allan deviation is biased high. A potentially more accurate first difference statistic that can be used in certain situations is also discussed. In addition, an experimental determination of the noise types and levels in common transfer techniques is presented. It is shown that FTUs approaching 1 part in 10(16) at 30 days are possible with current transfer methods. Finally, a method is presented for estimating the FTU in calibrating International Atomic Time (TAI) with a primary frequency standard.
C1 [Panfilo, Gianna] Bur Int Poids & Mesures, Sevres, France.
[Parker, Thomas E.] Natl Inst Stand & Technol, Boulder, CO USA.
RP Panfilo, G (reprint author), Bur Int Poids & Mesures, Sevres, France.
NR 23
TC 9
Z9 9
U1 2
U2 3
PU IOP PUBLISHING LTD
PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0026-1394
J9 METROLOGIA
JI Metrologia
PD OCT
PY 2010
VL 47
IS 5
BP 552
EP 560
DI 10.1088/0026-1394/47/5/005
PG 9
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA 653CB
UT WOS:000282060200008
ER
PT J
AU Becker, CA
Kramer, MJ
AF Becker, C. A.
Kramer, M. J.
TI Atomistic comparison of volume-dependent melt properties from four
models of aluminum
SO MODELLING AND SIMULATION IN MATERIALS SCIENCE AND ENGINEERING
LA English
DT Article
ID INITIO MOLECULAR-DYNAMICS; SIMPLE LIQUID-METALS; INTERATOMIC POTENTIALS;
COLLECTIVE DYNAMICS; TRANSITION-METALS; HIGH-TEMPERATURE; AL; ALLOYS;
DENSITY; DIFFRACTION
AB With the increasing use of simulations in materials research and design, it is important to quantify the differences between, and accuracy of, models used in these simulations. Here we present the results of such a comparison for four embedded-atom models of aluminum that were optimized to have good liquid properties, particularly the melting temperatures. The effects of temperature and volume are systematically examined in the melts for bulk thermodynamic quantities, pair correlation functions and structure factors and diffusion coefficients for each interatomic potential. Where possible, these are then compared with experimental values. We find quantitative differences in the properties determined from the various interatomic potentials despite the fact that they were fit with similar sets of data.
C1 [Becker, C. A.] NIST, Div Met, Gaithersburg, MD 20899 USA.
[Kramer, M. J.] Iowa State Univ, Ames Lab, Div Engn & Mat Sci, Ames, IA 50011 USA.
RP Becker, CA (reprint author), NIST, Div Met, Gaithersburg, MD 20899 USA.
FU Department of Energy, Office of Basic Energy Sciences
[DE-AC02-07CH11358]; US Department of Energy, Office of Science, Basic
Energy Sciences [DE-AC02-06CH11357]
FX Work at the Ames Laboratory was supported by the Department of Energy,
Office of Basic Energy Sciences, under Contract No DE-AC02-07CH11358.
The high-energy x-ray work at the MUCAT sector of the APS was supported
by the US Department of Energy, Office of Science, Basic Energy Sciences
under Contract No DE-AC02-06CH11357. CB would like to thank John Cahn,
Mikhail Mendelev, Ursula Kattner and Dan Samarov for helpful
discussions.
NR 48
TC 18
Z9 18
U1 2
U2 19
PU IOP PUBLISHING LTD
PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0965-0393
J9 MODEL SIMUL MATER SC
JI Model. Simul. Mater. Sci. Eng.
PD OCT
PY 2010
VL 18
IS 7
AR 074001
DI 10.1088/0965-0393/18/7/074001
PG 15
WC Materials Science, Multidisciplinary; Physics, Applied
SC Materials Science; Physics
GA 653XH
UT WOS:000282130700002
ER
PT J
AU Becker, CA
Mishin, Y
AF Becker, C. A.
Mishin, Y.
TI Temperature dependence of the pre-wetting transition at the (111)
anti-phase boundary in Ni3Al: an atomistic study
SO MODELLING AND SIMULATION IN MATERIALS SCIENCE AND ENGINEERING
LA English
DT Article
ID SOLID-SOLUTION; FCC ALLOYS; PHASE; SEGREGATION; BEHAVIOR; SYSTEM; ORDER;
MODEL
AB Chemical composition and ordering at the (1 1 1) anti-phase boundary (APB) in the Ni3Al-based gamma' phase have been studied by semi-grand canonical Monte Carlo simulations at temperatures from 700 to 1300 K. The atomic interactions are modeled with an embedded-atom potential reproducing the relevant part of the Ni-Al phase diagram. In a certain range of bulk compositions and temperatures within the gamma' phase stability domain, the APB undergoes a pre-wetting transformation by becoming a layer of disordered gamma phase. The pre-wetting transformation line is mapped onto the bulk phase diagram allowing predictions of the APB state under various thermochemical conditions.
C1 [Becker, C. A.] Natl Inst Stand & Technol, Mat Sci & Engn Lab, Div Met, Gaithersburg, MD 20899 USA.
[Mishin, Y.] George Mason Univ, Dept Phys & Astron, MSN 3F3, Fairfax, VA 22030 USA.
RP Becker, CA (reprint author), Natl Inst Stand & Technol, Mat Sci & Engn Lab, Div Met, Gaithersburg, MD 20899 USA.
EM chandler.becker@nist.gov
RI Mishin, Yuri/P-2020-2015
FU NIST-NRC; US Department of Energy (Office of Basic Energy Sciences);
NIST; DOE
FX CB would like to thank the NIST-NRC postdoctoral research associateship
program for research support, as well as W J Boettinger and J E Guyer
for helpful discussions. YM acknowledges support of the US Department of
Energy (Office of Basic Energy Sciences) and NIST. Both authors
acknowledge helpful discussions during coordination meetings of the
Computational Materials Science Network (CMSN) program sponsored by DOE.
NR 22
TC 1
Z9 1
U1 0
U2 8
PU IOP PUBLISHING LTD
PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0965-0393
J9 MODEL SIMUL MATER SC
JI Model. Simul. Mater. Sci. Eng.
PD OCT
PY 2010
VL 18
IS 7
AR 074004
DI 10.1088/0965-0393/18/7/074004
PG 11
WC Materials Science, Multidisciplinary; Physics, Applied
SC Materials Science; Physics
GA 653XH
UT WOS:000282130700005
ER
PT J
AU Canino, MF
Spies, IB
Cunningham, KM
Hauser, L
Grant, WS
AF Canino, Michael F.
Spies, Ingrid B.
Cunningham, Kathryn M.
Hauser, Lorenz
Grant, W. Stewart
TI Multiple ice-age refugia in Pacific cod, Gadus macrocephalus
SO MOLECULAR ECOLOGY
LA English
DT Article
DE Gadus macrocephalus; glacial refugia; Pacific cod; Pleistocene;
postglacial colonization; vicariance
ID QUEEN-CHARLOTTE-ISLANDS; QUATERNARY PALEOCEANOGRAPHIC CHANGES;
BIOCHEMICAL POPULATION-GENETICS; BERING-SEA; MITOCHONDRIAL-DNA; ATLANTIC
COD; BRITISH-COLUMBIA; GLACIAL REFUGIUM; WESTERN ALASKA; DATA SETS
AB Pleistocene ice-ages greatly influenced the historical abundances of Pacific cod, Gadus macrocephalus, in the North Pacific and its marginal seas. We surveyed genetic variation at 11 microsatellite loci and mitochondrial (mt) DNA in samples from twelve locations from the Sea of Japan to Washington State. Both microsatellite (mean H = 0.868) and mtDNA haplotype (mean h = 0.958) diversities were large and did not show any geographical trends. Genetic differentiation between samples was significantly correlated with geographical distance between samples for both microsatellites (F(ST) = 0.028, r2 = 0.33) and mtDNA (F(ST) = 0.027, r2 = 0.18). Both marker classes showed a strong genetic discontinuity between northwestern and northeastern Pacific populations that lik