FN Thomson Reuters Web of Science™
VR 1.0
PT J
AU Friend, DG
Bruno, TJ
Muzny, C
AF Friend, Daniel G.
Bruno, Thomas J.
Muzny, Chris
TI In Memoriam: William (Mickey) Haynes (1943 to 2016)
SO INTERNATIONAL JOURNAL OF THERMOPHYSICS
LA English
DT Biographical-Item
C1 [Friend, Daniel G.; Bruno, Thomas J.; Muzny, Chris] Natl Inst Stand & Technol, Appl Chem & Mat Div, Boulder, CO 80305 USA.
RP Friend, DG (reprint author), Natl Inst Stand & Technol, Appl Chem & Mat Div, Boulder, CO 80305 USA.
EM daniel.friend@nist.gov
NR 0
TC 0
Z9 0
U1 0
U2 0
PU SPRINGER/PLENUM PUBLISHERS
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0195-928X
EI 1572-9567
J9 INT J THERMOPHYS
JI Int. J. Thermophys.
PD MAY
PY 2016
VL 37
IS 5
AR 54
DI 10.1007/s10765-016-2060-2
PG 5
WC Thermodynamics; Chemistry, Physical; Mechanics; Physics, Applied
SC Thermodynamics; Chemistry; Mechanics; Physics
GA DI7KV
UT WOS:000373679400008
ER
PT J
AU Baranov, YI
AF Baranov, Yu. I.
TI On the significant enhancement of the continuum-collision induced
absorption in H2O + CO2 mixtures
SO JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER
LA English
DT Article
DE Atmospheric absorption; Water vapor IR spectra; Continuum absorption;
Collision induced absorption
ID CM(-1) SPECTRAL REGION; 4.3-MU-M BAND HEAD; WATER-VAPOR;
TEMPERATURE-DEPENDENCE; LINE-SHAPE; 363 K; CO2; O-2; N-2; MIXTURES
AB The IR spectra of water vapor-carbon dioxide mixtures as well as the spectra of pure gas samples have been recorded using a Fourier-transform infrared spectrometer at a resolution of 0.1 cm(-1) in order to explore the effect of colliding CO2 and H2O molecules on their continuum absorptions. The sample temperatures were 294, 311, 325 and 339 K. Measurements have been conducted at several different water vapor partial pressures depending on the cell temperature. Carbon dioxide pressures were kept close to the three values of 103, 207 and 311 kPa (1.02, 2.04 and 3.07 atm). The path length used in the study was 100 m. It was established that, in the region around 1100 cm(-1), the continuum absorption coefficient CH2O+CO2 is about 20 times stronger than the water-nitrogen continuum absorption coefficient CH2O+CO2 On the other hand, in the far wing region (2500 cm(-1)) of the nu(3) CO2 fundamental band, the binary absorption coefficient CCO2-H2O appears to be about one order of magnitude stronger than the absorption coefficient CCO2+CO2 in pure carbon dioxide. The continuum interpretation and the main problem of molecular band shape formation are discussed in light of these experimental facts. (C) 2016 Elsevier Ltd. All rights reserved.
C1 [Baranov, Yu. I.] NIST, Sensor Sci Div, Gaithersburg, MD 20899 USA.
[Baranov, Yu. I.] Inst Expt Meteorol, SPA Typhoon, 4 Pobedy St, Obninsk 249020, Kaluga Reg, Russia.
RP Baranov, YI (reprint author), NIST, Sensor Sci Div, Gaithersburg, MD 20899 USA.; Baranov, YI (reprint author), Inst Expt Meteorol, SPA Typhoon, 4 Pobedy St, Obninsk 249020, Kaluga Reg, Russia.
FU Upper Atmospheric Research Program of NASA; Russian Foundation for Basic
Researches [15-05-00736, 13-05-00751]
FX The author acknowledges a support from the Upper Atmospheric Research
Program of NASA, and partial financial support from the Russian
Foundation for Basic Researches through Grants 15-05-00736 and
13-05-00751. He would like to thank the NIST Physics Laboratory
Management for the opportunity to carry out the reported research. The
author acknowledges Dr. W.J. Lafferty for revision of the manuscript and
for many suggestions and corrections. The author also addresses many
special thanks to Dr. J.T. Hougen for his help in experiments and
related discussions. The author thanks Dr. A.A. Vigasin for his interest
in this work and useful advises.
NR 23
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U1 3
U2 3
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 MAY
PY 2016
VL 175
BP 100
EP 106
DI 10.1016/j.jqsrt.2016.02.017
PG 7
WC Optics; Spectroscopy
SC Optics; Spectroscopy
GA DI5MG
UT WOS:000373542700010
ER
PT J
AU Alexandrov, MD
Cairns, B
Emde, C
Ackerman, AS
Ottaviani, M
Wasilewski, AP
AF Alexandrov, Mikhail D.
Cairns, Brian
Emde, Claudia
Ackerman, Andrew S.
Ottaviani, Matteo
Wasilewski, Andrzej P.
TI Derivation of cumulus cloud dimensions and shape from the airborne
measurements by the Research Scanning Polarimeter
SO REMOTE SENSING OF ENVIRONMENT
LA English
DT Article
DE Cumulus clouds; Remote sensing; Cloud shape; Cloud dimensions
ID TOP HEIGHT; MISR; STEREO; RETRIEVAL; RECONSTRUCTION; GEOMETRY; IMPACT;
ASTER
AB The Research Scanning Polarimeter (RSP) is an airborne instrument, whose measurements have been extensively used for retrievals of microphysical properties of clouds. In this study we show that for cumulus clouds the information content of the RSP data can be extended by adding the macroscopic parameters of the cloud, such as its geometric shape, dimensions, and height above the ground. This extension is possible by virtue of the high angular resolution and high frequency of the RSP measurements, which allow for geometric constraint of the cloud's 2D cross section between a number of tangent lines of view. The retrieval method is tested on realistic 3D radiative transfer simulations and applied to actual RSP data. (C) 2016 Elsevier Inc. All rights reserved.
C1 [Alexandrov, Mikhail D.] Columbia Univ, Dept Appl Phys & Appl Math, 2880 Broadway, New York, NY 10025 USA.
[Alexandrov, Mikhail D.; Cairns, Brian; Ackerman, Andrew S.; Ottaviani, Matteo; Wasilewski, Andrzej P.] NASA, Goddard Inst Space Studies, 2880 Broadway, New York, NY 10025 USA.
[Emde, Claudia] Univ Munich, Fak Phys, Meteorol Inst, Theresienstr 37, D-80333 Munich, Germany.
[Ottaviani, Matteo] CUNY City Coll, CREST, Dept Elect Engn, NOAA, 160 Convent Ave, New York, NY 10031 USA.
[Wasilewski, Andrzej P.] Trinnovim LLC, 2880 Broadway, New York, NY 10025 USA.
RP Alexandrov, MD (reprint author), Columbia Univ, Dept Appl Phys & Appl Math, 2880 Broadway, New York, NY 10025 USA.
EM mda14@columbia.edu
RI Emde, Claudia/B-5447-2010;
OI Cairns, Brian/0000-0002-1980-1022
FU NASA Radiation Sciences Program; NASA HQ Science Mission
FX This research was supported by the NASA Radiation Sciences Program
managed by Hal Maring. We would like to acknowledge our gratitude to the
DEVOTE project team, the Research Services Directorate at NASA Langley
Research Center for supporting both King Air aircraft, and the HOPE
(Hands On Project Experience) Program co-funded though NASA HQ Science
Mission Directorate and Office of the Chief Engineer that enabled the
collection of the data used in this analysis. We would like to thank
four anonymous reviewers whose thoughtful comments helped us to
significantly improve the paper.
NR 31
TC 0
Z9 0
U1 1
U2 7
PU ELSEVIER SCIENCE INC
PI NEW YORK
PA 360 PARK AVE SOUTH, NEW YORK, NY 10010-1710 USA
SN 0034-4257
EI 1879-0704
J9 REMOTE SENS ENVIRON
JI Remote Sens. Environ.
PD MAY
PY 2016
VL 177
BP 144
EP 152
DI 10.1016/j.rse.2016.02.032
PG 9
WC Environmental Sciences; Remote Sensing; Imaging Science & Photographic
Technology
SC Environmental Sciences & Ecology; Remote Sensing; Imaging Science &
Photographic Technology
GA DI5PC
UT WOS:000373550100012
ER
PT J
AU Parson, W
Ballard, D
Budowle, B
Butler, JM
Gettings, KB
Gill, P
Gusmao, L
Hares, DR
Irwin, JA
King, JL
de Knijff, P
Morling, N
Prinz, M
Schneider, PM
Van Neste, C
Willuweit, S
Phillips, C
AF Parson, Walther
Ballard, David
Budowle, Bruce
Butler, John M.
Gettings, Katherine B.
Gill, Peter
Gusmao, Leonor
Hares, Douglas R.
Irwin, Jodi A.
King, Jonathan L.
de Knijff, Peter
Morling, Niels
Prinz, Mechthild
Schneider, Peter M.
Van Neste, Christophe
Willuweit, Sascha
Phillips, Christopher
TI Massively parallel sequencing of forensic STRs: Considerations of the
DNA commission of the International Society for Forensic Genetics (ISFG)
on minimal nomenclature requirements
SO FORENSIC SCIENCE INTERNATIONAL-GENETICS
LA English
DT Article
DE Massively parallel sequencing; MPS; Next generation sequencing; NGS;
Short tandem repeats; STRs; Nomenclature
ID TANDEM REPEAT LOCI; HUMAN MITOCHONDRIAL-DNA; PROFILING GROUP EDNAP;
NEXT-GENERATION; MASS-SPECTROMETRY; ALLELIC LADDER; GUIDELINES; PCR;
IDENTIFICATION; POLYMORPHISM
AB The DNA Commission of the International Society for Forensic Genetics (ISFG) is reviewing factors that need to be considered ahead of the adoption by the forensic community of short tandem repeat (STR) genotyping by massively parallel sequencing (MPS) technologies. MPS produces sequence data that provide a precise description of the repeat allele structure of a STR marker and variants that may reside in the flanking areas of the repeat region. When a STR contains a complex arrangement of repeat motifs, the level of genetic polymorphism revealed by the sequence data can increase substantially. As repeat structures can be complex and include substitutions, insertions, deletions, variable tandem repeat arrangements of multiple nucleotide motifs, and flanking region SNPs, established capillary electrophoresis (CE) allele descriptions must be supplemented by a new system of STR allele nomenclature, which retains backward compatibility with the CE data that currently populate national DNA databases and that will continue to be produced for the coming years. Thus, there is a pressing need to produce a standardized framework for describing complex sequences that enable comparison with currently used repeat allele nomenclature derived from conventional CE systems. It is important to discern three levels of information in hierarchical order (i) the sequence, (ii) the alignment, and (iii) the nomenclature of STR sequence data. We propose a sequence (text) string format the minimal requirement of data storage that laboratories should follow when adopting MPS of STRs. We further discuss the variant annotation and sequence comparison framework necessary to maintain compatibility among established and future data. This system must be easy to use and interpret by the DNA specialist, based on a universally accessible genome assembly, and in place before the uptake of MPS by the general forensic community starts to generate sequence data on a large scale. While the established nomenclature for CE-based STR analysis will remain unchanged in the future, the nomenclature of sequence-based STR genotypes will need to follow updated rules and be generated by expert systems that translate MPS sequences to match CE conventions in order to guarantee compatibility between the different generations of STR data. (C) 2016 Elsevier Ireland Ltd. All rights reserved.
C1 [Parson, Walther] Med Univ Innsbruck, Inst Legal Med, A-6020 Innsbruck, Austria.
[Parson, Walther] Penn State Univ, Forens Sci Program, University Pk, PA 16802 USA.
[Ballard, David] Kings Coll London, Fac Life Sci, London WC2R 2LS, England.
[Budowle, Bruce; King, Jonathan L.] Univ N Texas, Hlth Sci Ctr, Dept Mol & Med Genet, Inst Appl Genet, Ft Worth, TX USA.
[Budowle, Bruce] King Abdulaziz Univ, CEGMR, Jeddah 21413, Saudi Arabia.
[Butler, John M.; Gettings, Katherine B.] NIST, Gaithersburg, MD 20899 USA.
[Gill, Peter] Norwegian Inst Publ Hlth, Dept Forens Biol, Oslo, Norway.
[Gill, Peter] Univ Oslo, Dept Forens Med, Oslo, Norway.
[Gusmao, Leonor] State Univ Rio de Janeiro UERJ, DNA Diagnost Lab LDD, Rio De Janeiro, Brazil.
[Gusmao, Leonor] Univ Porto, Inst Mol Pathol & Immunol, IPATIMUP, Rua Campo Alegre 823, P-4100 Oporto, Portugal.
[Gusmao, Leonor] Univ Porto, Inst Invest & Inovacao Saude, Rua Campo Alegre 823, P-4100 Oporto, Portugal.
[Hares, Douglas R.; Irwin, Jodi A.] FBI Lab, Quantico, VA USA.
[de Knijff, Peter] Leiden Univ, Dept Human Genet, Med Ctr, NL-2300 RA Leiden, Netherlands.
[Morling, Niels] Univ Copenhagen, Fac Hlth & Med Sci, Dept Forens Med, Sect Forens Genet, Copenhagen, Denmark.
[Prinz, Mechthild] CUNY John Jay Coll Criminal Justice, Dept Sci, New York, NY 10019 USA.
[Schneider, Peter M.] Univ Cologne, Inst Legal Med, Fac Med, D-50931 Cologne, Germany.
[Van Neste, Christophe] Univ Ghent, Fac Pharmaceut Sci, Lab Pharmaceut Biotechnol, B-9000 Ghent, Belgium.
[Willuweit, Sascha] Humboldt Univ, Inst Legal Med, D-10099 Berlin, Germany.
[Phillips, Christopher] Univ Santiago de Compostela, Inst Forens Sci, Forens Genet Unit, Galicia, Spain.
RP Parson, W (reprint author), Med Univ Innsbruck, Muellerstr 44, A-6020 Innsbruck, Austria.
EM walther.parson@i-med.ac.at
RI Gusmao, Leonor/B-3122-2013;
OI Gusmao, Leonor/0000-0003-0432-6481; Van Neste,
Christophe/0000-0002-5958-5731
NR 47
TC 7
Z9 8
U1 4
U2 12
PU ELSEVIER IRELAND LTD
PI CLARE
PA ELSEVIER HOUSE, BROOKVALE PLAZA, EAST PARK SHANNON, CO, CLARE, 00000,
IRELAND
SN 1872-4973
EI 1878-0326
J9 FORENSIC SCI INT-GEN
JI Forensic Sci. Int.-Genet.
PD MAY
PY 2016
VL 22
BP 54
EP 63
DI 10.1016/j.fsigen.2016.01.009
PG 10
WC Genetics & Heredity; Medicine, Legal
SC Genetics & Heredity; Legal Medicine
GA DH3WX
UT WOS:000372718600017
PM 26844919
ER
PT J
AU Scheible, M
Just, R
Sturk-Andreaggi, K
Saunier, J
Parson, W
Parsons, T
Coble, M
Irwin, J
AF Scheible, M.
Just, R.
Sturk-Andreaggi, K.
Saunier, J.
Parson, W.
Parsons, T.
Coble, M.
Irwin, J.
TI The mitochondrial landscape of African Americans: An examination of more
than 2500 control region haplotypes from 22 US locations
SO FORENSIC SCIENCE INTERNATIONAL-GENETICS
LA English
DT Article
DE Mitochondrial DNA; Control region; African American
ID GENETIC POPULATION-DATA; UNITED-STATES; HIGH-QUALITY; DNA; ANCESTRY;
SEQUENCES; ADMIXTURE; GUIDELINES; PUBLICATION; PROPORTIONS
AB The mitochondrial DNA (mtDNA) control region (16024-576) was Sanger-sequenced for a total of 2563 self-identified African Americans, using automated processing techniques and data review standards exceeding guidelines for forensic applications. Genetic diversity ranged from 0.9952 to 0.9998 in 22 population samples from 20 different states.
Haplogroups of African ancestry, found in 82.48% of individuals overall, were most concentrated in the Southeast U.S. and decreased to the north and west. West African and West Central African haplotypes were well-represented in the population samples, especially in the southern U.S. states, while East African haplogroups were observed in low-frequency clusters in a handful of locations across the country. East Asian, Native American, and West Eurasian admixture was present in 3.16%, 2.93%, and 11.43% of samples, respectively. While some geographic substructure was detected across the population samples as clines in admixture frequencies, 20 of the 22 population samples were found to be statistically indistinguishable by pairwise comparisons and AMOVA calculations. Datasets from Hawaii and Idaho, however, were clear outliers. Overall, these more than 2500 control region sequences represent the most comprehensive regional sampling of African American mtDNA diversity to date, and are suitable for use in a forensic mtDNA database. The population data are made available via EMPOP (www.empop.org) and GenBank. (C) 2016 Elsevier Ireland Ltd. All rights reserved.
C1 [Scheible, M.; Just, R.; Sturk-Andreaggi, K.; Saunier, J.; Parsons, T.; Coble, M.; Irwin, J.] Armed Forces DNA Identificat Lab, 115 Purple Heart Dr, Dover AFB, DE 19902 USA.
[Scheible, M.; Just, R.; Sturk-Andreaggi, K.; Saunier, J.; Parsons, T.; Coble, M.; Irwin, J.] Amer Registry Pathol, 9210 Corp Blvd,Suite 120, Rockville, MD 20850 USA.
[Parson, W.] Med Univ Innsbruck, Inst Legal Med, Mullerstr 44, A-6020 Innsbruck, Austria.
[Parson, W.; Parsons, T.] Penn State Eberly Coll Sci, 517 Thomas Bldg, University Pk, PA 16802 USA.
[Scheible, M.] N Carolina State Univ, Forens Sci Inst, 1060 William Moore Dr, Raleigh, NC 27607 USA.
[Scheible, M.] N Carolina State Univ, Dept Mol Biomed Sci, 1060 William Moore Dr, Raleigh, NC 27607 USA.
[Just, R.; Irwin, J.] Fed Bur Invest Acad, 2501 Invest Pkwy, Quantico, VA 22135 USA.
[Parsons, T.] Int Commiss Missing Persons, Alipasina 45A, Sarajevo 71000, Bosnia & Herceg.
[Coble, M.] NIST, 100 Bur Dr,M-S 8312, Gaithersburg, MD 20899 USA.
RP Scheible, M; Sturk-Andreaggi, K (reprint author), Armed Forces DNA Identificat Lab, 115 Purple Heart Dr, Dover AFB, DE 19902 USA.; Scheible, M; Sturk-Andreaggi, K (reprint author), Amer Registry Pathol, 9210 Corp Blvd,Suite 120, Rockville, MD 20850 USA.; Scheible, M (reprint author), N Carolina State Univ, Forens Sci Inst, 1060 William Moore Dr, Raleigh, NC 27607 USA.; Scheible, M (reprint author), N Carolina State Univ, Dept Mol Biomed Sci, 1060 William Moore Dr, Raleigh, NC 27607 USA.
EM mkscheib@ncsu.edu; kimberly.s.andreaggi.ctr@mail.mil
FU National Institute of Justice [2005-DN-R-086]
FX The authors would like to thank the Emerging Technologies Section, past
and present, especially Toni Diegoli, Elizabeth Lyons, Katharine
Strouss, Joanne Lee, Amanda Lehrmann, Kyla Harris, Brittany Box, Leslie
Mounkes, Erin Gorden, Rachel Kinsel, Morgan Falk, Naila Bhatri (AFDIL)
for data generation, analysis and review; Odile Loreille for ongoing
support and fruitful discussion; Charla Marshall (AFDIL) for assistance
with analyses; Liane Fendt, Theresa Harm, Gabriela Huber, Simone Nagl,
Daniela Niederwieser, Alexander Rock, Christina Strobl, and Bettina
Zimmermann (EMPOP, University of Innsbruck, Austria) for data analysis
and assistance with database confirmation; an anonymous reviewer and
John Buckleton for manuscript review and feedback; James Canik, Lanelle
Chisolm, Brion Smith, COL Louis Finelli, CAPT Edward Reedy, Lt Col Laura
Regan, Timothy McMahon, James Ross, Jon Norris, the American Registry of
Pathology and the Armed Forces Medical Examiner System for logistical,
administrative, and technical support; and the National Institute of
Justice (InterAgency Agreement 2005-DN-R-086) for funding.
NR 48
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PU ELSEVIER IRELAND LTD
PI CLARE
PA ELSEVIER HOUSE, BROOKVALE PLAZA, EAST PARK SHANNON, CO, CLARE, 00000,
IRELAND
SN 1872-4973
EI 1878-0326
J9 FORENSIC SCI INT-GEN
JI Forensic Sci. Int.-Genet.
PD MAY
PY 2016
VL 22
BP 139
EP 148
DI 10.1016/j.fsigen.2016.01.002
PG 10
WC Genetics & Heredity; Medicine, Legal
SC Genetics & Heredity; Legal Medicine
GA DH3WX
UT WOS:000372718600026
PM 26919661
ER
PT J
AU Bergmann, C
Barbour, J
LaForce, L
Driggers, WB
AF Bergmann, Charles
Barbour, James
LaForce, Lionel
Driggers, William B., III
TI Line cutter for use when releasing large marine organisms caught on
longline gear
SO FISHERIES RESEARCH
LA English
DT Article
DE Bycatch; Gangion; Line cutter; Monofilament; Prohibited species
AB Releasing large marine organisms captured on longline gear can often be difficult due to problems associated with the use of conventional line cutters. For example, struggling animals can remain below the water's surface for extended periods, thus providing limited access to the end of the leader nearest the hook. We describe a new line cutter design that outperforms conventional designs. The line cutter described herein can be deployed by a single individual and severs leader material in close proximity to the location of hooks while negating the need to bring the captured organism to the surface. The use of the line cutter reduces stress and potential injury to captured animals, is easily and inexpensively constructed, and has applications beyond its intended use, such as freeing lines snagged or entangled under vessels. Published by Elsevier B.V.
C1 [Bergmann, Charles; Barbour, James; LaForce, Lionel; Driggers, William B., III] Natl Marine Fisheries Serv, Southeast Fisheries Sci Ctr, Mississippi Labs, PO Drawer 1207, Pascagoula, MS 39567 USA.
RP Driggers, WB (reprint author), Natl Marine Fisheries Serv, Southeast Fisheries Sci Ctr, Mississippi Labs, PO Drawer 1207, Pascagoula, MS 39567 USA.
EM william.driggers@noaa.gov
NR 5
TC 0
Z9 0
U1 1
U2 1
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0165-7836
EI 1872-6763
J9 FISH RES
JI Fish Res.
PD MAY
PY 2016
VL 177
BP 124
EP 127
DI 10.1016/j.fishres.2016.01.018
PG 4
WC Fisheries
SC Fisheries
GA DG9BU
UT WOS:000372378600014
ER
PT J
AU Zhang, MY
Wang, LY
Jajodia, S
Singhal, A
Albanese, M
AF Zhang, Mengyuan
Wang, Lingyu
Jajodia, Sushil
Singhal, Anoop
Albanese, Massimiliano
TI Network Diversity: A Security Metric for Evaluating the Resilience of
Networks Against Zero-Day Attacks
SO IEEE TRANSACTIONS ON INFORMATION FORENSICS AND SECURITY
LA English
DT Article
DE Biodiversity; computer security; firewalls; information security;
intrusion detection
ID DESIGN DIVERSITY; ACCESS-CONTROL; CLOUD; VULNERABILITY; SYSTEMS
AB Diversity has long been regarded as a security mechanism for improving the resilience of software and networks against various attacks. More recently, diversity has found new applications in cloud computing security, moving target defense, and improving the robustness of network routing. However, most existing efforts rely on intuitive and imprecise notions of diversity, and the few existing models of diversity are mostly designed for a single system running diverse software replicas or variants. At a higher abstraction level, as a global property of the entire network, diversity and its effect on security have received limited attention. In this paper, we take the first step toward formally modeling network diversity as a security metric by designing and evaluating a series of diversity metrics. In particular, we first devise a biodiversity-inspired metric based on the effective number of distinct resources. We then propose two complementary diversity metrics, based on the least and the average attacking efforts, respectively. We provide guidelines for instantiating the proposed metrics and present a case study on estimating software diversity. Finally, we evaluate the proposed metrics through simulation.
C1 [Zhang, Mengyuan; Wang, Lingyu] Concordia Univ, Concordia Inst Informat Syst Engn, Montreal, PQ H3G 1M8, Canada.
[Jajodia, Sushil; Albanese, Massimiliano] George Mason Univ, Ctr Secure Informat Syst, Fairfax, VA 22030 USA.
[Singhal, Anoop] NIST, Comp Secur Div, Gaithersburg, MD 20899 USA.
RP Zhang, MY; Wang, LY (reprint author), Concordia Univ, Concordia Inst Informat Syst Engn, Montreal, PQ H3G 1M8, Canada.; Jajodia, S; Albanese, M (reprint author), George Mason Univ, Ctr Secure Informat Syst, Fairfax, VA 22030 USA.; Singhal, A (reprint author), NIST, Comp Secur Div, Gaithersburg, MD 20899 USA.
EM mengy_zh@ciise.concordia.ca; wang@ciise.concordia.ca; jajodia@gmu.edu;
anoop.singhal@nist.gov; malbanes@gmu.edu
FU National Science Foundation [IIP-1266147]; Natural Sciences and
Engineering Research Council of Canada [N01035]; National Institute of
Standards and Technology [60NANB14D060, 60NANB15D091]; Office of Naval
Research [N00014-15-1-2007]; Army Research Office [W911NF-13-1-0421]
FX This work was supported in part by the National Science Foundation under
Grant IIP-1266147, in part by the Natural Sciences and Engineering
Research Council of Canada Discovery under Grant N01035, in part by the
National Institute of Standards and Technology under Grant 60NANB14D060
and Grant 60NANB15D091, in part by the Office of Naval Research under
Grant N00014-15-1-2007, and in part by the Army Research Office under
Grant W911NF-13-1-0421. The associate editor coordinating the review of
this manuscript and approving it for publication was Dr. Jianying Zhou.
NR 56
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U1 10
U2 25
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 1556-6013
EI 1556-6021
J9 IEEE T INF FOREN SEC
JI IEEE Trans. Inf. Forensic Secur.
PD MAY
PY 2016
VL 11
IS 5
BP 1071
EP 1086
DI 10.1109/TIFS.2016.2516916
PG 16
WC Computer Science, Theory & Methods; Engineering, Electrical & Electronic
SC Computer Science; Engineering
GA DG8SZ
UT WOS:000372355200015
ER
PT J
AU Pannkuk, EL
Laiakis, EC
Mak, TD
Astarita, G
Authier, S
Wong, KR
Fornace, AJ
AF Pannkuk, Evan L.
Laiakis, Evagelia C.
Mak, Tytus D.
Astarita, Giuseppe
Authier, Simon
Wong, Karen
Fornace, Albert J., Jr.
TI A lipidomic and metabolomic serum signature from nonhuman primates
exposed to ionizing radiation
SO METABOLOMICS
LA English
DT Article
DE Lipidomics; Metabolomics; Ionizing Radiation; Nonhuman Primate
ID POLYUNSATURATED FATTY-ACIDS; GAMMA-IRRADIATED RATS; BIOMARKER DISCOVERY;
URINARY BIOMARKERS; BODY IRRADIATION; LIVER-DISEASE; IDENTIFICATION;
MICE; MECHANISMS; INJURY
AB Introduction Due to dangers associated with potential accidents from nuclear energy and terrorist threats, there is a need for high-throughput biodosimetry to rapidly assess individual doses of radiation exposure. Lipidomics and metabolomics are becoming common tools for determining global signatures after disease or other physical insult and provide a "snapshot'' of potential cellular damage.
Objectives The current study assesses changes in the nonhuman primate (NHP) serum lipidome and metabolome 7 days following exposure to ionizing radiation (IR). Methods Serum sample lipids and metabolites were extracted using a biphasic liquid-liquid extraction and analyzed by ultra performance liquid chromatography quadrupole time-of-flight mass spectrometry. Global radiation signatures were acquired in data-independent mode.
Results Radiation exposure caused significant perturbations in lipid metabolism, affecting all major lipid species, including free fatty acids, glycerolipids, glycerophospholipids and esterified sterols. In particular, we observed a significant increase in the levels of polyunsaturated fatty acids (PUFA)-containing lipids in the serum of NHPs exposed to 10 Gy radiation, suggesting a primary role played by PUFAs in the physiological response to IR. Metabolomics profiling indicated an increase in the levels of amino acids, carnitine, and purine metabolites in the serum of NHPs exposed to 10 Gy radiation, suggesting perturbations to protein digestion/absorption, biological oxidations, and fatty acid b-oxidation.
Conclusions This is the first report to determine changes in the global NHP serum lipidome and metabolome following radiation exposure and provides information for developing metabolomic biomarker panels in human-based biodosimetry.
C1 [Pannkuk, Evan L.; Laiakis, Evagelia C.; Astarita, Giuseppe; Fornace, Albert J., Jr.] Georgetown Univ, Med Ctr, Dept Biochem & Mol & Cellular Biol, Washington, DC 20007 USA.
[Mak, Tytus D.] Natl Inst Stand & Technol, Mass Spectrometry Data Ctr, Gaithersburg, MD 20899 USA.
[Astarita, Giuseppe] Waters Corp, Hlth Sci, Milford, MA USA.
[Authier, Simon; Wong, Karen] CiToxLAB North Amer, Laval, PQ, Canada.
[Fornace, Albert J., Jr.] Lombardi Comprehens Canc Ctr, 3970 Reservoir Rd NW,New Res Bldg,Room E504, Washington, DC 20057 USA.
[Fornace, Albert J., Jr.] King Abdulaziz Univ, Ctr Excellence Genom Med Res CEGMR, Jeddah 21413, Saudi Arabia.
RP Fornace, AJ (reprint author), Georgetown Univ, Med Ctr, Dept Biochem & Mol & Cellular Biol, Washington, DC 20007 USA.; Fornace, AJ (reprint author), Lombardi Comprehens Canc Ctr, 3970 Reservoir Rd NW,New Res Bldg,Room E504, Washington, DC 20057 USA.; Fornace, AJ (reprint author), King Abdulaziz Univ, Ctr Excellence Genom Med Res CEGMR, Jeddah 21413, Saudi Arabia.
EM af294@georgetown.edu
OI Fornace, Albert/0000-0001-9695-085X
FU National Institutes of Health (National Institute of Allergy and
Infectious Diseases) [1R01AI101798]; Lombardi Comprehensive Cancer
Proteomics and Metabolomics Shared Resource (PMSR); National Cancer
Institute [P30CA051008]
FX National Institutes of Health (National Institute of Allergy and
Infectious Diseases) grant 1R01AI101798 (P.I. Albert J. Fornace, Jr.)
and Lombardi Comprehensive Cancer Proteomics and Metabolomics Shared
Resource (PMSR); partial support National Cancer Institute grant
P30CA051008 (P.I. Louis Weiner).
NR 54
TC 1
Z9 2
U1 6
U2 27
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1573-3882
EI 1573-3890
J9 METABOLOMICS
JI Metabolomics
PD MAY
PY 2016
VL 12
IS 5
AR 80
DI 10.1007/s11306-016-1010-0
PG 11
WC Endocrinology & Metabolism
SC Endocrinology & Metabolism
GA DG5YL
UT WOS:000372157700003
ER
PT J
AU Zhuang, ZR
Yussouf, N
Gao, JD
AF Zhuang, Zhaorong
Yussouf, Nusrat
Gao, Jidong
TI Analyses and forecasts of a tornadic supercell outbreak using a 3DVAR
system ensemble
SO ADVANCES IN ATMOSPHERIC SCIENCES
LA English
DT Article
DE ensemble 3DVAR analysis; radar data assimilation; probabilistic
forecast; supercell storm
ID VARIATIONAL STATISTICAL-ANALYSIS; MESOSCALE CONVECTIVE SYSTEM; DOPPLER
RADAR OBSERVATIONS; KALMAN FILTER APPROACH; WARN-ON-FORECAST; LEVEL-II
DATA; DATA ASSIMILATION; PART I; MICROPHYSICS SCHEME; RECURSIVE FILTERS
AB As part of NOAA's "Warn-On-Forecast" initiative, a convective-scale data assimilation and prediction system was developed using the WRF-ARW model and ARPS 3DVAR data assimilation technique. The system was then evaluated using retrospective short-range ensemble analyses and probabilistic forecasts of the tornadic supercell outbreak event that occurred on 24 May 2011 in Oklahoma, USA. A 36-member multi-physics ensemble system provided the initial and boundary conditions for a 3-km convective-scale ensemble system. Radial velocity and reflectivity observations from four WSR-88Ds were assimilated into the ensemble using the ARPS 3DVAR technique. Five data assimilation and forecast experiments were conducted to evaluate the sensitivity of the system to data assimilation frequencies, in-cloud temperature adjustment schemes, and fixed- and mixed-microphysics ensembles. The results indicated that the experiment with 5-min assimilation frequency quickly built up the storm and produced a more accurate analysis compared with the 10-min assimilation frequency experiment. The predicted vertical vorticity from the moist-adiabatic in-cloud temperature adjustment scheme was larger in magnitude than that from the latent heat scheme. Cycled data assimilation yielded good forecasts, where the ensemble probability of high vertical vorticity matched reasonably well with the observed tornado damage path. Overall, the results of the study suggest that the 3DVAR analysis and forecast system can provide reasonable forecasts of tornadic supercell storms.
C1 [Zhuang, Zhaorong; Yussouf, Nusrat] Univ Oklahoma, Cooperat Inst Mesoscale Meteorol Studies, Norman, OK 73072 USA.
[Zhuang, Zhaorong] China Meteorol Adm, Natl Meteorol Ctr, Ctr Numer Weather Predict, Beijing 100081, Peoples R China.
[Yussouf, Nusrat; Gao, Jidong] NOAA, Natl Severe Storms Lab, Norman, OK 73072 USA.
RP Zhuang, ZR (reprint author), Univ Oklahoma, Cooperat Inst Mesoscale Meteorol Studies, Norman, OK 73072 USA.; Zhuang, ZR (reprint author), China Meteorol Adm, Natl Meteorol Ctr, Ctr Numer Weather Predict, Beijing 100081, Peoples R China.
EM zhuangzr@cams.cma.gov.cn
FU NOAA/Office of Oceanic and Atmospheric Research under the
NOAA-University of Oklahoma Cooperative Agreement [NA17RJ1227]; U.S.
Department of Commerce; NSF [AGS-1341878]; National Natural Science
Foundation of China [41305092]; International S&T Cooperation Program of
China (ISTCP) [2011DFG23210]
FX Partial funding for this research was provided by the NOAA/Office of
Oceanic and Atmospheric Research under the NOAA-University of Oklahoma
Cooperative Agreement #NA17RJ1227, the U.S. Department of Commerce and
NSF AGS-1341878, the National Natural Science Foundation of China
(Project No. 41305092), and the International S&T Cooperation Program of
China (ISTCP) (Grant No. 2011DFG23210). We thank our colleague Dr.
Thomas JONES for proofreading the manuscript. Thanks also to Carrie
LANGSTON for the NMQ reflectivity data. The computing for this project
was performed at the University of Oklahoma (OU) Supercomputing Center
for Education & Research (OSCER). Local computer assistance was provided
by Brett MORROW, Steven FLETCHER, Brad SWAGOWITZ, and Karen COOPER.
NR 61
TC 1
Z9 1
U1 3
U2 13
PU SCIENCE PRESS
PI BEIJING
PA 16 DONGHUANGCHENGGEN NORTH ST, BEIJING 100717, PEOPLES R CHINA
SN 0256-1530
EI 1861-9533
J9 ADV ATMOS SCI
JI Adv. Atmos. Sci.
PD MAY
PY 2016
VL 33
IS 5
BP 544
EP 558
DI 10.1007/s00376-015-5072-0
PG 15
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DF3HI
UT WOS:000371234300002
ER
PT J
AU Chirico, RD
Steele, WV
Kazakov, AF
AF Chirico, Robert D.
Steele, William V.
Kazakov, Andrei F.
TI Thermodynamic properties of indan: Experimental and computational
results
SO JOURNAL OF CHEMICAL THERMODYNAMICS
LA English
DT Article
DE Computational chemistry; Density; Entropy; Heat capacity; Ideal-gas
properties; Indan; Phase-transition properties; Vapor pressure
ID THERMODATA ENGINE TDE; 3RD VIRIAL-COEFFICIENT; SOFTWARE IMPLEMENTATION;
VAPOR-PRESSURE; MUTUAL VALIDATION; TEMPERATURE-SCALE; HEAT-CAPACITIES;
RECONCILIATION; VAPORIZATION; HYDROCARBONS
AB Measurements leading to the calculation of thermodynamic properties in the ideal-gas state for indan (Chemical Abstracts registry number [496-11-7], 2,3-dihydro-1H-indene) are reported. Experimental methods were adiabatic heat-capacity calorimetry, differential scanning calorimetry, comparative ebulliometry, and vibrating-tube densitometry. Molar thermodynamic functions (enthalpies, entropies, and Gibbs energies) for the condensed and ideal-gas states were derived from the experimental studies at selected temperatures. Statistical calculations were performed based on molecular geometry optimization and vibrational frequencies calculated at the B3LYP/6-31+G(d, p) level of theory. Computed ideal-gas properties derived with the rigid-rotor harmonic-oscillator approximation are shown to be in excellent accord with ideal-gas entropies derived from thermophysical property measurements of this research, as well as with experimental heat capacities for the ideal-gas state reported in the literature. Literature spectroscopic studies and ab initio calculations report a range of values for the barrier to ring puckering. Results of the present work are consistent with a large barrier that allows use of the rigid-rotor harmonic-oscillator approximation for ideal-gas entropy and heat-capacity calculations, even with the stringent uncertainty requirements imposed by the calorimetric and physical property measurements reported here. All experimental results are compared with property values reported in the literature. (C) 2016 Published by Elsevier Ltd.
C1 [Chirico, Robert D.; Kazakov, Andrei F.] NIST, Thermodynam Res Ctr, Appl Chem & Mat Div, Boulder, CO 80305 USA.
[Steele, William V.] Univ Tennessee, Phys Properties Res Facil, Chem & Biomol Engn Dept, Knoxville, TN 37996 USA.
RP Chirico, RD (reprint author), NIST, Thermodynam Res Ctr, Appl Chem & Mat Div, Boulder, CO 80305 USA.
EM robert.chirico@nist.gov
FU Office of Fossil Energy of the U.S. Department of Energy (DOE);
Processing and Downstream Operations section of the Advanced Oil
Recovery (AOR) program; DOE [DE-AC22-94C91008]
FX We gratefully acknowledge the contributions of Stephen E. Knipmeyer in
the dsc studies, An (Andy) Nguyen in the vapor-pressure and density
measurements, and Aaron P. Rau and I. Alex Hossenlopp in vapor transfer
of chemical samples in preparation for the physical property
measurements. The authors acknowledge the financial support of the
Office of Fossil Energy of the U.S. Department of Energy (DOE). This
research was funded within the Processing and Downstream Operations
section of the Advanced Oil Recovery (AOR) program. The property
measurements were completed in Bartlesville, Oklahoma at the National
Institute of Petroleum and Energy Research through BDM-Oklahoma under
its contract with DOE for Management and Operations of the National Oil
and Related Programs (NORP), Contract Number DE-AC22-94C91008. The
article preparation and computations were carried out at the National
Institute of Standards and Technology (NIST). This article is, in part,
a contribution of NIST, and is not subject to copyright in the United
States for the authors R.D.C and A.F.K. Products or companies are named
solely for descriptive clarity and this neither constitutes nor implies
endorsement by NIST or by the U.S. government.
NR 70
TC 1
Z9 1
U1 2
U2 25
PU ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
PI LONDON
PA 24-28 OVAL RD, LONDON NW1 7DX, ENGLAND
SN 0021-9614
EI 1096-3626
J9 J CHEM THERMODYN
JI J. Chem. Thermodyn.
PD MAY
PY 2016
VL 96
BP 41
EP 51
DI 10.1016/j.jct.2015.12.005
PG 11
WC Thermodynamics; Chemistry, Physical
SC Thermodynamics; Chemistry
GA DC0JR
UT WOS:000368903600005
ER
PT J
AU Tewary, VK
Quardokus, RC
DelRio, FW
AF Tewary, V. K.
Quardokus, Rebecca C.
DelRio, Frank W.
TI Green's function modeling of response of two-dimensional materials to
point probes for scanning probe microscopy
SO PHYSICS LETTERS A
LA English
DT Article
DE Antidots; Graphene; Green's function; Materials characterization;
Scanning probe microscopy; Two-dimensional materials
ID SEMICONDUCTOR; GROWTH; HEAT; WS2
AB A Green's function (GF) method is developed for interpreting scanning probe microscopy (SPM) measurements on new two-dimensional (2D) materials. GFs for the Laplace/Poisson equations are calculated by using a virtual source method for two separate cases of a finite material containing a rectangular defect and a hexagonal defect. The prescribed boundary values are reproduced almost exactly by the calculated GFs. It is suggested that the GF is not just a mathematical artefact but a basic physical characteristic of material systems, which can be measured directly by SPM for 2D solids. This should make SPM an even more powerful technique for characterization of 2D materials. Published by Elsevier B.V.
C1 [Tewary, V. K.; Quardokus, Rebecca C.; DelRio, Frank W.] NIST, Appl Chem & Mat Div, Boulder, CO 80305 USA.
RP Tewary, VK (reprint author), NIST, Appl Chem & Mat Div, Boulder, CO 80305 USA.
EM vinod.tewary@nist.gov; rebecca.quardokus@nist.gov; frank.delrio@nist.gov
NR 41
TC 1
Z9 1
U1 4
U2 7
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0375-9601
EI 1873-2429
J9 PHYS LETT A
JI Phys. Lett. A
PD APR 29
PY 2016
VL 380
IS 20
BP 1750
EP 1756
DI 10.1016/j.physleta.2016.03.021
PG 7
WC Physics, Multidisciplinary
SC Physics
GA DK0KH
UT WOS:000374601200013
ER
PT J
AU Brown, PT
Lozier, MS
Zhang, R
Li, WH
AF Brown, Patrick T.
Lozier, M. Susan
Zhang, Rong
Li, Wenhong
TI The necessity of cloud feedback for a basin-scale Atlantic Multidecadal
Oscillation
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID MERIDIONAL OVERTURNING CIRCULATION; SEA-SURFACE TEMPERATURE; COUPLED
CLIMATE MODELS; NORTH-ATLANTIC; SAHEL RAINFALL; AIR-TEMPERATURE;
VARIABILITY; MECHANISMS; HEMISPHERE; SIGNATURE
AB The Atlantic Multidecadal Oscillation (AMO), characterized by basin-scale multidecadal variability in North Atlantic sea surface temperatures (SSTs), has traditionally been interpreted as the surface signature of variability in oceanic heat convergence (OHC) associated with the Atlantic Meridional Overturning Circulation (AMOC). This view has been challenged by recent studies that show that AMOC variability is not simultaneously meridionally coherent over the North Atlantic and that AMOC-induced low-frequency variability of OHC is weak in the tropical North Atlantic. Here we present modeling evidence that the AMO-related SST variability over the extratropical North Atlantic results directly from anomalous OHC associated with the AMOC but that the emergence of the coherent multidecadal SST variability over the tropical North Atlantic requires cloud feedback. Our study identifies atmospheric processes as a necessary component for the existence of a basin-scale AMO, thus amending the canonical view that the AMOC-AMO connection is solely attributable to oceanic processes.
C1 [Brown, Patrick T.; Lozier, M. Susan; Li, Wenhong] Duke Univ, Nicholas Sch Environm, Earth & Ocean Sci, Durham, NC 27708 USA.
[Zhang, Rong] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA.
RP Brown, PT (reprint author), Duke Univ, Nicholas Sch Environm, Earth & Ocean Sci, Durham, NC 27708 USA.
EM Patrick.Brown@duke.edu
RI Zhang, Rong/D-9767-2014
OI Zhang, Rong/0000-0002-8493-6556
FU NSF [AGS-1147608, OCE-1259102]; NIH [NIH-1R21AG044294-01A1]
FX We thank Ming Zhao and Xiaosong Yang for their internal reviews and
discussion of this work. We acknowledge the World Climate Research
Programme's Working Group on Coupled Modelling, which is responsible for
CMIP, and we thank the climate modeling groups for producing and making
available their model output. For CMIP the U.S. Department of Energy's
Program for Climate Model Diagnosis and Intercomparison provides
coordinating support and led development of software infrastructure in
partnership with the Global Organization for Earth System Science
Portals. The CMIP5 data used for this study can be downloaded at
http://cmip-pcmdi.llnl.gov/cmip5/data_portal.html, and the GFDL CM2.1
model output can be downloaded at http://data1.gfdl.noaa.gov/. Contact
Patrick Brown (patrick.brown@duke.edu) for other data and code requests.
This work was partially supported by NSF grants AGS-1147608 and
OCE-1259102, as well as by the NIH grant NIH-1R21AG044294-01A1.
NR 55
TC 5
Z9 5
U1 3
U2 7
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 APR 28
PY 2016
VL 43
IS 8
BP 3955
EP 3963
DI 10.1002/2016GL068303
PG 9
WC Geosciences, Multidisciplinary
SC Geology
GA DP2RQ
UT WOS:000378338800042
ER
PT J
AU Link, MF
Friedman, B
Fulgham, R
Brophy, P
Galang, A
Jathar, SH
Veres, P
Roberts, JM
Farmer, DK
AF Link, M. F.
Friedman, B.
Fulgham, R.
Brophy, P.
Galang, A.
Jathar, S. H.
Veres, P.
Roberts, J. M.
Farmer, D. K.
TI Photochemical processing of diesel fuel emissions as a large secondary
source of isocyanic acid (HNCO)
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID IONIZATION MASS-SPECTROMETRY; ION PROTON-TRANSFER; ORGANIC AEROSOL
FORMATION; NI-PT-CIMS; PROTEIN CARBAMYLATION; RADICAL CHEMISTRY; FLOW
REACTORS; AMBIENT AIR; OXIDATION; EXHAUST
AB Isocyanic acid (HNCO) is a well-known air pollutant that affects human health. Biomass burning, smoking, and combustion engines are known HNCO sources, but recent studies suggest that secondary production in the atmosphere may also occur. We directly observed photochemical production of HNCO from the oxidative aging of diesel exhaust during the Diesel Exhaust Fuel and Control experiments at Colorado State University using acetate ionization time-of-flight mass spectrometry. Emission ratios of HNCO were enhanced, after 1.5 days of simulated atmospheric aging, from 50 to 230 mg HNCO/kg fuel at idle engine operating conditions. Engines operated at higher loads resulted in less primary and secondary HNCO formation, with emission ratios increasing from 20 to 40 mg HNCO/kg fuel under 50% load engine operating conditions. These results suggest that photochemical sources of HNCO could be more significant than primary sources in urban areas.
C1 [Link, M. F.; Friedman, B.; Fulgham, R.; Brophy, P.; Farmer, D. K.] Colorado State Univ, Dept Chem, Ft Collins, CO 80523 USA.
[Galang, A.; Jathar, S. H.] Colorado State Univ, Dept Mech Engn, Ft Collins, CO 80523 USA.
[Veres, P.] Univ Colorado, NOAA, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Veres, P.; Roberts, J. M.] NOAA, Div Chem Sci, Earth Syst Res Lab, Boulder, CO USA.
RP Farmer, DK (reprint author), Colorado State Univ, Dept Chem, Ft Collins, CO 80523 USA.
EM delphine.farmer@rams.colostate.edu
RI Veres, Patrick/E-7441-2010; Roberts, James/A-1082-2009; Manager, CSD
Publications/B-2789-2015
OI Veres, Patrick/0000-0001-7539-353X; Roberts, James/0000-0002-8485-8172;
FU Arnold and Mabel Beckman Young Investigator Award; Colorado State
University; NOAA Health of the Atmosphere Initiative
FX We acknowledge an Arnold and Mabel Beckman Young Investigator Award for
funding this work. Fees associated with the engine dynamometer tests
(engine operation, equipment rental, fuel, and personnel) were supported
through Shantanu Jathar's startup funds as new faculty hire at Colorado
State University. We would like to thank Kirk Evans for technical
support and undergraduate researchers Liam Lewane and Nathan Reed for
test support during the campaign. The NOAA/Earth Systems Research
Laboratory Chemical Sciences Division effort was supported by the NOAA
Health of the Atmosphere Initiative. Any data presented and analyzed in
this study can be acquired per request to the corresponding author.
Detailed discussions of measurements and analysis are in the supporting
information.
NR 43
TC 3
Z9 3
U1 14
U2 17
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 APR 28
PY 2016
VL 43
IS 8
BP 4033
EP 4041
DI 10.1002/2016GL068207
PG 9
WC Geosciences, Multidisciplinary
SC Geology
GA DP2RQ
UT WOS:000378338800051
ER
PT J
AU Chremos, A
Douglas, JF
AF Chremos, Alexandros
Douglas, Jack F.
TI Influence of higher valent ions on flexible polyelectrolyte stiffness
and counter-ion distribution
SO JOURNAL OF CHEMICAL PHYSICS
LA English
DT Article
ID MOLECULAR-DYNAMICS SIMULATIONS; LIMITING LAWS; EXPLICIT SOLVENT; POOR
SOLVENTS; CONDENSATION; DNA; SPECTROSCOPY; CATIONS; BINDING; TRANSITIONS
AB We investigate the influence of counter-ion valency on the flexibility of highly charged flexible polymer chains using molecular dynamics simulations that include both salt and an explicit solvent. As observed experimentally, we find that divalent counter-ions greatly reduce the chain persistence length, l(p), in comparison with monovalent counter-ions. On the other hand, polyelectrolyte chains having trivalent counter-ions adopt a much more compact conformation than polyelectrolytes having monovalent and divalent counter-ions. We demonstrate that the tendency of polyelectrolyte chains to become deformed by proximal high valence counter-ions is due to chain "coiling" around the counterions. In particular, we find that the number of contacts that the proximal counter-ions have with the polyelectrolyte dictates the extent of chain coiling. This ion-binding induced coiling mechanism influences not only the conformational properties of the polyelectrolyte, but also the counter-ion distribution around the chain. Specifically, we find that higher valent counter-ions lead both to a counter-ion enrichment in close proximity to the polyelectrolyte and to a significant reduction in the spatial extent of the diffuse counter-ion cloud around the polyelectrolyte.
C1 [Chremos, Alexandros; Douglas, Jack F.] NIST, Mat Sci & Engn Div, Gaithersburg, MD 20899 USA.
RP Chremos, A; Douglas, JF (reprint author), NIST, Mat Sci & Engn Div, Gaithersburg, MD 20899 USA.
EM alexandros.chremos@nist.gov; jack.douglas@nist.gov
RI Chremos, Alexandros/B-8856-2009
OI Chremos, Alexandros/0000-0002-1254-3972
FU NIST Director's Office through the NIST Fellows' postdoctoral grants
program
FX We gratefully acknowledge the support of the NIST Director's Office
through the NIST Fellows' postdoctoral grants program. Official
contribution of the U.S. National Institute of Standards and Technology
- not subject to copyright in the United States.
NR 57
TC 1
Z9 1
U1 5
U2 11
PU AMER INST PHYSICS
PI MELVILLE
PA 1305 WALT WHITMAN RD, STE 300, MELVILLE, NY 11747-4501 USA
SN 0021-9606
EI 1089-7690
J9 J CHEM PHYS
JI J. Chem. Phys.
PD APR 28
PY 2016
VL 144
IS 16
AR 164904
DI 10.1063/1.4947221
PG 9
WC Chemistry, Physical; Physics, Atomic, Molecular & Chemical
SC Chemistry; Physics
GA DL6YK
UT WOS:000375785800049
PM 27131566
ER
PT J
AU Yoon, S
Liu, J
McMichael, RD
AF Yoon, Seungha
Liu, Jason
McMichael, Robert D.
TI Phase-resolved ferromagnetic resonance using a heterodyne detection
method
SO PHYSICAL REVIEW B
LA English
DT Article
ID MAGNETIC TUNNEL-JUNCTIONS; SPIN-TRANSFER-TORQUE; MICROSCOPE; FIELD
AB This paper describes a phase-resolved ferromagnetic resonance (FMR) measurement using a heterodyne method. Spin precession is driven by microwave fields and detected by 1550 nm laser light that is modulated at a frequency slightly shifted with respected to the FMR driving frequency. The evolving phase difference between the spin precession and the modulated light produces a slowly oscillating Kerr rotation signal with a phase equal to the precession phase plus a phase due to the path length difference between the excitation microwave signal and the optical signal. We estimate the accuracy of the precession phase measurement to be 0.1 rad. This heterodyne FMR detection method eliminates the need for field modulation and allows a stronger detection signal at higher intermediate frequency where the 1/f noise floor is reduced.
C1 [Yoon, Seungha; Liu, Jason; McMichael, Robert D.] NIST, Ctr Nanoscale Sci & Technol, Gaithersburg, MD 20899 USA.
[Yoon, Seungha] Univ Maryland, Maryland Nanoctr, College Pk, MD 20742 USA.
RP Yoon, S (reprint author), NIST, Ctr Nanoscale Sci & Technol, Gaithersburg, MD 20899 USA.
FU University of Maryland [70NANB10H193]; National Institute of Standards
and Technology Center for Nanoscale Science and Technology through the
University of Maryland [70NANB10H193]
FX S.Y. acknowledges support under the Cooperative Research Agreement
between the University of Maryland and the National Institute of
Standards and Technology Center for Nanoscale Science and Technology,
Award No. 70NANB10H193, through the University of Maryland.
NR 40
TC 0
Z9 0
U1 5
U2 15
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 2469-9950
EI 2469-9969
J9 PHYS REV B
JI Phys. Rev. B
PD APR 28
PY 2016
VL 93
IS 14
AR 144423
DI 10.1103/PhysRevB.93.144423
PG 8
WC Physics, Condensed Matter
SC Physics
GA DK5FR
UT WOS:000374945800002
ER
PT J
AU Ye, CX
Zhou, XL
Pu, D
Stutz, J
Festa, J
Spolaor, M
Tsai, C
Cantrell, C
Mauldin, RL
Campos, T
Weinheimer, A
Hornbrook, RS
Apel, EC
Guenther, A
Kaser, L
Yuan, B
Karl, T
Haggerty, J
Hall, S
Ullmann, K
Smith, JN
Ortega, J
Knote, C
AF Ye, Chunxiang
Zhou, Xianliang
Pu, Dennis
Stutz, Jochen
Festa, James
Spolaor, Max
Tsai, Catalina
Cantrell, Christopher
Mauldin, Roy L., III
Campos, Teresa
Weinheimer, Andrew
Hornbrook, Rebecca S.
Apel, Eric C.
Guenther, Alex
Kaser, Lisa
Yuan, Bin
Karl, Thomas
Haggerty, Julie
Hall, Samuel
Ullmann, Kirk
Smith, James N.
Ortega, John
Knote, Christoph
TI Rapid cycling of reactive nitrogen in the marine boundary layer
SO NATURE
LA English
DT Article
ID VOLATILE ORGANIC-COMPOUNDS; MASTER CHEMICAL MECHANISM; NITRIC-ACID
PHOTOLYSIS; MCM V3 PART; TROPOSPHERIC DEGRADATION; PHOTOCHEMICAL
PRODUCTION; FOREST CANOPY; AIR-QUALITY; DUST STORM; GAS-PHASE
AB Nitrogen oxides are essential for the formation of secondary atmospheric aerosols and of atmospheric oxidants such as ozone and the hydroxyl radical, which controls the self-cleansing capacity of the atmosphere(1). Nitric acid, a major oxidation product of nitrogen oxides, has traditionally been considered to be a permanent sink of nitrogen oxides(1). However, model studies predict higher ratios of nitric acid to nitrogen oxides in the troposphere than are observed(2,3). A 'renoxification' process that recycles nitric acid into nitrogen oxides has been proposed to reconcile observations with model studies(2-4), but the mechanisms responsible for this process remain uncertain(5-9). Here we present data from an aircraft measurement campaign over the North Atlantic Ocean and find evidence for rapid recycling of nitric acid to nitrous acid and nitrogen oxides in the clean marine boundary layer via particulate nitrate photolysis. Laboratory experiments further demonstrate the photolysis of particulate nitrate collected on filters at a rate more than two orders of magnitude greater than that of gaseous nitric acid, with nitrous acid as the main product. Box model calculations based on the Master Chemical Mechanism(10,11) suggest that particulate nitrate photolysis mainly sustains the observed levels of nitrous acid and nitrogen oxides at midday under typical marine boundary layer conditions. Given that oceans account for more than 70 per cent of Earth's surface, we propose that particulate nitrate photolysis could be a substantial tropospheric nitrogen oxide source. Recycling of nitrogen oxides in remote oceanic regions with minimal direct nitrogen oxide emissions could increase the formation of tropospheric oxidants and secondary atmospheric aerosols on a global scale.
C1 [Ye, Chunxiang; Zhou, Xianliang] New York State Dept Hlth, Wadsworth Ctr, Albany, NY USA.
[Zhou, Xianliang; Pu, Dennis] SUNY Albany, Dept Environm Hlth Sci, Albany, NY 12222 USA.
[Stutz, Jochen; Festa, James; Spolaor, Max; Tsai, Catalina] Univ Calif Los Angeles, Dept Atmospher & Ocean Sci, Los Angeles, CA 90024 USA.
[Cantrell, Christopher; Mauldin, Roy L., III] Univ Colorado, Dept Atmospher & Ocean Sci, Boulder, CO 80309 USA.
[Mauldin, Roy L., III] Univ Helsinki, Dept Phys, Helsinki, Finland.
[Campos, Teresa; Weinheimer, Andrew; Hornbrook, Rebecca S.; Apel, Eric C.; Kaser, Lisa; Haggerty, Julie; Hall, Samuel; Ullmann, Kirk; Smith, James N.; Ortega, John; Knote, Christoph] Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA.
[Guenther, Alex] Pacific NW Natl Lab, Richland, WA 99352 USA.
[Yuan, Bin] NOAA, Earth Syst Res Lab, Div Chem Sci, Boulder, CO USA.
[Yuan, Bin] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Karl, Thomas] Univ Innsbruck, Inst Meteorol & Geophys, A-6020 Innsbruck, Austria.
[Smith, James N.] Univ Eastern Finland, Kuopio, Finland.
[Knote, Christoph] Univ Munich, Inst Meteorol, Marchioninistr 15, D-81377 Munich, Germany.
RP Zhou, XL (reprint author), New York State Dept Hlth, Wadsworth Ctr, Albany, NY USA.; Zhou, XL (reprint author), SUNY Albany, Dept Environm Hlth Sci, Albany, NY 12222 USA.
EM xianliang.zhou@health.ny.gov
RI Smith, James/C-5614-2008; Karl, Thomas/D-1891-2009; Yuan,
Bin/A-1223-2012; Knote, Christoph/A-9809-2010; Manager, CSD
Publications/B-2789-2015
OI Smith, James/0000-0003-4677-8224; Karl, Thomas/0000-0003-2869-9426;
Yuan, Bin/0000-0003-3041-0329; Knote, Christoph/0000-0001-9105-9179;
FU National Science Foundation (NSF) [AGS-1216166, AGS-1215712,
AGS-1216743]; National Science Foundation
FX This research is funded by National Science Foundation (NSF) grants
(AGS-1216166, AGS-1215712, and AGS-1216743). We would like to
acknowledge operational, technical and scientific support provided by
NCAR's Earth Observing Laboratory, sponsored by the National Science
Foundation. Any opinions, findings, conclusions or recommendations
expressed in this paper are those of the authors and do not necessarily
reflect the views of NSF.
NR 51
TC 5
Z9 5
U1 37
U2 93
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 0028-0836
EI 1476-4687
J9 NATURE
JI Nature
PD APR 28
PY 2016
VL 532
IS 7600
BP 489
EP 491
DI 10.1038/nature17195
PG 3
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DK3KQ
UT WOS:000374815900044
PM 27064904
ER
PT J
AU Shingler, T
Crosbie, E
Ortega, A
Shiraiwa, M
Zuend, A
Beyersdorf, A
Ziemba, L
Anderson, B
Thornhill, L
Perring, AE
Schwarz, JP
Campazano-Jost, P
Day, DA
Jimenez, JL
Hair, JW
Mikoviny, T
Wisthaler, A
Sorooshian, A
AF Shingler, Taylor
Crosbie, Ewan
Ortega, Amber
Shiraiwa, Manabu
Zuend, Andreas
Beyersdorf, Andreas
Ziemba, Luke
Anderson, Bruce
Thornhill, Lee
Perring, Anne E.
Schwarz, Joshua P.
Campazano-Jost, Pedro
Day, Douglas A.
Jimenez, Jose L.
Hair, Johnathan W.
Mikoviny, Tomas
Wisthaler, Armin
Sorooshian, Armin
TI Airborne characterization of subsaturated aerosol hygroscopicity and dry
refractive index from the surface to 6.5km during the SEAC(4)RS campaign
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID ORGANIC-INORGANIC AEROSOLS; SINGLE-SCATTERING ALBEDO; LIQUID-LIQUID
EQUILIBRIA; OPTICAL-PROPERTIES; AMMONIUM-SULFATE; LIGHT-SCATTERING;
ACTIVITY-COEFFICIENTS; RADIATIVE PROPERTIES; CHEMICAL-COMPOSITION;
THERMODYNAMIC MODEL
AB In situ aerosol particle measurements were conducted during 21 NASA DC-8 flights in the Studies of Emissions and Atmospheric Composition, Clouds, and Climate Coupling by Regional Surveys field campaign over the United States, Canada, Pacific Ocean, and Gulf of Mexico. For the first time, this study reports rapid, size-resolved hygroscopic growth and real refractive index (RI at 532 nm) data between the surface and upper troposphere in a variety of air masses including wildfires, agricultural fires, biogenic, marine, and urban outflow. The Differential Aerosol Sizing and Hygroscopicity Spectrometer Probe (DASH-SP) quantified size-resolved diameter growth factors (GF = D-p,D-wet/D-p,D-dry) that are used to infer the hygroscopicity parameter kappa. Thermokinetic simulations were conducted to estimate the impact of partial particle volatilization within the DASH-SP across a range of sampling conditions. Analyses of GF and RI data as a function of air mass origin, dry size, and altitude are reported, in addition to kappa values for the inorganic and organic fractions of aerosol. Average RI values are found to be fairly constant (1.52-1.54) for all air mass categories. An algorithm is used to compare size-resolved DASH-SP GF with bulk scattering f(RH=80%) data obtained from a pair of nephelometers, and the results show that the two can only be reconciled if GF is assumed to decrease with increasing dry size above 400 nm (i.e., beyond the upper bound of DASH-SP measurements). Individual case studies illustrate variations of hygroscopicity as a function of dry size, environmental conditions, altitude, and composition.
C1 [Shingler, Taylor; Ortega, Amber; Sorooshian, Armin] Univ Arizona, Dept Chem & Environm Engn, Tucson, AZ USA.
[Crosbie, Ewan; Beyersdorf, Andreas; Ziemba, Luke; Anderson, Bruce; Thornhill, Lee; Hair, Johnathan W.] NASA, Langley Res Ctr, Chem & Dynam Branch, Hampton, VA 23665 USA.
[Crosbie, Ewan] Oak Ridge Associated Univ, Oak Ridge, TN USA.
[Shiraiwa, Manabu] Max Planck Inst Chem, Multiphase Chem Dept, Mainz, Germany.
[Zuend, Andreas] McGill Univ, Dept Atmospher & Ocean Sci, Montreal, PQ, Canada.
[Thornhill, Lee] Sci Syst & Applicat Inc, Hampton, VA USA.
[Perring, Anne E.; Schwarz, Joshua P.] NOAA, Chem Sci Div, Earth Syst Res Lab, Boulder, CO USA.
[Perring, Anne E.; Campazano-Jost, Pedro; Day, Douglas A.; Jimenez, Jose L.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Campazano-Jost, Pedro; Day, Douglas A.; Jimenez, Jose L.] Univ Colorado, Dept Chem & Biochem, Campus Box 215, Boulder, CO 80309 USA.
[Mikoviny, Tomas; Wisthaler, Armin] Univ Oslo, Dept Chem, Oslo, Norway.
[Wisthaler, Armin] Univ Innsbruck, Inst Ion Phys & Appl Phys, A-6020 Innsbruck, Austria.
[Sorooshian, Armin] Univ Arizona, Dept Atmospher Sci, Tucson, AZ USA.
RP Sorooshian, A (reprint author), Univ Arizona, Dept Chem & Environm Engn, Tucson, AZ USA.; Sorooshian, A (reprint author), Univ Arizona, Dept Atmospher Sci, Tucson, AZ USA.
EM armin@email.arizona.edu
RI Perring, Anne/G-4597-2013; Jimenez, Jose/A-5294-2008; schwarz,
joshua/G-4556-2013; Manager, CSD Publications/B-2789-2015
OI Perring, Anne/0000-0003-2231-7503; Jimenez, Jose/0000-0001-6203-1847;
schwarz, joshua/0000-0002-9123-2223;
FU NASA [NNX12AC10G, NNX14AP75G, NNX12AC03G, NNX15AT96G]; ONR
[N00014-10-1-0811]; NASA Earth and Space Science Fellowship
[NNX14AK79H]; Visiting Scientist Program at the National Institute of
Aerospace
FX All data and results are available from the corresponding author
(armin@email.arizona.edu). This research was funded by NASA grants
NNX12AC10G and NNX14AP75G. The development of the DASH-SP instrument was
funded by ONR grant N00014-10-1-0811. T.S. acknowledges support from a
NASA Earth and Space Science Fellowship (NNX14AK79H). P.C.J., D.A.D.,
and J.L.J. were supported by NASA grants NNX12AC03G and NNX15AT96G.
PTR-MS measurements during SEAC4RS were supported by the
Austrian Federal Ministry for Transport, Innovation and Technology
(bmvit) through the Austrian Space Applications Programme of the
Austrian Research Promotion Agency (FFG). A.W. and T.M. received support
from the Visiting Scientist Program at the National Institute of
Aerospace.
NR 98
TC 5
Z9 5
U1 8
U2 10
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 APR 27
PY 2016
VL 121
IS 8
BP 4188
EP 4210
DI 10.1002/2015JD024498
PG 23
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DP2KU
UT WOS:000378318100028
ER
PT J
AU Griffith, SM
Hansen, RF
Dusanter, S
Michoud, V
Gilman, JB
Kuster, WC
Veres, PR
Graus, M
de Gouw, JA
Roberts, J
Young, C
Washenfelder, R
Brown, SS
Thalman, R
Waxman, E
Volkamer, R
Tsai, C
Stutz, J
Flynn, JH
Grossberg, N
Lefer, B
Alvarez, SL
Rappenglueck, B
Mielke, LH
Osthoff, HD
Stevens, PS
AF Griffith, S. M.
Hansen, R. F.
Dusanter, S.
Michoud, V.
Gilman, J. B.
Kuster, W. C.
Veres, P. R.
Graus, M.
de Gouw, J. A.
Roberts, J.
Young, C.
Washenfelder, R.
Brown, S. S.
Thalman, R.
Waxman, E.
Volkamer, R.
Tsai, C.
Stutz, J.
Flynn, J. H.
Grossberg, N.
Lefer, B.
Alvarez, S. L.
Rappenglueck, B.
Mielke, L. H.
Osthoff, H. D.
Stevens, P. S.
TI Measurements of hydroxyl and hydroperoxy radicals during CalNex-LA:
Model comparisons and radical budgets
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID LASER-INDUCED FLUORESCENCE; IONIZATION MASS-SPECTROMETRY; VOLATILE
ORGANIC-COMPOUNDS; MCMA-2006 FIELD CAMPAIGN; MEXICO-CITY ATMOSPHERE;
MISSING OH SOURCE; NEW-YORK-CITY; NI-PT-CIMS; HO2 CONCENTRATIONS;
LOS-ANGELES
AB Measurements of hydroxyl (OH) and hydroperoxy (HO2*) radical concentrations were made at the Pasadena ground site during the CalNex-LA 2010 campaign using the laser-induced fluorescence-fluorescence assay by gas expansion technique. The measured concentrations of OH and HO2* exhibited a distinct weekend effect, with higher radical concentrations observed on the weekends corresponding to lower levels of nitrogen oxides (NOx). The radical measurements were compared to results from a zero-dimensional model using the Regional Atmospheric Chemical Mechanism-2 constrained by NOx and othermeasured trace gases. The chemical model overpredicted measured OH concentrations during the weekends by a factor of approximately 1.4 +/- 0.3 (1 sigma), but the agreement was better during the weekdays (ratio of 1.0 +/- 0.2). Model predicted HO2* concentrations underpredicted by a factor of 1.3 +/- 0.2 on the weekends, while measured weekday concentrations were underpredicted by a factor of 3.0 +/- 0.5. However, increasing the modeled OH reactivity to match the measured total OH reactivity improved the overall agreement for both OH and HO2* on all days. A radical budget analysis suggests that photolysis of carbonyls and formaldehyde together accounted for approximately 40% of radical initiation with photolysis of nitrous acid accounting for 30% at the measurement height and ozone photolysis contributing less than 20%. An analysis of the ozone production sensitivity reveals that during the week, ozone production was limited by volatile organic compounds throughout the day during the campaign but NOx limited during the afternoon on the weekends.
C1 [Griffith, S. M.; Dusanter, S.; Stevens, P. S.] Indiana Univ, Sch Publ & Environm Affairs, Bloomington, IN USA.
[Griffith, S. M.] Hong Kong Univ Sci & Technol, Dept Chem, Hong Kong, Hong Kong, Peoples R China.
[Hansen, R. F.; Stevens, P. S.] Indiana Univ, Dept Chem, Bloomington, IN USA.
[Hansen, R. F.] Univ Leeds, Sch Chem, Leeds LS2 9JT, W Yorkshire, England.
[Dusanter, S.; Michoud, V.] SAGE, Mines Douai, Douai, France.
[Dusanter, S.; Michoud, V.] Univ Lille, Lille, France.
[Michoud, V.] UPEC, Lab Interunivers Syst Atmospher, LISA IPSL, UMR CNRS 7583, Creteil, France.
[Michoud, V.] UPD, Creteil, France.
[Gilman, J. B.; Veres, P. R.; Graus, M.; de Gouw, J. A.; Roberts, J.; Young, C.; Washenfelder, R.; Brown, S. S.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Gilman, J. B.; Kuster, W. C.; Veres, P. R.; Graus, M.; de Gouw, J. A.; Roberts, J.; Young, C.; Washenfelder, R.; Brown, S. S.] NOAA, Chem Sci Div, Earth Syst Res Lab, Boulder, CO USA.
[Graus, M.] Univ Innsbruck, Inst Atmospher & Cryospher Sci, A-6020 Innsbruck, Austria.
[Young, C.] Mem Univ Newfoundland, Dept Chem, St John, NF A1B 3X7, Canada.
[Thalman, R.; Waxman, E.; Volkamer, R.] Univ Colorado, Dept Chem & Biochem, Campus Box 215, Boulder, CO 80309 USA.
[Thalman, R.; Waxman, E.; Volkamer, R.] Univ Colorado, CIRES, Boulder, CO 80309 USA.
[Thalman, R.] Snow Coll, Dept Chem, Ephraim, UT USA.
[Tsai, C.; Stutz, J.] Univ Calif Los Angeles, Dept Atmospher & Ocean Sci, Los Angeles, CA USA.
[Flynn, J. H.; Grossberg, N.; Lefer, B.; Alvarez, S. L.; Rappenglueck, B.] Univ Houston, Dept Earth & Atmospher Sci, Houston, TX USA.
[Lefer, B.] NASA Headquarters, Div Earth Sci, Washington, DC USA.
[Mielke, L. H.; Osthoff, H. D.] Univ Calgary, Dept Chem, Calgary, AB T2N 1N4, Canada.
[Mielke, L. H.] Univ Indianapolis, Dept Chem, Indianapolis, IN 46227 USA.
RP Stevens, PS (reprint author), Indiana Univ, Sch Publ & Environm Affairs, Bloomington, IN USA.; Stevens, PS (reprint author), Indiana Univ, Dept Chem, Bloomington, IN USA.
EM pstevens@indiana.edu
RI de Gouw, Joost/A-9675-2008; Veres, Patrick/E-7441-2010; Young,
Cora/A-4551-2010; Volkamer, Rainer/B-8925-2016; Gilman,
Jessica/E-7751-2010; Brown, Steven/I-1762-2013; Graus,
Martin/E-7546-2010; Roberts, James/A-1082-2009; Washenfelder,
Rebecca/E-7169-2010; Lefer, Barry/B-5417-2012; Manager, CSD
Publications/B-2789-2015;
OI de Gouw, Joost/0000-0002-0385-1826; Veres, Patrick/0000-0001-7539-353X;
Young, Cora/0000-0002-6908-5829; Volkamer, Rainer/0000-0002-0899-1369;
Gilman, Jessica/0000-0002-7899-9948; Graus, Martin/0000-0002-2025-9242;
Roberts, James/0000-0002-8485-8172; Washenfelder,
Rebecca/0000-0002-8106-3702; Lefer, Barry/0000-0001-9520-5495; Osthoff,
Hans/0000-0001-7155-6493
FU National Science Foundation [AGS-0612738, AGS-1104880]
FX This work was supported by grants from the National Science Foundation
(AGS-0612738 and AGS-1104880). We would also like to thank the
California Air Resources Board and the California Institute of
Technology for their support of the CalNex-LA ground site. We would also
like to thank Jean Francois Doussin and Marie Camredon from LISA for
their valuable discussion. Data presented in this manuscript can be
requested by contacting the corresponding author and can also be found
at http://www.esrl.noaa.gov/csd/projects/calnex/.
NR 83
TC 4
Z9 4
U1 22
U2 33
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 APR 27
PY 2016
VL 121
IS 8
BP 4211
EP 4232
DI 10.1002/2015JD024358
PG 22
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DP2KU
UT WOS:000378318100029
ER
PT J
AU Barth, MC
Bela, MM
Fried, A
Wennberg, PO
Crounse, JD
St Clair, JM
Blake, NJ
Blake, DR
Homeyer, CR
Brune, WH
Zhang, L
Mao, J
Ren, X
Ryerson, TB
Pollack, IB
Peischl, J
Cohen, RC
Nault, BA
Huey, LG
Liu, X
Cantrell, CA
AF Barth, M. C.
Bela, M. M.
Fried, A.
Wennberg, P. O.
Crounse, J. D.
St Clair, J. M.
Blake, N. J.
Blake, D. R.
Homeyer, C. R.
Brune, W. H.
Zhang, L.
Mao, J.
Ren, X.
Ryerson, T. B.
Pollack, I. B.
Peischl, J.
Cohen, R. C.
Nault, B. A.
Huey, L. G.
Liu, X.
Cantrell, C. A.
TI Convective transport and scavenging of peroxides by thunderstorms
observed over the central US during DC3
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID VOLATILE ORGANIC-COMPOUNDS; STRATOSPHERIC-TROPOSPHERIC EXPERIMENT;
TROPICAL UPPER TROPOSPHERE; GAS-PHASE; NUMERICAL SIMULATIONS; RADAR
OBSERVATIONS; HYDROGEN-PEROXIDE; UNITED-STATES; TRACE GASES; JULY 10
AB One of the objectives of the Deep Convective Clouds and Chemistry (DC3) field experiment was to determine the scavenging of soluble trace gases by thunderstorms. We present an analysis of scavenging of hydrogen peroxide (H2O2) and methyl hydrogen peroxide (CH3OOH) from six DC3 cases that occurred in Oklahoma and northeast Colorado. Estimates of H2O2 scavenging efficiencies are comparable to previous studies ranging from 79 to 97% with relative uncertainties of 5-25%. CH3OOH scavenging efficiencies ranged from 12 to 84% with relative uncertainties of 18-558%. The wide range of CH3OOH scavenging efficiencies is surprising, as previous studies suggested that CH3OOH scavenging efficiencies would be < 10%. Cloud chemistry model simulations of one DC3 storm produced CH3OOH scavenging efficiencies of 26-61% depending on the ice retention factor of CH3OOH during cloud drop freezing, suggesting ice physics impacts CH3OOH scavenging. The highest CH3OOH scavenging efficiencies occurred in two severe thunderstorms, but there is no obvious correlation between the CH3OOH scavenging efficiency and the storm thermodynamic environment. We found a moderate correlation between the estimated entrainment rates and CH3OOH scavenging efficiencies. Changes in gas-phase chemistry due to lightning production of nitric oxide and aqueous-phase chemistry have little effect on CH3OOH scavenging efficiencies. To determine why CH3OOH can be substantially removed from storms, future studies should examine effects of entrainment rate, retention of CH3OOH in frozen cloud particles during drop freezing, and lightning-NOx production.
C1 [Barth, M. C.] Natl Ctr Atmospher Res, Atmospher Chem Observat & Modeling Lab, POB 3000, Boulder, CO 80307 USA.
[Barth, M. C.] Natl Ctr Atmospher Res, Mesoscale & Microscale Meteorol Lab, POB 3000, Boulder, CO 80307 USA.
[Bela, M. M.; Cantrell, C. A.] Univ Colorado, Dept Atmospher & Ocean Sci, Boulder, CO 80309 USA.
[Bela, M. M.] Univ Colorado, Atmospher & Space Phys Lab, Campus Box 392, Boulder, CO 80309 USA.
[Fried, A.] Univ Colorado, Inst Arctic & Alpine Res, Boulder, CO 80309 USA.
[Wennberg, P. O.; Crounse, J. D.] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA.
[St Clair, J. M.] Univ Maryland Baltimore Cty, Joint Ctr Earth Syst Technol, NASA Goddard Space Flight Ctr, Greenbelt, MD USA.
[Blake, N. J.; Blake, D. R.] Univ Calif Irvine, Dept Chem, Irvine, CA 92717 USA.
[Homeyer, C. R.] Univ Oklahoma, Sch Meteorol, Norman, OK 73019 USA.
[Brune, W. H.; Zhang, L.] Penn State Univ, Dept Meteorol, 503 Walker Bldg, University Pk, PA 16802 USA.
[Mao, J.] Princeton Univ, Program Atmospher & Ocean Sci, Princeton, NJ 08544 USA.
[Mao, J.] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA.
[Ren, X.] NOAA Air Resources Lab, College Pk, MD USA.
[Ryerson, T. B.; Peischl, J.] NOAA, Chem Sci Div, Earth Syst Res Lab, Boulder, CO USA.
[Pollack, I. B.] Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA.
[Peischl, J.; Nault, B. A.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Cohen, R. C.; Nault, B. A.] Univ Calif Berkeley, Berkeley, CA 94720 USA.
[Nault, B. A.] Univ Colorado, Dept Chem & Biochem, Campus Box 215, Boulder, CO 80309 USA.
[Huey, L. G.; Liu, X.] Georgia Inst Technol, Atlanta, GA 30332 USA.
RP Barth, MC (reprint author), Natl Ctr Atmospher Res, Atmospher Chem Observat & Modeling Lab, POB 3000, Boulder, CO 80307 USA.; Barth, MC (reprint author), Natl Ctr Atmospher Res, Mesoscale & Microscale Meteorol Lab, POB 3000, Boulder, CO 80307 USA.
EM barthm@ucar.edu
RI Peischl, Jeff/E-7454-2010; Cohen, Ronald/A-8842-2011; Ren,
Xinrong/E-7838-2015; Pollack, Ilana/F-9875-2012; Mao,
Jingqiu/F-2511-2010; Homeyer, Cameron/D-5034-2013; Crounse,
John/C-3700-2014; Manager, CSD Publications/B-2789-2015
OI Peischl, Jeff/0000-0002-9320-7101; Cohen, Ronald/0000-0001-6617-7691;
Ren, Xinrong/0000-0001-9974-1666; Mao, Jingqiu/0000-0002-4774-9751;
Homeyer, Cameron/0000-0002-4883-6670; Crounse, John/0000-0001-5443-729X;
FU National Science Foundation; NSF [AGS-1261559, AGS-1522910, DGE
1106400]; NASA [NNX12AMO8G, NNX12AC06G, NNX14AP46G-ACCDAM, NNX12AB76G,
NNX12AB84G, NNX12AB79G, NNX12AB77G]; NOAA Climate Change program by NASA
[NNH12AT30I]; NOAA Health of the Atmosphere program [NNH12AT30I]
FX The authors thank the DC3 Science and Logistics teams for the successful
execution of the DC3 field campaign. Data from the DC3 field project can
be found at http://data.eol.ucar.edu/master_list/?project=DC3. The
aircraft data are also located at
http://www-air.larc.nasa.gov/cgi-bin/ArcView/dc3-seac4rs. Output from
the model simulations can be obtained upon request to M. Barth
(barthm@ucar.edu). We appreciate Conrad Ziegler (NOAA/NSSL) and his team
as well as the NCAR/EOL ISS team for the radiosonde data. G. Diskin and
his team are acknowledged for their DC-8 water vapor and CO
measurements. We are grateful for the informative weather summaries
provided by Morris Weisman and Craig Schwartz during the DC3 field
campaign. We value the contributions of John Orlando and the comments on
the paper by Sasha Madronich, Rebecca Hornbrook and the three anonymous
reviewers. The National Center for Atmospheric Research is sponsored by
the National Science Foundation. The INSTAAR group acknowledges NSF and
NASA under grant awards AGS-1261559 and NNX12AMO8G, respectively, for
funding their participation in the measurements and analysis. The
Caltech group thanks NASA for funding their participation in DC3 and
contribution to this analysis via grants NNX12AC06G and
NNX14AP46G-ACCDAM. N. Blake and D. Blake acknowledge support for DC3
measurements from NASA award NNX12AB76G. C. Homeyer was supported by NSF
under grant AGS-1522910. W. H. Brune, L. Zhang, J. Mao, and X. Ren were
supported by NASA grant NNX12AB84G. T. B. Ryerson, J. Peischl, and I. B.
Pollack were supported under the NOAA Climate Change and NOAA Health of
the Atmosphere programs, with participation in DC3 made possible by NASA
grant NNH12AT30I. R. C. Cohen and B. A. Nault were supported by NASA
grant NNX12AB79G. B. A. Nault was also supported by the NSF Graduate
Research Fellowship under grant DGE 1106400. L. G. Huey and X. Liu were
supported by NASA grant NNX12AB77G.
NR 70
TC 3
Z9 3
U1 5
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 APR 27
PY 2016
VL 121
IS 8
BP 4272
EP 4295
DI 10.1002/2015JD024570
PG 24
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DP2KU
UT WOS:000378318100032
ER
PT J
AU Chakraborty, A
Ervens, B
Gupta, T
Tripathi, SN
AF Chakraborty, Abhishek
Ervens, Barbara
Gupta, Tarun
Tripathi, Sachchida N.
TI Characterization of organic residues of size-resolved fog droplets and
their atmospheric implications
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
ID AEROSOL MASS-SPECTROMETER; DEPENDENT CHEMICAL-COMPOSITION;
AQUEOUS-PHASE; HIGH-RESOLUTION; CLOUD DROPLETS; ORGANOSULFATE FORMATION;
VOLATILITY MEASUREMENTS; STRATOCUMULUS CLOUDS; MODEL-CALCULATIONS;
URBAN-ENVIRONMENT
AB Size-resolved fog water samples were collected in two consecutive winters at Kanpur, a heavily polluted urban area of India. Samples were analyzed by an aerosol mass spectrometer after drying and directly in other instruments. Residues of fine fog droplets (diameter: 4-16 mu m) are found to be more enriched with oxidized (oxygen to carbon ratio, O/C = 0.88) and low volatility organics than residues of coarse (diameter > 22 mu m) and medium size (diameter: 16-22 mu m) droplets with O/C of 0.68 and 0.74, respectively. These O/C ratios are much higher than those observed for background ambient organic aerosols, indicating efficient oxidation in fog water. Accompanying box model simulations reveal that longer residence times, together with high aqueous OH concentrations in fine droplets, can explain these trends. High aqueous OH concentrations in smaller droplets are caused by their highest surface-volume ratio and high Fe and Cu concentrations, allowing more uptake of gas phase OH and enhanced Fenton reaction rates, respectively. Although some volatile organic species may have escaped during droplet evaporation, these findings indicate that aqueous processing of dissolved organics varies with droplet size. Therefore, large (regional, global)-scale models need to consider the variable reaction rates, together with metal-catalyzed radical formation throughout droplet populations for accurately predicting aqueous secondary organic aerosol formation.
C1 [Chakraborty, Abhishek; Gupta, Tarun; Tripathi, Sachchida N.] Indian Inst Technol, Dept Civil Engn, Kanpur 208016, Uttar Pradesh, India.
[Ervens, Barbara] Univ Colorado, CIRES, Boulder, CO 80309 USA.
[Ervens, Barbara] NOAA, ESRL CSD, Boulder, CO USA.
[Gupta, Tarun; Tripathi, Sachchida N.] Indian Inst Technol, Ctr Environm Sci & Engn, Kanpur 208016, Uttar Pradesh, India.
RP Gupta, T; Tripathi, SN (reprint author), Indian Inst Technol, Dept Civil Engn, Kanpur 208016, Uttar Pradesh, India.; Gupta, T; Tripathi, SN (reprint author), Indian Inst Technol, Ctr Environm Sci & Engn, Kanpur 208016, Uttar Pradesh, India.
EM tarun@iitk.ac.in; snt@iitk.ac.in
RI Tripathi, Sachchida/J-4840-2016; Manager, CSD Publications/B-2789-2015;
OI Chakraborty, Abhishek/0000-0001-9531-6419
FU IIT Kanpur; Indian Ministry of Human Resource and Development
[3-21/2014-TS.1]; U.S. Agency for International Development
[AID-OAA-A-11- 00012]
FX We acknowledge the support of IIT Kanpur for providing us with an
HR-ToF-AMS for PG research and teaching. We would also like to
acknowledge support of the Indian Ministry of Human Resource and
Development (3-21/2014-TS.1) for providing us some financial assistance
to carry out this research. This research is also partially supported by
the U.S. Agency for International Development (AID-OAA-A-11- 00012). In
addition we thank Deepika Bahttu for useful discussions. All the data
and results that are used to support the conclusions of this article can
be obtained upon request from the corresponding authors by sending
emails to tarun@iitk.ac.in and/or snt@iitk.ac.in. This article contains
supporting information of 11 pages (S1-S11) with seven figures (Figures
S1-S7) and three tables (Tables S1-S3).
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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 APR 27
PY 2016
VL 121
IS 8
BP 4317
EP 4332
DI 10.1002/2015JD024508
PG 16
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DP2KU
UT WOS:000378318100034
ER
PT J
AU Somera, TM
Bailey, B
Barott, K
Grasis, J
Hatay, M
Hilton, BJ
Hisakawa, N
Nosrat, B
Nulton, J
Silveira, CB
Sullivan, C
Brainard, RE
Rohwer, F
AF Somera, Tracey McDole
Bailey, Barbara
Barott, Katie
Grasis, Juris
Hatay, Mark
Hilton, Brett J.
Hisakawa, Nao
Nosrat, Bahador
Nulton, James
Silveira, Cynthia B.
Sullivan, Chris
Brainard, Russell E.
Rohwer, Forest
TI Energetic differences between bacterioplankton trophic groups and coral
reef resistance
SO PROCEEDINGS OF THE ROYAL SOCIETY B-BIOLOGICAL SCIENCES
LA English
DT Article
DE microbialization; coral reef; resistance; metabolic theory; disease
dissolved organic carbon algae and microbe
ID ORGANIC-MATTER RELEASE; NORTHERN LINE ISLANDS; MICROBIAL ECOLOGY;
METABOLIC BALANCE; MARINE VIRUSES; CELL-CYCLE; FOOD WEBS; RED-SEA;
ECOSYSTEMS; PHOTOSYNTHESIS
AB Coral reefs are among the most productive and diverse marine ecosystems on the Earth. They are also particularly sensitive to changing energetic requirements by different trophic levels. Microbialization specifically refers to the increase in the energetic metabolic demands of microbes relative to macrobes and is significantly correlated with increasing human influence on coral reefs. In this study, metabolic theory of ecology is used to quantify the relative contributions of two broad bacterioplankton groups, autotrophs and heterotrophs, to energy flux on 27 Pacific coral reef ecosystems experiencing human impact to varying degrees. The effective activation energy required for photosynthesis is lower than the average energy of activation for the biochemical reactions of the Krebs cycle, and changes in the proportional abundance of these two groups can greatly affect rates of energy and materials cycling. We show that reef-water communities with a higher proportional abundance of microbial autotrophs expend more metabolic energy per gram of microbial biomass. Increased energy and materials flux through fast energy channels (i.e. water-column associated microbial autotrophs) may dampen the detrimental effects of increased heterotrophic loads (e.g. coral disease) on coral reef systems experiencing anthropogenic disturbance.
C1 [Somera, Tracey McDole; Barott, Katie; Grasis, Juris; Hatay, Mark; Hilton, Brett J.; Hisakawa, Nao; Nosrat, Bahador; Silveira, Cynthia B.; Rohwer, Forest] San Diego State Univ, Dept Biol, 5500 Campanile Dr, San Diego, CA 92182 USA.
[Bailey, Barbara; Nulton, James] San Diego State Univ, Dept Math & Stat, 5500 Campanile Dr, San Diego, CA 92182 USA.
[Brainard, Russell E.] NOAA Fisheries, Pacific Islands Fisheries Sci Ctr, 1125 B Ala Moana Blvd, Honolulu, HI 96814 USA.
[Sullivan, Chris] Univ Calif San Diego, Scripps Inst Oceanog, 9500 Gillman Dr, La Jolla, CA 92093 USA.
RP Somera, TM (reprint author), San Diego State Univ, Dept Biol, 5500 Campanile Dr, San Diego, CA 92182 USA.
EM tsmcdole@yahoo.com
OI Grasis, Juris/0000-0002-3945-0135
FU NSF [OCE-0927415]; CIFAR [LTRDTD62207]; NOAA's Coral Reef Ecosystem
Division and Pacific Reef Assessment and Monitoring Program
FX This work was supported by NSF (OCE-0927415) and a grant from CIFAR
(LTRDTD62207). NOAA's Coral Reef Ecosystem Division and Pacific Reef
Assessment and Monitoring Program also supported this work.
NR 75
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U2 13
PU ROYAL SOC
PI LONDON
PA 6-9 CARLTON HOUSE TERRACE, LONDON SW1Y 5AG, ENGLAND
SN 0962-8452
EI 1471-2954
J9 P ROY SOC B-BIOL SCI
JI Proc. R. Soc. B-Biol. Sci.
PD APR 27
PY 2016
VL 283
IS 1829
AR 20160467
DI 10.1098/rspb.2016.0467
PG 9
WC Biology; Ecology; Evolutionary Biology
SC Life Sciences & Biomedicine - Other Topics; Environmental Sciences &
Ecology; Evolutionary Biology
GA DM2EE
UT WOS:000376158600020
ER
PT J
AU Roseland, JM
Patterson, KY
Andrews, KW
Phillips, KM
Phillips, MM
Pehrsson, PR
Dufresne, GL
Jakobsen, J
Gusev, PA
Savarala, S
Nguyen, QV
Makowski, AJ
Scheuerell, CR
Larouche, GP
Wise, SA
Harnly, JM
Williams, JR
Betz, JM
Taylor, CL
AF Roseland, Janet Maxwell
Patterson, Kristine Y.
Andrews, Karen W.
Phillips, Katherine M.
Phillips, Melissa M.
Pehrsson, Pamela R.
Dufresne, Guy L.
Jakobsen, Jette
Gusev, Pavel A.
Savarala, Sushma
Nguyen, Quynhanh V.
Makowski, Andrew J.
Scheuerell, Chad R.
Larouche, Guillaume P.
Wise, Stephen A.
Harnly, James M.
Williams, Juhi R.
Betz, Joseph M.
Taylor, Christine L.
TI Interlaboratory Trial for Measurement of Vitamin D and 25-Hydroxyvitamin
D [25(OH)D] in Foods and a Dietary Supplement Using Liquid
Chromatography-Mass Spectrometry
SO JOURNAL OF AGRICULTURAL AND FOOD CHEMISTRY
LA English
DT Article
DE reference material; food; dietary supplement; vitamin D-3
(cholecalciferol); 25-hydroxyvitamin D-3 (25-hydroxycholcalciferol)
ID NUTRIENT ANALYSIS PROGRAM; CARDIOVASCULAR-DISEASE; BIOLOGICAL-ACTIVITY;
NATIONAL FOOD; D-3; SERUM; EGGS; MEAT; HEALTH; FISH
AB Assessment of total vitamin D intake from foods and dietary supplements (DSs) may be incomplete if 25-hydroxyvitamin D [25(OH)D] intake is not included. However, 25(OH)D data for such intake assessments are lacking, no food or DS reference materials (RMs) are available, and comparison of laboratory performance has been needed. The primary goal of this study was to evaluate whether vitamin D-3 and 25(OH)D-3 concentrations in food and DS materials could be measured with acceptable reproducibility. Five experienced laboratories from the United States and other countries participated, all using liquid chromatography tandem mass spectrometry but no common analytical protocol; however, various methods were used for determining vitamin D-3 in the DS. Five animal-based materials (including three commercially available RMs) and one DS were analyzed. Reproducibility results for the materials were acceptable. Thus, it is possible to obtain consistent results among experienced laboratories for vitamin D-3 and 25(OH)D-3, in foods and a DS.
C1 [Roseland, Janet Maxwell; Patterson, Kristine Y.; Andrews, Karen W.; Pehrsson, Pamela R.; Gusev, Pavel A.; Savarala, Sushma; Nguyen, Quynhanh V.; Williams, Juhi R.] USDA ARS, Nutrient Data Lab, BARC West, 10300 Baltimore Ave,Bldg 005, Beltsville, MD 20705 USA.
[Phillips, Katherine M.] Virginia Tech, Biochem Dept 0308, 304 Engel Hall, Blacksburg, VA 24061 USA.
[Phillips, Melissa M.; Wise, Stephen A.] NIST, Div Chem Sci, MS 8392,100 Bur Dr, Gaithersburg, MD 20899 USA.
[Dufresne, Guy L.] Hlth Canada, Food & Nutr Lab, 1001 St Laurent Ouest, Longueuil, PQ J4K 1C7, Canada.
[Jakobsen, Jette] Tech Univ Denmark, Natl Food Inst, Div Food Chem, Soborg, Denmark.
[Makowski, Andrew J.] Heartland Assays LLC, Suite 4400,2711 South Loop Dr, Ames, IA 50010 USA.
[Scheuerell, Chad R.] Covance Labs, 3301 Kinsman Blvd, Madison, WI 53704 USA.
[Betz, Joseph M.; Taylor, Christine L.] NIH, Off Dietary Supplements, 3B01,MSC 7517,6100 Execut Blvd, Bethesda, MD 20892 USA.
[Harnly, James M.] USDA ARS, Food Composit & Method Dev Lab, BARC East, Bldg 161,10300 Baltimore Ave, Beltsville, MD 20705 USA.
RP Roseland, JM (reprint author), USDA ARS, Nutrient Data Lab, BARC West, 10300 Baltimore Ave,Bldg 005, Beltsville, MD 20705 USA.
EM janet.roseland@ars.usda.gov
FU Office of Dietary Supplements of the National Institutes of Health [60
1235 3012]
FX Partial funding for this work was provided under Agreement 60 1235 3012
from Office of Dietary Supplements of the National Institutes of Health.
NR 47
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U1 5
U2 11
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0021-8561
EI 1520-5118
J9 J AGR FOOD CHEM
JI J. Agric. Food Chem.
PD APR 27
PY 2016
VL 64
IS 16
BP 3167
EP 3175
DI 10.1021/acs.jafc.5b05016
PG 9
WC Agriculture, Multidisciplinary; Chemistry, Applied; Food Science &
Technology
SC Agriculture; Chemistry; Food Science & Technology
GA DK9IO
UT WOS:000375244300008
PM 27045951
ER
PT J
AU Ayres, CM
Scott, DR
Corcelli, SA
Baker, BM
AF Ayres, Cory M.
Scott, Daniel R.
Corcelli, Steven A.
Baker, Brian M.
TI Differential utilization of binding loop flexibility in T cell receptor
ligand selection and cross-reactivity
SO SCIENTIFIC REPORTS
LA English
DT Article
ID MHC CLASS-II; MAJOR HISTOCOMPATIBILITY COMPLEX; MOLECULAR-DYNAMICS
SIMULATIONS; PEPTIDE-MHC; CONFORMATIONAL PLASTICITY; IMMUNE RECOGNITION;
PROTEIN STRUCTURES; SELF-PEPTIDE; ALPHA-BETA; SPECIFICITY
AB Complementarity determining region (CDR) loop flexibility has been suggested to play an important role in the selection and binding of ligands by T cell receptors (TCRs) of the cellular immune system. However, questions remain regarding the role of loop motion in TCR binding, and crystallographic structures have raised questions about the extent to which generalizations can be made. Here we studied the flexibility of two structurally well characterized alpha beta TCRs, A6 and DMF5. We found that the two receptors utilize loop motion very differently in ligand binding and cross-reactivity. While the loops of A6 move rapidly in an uncorrelated fashion, those of DMF5 are substantially less mobile. Accordingly, the mechanisms of binding and cross-reactivity are very different between the two TCRs: whereas A6 relies on conformational selection to select and bind different ligands, DMF5 uses a more rigid, permissive architecture with greater reliance on slower motions or induced-fit. In addition to binding site flexibility, we also explored whether ligand-binding resulted in common dynamical changes in A6 and DMF5 that could contribute to TCR triggering. Although binding-linked motional changes propagated throughout both receptors, no common features were observed, suggesting that changes in nanosecond-level TCR structural dynamics do not contribute to T cell signaling.
C1 [Ayres, Cory M.; Scott, Daniel R.; Corcelli, Steven A.; Baker, Brian M.] Univ Notre Dame, Dept Chem & Biochem, Notre Dame, IN 46556 USA.
[Ayres, Cory M.; Baker, Brian M.] Univ Notre Dame, Harper Canc Res Inst, Notre Dame, IN 46556 USA.
[Scott, Daniel R.] NIST, Neutron Condensed Matter Grp, Gaithersburg, MD 20899 USA.
RP Baker, BM (reprint author), Univ Notre Dame, Dept Chem & Biochem, Notre Dame, IN 46556 USA.; Baker, BM (reprint author), Univ Notre Dame, Harper Canc Res Inst, Notre Dame, IN 46556 USA.
EM brian-baker@nd.edu
FU NIGMS, NIH [GM067079, GM103773]; Carole and Ray Neag Comprehensive
Cancer Center
FX We thank Paul Brenner and the staff of the Notre Dame Center for
Research Computing for assistance. Supported by grants GM067079 and
GM103773 from NIGMS, NIH and a grant from the Carole and Ray Neag
Comprehensive Cancer Center.
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U1 7
U2 17
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 2045-2322
J9 SCI REP-UK
JI Sci Rep
PD APR 27
PY 2016
VL 6
AR 25070
DI 10.1038/srep25070
PG 14
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DK3ZD
UT WOS:000374855000001
PM 27118724
ER
PT J
AU Lam, S
Zheng, M
Fagan, JA
AF Lam, Stephanie
Zheng, Ming
Fagan, Jeffrey A.
TI Characterizing the Effect of Salt and Surfactant Concentration on the
Counterion Atmosphere around Surfactant Stabilized SWCNTs Using
Analytical Ultracentrifugation
SO LANGMUIR
LA English
DT Article
ID WALLED CARBON NANOTUBES; MOLECULAR-DYNAMICS SIMULATION; SODIUM
DEOXYCHOLATE; SIZE-DISTRIBUTION; DENSITY; LENGTH; NANOPARTICLES;
SEDIMENTATION; SEPARATION; PARTITION
AB Accurate characterization of dispersed-phase nano particle properties such as density, size, solvation, and charge is necessary for their utilization in applications such as medicine, energy, and materials. Herein, analytical ultracentrifugation (AUC) is used to quantify bile salt surfactant adsorption on length sorted (7,6) single-wall carbon nanotubes (SWCNTs) as a function of bulk surfactant concentration and in the presence of varying quantities of a monovalent salt sodium chloride. These measurements provide high precision adsorbed surfactant density values in the literature for only the second SWCNT structure to date and report the quantity of adsorbed surfactant across a broad range of bulk surfactant concentrations utilized in SWCNT dispersion processing. Second, the measurements presented herein unambiguously demonstrate, via AUC, a direct relation between the size of the counterion cloud around a surfactant-stabilized SWCNT and solution ionic strength. The results show that changes in the size of the counterion cloud around surfactant-stabilized SWCNT are attributable to electrostatic phenomenon and not to changes in the quantity of adsorbed surfactant with salt addition. These results provide important reference values for projecting SWCNT dispersion behavior as a function of solution conditions and extend the range of nanoparticle properties measurable via AUC.
C1 [Lam, Stephanie; Zheng, Ming; Fagan, Jeffrey A.] Natl Inst Stand & Technol, Mat Sci & Engn Div, Gaithersburg, MD 20899 USA.
RP Fagan, JA (reprint author), Natl Inst Stand & Technol, Mat Sci & Engn Div, Gaithersburg, MD 20899 USA.
EM jfagan@nist.gov
OI Fagan, Jeffrey/0000-0003-1483-5554
FU National Research Council; NSF XSEDE Grant [MCB070038]; NSF
[OCI-1053575]
FX S.L. acknowledges the National Research Council for her postdoctoral
fellowship. The authors also acknowledge the computing time which was
utilized for AUC data analysis performed in UltraScan. Calculations were
performed on the UltraScan LIMS cluster at the Bioinformatics Core
Facility at the University of Texas Health Science Center in San Antonio
and XSEDE resources supported by NSF XSEDE Grant #MCB070038 (to Borries
Demeler). The Gateway is made possible by the use of XSEDE resources and
the Extended Collaborative Support Service (ECSS) Program funded by the
NSF through Award OCI-1053575.
NR 47
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U1 10
U2 20
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0743-7463
J9 LANGMUIR
JI Langmuir
PD APR 26
PY 2016
VL 32
IS 16
BP 3926
EP 3936
DI 10.1021/acs.langmuir.6b00605
PG 11
WC Chemistry, Multidisciplinary; Chemistry, Physical; Materials Science,
Multidisciplinary
SC Chemistry; Materials Science
GA DK9IE
UT WOS:000375243300014
PM 27031248
ER
PT J
AU Mineart, KP
Lee, B
Spontak, RJ
AF Mineart, Kenneth P.
Lee, Byeongdu
Spontak, Richard J.
TI A Solvent-Vapor Approach toward the Control of Block lonomer
Morphologies
SO MACROMOLECULES
LA English
DT Article
ID ABC TRIBLOCK COPOLYMERS; DILUTION APPROXIMATION; SULFONATED POLYSTYRENE;
PENTABLOCK COPOLYMERS; MEMBRANE APPLICATIONS; TRANSPORT-PROPERTIES;
PHYSICAL-PROPERTIES; PHASE-BEHAVIOR; LINEAR ABCBA; THIN-FILMS
AB Sulfonated block ionomers possess advantageous properties for a wide range of diverse applications such as desalination membranes, fuel cells, electroactive media, and photovoltaic devices. Unfortunately, their inherently high incompatibilities and glass transition temperatures effectively prevent the use of thermal annealing, routinely employed to refine the morphologies of nonionic block copolymers. An alternative approach is therefore required to promote morphological equilibration in block ionomers. The present study explores the morphological characteristics of midblock-sulfonated pentablock ionomers (SBIs) differing in their degree of sulfonation (DOS) and cast from solution followed by solvent-vapor annealing (SVA). Transmission electron microscopy confirms that films deposited from different solvent systems form nonequilibrium morphologies due to solvent-regulated self-assembly and drying. A series of SVA tests performed with solvents varying in polarity reveals that exposing cast films to tetrahydrofuran (THF) vapor for at least 2 h constitutes the most effective SVA protocol, yielding the anticipated equilibrium morphology. That is, three SBI grades subjected to THF-SVA self-assemble into well-ordered lamellae wherein the increase in DOS is accompanied by an increase in lamellar periodicity, as measured by small-angle X-ray scattering.
C1 [Mineart, Kenneth P.; Spontak, Richard J.] N Carolina State Univ, Dept Chem & Biomol Engn, Raleigh, NC 27695 USA.
[Spontak, Richard J.] N Carolina State Univ, Dept Mat Sci & Engn, Raleigh, NC 27695 USA.
[Lee, Byeongdu] Argonne Natl Lab, Adv Photon Source, Argonne, IL 60439 USA.
[Mineart, Kenneth P.] Natl Inst Stand & Technol, Mat Sci & Engn Div, Gaithersburg, MD 20899 USA.
RP Spontak, RJ (reprint author), N Carolina State Univ, Dept Chem & Biomol Engn, Raleigh, NC 27695 USA.; Spontak, RJ (reprint author), N Carolina State Univ, Dept Mat Sci & Engn, Raleigh, NC 27695 USA.
EM Rich_Spontak@ncsu.edu
OI Mineart, Kenneth/0000-0003-2374-4670
FU Nonwovens Institute at North Carolina State University; MANN+HUMMEL
GmbH; DOE Office of Science by Argonne National Laboratory
[DE-AC02-06CH11357]
FX This work was supported by the Nonwovens Institute at North Carolina
State University and MANN+HUMMEL GmbH. In addition, this research used
resources of the Advanced Photon Source, a U.S. Department of Energy
(DOE) Office of Science User Facility operated for the DOE Office of
Science by Argonne National Laboratory under Contract DE-AC02-06CH11357.
NR 63
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U2 25
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0024-9297
EI 1520-5835
J9 MACROMOLECULES
JI Macromolecules
PD APR 26
PY 2016
VL 49
IS 8
BP 3126
EP 3137
DI 10.1021/acs.macromol.6b00134
PG 12
WC Polymer Science
SC Polymer Science
GA DK9IR
UT WOS:000375244600025
ER
PT J
AU Torrisi, SB
Britton, JW
Bohnet, JG
Bollinger, JJ
AF Torrisi, Steven B.
Britton, Joseph W.
Bohnet, Justin G.
Bollinger, John J.
TI Perpendicular laser cooling with a rotating-wall potential in a Penning
trap
SO PHYSICAL REVIEW A
LA English
DT Article
ID NONNEUTRAL PLASMAS; ION PLASMAS; CRYSTALS
AB We investigate the impact of a rotating-wall potential on perpendicular laser cooling in a Penning ion trap. By including energy exchange with the rotating wall, we extend previous Doppler laser-cooling theory and show that low perpendicular temperatures are more readily achieved with a rotating wall than without. Detailed numerical studies determine optimal operating parameters for producing low-temperature, stable two-dimensional crystals, important for quantum information processing experiments employing Penning traps.
C1 [Torrisi, Steven B.; Britton, Joseph W.; Bohnet, Justin G.; Bollinger, John J.] NIST, Boulder, CO 80305 USA.
[Torrisi, Steven B.] Univ Rochester, Dept Phys & Astron, Rochester, NY 14627 USA.
[Britton, Joseph W.] US Army Res Lab, Adelphi, MD 20783 USA.
RP Torrisi, SB (reprint author), NIST, Boulder, CO 80305 USA.; Torrisi, SB (reprint author), Univ Rochester, Dept Phys & Astron, Rochester, NY 14627 USA.
FU Summer Undergraduate Research Fellowship through NIST; NIST NRC
postdoctoral fellowship
FX We acknowledge useful discussions with D. H. E. Dubin, R. C. Thompson,
A. Keith, and D. Meiser. We thank K. Gilmore and R. Fox for their
comments on the manuscript. S.B.T. was supported by Summer Undergraduate
Research Fellowship funding through NIST. J.G.B. was supported by a NIST
NRC postdoctoral fellowship. This manuscript is a contribution of NIST
and not subject to U.S. copyright.
NR 25
TC 1
Z9 1
U1 4
U2 4
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 2469-9926
EI 2469-9934
J9 PHYS REV A
JI Phys. Rev. A
PD APR 26
PY 2016
VL 93
IS 4
AR 043421
DI 10.1103/PhysRevA.93.043421
PG 8
WC Optics; Physics, Atomic, Molecular & Chemical
SC Optics; Physics
GA DK4ZJ
UT WOS:000374928600012
ER
PT J
AU Bowden, JA
Cantu, TM
Chapman, RW
Somerville, SE
Guillette, MP
Botha, H
Hoffman, A
Luus-Powell, WJ
Smit, WJ
Lebepe, J
Myburgh, J
Govender, D
Tucker, J
Boggs, ASP
Guillette, LJ
AF Bowden, John A.
Cantu, Theresa M.
Chapman, Robert W.
Somerville, Stephen E.
Guillette, Matthew P.
Botha, Hannes
Hoffman, Andre
Luus-Powell, Wilmien J.
Smit, Willem J.
Lebepe, Jeffrey
Myburgh, Jan
Govender, Danny
Tucker, Jonathan
Boggs, Ashley S. P.
Guillette, Louis J., Jr.
TI Predictive Blood Chemistry Parameters for Pansteatitis-Affected
Mozambique Tilapia (Oreochromis mossambicus)
SO PLOS ONE
LA English
DT Article
ID KRUGER-NATIONAL-PARK; CROCODILE CROCODYLUS-NILOTICUS; CLARIAS-GARIEPINUS
BURCHELL; TURTLES CARETTA-CARETTA; SOUTH-AFRICA; OLIFANTS RIVER; NILE
CROCODILE; SHARPTOOTH CATFISH; CLINICAL-CHEMISTRY; OXIDATIVE STRESS
AB One of the largest river systems in South Africa, the Olifants River, has experienced significant changes in water quality due to anthropogenic activities. Since 2005, there have been various "outbreaks" of the inflammatory disease pansteatitis in several vertebrate species. Large-scale pansteatitis-related mortality events have decimated the crocodile population at Lake Loskop and decreased the population at Kruger National Park. Most pansteatitis-related diagnoses within the region are conducted post-mortem by either gross pathology or histology. The application of a non-lethal approach to assess the prevalence and pervasiveness of pansteatitis in the Olifants River region would be of great importance for the development of a management plan for this disease. In this study, several plasma-based biomarkers accurately classified pansteatitis in Mozambique tilapia (Oreochromis mossambicus) collected from Lake Loskop using a commercially available benchtop blood chemistry analyzer combined with data interpretation via artificial neural network analysis. According to the model, four blood chemistry parameters (calcium, sodium, total protein and albumin), in combination with total length, diagnose pansteatitis to a predictive accuracy of 92 percent. In addition, several morphometric traits (total length, age, weight) were also associated with pansteatitis. On-going research will focus on further evaluating the use of blood chemistry to classify pansteatitis across different species, trophic levels, and within different sites along the Olifants River.
C1 [Bowden, John A.; Boggs, Ashley S. P.] NIST, Mat Measurement Lab, Div Chem Sci, Environm Chem Sci Grp,Hollings Marine Lab, Charleston, SC USA.
[Cantu, Theresa M.; Somerville, Stephen E.; Guillette, Matthew P.; Guillette, Louis J., Jr.] Med Univ S Carolina, Dept Obstet & Gynecol, Charleston, SC 29425 USA.
[Chapman, Robert W.; Tucker, Jonathan] South Carolina Dept Nat Resources, Marine Resources Res Inst, Hollings Marine Lab, Charleston, SC USA.
[Botha, Hannes; Hoffman, Andre] Mpumalanga Tourism & Pk Agcy, Sci Serv, Nelspruit, South Africa.
[Botha, Hannes; Luus-Powell, Wilmien J.; Smit, Willem J.; Lebepe, Jeffrey] Univ Limpopo, Dept Biodivers, Sovenga, South Africa.
[Myburgh, Jan; Govender, Danny; Guillette, Louis J., Jr.] Univ Pretoria, Fac Vet Sci, Dept Paraclin Sci, ZA-0110 Onderstepoort, South Africa.
[Govender, Danny] South African Natl Pk, Sci Serv, Skukuza, South Africa.
RP Bowden, JA (reprint author), NIST, Mat Measurement Lab, Div Chem Sci, Environm Chem Sci Grp,Hollings Marine Lab, Charleston, SC USA.
EM john.bowden@nist.gov
FU CoEE Center for Marine Genomics; MUSC Center for Global Health; Heinz
Foundation: Environmental Health and Sentinel Species; Biodiversity
Research Chair, University of Limpopo
FX This work was partially funded in part by the CoEE Center for Marine
Genomics (LJG), MUSC Center for Global Health, Heinz Foundation:
Environmental Health and Sentinel Species (2011, LJG), and the
Biodiversity Research Chair, University of Limpopo (WJLP). The funders
had no role in study design, data collection and analysis, decision to
publish, or preparation of the manuscript.
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PU PUBLIC LIBRARY SCIENCE
PI SAN FRANCISCO
PA 1160 BATTERY STREET, STE 100, SAN FRANCISCO, CA 94111 USA
SN 1932-6203
J9 PLOS ONE
JI PLoS One
PD APR 26
PY 2016
VL 11
IS 4
AR e0153874
DI 10.1371/journal.pone.0153874
PG 19
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DK5QB
UT WOS:000374973600032
PM 27115488
ER
PT J
AU Herzing, AA
Guler, U
Zhou, XL
Boltasseva, A
Shalaev, V
Norris, TB
AF Herzing, Andrew A.
Guler, Urcan
Zhou, Xiuli
Boltasseva, Alexandra
Shalaev, Vladimir
Norris, Theodore B.
TI Electron energy loss spectroscopy of plasmon resonances in titanium
nitride thin films
SO APPLIED PHYSICS LETTERS
LA English
DT Article
ID SILVER; SURFACE; GOLD
AB The plasmon resonance characteristics of refractory TiN thin films were analyzed using electron energy-loss spectroscopy (EELS). A bulk plasmon resonance was observed at 2.81 eV and a weaker surface plasmon resonance peak was detected at 2.05 eV. These findings are compared to finite-difference time-domain simulations based on measured optical data. The calculated values for both the bulk and surface resonances (2.74 eV and 2.15 eV, respectively) show reasonable agreement with those measured via EELS. The amplitude of the experimentally observed surface resonance was weaker than that typically encountered in noble metal nanostructures, and this is discussed in the context of electron density and reduced spatial confinement of the resonance mode in the thin-film geometry. Published by AIP Publishing.
C1 [Herzing, Andrew A.] Natl Inst Stand & Technol, Mat Measurement Lab, Gaithersburg, MD 20899 USA.
[Guler, Urcan; Boltasseva, Alexandra; Shalaev, Vladimir] Purdue Univ, Sch Elect & Comp Engn, W Lafayette, IN 47907 USA.
[Guler, Urcan; Boltasseva, Alexandra; Shalaev, Vladimir] Purdue Univ, Birck Nanotechnol Ctr, W Lafayette, IN 47907 USA.
[Guler, Urcan] Nanometa Technol Inc, 1281 Win Hentschel Blvd, W Lafayette, IN 47906 USA.
[Zhou, Xiuli; Norris, Theodore B.] Univ Michigan, Ctr Ultrafast Opt Sci, Ann Arbor, MI 48109 USA.
RP Herzing, AA (reprint author), Natl Inst Stand & Technol, Mat Measurement Lab, Gaithersburg, MD 20899 USA.
EM andrew.herzing@nist.gov
OI Zhou, Xiuli/0000-0002-0993-6767; Guler, Urcan/0000-0002-8807-6274
FU NSF MRSEC [DMR-1120923]
FX The authors acknowledge generous support from NSF MRSEC Grant No.
DMR-1120923.
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U1 18
U2 44
PU AMER INST PHYSICS
PI MELVILLE
PA 1305 WALT WHITMAN RD, STE 300, MELVILLE, NY 11747-4501 USA
SN 0003-6951
EI 1077-3118
J9 APPL PHYS LETT
JI Appl. Phys. Lett.
PD APR 25
PY 2016
VL 108
IS 17
AR 171107
DI 10.1063/1.4947442
PG 4
WC Physics, Applied
SC Physics
GA DL7UW
UT WOS:000375846600007
ER
PT J
AU Simons, MT
Gordon, JA
Holloway, CL
Anderson, DA
Miller, SA
Raithel, G
AF Simons, Matt T.
Gordon, Joshua A.
Holloway, Christopher L.
Anderson, David A.
Miller, Stephanie A.
Raithel, Georg
TI Using frequency detuning to improve the sensitivity of electric field
measurements via electromagnetically induced transparency and
Autler-Townes splitting in Rydberg atoms
SO APPLIED PHYSICS LETTERS
LA English
DT Article
AB In this work, we demonstrate an approach for improved sensitivity in weak radio frequency (RF) electric-field strength measurements using Rydberg electromagnetically induced transparency (EIT) in an atomic vapor. This is accomplished by varying the RF frequency around a resonant atomic transition and extrapolating the weak on-resonant field strength from the resulting off-resonant Autler-Townes (AT) splittings. This measurement remains directly traceable to SI compared to previous techniques, precluding any knowledge of experimental parameters such as optical beam powers as is the case when using the curvature of the EIT line shape to measure weak fields. We use this approach to measure weak RF fields at 182 GHz and 208 GHz demonstrating improvement greater than a factor of 2 in the measurement sensitivity compared to on-resonant AT splitting RF electric field measurements.
C1 [Simons, Matt T.; Gordon, Joshua A.; Holloway, Christopher L.] NIST, Boulder, CO 80305 USA.
[Anderson, David A.; Miller, Stephanie A.; Raithel, Georg] Univ Michigan, Dept Phys, Ann Arbor, MI 48109 USA.
[Anderson, David A.] Rydberg Technol, Ann Arbor, MI 48104 USA.
RP Holloway, CL (reprint author), NIST, Boulder, CO 80305 USA.
EM holloway@boulder.nist.gov
OI Miller, Stephanie/0000-0001-7944-3979; SIMONS,
MATTHEW/0000-0001-9418-7520
FU Defense Advanced Research Projects Agency (DARPA) under QuASAR Program;
NIST through Embedded Standards program
FX This work was partially supported by the Defense Advanced Research
Projects Agency (DARPA) under the QuASAR Program and by NIST through the
Embedded Standards program.
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U1 5
U2 13
PU AMER INST PHYSICS
PI MELVILLE
PA 1305 WALT WHITMAN RD, STE 300, MELVILLE, NY 11747-4501 USA
SN 0003-6951
EI 1077-3118
J9 APPL PHYS LETT
JI Appl. Phys. Lett.
PD APR 25
PY 2016
VL 108
IS 17
AR 174101
DI 10.1063/1.4947231
PG 5
WC Physics, Applied
SC Physics
GA DL7UW
UT WOS:000375846600053
ER
PT J
AU Farmer, B
Bhat, VS
Balk, A
Teipel, E
Smith, N
Unguris, J
Keavney, DJ
Hastings, JT
De Long, LE
AF Farmer, B.
Bhat, V. S.
Balk, A.
Teipel, E.
Smith, N.
Unguris, J.
Keavney, D. J.
Hastings, J. T.
De Long, L. E.
TI Direct imaging of coexisting ordered and frustrated sublattices in
artificial ferromagnetic quasicrystals
SO PHYSICAL REVIEW B
LA English
DT Article
ID SPIN ICE; FILMS
AB We have used scanning electron microscopy with polarization analysis and photoemission electron microscopy to image the two-dimensional magnetization of permalloy films patterned into Penrose P2 tilings (P2T). The interplay of exchange interactions in asymmetrically coordinated vertices and short-range dipole interactions among connected film segments stabilize magnetically ordered, spatially distinct sublattices that coexist with frustrated sublattices at room temperature. Numerical simulations that include long-range dipole interactions between sublattices agree with images of as-grown P2T samples and predict a magnetically ordered ground state for a two-dimensional quasicrystal lattice of classical Ising spins.
C1 [Farmer, B.; Bhat, V. S.; Teipel, E.; Smith, N.; De Long, L. E.] Univ Kentucky, Dept Phys & Astron, 505 Rose St, Lexington, KY 40506 USA.
[Balk, A.; Unguris, J.] NIST, Ctr Nanoscale Sci & Technol, 100 Bur Dr, Gaithersburg, MD 20899 USA.
[Balk, A.] Univ Maryland, Maryland Nanoctr, College Pk, MD 20742 USA.
[Keavney, D. J.] Argonne Natl Lab, Adv Photon Source 431 E007, 9700 S Cass Ave, Argonne, IL 60439 USA.
[Hastings, J. T.] Univ Kentucky, Dept Elect & Comp Engn, 453F Paul Anderson Tower, Lexington, KY 40506 USA.
RP De Long, LE (reprint author), Univ Kentucky, Dept Phys & Astron, 505 Rose St, Lexington, KY 40506 USA.
EM delong@pa.uky.edu
FU U.S. DoE [DE-FG02-97ER45653]; U.S. NSF [DMR-1506979]; UK Center for
Advanced Materials; UK Center for Computational Sciences; UK Center for
Nanoscale Science and Engineering; University of Maryland
[70NANB10H193]; National Institute of Standards and Technology Center
for Nanoscale Science and Technology through the University of Maryland
[70NANB10H193]; Research at the Advanced Photon Source, a U.S.
Department of Energy Office of Science User Facility [DE-AC02-06CH11357]
FX Research at University of Kentucky was supported by U.S. DoE Grant
DE-FG02-97ER45653, U.S. NSF Grant DMR-1506979, the UK Center for
Advanced Materials, the UK Center for Computational Sciences, and the UK
Center for Nanoscale Science and Engineering. AB acknowledges support of
this research under the Cooperative Research Agreement between the
University of Maryland and National Institute of Standards and
Technology Center for Nanoscale Science and Technology, Award
70NANB10H193, through the University of Maryland. Research at the
Advanced Photon Source, a U.S. Department of Energy Office of Science
User Facility operated by Argonne National Laboratory, was supported
under Contract No. DE-AC02-06CH11357. J. P. Straley, K. Ross, and F. Guo
contributed helpful criticism.
NR 45
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PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 2469-9950
EI 2469-9969
J9 PHYS REV B
JI Phys. Rev. B
PD APR 25
PY 2016
VL 93
IS 13
AR 134428
DI 10.1103/PhysRevB.93.134428
PG 11
WC Physics, Condensed Matter
SC Physics
GA DK5DA
UT WOS:000374938700005
ER
PT J
AU Gunasekera, J
Harriger, L
Dahal, A
Maurya, A
Heitmann, T
Disseler, SM
Thamizhavel, A
Dhar, S
Singh, DJ
Singh, DK
AF Gunasekera, J.
Harriger, L.
Dahal, A.
Maurya, A.
Heitmann, T.
Disseler, S. M.
Thamizhavel, A.
Dhar, S.
Singh, D. J.
Singh, D. K.
TI Electronic nature of the lock-in magnetic transition in CeXAl4Si2
SO PHYSICAL REVIEW B
LA English
DT Article
ID HEAVY-FERMION METALS; PHASE-TRANSITIONS; ANTIFERROMAGNETISM
AB We have investigated the underlying magnetism in newly discovered single crystal Kondo lattices CeXAl4Si2, where X = Rh, Ir. We show that the compound undergoes an incommensurate-to-commensurate magnetic transition at T-c = 9.19 K (10.75 K in Ir). The spin correlation in the incommensurate phase is described by a spin density wave configuration of Ce ions, which locks in to the long-range antiferromagnetic order at T = T-c. The analysis of the experimental data, combined with the calculation of the electronic properties, suggests the role of the Fermi surface nesting as the primary mechanism behind this phenomenon.
C1 [Gunasekera, J.; Dahal, A.; Singh, D. J.; Singh, D. K.] Univ Missouri, Dept Phys & Astron, Columbia, MO 65211 USA.
[Harriger, L.; Disseler, S. M.] NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Maurya, A.; Thamizhavel, A.; Dhar, S.] Tata Inst Fundamental Res, Mumbia, India.
[Heitmann, T.] Univ Missouri, Res Reactor, Columbia, MO 65211 USA.
RP Singh, DK (reprint author), Univ Missouri, Dept Phys & Astron, Columbia, MO 65211 USA.
EM singhdk@missouri.edu
FU Department of Commerce facility NIST Center for Neutron Research
FX Authors acknowledge the support provided by the Department of Commerce
facility NIST Center for Neutron Research. Authors are thankful to J.
Leo and A. Ye for help with the neutron scattering experiments.
NR 24
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U1 1
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PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 2469-9950
EI 2469-9969
J9 PHYS REV B
JI Phys. Rev. B
PD APR 25
PY 2016
VL 93
IS 15
AR 155151
DI 10.1103/PhysRevB.93.155151
PG 5
WC Physics, Condensed Matter
SC Physics
GA DK5GD
UT WOS:000374947100005
ER
PT J
AU Li, JW
Haney, PM
AF Li, Junwen
Haney, Paul M.
TI Optical spintronics in organic-inorganic perovskite photovoltaics
SO PHYSICAL REVIEW B
LA English
DT Article
ID SOLAR-CELLS; HALIDE PEROVSKITES; GRAIN-BOUNDARIES; THIN-FILMS;
FERROELECTRIC POLARIZATION; CH3NH3PBI3 PEROVSKITE; IODIDE PEROVSKITES;
SPIN PHOTOCURRENTS; PHASE-TRANSITIONS; RASHBA
AB Organic-inorganic halide CH3NH3PbI3 solar cells have attracted enormous attention in recent years due to their remarkable power conversion efficiency. When inversion symmetry is broken, these materials should exhibit interesting spin-dependent properties as well, owing to their strong spin-orbit coupling. In this work, we consider the spin-dependent optical response of CH3NH3PbI3. We first use density functional theory to compute the ballistic spin current generated by absorption of unpolarized light. We then consider diffusive transport of photogenerated charge and spin for a thin CH3NH3PbI3 layer with a passivated surface and an Ohmic, nonselective contact. The spin density and spin current are evaluated by solving the drift-diffusion equations for a simplified three-dimensional Rashba model of the electronic structure of the valence and conduction bands. We provide analytic expressions for the photon flux required to induce measurable spin densities, and propose that these spin densities can provide useful information about the role of grain boundaries in the photovoltaic behavior of these materials. We also discuss the prospects for measuring the optically generated spin current with the inverse spin Hall effect.
C1 [Li, Junwen; Haney, Paul M.] NIST, Ctr Nanoscale Sci & Technol, Gaithersburg, MD 20899 USA.
[Li, Junwen] Univ Maryland, Maryland NanoCtr, College Pk, MD 20742 USA.
RP Li, JW (reprint author), NIST, Ctr Nanoscale Sci & Technol, Gaithersburg, MD 20899 USA.; Li, JW (reprint author), Univ Maryland, Maryland NanoCtr, College Pk, MD 20742 USA.
FU University of Maryland [70NANB10H193]; National Institute of Standards
and Technology Center for Nanoscale Science and Technology
[70NANB10H193]
FX We acknowledge helpful conversations with Allan Mac-Donald, Mark Stiles,
and Tom Silva. J.L. acknowledges support under the Cooperative Research
Agreement between the University of Maryland and the National Institute
of Standards and Technology Center for Nanoscale Science and Technology,
Award 70NANB10H193, through the University of Maryland.
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PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 2469-9950
EI 2469-9969
J9 PHYS REV B
JI Phys. Rev. B
PD APR 25
PY 2016
VL 93
IS 15
AR 155432
DI 10.1103/PhysRevB.93.155432
PG 9
WC Physics, Condensed Matter
SC Physics
GA DK5GD
UT WOS:000374947100012
ER
PT J
AU Pershing, AJ
Alexander, MA
Hernandez, CM
Kerr, LA
Le Bris, A
Mills, KE
Nye, JA
Record, NR
Scannell, HA
Scott, JD
Sherwood, GD
Thomas, AC
AF Pershing, Andrew J.
Alexander, Michael A.
Hernandez, Christina M.
Kerr, Lisa A.
Le Bris, Arnault
Mills, Katherine E.
Nye, Janet A.
Record, Nicholas R.
Scannell, Hillary A.
Scott, James D.
Sherwood, Graham D.
Thomas, Andrew C.
TI Response to Comments on "Slow adaptation in the face of rapid warming
leads to collapse of the Gulf of Maine cod fishery"
SO SCIENCE
LA English
DT Editorial Material
ID METABOLIC-RATE; TEMPERATURE; CLIMATE
AB Palmer et al. and Swain et al. suggest that our "extra mortality" time series is spurious. In response, we show that including temperature-dependent mortality improves abundance estimates and that warming waters reduce growth rates in Gulf of Maine cod. Far from being spurious, temperature effects on this stock are clear, and continuing to ignore them puts the stock in jeopardy.
C1 [Pershing, Andrew J.; Kerr, Lisa A.; Le Bris, Arnault; Mills, Katherine E.; Sherwood, Graham D.] Gulf Maine Res Inst, 350 Commercial St, Portland, ME 04101 USA.
[Alexander, Michael A.; Scott, James D.] NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA.
[Hernandez, Christina M.] Woods Hole Oceanog Inst, 86 Water St, Woods Hole, MA 02543 USA.
[Nye, Janet A.] SUNY Stony Brook, Sch Marine & Atmospher Sci, Stony Brook, NY 11794 USA.
[Record, Nicholas R.] Bigelow Lab Ocean Sci, 60 Bigelow Dr, East Boothbay, ME 04544 USA.
[Scannell, Hillary A.] Univ Washington, Sch Oceanog, 1503 Northeast Boat St, Seattle, WA 98105 USA.
[Scott, James D.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Thomas, Andrew C.] Univ Maine, Sch Marine Sci, 5706 Aubert Hall, Orono, ME 04469 USA.
RP Pershing, AJ (reprint author), Gulf Maine Res Inst, 350 Commercial St, Portland, ME 04101 USA.
EM apershing@gmri.org
RI Alexander, Michael/A-7097-2013
OI Alexander, Michael/0000-0001-9646-6427
NR 13
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U1 7
U2 15
PU AMER ASSOC ADVANCEMENT SCIENCE
PI WASHINGTON
PA 1200 NEW YORK AVE, NW, WASHINGTON, DC 20005 USA
SN 0036-8075
EI 1095-9203
J9 SCIENCE
JI Science
PD APR 22
PY 2016
VL 352
IS 6284
DI 10.1126/science.aae0463
PG 2
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DJ8RH
UT WOS:000374479700036
PM 27102475
ER
PT J
AU Cartamil, D
Wraith, J
Wegner, NC
Kacev, D
Lam, CH
Santana-Morales, O
Sosa-Nishizaki, O
Escobedo-Olvera, M
Kohin, S
Graham, JB
Hastings, P
AF Cartamil, D.
Wraith, J.
Wegner, N. C.
Kacev, D.
Lam, C. H.
Santana-Morales, O.
Sosa-Nishizaki, O.
Escobedo-Olvera, M.
Kohin, S.
Graham, J. B.
Hastings, P.
TI Movements and distribution of juvenile common thresher sharks Alopias
vulpinus in Pacific coast waters of the USA and Mexico
SO MARINE ECOLOGY PROGRESS SERIES
LA English
DT Article
DE Thresher shark; Shark nursery; Movements; Satellite telemetry; Fishery
management; Zoogeography; Juvenile
ID SOUTHERN CALIFORNIA BIGHT; SARDINE SARDINOPS-SAGAX; ARCHIVAL TAGGING
DATA; HABITAT PREFERENCES; CURRENT ECOSYSTEM; BEHAVIOR; FISHERY;
TRANSITION; MIGRATION; PATTERNS
AB The common thresher shark Alopias vulpinus constitutes an important commercial fishery on the Pacific coasts of both the USA and Mexico. However, little is known about the juvenile phase of this species. This study used a combination of pop-up archival satellite tagging, tag-recapture, and fishery catch data to investigate the movement patterns, habitat preferences, ecology, and geographic distribution of juvenile common thresher sharks along the Pacific coast of the USA and Mexico. Juvenile threshers primarily utilized continental shelf waters, with a geographic range extending from Punta Eugenia in Baja California, Mexico (27.8 degrees N) north to Morro Bay, California (35.3 degrees N). Within this range, sharks were found at significantly lower latitudes in March and April. Satellite-tagged juvenile threshers exhibited diel patterns of vertical distribution, primarily inhabiting the upper 20 m of the water column by night, and significantly greater depths by day. In addition, juvenile threshers made frequent daytime dives to depths exceeding 50 m, with a maximum recorded dive depth of 192 m. Tracked sharks were most commonly associated with ambient water temperatures between 14 and 17 degrees C, and inhabited significantly warmer temperatures at night than during the day. No tidal or lunar influence on vertical distribution was found, and vertical habitat utilization did not increase concomitantly with shark size. This study is the first to document movements of juvenile threshers between US and Mexican waters, highlighting the need for bi-national management strategies for this shared fishery resource.
C1 [Cartamil, D.; Graham, J. B.; Hastings, P.] Univ Calif San Diego, Scripps Inst Oceanog, Marine Biol Res Div, 9500 Gilman Dr, La Jolla, CA 92093 USA.
[Wraith, J.; Wegner, N. C.; Kohin, S.] Natl Marine Fisheries Serv, Southwest Fisheries Sci Ctr, 8901 La Jolla Shores Dr, La Jolla, CA 92037 USA.
[Kacev, D.] San Diego State Univ, Biol Dept, 5500 Campanile Dr, San Diego, CA 92182 USA.
[Lam, C. H.] Univ Massachusetts Boston, Sch Environm, Large Pelag Res Ctr, POB 3188, Gloucester, MA 01931 USA.
[Santana-Morales, O.; Sosa-Nishizaki, O.; Escobedo-Olvera, M.] CICESE, Dept Ecol, Lab Ecol Pesquera, Km 107,Carretera Tijuana Ensenada, Ensenada 22880, Baja California, Mexico.
RP Cartamil, D (reprint author), Univ Calif San Diego, Scripps Inst Oceanog, Marine Biol Res Div, 9500 Gilman Dr, La Jolla, CA 92093 USA.
EM dcartamil@ucsd.edu
FU Moore Family Foundation; California Sea Grant; Ocean Protection Council;
Save Our Seas Foundation; NOAA's National Cooperative Research Program
FX Funding was provided by The Moore Family Foundation, California Sea
Grant, the Ocean Protection Council, the Save Our Seas Foundation,
NOAA's National Cooperative Research Program, and a gift from Jeffrey
Bohn. Tim Athens and the crew of the FV 'Outer Banks', Daniel Yanagi,
and Eddie Kisfaludy assisted with fieldwork. Thanks to Mike Kinney and
Tim Sippel for their helpful reviews of this manuscript. The manuscript
is dedicated to the memories of co-authors Jeffrey B. Graham and Miguel
Escobedo-Olvera.
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U2 22
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 0171-8630
EI 1616-1599
J9 MAR ECOL PROG SER
JI Mar. Ecol.-Prog. Ser.
PD APR 21
PY 2016
VL 548
BP 153
EP 163
DI 10.3354/meps11673
PG 11
WC Ecology; Marine & Freshwater Biology; Oceanography
SC Environmental Sciences & Ecology; Marine & Freshwater Biology;
Oceanography
GA DM5GF
UT WOS:000376375000011
ER
PT J
AU Giles, JL
Riginos, C
Naylor, GJP
Dharmadi
Ovenden, JR
AF Giles, Jenny L.
Riginos, Cynthia
Naylor, Gavin J. P.
Dharmadi
Ovenden, Jennifer R.
TI Genetic and phenotypic diversity in the wedgefish Rhynchobatus
australiae, a threatened ray of high value in the shark fin trade
SO MARINE ECOLOGY PROGRESS SERIES
LA English
DT Article
DE Wedgefishes; Rays; Shark fin trade; Phylogeography; Southeast Asia
ID MITOCHONDRIAL-DNA; CONTROL REGION; FISHERIES; CONSERVATION; BATOIDS;
FISH; CHONDRICHTHYES; DISPERSAL; INFERENCE; MRBAYES
AB Rhynchobatus spp. (wedgefishes) are large benthopelagic shark-like rays with fins that are highly prized in the international shark fin trade. They are among the most threatened groups of sharks and rays globally. While Rhynchobatus spp. are known to be under considerable fishing pressure as a group, taxonomic confusion among species within the genus has compromised species-specific fishery and demographic data that are urgently needed for developing effective management strategies. Rhynchobatus australiae (Whitley, 1939) is a large Indo-West Pacific species reaching 2 to 3 m that is classified as Vulnerable on the IUCN Red List. This study combines new empirical data from field surveys with data obtained from verified reference specimens to investigate genetic and phenotypic variation in R. australiae and its relative incidence in fisheries. R. australiae dominated Rhynchobatus catch in fisheries surveys across Southeast Asia, and was the most commonly recorded species of the genus in Australia (94% and 58% of captures respectively, n = 207). Study specimens were consistent with a single species with moderate spatial mtDNA variation (Phi(ST) = 0.198, p < 0.0001). We show that R. australiae can be reliably differentiated from other Indo-Pacific species with nadh2 (1044bp), and a section of the control region (456bp) short enough to amplify DNA from processed fins in international trade. We document aspects of morphological variability to assist in the description of external characters that differentiate this species. This is the first range-wide intraspecific study on any wedgefish species, and provides the most complete synthesis of mtDNA data to date for identifying Rhynchobatus fins in the global shark fin trade.
C1 [Giles, Jenny L.; Riginos, Cynthia] Univ Queensland, Sch Biol Sci, St Lucia, Qld 4072, Australia.
[Naylor, Gavin J. P.] Hollings Marine Lab, Charleston, SC 29412 USA.
[Dharmadi] Minist Marine Affairs & Fisheries, Res Ctr Capture Fisheries, Jl Pasir Putih 1, Ancol Timur 14430, Jakarta Utara, Indonesia.
[Ovenden, Jennifer R.] Univ Queensland, Sch Biomed Sci, Mol Fisheries Lab, St Lucia, Qld 4072, Australia.
[Giles, Jenny L.] NOAA, Natl Acad Sci, Northwest Fisheries Sci Ctr, Natl Marine Fisheries Serv,Forens Lab, 2725 Montlake Blvd E, Seattle, WA 98112 USA.
RP Giles, JL (reprint author), Univ Queensland, Sch Biol Sci, St Lucia, Qld 4072, Australia.; Giles, JL (reprint author), NOAA, Natl Acad Sci, Northwest Fisheries Sci Ctr, Natl Marine Fisheries Serv,Forens Lab, 2725 Montlake Blvd E, Seattle, WA 98112 USA.
EM jennylgiles@gmail.com
RI Riginos, Cynthia/G-3320-2010
OI Riginos, Cynthia/0000-0002-5485-4197
FU Sea World Research and Rescue Foundation Australia; PADI Foundation;
University Women Australia; Phuket Marine Biological Station in
Thailand; Australian-American Fulbright Commission; Ministry of Marine
Affairs and Fisheries' Research Center for Capture Fisheries (RCCF)
[FIS/2003/037]
FX This work was undertaken on an Australian postgraduate award. We thank
the Sea World Research and Rescue Foundation Australia, PADI Foundation
and University Women Australia for funding this research, and the many
collaborators who assisted in the field, contributed samples, and
assisted in accessing reference specimens. In particular, we thank L.
Marshall, K. Khampetch, S. Woranchananant, V. Schluessel, Fahmi, W.
White, P. Last, E. Garvilles, N. Barut, E. Alesna, M. Sarmiento, A.
Gutteridge, G. Johnson, A. Harry, O. Bittar, C. Dudgeon, J. White, S.
Peverell, R. Pillans, J. Salini, R. Buckworth, D. Almojil, A. Graham, M.
McGrouther, M. Shivji, M. Heithaus, D. Catania, the staff at the PengHu
Islands Marine Biological Research Station, Taiwan and Phuket Marine
Biological Station in Thailand, and the Australian-American Fulbright
Commission for funding US activities. Fieldwork was under the Guidelines
of the University of Queensland Animal Ethics Committee (Approval
ANRFA/615/08). Collection in the Philippines was undertaken under an MOA
with the Department of Agriculture (Marine Fisheries Research Division,
BFAR-NFRDI), Commodity clearance No. 09-5295. Indonesian field
collections were part of a project of the Australian Centre for
International Agricultural Research (ACIAR) in association with the
Indonesian Institute of Sciences (LIPI) and Ministry of Marine Affairs
and Fisheries' Research Center for Capture Fisheries (RCCF) (Project
FIS/2003/037). In Thailand, field surveys were undertaken as part of a
visiting studentship at Kasetsart University's Department of Marine
Science.
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U2 10
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 0171-8630
EI 1616-1599
J9 MAR ECOL PROG SER
JI Mar. Ecol.-Prog. Ser.
PD APR 21
PY 2016
VL 548
BP 165
EP 180
DI 10.3354/meps11617
PG 16
WC Ecology; Marine & Freshwater Biology; Oceanography
SC Environmental Sciences & Ecology; Marine & Freshwater Biology;
Oceanography
GA DM5GF
UT WOS:000376375000012
ER
PT J
AU Johnson, RC
Garza, JC
MacFarlane, RB
Grimes, CB
Phillis, CC
Koch, PL
Weber, PK
Carr, MH
AF Johnson, Rachel C.
Garza, John Carlos
MacFarlane, R. Bruce
Grimes, Churchill B.
Phillis, Corey C.
Koch, Paul L.
Weber, Peter K.
Carr, Mark H.
TI Isotopes and genes reveal freshwater origins of Chinook salmon
Oncorhynchus tshawytscha aggregations in California's coastal ocean
SO MARINE ECOLOGY PROGRESS SERIES
LA English
DT Article
DE Winter-run Chinook salmon; Schooling; Otolith microchemistry; Strontium;
Navigation
ID WIRE TAG RECOVERIES; LA-MC-ICPMS; PACIFIC SALMON; STOCK IDENTIFICATION;
POPULATION-STRUCTURE; MICROSATELLITE DNA; CENTRAL VALLEY; OTOLITH
MICROCHEMISTRY; SPATIAL-DISTRIBUTION; ATLANTIC SALMON
AB The ability of salmon to navigate from the ocean back to their river of origin to spawn acts to reinforce local adaptation and maintenance of unique and heritable traits among salmon populations. Here, the extent to which Chinook salmon Oncorhynchus tshawytscha from the same freshwater breeding groups associate together in the ocean at regional and smaller-scale aggregations prior to homeward migration is evaluated. Natural variation in salmon otolith daily growth bands, strontium isotopes (Sr-87/Sr-86), and microsatellite DNA were used as intrinsic tags to link the distributions of fish caught in the ocean with their freshwater origins. Adults were caught from vessels by hook and line in small aggregations (7-18 ind.) at the same geographic location (1-24 km of coastline) and time (4-36 h) from 3 ocean regions along central California, USA. Salmon caught together in aggregations were from the same genetic group, and to a lesser extent, of the same natal origin (individual rivers or hatcheries). However, at regional scales, adult salmon mixed. Central Valley winter-run Chinook salmon caught together in the ocean varied in the duration of freshwater rearing for up to 2-3 mo prior to seaward migration, suggesting associations within the group were not established in freshwater or maintained over the lifetime of the fish. Our findings are consistent with coarser information indicating stocks are distributed differently in time and space, but larger sample sizes are required to evaluate the consistency of patterns at smaller spatial scales. This study uncovers freshwater associations prior to homeward migration, a principle and undocumented prerequisite of the collective navigation hypothesis.
C1 [Johnson, Rachel C.; Garza, John Carlos; MacFarlane, R. Bruce; Grimes, Churchill B.] NOAA, Fisheries Ecol Div, Southwest Fisheries Sci Ctr, Natl Marine Fisheries Serv, 110 Shaffer Rd, Santa Cruz, CA 95060 USA.
[Johnson, Rachel C.; Carr, Mark H.] Univ Calif Santa Cruz, Dept Ecol & Evolutionary Biol, 110 Shaffer Rd, Santa Cruz, CA 95060 USA.
[Garza, John Carlos] Univ Calif Santa Cruz, Dept Ocean Sci, 1156 High St, Santa Cruz, CA 95060 USA.
[MacFarlane, R. Bruce; Grimes, Churchill B.] Univ Calif Santa Cruz, Inst Marine Sci, 110 Shaffer Rd, Santa Cruz, CA 95060 USA.
[Phillis, Corey C.] Univ Calif Berkeley, Dept Earth & Planetary Sci, 307 McCone Hall, Berkeley, CA 94720 USA.
[Koch, Paul L.] Univ Calif Santa Cruz, Dept Earth & Planetary Sci, 1156 High St, Santa Cruz, CA 95060 USA.
[Weber, Peter K.] Lawrence Livermore Natl Lab, Glenn T Seaborg Inst, 7000 East Ave, Livermore, CA 94550 USA.
[Phillis, Corey C.] Metropolitan Water Dist Southern Calif, 1121 L St Suite 900, Sacramento, CA 95814 USA.
RP Johnson, RC (reprint author), NOAA, Fisheries Ecol Div, Southwest Fisheries Sci Ctr, Natl Marine Fisheries Serv, 110 Shaffer Rd, Santa Cruz, CA 95060 USA.; Johnson, RC (reprint author), Univ Calif Santa Cruz, Dept Ecol & Evolutionary Biol, 110 Shaffer Rd, Santa Cruz, CA 95060 USA.
EM rachel.johnson@noaa.gov
FU NOAA Fisheries through the Student Careers' Experience Program;
University of California's Coastal Environmental Quality Initiative;
Partnership for Interdisciplinary Studies of Coastal Oceans (PISCO);
Gordon and Betty Moore Foundation; David and Lucile Packard Foundation;
Myers Oceanographic Trust
FX We thank W. Satterthwaite and S. Lindley for discussions and significant
improvements to the manuscript, F. Ramos and D. Tollstrup for assistance
with Sr isotopic measurements, E. Anderson and A. Clemento for
assistance with genetic analyses, and P. Raimondi and C. Syms for
statistical advice. Special thanks to M. Kilgour, A. Nickels, S. Reins,
and A. Bachar for tissue collection and preparation. This project would
not have been possible without the fishing skills of P. Parravano, J.
Hie, R. Block, J. Estes, S. Berkeley, J. Figurski, S. Sogard and the
crew and patrons of the 'New Captain Pete', 'The Outer Limits', and
'Dave's Albacore'. A. Smith provided GIS assistance for Fig. 1, and G.
Whitman provided editorial assistance. We thank the programs that funded
this work: NOAA Fisheries through the Student Careers' Experience
Program, University of California's Coastal Environmental Quality
Initiative, and the Partnership for Interdisciplinary Studies of Coastal
Oceans (PISCO), which is funded primarily by the Gordon and Betty Moore
Foundation, the David and Lucile Packard Foundation, and the Myers
Oceanographic Trust.
NR 86
TC 0
Z9 0
U1 5
U2 6
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 0171-8630
EI 1616-1599
J9 MAR ECOL PROG SER
JI Mar. Ecol.-Prog. Ser.
PD APR 21
PY 2016
VL 548
BP 181
EP 196
DI 10.3354/meps11623
PG 16
WC Ecology; Marine & Freshwater Biology; Oceanography
SC Environmental Sciences & Ecology; Marine & Freshwater Biology;
Oceanography
GA DM5GF
UT WOS:000376375000013
ER
PT J
AU Crear, DP
Lawson, DD
Seminoff, JA
Eguchi, T
LeRoux, RA
Lowe, CG
AF Crear, Daniel P.
Lawson, Daniel D.
Seminoff, Jeffrey A.
Eguchi, Tomoharu
LeRoux, Robin A.
Lowe, Christopher G.
TI Seasonal shifts in the movement and distribution of green sea turtles
Chelonia mydas in response to anthropogenically altered water
temperatures
SO MARINE ECOLOGY PROGRESS SERIES
LA English
DT Article
DE Thermal refuge; Ectotherm; Warm water effluent; Power plants; Acoustic
telemetry; Foraging aggregation
ID GULF-OF-CALIFORNIA; MARINE-ENVIRONMENT; SCALE MOVEMENTS; FORAGING AREA;
GROWTH-RATES; MODELS; FLORIDA; LAGOON; DORMANCY; ECOLOGY
AB Anthropogenically altered water temperatures (AAWT) have the potential to affect the movement and distribution of marine ectothermic species. Green sea turtles (GSTs) Chelonia mydas are an ectothermic species observed inhabiting 2 sites with AAWT at the northern point of their geographical range in the eastern Pacific. An acoustic receiver array was deployed with temperature loggers at the San Gabriel River, Long Beach, CA, where 2 power plants discharge warm water into the river, and at the 7th St. Basin, Seal Beach, CA, a dredged shallow basin with warmer water compared to surrounding coastal habitats during the summer months. Juvenile GSTs (n = 22, straight carapace length = 45.2 to 96.8 cm) were tagged with acoustic transmitters. Turtles in the basin migrated into the river during winter months when temperatures dropped below 15 degrees C. During the winter, turtles were most frequently detected at the river receiver stations adjacent to and downstream of the power plants. This suggests that GSTs use the warm effluent as a thermal refuge, avoiding colder areas upstream of the power plants and near the river mouth. In the summer, turtles were most frequently detected at receiver stations upstream of the power plants, potentially exploiting areas of the river with higher primary productivity. AAWT sustain the northernmost aggregation of GSTs in the eastern Pacific year round; however, based on GST thermal tolerance, this population is expected to change their movement patterns when the power plants discontinue discharging warm water by 2029.
C1 [Crear, Daniel P.] Coll William & Mary, Virginia Inst Marine Sci, POB 1346, Gloucester Point, VA 23062 USA.
[Lawson, Daniel D.] NOAA, Protected Resources Div, West Coast Reg Off, Natl Marine Fisheries Serv, 501 West Ocean Blvd,Suite 4200, Long Beach, CA 90802 USA.
[Seminoff, Jeffrey A.; Eguchi, Tomoharu; LeRoux, Robin A.] NOAA, Protected Resources Div, Southwest Fisheries Sci Ctr, Natl Marine Fisheries Serv, 8901 La Jolla Shores Dr, La Jolla, CA 92037 USA.
[Lowe, Christopher G.] Calif State Univ Long Beach, Dept Biol Sci, 1250 Bellflower Blvd, Long Beach, CA 90840 USA.
RP Crear, DP (reprint author), Coll William & Mary, Virginia Inst Marine Sci, POB 1346, Gloucester Point, VA 23062 USA.
EM dcrear8@gmail.com
FU NOAA Fisheries West Coast Regional Office; SCTC Marine Biology
Foundation; Los Angeles Rod and Reel Club
FX Financial support was provided by the NOAA Fisheries West Coast Regional
Office, SCTC Marine Biology Foundation, and the Los Angeles Rod and Reel
Club. We thank US Fish and Wildlife manager K. Gilligan, US Navy
Ecologist B. Schallmann, and Los Cerritos Wetlands for logical support.
We also thank the following individuals for their support in the field:
D. Prosperi, J. Schumacher, B. MacDonald, and the entire NOAA-NMFS team
that assisted with turtle capture. We especially thank numerous
volunteers who helped with data-collection, including J. Hinricher, A.
Jimenez, C. White, and W. Stahnke. We particularly thank D. Johnson, J.
Archie, and T. Fahy for their input and guidance during the project. All
research and animal handling was carried out under the National Marine
Fisheries Service Permit #14510
NR 47
TC 1
Z9 1
U1 17
U2 28
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 0171-8630
EI 1616-1599
J9 MAR ECOL PROG SER
JI Mar. Ecol.-Prog. Ser.
PD APR 21
PY 2016
VL 548
BP 219
EP 232
DI 10.3354/meps11696
PG 14
WC Ecology; Marine & Freshwater Biology; Oceanography
SC Environmental Sciences & Ecology; Marine & Freshwater Biology;
Oceanography
GA DM5GF
UT WOS:000376375000016
ER
PT J
AU Lindsay, RE
Constantine, R
Robbins, J
Mattila, DK
Tagarino, A
Dennis, TE
AF Lindsay, Rebecca E.
Constantine, Rochelle
Robbins, Jooke
Mattila, David K.
Tagarino, Alden
Dennis, Todd E.
TI Characterising essential breeding habitat for whales informs the
development of large-scale Marine Protected Areas in the South Pacific
SO MARINE ECOLOGY PROGRESS SERIES
LA English
DT Article
DE Habitat; Maximum Entropy Modelling; Humpback whale; MPA; Megaptera
novaeangliae
ID SPECIES DISTRIBUTION MODELS; HUMPBACK WHALES; MEGAPTERA-NOVAEANGLIAE;
SAMPLE-SIZE; DISTRIBUTIONS; MAXENT; CONSERVATION; IDENTIFICATION;
PERFORMANCE; HAWAII
AB There are significant challenges associated with mapping critical habitat for large, migratory species. The humpback whales of Oceania in the South Pacific are no exception, with their winter breeding grounds spanning > 4000 km of ocean basin. This subpopulation is listed as endangered, but there are few systematic spatial data with which to prioritise specific areas for additional research or conservation. A few sites in Oceania have been the focus of long-term, non-systematic population surveys. Using the maximum entropy algorithm, we developed predictive habitat models for 2 such sites: American Samoa 2003-2010 (n = 300) and Tonga 1996-2007 (n = 475), using sightings of whale groups and environmental factors hypothesised to influence their space-use patterns. At both sites, shallow water was the best predictor of the spatial distribution of mother-calf pairs. In contrast, access to deep water was important for adult groups, and seafloor slope and rugosity influenced habitat suitability for males engaged in acoustic breeding displays. Our study illustrates the value of predictive modelling for identifying habitat partitioning for specific sub-groups of a wider population. Similarities between habitat requirements predicted in our study to those identified for other populations suggest that the slow recovery of Oceania humpback whales cannot be attributed to unusual breeding-habitat needs; instead, there may be other factors influencing the slow increase in population size. We recommend that the modelling techniques utilised here be used to identify other breeding sites within Oceania for future research and conservation efforts across the South Pacific region.
C1 [Lindsay, Rebecca E.; Constantine, Rochelle; Dennis, Todd E.] Univ Auckland, Sch Biol Sci, Auckland 1, New Zealand.
[Constantine, Rochelle] Univ Auckland, Inst Marine Sci, Auckland 1, New Zealand.
[Robbins, Jooke; Mattila, David K.] Ctr Coastal Studies, Provincetown, MA USA.
[Mattila, David K.] Hawaiian Isl Humpback Whale Natl Marine Sanctuary, Kihei, HI USA.
[Tagarino, Alden] Amer Samoa Dept Marine & Wildlife Resources, Pago Pago, AS USA.
[Tagarino, Alden] Univ Philippines, Inst Renewable & Nat Resources, Laguna, Philippines.
RP Constantine, R (reprint author), Univ Auckland, Sch Biol Sci, Auckland 1, New Zealand.; Constantine, R (reprint author), Univ Auckland, Inst Marine Sci, Auckland 1, New Zealand.
EM r.constantine@auckland.ac.nz
OI Constantine, Rochelle/0000-0003-3260-539X
NR 59
TC 0
Z9 0
U1 11
U2 15
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 0171-8630
EI 1616-1599
J9 MAR ECOL PROG SER
JI Mar. Ecol.-Prog. Ser.
PD APR 21
PY 2016
VL 548
BP 263
EP 275
DI 10.3354/meps11663
PG 13
WC Ecology; Marine & Freshwater Biology; Oceanography
SC Environmental Sciences & Ecology; Marine & Freshwater Biology;
Oceanography
GA DM5GF
UT WOS:000376375000019
ER
PT J
AU Olivieri, G
Parry, KM
Powell, CJ
Tobias, DJ
Brown, MA
AF Olivieri, Giorgia
Parry, Krista M.
Powell, Cedric J.
Tobias, Douglas J.
Brown, Matthew A.
TI Quantitative interpretation of molecular dynamics simulations for X-ray
photoelectron spectroscopy of aqueous solutions
SO JOURNAL OF CHEMICAL PHYSICS
LA English
DT Article
ID MEAN FREE PATHS; AUGER-ELECTRON-SPECTROSCOPY; AIR-WATER-INTERFACE;
50-2000 EV RANGE; LIQUID/VAPOR INTERFACE; SPATIAL-DISTRIBUTION; BULK
WATER; NANOPARTICLES; PARAMETERS; SURFACES
AB Over the past decade, energy-dependent ambient pressure X-ray photoelectron spectroscopy (XPS) has emerged as a powerful analytical probe of the ion spatial distributions at the vapor (vacuum)aqueous electrolyte interface. These experiments are often paired with complementary molecular dynamics (MD) simulations in an attempt to provide a complete description of the liquid interface. There is, however, no systematic protocol that permits a straightforward comparison of the two sets of results. XPS is an integrated technique that averages signals from multiple layers in a solution even at the lowest photoelectron kinetic energies routinely employed, whereas MD simulations provide a microscopic layer-by-layer description of the solution composition near the interface. Here, we use the National Institute of Standards and Technology database for the Simulation of Electron Spectra for Surface Analysis (SESSA) to quantitatively interpret atom-density profiles from MD simulations for XPS signal intensities using sodium and potassium iodide solutions as examples. We show that electron inelastic mean free paths calculated from a semi-empirical formula depend strongly on solution composition, varying by up to 30% between pure water and concentrated NaI. The XPS signal thus arises from different information depths in different solutions for a fixed photoelectron kinetic energy. XPS signal intensities are calculated using SESSA as a function of photoelectron kinetic energy (probe depth) and compared with a widely employed ad hoc method. SESSA simulations illustrate the importance of accounting for elastic-scattering events at low photoelectron kinetic energies (<300 eV) where the ad hoc method systematically underestimates the preferential enhancement of anions over cations. Finally, some technical aspects of applying SESSA to liquid interfaces are discussed. Published by AIP Publishing.
C1 [Olivieri, Giorgia; Brown, Matthew A.] ETH, Dept Mat, Lab Surface Sci & Technol, CH-8093 Zurich, Switzerland.
[Parry, Krista M.; Tobias, Douglas J.] Univ Calif Irvine, Dept Chem, Irvine, CA 92697 USA.
[Powell, Cedric J.] NIST, Mat Measurement Sci Div, Gaithersburg, MD 20899 USA.
RP Brown, MA (reprint author), ETH, Dept Mat, Lab Surface Sci & Technol, CH-8093 Zurich, Switzerland.
EM matthew.brown@mat.ethz.ch
RI Brown, Matthew/D-9236-2012; Tobias, Douglas/B-6799-2015
FU ETH Research Grant [ETH-20 13-2]; National Science Foundation
[CHE-0431312]; Laboratory for Surface Science and Technology at ETH
Zurich
FX G.O. is funded through an ETH Research Grant (No. ETH-20 13-2). The work
at UC Irvine is supported in part by a grant from the National Science
Foundation (No. CHE-0431312). G.O. and M.A.B. are indebted to Professor
Nicholas D. Spencer and the Laboratory for Surface Science and
Technology at ETH Zurich for continued support. Professor John C.
Hemminger is acknowledged for insightful discussions.
NR 46
TC 3
Z9 3
U1 8
U2 24
PU AMER INST PHYSICS
PI MELVILLE
PA 1305 WALT WHITMAN RD, STE 300, MELVILLE, NY 11747-4501 USA
SN 0021-9606
EI 1089-7690
J9 J CHEM PHYS
JI J. Chem. Phys.
PD APR 21
PY 2016
VL 144
IS 15
AR 154704
DI 10.1063/1.4947027
PG 9
WC Chemistry, Physical; Physics, Atomic, Molecular & Chemical
SC Chemistry; Physics
GA DL6YM
UT WOS:000375786000035
PM 27389231
ER
PT J
AU Patrone, PN
Rosch, TW
Phelan, FR
AF Patrone, Paul N.
Rosch, Thomas W.
Phelan, Frederick R., Jr.
TI Bayesian calibration of coarse-grained forces: Efficiently addressing
transferability
SO JOURNAL OF CHEMICAL PHYSICS
LA English
DT Article
ID ITERATIVE BOLTZMANN INVERSION; UNCERTAINTY QUANTIFICATION;
MOLECULAR-DYNAMICS; POTENTIALS; TEMPERATURE; POLYSTYRENE; SYSTEMS;
SIMULATIONS; MODELS
AB Generating and calibrating forces that are transferable across a range of state-points remains a challenging task in coarse-grained (CG) molecular dynamics. In this work, we present a coarse-graining workflow, inspired by ideas from uncertainty quantification and numerical analysis, to address this problem. The key idea behind our approach is to introduce a Bayesian correction algorithm that uses functional derivatives of CG simulations to rapidly and inexpensively recalibrate initial estimates f(0) of forces anchored by standard methods such as force-matching. Taking density-temperature relationships as a running example, we demonstrate that this algorithm, in concert with various interpolation schemes, can be used to efficiently compute physically reasonable force curves on a fine grid of state-points. Importantly, we show that our workflow is robust to several choices available to the modeler, including the interpolation schemes and tools used to construct f(0). In a related vein, we also demonstrate that our approach can speed up coarse-graining by reducing the number of atomistic simulations needed as inputs to standard methods for generating CG forces.
C1 [Patrone, Paul N.; Rosch, Thomas W.; Phelan, Frederick R., Jr.] NIST, Gaithersburg, MD 20899 USA.
RP Patrone, PN (reprint author), NIST, Gaithersburg, MD 20899 USA.
EM paul.patrone@nist.gov
FU NIST [506]; National Science Foundation Math Institute 507 [DMS-0931945]
FX All authors thank Debra Audus, Timothy Burns, Andrew Dienstfrey, and
Anthony Kearsley for useful comments during preparation of the
manuscript. T.R. thanks Sergei Izvekov (Army Research Lab) for the use
of his FM code implemented on the Garnet cluster located at the ERDC
DSRC. Part of this work was completed while P.P. was a postdoctoral
fellow at the Institute for Mathematics and its Applications (IMA) under
a 506 grant from NIST to the IMA. The IMA is a National Science
Foundation Math Institute 507 funded under Award No. DMS-0931945.
NR 43
TC 1
Z9 1
U1 1
U2 4
PU AMER INST PHYSICS
PI MELVILLE
PA 1305 WALT WHITMAN RD, STE 300, MELVILLE, NY 11747-4501 USA
SN 0021-9606
EI 1089-7690
J9 J CHEM PHYS
JI J. Chem. Phys.
PD APR 21
PY 2016
VL 144
IS 15
AR 154101
DI 10.1063/1.4945380
PG 15
WC Chemistry, Physical; Physics, Atomic, Molecular & Chemical
SC Chemistry; Physics
GA DL6YM
UT WOS:000375786000007
PM 27389203
ER
PT J
AU Nguyen, TB
Tyndall, GS
Crounse, JD
Teng, AP
Bates, KH
Schwantes, RH
Coggon, MM
Zhang, L
Feiner, P
Milller, DO
Skog, KM
Rivera-Rios, JC
Dorris, M
Olson, KF
Koss, A
Wild, RJ
Brown, SS
Goldstein, AH
de Gouw, JA
Brune, WH
Keutsch, FN
Seinfeldcj, JH
Wennberg, PO
AF Nguyen, Tran B.
Tyndall, Geoffrey S.
Crounse, John D.
Teng, Alexander P.
Bates, Kelvin H.
Schwantes, Rebecca H.
Coggon, Matthew M.
Zhang, Li
Feiner, Philip
Milller, David O.
Skog, Kate M.
Rivera-Rios, Jean C.
Dorris, Matthew
Olson, Kevin F.
Koss, Abigail
Wild, Robert J.
Brown, Steven S.
Goldstein, Allen H.
de Gouw, Joost A.
Brune, William H.
Keutsch, Frank N.
Seinfeldcj, John H.
Wennberg, Paul O.
TI Atmospheric fates of Criegee intermediates in the ozonolysis of isoprene
SO PHYSICAL CHEMISTRY CHEMICAL PHYSICS
LA English
DT Article
ID GAS-PHASE OZONOLYSIS; LASER-INDUCED FLUORESCENCE; CONFORMER-DEPENDENT
REACTIVITY; IONIZATION MASS-SPECTROMETRY; VOLATILE ORGANIC-COMPOUNDS;
PEROXY RADICAL REACTIONS; OZONE-ALKENE REACTIONS; METHYL VINYL KETONE;
CARBONYL OXIDES; WATER-VAPOR
AB We use a large laboratory, modeling, and field dataset to investigate the isoprene + O-3 reaction, with the goal of better understanding the fates of the C-1 and C-4 Criegee intermediates in the atmosphere. Although ozonolysis can produce several distinct Criegee intermediates, the C-1 stabilized Criegee (CH2OO, 61 +/- 9%) is the only one observed to react bimolecularly. We suggest that the C-4 Criegees have a low stabilization fraction and propose pathways for their decomposition. Both prompt and non-prompt reactions are important in the production of OH (28% +/- 5%) and formaldehyde (81% +/- 16%). The yields of unimolecular products (OH, formaldehyde, methacrolein (42 +/- 6%) and methyl vinyl ketone (18 +/- 6%)) are fairly insensitive to water, i.e., changes in yields in response to water vapor (<= 4% absolute) are within the error of the analysis. We propose a comprehensive reaction mechanism that can be incorporated into atmospheric models, which reproduces laboratory data over a wide range of relative humidities. The mechanism proposes that CH2OO + H2O (k((H2O)) similar to 1 x 10(-15) cm(3) molec(-1) s(-1)) yields 73% hydroxymethyl hydroperoxide (HMHP), 6% formaldehyde + H2O2, and 21% formic acid + H2O; and CH2OO + (H2O)(2) (k((H2O)2) similar to 1 x 10(-12) cm(3) molec(-1) s(-1)) yields 40% HMHP, 6% formaldehyde + H2O2, and 54% formic acid + H2O. Competitive rate determinations (k(SO2)/k((H2O)n=1,2) similar to 2.2 (+/- 0.3) x 10(4)) and field observations suggest that water vapor is a sink for greater than 98% of CH2OO in a Southeastern US forest, even during pollution episodes ([SO2] similar to 10 ppb). The importance of the CH2OO + (H2O)(n) reaction is demonstrated by high HMHP mixing ratios observed over the forest canopy. We find that CH2OO does not substantially affect the lifetime of SO2 or HCOOH in the Southeast US, e.g., CH2OO + SO2 reaction is a minor contribution (<6%) to sulfate formation. Extrapolating, these results imply that sulfate production by stabilized Criegees is likely unimportant in regions dominated by the reactivity of ozone with isoprene. In contrast, hydroperoxide, organic acid, and formaldehyde formation from isoprene ozonolysis in those areas may be significant.
C1 [Nguyen, Tran B.; Crounse, John D.; Teng, Alexander P.; Schwantes, Rebecca H.; Wennberg, Paul O.] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA.
[Tyndall, Geoffrey S.] Natl Ctr Atmospher Res, Atmospher Chem Observat & Modeling Lab, POB 3000, Boulder, CO 80307 USA.
[Bates, Kelvin H.; Coggon, Matthew M.; Seinfeldcj, John H.] CALTECH, Div Chem & Chem Engn, Pasadena, CA 91125 USA.
[Zhang, Li; Feiner, Philip; Milller, David O.; Brune, William H.] Penn State Univ, Dept Meteorol, 503 Walker Bldg, University Pk, PA 16802 USA.
[Skog, Kate M.; Rivera-Rios, Jean C.; Dorris, Matthew; Keutsch, Frank N.] Univ Wisconsin, Dept Chem, 1101 Univ Ave, Madison, WI 53706 USA.
[Olson, Kevin F.; Goldstein, Allen H.] Univ Calif Berkeley, Dept Environm Sci Policy & Management, Berkeley, CA 94720 USA.
[Olson, Kevin F.; Goldstein, Allen H.] Univ Calif Berkeley, Dept Civil & Environm Engn, Berkeley, CA 94720 USA.
[Coggon, Matthew M.; Koss, Abigail; Wild, Robert J.; Brown, Steven S.; de Gouw, Joost A.] NOAA, Earth Syst Res Lab, Div Chem Sci, Boulder, CO USA.
[Wild, Robert J.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Seinfeldcj, John H.; Wennberg, Paul O.] CALTECH, Div Engn & Appl Sci, Pasadena, CA 91125 USA.
[Nguyen, Tran B.] Univ Calif Davis, Dept Environm Toxicol, Davis, CA 95616 USA.
[Rivera-Rios, Jean C.; Keutsch, Frank N.] Harvard Univ, Dept Chem & Chem Biol, Cambridge, MA 02138 USA.
[Olson, Kevin F.] Chevron Corp, San Ramon, CA USA.
RP Nguyen, TB (reprint author), CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA.; Nguyen, TB (reprint author), Univ Calif Davis, Dept Environm Toxicol, Davis, CA 95616 USA.
EM tbn@ucdavis.edu
RI de Gouw, Joost/A-9675-2008; Coggon, Matthew/I-8604-2016; Brown,
Steven/I-1762-2013; Koss, Abigail/B-5421-2015; Crounse,
John/C-3700-2014; Manager, CSD Publications/B-2789-2015
OI de Gouw, Joost/0000-0002-0385-1826; Coggon, Matthew/0000-0002-5763-1925;
Crounse, John/0000-0001-5443-729X;
FU U.S. National Science Foundation (NSF) [AGS-1331360]; NSF [AGS-1240604];
Electric Power Research Institute [EPRI-10003903]
FX Funding for this work was provided by the U.S. National Science
Foundation (NSF) Postdoctoral Research Fellowship award AGS-1331360, NSF
grant AGS-1240604, and the Electric Power Research Institute grant
EPRI-10003903. We thank the organizers and participants of the FIXCIT
chamber campaign and SOAS field campaign.
NR 107
TC 11
Z9 11
U1 39
U2 95
PU ROYAL SOC CHEMISTRY
PI CAMBRIDGE
PA THOMAS GRAHAM HOUSE, SCIENCE PARK, MILTON RD, CAMBRIDGE CB4 0WF, CAMBS,
ENGLAND
SN 1463-9076
EI 1463-9084
J9 PHYS CHEM CHEM PHYS
JI Phys. Chem. Chem. Phys.
PD APR 21
PY 2016
VL 18
IS 15
BP 10241
EP 10254
DI 10.1039/c6cp00053c
PG 14
WC Chemistry, Physical; Physics, Atomic, Molecular & Chemical
SC Chemistry; Physics
GA DJ6VF
UT WOS:000374350600043
PM 27021601
ER
PT J
AU Schwarz, S
Bollen, G
Ringle, R
Savory, J
Schury, P
AF Schwarz, S.
Bollen, G.
Ringle, R.
Savory, J.
Schury, P.
TI The LEBIT ion cooler and buncher
SO NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION A-ACCELERATORS
SPECTROMETERS DETECTORS AND ASSOCIATED EQUIPMENT
LA English
DT Article
DE Radiofrequency quadrupole; Radioactive ion beams; Beam transport
ID PROJECTILE FRAGMENTS; CHARGED-PARTICLES; MASS MEASUREMENTS; RARE
ISOTOPES; BEAM BUNCHER; GAS CELL; TRAP; PERFORMANCE; EXTRACTION;
FACILITY
AB This paper presents a detailed description of the ion cooler and buncher, installed at the Low Energy Beam and Ion Trap Facility (LEBIT) at the National Superconducting Cyclotron Laboratory (NSCL). NSCL uses gas stopping to provide rare isotopes from projectile fragmentation for its low-energy physics program and to the re-accelerator ReA. The LEBIT ion buncher converts the continuous rare-isotope beam, delivered from the gas stopping cell, into short, low-emittance ion pulses, required for high precision mass measurements with a 9.4 T Penning trap mass spectrometer. Operation at cryogenic temperatures, a simplified electrode structure and dedicated rugged electronics contribute to the high performance and reliability of the device, which have been essential to the successful LEBIT physics program since 2005. (C) 2016 Elsevier B.V. All rights reserved.
C1 [Schwarz, S.; Ringle, R.] MSU, Natl Superconducting Cyclotron Lab, E Lansing, MI USA.
[Bollen, G.] MSU, Facil Rare Isotope Beams, E Lansing, MI USA.
[Bollen, G.] MSU, Dept Phys & Astron, E Lansing, MI USA.
[Savory, J.] NIST, Boulder, CO USA.
[Schury, P.] Univ Tsukuba, Tsukuba, Ibaraki 3058577, Japan.
RP Schwarz, S (reprint author), MSU, Natl Superconducting Cyclotron Lab, E Lansing, MI USA.
NR 29
TC 2
Z9 2
U1 1
U2 3
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0168-9002
EI 1872-9576
J9 NUCL INSTRUM METH A
JI Nucl. Instrum. Methods Phys. Res. Sect. A-Accel. Spectrom. Dect. Assoc.
Equip.
PD APR 21
PY 2016
VL 816
BP 131
EP 141
DI 10.1016/j.nima.2016.01.078
PG 11
WC Instruments & Instrumentation; Nuclear Science & Technology; Physics,
Nuclear; Physics, Particles & Fields
SC Instruments & Instrumentation; Nuclear Science & Technology; Physics
GA DF0DO
UT WOS:000371009400019
ER
PT J
AU Bower, GC
Deller, A
Demorest, P
Brunthaler, A
Falcke, H
Moscibrodzka, M
O'Leary, RM
Eatough, RP
Kramer, M
Lee, KJ
Spitler, L
Desvignes, G
Rushton, AP
Doeleman, S
Reid, MJ
AF Bower, Geoffrey C.
Deller, Adam
Demorest, Paul
Brunthaler, Andreas
Falcke, Heino
Moscibrodzka, Monika
O'Leary, Ryan M.
Eatough, Ralph P.
Kramer, Michael
Lee, K. J.
Spitler, Laura
Desvignes, Gregory
Rushton, Anthony P.
Doeleman, Sheperd
Reid, Mark J.
TI THE PROPER MOTION OF THE GALACTIC CENTER PULSAR RELATIVE TO SAGITTARIUS
A (vol 798, 120, 2015)
SO ASTROPHYSICAL JOURNAL
LA English
DT Correction
C1 [Bower, Geoffrey C.] Acad Sinica, Inst Astron & Astrophys, 645 N Aohoku Pl, Hilo, HI 96720 USA.
[Deller, Adam; Falcke, Heino] ASTRON, POB 2, NL-7990 AA Dwingeloo, Netherlands.
[Demorest, Paul] NRAO, 520 Edgemont Rd, Charlottesville, VA 22903 USA.
[Brunthaler, Andreas; Falcke, Heino; Eatough, Ralph P.; Kramer, Michael; Lee, K. J.; Spitler, Laura; Desvignes, Gregory] Max Planck Inst Radioastron, Hugel 69, D-53121 Bonn, Germany.
[Falcke, Heino; Moscibrodzka, Monika] Radboud Univ Nijmegen, Inst Math Astrophys & Particle Phys IMAPP, Dept Astrophys, POB 9010, NL-6500 GL Nijmegen, Netherlands.
[O'Leary, Ryan M.] Univ Colorado, JILA, 440 UCB, Boulder, CO 80309 USA.
[O'Leary, Ryan M.] NIST, 440 UCB, Boulder, CO 80309 USA.
[Kramer, Michael] Univ Manchester, Jodrell Bank Ctr Astrophys, Manchester M13 9PL, Lancs, England.
[Rushton, Anthony P.] Univ Oxford, Dept Phys, Astrophys, Keble Rd, Oxford OX1 3RH, England.
[Rushton, Anthony P.] Univ Southampton, Sch Phys & Astron, Southampton SO17 1BJ, Hants, England.
[Doeleman, Sheperd] MIT, Haystack Observ, Route 40, Westford, MA 01886 USA.
[Doeleman, Sheperd; Reid, Mark J.] Harvard Smithsonian Ctr Astrophys, 60 Garden St, Cambridge, MA 02138 USA.
RP Bower, GC (reprint author), Acad Sinica, Inst Astron & Astrophys, 645 N Aohoku Pl, Hilo, HI 96720 USA.
EM gbower@asiaa.sinica.edu.tw
NR 1
TC 0
Z9 0
U1 2
U2 2
PU IOP PUBLISHING LTD
PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0004-637X
EI 1538-4357
J9 ASTROPHYS J
JI Astrophys. J.
PD APR 20
PY 2016
VL 821
IS 2
AR 133
DI 10.3847/0004-637X/821/2/133
PG 2
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA DN5JM
UT WOS:000377102700062
ER
PT J
AU Tang, WS
Matsuo, M
Wu, H
Stavila, V
Zhou, W
Talin, AA
Soloninin, AV
Skoryunov, RV
Babanova, OA
Skripov, AV
Unemoto, A
Orimo, SI
Udovic, TJ
AF Tang, Wan Si
Matsuo, Motoaki
Wu, Hui
Stavila, Vitalie
Zhou, Wei
Talin, Albert Alec
Soloninin, Alexei V.
Skoryunov, Roman V.
Babanova, Olga A.
Skripov, Alexander V.
Unemoto, Atsushi
Orimo, Shin-Ichi
Udovic, Terrence J.
TI Liquid-Like Ionic Conduction in Solid Lithium and Sodium
Monocarba-closo-Decaborates Near or at Room Temperature
SO ADVANCED ENERGY MATERIALS
LA English
DT Article
ID ANION REORIENTATIONS; SUPERIONIC CONDUCTION; NA2B12H12; PHASE;
LI2B12H12; LIBH4
C1 [Tang, Wan Si] Univ Maryland, Dept Mat Sci & Engn, College Pk, MD 20742 USA.
[Tang, Wan Si; Wu, Hui; Zhou, Wei; Udovic, Terrence J.] NIST, NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Matsuo, Motoaki; Orimo, Shin-Ichi] Tohoku Univ, Inst Mat Res, Sendai, Miyagi 9808577, Japan.
[Stavila, Vitalie; Talin, Albert Alec] Sandia Natl Labs, Energy Nanomat, Livermore, CA 94551 USA.
[Soloninin, Alexei V.; Skoryunov, Roman V.; Babanova, Olga A.; Skripov, Alexander V.] Russian Acad Sci, Ural Branch, Inst Met Phys, Ekaterinburg 620990, Russia.
[Unemoto, Atsushi; Orimo, Shin-Ichi] Tohoku Univ, WPI Adv Inst Mat Res, Sendai, Miyagi 9808577, Japan.
RP Tang, WS (reprint author), Univ Maryland, Dept Mat Sci & Engn, College Pk, MD 20742 USA.; Tang, WS; Udovic, TJ (reprint author), NIST, NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA.; Orimo, SI (reprint author), Tohoku Univ, Inst Mat Res, Sendai, Miyagi 9808577, Japan.; Orimo, SI (reprint author), Tohoku Univ, WPI Adv Inst Mat Res, Sendai, Miyagi 9808577, Japan.
EM wansi.tang@nist.gov; orimo@imr.tohoku.ac.jp; udovic@nist.gov
RI Babanova, Olga/J-4821-2013; Wu, Hui/C-6505-2008; Zhou, Wei/C-6504-2008;
ORIMO, Shin-ichi/A-4971-2011; Unemoto, Atsushi/D-3051-2013; Skripov,
Alexander/K-4525-2013; Soloninin, Alexey/J-8580-2013;
OI Babanova, Olga/0000-0002-2422-3263; Wu, Hui/0000-0003-0296-5204; Zhou,
Wei/0000-0002-5461-3617; ORIMO, Shin-ichi/0000-0002-4216-0446; Skripov,
Alexander/0000-0002-0610-5538; Soloninin, Alexey/0000-0001-7127-9641;
Skoryunov, Roman/0000-0001-6158-9056
FU Nanostructures for Electrical Energy Storage (NEES), an Energy Frontier
Research Center - US Department of Energy, Office of Science, Basic
Energy Sciences [DESC0001160]; Collaborative Research Center on Energy
Materials, Tohoku University; Advanced Low Carbon Technology Research
and Development Program (ALCA) from the Japan Science and Technology
Agency (JST); JSPS [25220911, 26820311]; Russian Federal Agency of
Scientific Organizations under Program "Spin" [01201463330]; Russian
Foundation for Basic Research [15-03-01114]; NSF [DMR-0944772]; US DOE
National Nuclear Security Administration [DE-AC04-94AL85000]
FX This work was performed, in part, in collaboration between members of
IEA HIA Task 32- Hydrogen-based Energy Storage. The authors gratefully
acknowledge support from the Nanostructures for Electrical Energy
Storage (NEES), an Energy Frontier Research Center funded by the US
Department of Energy, Office of Science, Basic Energy Sciences under
Award number DESC0001160; the Collaborative Research Center on Energy
Materials, Tohoku University; the Advanced Low Carbon Technology
Research and Development Program (ALCA) from the Japan Science and
Technology Agency (JST); JSPS KAKENHI under Grant Nos. 25220911 and
26820311; the Russian Federal Agency of Scientific Organizations under
Program "Spin" No. 01201463330; and the Russian Foundation for Basic
Research under Grant No. 15-03-01114. This work utilized facilities
supported in part by the NSF under Agreement No. DMR-0944772. Sandia is
a multi-program laboratory operated by Sandia Corporation, a Lockheed
Martin Company, for the US DOE National Nuclear Security Administration
under Contract DE-AC04-94AL85000.
NR 22
TC 11
Z9 11
U1 21
U2 40
PU WILEY-V C H VERLAG GMBH
PI WEINHEIM
PA POSTFACH 101161, 69451 WEINHEIM, GERMANY
SN 1614-6832
EI 1614-6840
J9 ADV ENERGY MATER
JI Adv. Energy Mater.
PD APR 20
PY 2016
VL 6
IS 8
AR 1502237
DI 10.1002/aenm.201502237
PG 6
WC Chemistry, Physical; Energy & Fuels; Materials Science,
Multidisciplinary; Physics, Applied; Physics, Condensed Matter
SC Chemistry; Energy & Fuels; Materials Science; Physics
GA DK1VU
UT WOS:000374703900011
ER
PT J
AU Coddington, I
Newbury, N
Swann, W
AF Coddington, Ian
Newbury, Nathan
Swann, William
TI Dual-comb spectroscopy
SO OPTICA
LA English
DT Review
ID FOURIER-TRANSFORM SPECTROSCOPY; OPTICAL PARAMETRIC OSCILLATOR;
MIDINFRARED FREQUENCY-COMB; TIME-DOMAIN SPECTROSCOPY; CONTINUOUS-WAVE
LASER; HIGH-RESOLUTION; FIBER LASER; TERAHERTZ SPECTROSCOPY; FEMTOSECOND
LASERS; RESOLVED MODES
AB Dual-comb spectroscopy is an emerging new spectroscopic tool that exploits the frequency resolution, frequency accuracy, broad bandwidth, and brightness of frequency combs for ultrahigh-resolution, high-sensitivity broadband spectroscopy. By using two coherent frequency combs, dual-comb spectroscopy allows a sample's spectral response to be measured on a comb tooth-by-tooth basis rapidly and without the size constraints or instrument response limitations of conventional spectrometers. This review describes dual-comb spectroscopy and summarizes the current state of the art. As frequency comb technology progresses, dual-comb spectroscopy will continue to mature and could surpass conventional broadband spectroscopy for a wide range of laboratory and field applications.
C1 [Coddington, Ian; Newbury, Nathan; Swann, William] NIST, 325 Broadway, Boulder, CO 80305 USA.
RP Coddington, I (reprint author), NIST, 325 Broadway, Boulder, CO 80305 USA.
EM ian.coddington@nist.gov; nathan.newbury@nist.gov
FU Defense Sciences Office, DARPA (DSO); Advanced Research Projects Agency
- Energy (ARPA-E); National Institute of Standards and Technology (NIST)
FX Defense Sciences Office, DARPA (DSO); Advanced Research Projects Agency
- Energy (ARPA-E); National Institute of Standards and Technology
(NIST).
NR 117
TC 24
Z9 24
U1 23
U2 49
PU OPTICAL SOC AMER
PI WASHINGTON
PA 2010 MASSACHUSETTS AVE NW, WASHINGTON, DC 20036 USA
SN 2334-2536
J9 OPTICA
JI Optica
PD APR 20
PY 2016
VL 3
IS 4
BP 414
EP 426
DI 10.1364/OPTICA.3.000414
PG 13
WC Optics
SC Optics
GA DK2MQ
UT WOS:000374749100012
ER
PT J
AU Loredo, JC
Zakaria, NA
Somaschi, N
Anton, C
de Santis, L
Giesz, V
Grange, T
Broome, MA
Gazzano, O
Coppola, G
Sagnes, I
Lemaitre, A
Auffeves, A
Senellart, P
Almeida, MP
White, AG
AF Loredo, Juan C.
Zakaria, Nor A.
Somaschi, Niccolo
Anton, Carlos
de Santis, Lorenzo
Giesz, Valerian
Grange, Thomas
Broome, Matthew A.
Gazzano, Olivier
Coppola, Guillaume
Sagnes, Isabelle
Lemaitre, Aristide
Auffeves, Alexia
Senellart, Pascale
Almeida, Marcelo P.
White, Andrew G.
TI Scalable performance in solid-state single-photon sources
SO OPTICA
LA English
DT Article
ID QUANTUM-DOT; ULTRABRIGHT SOURCE; INDISTINGUISHABILITY; DEVICE;
TELEPORTATION; MICROCAVITY; EMISSION
AB The desiderata for an ideal photon source are high brightness, high single-photon purity, and high indistinguishability. Defining brightness at the first collection lens, these properties have been simultaneously demonstrated with solid-state sources; however, absolute source efficiencies remain close to the 1% level and indistinguishability has only been demonstrated for photons emitted consecutively on the few-nanoseconds scale. Here, we employ deterministic quantum dot-micropillar devices to demonstrate solid-state single-photon sources with scalable performances. In one device, an absolute brightness at the output of a single-mode fiber of 14% and purities of 97.1%-99.0% are demonstrated. When nonresontantly excited, it emits a long stream of photons that exhibit indistinguishability up to 70%-above the classical limit of 50%-even after 33 consecutively emitted photons with a 400 ns separation between them. Resonant excitation in other devices results in near-optimal indistinguishability values: 96% at short timescales, remaining at 88% in timescales as large as 463 ns after 39 emitted photons. The performance attained by our devices brings solid-state sources into a regime suitable for scalable implementations. (C) 2016 Optical Society of America
C1 [Loredo, Juan C.; Zakaria, Nor A.; Broome, Matthew A.; Almeida, Marcelo P.; White, Andrew G.] Univ Queensland, Sch Math & Phys, Ctr Quantum Computat & Commun Technol, Ctr Engn Quantum Syst, Brisbane, Qld 4072, Australia.
[Somaschi, Niccolo; Anton, Carlos; de Santis, Lorenzo; Giesz, Valerian; Gazzano, Olivier; Coppola, Guillaume; Sagnes, Isabelle; Lemaitre, Aristide; Senellart, Pascale] Univ Paris Saclay, CNRS, LPN, F-91460 Marcoussis, France.
[de Santis, Lorenzo] Univ Paris Saclay, Univ Paris 11, F-91405 Orsay, France.
[Grange, Thomas; Auffeves, Alexia] Univ Grenoble Alpes, CNRS, Inst Neel, Nanophys & Semicond Grp, F-38000 Grenoble, France.
[Senellart, Pascale] Univ Paris Saclay, Ecole Polytech, Dept Phys, F-91128 Palaiseau, France.
[Broome, Matthew A.] Univ New S Wales, Sch Phys, Ctr Excellence Quantum Computat & Commun Technol, Sydney, NSW 2052, Australia.
[Gazzano, Olivier] Univ Maryland, NIST, Joint Quantum Inst, Gaithersburg, MD 20899 USA.
RP Loredo, JC (reprint author), Univ Queensland, Sch Math & Phys, Ctr Quantum Computat & Commun Technol, Ctr Engn Quantum Syst, Brisbane, Qld 4072, Australia.
EM juan.loredo1@gmail.com
RI Lemaitre, Aristide/B-9899-2009; Broome, Matthew/D-2560-2010; Loredo
Rosillo, Juan Carlos/M-8117-2016; SENELLART, Pascale/C-1771-2017;
OI Lemaitre, Aristide/0000-0003-1892-9726; Loredo Rosillo, Juan
Carlos/0000-0001-9117-1187; SENELLART, Pascale/0000-0002-8727-1086;
Anton, Carlos/0000-0002-9316-4340
FU Centre for Engineered Quantum Systems [CE110001013]; Centre for Quantum
Computation and Communication Technology [CE110001027]; Asian Office of
Aerospace Research and Development [FA2386-13-1-4070]; ARC Discovery
Early Career Research Award [DE120101899]; ERC Starting Grant [277885
QD-CQED]; French Agence Nationale pour la Recherche (ANR DELIGHT, ANR
USSEPP); French RENATECH network Labex NanoSaclay; European Union's
Seventh Framework Programme FP7 [618078 WASPS]
FX Centre for Engineered Quantum Systems (CE110001013); Centre for Quantum
Computation and Communication Technology (CE110001027); Asian Office of
Aerospace Research and Development (FA2386-13-1-4070); ARC Discovery
Early Career Research Award (DE120101899); ERC Starting Grant (277885
QD-CQED); French Agence Nationale pour la Recherche (ANR DELIGHT, ANR
USSEPP); French RENATECH network Labex NanoSaclay; European Union's
Seventh Framework Programme FP7 (618078 WASPS).
NR 48
TC 12
Z9 12
U1 9
U2 18
PU OPTICAL SOC AMER
PI WASHINGTON
PA 2010 MASSACHUSETTS AVE NW, WASHINGTON, DC 20036 USA
SN 2334-2536
J9 OPTICA
JI Optica
PD APR 20
PY 2016
VL 3
IS 4
BP 433
EP 440
DI 10.1364/OPTICA.3.000433
PG 8
WC Optics
SC Optics
GA DK2MQ
UT WOS:000374749100014
ER
PT J
AU Bergeron, H
Sinclair, LC
Swann, WC
Nelson, CW
Deschenes, JD
Baumann, E
Giorgetta, FR
Coddington, I
Newbury, NR
AF Bergeron, Hugo
Sinclair, Laura C.
Swann, William C.
Nelson, Craig W.
Deschenes, Jean-Daniel
Baumann, Esther
Giorgetta, Fabrizio R.
Coddington, Ian
Newbury, Nathan R.
TI Tight real-time synchronization of a microwave clock to an optical clock
across a turbulent air path
SO OPTICA
LA English
DT Article
ID CRYOCOOLED SAPPHIRE OSCILLATOR; BASE-LINE INTERFEROMETRY; LOW
PHASE-NOISE; FREQUENCY TRANSFER; FIBER; GENERATION; TRANSMISSION;
CANCELLATION; ATMOSPHERE
AB The ability to distribute the precise time and frequency from an optical clock to remote platforms could enable future precise navigation and sensing systems. Here, we demonstrate tight, real-time synchronization of a remote microwave clock to a master optical clock over a turbulent 4 km open-air path via optical two-way time-frequency transfer. Once synchronized, the 10 GHz frequency signals generated at each site agree to 10(-14) at 1 s and below 10(-17) at 1000 s. In addition, the two clock times are synchronized to +/- 13 fs over an 8-hour period. The ability to phase-synchronize 10 GHz signals across platforms supports future distributed coherent sensing, while the ability to time-synchronize multiple microwave-based clocks to a high-performance master optical clock supports future precision navigation/timing systems.
C1 [Bergeron, Hugo; Sinclair, Laura C.; Swann, William C.; Nelson, Craig W.; Deschenes, Jean-Daniel; Baumann, Esther; Giorgetta, Fabrizio R.; Coddington, Ian; Newbury, Nathan R.] NIST, 325 Broadway, Boulder, CO 80305 USA.
[Bergeron, Hugo; Deschenes, Jean-Daniel] Univ Laval, 2325 Rue Univ, Quebec City, PQ G1V 0A6, Canada.
RP Bergeron, H; Newbury, NR (reprint author), NIST, 325 Broadway, Boulder, CO 80305 USA.; Bergeron, H (reprint author), Univ Laval, 2325 Rue Univ, Quebec City, PQ G1V 0A6, Canada.
EM hugo.bergeron@nist.gov; nathan.newbury@nist.gov
FU National Institute of Standards and Technology (NIST); Defense Sciences
Office, DARPA (DSO)
FX National Institute of Standards and Technology (NIST); Defense Sciences
Office, DARPA (DSO).
NR 31
TC 1
Z9 1
U1 3
U2 6
PU OPTICAL SOC AMER
PI WASHINGTON
PA 2010 MASSACHUSETTS AVE NW, WASHINGTON, DC 20036 USA
SN 2334-2536
J9 OPTICA
JI Optica
PD APR 20
PY 2016
VL 3
IS 4
BP 441
EP 447
DI 10.1364/OPTICA.3.000441
PG 7
WC Optics
SC Optics
GA DK2MQ
UT WOS:000374749100015
ER
PT J
AU Chen, X
Harriger, L
Sefat, A
Birgeneau, RJ
Wilson, SD
AF Chen, Xiang
Harriger, Leland
Sefat, Athena
Birgeneau, R. J.
Wilson, Stephen D.
TI Strain-activated structural anisotropy in BaFe2As2
SO PHYSICAL REVIEW B
LA English
DT Article
ID IRON ARSENIDE SUPERCONDUCTOR; TRANSITION; ORDER
AB High-resolution single crystal neutron diffraction measurements are presented probing the magnetostructural response to uniaxial pressure in the iron pnictide parent system BaFe2As2. Scattering data reveal a strain-activated, anisotropic broadening of nuclear Bragg reflections, which increase upon cooling below the resolvable onset of global orthorhombicity. This anisotropy in lattice coherence continues to build until a lower temperature scale-the first-order onset of antiferromagnetism-is reached. Our data suggest that antiferromagnetism and strong magnetoelastic coupling drive the strain-activated lattice response in thismaterial and that the development of anisotropic lattice correlation lengths under strain is a possible origin for the high temperature transport anisotropy in this compound.
C1 [Chen, Xiang] Boston Coll, Dept Phys, Chestnut Hill, MA 02467 USA.
[Chen, Xiang; Wilson, Stephen D.] Univ Calif Santa Barbara, Dept Mat, Santa Barbara, CA 93106 USA.
[Harriger, Leland] NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Sefat, Athena] Oak Ridge Natl Lab, Div Mat Sci & Technol, POB 2008, Oak Ridge, TN 37831 USA.
[Birgeneau, R. J.] Univ Calif Berkeley, Dept Phys, Berkeley, CA 94720 USA.
[Birgeneau, R. J.] Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Div Mat Sci, Berkeley, CA 94720 USA.
[Birgeneau, R. J.] Univ Calif Berkeley, Dept Mat Sci, Berkeley, CA 94720 USA.
RP Wilson, SD (reprint author), Univ Calif Santa Barbara, Dept Mat, Santa Barbara, CA 93106 USA.
EM stephendwilson@engineering.ucsb.edu
RI Sefat, Athena/R-5457-2016
OI Sefat, Athena/0000-0002-5596-3504
FU NSF CAREER [DMR-1056625]; US Department of Energy (DOE), Office of Basic
Energy Sciences (BES), Materials Sciences and Engineering Division; US
Department of Energy (DOE), Office of Basic Energy Sciences, Materials
Science and Engineering Division [DE-AC02-05CH11231]
FX This work was supported by NSF CAREER Award DMR-1056625 (S.D.W.).
Partial support given by the US Department of Energy (DOE), Office of
Basic Energy Sciences (BES), Materials Sciences and Engineering Division
(A.S.). The work at Lawrence Berkeley National Laboratory was supported
by the US Department of Energy (DOE), Office of Basic Energy Sciences,
Materials Science and Engineering Division, under Contract No.
DE-AC02-05CH11231.
NR 27
TC 0
Z9 0
U1 1
U2 8
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 2469-9950
EI 2469-9969
J9 PHYS REV B
JI Phys. Rev. B
PD APR 20
PY 2016
VL 93
IS 14
AR 144118
DI 10.1103/PhysRevB.93.144118
PG 5
WC Physics, Condensed Matter
SC Physics
GA DJ9KD
UT WOS:000374531500003
ER
PT J
AU Dietz, TC
Tomaszewski, CE
Tsinas, Z
Poster, D
Barkatt, A
Adel-Hadadi, M
Bateman, FB
Cumberland, LT
Schneider, E
Gaskell, K
LaVerne, J
Al-Sheikhly, M
AF Dietz, Travis C.
Tomaszewski, Claire E.
Tsinas, Zois
Poster, Dianne
Barkatt, Aaron
Adel-Hadadi, Mohammad
Bateman, Fred B.
Cumberland, Lonnie T.
Schneider, Erich
Gaskell, Karen
LaVerne, Jay
Al-Sheikhly, Mohamad
TI Uranium Removal from Seawater by Means of Polyamide 6 Fibers Directly
Grafted with Diallyl Oxalate through a Single-Step, Solvent-Free
Irradiation Process
SO INDUSTRIAL & ENGINEERING CHEMISTRY RESEARCH
LA English
DT Article
ID URANYL; COMPLEXES; DIFFRACTION; CRYSTAL
AB To test the effectiveness of oxalate-based polymeric adsorbents in the recovery of uranium from seawater, diallyl oxalate (DAOx) was grafted onto polyamide 6 fabrics by exposing the fabric, immersed in pure liquid DAOx or in a surfactant-stabilized dispersion of DAOx in water, to electron beam or gamma radiation. After the fabrics were dried and weighed to determine the degree of grafting (DoG), the presence of oxalate in the fabrics was verified using XPS. Zeta potential measurements showed the fabric surfaces to be negatively charged. The fabrics were tested by rotating them for 7 days in a rotary agitator with actual seawater spiked with 0.2 or 1.0 mg.L-1 uranium. The fraction of uranium in the solution which was removed due to uptake on the fabrics was found to rise with increasing DoG at both uranium concentrations. EDS measurements were used to map the distribution of adsorbed uranium on the polymeric fibers.
C1 [Dietz, Travis C.; Tomaszewski, Claire E.; Al-Sheikhly, Mohamad] Univ Maryland, Dept Mat Sci & Engn, College Pk, MD 20742 USA.
[Tsinas, Zois] Univ Maryland, Dept Bioengn, College Pk, MD 20742 USA.
[Gaskell, Karen] Univ Maryland, Dept Chem, College Pk, MD 20742 USA.
[Poster, Dianne; Bateman, Fred B.; Cumberland, Lonnie T.] NIST, Gaithersburg, MD 20899 USA.
[Barkatt, Aaron; Adel-Hadadi, Mohammad] Catholic Univ, Dept Chem, Washington, DC 20064 USA.
[Schneider, Erich] Univ Texas Austin, Dept Nucl & Radiat Engn, Austin, TX 78712 USA.
[LaVerne, Jay] Univ Notre Dame, Dept Phys, Notre Dame, IN 46556 USA.
RP Al-Sheikhly, M (reprint author), Univ Maryland, Dept Mat Sci & Engn, College Pk, MD 20742 USA.
EM mohamad@cua.edu
FU USA Department of Energy Nuclear Energy University Program (NEUP)
[DE-NE0000723]
FX The authors are indebted to the USA Department of Energy Nuclear Energy
University Program (NEUP) for the financial support of this work through
Award No. DE-NE0000723. The authors acknowledge support of the Maryland
NanoCenter and its FabLab where the scanning electron microscopy with
energy dispersive X-ray spectroscopy was performed. The authors also
acknowledge the support of Tim Maugel with the Laboratory for Biological
Ultrastructure at the University of Maryland where scanning electron
microscopy was also performed. Certain commercial equipment,
instruments, or materials (or suppliers, or software, ... ) are
identified in this paper to foster understanding. Such identification
does not imply recommendation or endorsement by the National Institute
of Standards and Technology, nor does it imply that the materials or
equipment identified are necessarily the best available for the purpose.
NR 20
TC 0
Z9 0
U1 5
U2 8
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0888-5885
J9 IND ENG CHEM RES
JI Ind. Eng. Chem. Res.
PD APR 20
PY 2016
VL 55
IS 15
BP 4179
EP 4186
DI 10.1021/acs.iecr.5b03401
PG 8
WC Engineering, Chemical
SC Engineering
GA DK3JH
UT WOS:000374812400011
ER
PT J
AU Altman, RB
Prabhu, S
Sidow, A
Zook, JM
Goldfeder, R
Litwack, D
Ashley, E
Asimenos, G
Bustamante, CD
Donigan, K
Giacomini, KM
Johansen, E
Khuri, N
Lee, E
Liang, XS
Salit, M
Serang, O
Tezak, Z
Wall, DP
Mansfield, E
Kass-Hout, T
AF Altman, Russ B.
Prabhu, Snehit
Sidow, Arend
Zook, Justin M.
Goldfeder, Rachel
Litwack, David
Ashley, Euan
Asimenos, George
Bustamante, Carlos D.
Donigan, Katherine
Giacomini, Kathleen M.
Johansen, Elaine
Khuri, Natalia
Lee, Eunice
Liang, Xueying Sharon
Salit, Marc
Serang, Omar
Tezak, Zivana
Wall, Dennis P.
Mansfield, Elizabeth
Kass-Hout, Taha
TI A research roadmap for next-generation sequencing informatics
SO SCIENCE TRANSLATIONAL MEDICINE
LA English
DT Article
AB Next-generation sequencing technologies are fueling a wave of new diagnostic tests. Progress on a key set of nine research challenge areas will help generate the knowledge required to advance effectively these diagnostics to the clinic.
C1 [Altman, Russ B.] Stanford Univ, Bioengn Genet & Med, Stanford, CA 94305 USA.
[Prabhu, Snehit; Bustamante, Carlos D.] Stanford Univ, Biomed Data Sci & Genet, Stanford, CA 94305 USA.
[Sidow, Arend] Stanford Univ, Pathol & Genet, Stanford, CA 94305 USA.
[Zook, Justin M.; Salit, Marc] NIST, Mat Measurement Lab, Gaithersburg, MD 20899 USA.
[Goldfeder, Rachel] Stanford Univ, Biomed Informat, Stanford, CA 94305 USA.
[Litwack, David; Donigan, Katherine; Johansen, Elaine; Lee, Eunice; Liang, Xueying Sharon; Tezak, Zivana; Mansfield, Elizabeth; Kass-Hout, Taha] US FDA, Silver Spring, MD 20993 USA.
[Ashley, Euan] Stanford Univ, Med Genet & Pathol, Stanford, CA 94305 USA.
[Asimenos, George; Serang, Omar] DNAnexus, Mountain View, CA 94040 USA.
[Giacomini, Kathleen M.] Univ Calif San Francisco, Bioengn & Therapeut Sci, San Francisco, CA 94143 USA.
[Khuri, Natalia; Salit, Marc] Stanford Univ, Bioengn, Stanford, CA 94305 USA.
[Zook, Justin M.; Salit, Marc] Stanford Univ, NIST, Mat Measurement Lab, Stanford, CA 94305 USA.
[Wall, Dennis P.] Stanford Univ, Syst Med & Psychiat, Stanford, CA 94305 USA.
RP Altman, RB (reprint author), Stanford Univ, Bioengn Genet & Med, Stanford, CA 94305 USA.
EM russ.altman@stanford.edu
OI Kass-Hout, Taha/0000-0002-0123-5157
NR 2
TC 6
Z9 6
U1 1
U2 2
PU AMER ASSOC ADVANCEMENT SCIENCE
PI WASHINGTON
PA 1200 NEW YORK AVE, NW, WASHINGTON, DC 20005 USA
SN 1946-6234
EI 1946-6242
J9 SCI TRANSL MED
JI Sci. Transl. Med.
PD APR 20
PY 2016
VL 8
IS 335
AR 335ps10
DI 10.1126/scitranslmed.aaf7314
PG 4
WC Cell Biology; Medicine, Research & Experimental
SC Cell Biology; Research & Experimental Medicine
GA DJ7SM
UT WOS:000374412300003
PM 27099173
ER
PT J
AU Gruss, D
Velizhanin, KA
Zwolak, M
AF Gruss, Daniel
Velizhanin, Kirill A.
Zwolak, Michael
TI Landauer's formula with finite-time relaxation: Kramers' crossover in
electronic transport
SO SCIENTIFIC REPORTS
LA English
DT Article
ID FIELD-EFFECT TRANSISTOR; CARBON NANOTUBE; QUANTUM TRANSPORT; QUANTIZED
CONDUCTANCE; DEPENDENT TRANSPORT; POINT CONTACTS; SINGLE; DNA; SYSTEMS;
NUCLEOTIDES
AB Landauer's formula is the standard theoretical tool to examine ballistic transport in nano-and mesoscale junctions, but it necessitates that any variation of the junction with time must be slow compared to characteristic times of the system, e.g., the relaxation time of local excitations. Transport through structurally dynamic junctions is, however, increasingly of interest for sensing, harnessing fluctuations, and real-time control. Here, we calculate the steady-state current when relaxation of electrons in the reservoirs is present and demonstrate that it gives rise to three regimes of behavior: weak relaxation gives a contact-limited current; strong relaxation localizes electrons, distorting their natural dynamics and reducing the current; and in an intermediate regime the Landauer view of the system only is recovered. We also demonstrate that a simple equation of motion emerges, which is suitable for efficiently simulating time-dependent transport.
C1 [Gruss, Daniel; Zwolak, Michael] NIST, Ctr Nanoscale Sci & Technol, Gaithersburg, MD 20899 USA.
[Gruss, Daniel] Univ Maryland, Maryland Nanoctr, College Pk, MD 20742 USA.
[Gruss, Daniel] Oregon State Univ, Dept Phys, Corvallis, OR 97331 USA.
[Velizhanin, Kirill A.] Los Alamos Natl Lab, Div Theoret, Los Alamos, NM 87545 USA.
RP Zwolak, M (reprint author), NIST, Ctr Nanoscale Sci & Technol, Gaithersburg, MD 20899 USA.
EM mpz@nist.gov
RI Velizhanin, Kirill/C-4835-2008; Zwolak, Michael/G-2932-2013
OI Zwolak, Michael/0000-0001-6443-7816
FU University of Maryland [70NANB10H193]; National Institute of Standards
and Technology Center for Nanoscale Science and Technology through the
University of Maryland [70NANB10H193]; U.S. Department of Energy through
the LANL/LDRD Program
FX Daniel Gruss acknowledges support under the Cooperative Research
Agreement between the University of Maryland and the National Institute
of Standards and Technology Center for Nanoscale Science and Technology,
Award 70NANB10H193, through the University of Maryland. Kirill A.
Velizhanin was supported by the U.S. Department of Energy through the
LANL/LDRD Program.
NR 55
TC 0
Z9 0
U1 2
U2 7
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 2045-2322
J9 SCI REP-UK
JI Sci Rep
PD APR 20
PY 2016
VL 6
AR 24514
DI 10.1038/srep24514
PG 8
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DJ7JG
UT WOS:000374387100001
PM 27094206
ER
PT J
AU Schimmelrnann, A
Qi, HP
Coplen, TB
Brand, WA
Fong, J
Meier-Augenstein, W
Kemp, HF
Toman, B
Ackermann, A
Assonov, S
Aerts-Bijma, AT
Brejcha, R
Chikaraishi, Y
Darwish, T
Elsner, M
Gehre, M
Geilmann, H
Groing, M
Helie, JF
Herrero-Martin, S
Meijer, HAJ
Sauer, PE
Sessions, AL
Werner, RA
AF Schimmelrnann, Arndt
Qi, Haiping
Coplen, Tyler B.
Brand, Willi A.
Fong, Jon
Meier-Augenstein, Wolfram
Kemp, Helen F.
Toman, Blaza
Ackermann, Annika
Assonov, Sergey
Aerts-Bijma, Anita T.
Brejcha, Ramona
Chikaraishi, Yoshito
Darwish, Tamim
Elsner, Martin
Gehre, Matthias
Geilmann, Heike
Groeing, Manfred
Helie, Jean-Francois
Herrero-Martin, Sara
Meijer, Harro A. J.
Sauer, Peter E.
Sessions, Alex L.
Werner, Roland A.
TI Organic Reference Materials for Hydrogen, Carbon, and Nitrogen Stable
Isotope-Ratio Measurements: Caffeines, n-Alkanes, Fatty Acid Methyl
Esters, Glycines, L-Valines, Polyethylenes, and Oils
SO ANALYTICAL CHEMISTRY
LA English
DT Article
ID MASS-SPECTROMETRY; GAS-CHROMATOGRAPHY; DELTA-C-13; NORMALIZATION;
CALIBRATION; GUIDELINES; PRECISION; ABUNDANCE; CHROMIUM; OXYGEN
AB An international project developed, quality-tested, and determined isotope-delta values of 19 new organic reference materials (RMs) for hydrogen, carbon, and nitrogen stable isotope-ratio measurements, in addition to analyzing pre-existing RMs NBS 22 (oil), IAEA-CH-7 (polyethylene foil), and IAEA-600 (caffeine). These new RMs enable users to normalize measurements of samples to isotope-delta scales. The RMs span a range of delta H-2(VSMOW-SLAP) values from -210.8 to +397.0 mUr or parts per thousand, for delta C-13(VPDB-LSVEC) from -40.81 to +0.49 mUr and for delta N-15(Air) from -5.21 to +61.53 mUr. Many of the new RMs are amenable to gas and liquid chromatography. The RMs include triads of isotopically contrasting caffeines, C-16 n-alkanes, n-C-20-fatty acid methyl esters (FAMEs), glycines, and L-valines, together with polyethylene powder and string, one n-C-17-FAME, a vacuum oil (NBS 22a) to replace NBS 22 oil, and a H-2-enriched vacuum oil. A total of 11 laboratories from 7 countries used multiple analytical approaches and instrumentation for 2-point isotopic normalization against international primary measurement standards. The use of reference waters in silver tubes allowed direct normalization of delta H-2 values of organic materials against isotopic reference waters following the principle of identical treatment. Bayesian statistical analysis yielded the mean values reported here. New RMs are numbered from USGS61 through USGS78, in addition to NBS 22a. Because of exchangeable hydrogen, amino acid RMs currently are recommended only for carbon- and nitrogen-isotope measurements. Some amino acids contain C-13 and carbon-bound organic H-2-enrichments at different molecular sites to provide RMs for potential site-specific isotopic analysis in future studies.
C1 [Schimmelrnann, Arndt; Fong, Jon; Sauer, Peter E.] Indiana Univ, Dept Geol Sci, 1001 East 10th St, Bloomington, IN 47405 USA.
[Qi, Haiping; Coplen, Tyler B.] US Geol Survey, 431 Natl Ctr, Reston, VA 20192 USA.
[Brand, Willi A.; Geilmann, Heike] Max Planck Inst Biogeochem, Beutenberg Campus,POB 100164, D-07701 Jena, Germany.
[Meier-Augenstein, Wolfram; Kemp, Helen F.] James Hutton Inst, Stable Isotope Forens Lab, Dundee DD2 5DA, Scotland.
[Toman, Blaza] NIST, Informat Technol Lab, 100 Bur Dr,M-S 8980, Gaithersburg, MD 20899 USA.
[Ackermann, Annika; Werner, Roland A.] ETH, Inst Agrarwissensch, LFW C48-1,Univ Str 2, CH-8092 Zurich, Switzerland.
[Assonov, Sergey; Groeing, Manfred] IAEA, Dept Nucl Applicat, Environm Labs, Terr Environm Lab, A-1400 Vienna, Austria.
[Aerts-Bijma, Anita T.; Meijer, Harro A. J.] Univ Groningen, ESRIG, CIO, Nijenborgh 4, NL-9747 AG Groningen, Netherlands.
[Brejcha, Ramona; Elsner, Martin] Helmholtz Zentrum Munchen, Inst Grundwasserokol, Ingolstadter Landstr 1, D-85764 Neuherberg, Germany.
[Chikaraishi, Yoshito] Japan Agcy Marine Earth Sci & Technol JAMSTEC, Dept Biogeochem, 2-15 Natsushima Cho, Yokosuka, Kanagawa, Japan.
[Darwish, Tamim] Australian Nucl Sci & Technol Org, Natl Deuterat Facil, Locked Bag 2001, Kirrawee DC, NSW 2232, Australia.
[Gehre, Matthias; Meijer, Harro A. J.] Helmholtz Centre Environm Res UFZ, Dept Isotope Biogeochem, Permoserstr 15, D-04318 Leipzig, Germany.
[Helie, Jean-Francois] Univ Quebec, Ctr Rech GEOTOP, Dept Sci Terre & Atmosphere, Montreal, PQ H3C 3P8, Canada.
[Sessions, Alex L.] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA.
Robert Gordon Univ, Sch Pharm & Life Sci, Sir Ian Wood Bldg, Aberdeen AB10 7GJ, Scotland.
RP Schimmelrnann, A (reprint author), Indiana Univ, Dept Geol Sci, 1001 East 10th St, Bloomington, IN 47405 USA.
EM aschimme@indiana.edu
RI Elsner, Martin/J-4637-2012
OI Elsner, Martin/0000-0003-4746-9052
FU U.S. National Science Foundation [EAR-1052927]; National Collaborative
Research Infrastructure Strategy (NCRIS), an initiative of the
Australian Government; U.S. Geological Survey National Research Program
FX We are indebted to Marilyn Fogel, Libby Stern, and Michael Wieser for
assisting with the initiation of this project. Stefanie Poppenhager
(Amino GmbH, Frellstedt, Germany; www.amino.de) donated pure L-valine.
Tetyana Gilevska, Henk Jansen, Steffen Kummel, and Harald Lowag provided
analytical assistance. The manuscript benefited from constructive
reviews by L. I. Wassenaar, Linda Stalker, and two anonymous reviewers.
This project was supported by U.S. National Science Foundation Grant
EAR-1052927. The National Deuteration Facility is partly supported by
the National Collaborative Research Infrastructure Strategy (NCRIS), an
initiative of the Australian Government. The support of the U.S.
Geological Survey National Research Program made this report possible.
Any use of trade, firm, or product names is for descriptive purposes
only and does not imply endorsement by the U.S. Government.
NR 37
TC 5
Z9 5
U1 12
U2 32
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0003-2700
EI 1520-6882
J9 ANAL CHEM
JI Anal. Chem.
PD APR 19
PY 2016
VL 88
IS 8
BP 4294
EP 4302
DI 10.1021/acs.analchem.5b04392
PG 9
WC Chemistry, Analytical
SC Chemistry
GA DK1WP
UT WOS:000374706000020
PM 26974360
ER
PT J
AU Cox, LM
Killgore, JP
Li, ZW
Long, R
Sanders, AW
Xiao, JL
Ding, YF
AF Cox, Lewis M.
Killgore, Jason P.
Li, Zhengwei
Long, Rong
Sanders, Aric W.
Xiao, Jianliang
Ding, Yifu
TI Influences of Substrate Adhesion and Particle Size on the Shape Memory
Effect of Polystyrene Particles
SO LANGMUIR
LA English
DT Article
ID VOLUME PHASE-TRANSITION; POLYMER PARTICLES; SURFACE-ENERGY; ELASTIC
SOLIDS; NANOPARTICLES; DEFORMATION; FRICTION; FILMS; GELS; COMPRESSION
AB Formulations and applications of micro- and nanoscale polymer particles have proliferated rapidly in recent years, yet knowledge of their mechanical behavior has not grown accordingly. In this study, we examine the ways that compressive strain, substrate surface energy, and particle size influence the shape memory cycle of polystyrene particles. Using nanoimprint lithography, differently sized particles are programmed into highly deformed, temporary shapes in contact with substrates of differing surface energies. Atomic force microscopy is used to obtain in situ measurements of particle shape recovery kinetics, and scanning electron microscopy is employed to assess differences in the profiles of particles at the conclusion of the shape memory cycle. Finally, finite element models are used to investigate the growing impact of surface energies at smaller length scales. Results reveal that the influence of substrate adhesion on particle recovery is size-dependent and can become dominating at submicron length scales.
C1 [Cox, Lewis M.; Li, Zhengwei; Long, Rong; Xiao, Jianliang; Ding, Yifu] Univ Colorado, Dept Mech Engn, Boulder, CO 80309 USA.
[Ding, Yifu] Univ Colorado, Mat Sci & Engn Program, Boulder, CO 80309 USA.
[Killgore, Jason P.] Natl Inst Stand & Technol, Appl Chem & Mat Div, Boulder, CO 80305 USA.
[Sanders, Aric W.] Natl Inst Stand & Technol, Radio Frequency Technol Div, Boulder, CO 80305 USA.
RP Cox, LM; Ding, YF (reprint author), Univ Colorado, Dept Mech Engn, Boulder, CO 80309 USA.; Ding, YF (reprint author), Univ Colorado, Mat Sci & Engn Program, Boulder, CO 80309 USA.
EM lewis.cox@colorado.edu; yifu.ding@colorado.edu
RI Li, Zhengwei/D-4523-2014; Xiao, Jianliang/B-4535-2008
FU National Science Foundation [CMMI-1233626, CBET-1264276, EFRI-1038305]
FX We acknowledge funding support from the National Science Foundation
under grant number CMMI-1233626, CBET-1264276, and EFRI-1038305. Certain
commercial equipment, instruments, or materials are identified in this
paper to specify the experimental procedures adequately, such
identification does not imply recommendation or endorsement by NIST nor
does it imply that the materials or equipment identified are necessarily
the best available for the purpose.
NR 46
TC 3
Z9 3
U1 15
U2 30
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0743-7463
J9 LANGMUIR
JI Langmuir
PD APR 19
PY 2016
VL 32
IS 15
BP 3691
EP 3698
DI 10.1021/acs.langmuir.6b00588
PG 8
WC Chemistry, Multidisciplinary; Chemistry, Physical; Materials Science,
Multidisciplinary
SC Chemistry; Materials Science
GA DK1WV
UT WOS:000374706700016
PM 27023181
ER
PT J
AU Paul, S
Johnson, PR
Tiesinga, E
AF Paul, Saurabh
Johnson, P. R.
Tiesinga, Eite
TI Hubbard model for ultracold bosonic atoms interacting via
zero-point-energy-induced three-body interactions
SO PHYSICAL REVIEW A
LA English
DT Article
ID QUANTUM PHASE-TRANSITION; COLD ATOMS; FESHBACH RESONANCES; OPTICAL
LATTICES; COLLISIONS; GAS; SCATTERING; PHYSICS
AB We show that, for ultracold neutral bosonic atoms held in a three-dimensional periodic potential or optical lattice, a Hubbard model with dominant, attractive three-body interactions can be generated. In fact, we derive that the effect of pairwise interactions can be made small or zero starting from the realization that collisions occur at the zero-point energy of an optical lattice site and the strength of the interactions is energy dependent from effective-range contributions. We determine the strength of the two- and three-body interactions for scattering from van der Waals potentials and near Fano-Feshbach resonances. For van der Waals potentials, which for example describe scattering of alkaline-earth atoms, we find that the pairwise interaction can only be turned off for species with a small negative scattering length, leaving the Sr-88 isotope a possible candidate. Interestingly, for collisional magnetic Feshbach resonances this restriction does not apply and there often exist magnetic fields where the two-body interaction is small. We illustrate this result for several known narrow resonances between alkali-metal atoms as well as chromium atoms. Finally, we compare the size of the three-body interaction with hopping rates and describe limits due to three-body recombination.
C1 [Paul, Saurabh] Univ Maryland, Ctr Quantum Informat & Comp Sci, College Pk, MD 20742 USA.
[Paul, Saurabh] Univ Maryland, Joint Quantum Inst, College Pk, MD 20742 USA.
[Johnson, P. R.] Amer Univ, Dept Phys, Washington, DC 20016 USA.
[Tiesinga, Eite] NIST, Joint Quantum Inst, Gaithersburg, MD 20899 USA.
[Tiesinga, Eite] NIST, Ctr Quantum Informat & Comp Sci, Gaithersburg, MD 20899 USA.
[Tiesinga, Eite] Univ Maryland, Gaithersburg, MD 20899 USA.
RP Paul, S (reprint author), Univ Maryland, Ctr Quantum Informat & Comp Sci, College Pk, MD 20742 USA.; Paul, S (reprint author), Univ Maryland, Joint Quantum Inst, College Pk, MD 20742 USA.
FU National Science Foundation [PHY-1506343]
FX This work has been supported by the National Science Foundation Grant
No. PHY-1506343.
NR 65
TC 1
Z9 1
U1 9
U2 9
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 2469-9926
EI 2469-9934
J9 PHYS REV A
JI Phys. Rev. A
PD APR 19
PY 2016
VL 93
IS 4
AR 043616
DI 10.1103/PhysRevA.93.043616
PG 7
WC Optics; Physics, Atomic, Molecular & Chemical
SC Optics; Physics
GA DJ9FR
UT WOS:000374519900003
ER
PT J
AU Isaak, DJ
Young, MK
Luce, CH
Hostetler, SW
Wenger, SJ
Peterson, EE
Hoef, JMV
Groce, MC
Horan, DL
Nagel, DE
AF Isaak, Daniel J.
Young, Michael K.
Luce, Charles H.
Hostetler, Steven W.
Wenger, Seth J.
Peterson, Erin E.
Hoef, Jay M. Ver
Groce, Matthew C.
Horan, Dona L.
Nagel, David E.
TI Slow climate velocities of mountain streams portend their role as
refugia for cold-water biodiversity
SO PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF
AMERICA
LA English
DT Article
DE climate refugia; climate velocity; biodiversity; fish; network
ID CUTTHROAT TROUT; THERMAL SENSITIVITY; AIR-TEMPERATURE; BROOK TROUT;
NETWORKS; HABITAT; FISHES; POPULATIONS; PERSISTENCE; TELEOSTEI
AB The imminent demise of montane species is a recurrent theme in the climate change literature, particularly for aquatic species that are constrained to networks and elevational rather than latitudinal retreat as temperatures increase. Predictions of widespread species losses, however, have yet to be fulfilled despite decades of climate change, suggesting that trends are much weaker than anticipated and may be too subtle for detection given the widespread use of sparse water temperature datasets or imprecise surrogates like elevation and air temperature. Through application of large water-temperature databases evaluated for sensitivity to historical air-temperature variability and computationally interpolated to provide high-resolution thermal habitat information for a 222,000-km network, we estimate a less dire thermal plight for cold-water species within mountains of the northwestern United States. Stream warming rates and climate velocities were both relatively low for 1968-2011 (average warming rate = 0.101 degrees C/ decade; median velocity = 1.07 km/decade) when air temperatures warmed at 0.21 degrees C/decade. Many cold-water vertebrate species occurred in a subset of the network characterized by low climate velocities, and three native species of conservation concern occurred in extremely cold, slow velocity environments (0.33-0.48 km/decade). Examination of aggressive warming scenarios indicated that although network climate velocities could increase, they remain low in headwaters because of strong local temperature gradients associated with topographic controls. Better information about changing hydrology and disturbance regimes is needed to complement these results, but rather than being climatic cul-de-sacs, many mountain streams appear poised to be redoubts for cold-water biodiversity this century.
C1 [Isaak, Daniel J.; Luce, Charles H.; Groce, Matthew C.; Horan, Dona L.; Nagel, David E.] US Forest Serv, Rocky Mt Res Stn, Boise, ID 83702 USA.
[Young, Michael K.] US Forest Serv, Rocky Mt Res Stn, Missoula, MT 59801 USA.
[Hostetler, Steven W.] US Geol Survey, Corvallis, OR 97331 USA.
[Wenger, Seth J.] Univ Georgia, River Basins Ctr, Athens, GA 30602 USA.
[Peterson, Erin E.] Queensland Univ Technol, Australian Res Council, Ctr Excellence Math & Stat Frontiers, Brisbane, Qld 4000, Australia.
[Peterson, Erin E.] Queensland Univ Technol, Inst Future Environm, Brisbane, Qld 4000, Australia.
[Hoef, Jay M. Ver] NOAA, Natl Marine Fisheries Serv, Alaska Fisheries Sci Ctr, Natl Marine Mammal Lab, Seattle, WA 98112 USA.
RP Isaak, DJ (reprint author), US Forest Serv, Rocky Mt Res Stn, Boise, ID 83702 USA.
EM disaak@fs.fed.us
RI Luce, Charles/A-9267-2008;
OI Luce, Charles/0000-0002-6938-9662; Peterson, Erin/0000-0003-2992-0372;
Ver Hoef, Jay/0000-0003-4302-6895
FU US Forest Service Rocky Mountain Research Station; US Fish and Wildlife
Service's Great Northern; North Pacific Landscape Conservation
Cooperatives
FX This research was supported by the US Forest Service Rocky Mountain
Research Station and grants from the US Fish and Wildlife Service's
Great Northern and North Pacific Landscape Conservation Cooperatives.
NR 54
TC 8
Z9 8
U1 14
U2 24
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 APR 19
PY 2016
VL 113
IS 16
BP 4374
EP 4379
DI 10.1073/pnas.1522429113
PG 6
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DJ7LV
UT WOS:000374393800048
PM 27044091
ER
PT J
AU Paez, E
Arnold, KJ
Hajiyev, E
Porsev, SG
Dzuba, VA
Safronova, UI
Safronova, MS
Barrett, MD
AF Paez, Eduardo
Arnold, K. J.
Hajiyev, Elnur
Porsev, S. G.
Dzuba, V. A.
Safronova, U. I.
Safronova, M. S.
Barrett, M. D.
TI Atomic properties of Lu+
SO PHYSICAL REVIEW A
LA English
DT Article
ID OPTICAL LATTICE CLOCK; PERTURBATION-THEORY; SPECTROSCOPY; UNCERTAINTY;
MOMENTS; ION
AB Singly ionized lutetium has recently been suggested as a potential clock candidate. Here we report a joint experimental and theoretical investigation of Lu+. Measurements relevant to practical clock operation are made and compared to atomic structure calculations. Calculations of scalar and tensor polarizabilities for clock states over a range of wavelengths are also given. These results will be useful for future work with this clock candidate.
C1 [Paez, Eduardo; Arnold, K. J.; Hajiyev, Elnur; Barrett, M. D.] Ctr Quantum Technol, 3 Sci Dr 2, Singapore 117543, Singapore.
[Paez, Eduardo; Arnold, K. J.; Hajiyev, Elnur; Barrett, M. D.] Natl Univ Singapore, Dept Phys, 2 Sci Dr 3, Singapore 117551, Singapore.
[Porsev, S. G.; Safronova, M. S.] Univ Delaware, Dept Phys & Astron, Newark, DC 19716 USA.
[Porsev, S. G.] Petersburg Nucl Phys Inst, Gatchina 188300, Leningrad Distr, Russia.
[Dzuba, V. A.] Univ New S Wales, Sch Phys, Sydney, NSW 2052, Australia.
[Safronova, U. I.] Univ Nevada, Dept Phys, Reno, NV 89557 USA.
[Safronova, M. S.] NIST, Joint Quantum Inst, College Pk, MD 20742 USA.
[Safronova, M. S.] Univ Maryland, College Pk, MD 20742 USA.
RP Barrett, MD (reprint author), Ctr Quantum Technol, 3 Sci Dr 2, Singapore 117543, Singapore.; Barrett, MD (reprint author), Natl Univ Singapore, Dept Phys, 2 Sci Dr 3, Singapore 117551, Singapore.
EM phybmd@nus.edu.sg
RI Barrett, Murray/G-2732-2012;
OI Arnold, Kyle/0000-0003-3544-8246
FU National Research Foundation; Ministry of Education, Singapore under the
Research Centres of Excellence programme; U.S. NSF Grant [PHY-1520993];
Australian Research Council; Prime Minister's Office, Singapore
FX This research is supported by the National Research Foundation, Prime
Minister's Office, Singapore and the Ministry of Education, Singapore
under the Research Centres of Excellence programme. This work was
supported in part by U.S. NSF Grant No. PHY-1520993 and the Australian
Research Council.
NR 29
TC 4
Z9 4
U1 3
U2 6
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 2469-9926
EI 2469-9934
J9 PHYS REV A
JI Phys. Rev. A
PD APR 18
PY 2016
VL 93
IS 4
AR 042112
DI 10.1103/PhysRevA.93.042112
PG 11
WC Optics; Physics, Atomic, Molecular & Chemical
SC Optics; Physics
GA DJ9FM
UT WOS:000374519400003
ER
PT J
AU Bagwell, CE
Abernathy, A
Barnwell, R
Milliken, CE
Noble, PA
Dale, T
Beauchesne, KR
Moeller, PDR
AF Bagwell, Christopher E.
Abernathy, Amanda
Barnwell, Remy
Milliken, Charles E.
Noble, Peter A.
Dale, Taraka
Beauchesne, Kevin R.
Moeller, Peter D. R.
TI Discovery of Bioactive Metabolites in Biofuel Microalgae That Offer
Protection against Predatory Bacteria
SO FRONTIERS IN MICROBIOLOGY
LA English
DT Article
DE microalgae; bioactive metabolites; iron; crop protection; predation
ID MARINE CHEMICAL ECOLOGY; PREVENT POND CRASHES; HARMFUL ALGAL BLOOMS;
FRESH-WATER; CHLORELLA-VULGARIS; PRYMNESIUM-PARVUM; SECONDARY
METABOLITES; GROWTH-RATE; GREEN-ALGA; IRON
AB Microalgae could become an important resource for addressing increasing global demand for food, energy, and commodities while helping to reduce atmospheric greenhouse gasses. Even though Chlorophytes are generally regarded safe for human consumption, there is still much we do not understand about the metabolic and biochemical potential of microscopic algae. The aim of this study was to evaluate biofuel candidate strains of Chlorella and Scenedesmus for the potential to produce bioactive metabolites when grown under nutrient depletion regimes intended to stimulate production of triacylglycerides. Strain specific combinations of macro- and micro nutrient restricted growth media did stimulate neutral lipid accumulation by microalgal cultures. However, cultures that were restricted for iron consistently and reliably tested positive for cytotoxicity by in vivo bioassays. The addition of iron back to these cultures resulted in the disappearance of the bioactive components by LC/MS fingerprinting and loss of cytotoxicity by in vivo bioassay. Incomplete NMR characterization of the most abundant cytotoxic fractions suggested that small molecular weight peptides and glycosides could be responsible for Chlorella cytotoxicity. Experiments were conducted to determine if the bioactive metabolites induced by Fe-limitation in Chlorella sp. cultures would elicit protection against Vampirovibrio chlorellavorus, an obligate predator of Chlorella. Introduction of V chlorellavorus resulted in a 72% decrease in algal biomass in the experimental controls after 7 days. Conversely, only slight losses of algal biomass were measured for the iron limited Chlorella cultures (0-9%). This study demonstrates a causal linkage between iron bioavailability and bioactive metabolite production in strains of Chlorella and Scenedesmus. Further study of this phenomenon could contribute to the development of new strategies to extend algal production cycles in open, outdoor systems while ensuring the protection of biomass from predatory losses.
C1 [Bagwell, Christopher E.; Abernathy, Amanda; Barnwell, Remy; Milliken, Charles E.] Savannah River Natl Lab, Environm Sci & Biotechnol, Aiken, SC USA.
[Noble, Peter A.] Alabama State Univ, Dept Biol Sci, Montgomery, AL 36101 USA.
[Dale, Taraka] Los Alamos Natl Lab, Biosci Div, Los Alamos, NM USA.
[Beauchesne, Kevin R.; Moeller, Peter D. R.] NOAA, Natl Ctr Coastal Ocean Sci, Ctr Human Hlth Res, Hollings Marine Lab, Charleston, SC USA.
RP Bagwell, CE (reprint author), Savannah River Natl Lab, Environm Sci & Biotechnol, Aiken, SC USA.
EM christopher.bagwell@srnl.doe.gov
OI Noble, Peter/0000-0002-6013-2588
FU SRNL's Laboratory Directed Research and Development Program; U.S.
Department of Energy, Office of Energy Efficiency and Renewable Energy,
Biomass Program [DE-NL0022905]
FX This research was jointly supported by the SRNL's Laboratory Directed
Research and Development Program and the U.S. Department of Energy,
Office of Energy Efficiency and Renewable Energy, Biomass Program (Award
# DE-NL0022905).
NR 74
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U1 12
U2 31
PU FRONTIERS MEDIA SA
PI LAUSANNE
PA PO BOX 110, EPFL INNOVATION PARK, BUILDING I, LAUSANNE, 1015,
SWITZERLAND
SN 1664-302X
J9 FRONT MICROBIOL
JI Front. Microbiol.
PD APR 18
PY 2016
VL 7
AR 516
DI 10.3389/fmicb.2016.00516
PG 12
WC Microbiology
SC Microbiology
GA DJ5SS
UT WOS:000374271000001
PM 27148205
ER
PT J
AU Williams, NL
Juranek, LW
Johnson, KS
Feely, RA
Riser, SC
Talley, LD
Russell, JL
Sarmiento, JL
Wanninkhof, R
AF Williams, N. L.
Juranek, L. W.
Johnson, K. S.
Feely, R. A.
Riser, S. C.
Talley, L. D.
Russell, J. L.
Sarmiento, J. L.
Wanninkhof, R.
TI Empirical algorithms to estimate water column pH in the Southern Ocean
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID ANTHROPOGENIC CARBON; SEAWATER; CO2; ACIDIFICATION; ALKALINITY
AB Empirical algorithms are developed using high-quality GO-SHIP hydrographic measurements of commonly measured parameters (temperature, salinity, pressure, nitrate, and oxygen) that estimate pH in the Pacific sector of the Southern Ocean. The coefficients of determination, R-2, are 0.98 for pH from nitrate (pH(N)) and 0.97 for pH from oxygen (pH(Ox)) with RMS errors of 0.010 and 0.008, respectively. These algorithms are applied to Southern Ocean Carbon and Climate Observations and Modeling (SOCCOM) biogeochemical profiling floats, which include novel sensors (pH, nitrate, oxygen, fluorescence, and backscatter). These algorithms are used to estimate pH on floats with no pH sensors and to validate and adjust pH sensor data from floats with pH sensors. The adjusted float data provide, for the first time, seasonal cycles in surface pH on weekly resolution that range from 0.05 to 0.08 on weekly resolution for the Pacific sector of the Southern Ocean.
C1 [Williams, N. L.; Juranek, L. W.] Oregon State Univ, Coll Earth Ocean & Atmospher Sci, Corvallis, OR 97331 USA.
[Johnson, K. S.] Monterey Bay Aquarium Res Inst, Moss Landing, CA USA.
[Feely, R. A.] NOAA, Pacific Marine Environm Lab, 7600 Sand Point Way Ne, Seattle, WA 98115 USA.
[Riser, S. C.] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA.
[Talley, L. D.] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA.
[Russell, J. L.] Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA.
[Sarmiento, J. L.] Princeton Univ, Program Atmospher & Ocean Sci, Princeton, NJ 08544 USA.
[Wanninkhof, R.] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
RP Williams, NL (reprint author), Oregon State Univ, Coll Earth Ocean & Atmospher Sci, Corvallis, OR 97331 USA.
EM nancy.williams@oregonstate.edu
RI Johnson, Kenneth/F-9742-2011; Williams, Nancy/I-3472-2015
OI Johnson, Kenneth/0000-0001-5513-5584; Williams,
Nancy/0000-0002-6541-9385
FU U.S. National Science Foundation's Southern Ocean Carbon and Climate
Observations and Modeling (SOCCOM) Project under the NSF Award
[PLR-1425989]; U.S. Argo through NOAA/JISAO grant [NA17RJ1232]; ARCS
Foundation Portland Chapter
FX The measurement methods, calibration, and quality control for all
discrete bottle data used in this study are available at
http://cchdo.ucsd.edu, and all SOCCOM float data are available at
http://soccom.princeton.edu/soccomviz.php. This work was sponsored by
the U.S. National Science Foundation's Southern Ocean Carbon and Climate
Observations and Modeling (SOCCOM) Project under the NSF Award
PLR-1425989. Logistical support for this project in Antarctic waters was
provided by the U.S. National Science Foundation through the U.S.
Antarctic Program. Additionally, we acknowledge support from U.S. Argo
through NOAA/JISAO grant NA17RJ1232 to the University of Washington.
Nancy Williams is also supported by the ARCS Foundation Portland
Chapter. This is PMEL contribution 4417.
NR 37
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U1 5
U2 10
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 APR 16
PY 2016
VL 43
IS 7
BP 3415
EP 3422
DI 10.1002/2016GL068539
PG 8
WC Geosciences, Multidisciplinary
SC Geology
GA DL3MG
UT WOS:000375537300048
ER
PT J
AU Lopez, H
Kirtman, B
AF Lopez, Hosmay
Kirtman, Ben P.
TI Investigating the seasonal predictability of significant wave height in
the West Pacific and Indian Oceans
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID TROPICAL CYCLONES; WIND-WAVES; VARIABILITY; CLIMATE; LAYER; NCEP
AB This study investigates seasonal prediction skill of significant wave height (SWH) in the West Pacific and Indian Oceans. We forced the WAVEWATCH III model with 10m winds from the National Centers for Environmental Prediction Reanalysis-2 and from the Community Climate System Model version 4 North American Multi-Model Ensemble retrospective forecasts for the period of January 1979 to December 2013. Results indicate potential for predicting SWH with several months lead time during boreal summers after the warm phase of El Nino-Southern Oscillation (ENSO) measured by deterministic and probabilistic skill scores in the Northwest Pacific and Bay of Bengal. During these summers, SWH is smaller than normal due to reduced atmospheric synoptic activity associated with an anomalously anticyclone in the western Pacific, leading to larger signal-to-noise ratio in the 10m winds, hence increasing SWH prediction skill. It is shown that ENSO has a nonlinear influence on the number of extremely large SWH events, with reduced number of extreme occurrences during boreal summers after the warm phase of ENSO.
C1 [Lopez, Hosmay] Univ Miami, Cooperat Inst Marine & Atmospher Studies, Coral Gables, FL 33124 USA.
[Lopez, Hosmay] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
[Kirtman, Ben P.] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Coral Gables, FL 33124 USA.
RP Lopez, H (reprint author), Univ Miami, Cooperat Inst Marine & Atmospher Studies, Coral Gables, FL 33124 USA.; Lopez, H (reprint author), NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
EM hlopez@rsmas.miami.edu
RI Lopez, Hosmay/M-3278-2015
FU ONR award [N000141310439]; NOAA awards [NA15OAR4320064, NA12OAR4310089]
FX We would like to acknowledge the three anonymous reviewers for their
insightful comments. Data can be obtained upon request by contacting the
corresponding author at hlopez@rsmas.miami.edu. The authors acknowledge
support from ONR award N000141310439 and NOAA awards NA15OAR4320064 and
NA12OAR4310089.
NR 25
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U1 1
U2 4
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 APR 16
PY 2016
VL 43
IS 7
BP 3451
EP 3458
DI 10.1002/2016GL068653
PG 8
WC Geosciences, Multidisciplinary
SC Geology
GA DL3MG
UT WOS:000375537300053
ER
PT J
AU Schnell, JL
Prather, MJ
Josse, B
Naik, V
Horowitz, LW
Zeng, G
Shindell, DT
Faluvegi, G
AF Schnell, Jordan L.
Prather, Michael J.
Josse, Beatrice
Naik, Vaishali
Horowitz, Larry W.
Zeng, Guang
Shindell, Drew T.
Faluvegi, Greg
TI Effect of climate change on surface ozone over North America, Europe,
and East Asia
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
ID INTERCOMPARISON PROJECT ACCMIP; REGIONAL AIR-POLLUTION; UNITED-STATES;
ATMOSPHERIC CHEMISTRY; TROPOSPHERIC OZONE; FUTURE CLIMATE; EMISSIONS
CHANGES; SUMMERTIME OZONE; MODEL; QUALITY
AB The effect of future climate change on surface ozone over North America, Europe, and East Asia is evaluated using present-day (2000s) and future (2100s) hourly surface ozone simulated by four global models. Future climate follows RCP8.5, while methane and anthropogenic ozone precursors are fixed at year 2000 levels. Climate change shifts the seasonal surface ozone peak to earlier in the year and increases the amplitude of the annual cycle. Increases in mean summertime and high-percentile ozone are generally found in polluted environments, while decreases are found in clean environments. We propose that climate change augments the efficiency of precursor emissions to generate surface ozone in polluted regions, thus reducing precursor export to neighboring downwind locations. Even with constant biogenic emissions, climate change causes the largest ozone increases at high percentiles. In most cases, air quality extreme episodes become larger and contain higher ozone levels relative to the rest of the distribution.
C1 [Schnell, Jordan L.; Prather, Michael J.] Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA USA.
[Josse, Beatrice] CNRS, Ctr Natl Rech Meteorol, Meteo France, GAME CNRM, Toulouse, France.
[Naik, Vaishali] NOAA, UCAR, Geophys Fluid Dynam Lab, Princeton, NJ USA.
[Horowitz, Larry W.] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA.
[Zeng, Guang] Natl Inst Water & Atmospher Res, Lauder, New Zealand.
[Shindell, Drew T.] Duke Univ, Nicholas Sch Environm, Durham, NC 27708 USA.
[Faluvegi, Greg] Columbia Univ, NASA, Goddard Inst Space Studies, New York, NY USA.
[Faluvegi, Greg] Columbia Univ, Columbia Earth Inst, New York, NY USA.
RP Schnell, JL (reprint author), Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA USA.
EM jschnell@uci.edu
RI Naik, Vaishali/A-4938-2013
OI Naik, Vaishali/0000-0002-2254-1700
FU NASA [NNX09AJ47G, NNX13AL12G, NNX15AE35G]; DOE [DE-SC0007021]; National
Science Foundation's Graduate Research Fellowship Program [DGE-1321846];
NeSI's collaborator institutions; Ministry of Business, Innovation and
Employment's Research Infrastructure Programme
FX Research at UCI was supported by NASA grants NNX09AJ47G, NNX13AL12G, and
NNX15AE35G and DOE award DE-SC0007021. J.L. Schnell was supported by the
National Science Foundation's Graduate Research Fellowship Program
(DGE-1321846). G. Zeng acknowledges the use of New Zealand's national
HPC facilities that are provided by the NZ eScience Infrastructure and
funded jointly by NeSI's collaborator institutions and through the
Ministry of Business, Innovation and Employment's Research
Infrastructure Programme. We are grateful to the British Atmospheric
Data Centre (BADC), which is part of the NERC National Centre for
Atmospheric Science (NCAS), for collecting and archiving the ACCMIP
data. The hourly ACCMIP data at the models' native resolutions can be
obtained at http://badc.nerc.ac.uk, while the remapped MDA8 ozone data
can be obtained by contacting the corresponding author.
NR 44
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U1 11
U2 17
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 APR 16
PY 2016
VL 43
IS 7
BP 3509
EP 3518
DI 10.1002/2016GL068060
PG 10
WC Geosciences, Multidisciplinary
SC Geology
GA DL3MG
UT WOS:000375537300060
ER
PT J
AU Pu, B
Dickinson, RE
Fu, R
AF Pu, Bing
Dickinson, Robert E.
Fu, Rong
TI Dynamical connection between Great Plains low-level winds and
variability of central Gulf States precipitation
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
DE Great Plains low-level jet; summer precipitation; central Gulf States
ID SOUTHEASTERN UNITED-STATES; AMERICAN REGIONAL REANALYSIS; SUMMER
RAINFALL VARIABILITY; MOISTURE TRANSPORT; WATER-BALANCE; JET; DROUGHT;
INTENSIFICATION; EVOLUTION; IMPACTS
AB The Great Plains low-level jet has been related to summer precipitation over the northern Great Plains and Midwest through its moisture transport and convergence at the jet exit area. Much less studied has been its negative relationship with precipitation over the southern Great Plains and the Gulf coastal area. This work shows that the southerly low-level winds at 30 degrees-40 degrees N over the southern Great Plains are significantly correlated with anticyclonic vorticity to its east over the central Gulf States (30 degrees-35 degrees N, 85 degrees-95 degrees W) from May to July. When the low-level jet is strong in June and July, anomalous anticyclonic vorticity over the central Gulf States leads to divergence and consequent subsidence suppressing precipitation over that region. In contrast, an enhanced southerly flow at the entrance region of the jet over the Gulf of Mexico, largely uncorrelated with the meridional wind over the southern Great Plains, is correlated with increased precipitation over the central Gulf States. Precipitation is large over the central Gulf States when the meridional wind over the southern Great Plains is weakest and over the Gulf of Mexico is strongest. This increase is consistent with the increased moisture transport and dynamic balance between loss of vorticity by advection and friction and gain by convergence.
C1 [Pu, Bing; Dickinson, Robert E.; Fu, Rong] Univ Texas Austin, Dept Geol Sci, Jackson Sch Geosci, Austin, TX USA.
[Pu, Bing] Princeton Univ, Geophys Fluid Dynam Lab, Atmospher & Ocean Sci, NOAA, Princeton, NJ 08544 USA.
RP Pu, B (reprint author), Univ Texas Austin, Dept Geol Sci, Jackson Sch Geosci, Austin, TX USA.; Pu, B (reprint author), Princeton Univ, Geophys Fluid Dynam Lab, Atmospher & Ocean Sci, NOAA, Princeton, NJ 08544 USA.
EM bing.pu@noaa.gov
FU U.S. Department of Energy DOE [DE-FG02-09ER64746]; NASA [NNX13AN39G];
NOAA's Climate Program Office's Modeling, Analysis, Predictions, and
Projections Program [NA10OAR4310157]
FX We thank the three anonymous reviewers for their extremely thorough and
constructive comments that lead to substantial improvement of this work.
The North American Regional Reanalysis used in this paper is available
to download from
http://www.esrl.noaa.gov/psd/data/gridded/data.narr.html. This work was
supported by a grant from the U.S. Department of Energy DOE
(DE-FG02-09ER64746), the NASA Indicators for the National Climate
Assessment Program (grant NNX13AN39G), and NOAA's Climate Program
Office's Modeling, Analysis, Predictions, and Projections Program (grant
award NA10OAR4310157).
NR 25
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U1 2
U2 3
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 APR 16
PY 2016
VL 121
IS 7
BP 3421
EP 3434
DI 10.1002/2015JD024045
PG 14
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DK7QG
UT WOS:000375120200021
ER
PT J
AU Ge, C
Wang, J
Carn, S
Yang, K
Ginoux, P
Krotkov, N
AF Ge, Cui
Wang, Jun
Carn, Simon
Yang, Kai
Ginoux, Paul
Krotkov, Nickolay
TI Satellite-based global volcanic SO2 emissions and sulfate direct
radiative forcing during 2005-2012
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
DE OMI SO2; volcanic sulfate aerosols; direct radiative forcing; injection
height; volcanic emission inventory; volcanic degassing
ID OZONE MONITORING INSTRUMENT; SULFUR-DIOXIDE EMISSIONS; SIERRA-NEGRA
VOLCANO; 2005 ERUPTION; EAST-ASIA; AEROSOL; CLIMATE; OMI; CLOUDS; MODEL
AB An 8year volcanic SO2 emission inventory for 2005-2012 is obtained based on satellite measurements of SO2 from OMI (Ozone Monitoring Instrument) and ancillary information from the Global Volcanism Program. It includes contributions from global volcanic eruptions and from eight persistently degassing volcanoes in the tropics. It shows significant differences in the estimate of SO2 amount and injection height for medium to large volcanic eruptions as compared to the counterparts in the existing volcanic SO2 database. Emissions from Nyamuragira (DR Congo) in November 2006 and Grimsvotn (Iceland) in May 2011 that were not included in the Intergovernmental Panel on Climate Change 5 (IPCC) inventory are included here. Using the updated emissions, the volcanic sulfate (SO42-) distribution is simulated with the global transport model Goddard Earth Observing System (GEOS)-Chem. The simulated time series of sulfate aerosol optical depth (AOD) above 10km captures every eruptive volcanic sulfate perturbation with a similar magnitude to that measured by Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO). The 8year average contribution of eruptive SO42- to total SO42- loading above 10km is similar to 10% over most areas of the Northern Hemisphere, with a maxima of 30% in the tropics where the anthropogenic emissions are relatively smaller. The persistently degassing volcanic SO42- in the tropics barely reaches above 10km, but in the lower atmosphere it is regionally dominant (60%+ in terms of mass) over Hawaii and other oceanic areas northeast of Australia. Although the 7year average (2005-2011) of eruptive volcanic sulfate forcing of -0.10Wm(-2) in this study is comparable to that in the 2013 IPCC report (-0.09Wm(-2)), significant discrepancies exist for each year. Our simulations also imply that the radiative forcing per unit AOD for volcanic eruptions can vary from -40 to -80Wm(-2), much higher than the -25Wm(-2) implied in the IPCC calculations. In terms of sulfate forcing efficiency with respect to SO2 emission, eruptive volcanic sulfate is 5 times larger than anthropogenic sulfate. The sulfate forcing efficiency from degassing volcanic sources is close to that of anthropogenic sources. This study highlights the importance of characterizing both volcanic emission amount and injection altitude as well as the key role of satellite observations in maintaining accurate volcanic emissions inventories.
C1 [Ge, Cui; Wang, Jun] Univ Nebraska, Dept Earth & Atmospher Sci, Lincoln, NE USA.
[Carn, Simon] Michigan Technol Univ, Dept Geol & Min Engn & Sci, Houghton, MI 49931 USA.
[Yang, Kai] Univ Maryland, Dept Atmospher & Ocean Sci, College Pk, MD 20742 USA.
[Ginoux, Paul] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA.
[Krotkov, Nickolay] NASA, Goddard Space Flight Ctr, Atmospher Chem & Dynam Lab, Greenbelt, MD USA.
RP Wang, J (reprint author), Univ Nebraska, Dept Earth & Atmospher Sci, Lincoln, NE USA.
EM jwang7@unl.edu
RI Ge, Cui/I-6353-2016; Krotkov, Nickolay/E-1541-2012; Chem,
GEOS/C-5595-2014; Ginoux, Paul/C-2326-2008; Wang, Jun/A-2977-2008
OI Ge, Cui/0000-0002-6182-6856; Krotkov, Nickolay/0000-0001-6170-6750;
Ginoux, Paul/0000-0003-3642-2988; Wang, Jun/0000-0002-7334-0490
FU NASA [NNX10AG60G]
FX Levi Boggs and Frances Wiles are acknowledged for their work on
collecting the volcano injection altitudes data. The authors gratefully
acknowledge the Smithsonian Global Volcanism Program, Thomas Diehl, Tom
Simkin, and Lee Siebert for providing AeroCom volcano emission data. We
appreciate Brendam McCormick and two other reviewers for their
constructive comments. The authors thank the Holland Computing Center of
University of Nebraska-Lincoln, its director David Swanson, and his
staff Adam Caprez and Jingchao Zhang for their helpful efforts with
modeling work. The GEOS-Chem developers and support team in Harvard
University are acknowledged for their help. This work is supported by
NASA Atmospheric Chemistry Modeling and Analysis Program (NNX10AG60G)
managed by Richard S. Eckman, NASA Atmospheric Composition program, and
Radiation Sciences Program managed by Hal B. Maring. Data shown in the
paper can be obtained from the corresponding author through e-mail
(jwang7@unl.edu), and part of the emission data can be obtained from
ftp://measures.gsfc.nasa.gov/data/s4pa/SO2/MSVOLSO2L4.1/MSVOLSO2L4_v01-0
0-2014m1002.txt.
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U1 8
U2 19
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 APR 16
PY 2016
VL 121
IS 7
BP 3446
EP 3464
DI 10.1002/2015JD023134
PG 19
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DK7QG
UT WOS:000375120200023
ER
PT J
AU Kumjian, MR
Mishra, S
Giangrande, SE
Toto, T
Ryzhkov, AV
Bansemer, A
AF Kumjian, Matthew R.
Mishra, Subashree
Giangrande, Scott E.
Toto, Tami
Ryzhkov, Alexander V.
Bansemer, Aaron
TI Polarimetric radar and aircraft observations of saggy bright bands
during MC3E
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
DE radar; microphysics; precipitation
ID BACKSCATTER DIFFERENTIAL PHASE; MELTING LAYER; PART I; VERTICAL
VELOCITY; FALL SPEEDS; MICROPHYSICS; CLOUD; PRECIPITATION;
DISTRIBUTIONS; EVOLUTION
AB Polarimetric radar observations increasingly are used to understand cloud microphysical processes, which is critical for improving their representation in cloud and climate models. In particular, there has been recent focus on improving representations of ice collection processes (e.g., aggregation and riming), as these influence precipitation rate, heating profiles, and ultimately cloud life cycles. However, distinguishing these processes using conventional polarimetric radar observations is difficult, as they produce similar fingerprints. This necessitates improved analysis techniques and integration of complementary data sources. The Midlatitude Continental Convective Clouds Experiment (MC3E) provided such an opportunity. Quasi-vertical profiles of polarimetric radar variables in two MC3E stratiform precipitation events reveal episodic melting layer sagging. Integrated analyses using scanning and vertically pointing radar and aircraft measurements reveal that saggy bright band signatures are produced when denser, faster-falling, more isometric hydrometeors (relative to adjacent times) descend into the melting layer. In one case, strong circumstantial evidence for riming is found during bright band sagging times. A bin microphysical melting layer model successfully reproduces many aspects of the signature, supporting the observational analysis. If found to be a reliable indicator of riming, saggy bright bands could be a proxy for the presence of supercooled liquid water in stratiform precipitation, which may provide important information for mitigating aircraft icing risks and for constraining microphysical models.
C1 [Kumjian, Matthew R.] Penn State Univ, Dept Meteorol, 503 Walker Bldg, University Pk, PA 16802 USA.
[Mishra, Subashree] US DOE, Washington, DC 20585 USA.
[Mishra, Subashree; Ryzhkov, Alexander V.] NOAA OAR Natl Severe Storms Lab, Norman, OK USA.
[Giangrande, Scott E.; Toto, Tami] Brookhaven Natl Lab, Atmospher Sci Div, Upton, NY 11973 USA.
[Ryzhkov, Alexander V.] Cooperat Inst Mesoscale Meteorol Studies, Norman, OK USA.
[Ryzhkov, Alexander V.] Univ Oklahoma, Norman, OK 73019 USA.
[Bansemer, Aaron] Natl Ctr Atmospher Res, Mesoscale & Microscale Meteorol Div, POB 3000, Boulder, CO 80307 USA.
RP Kumjian, MR (reprint author), Penn State Univ, Dept Meteorol, 503 Walker Bldg, University Pk, PA 16802 USA.
EM kumjian@psu.edu
RI Giangrande, Scott/I-4089-2016; Measurement, Global/C-4698-2015
OI Giangrande, Scott/0000-0002-8119-8199;
FU U.S. Department of Energy [ER65459]; NOAA/Office and Atmospheric
Research under NOAA-University of Oklahoma, U.S. Department of Commerce
[NA11OAR4320072]; DOE ASR [DE-SC0008648]; National Science Foundation
FX Support for this work comes from grant ER65459 from the U.S. Department
of Energy Atmospheric System Research program. Support for A. Ryzhkov
and S. Mishra comes from NOAA/Office and Atmospheric Research under
NOAA-University of Oklahoma cooperative agreement NA11OAR4320072, U.S.
Department of Commerce. Support for A. Bansemer is from DOE ASR grant
DE-SC0008648. We would like to thank Mike Poellet and his research group
at UND for processing and providing the in situ aircraft data. Radar
data are available at the Department of Energy Atmospheric Radiation
Measurement program data archive. We would also like to thank Sandra
Yuter (NCSU) for helpful criticisms of our work. The comments and
suggestions from three anonymous reviewers significantly improved the
clarity and presentation of the manuscript. The National Center for
Atmospheric Research is sponsored by the National Science Foundation.
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SN 2169-897X
EI 2169-8996
J9 J GEOPHYS RES-ATMOS
JI J. Geophys. Res.-Atmos.
PD APR 16
PY 2016
VL 121
IS 7
BP 3584
EP 3607
DI 10.1002/2015JD024446
PG 24
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DK7QG
UT WOS:000375120200032
ER
PT J
AU Vollmer, MK
Muhle, J
Trudinger, CM
Rigby, M
Montzka, SA
Harth, CM
Miller, BR
Henne, S
Krummel, PB
Hall, BD
Young, D
Kim, J
Arduini, J
Wenger, A
Yao, B
Reimann, S
O'Doherty, S
Maione, M
Etheridge, DM
Li, SL
Verdonik, DP
Park, S
Dutton, G
Steele, LP
Lunder, CR
Rhee, TS
Hermansen, O
Schmidbauer, N
Wang, RHJ
Hill, M
Salameh, PK
Langenfelds, RL
Zhou, LX
Blunier, T
Schwander, J
Elkins, JW
Butler, JH
Simmonds, PG
Weiss, RF
Prinn, RG
Fraser, PJ
AF Vollmer, Martin K.
Muhle, Jens
Trudinger, Cathy M.
Rigby, Matthew
Montzka, Stephen A.
Harth, Christina M.
Miller, Benjamin R.
Henne, Stephan
Krummel, Paul B.
Hall, Bradley D.
Young, Dickon
Kim, Jooil
Arduini, Jgor
Wenger, Angelina
Yao, Bo
Reimann, Stefan
O'Doherty, Simon
Maione, Michela
Etheridge, David M.
Li, Shanlan
Verdonik, Daniel P.
Park, Sunyoung
Dutton, Geoff
Steele, L. Paul
Lunder, Chris R.
Rhee, Tae Siek
Hermansen, Ove
Schmidbauer, Norbert
Wang, Ray H. J.
Hill, Matthias
Salameh, Peter K.
Langenfelds, Ray L.
Zhou, Lingxi
Blunier, Thomas
Schwander, Jakob
Elkins, James W.
Butler, James H.
Simmonds, Peter G.
Weiss, Ray F.
Prinn, Ronald G.
Fraser, Paul J.
TI Atmospheric histories and global emissions of halons H-1211 (CBrClF2),
H-1301 (CBrF3), and H-2402 (CBrF2CBrF2)
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
DE halons; ozone depletion; bromine
ID OZONE DEPLETION POTENTIALS; PARTICLE DISPERSION MODEL; IN-SITU
MEASUREMENTS; POLAR FIRN AIR; WARMING POTENTIALS; MONTREAL PROTOCOL;
TRENDS; GASES; HALOCARBONS; GROWTH
AB We report ground-based atmospheric measurements and emission estimates for the halons H-1211 (CBrClF2), H-1301 (CBrF3), and H-2402 (CBrF2CBrF2) from the AGAGE (Advanced Global Atmospheric Gases Experiment) and the National Oceanic and Atmospheric Administration global networks. We also include results from archived air samples in canisters and from polar firn in both hemispheres, thereby deriving an atmospheric record of nearly nine decades (1930s to present). All three halons were absent from the atmosphere until approximate to 1970, when their atmospheric burdens started to increase rapidly. In recent years H-1211 and H-2402 mole fractions have been declining, but H-1301 has continued to grow. High-frequency observations show continuing emissions of H-1211 and H-1301 near most AGAGE sites. For H-2402 the only emissions detected were derived from the region surrounding the Sea of Japan/East Sea. Based on our observations, we derive global emissions using two different inversion approaches. Emissions for H-1211 declined from a peak of 11ktyr(-1) (late 1990s) to 3.9ktyr(-1) at the end of our record (mean of 2013-2015), for H-1301 from 5.4ktyr(-1) (late 1980s) to 1.6ktyr(-1), and for H-2402 from 1.8ktyr(-1) (late 1980s) to 0.38ktyr(-1). Yearly summed halon emissions have decreased substantially; nevertheless, since 2000 they have accounted for approximate to 30% of the emissions of all major anthropogenic ozone depletion substances, when weighted by ozone depletion potentials.
C1 [Vollmer, Martin K.; Henne, Stephan; Reimann, Stefan; Hill, Matthias] Empa, Swiss Fed Labs Mat Sci & Technol, Lab Air Pollut & Environm Technol, Dubendorf, Switzerland.
[Muhle, Jens; Harth, Christina M.; Kim, Jooil; Salameh, Peter K.; Weiss, Ray F.] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA.
[Trudinger, Cathy M.; Krummel, Paul B.; Etheridge, David M.; Steele, L. Paul; Langenfelds, Ray L.; Fraser, Paul J.] CSIRO Oceans & Atmosphere, Aspendale, Vic, Australia.
[Rigby, Matthew; Young, Dickon; Wenger, Angelina; O'Doherty, Simon; Simmonds, Peter G.] Univ Bristol, Sch Chem, Atmospher Chem Res Grp, Bristol, Avon, England.
[Montzka, Stephen A.; Miller, Benjamin R.; Hall, Bradley D.; Dutton, Geoff; Elkins, James W.; Butler, James H.] NOAA, Earth Syst Res Lab, Boulder, CO USA.
[Miller, Benjamin R.; Dutton, Geoff] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO USA.
[Arduini, Jgor; Maione, Michela] Univ Urbino, Dept Pure & Appl Sci, I-61029 Urbino, Italy.
[Arduini, Jgor; Maione, Michela] Italian Natl Res Council, Inst Atmospher Sci & Climate, Bologna, Italy.
[Yao, Bo] China Meteorol Adm, Meteorol Observat Ctr, Beijing, Peoples R China.
[Li, Shanlan; Park, Sunyoung] Kyungpook Natl Univ, Kyungpook Inst Oceanog, Taegu 702701, South Korea.
[Verdonik, Daniel P.] JENSEN HUGHES, Baltimore, MD USA.
[Lunder, Chris R.; Hermansen, Ove; Schmidbauer, Norbert] Norwegian Inst Air Res, Kjeller, Norway.
[Rhee, Tae Siek] KIOST, Korea Polar Res Inst, Inchon, South Korea.
[Wang, Ray H. J.] Georgia Inst Technol, Sch Earth & Atmospher Sci, Atlanta, GA 30332 USA.
[Zhou, Lingxi] China Meteorol Adm, Chinese Acad Meteorol Sci, Beijing, Peoples R China.
[Blunier, Thomas] Univ Copenhagen, Niels Bohr Inst, Ctr Ice & Climate, Blegdamsvej 17, DK-2100 Copenhagen, Denmark.
[Schwander, Jakob] Univ Bern, Inst Phys, Climate & Environm Phys, Bern, Switzerland.
[Schwander, Jakob] Univ Bern, Oeschger Ctr Climate Change Res, Bern, Switzerland.
[Prinn, Ronald G.] MIT, Ctr Global Change Sci, 77 Massachusetts Ave, Cambridge, MA 02139 USA.
RP Vollmer, MK (reprint author), Empa, Swiss Fed Labs Mat Sci & Technol, Lab Air Pollut & Environm Technol, Dubendorf, Switzerland.
EM martin.vollmer@empa.ch
RI Steele, Paul/B-3185-2009; Krummel, Paul/A-4293-2013; Rigby,
Matthew/A-5555-2012; Henne, Stephan/A-3467-2009; Reimann,
Stefan/A-2327-2009; arduini, jgor/N-2798-2016; Etheridge,
David/B-7334-2013; Langenfelds, Raymond/B-5381-2012; Trudinger,
Cathy/A-2532-2008
OI Steele, Paul/0000-0002-8234-3730; Krummel, Paul/0000-0002-4884-3678;
Rigby, Matthew/0000-0002-2020-9253; Reimann, Stefan/0000-0002-9885-7138;
arduini, jgor/0000-0002-5199-3853; Trudinger, Cathy/0000-0002-4844-2153
FU National Aeronautic and Space Administration (NASA) [NAG5-12669,
NNX07AE89G, NNX11AF17G, NNX07AE87G, NNX07AF09G, NNX11AF15G, NNX11AF16G];
Department of Energy and Climate Change (DECC, UK) [GA01081]; Swiss
National Program HALCLIM (Swiss Federal Office for the Environment,
FOEN); International Foundation High Altitude Research Stations
Jungfraujoch and Gornergrat (HFSJG); Norwegian Environment Agency;
National Research Council of Italy; Italian Ministry of Education,
University and Research; InGOS (Integrated Non-CO2 Greenhouse
gas Observing System, European FP-7 Infrastructure project) [284274];
Korea Meteorological Administration Research and Development Program
[CATER 2014-6020]; CAMS Fundamental Research Funds [2014Y005]; Korean
Polar Research Programs [PE13410, PP16102]; Australian Climate Change
Science Program (ACCSP), an Australian Government Initiative; FNRS-CFB
in Belgium; FWO in Belgium; NRCan/GSC in Canada; CAS in China; FIST in
Denmark; IPEV in France; CNRS/INSU in France; CEA in France; ANR in
France; AWI in Germany; RannIs in Iceland; NIPR in Japan; KOPRI in
Korea; NWO/ALW in Netherlands; VR in Sweden; SNF in Switzerland; NERC in
United Kingdom; U.S. NSF in U.S.; Office of Polar Programs in U.S.;
CSIRO Office of the Chief Executive; UK Natural Environment Research
Council (NERC) [NE/1021365/1]
FX We acknowledge the station personnel at all stations for their
continuous support in conducting in situ measurements and flask sampling
activities, the many providers of flask samples composing the archived
air sample data set of the Northern Hemisphere, and David Catchpole for
clarification on the HTOC activities and reports. The operation of the
AGAGE instruments at Mace Head, Trinidad Head, Cape Matatula, Ragged
Point, and Cape Grim is supported by the National Aeronautic and Space
Administration (NASA) (grants NAG5-12669, NNX07AE89G, and NNX11AF17G to
MIT and grants NNX07AE87G, NNX07AF09G, NNX11AF15G, and NNX11AF16G to
SIO), the Department of Energy and Climate Change (DECC, UK) contract
GA01081 to the University of Bristol, and the Commonwealth Scientific
and Industrial Research Organization (CSIRO Australia) and Bureau of
Meteorology (Australia). NOAA measurements of halons are supported in
part by the NOAA Climate Program Office's AC4 program and benefit from
C. Siso for the technical assistance in analyzing NOAA flasks. Financial
support for the measurements at the other sites is provided for
Jungfraujoch by the Swiss National Program HALCLIM (Swiss Federal Office
for the Environment, FOEN) and by the International Foundation High
Altitude Research Stations Jungfraujoch and Gornergrat (HFSJG), for
Zeppelin by the Norwegian Environment Agency, and for Monte Cimone by
the National Research Council of Italy and the Italian Ministry of
Education, University and Research, through the Project of National
Interest Nextdata. Activities at Mace Head (Bristol University),
Jungfraujoch (Empa), Monte Cimone (University of Urbino), and Zeppelin
(NILU) are also supported through InGOS (Integrated Non-CO2
Greenhouse gas Observing System, European FP-7 Infrastructure project
grant agreement 284274). Observations at Gosan were supported by the
Korea Meteorological Administration Research and Development Program
under grant CATER 2014-6020. Support for Shangdianzi observations comes
from the Key Project Natural Science Foundation of China (41030107), the
CMA Fundation for Climate Change Research (CCSF201331), and the CAMS
Fundamental Research Funds (2014Y005). Support for King Sejong flask
samples comes from the Swiss State Secretariat for Education and
Research and Innovation (SERI), the National Research Foundation of
Korea for the Korean-Swiss Science and Technology Cooperation Program,
and the Korean Polar Research ProgramsPE13410 and PP16102. CSIRO's
contribution was supported in part by the Australian Climate Change
Science Program (ACCSP), an Australian Government Initiative. Australian
firn activities in the Antarctic are specifically supported by the
Australian Antarctic Science Program. We acknowledge the members of the
firn air sampling teams for provision of the samples from Law Dome,
NEEM, and South Pole. NEEM is directed and organized by the Center of
Ice and Climate at the Niels Bohr Institute and US NSF, Office of Polar
Programs. It is supported by funding agencies and institutions in
Belgium (FNRS-CFB and FWO), Canada (NRCan/GSC), China (CAS), Denmark
(FIST), France (IPEV, CNRS/INSU, CEA, and ANR), Germany (AWI), Iceland
(RannIs), Japan (NIPR), Korea (KOPRI), the Netherlands (NWO/ALW), Sweden
(VR), Switzerland (SNF), United Kingdom (NERC), and the U.S. (U.S. NSF,
Office of Polar Programs). M.K.V. acknowledges a CSIRO Office of the
Chief Executive Distinguished Visiting Scientist grant to CSIRO
Aspendale for firn air measurements. M.R.; is supported by Advanced
Research Fellowships from the UK Natural Environment Research Council
(NERC, NE/1021365/1). Data used in this study are available from the
supporting information, from https://agage.mit.edu/, and from
http://www.esrl.noaa.gov/gmd/.
NR 64
TC 1
Z9 1
U1 9
U2 19
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 APR 16
PY 2016
VL 121
IS 7
BP 3663
EP 3686
DI 10.1002/2015JD024488
PG 24
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DK7QG
UT WOS:000375120200037
ER
PT J
AU Ott, LE
Duncan, BN
Thompson, AM
Diskin, G
Fasnacht, Z
Langford, AO
Lin, MY
Molod, AM
Nielsen, JE
Pusede, SE
Wargan, K
Weinheimer, AJ
Yoshida, Y
AF Ott, Lesley E.
Duncan, Bryan N.
Thompson, Anne M.
Diskin, Glenn
Fasnacht, Zachary
Langford, Andrew O.
Lin, Meiyun
Molod, Andrea M.
Nielsen, J. Eric
Pusede, Sally E.
Wargan, Krzysztof
Weinheimer, Andrew J.
Yoshida, Yasuko
TI Frequency and impact of summertime stratospheric intrusions over
Maryland during DISCOVER-AQ (2011): New evidence from NASA's GEOS-5
simulations
SO JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
LA English
DT Article
DE ozone; stratospheric intrusion; air quality
ID LONG-RANGE TRANSPORT; TROPOSPHERE EXCHANGE; OZONE CONCENTRATIONS; GLOBAL
CLIMATOLOGY; BACKGROUND OZONE; TROPOPAUSE FOLDS; UNITED-STATES;
PACIFIC-OCEAN; AIR-QUALITY; SURFACE AIR
AB Aircraft observations and ozonesonde profiles collected on 14 and 27 July 2011, during the Maryland month-long Deriving Information on Surface conditions from Column and Vertically Resolved Observations Relevant to Air Quality (DISCOVER-AQ) campaign, indicate the presence of stratospheric air just above the planetary boundary layer (PBL). This raises the question of whether summer stratospheric intrusions (SIs) elevate surface ozone levels and to what degree they influence background ozone levels and contribute to ozone production. We used idealized stratospheric air tracers, along with observations, to determine the frequency and extent of SIs in Maryland during July 2011. On 4 of 14 flight days, SIs were detected in layers that the aircraft encountered above the PBL from the coincidence of enhanced ozone, moderate CO, and low moisture. Satellite observations of lower tropospheric humidity confirmed the occurrence of synoptic-scale influence of SIs as do simulations with the GEOS-5 atmospheric general circulation model. The evolution of GEOS-5 stratospheric air tracers agrees with the timing and location of observed stratospheric influence and indicates that more than 50% of air in SI layers above the PBL had resided in the stratosphere within the previous 14days. Despite having a strong influence in the lower free troposphere, these events did not significantly affect surface ozone, which remained low on intrusion days. The model indicates similar frequencies of stratospheric influence during all summers from 2009 to 2013. GEOS-5 results suggest that over Maryland, the strong inversion capping the summer PBL limits downward mixing of stratospheric air during much of the day, helping to preserve low surface ozone associated with frontal passages that precede SIs.
C1 [Ott, Lesley E.; Duncan, Bryan N.; Thompson, Anne M.; Molod, Andrea M.; Nielsen, J. Eric; Wargan, Krzysztof; Yoshida, Yasuko] NASA, Goddard Space Flight Ctr, Greenbelt, MD USA.
[Diskin, Glenn] NASA, Langley Res Ctr, Hampton, VA 23665 USA.
[Fasnacht, Zachary] Univ Maryland, Dept Atmospher & Ocean Sci, College Pk, MD 20742 USA.
[Langford, Andrew O.] NOAA, Earth Syst Res Lab, Chem Sci Div, Boulder, CO USA.
[Lin, Meiyun] Princeton Univ, Program Atmospher & Ocean Sci, Princeton, NJ 08544 USA.
[Lin, Meiyun] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA.
[Molod, Andrea M.] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20742 USA.
[Nielsen, J. Eric; Wargan, Krzysztof; Yoshida, Yasuko] Sci Syst & Applicat Inc, Lanham, MD USA.
[Pusede, Sally E.] Univ Virginia, Dept Environm Sci, Clark Hall, Charlottesville, VA 22903 USA.
[Weinheimer, Andrew J.] Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA.
RP Ott, LE (reprint author), NASA, Goddard Space Flight Ctr, Greenbelt, MD USA.
EM lesley.e.ott@nasa.gov
RI Lin, Meiyun/D-6107-2013; Langford, Andrew/D-2323-2009; Ott,
Lesley/E-2250-2012; Duncan, Bryan/A-5962-2011; Manager, CSD
Publications/B-2789-2015; Thompson, Anne /C-3649-2014
OI Lin, Meiyun/0000-0003-3852-3491; Langford, Andrew/0000-0002-2932-7061;
Wargan, Krzysztof/0000-0002-3795-2983; Thompson, Anne
/0000-0002-7829-0920
FU NASA's Atmospheric Composition Campaign Data Analysis and Modeling
program; NASA's DISCOVER-AQ campaign
FX This work was supported by funding from NASA's Atmospheric Composition
Campaign Data Analysis and Modeling program and NASA's DISCOVER-AQ
campaign. MERRA and MERRA-2 data have been provided by the GMAO at
NASA's Goddard Space Flight Center through the NASA GES DISC online
archive. AIRS data are also available through the GES DISC. DISCOVER-AQ
aircraft and ozonesonde observations were provided by NASA's Langley
Research Center at
http://www-air.larc.nasa.gov/missions/discover-aq/discover-aq.html.
GEOS-5 stratospheric tracer simulations will be provided upon request.
NR 78
TC 4
Z9 4
U1 5
U2 14
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 APR 16
PY 2016
VL 121
IS 7
BP 3687
EP 3706
DI 10.1002/2015JD024052
PG 20
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DK7QG
UT WOS:000375120200038
ER
PT J
AU Zhu, JM
Vaghefi, SA
Jafari, MA
Lu, Y
Ghofrani, A
AF Zhu, Jianmin
Vaghefi, Seyed A.
Jafari, Mohsen A.
Lu, Yan
Ghofrani, Ali
TI Managing demand uncertainty with cost-for-deviation retail pricing
SO ENERGY AND BUILDINGS
LA English
DT Article
DE Electricity retailing; Demand side management; Transactive energy;
Demand uncertainty; Model-predictive control
ID VALUE-AT-RISK; ENERGY-CONSUMPTION; STOCHASTIC PROGRAMS; ELECTRICITY
MARKETS; SELLING PRICE; BUILDINGS; MODEL; STRATEGIES; CUSTOMERS; SYSTEMS
AB The current rate structures for the electricity retailing exposes utility providers to the full wholesale market risks, and fail to incentivize end-use customers to better estimate and track their loads. In this paper, we propose a Cost-for-Deviation (CfD) retail-pricing scheme, which is designed to minimize the demand uncertainty of individual customers or communities. We formulate day-ahead planning and real-time tracking optimization problems for individual buildings. We also formulate CfD pricing scheme for community of two buildings and devise a collaboration scheme by which the two buildings negotiate. Both centralized and distributed negotiation mechanisms are presented, and the significance of adopting a transaction cost for fair-trading is discussed. A series of experiments demonstrate that CfD pricing is able to reduce demand uncertainty in a building or a community. Hence, a community's cost of hedging quantity risk in the real-time market also reduces. Our conjecture is that by the virtue of end users being in a position to closely monitor their daily loads and by paying fines for not adhering to their plans would ultimately benefit energy efficiency and will reduce infrastructure costs. (C) 2016 Elsevier B.V. All rights reserved.
C1 [Zhu, Jianmin] Liberty Mutual Insurance, Boston, MA 02116 USA.
[Vaghefi, Seyed A.; Jafari, Mohsen A.; Ghofrani, Ali] Rutgers State Univ, Dept Ind & Syst Engn, Piscataway, NJ 08904 USA.
[Lu, Yan] NIST, Gaithersburg, MD 20899 USA.
RP Ghofrani, A (reprint author), Rutgers State Univ, Dept Ind & Syst Engn, Piscataway, NJ 08904 USA.
EM a.ghofrani1@gmail.com
NR 35
TC 1
Z9 1
U1 3
U2 6
PU ELSEVIER SCIENCE SA
PI LAUSANNE
PA PO BOX 564, 1001 LAUSANNE, SWITZERLAND
SN 0378-7788
EI 1872-6178
J9 ENERG BUILDINGS
JI Energy Build.
PD APR 15
PY 2016
VL 118
BP 46
EP 56
DI 10.1016/j.enbuild.2016.02.025
PG 11
WC Construction & Building Technology; Energy & Fuels; Engineering, Civil
SC Construction & Building Technology; Energy & Fuels; Engineering
GA DJ7CM
UT WOS:000374369500005
ER
PT J
AU Stout, SA
Payne, JR
Emsbo-Mattingly, SD
Baker, G
AF Stout, Scott A.
Payne, James R.
Emsbo-Mattingly, Stephen D.
Baker, Gregory
TI Weathering of field-collected floating and stranded Macondo oils during
and shortly after the Deepwater Horizon oil spill
SO MARINE POLLUTION BULLETIN
LA English
DT Review
DE Oil spill; Weathering; Polycyclic aromatic hydrocarbons; Biomarkers;
Photo-oxidation
ID CRUDE-OIL; BIODEGRADATION; PHOTOOXIDATION; DEGRADATION; PETROLEUM;
TOXICITY; PRODUCTS; BIOMARKERS; STABILITY; ROLES
AB Chemical analysis of large populations of floating (n = 62) and stranded (n = 1174) Macondo oils collected from the northern Gulf of Mexico sea surface and shorelines during or within seven weeks of the end of the Deepwater Horizon oil spill demonstrates the range, rates, and processes affecting surface oil weathering. Oil collected immediately upon reaching the sea surface had already lost most mass below n-C-8 from dissolution of soluble aliphatics, monoaromatics, and naphthalenes during the oil's ascent with further reductions extending up to n-C-13 due to the onset of evaporation. With additional time, weathering of the floating and stranded oils advanced with total PAH (TPAH(50)) depletions averaging 69 +/- 23% for floating oils and 94 +/- 3% for stranded oils caused by the combined effects of evaporation, dissolution, and photo-oxidation, the latter of which also reduced triaromatic steroid biomarkers. Biodegradation was not evident among the coalesced floating oils studied, but had commenced in some stranded oils. (C) 2016 Elsevier Ltd. All rights reserved.
C1 [Stout, Scott A.; Emsbo-Mattingly, Stephen D.] NewFields Environm Forens Practice LLC, 300 Ledgewood Pl,Suite 305, Rockland, MA USA.
[Payne, James R.] Payne Environm Consultants Inc, 1651 Linda Sue Lane, Encinitas, CA USA.
[Baker, Gregory] NOAA, Assessment & Restorat Div, 345 Middlefield Rd,MS-999, Menlo Pk, CA USA.
RP Stout, SA (reprint author), NewFields Environm Forens Practice LLC, 300 Ledgewood Pl,Suite 305, Rockland, MA USA.
EM sstout@newfields.com
FU NOAA through Industrial Economics, Corp. (Cambridge, MA) as part of the
NRDA process
FX This study was conducted within the Deepwater Horizon NRDA
investigation, which was cooperatively conducted by NOAA, other Federal
and State Trustees, and BP. The scientific results and conclusion of
this publication, as well as any views or opinions expressed herein, are
those of the authors only. The authors declare no competing financial
interest in the publication of this study. Funding for the study was
provided by NOAA through Industrial Economics, Corp. (Cambridge, MA) as
part of the NRDA process.
NR 44
TC 9
Z9 9
U1 18
U2 20
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0025-326X
EI 1879-3363
J9 MAR POLLUT BULL
JI Mar. Pollut. Bull.
PD APR 15
PY 2016
VL 105
IS 1
BP 7
EP 22
DI 10.1016/j.marpolbul.2016.02.044
PG 16
WC Environmental Sciences; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA DL7JC
UT WOS:000375816000014
PM 26936118
ER
PT J
AU Melvin, AT
Thibodeaux, LJ
Parsons, AR
Overton, E
Valsaraj, KT
Nandakumar, K
AF Melvin, A. T.
Thibodeaux, L. J.
Parsons, A. R.
Overton, E.
Valsaraj, K. T.
Nandakumar, K.
TI Oil-material fractionation in Gulf deep water horizontal intrusion
layer: Field data analysis with chemodynamic fate model for Macondo 252
oil spill
SO MARINE POLLUTION BULLETIN
LA English
DT Article
DE Deepwater horizon; Oil-material trapping layer; Chemodynamics;
Sub-surface plume; Far field modeling
ID DROPLET SIZE; OF-MEXICO; WELL BLOWOUT; GAS; TRANSPORT; TEMPERATURE;
PYCNOCLINE; DIFFUSION; PLUMES
AB Among the discoveries of the Deepwater Horizon blowout was the so-called "sub-surface plume"; herein termed the "oil-trapping layer". Hydrocarbons were found positioned at similar to 1100-1300 m with thickness similar to 100-150 m and moving horizontally to the SW in a vertically stratified layer at the junction of the cold abyssal water and the permanent thermocline. This study focuses on its formation process and fate of the hydrocarbons within. The originality of this work to the field is two-fold, first it provides a conceptual framework which places layer origin in the context of a horizontal "intrusion" from the near-field, vertical, blow-out plume and second, it offers a theoretical model for the hydrocarbon chemicals within the horizontal layer as it moves far-afield. The model quantifies the oil-material fractionation process for the soluble and fine particle. The classical Box model, retrofitted with an internal gradient, the "G-Box", allows an approach that includes turbulent-eddy diffusion coupled with droplet rise velocity and reactive decay to produce a simple, explicit, transparent, algebraic model with few parameters for the fate of the individual fractions. Computations show the soluble and smallest liquid droplets moving very slowly vertically through the layer appearing within the trapping layer at low concentration with high persistence. The larger droplets move-through this trapping zone quickly, attain high concentrations, and eventually form the sea surface slick. It impacts the field of oil spill engineering science by providing the conceptual idea and the algorithms for projecting the quantities and fractions of oil-material in a deep water, horizontal marine current being dispersed and moving far afield. In the field of oil spill modeling this work extends the current generation near-field plume source models to the far-field. The theory portrays the layer as an efficient oil material trap. The model-forecasted concentration profiles for alkanes and aromatics against the available field data support the proposed theory and the resulting model. (C) 2016 Elsevier Ltd. All rights reserved.
C1 [Melvin, A. T.; Thibodeaux, L. J.; Valsaraj, K. T.; Nandakumar, K.] Louisiana State Univ, Cain Dept Chem Engn, Baton Rouge, LA 70803 USA.
[Overton, E.] Louisiana State Univ, Dept Environm Sci, Baton Rouge, LA 70803 USA.
[Parsons, A. R.] NOAA, Natl Oceanog Data Ctr, Washington, DC USA.
RP Thibodeaux, LJ (reprint author), Louisiana State Univ, Cain Dept Chem Engn, Baton Rouge, LA 70803 USA.
EM thibod@lsu.edu
RI Nandakumar, K/C-9995-2011; Valsaraj, Kalliat/B-6451-2008
OI Nandakumar, K/0000-0003-0795-9284; Valsaraj, Kalliat/0000-0003-0251-1739
NR 45
TC 0
Z9 0
U1 4
U2 9
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0025-326X
EI 1879-3363
J9 MAR POLLUT BULL
JI Mar. Pollut. Bull.
PD APR 15
PY 2016
VL 105
IS 1
BP 110
EP 119
DI 10.1016/j.marpolbul.2016.02.043
PG 10
WC Environmental Sciences; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA DL7JC
UT WOS:000375816000027
PM 26947926
ER
PT J
AU Deshpande, AD
Dickhut, RM
Dockum, BW
Brill, RW
Farrington, C
AF Deshpande, Ashok D.
Dickhut, Rebecca M.
Dockum, Bruce W.
Brill, Richard W.
Farrington, Cameron
TI Polychlorinated biphenyls and organochlorine pesticides as intrinsic
tracer tags of foraging grounds of bluefin tuna in the northwest
Atlantic Ocean
SO MARINE POLLUTION BULLETIN
LA English
DT Article
DE Atlantic bluefin tuna; PCB fingerprints; Trans-nonachlor/PCB 153 ratio;
Metapopulation
ID NEW-YORK BIGHT; THUNNUS-THYNNUS; MEDITERRANEAN SEA;
POPULATION-STRUCTURE; FATTY-ACID; NEWARK BAY; ECOLOGY; MUSCLE; GULF;
FISH
AB Researchers have utilized chemical fingerprints in the determination of habitat utilization and movements of the aquatic animals. In the present effort, we analyzed polychlorinated biphenyl (PCB) congeners and organochlorine pesticides in the samples of juvenile bluefin tuna caught offshore of Virginia, and in larger bluefin tuna from the Gulf of Maine and near Nova Scotia. For a given specimen, or a given location, PCB concentrations were highest, followed by DDTs, and chlordanes. Average contaminant concentrations from fish captured from the three locations were not significantly different; and PCBs, DDTs, and chlordanes correlated well with each other. Trans-nonachlor/PCB 153 ratios in bluefin tuna of eastern Atlantic (i.e., Mediterranean) origin are low compared to the corresponding ratios in fish in the western Atlantic. As the former migrate to the western Atlantic, these ratios gradually turnover due to the accumulation of biomass from forage contaminated with higher trans-nonachlor/PCB 153 ratio reflecting dissimilar use of chlordane pesticides on two sides of the Atlantic Ocean. The trans-nonachlor/PCB 153 ratio indicated that one juvenile bluefin tuna from offshore of Virginia and one large bluefin tuna from Gulf of Maine in the present study originated from foraging grounds in the Mediterranean Sea, and that they have made the trans-Atlantic migrations. The remaining individuals were determined to be either spawned in the Gulf of Mexico or the trans-nonachlor/PCB 153 ratio for the putative Mediterranean bluefin tuna was completely turned over to resemble the ratio characteristic to the western Atlantic. Based on the turnover time for trans-nonachlor/PCB 153 ratio previously determined, the residence time of juvenile bluefin tuna offshore Virginia was estimated to be at least 0.8 to 1.6 years. A discriminant function analysis (DFA) plot of total PCB normalized signatures of PCB congeners showed three separate clusters, which suggested that bluefin tuna from offshore Virginia, Gulf of Maine, and Nova Scotia could have had extended residences and foraging within the areas of capture to be able to sustain the stable signatures of PCB congeners. The DFA cluster results supported the concept of metapopulation theory of spatial ecology comprising discrete aggregates of local populations of bluefin tuna where the desired prey species are likely to be abundant. Despite their highly migratory trait and endothermic advantage of foraging in broader and colder habitats, the movements and mixing across the aggregation ranges related to feeding did not appear to be extensive. Advancement in the understanding of bluefin tuna population dynamics beyond the coarse concept of trans-Atlantic migrations to the metapopulation hypothesis provides a novel exploratory tool in the stock assessment and resource management. As the chemical tracer tags are fortified naturally and document the time- and space-integrated foraging history, they promise to serve as the low-cost alternatives to the high-cost electronic data recording tags employed for addressing the migratory movements of bluefin tuna. Between the different potential chemical tracer tags, a distinct advantage of PCB/pesticide analysis over the otolith micro-constituent analysis is that the muscle tissue of a given individual bluefin tuna can be sampled repeatedly for PCB/pesticide analysis over different spatial and temporal scales in a non-lethal manner. Published by Elsevier Ltd.
C1 [Deshpande, Ashok D.; Dockum, Bruce W.; Brill, Richard W.; Farrington, Cameron] NOAA Fisheries, James J Howard Marine Sci Lab, Northeast Fisheries Sci Ctr, Sandy Hook, NJ USA.
[Dickhut, Rebecca M.] Virginia Inst Marine Sci, Gloucester Point, VA 23062 USA.
RP Deshpande, AD (reprint author), NOAA Fisheries, James J Howard Marine Sci Lab Sandy Hook, 74 Magruder Rd, Highlands, NJ 07732 USA.
EM ashok.deshpande@noaa.gov
FU NOAA [NA04NMF4550391]; NOAA/UNH-LPRC
FX The authors are thankful to Molly Lutcavage and John Logan at University
of New Hampshire's Large Pelagic Research Center (UNH-LPRC) for
providing the samples of bluefin tuna from Gulf of Maine and Nova
Scotia. We thank David Richardson, Robert Pikanowski, and Nathaniel
Newlands for the critical reviews of the manuscript. We also thank the
two unknown reviewers of the Marine Pollution Bulletin for their
critical reviews and excellent feedback. The study was partly funded by
a grant from NOAA/UNH-LPRC to the Virginia Institute of Marine Science
entitled "PCBs as novel tracers for determining Bluefin tuna (Thunnus
thynnus) population mixing in the North Atlantic", which was coauthored
by Rebecca M. Dickhut (Virginia Institute of Marine Science) and Ashok
D. Deshpande (NOAA) (a sub-award under the grant number NA04NMF4550391
from NOAA to UNH-LPRC).
NR 57
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Z9 0
U1 10
U2 17
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0025-326X
EI 1879-3363
J9 MAR POLLUT BULL
JI Mar. Pollut. Bull.
PD APR 15
PY 2016
VL 105
IS 1
BP 265
EP 276
DI 10.1016/j.marpolbul.2016.02.016
PG 12
WC Environmental Sciences; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA DL7JC
UT WOS:000375816000044
PM 26895594
ER
PT J
AU Disseler, SM
Lynn, JW
Jardim, RF
Torikachvili, MS
Granado, E
AF Disseler, S. M.
Lynn, J. W.
Jardim, R. F.
Torikachvili, M. S.
Granado, E.
TI Spin dynamics and two-dimensional correlations in the fcc
antiferromagnetic Sr2YRuO6
SO PHYSICAL REVIEW B
LA English
DT Article
ID DOUBLE PEROVSKITE SR2YRUO6; MAGNETIC-STRUCTURES; CRYSTAL; DIFFRACTION;
NEUTRON
AB The face-centered-cubic (fcc) lattice of Ru5+ spins in the double perovskite Sr2YRuO6 shows a delicate, three-dimensional antiferromagnetic (AFM) ground state composed of stacked square AFM layers. Inelastic neutron scattering data taken on this state reveal a gapped low-energy excitation band emerging from [001] with spin excitations extending to 8meV. These magnetic excitations are modeled by a simple J(1)-J(2) interaction scheme allowing quantitative comparisons with similar materials. At higher temperatures, the low-energy excitation spectrum is dominated by a quasielastic component associated with size fluctuations of two-dimensional AFM clusters that exhibit asymmetric correlations even at low temperatures. Thus, the fcc lattice in general and the double-perovskite structure in particular emerge as hosts of both two-dimensional and three-dimensional dynamics resulting from frustration.
C1 [Disseler, S. M.; Lynn, J. W.] NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Jardim, R. F.] Univ Sao Paulo, Inst Fis, CP 66318, BR-05315970 Sao Paulo, Brazil.
[Torikachvili, M. S.] San Diego State Univ, Dept Phys, San Diego, CA 92182 USA.
[Granado, E.] Univ Estadual Campinas, UNICAMP, Inst Phys Gleb Wataghin, BR-13083859 Sao Paulo, Brazil.
RP Disseler, SM (reprint author), NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
RI Jardim, Renato/J-8068-2014; Granado, Eduardo/F-5389-2012; FAPESP,
CDMF/J-3591-2015
OI Jardim, Renato/0000-0002-2000-0257;
FU FAPESP [2012/04870-7, 2013/07296-2, 2014/19245-6]; CNPq, Brazil; NSF,
USA [DMR-0805335]
FX This work was supported in part by FAPESP Grants No. 2012/04870-7,
2013/07296-2 and No. 2014/19245-6 and CNPq, Brazil, and NSF Grant No.
DMR-0805335, USA.
NR 36
TC 1
Z9 1
U1 10
U2 29
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 2469-9950
EI 2469-9969
J9 PHYS REV B
JI Phys. Rev. B
PD APR 15
PY 2016
VL 93
IS 14
AR 140407
DI 10.1103/PhysRevB.93.140407
PG 5
WC Physics, Condensed Matter
SC Physics
GA DJ6CW
UT WOS:000374298600001
ER
PT J
AU Xu, MH
Jager, SB
Schutz, S
Cooper, J
Morigi, G
Holland, MJ
AF Xu, Minghui
Jaeger, Simon B.
Schuetz, S.
Cooper, J.
Morigi, Giovanna
Holland, M. J.
TI Supercooling of Atoms in an Optical Resonator
SO PHYSICAL REVIEW LETTERS
LA English
DT Article
ID LASER; GASES; LIGHT
AB We investigate laser cooling of an ensemble of atoms in an optical cavity. We demonstrate that when atomic dipoles are synchronized in the regime of steady-state superradiance, the motion of the atoms may be subject to a giant frictional force leading to potentially very low temperatures. The ultimate temperature limits are determined by a modified atomic linewidth, which can be orders of magnitude smaller than the cavity linewidth. The cooling rate is enhanced by the superradiant emission into the cavity mode allowing reasonable cooling rates even for dipolar transitions with ultranarrow linewidth.
C1 [Xu, Minghui; Cooper, J.; Holland, M. J.] Univ Colorado, NIST, Joint Inst Lab Astrophys, Boulder, CO 80309 USA.
[Xu, Minghui; Cooper, J.; Holland, M. J.] Univ Colorado, Dept Phys, Boulder, CO 80309 USA.
[Xu, Minghui; Holland, M. J.] Univ Colorado, Ctr Theory Quantum Matter, Boulder, CO 80309 USA.
[Jaeger, Simon B.; Schuetz, S.; Morigi, Giovanna] Univ Saarland, Theoret Phys, D-66123 Saarbrucken, Germany.
RP Xu, MH (reprint author), Univ Colorado, NIST, Joint Inst Lab Astrophys, Boulder, CO 80309 USA.; Xu, MH (reprint author), Univ Colorado, Dept Phys, Boulder, CO 80309 USA.; Xu, MH (reprint author), Univ Colorado, Ctr Theory Quantum Matter, Boulder, CO 80309 USA.
RI Xu, Minghui/D-4701-2017
FU DARPA QuASAR program; NSF [AMO-1404263, PFC-1125844, QIS-1521080]; NIST;
German Research Foundation (DACH project "Quantum crystals of matter and
light"); German Ministry of Education and Research BMBF (Q.Com)
FX We acknowledge helpful discussions with A. M. Rey, J. Ye, and J. K.
Thompson. This work has been supported by the DARPA QuASAR program, the
NSF (Grants No. AMO-1404263, No. PFC-1125844, and No. QIS-1521080),
NIST, the German Research Foundation (DACH project "Quantum crystals of
matter and light"), and the German Ministry of Education and Research
BMBF (Q.Com).
NR 35
TC 1
Z9 1
U1 3
U2 7
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 0031-9007
EI 1079-7114
J9 PHYS REV LETT
JI Phys. Rev. Lett.
PD APR 15
PY 2016
VL 116
IS 15
AR 153002
DI 10.1103/PhysRevLett.116.153002
PG 5
WC Physics, Multidisciplinary
SC Physics
GA DJ6BN
UT WOS:000374295100005
PM 27127966
ER
PT J
AU Ona-Ruales, JO
Ruiz-Morales, Y
Wise, SA
AF Ona-Ruales, Jorge O.
Ruiz-Morales, Yosadara
Wise, Stephen A.
TI Identification and quantification of seven fused aromatic rings C26H14
pen-condensed benzenoid polycyclic aromatic hydrocarbons in a complex
mixture of polycyclic aromatic hydrocarbons from coal tar
SO JOURNAL OF CHROMATOGRAPHY A
LA English
DT Article
DE Coal tar; Polycyclic aromatic hydrocarbons (PAHs); Normal-phase liquid
chromatography with ultraviolet-visible spectroscopy (NPLC/IJV-vis); Gas
chromatography with mass; spectrometry (GC/MS); Annellation theory;
ZINDO/S calculations
ID LIQUID-CHROMATOGRAPHIC SEPARATION; STANDARD REFERENCE MATERIALS;
MASS-SPECTROMETRY; Y-RULE; DIESEL PARTICULATE; PYROLYSIS; PRODUCTS; PAHS
AB A methodology for the characterization of groups of polycyclic aromatic hydrocarbons (PAHs) using a combination of normal phase liquid chromatography with ultraviolet -visible spectroscopy (NPLC/UV-vis) and gas chromatography with mass spectrometry (GC/MS) was used for the identification and quantification of seven fused aromatic rings C26H14 peri-condensed benzenoid polycyclic aromatic hydrocarbons, PAHs, in standard reference material (SRM) 1597a, complex mixture of PAHs from coal tar. The NPLC/UV-vis isolated the fractions based on the number of aromatic carbons and the GC/MS allowed the identification and quantification of five of the nine C26H14 PAH isomers; naphtho[1,2,3,4-ghi]perylene, dibenzo[b,ghi]perylene, dibenzo[b,pqr]perylene, naphtho[8,1,2-bcd]perylene, and dibenzo[cd,/m]perylene using a retention time comparison with authentic reference standards. For the other four benzenoid isomers with no available reference standards the following two approaches were used. First, the annellation theory was used to achieve the potential identification of benzo[qr]naphtho[3,2,1,8-defg]chrysene, and second, the elution distribution in the GC fractions was used to support the potential identification of benzo[qdnaphtho[3,2,1,8-defg]chrysene and to reach the tentative identifications of dibenzo[a,ghi]perylene, naphtho[7,8,1,2,3-pqrst]pentaphene, and anthra[2,1,9,8opqra]naphthacene. It is the first time that naphtho[1,2,3,4-ghi]perylene, dibenzo[b,ghi]perylene, dibenzo[b,pqr]perylene, naphtho[8,1,2-bcd]perylene, and dibenzo[cd,lm]perylene are quantified, and the first time that benzo[qr]naphtho[3,2,1,8-defg]chrysene is potentially identified, in any sample, in any context. (C) 2016 Elsevier B.V. All rights reserved.
C1 [Ona-Ruales, Jorge O.; Wise, Stephen A.] NIST, Gaithersburg, MD 20899 USA.
[Ruiz-Morales, Yosadara] Inst Mexicano Petr, Eje Cent Lazaro Cardenas Norte 152, Mexico City 07730, DF, Mexico.
RP Ona-Ruales, JO (reprint author), NIST, Gaithersburg, MD 20899 USA.
EM Jorge.ona-ruales@nist.gov
NR 36
TC 2
Z9 2
U1 8
U2 27
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0021-9673
EI 1873-3778
J9 J CHROMATOGR A
JI J. Chromatogr. A
PD APR 15
PY 2016
VL 1442
BP 83
EP 93
DI 10.1016/j.chroma.2016.02.082
PG 11
WC Biochemical Research Methods; Chemistry, Analytical
SC Biochemistry & Molecular Biology; Chemistry
GA DJ3CT
UT WOS:000374083100010
PM 26976350
ER
PT J
AU Ainsworth, TD
Heron, SF
Ortiz, JC
Mumby, PJ
Grech, A
Ogawa, D
Eakin, CM
Leggat, W
AF Ainsworth, Tracy D.
Heron, Scott F.
Ortiz, Juan Carlos
Mumby, Peter J.
Grech, Alana
Ogawa, Daisie
Eakin, C. Mark
Leggat, William
TI Climate change disables coral bleaching protection on the Great Barrier
Reef
SO SCIENCE
LA English
DT Article
ID STRESS; PROJECTIONS; RESISTANCE; EMISSIONS; RESPONSES
AB Coral bleaching events threaten the sustainability of the Great Barrier Reef (GBR). Here we show that bleaching events of the past three decades have been mitigated by induced thermal tolerance of reef-building corals, and this protective mechanism is likely to be lost under near-future climate change scenarios. We show that 75% of past thermal stress events have been characterized by a temperature trajectory that subjects corals to a protective, sub-bleaching stress, before reaching temperatures that cause bleaching. Such conditions confer thermal tolerance, decreasing coral cell mortality and symbiont loss during bleaching by over 50%. We find that near-future increases in local temperature of as little as 0.5 degrees C result in this protective mechanism being lost, which may increase the rate of degradation of the GBR.
C1 [Ainsworth, Tracy D.; Ogawa, Daisie; Leggat, William] James Cook Univ, Australian Res Council Ctr Excellence Coral Reef, Townsville, Qld 4810, Australia.
[Heron, Scott F.; Eakin, C. Mark] NOAA, Coral Reef Watch, College Pk, MD 20740 USA.
[Heron, Scott F.] James Cook Univ, Coll Sci Technol & Engn, Marine Geophys Lab, Townsville, Qld 4811, Australia.
[Ortiz, Juan Carlos; Mumby, Peter J.] Univ Queensland, Sch Biol Sci, Marine Spatial Ecol Lab, Brisbane, Qld 4072, Australia.
[Ortiz, Juan Carlos; Mumby, Peter J.] Univ Queensland, Australian Res Council Ctr Excellence Coral Reef, Brisbane, Qld 4072, Australia.
[Grech, Alana] Macquarie Univ, Dept Environm Sci, Sydney, NSW 2109, Australia.
[Ogawa, Daisie; Leggat, William] James Cook Univ, Coll Publ Hlth Med & Vet Sci, Townsville, Qld 4810, Australia.
RP Ainsworth, TD (reprint author), James Cook Univ, Australian Res Council Ctr Excellence Coral Reef, Townsville, Qld 4810, Australia.
EM tracy.ainsworth@jcu.edu.au
RI Eakin, C. Mark/F-5585-2010; Heron, Scott/E-7928-2011; AINSWORTH,
TRACY/L-7309-2016;
OI AINSWORTH, TRACY/0000-0001-6476-9263; Leggat,
William/0000-0003-4148-2555; Grech, Alana/0000-0003-4117-3779
FU Australian Research Council Discovery Program [DP130101421]; Australian
Research Council Super Science Program [FS110200046]; Australian
Research Council Centre of Excellence for Coral Reef Studies
[CE0561435]; Great Barrier Reef Foundation (Coral Health Grant); NOAA
National Environmental Satellite, Data, and Information Service; NOAA
Coral Reef Conservation Program; FigShare project [12040]
FX The authors thank the following funding bodies: Australian Research
Council Discovery Program grant DP130101421 (awarded to W.L. and
T.D.A.); Australian Research Council Super Science Program grant
FS110200046 (awarded to Terry P. Hughes, Director, Australian Research
Council Centre of Excellence for Coral Reef Studies); Australian
Research Council Centre of Excellence for Coral Reef Studies grant
CE0561435; the Great Barrier Reef Foundation (Coral Health Grant); the
NOAA National Environmental Satellite, Data, and Information Service;
and the NOAA Coral Reef Conservation Program. The authors thank N. Wolff
for providing SST projections and help in analysis of ecosystem model
components and M. De Freitas Prazeres for cell counts. The contents in
this manuscript 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. T.D.A., S.F.H., J.C.O., and W.L. designed
the study. T.D.A., D.O., and W.L. conducted experimental procedures and
physiological analyses. S.F.H. and C.M.E. conducted SST and
oceanographic analyses. J.C.O. and P.J.M. conducted predictive modeling
and model validation. T.D.A., S.F.H., J.C.O., P.J.M., A.G., C.M.E., and
W.L. wrote and finalized the manuscript. Code for the analysis of SST
data is available through contact and collaboration with S. Heron
(scott.heron@noaa.gov). Code for the ecosystem model is available
through contact and collaboration with J.-C. Ortiz (j.ortiz@uq.edu.au).
The NOAA data and code are available from a dedicated web page:
http://coralreefwatch.noaa.gov/publications/AinsworthEtAl_2016.php. All
data and code are available at FigShare project number 12040: Ecosystems
model code and scripts (DOI 10.6084/m9.figshare.3081127); Bleaching on
the GBR data release (DOI 10.6084/m9.figshare.3081127); Physiology and
gene expression data (DOI 10.6084/m9.figshare.3081064). D.O. is
currently employed by Boehringer Ingelheim, Fremont, CA. The authors
declare no competing financial interests.
NR 23
TC 15
Z9 16
U1 97
U2 233
PU AMER ASSOC ADVANCEMENT SCIENCE
PI WASHINGTON
PA 1200 NEW YORK AVE, NW, WASHINGTON, DC 20005 USA
SN 0036-8075
EI 1095-9203
J9 SCIENCE
JI Science
PD APR 15
PY 2016
VL 352
IS 6283
BP 338
EP 342
DI 10.1126/science.aac7125
PG 5
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DJ1UK
UT WOS:000373990100039
PM 27081069
ER
PT J
AU Yang, YB
Liu, SQ
Zhao, H
Yang, WY
Wu, R
Huang, QZ
Zhou, D
Du, HL
Wang, CS
Yang, YC
Xu, H
Zhu, JL
Gourdon, O
Vogel, S
Yang, JB
AF Yang, Y. B.
Liu, S. Q.
Zhao, H.
Yang, W. Y.
Wu, R.
Huang, Q. Z.
Zhou, D.
Du, H. L.
Wang, C. S.
Yang, Y. C.
Xu, H.
Zhu, J. L.
Gourdon, O.
Vogel, S.
Yang, J. B.
TI Magnetic structure and phase transition of Ni2Mn1.48Sb0.52 magnetic
shape memory compound
SO SCRIPTA MATERIALIA
LA English
DT Article
DE Neutron diffraction; Shape memory compound; Martensitic phase
transition; Exchange bias effect
ID MARTENSITIC TRANSFORMATIONS; HEUSLER ALLOY
AB A comprehensive study of the structural and magnetic properties of the Ni2Mn1.48Sb0.52 compound is presented using neutron diffraction and magnetic measurements. It is found that Mn atoms on 4a and 4b sites are ferrimagnetic coupled in the austenitic phase. At 300 K, the magnetic moments of Mn (4a) and Mn (4b) are determined to be 2.72(3) mu(B) and -2.67(5) mu(B), respectively. From 260 K to 4 K, the compound is in martensite phase and the magnetic moments of Mn (2a), Mn (2f), Mn (2b), Mn (2e) at 4 K are 2.2(5) mu(B), 2.3(5) Pat -2.1(5) mu(B), and -2.6(5) mu(B), respectively. (C) 2016 Elsevier Ltd. All rights reserved.
C1 [Yang, Y. B.; Liu, S. Q.; Zhao, H.; Yang, W. Y.; Wu, R.; Zhou, D.; Du, H. L.; Wang, C. S.; Yang, Y. C.; Yang, J. B.] Peking Univ, Sch Phys, State Key Lab Mesoscop Phys, Beijing 100871, Peoples R China.
[Yang, J. B.] Collaborat Innovat Ctr Quantum Matter, Beijing 100871, Peoples R China.
[Huang, Q. Z.] NIST, Gaithersburg, MD 20878 USA.
[Xu, H.; Zhu, J. L.; Gourdon, O.; Vogel, S.] Los Alamos Natl Lab, POB 1663, Los Alamos, NM 87545 USA.
RP Yang, JB (reprint author), Peking Univ, Sch Phys, State Key Lab Mesoscop Phys, Beijing 100871, Peoples R China.
EM jbyang@pku.edu.cn
OI Xu, Hongwu/0000-0002-0793-6923
FU National Natural Science Foundation of China [51371009, 50971003,
51171001]; National Basic Research Program of China (MOST of China)
[2010CB833104]
FX This work was supported by the National Natural Science Foundation of
China (Grant Nos. 51371009, 50971003 and 51171001), the National Basic
Research Program of China (No. 2010CB833104, MOST of China).
NR 28
TC 1
Z9 1
U1 8
U2 27
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 1359-6462
J9 SCRIPTA MATER
JI Scr. Mater.
PD APR 15
PY 2016
VL 116
BP 31
EP 35
DI 10.1016/j.scriptamat.2016.01.028
PG 5
WC Nanoscience & Nanotechnology; Materials Science, Multidisciplinary;
Metallurgy & Metallurgical Engineering
SC Science & Technology - Other Topics; Materials Science; Metallurgy &
Metallurgical Engineering
GA DH1QP
UT WOS:000372560300007
ER
PT J
AU Bokusheva, R
Kogan, F
Vitkovskaya, I
Conradt, S
Batyrbayeva, M
AF Bokusheva, R.
Kogan, F.
Vitkovskaya, I.
Conradt, S.
Batyrbayeva, M.
TI Satellite-based vegetation health indices as a criteria for insuring
against drought-related yield losses
SO AGRICULTURAL AND FOREST METEOROLOGY
LA English
DT Article
DE Satellite-based vegetation health index; Drought-related yield losses;
Wheat; Agricultural insurance; Copula approach
ID SOUTHERN AFRICA; AVHRR DATA; INSURANCE
AB This paper considers the use of indices built on the basis of remote-sensing data for crop insurance purposes. In our analysis, we compare the capacity of two satellite-based vegetation health (VH) indices, the vegetation condition index (VCI) and the temperature condition index (TCI), measured for important periods of the crop vegetation to predict farmers' wheat yields in two main grain producing regions of Kazakhstan. The selected indices are used for the design of index-based insurance contracts. The dependence of wheat yields on vegetation conditions as measured by VCI and TCI, is modeled by applying the copula approach. Our empirical results for 47 grain-producing farms in the Northern Kazakhstan show that insurance contracts built on VH indices can provide substantial risk reductions for a group of farms, though on average for the whole sample, risk reductions were found to be moderate. The study results suggest that the effectiveness of insurance contracts can be improved using satellite data of higher resolutions and measuring indices at more disaggregated levels. (C) 2016 Elsevier B.V. All rights reserved.
C1 [Bokusheva, R.; Conradt, S.] Swiss Fed Inst Technol, Swiss Fed Inst Technol, Zurich, Switzerland.
[Kogan, F.] Natl Space Agcy Republ Kazakhstan, Space Res Inst, Astana, Kazakhstan.
[Vitkovskaya, I.; Batyrbayeva, M.] NOAA, Natl Environm Satellite Data & Informat Serv, Silver Spring, MD USA.
RP Bokusheva, R (reprint author), Swiss Fed Inst Technol, Swiss Fed Inst Technol, Zurich, Switzerland.
EM bokushev@ethz.ch
RI Kogan, Felix/F-5600-2010
OI Kogan, Felix/0000-0001-8216-900X
FU Swiss National Science Foundation within its Program of Scientific
Co-operation between Eastern Europe and Switzerland (SCOPES)
FX The authors thank financial support of the Swiss National Science
Foundation within its Program of Scientific Co-operation between Eastern
Europe and Switzerland (SCOPES).
NR 31
TC 0
Z9 0
U1 10
U2 28
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0168-1923
EI 1873-2240
J9 AGR FOREST METEOROL
JI Agric. For. Meteorol.
PD APR 15
PY 2016
VL 220
BP 200
EP 206
DI 10.1016/j.agrformet.2015.12.066
PG 7
WC Agronomy; Forestry; Meteorology & Atmospheric Sciences
SC Agriculture; Forestry; Meteorology & Atmospheric Sciences
GA DG9EH
UT WOS:000372385100019
ER
PT J
AU Del Buffa, S
Fratini, E
Ridi, F
Faraone, A
Baglioni, P
AF Del Buffa, Stefano
Fratini, Emiliano
Ridi, Francesca
Faraone, Antonio
Baglioni, Piero
TI State of Water in Hydrating Tricalcium Silicate Pastes: The Effect of a
Cellulose Ether
SO JOURNAL OF PHYSICAL CHEMISTRY C
LA English
DT Article
ID ELASTIC NEUTRON-SCATTERING; C-S-H; CEMENT PASTE; CALCIUM SILICATE;
POROUS-GLASS; DYNAMICS; KINETICS; MICROSTRUCTURE; CALORIMETRY; MOTIONS
AB Time-dependent quasi-elastic neutron scattering (QENS) and differential scanning calorimetry (DSC) were applied to study water dynamics and hydration kinetic of the hydration reaction of tricalcium silicate in the presence of a methyl hydroxyethyl cellulose (MHEC) additive. The translational dynamics of the water confined in the developing hydrated calcium silicate matrix was probed at the molecular scale by QENS during the first 4 days, while the evolution of the matrix porosity and the hydration kinetics were determined up to 28 days of hydration by differential scanning calorimetry. The application of the boundary nucleation and growth model consistently improved the hydration kinetics picture, usually obtained from the application of the classical Avrami-Erove'ev model, allowing the evaluation of the individual contributions of nucleation and growth. over the entire hydration process. In the presence of the cellulose ether the nature of the nucleation process is strongly modified, approaching a "spatially random" hydration mechanism. The water contained in the nanometric porosity of the hydrated calcium silicate matrix, which is fundamental for the efficiency of the hydration process, results increased when MHEC is added, leading to a delay of the onset of the hydration process and the enhancement of the efficiency of the reaction.
C1 [Del Buffa, Stefano; Fratini, Emiliano; Ridi, Francesca; Baglioni, Piero] Univ Florence, Dept Chem Ugo Schiff, Via Lastruccia 3, I-50019 Florence, Italy.
[Del Buffa, Stefano; Fratini, Emiliano; Ridi, Francesca; Baglioni, Piero] Univ Florence, CSGI, Via Lastruccia 3, I-50019 Florence, Italy.
[Faraone, Antonio] NIST, Ctr Neutron Res, 100 Bur Dr, Gaithersburg, MD 20899 USA.
[Faraone, Antonio] Univ Maryland, Dept Mat Sci & Engn, College Pk, MD 20742 USA.
RP Baglioni, P (reprint author), Univ Florence, Dept Chem Ugo Schiff, Via Lastruccia 3, I-50019 Florence, Italy.; Baglioni, P (reprint author), Univ Florence, CSGI, Via Lastruccia 3, I-50019 Florence, Italy.
EM piero.baglioni@unifi.it
RI Baglioni, Piero/B-1208-2011
OI Baglioni, Piero/0000-0003-1312-8700
FU Ministero dell'Istruzione, dell'Universita e della Ricerca Scientifica
(MiUR); Consorzio Interuniversitario per lo Sviluppo dei Sistemi a
Grande Interfase (CSGI)
FX S.D.B., E.F., F.R., and P.B. acknowledge financial support from
Ministero dell'Istruzione, dell'Universita e della Ricerca Scientifica
(MiUR), and Consorzio Interuniversitario per lo Sviluppo dei Sistemi a
Grande Interfase (CSGI). Authors kindly acknowledge Dr. J. M. Zanotti
and R. Connatser for the help with the setup of the QENS spectrometer.
Dr. J. M. Zanotti is also acknowledged for providing the data reduction
routines. E.F. acknowledges Dr. I. Ciullini for the practical help
during the QENS experiment.
NR 38
TC 1
Z9 1
U1 4
U2 8
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 APR 14
PY 2016
VL 120
IS 14
BP 7612
EP 7620
DI 10.1021/acs.jpcc.6b00691
PG 9
WC Chemistry, Physical; Nanoscience & Nanotechnology; Materials Science,
Multidisciplinary
SC Chemistry; Science & Technology - Other Topics; Materials Science
GA DJ7ZJ
UT WOS:000374431400019
ER
PT J
AU Rubinson, KA
Buhlmann, P
Allison, TC
AF Rubinson, Kenneth A.
Buehlmann, Philippe
Allison, Thomas C.
TI One-dimensional ionic self-assembly in a fluorous solution: the
structure of tetra-n-butylammonium
tetrakis[3,5-bis(perfluorohexyl)phenyl]borate in
perfluoromethylcyclohexane by small-angle neutron scattering (SANS)
SO PHYSICAL CHEMISTRY CHEMICAL PHYSICS
LA English
DT Article
ID POTENTIOMETRIC SENSORS; MEMBRANES; SOLVENT; SELECTIVITY; IONOPHORES;
CATALYSIS; SYSTEMS
AB Fluorous liquids are the least polarizable condensed phases known, and their nonpolar members form solutions with conditions the closest to being in vacuo. A soluble salt consisting of a large fluorophilic anion, tetrakis[3,5-bis(perfluorohexyl)phenyl]borate, and its counterion, tetra-n-butylammonium, dissolved in perfluoromethylcyclohexane produces ionic solutions with extremely low conductivity. These solutions were subjected to small-angle neutron scattering (SANS) to ascertain the solute structure. At concentrations of 9% mass fraction, the fluorophilic electrolyte forms straight, long (>160 angstrom) self-assembled structures that are, in essence, long, homogeneous cylinders. Molecular models were made assuming a requirement for electroneutrality on the shortest length scale possible. This shows a structure formed from a stack of alternating anions and cations, and the structures fit the experimental scattering well. At the lower concentration of 1%, the stacks of ion pairs are shorter and eventually break up to form solitary ion pairs in the solution. These characteristics suggest such conditions provide an interesting new way to form long, self-assembling ionic nanostructures with single-molecule diameters in free solution onto which various moieties could be attached.
C1 [Rubinson, Kenneth A.] NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Rubinson, Kenneth A.] Wright State Univ, Dept Biochem & Mol Biol, Dayton, OH 45435 USA.
[Buehlmann, Philippe] Univ Minnesota, Dept Chem, 207 Pleasant St SE, Minneapolis, MN 55455 USA.
[Allison, Thomas C.] NIST, Computat Informat Res Grp, Mat Measurement Lab, Gaithersburg, MD 20899 USA.
RP Rubinson, KA (reprint author), NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.; Rubinson, KA (reprint author), Wright State Univ, Dept Biochem & Mol Biol, Dayton, OH 45435 USA.
EM Rubinson@nist.gov; buhlmann@umn.edu; thomas.allison@nist.gov
NR 30
TC 1
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U1 4
U2 11
PU ROYAL SOC CHEMISTRY
PI CAMBRIDGE
PA THOMAS GRAHAM HOUSE, SCIENCE PARK, MILTON RD, CAMBRIDGE CB4 0WF, CAMBS,
ENGLAND
SN 1463-9076
EI 1463-9084
J9 PHYS CHEM CHEM PHYS
JI Phys. Chem. Chem. Phys.
PD APR 14
PY 2016
VL 18
IS 14
BP 9470
EP 9475
DI 10.1039/c6cp00393a
PG 6
WC Chemistry, Physical; Physics, Atomic, Molecular & Chemical
SC Chemistry; Physics
GA DI5WC
UT WOS:000373570200019
PM 26980055
ER
PT J
AU Dubernet, ML
Antony, BK
Ba, YA
Babikov, YL
Bartschat, K
Boudon, V
Braams, BJ
Chung, HK
Daniel, F
Delahaye, F
Del Zanna, G
de Urquijo, J
Dimitrijevic, MS
Domaracka, A
Doronin, M
Drouin, BJ
Endres, CP
Fazliev, AZ
Gagarin, SV
Gordon, IE
Gratier, P
Heiter, U
Hill, C
Jevremovic, D
Joblin, C
Kasprzak, A
Krishnakumar, E
Leto, G
Loboda, PA
Louge, T
Maclot, S
Marinkovic, BP
Markwick, A
Marquart, T
Mason, HE
Mason, NJ
Mendoza, C
Mihajlov, AA
Millar, TJ
Moreau, N
Mulas, G
Pakhomov, Y
Palmeri, P
Pancheshnyi, S
Perevalov, VI
Piskunov, N
Postler, J
Quinet, P
Quintas-Sanchez, E
Ralchenko, Y
Rhee, YJ
Rixon, G
Rothman, LS
Roueff, E
Ryabchikova, T
Sahal-Brechot, S
Scheier, P
Schlemmer, S
Schmitt, B
Stempels, E
Tashkun, S
Tennyson, J
Tyuterev, VG
Vujcic, V
Wakelam, V
Walton, NA
Zatsarinny, O
Zeippen, CJ
Zwolf, CM
AF Dubernet, M. L.
Antony, B. K.
Ba, Y. A.
Babikov, Yu L.
Bartschat, K.
Boudon, V.
Braams, B. J.
Chung, H-K
Daniel, F.
Delahaye, F.
Del Zanna, G.
de Urquijo, J.
Dimitrijevic, M. S.
Domaracka, A.
Doronin, M.
Drouin, B. J.
Endres, C. P.
Fazliev, A. Z.
Gagarin, S. V.
Gordon, I. E.
Gratier, P.
Heiter, U.
Hill, C.
Jevremovic, D.
Joblin, C.
Kasprzak, A.
Krishnakumar, E.
Leto, G.
Loboda, P. A.
Louge, T.
Maclot, S.
Marinkovic, B. P.
Markwick, A.
Marquart, T.
Mason, H. E.
Mason, N. J.
Mendoza, C.
Mihajlov, A. A.
Millar, T. J.
Moreau, N.
Mulas, G.
Pakhomov, Yu
Palmeri, P.
Pancheshnyi, S.
Perevalov, V. I.
Piskunov, N.
Postler, J.
Quinet, P.
Quintas-Sanchez, E.
Ralchenko, Yu
Rhee, Y-J
Rixon, G.
Rothman, L. S.
Roueff, E.
Ryabchikova, T.
Sahal-Brechot, S.
Scheier, P.
Schlemmer, S.
Schmitt, B.
Stempels, E.
Tashkun, S.
Tennyson, J.
Tyuterev, Vl G.
Vujcic, V.
Wakelam, V.
Walton, N. A.
Zatsarinny, O.
Zeippen, C. J.
Zwoelf, C. M.
TI The virtual atomic and molecular data centre (VAMDC) consortium
SO JOURNAL OF PHYSICS B-ATOMIC MOLECULAR AND OPTICAL PHYSICS
LA English
DT Article
DE databases; atoms; molecules; spectroscopy; kinetic data; astrophysics
ID LOW-ENERGY-ELECTRON; LINE-DATA-BASE; IRRADIATION EXPERIMENTS RELEVANT;
STIMULATED RAMAN-SPECTROSCOPY; HIGH-RESOLUTION SPECTROSCOPY; R-MATRIX
METHOD; CW-CAVITY RING; ION IRRADIATION; CROSS-SECTIONS; COLLISIONAL
DATABASE
AB The Virtual Atomic and Molecular Data Centre (VAMDC) Consortium is a worldwide consortium which federates atomic and molecular databases through an e-science infrastructure and an organisation to support this activity. About 90% of the inter-connected databases handle data that are used for the interpretation of astronomical spectra and for modelling in many fields of astrophysics. Recently the VAMDC Consortium has connected databases from the radiation damage and the plasma communities, as well as promoting the publication of data from Indian institutes. This paper describes how the VAMDC Consortium is organised for the optimal distribution of atomic and molecular data for scientific research. It is noted that the VAMDC Consortium strongly advocates that authors of research papers using data cite the original experimental and theoretical papers as well as the relevant databases.
C1 [Dubernet, M. L.; Ba, Y. A.; Delahaye, F.; Dimitrijevic, M. S.; Doronin, M.; Moreau, N.; Quintas-Sanchez, E.; Roueff, E.; Sahal-Brechot, S.; Zeippen, C. J.; Zwoelf, C. M.] Univ Paris 06, Univ Sorbonne, CNRS, LERMA,Observ Paris,PSL Res Univ, 5 Pl Janssen, F-92190 Meudon, France.
[Antony, B. K.] Indian Sch Mines, Dept Appl Phys, Dhanbad 826004, Bihar, India.
[Babikov, Yu L.; Fazliev, A. Z.; Perevalov, V. I.; Tashkun, S.] Russian Acad Sci, Inst Atmospher Opt, Zuev Sq 1, Tomsk 634021, Russia.
[Babikov, Yu L.] Tomsk State Univ, Tomsk 634050, Russia.
[Bartschat, K.; Zatsarinny, O.] Drake Univ, Dept Phys & Astron, Des Moines, IA 50311 USA.
[Boudon, V.] Univ Bourgogne Franche Comte, CNRS, UMR 6303, Lab Interdisciplinaire Carnot Bourgogne, 9 Ave Alain Savary,BP 47 870, F-21078 Dijon, France.
[Braams, B. J.; Chung, H-K] IAEA, Vienna Int Ctr, Div Phys & Chem Sci, Nucl Data Sect, A-1400 Vienna, Austria.
[Daniel, F.; Schmitt, B.] Univ Grenoble Alpes, CNRS, IPAG, F-38000 Grenoble, France.
[Del Zanna, G.; Mason, H. E.] Ctr Math Sci, DAMTP, Wilberforce Rd, Cambridge CB3 0WA, England.
[de Urquijo, J.] Univ Nacl Autonoma Mexico, Inst Ciencias Fis, POB 48-3, Cuernavaca 62251, Morelos, Mexico.
[Dimitrijevic, M. S.; Jevremovic, D.; Vujcic, V.] Astron Observ, Volgina 7, Belgrade 11060, Serbia.
[Domaracka, A.; Maclot, S.] UCN, ENSICAEN, CNRS, CIMAP,UMR 6252,CEA, Bd Henri Becquerel,BP 5133, F-14070 Caen 5, France.
[Drouin, B. J.] CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91109 USA.
[Endres, C. P.] Max Planck Inst Extraterr Phys, Giessenbachstr, D-85748 Garching, Germany.
[Gagarin, S. V.; Loboda, P. A.] Russian Fed Nucl Ctr All Russian Inst Tech Phys R, Snezhinsk, Russia.
[Gordon, I. E.; Rothman, L. S.] Harvard Smithsonian Ctr Astrophys, Atom & Mol Phys Div, MS50,60 Garden St, Cambridge, MA 02138 USA.
[Gratier, P.; Wakelam, V.] Univ Bordeaux, LAB, UMR 5804, F-33270 Florac, France.
[Gratier, P.; Wakelam, V.] CNRS, LAB, UMR 5804, F-33270 Florac, France.
[Heiter, U.; Marquart, T.; Piskunov, N.; Stempels, E.] Uppsala Univ, Dept Phys & Astron, Box 516, SE-75120 Uppsala, Sweden.
[Hill, C.; Tennyson, J.] UCL, Dept Phys & Astron, Mortimer St, London WC1E 6BT, England.
[Joblin, C.; Louge, T.; Mulas, G.] Univ Toulouse, UPS OMP, CNRS, Inst Rech Astrophys & Planetol, 9 Av Colonel Roche, F-31028 Toulouse 4, France.
[Kasprzak, A.] Observ Paris, SRCV, 61 Av Denfert Rochereau, F-75014 Paris, France.
[Krishnakumar, E.] Tata Inst Fundamental Res, Dept Nucl & Atom Phys, Homi Bhabha Rd, Bombay 400005, Maharashtra, India.
[Leto, G.] INAF Osservatorio Astrofis Catania, Via S Sofia 78, I-95123 Catania, Italy.
[Loboda, P. A.] Natl Res Nucl Univ, Moscow Engn Phys Inst MEPhI, Moscow, Russia.
[Maclot, S.] Univ Caen Normandie, Esplanade Paix, CS 14032, F-14032 Caen 5, France.
[Marinkovic, B. P.; Mihajlov, A. A.] Univ Belgrade, Inst Phys Belgrade, POB 57, Belgrade 11001, Serbia.
[Markwick, A.] Univ Manchester, Sch Phys & Astron, Jodrell Bank Ctr Astrophys, Oxford Rd, Manchester M13 9PL, Lancs, England.
[Mason, N. J.] Open Univ, Dept Phys Sci, Walton Hall, Milton Keynes MK7 6AA, Bucks, England.
[Mendoza, C.] IVIC, Ctr Fis, POB 20632, Caracas 1020A, Venezuela.
[Millar, T. J.] Queens Univ Belfast, Sch Math & Phys, Univ Rd, Belfast BT7 1NN, Antrim, North Ireland.
[Mulas, G.] Osservatorio Astron Cagliari, Ist Nazl AstroFis, Via Sci 5, I-09047 Selargius, CA, Italy.
[Pakhomov, Yu; Ryabchikova, T.] RAS, Inst Astron, Pyatnitskaya 48, Moscow 119017, Russia.
[Palmeri, P.; Quinet, P.] Univ Mons, Phys Atom & Astrophys, B-7000 Mons, Belgium.
[Pancheshnyi, S.] ABB Corp Res, Segelhofstr 1K, CH-5405 Baden, Switzerland.
[Postler, J.; Scheier, P.] Univ Innsbruck, Inst Ion Phys & Appl Phys, Technikerstr 25-3, A-6020 Innsbruck, Austria.
[Quinet, P.] Univ Liege, IPNAS, B-4000 Liege, Belgium.
[Ralchenko, Yu] NIST, Atom Spect Grp, Gaithersburg, MD 20899 USA.
[Rhee, Y-J] Korea Atom Energy Res Inst, Nucl Data Ctr, Taejon 305353, South Korea.
[Rixon, G.; Walton, N. A.] Univ Cambridge, Inst Astron, Madingley Rd, Cambridge CB3 0HA, England.
[Schlemmer, S.] Univ Cologne, Inst Phys 1, zulpicher Str 77, D-50937 Kln, Germany.
[Tyuterev, Vl G.] Univ Reims, GSMA, UMR CNRS 7331, Reims, France.
[Vujcic, V.] Univ Belgrade, Fac Org Sci, Jove Ilica 33, Belgrade 11000, Serbia.
RP Dubernet, ML (reprint author), Univ Paris 06, Univ Sorbonne, CNRS, LERMA,Observ Paris,PSL Res Univ, 5 Pl Janssen, F-92190 Meudon, France.
EM marie-lise.dubernet@obspm.fr
RI Tennyson, Jonathan/I-2222-2012; Scheier, Paul/E-3088-2010; Tashkun,
Sergey/E-8682-2014; Marinkovic, Bratislav/D-3589-2012; Babikov,
Yurii/E-8686-2014; Antony, Bobby Kachappilly/H-5302-2015; Pakhomov,
Yury/B-5172-2014;
OI Millar, Tom/0000-0001-5178-3656; Tennyson, Jonathan/0000-0002-4994-5238;
Marinkovic, Bratislav/0000-0002-6904-6360; Antony, Bobby
Kachappilly/0000-0003-2073-9681; Leto, Giuseppe/0000-0002-0040-5011;
Wakelam, Valentine/0000-0001-9676-2605; Mulas,
Giacomo/0000-0003-0602-6669
FU VAMDC project; SUP@VAMDC project [INFRA-2008-1.2.2, 239108, 313284];
Paris Astronomical Data Center; UK Science and Technology Facilities
Council (STFC) [ST/M007731/1, ST/M007774/1, ST/M007766/1]; NASA; UK
STFC; SOLID (First European SOLar Irradiance Data Exploitation), a
collaborative SPACE Project under the Seventh Framework Programme (FP7)
of the European Commission [313188]; Russian Foundation for Basic
Research, RFBR grant [14-07-00863]; NASA Planetary Atmospheres Grant
[NNX13AI59G]; ERC Advanced Investigator Project [267219]; United States
National Science Foundation [PHY-1403245, PHY-1520970]; Dept. of Science
and Technology (DST), Govt. of India; Austrian Science Fund (FWF)
[P26635]; Nano-IBCT COST Action MP1002 (Nano-scale Insights into Ion
Beam Cancer Therapy); LIA SAMIA; Tomsk State University D Mendeleev
funding program; Ministry of Education, Science and Technological
Development of Republic of Serbia [III44002, 176002, 171020]; XSEDE
supercomputer allocation [PHY-090031]
FX Support for VAMDC has been provided through the VAMDC and the SUP@VAMDC
projects 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 and INFRA-2012
Scientific Data Infrastructure. Grant Agreement numbers: 239108 and
313284. In addition we acknowledge support from Paris Astronomical Data
Center. The UK nodes acknowledge support from the UK Science and
Technology Facilities Council (STFC) under grants ST/M007731/1,
ST/M007774/1 and ST/M007766/1. Portions of the research described in
this paper were performed at the Jet Propulsion Laboratory, California
Institute of Technology, under contract with the National Aeronautics
and Space Administration. The NIST ASD development is supported in part
by NASA. GDZ and HEM work on CHIANTI has been supported by the UK STFC
and SOLID (First European SOLar Irradiance Data Exploitation), a
collaborative SPACE Project under the Seventh Framework Programme
(FP7/2007-2013) of the European Commission under Grant Agreement N
313188. The Spectr-W3 project activities are currently
supported in part by the Russian Foundation for Basic Research, RFBR
grant Nr. 14-07-00863. LSR and IEG wish to thank the support from NASA
Planetary Atmospheres Grant NNX13AI59G. ExoMol is supported by ERC
Advanced Investigator Project 267219. ZB and KB acknowledge support from
the United States National Science Foundation under grants PHY-1403245
and PHY-1520970, and by the XSEDE supercomputer allocation PHY-090031.
AD and SM thank P Rousseau and B A Huber for fruitful discussions,
Quentin Marie for the preparing of the RADAM-ION database website
structure and Universite de Caen Normandie for hosting the website. BA
is supported by the Dept. of Science and Technology (DST), Govt. of
India. Part of this research was supported by the Austrian Science Fund
(FWF): P26635. Support from Nano-IBCT COST Action MP1002 (Nano-scale
Insights into Ion Beam Cancer Therapy) is also acknowledged. YLB and VGT
acknowledge support from LIA SAMIA and from Tomsk State University D
Mendeleev funding program. Belgrade node activities and the
corresponding research are supported by projects III44002, 176002 and
171020 of the Ministry of Education, Science and Technological
Development of Republic of Serbia.
NR 162
TC 10
Z9 10
U1 11
U2 30
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 APR 14
PY 2016
VL 49
IS 7
AR 074003
DI 10.1088/0953-4075/49/7/074003
PG 18
WC Optics; Physics, Atomic, Molecular & Chemical
SC Optics; Physics
GA DH6OS
UT WOS:000372911000003
ER
PT J
AU Hammouda, B
AF Hammouda, Boualem
TI Form Factors for Branched Polymers with Excluded Volume
SO JOURNAL OF RESEARCH OF THE NATIONAL INSTITUTE OF STANDARDS AND
TECHNOLOGY
LA English
DT Article
DE dendrimers; excluded volume effect; looping branches; polymer ring;
small-angle scattering form factors; star-branched polymers
ID ANGLE NEUTRON-SCATTERING; STAR; MACROMOLECULES; DILUTE; CHAIN
AB The form factors for star-branched polymers with linear branches or with looping branches are calculated. The effect of chain swelling excluded volume is incorporated through an excluded volume parameter approach. The form factor for ring polymers is also included, since it is nicely derived as a special case. Furthermore, the form factor for dendrimers with excluded volume is also calculated. In order to evaluate the form factor for stars with looping branches, the multivariate Gaussian function is used to close the looping branches. Analytical results are possible in the Gaussian chain case (i.e., with no excluded volume), but the calculations are left in a form involving summations over monomers when the general case incorporates excluded volume.
C1 [Hammouda, Boualem] NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
RP Hammouda, B (reprint author), NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
EM hammouda@nist.gov
FU National Science Foundation [DMR-1508249]
FX Informative discussions with Vivek Prabhu and Wei-Ren Chen are
appreciated. This work is based upon activities supported in part by the
National Science Foundation under Agreement No. DMR-1508249.
NR 18
TC 1
Z9 1
U1 5
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 APR 13
PY 2016
VL 121
BP 139
EP 164
DI 10.6028/jres.121.006
PG 26
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA DQ5BE
UT WOS:000379218600001
ER
PT J
AU Williams, TS
Orloff, ND
Baker, JS
Miller, SG
Natarajan, B
Obrzut, J
McCorkle, LS
Lebron-Colon, M
Gaier, J
Meador, MA
Liddle, JA
AF Williams, Tiffany S.
Orloff, Nathan D.
Baker, James S.
Miller, Sandi G.
Natarajan, Bharath
Obrzut, Jan
McCorkle, Linda S.
Lebron-Colon, Marisabel
Gaier, James
Meador, Michael A.
Liddle, J. Alexander
TI Trade-off between the Mechanical Strength and Microwave Electrical
Properties of Functionalized and Irradiated Carbon Nanotube Sheets
SO ACS APPLIED MATERIALS & INTERFACES
LA English
DT Article
DE multiwalled carbon nanotubes; carbon nanotube sheets; chemical
functionalization; tensile strength; electrical conductivity; microwave
spectroscopy; electron beam irradiation
ID SHEET/BISMALEIMIDE NANOCOMPOSITES; HIGH-PERFORMANCE; CONDUCTIVITY;
BUNDLES; COMPOSITES; FIBERS; YARNS; BEAM
AB Carbon nanotube (CNT) sheets represent a novel implementation of CNTs that enable the tailoring of electrical and mechanical properties for applications in the automotive and aerospace industries. Small molecule functionalization and postprocessing techniques, such as irradiation with high-energy particles, are methods that can enhance the mechanical properties of CNTs. However, the effect that these modifications have on the electrical conduction mechanisms has not been extensively explored. By characterizing the mechanical and electrical properties of multiwalled carbon nanotube (MWCNT) sheets with different functional groups and irradiation doses, we can expand our insights into the extent of the trade-off that exists between mechanical strength and electrical conductivity for commercially available CNT sheets. Such insights allow for the optimization of design pathways for engineering applications that require a balance of material property enhancements.
C1 [Williams, Tiffany S.; Miller, Sandi G.; Lebron-Colon, Marisabel; Gaier, James; Meador, Michael A.] NASA, John H Glenn Res Ctr Lewis Field, Cleveland, OH 44135 USA.
[Orloff, Nathan D.; Obrzut, Jan] NIST, Mat Measurement Lab, Gaithersburg, MD 20899 USA.
[Orloff, Nathan D.; Liddle, J. Alexander] NIST, Commun Technol Lab, Boulder, CO 80305 USA.
[Baker, James S.] NASA, Postdoctoral Program, Glenn Res Ctr, Cleveland, OH 44135 USA.
[Natarajan, Bharath] NIST, Ctr Nanoscale Sci & Technol, Gaithersburg, MD 20899 USA.
[McCorkle, Linda S.] Ohio Aerosp Inst, Cleveland, OH 44142 USA.
RP Williams, TS (reprint author), NASA, John H Glenn Res Ctr Lewis Field, Cleveland, OH 44135 USA.
EM tiffany.s.williams@nasa.gov
RI Liddle, James/A-4867-2013;
OI Liddle, James/0000-0002-2508-7910; Obrzut, Jan/0000-0001-6667-9712
FU NASA Game Changing Development Program/Nanotechnology Project; NASA
Postdoctoral Program at the NASA Glenn Research Center - Oak Ridge
Associated Universities; Rice University [70NANB12H188]; National
Institute of Standards and Technology [70NANB12H188]
FX This effort was funded through the NASA Game Changing Development
Program/Nanotechnology Project. Support was also received from the
following sources: the NASA Postdoctoral Program at the NASA Glenn
Research Center sponsored by Oak Ridge Associated Universities, and a
Cooperative Research Agreement between Rice University and the National
Institute of Standards and Technology (grant 70NANB12H188). We thank Dr.
Jeffrey Eldrige for assistance with Raman Spectroscopy and Nathan
Wilmoth for his assistance with mechanical testing. Microwave
spectroscopy measurements were carried out at the NIST Materials
Measurement Laboratory in support of the National Nano technology
Initiative.
NR 35
TC 0
Z9 0
U1 3
U2 8
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 APR 13
PY 2016
VL 8
IS 14
BP 9327
EP 9334
DI 10.1021/acsami.5b12303
PG 8
WC Nanoscience & Nanotechnology; Materials Science, Multidisciplinary
SC Science & Technology - Other Topics; Materials Science
GA DJ5UF
UT WOS:000374274900057
PM 27044063
ER
PT J
AU Hardison, DR
Holland, WC
McCall, JR
Bourdelais, AJ
Baden, DG
Darius, HT
Chinain, M
Tester, PA
Shea, D
Quintana, HAF
Morris, JA
Litaker, RW
AF Hardison, D. Ransom
Holland, William C.
McCall, Jennifer R.
Bourdelais, Andrea J.
Baden, Daniel G.
Darius, H. Taiana
Chinain, Mireille
Tester, Patricia A.
Shea, Damian
Quintana, Harold A. Flores
Morris, James A., Jr.
Litaker, R. Wayne
TI Fluorescent Receptor Binding Assay for Detecting Ciguatoxins in Fish
SO PLOS ONE
LA English
DT Article
ID SENSITIVE SODIUM-CHANNELS; CELL-BASED ASSAY; SITE 5; CIGUATERA;
BREVETOXINS; TOXINS; TOXICITY; LIONFISH; PACIFIC; ISLANDS
AB Ciguatera fish poisoning is an illness suffered by > 50,000 people yearly after consumption of fish containing ciguatoxins (CTXs). One of the current methodologies to detect ciguatoxins in fish is a radiolabeled receptor binding assay (RBA((R))). However, the license requirements and regulations pertaining to radioisotope utilization can limit the applicability of the RBA((R)) in certain labs. A fluorescence based receptor binding assay (RBA((F))) was developed to provide an alternative method of screening fish samples for CTXs in facilities not certified to use radioisotopes. The new assay is based on competition binding between CTXs and fluorescently labeled brevetoxin-2 (BODIPY (R)-PbTx-2) for voltage-gated sodium channel receptors at site 5 instead of a radiolabeled brevetoxin. Responses were linear in fish tissues spiked from 0.1 to 1.0 ppb with Pacific ciguatoxin-3C (P-CTX-3C) with a detection limit of 0.075 ppb. Carribean ciguatoxins were confirmed in Caribbean fish by LC-MS/MS analysis of the regional biomarker (C-CTX-1). Fish (N = 61) of six different species were screened using the RBA((F)). Results for corresponding samples analyzed using the neuroblastoma cell-based assay (CBA-N2a) correlated well (R-2 = 0.71) with those of the RBA((F)), given the low levels of CTX present in positive fish. Data analyses also showed the resulting toxicity levels of P-CTX-3C equivalents determined by CBA-N2a were consistently lower than the RBA((F)) affinities expressed as% binding equivalents, indicating that a given amount of toxin bound to the site 5 receptors translates into corresponding lower cytotoxicity. Consequently, the RBA((F)), which takes approximately two hours to perform, provides a generous estimate relative to the widely used CBA-N2a which requires 2.5 days to complete. Other RBA((F)) advantages include the long-term(> 5 years) stability of the BODIPY (R)-PbTx-2 and having similar results as the commonly used RBA((R)). The RBA((F)) is cost-effective, allows high sample throughput, and is well-suited for routine CTX monitoring programs.
C1 [Hardison, D. Ransom; Holland, William C.; Tester, Patricia A.; Morris, James A., Jr.; Litaker, R. Wayne] NOAA, Ctr Coastal Fisheries & Habitat Res, Beaufort, NC USA.
[McCall, Jennifer R.; Bourdelais, Andrea J.; Baden, Daniel G.] Univ N Carolina, MARBIONC CREST Res Pk, Wilmington, NC 28401 USA.
[McCall, Jennifer R.] SeaTox Res Inc, UNCW CREST Res Pk, Wilmington, NC USA.
[Darius, H. Taiana; Chinain, Mireille] ILM, UMR EIO 241, Lab Tox Microalgae, Papeete, Tahiti, Fr Polynesia.
[Tester, Patricia A.] JHT Inc, Orlando, FL USA.
[Shea, Damian] N Carolina State Univ, Environm Chem & Toxicol Lab, Raleigh, NC 27695 USA.
[Quintana, Harold A. Flores] US FDA, Div Seafood Sci & Technol, Gulf Coast Seafood Lab, Dauphin Isl, AL USA.
RP Hardison, DR (reprint author), NOAA, Ctr Coastal Fisheries & Habitat Res, Beaufort, NC USA.
EM rance.hardison@noaa.gov
OI DARIUS, Helene Taiana/0000-0002-1184-7034
FU National Oceanic and Atmospheric Administration's Ecology and
Oceanography of Harmful Algae Blooms contribution [843]; National
Oceanic and Atmospheric Administration; National Ocean Service; Centers
for Coastal Ocean Science; Center for Coastal Fisheries and Habitat
Research; Cooperative Institute for Ocean Exploration, Research, and
Technology CIOERT [NA14OAR4320260]; NOAA; DOC
FX Funding was provided by the National Oceanic and Atmospheric
Administration's Ecology and Oceanography of Harmful Algae Blooms
contribution #843 - http://coastalscience.noaa.gov/research/habs/ecohab
RWL PAT DRH WCH DS. Program funds were provided by the National Oceanic
and Atmospheric Administration, National Ocean Service, Centers for
Coastal Ocean Science, Center for Coastal Fisheries and Habitat
Research-DRH WCH RWL PAT JAM. The UNCW partnership is in part funded
through the Cooperative Institute for Ocean Exploration, Research, and
Technology CIOERT, award number NA14OAR4320260, NOAA, DOC. Authors
associated with this are DGB, AJB, and JRM. NOAA National Marine
Fisheries, Office of International Affairs-United States Department of
State-JAM. The commercial partner SeaTox Research Inc. was not
responsible the design or execution of the project, nor did they provide
salary support to any of the collaborators. Their role was limited to
providing reagents and running the radioactive receptor binding assay
using extracts prepared by DRH and WCH. JHT provided support in the form
of salary for PT, but did not have any additional role in the study
design, data collection and analysis, decision to publish, or
preparation of the manuscript. The funders had no role in study design,
data collection and analysis, decision to publish, or preparation of the
manuscript.
NR 24
TC 1
Z9 1
U1 11
U2 21
PU PUBLIC LIBRARY SCIENCE
PI SAN FRANCISCO
PA 1160 BATTERY STREET, STE 100, SAN FRANCISCO, CA 94111 USA
SN 1932-6203
J9 PLOS ONE
JI PLoS One
PD APR 13
PY 2016
VL 11
IS 4
AR e0153348
DI 10.1371/journal.pone.0153348
PG 19
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DJ3UC
UT WOS:000374131200077
PM 27073998
ER
PT J
AU Butch, NP
Paglione, J
Chow, P
Xiao, YM
Marianetti, CA
Booth, CH
Jeffries, JR
AF Butch, Nicholas P.
Paglione, Johnpierre
Chow, Paul
Xiao, Yuming
Marianetti, Chris A.
Booth, Corwin H.
Jeffries, Jason R.
TI Pressure-Resistant Intermediate Valence in the Kondo Insulator SmB6
SO PHYSICAL REVIEW LETTERS
LA English
DT Article
ID EMISSION-SPECTROSCOPY; SAMARIUM; SUSCEPTIBILITY; TRANSITION; HEXABORIDE;
STATES
AB Resonant x-ray emission spectroscopy was used to determine the pressure dependence of the f-electron occupancy in the Kondo insulator SmB6. Applied pressure reduces the f occupancy, but surprisingly, the material maintains a significant divalent character up to a pressure of at least 35 GPa. Thus, the closure of the resistive activation energy gap and onset of magnetic order are not driven by stabilization of an integer valent state. Over the entire pressure range, the material maintains a remarkably stable intermediate valence that can in principle support a nontrivial band structure.
C1 [Butch, Nicholas P.; Paglione, Johnpierre] Univ Maryland, Dept Phys, Ctr Nanophys & Adv Mat, College Pk, MD 20742 USA.
[Butch, Nicholas P.] NIST, Ctr Neutron Res, 100 Bur Dr, Gaithersburg, MD 20899 USA.
[Butch, Nicholas P.; Jeffries, Jason R.] Lawrence Livermore Natl Lab, 7000 East Ave, Livermore, CA 94550 USA.
[Chow, Paul; Xiao, Yuming] Carnegie Inst Sci, Geophys Lab, HP CAT, Argonne, IL 60439 USA.
[Marianetti, Chris A.] Columbia Univ, Dept Appl Phys & Appl Math, New York, NY 10027 USA.
[Booth, Corwin H.] Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Div Chem Sci, Berkeley, CA 94720 USA.
RP Butch, NP (reprint author), Univ Maryland, Dept Phys, Ctr Nanophys & Adv Mat, College Pk, MD 20742 USA.; Butch, NP (reprint author), NIST, Ctr Neutron Res, 100 Bur Dr, Gaithersburg, MD 20899 USA.; Butch, NP (reprint author), Lawrence Livermore Natl Lab, 7000 East Ave, Livermore, CA 94550 USA.
EM nicholas.butch@nist.gov
FU CNAM; LLNL PLS directorate; Science Campaign; DOE-NNSA [DE-NA0001974];
DOE-BES [DE-FG02-99ER45775]; NSF; DOE Office of Science
[DE-AC02-06CH11357]; DOE, NNSA [DE-AC52-07NA27344]; AFOSR-MURI
[FA9550-09-1-0603]; NSF MRSEC program through Columbia in the Center for
Precision Assembly of Superstratic and Superatomic Solids [DMR-1420634];
Office of Science (OS), Office of Basic Energy Sciences (OBES), Chemical
Sciences, Geosciences, and Biosciences Division of the U.S. Department
of Energy (DOE) [DE-AC02-05CH11231]
FX N. P. B. acknowledges support by CNAM and the LLNL PLS directorate. J.
R. J. is partially supported by the Science Campaign. Portions of this
work were performed under LDRD (Tracking Code 14-ERD-041). This work was
performed at HPCAT (Sector 16), Advanced Photon Source (APS), Argonne
National Laboratory. HPCAT operations are supported by DOE-NNSA under
Award No. DE-NA0001974 and DOE-BES under Award No. DE-FG02-99ER45775,
with partial instrumentation funding by NSF. The Advanced Photon Source
is a U.S. Department of Energy (DOE) Office of Science User Facility
operated for the DOE Office of Science by Argonne National Laboratory
under Contract No. DE-AC02-06CH11357. LLNL is operated by Lawrence
Livermore National Security, LLC, for the DOE, NNSA under Contract No.
DE-AC52-07NA27344. Crystal growth at UMD was supported by AFOSR-MURI
(FA9550-09-1-0603). C. A. M. was supported by the NSF MRSEC program
through Columbia in the Center for Precision Assembly of Superstratic
and Superatomic Solids (DMR-1420634). Work at Lawrence Berkeley National
Laboratory was supported by the Director, Office of Science (OS), Office
of Basic Energy Sciences (OBES), Chemical Sciences, Geosciences, and
Biosciences Division of the U.S. Department of Energy (DOE) under
Contract No. DE-AC02-05CH11231.
NR 51
TC 1
Z9 1
U1 15
U2 33
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 0031-9007
EI 1079-7114
J9 PHYS REV LETT
JI Phys. Rev. Lett.
PD APR 13
PY 2016
VL 116
IS 15
AR 156401
DI 10.1103/PhysRevLett.116.156401
PG 5
WC Physics, Multidisciplinary
SC Physics
GA DJ0IA
UT WOS:000373884500005
PM 27127976
ER
PT J
AU Colegrove, KM
Venn-Watson, S
Litz, J
Kinsel, MJ
Terio, KA
Fougeres, E
Ewing, R
Pabst, DA
McLellan, WA
Raverty, S
Saliki, J
Fire, S
Rappucci, G
Bowen-Stevens, S
Noble, L
Costidis, A
Barbieri, M
Field, C
Smith, S
Carmichael, RH
Chevis, C
Hatchett, W
Shannon, D
Tumlin, M
Lovewell, G
Mcfee, W
Rowles, TK
AF Colegrove, Kathleen M.
Venn-Watson, Stephanie
Litz, Jenny
Kinsel, Michael J.
Terio, Karen A.
Fougeres, Erin
Ewing, Ruth
Pabst, D. Ann
McLellan, William A.
Raverty, Stephen
Saliki, Jeremiah
Fire, Spencer
Rappucci, Gina
Bowen-Stevens, Sabrina
Noble, Lauren
Costidis, Alex
Barbieri, Michelle
Field, Cara
Smith, Suzanne
Carmichael, Ruth H.
Chevis, Connie
Hatchett, Wendy
Shannon, Delphine
Tumlin, Mandy
Lovewell, Gretchen
Mcfee, Wayne
Rowles, Teresa K.
TI Fetal distress and in utero pneumonia in perinatal dolphins during the
Northern Gulf of Mexico unusual mortality event
SO DISEASES OF AQUATIC ORGANISMS
LA English
DT Article
DE Bottlenose dolphin; Brucella; Fetal distress; Fetal loss; Oil spill;
Pneumonia; Tursiops truncatus; Unusual mortality event
ID BOTTLE-NOSED-DOLPHIN; HORIZON OIL-SPILL; TURSIOPS-TRUNCATUS;
BRUCELLA-CETI; MISSISSIPPI SOUND; INFECTION; EXPOSURE; ASSOCIATION;
MENINGOENCEPHALITIS; OPTIMIZATION
AB An unusual mortality event (UME) involving primarily common bottlenose dolphins Tursiops truncatus of all size classes stranding along coastal Louisiana, Mississippi, and Alabama, USA, started in early 2010 and continued into 2014. During this northern Gulf of Mexico UME, a distinct cluster of perinatal dolphins (total body length < 115 cm) stranded in Mississippi and Alabama during 2011. The proportion of annual dolphin strandings that were perinates between 2009 and 2013 were compared to baseline strandings (2000-2005). A case-reference study was conducted to compare demographics, histologic lesions, and Brucella sp. infection prevalence in 69 UME perinatal dolphins to findings from 26 reference perinates stranded in South Carolina and Florida outside of the UME area. Compared to reference perinates, UME perinates were more likely to have died in utero or very soon after birth (presence of atelectasis in 88 vs. 15%, p < 0.0001), have fetal distress (87 vs. 27%, p < 0.0001), and have pneumonia not associated with lungworm infection (65 vs. 19%, p = 0.0001). The percentage of perinates with Brucella sp. infections identified via lung PCR was higher among UME perinates stranding in Mississippi and Alabama compared to reference perinates (61 vs. 24%, p = 0.01), and multiple different Brucella omp genetic sequences were identified in UME perinates. These results support that from 2011 to 2013, during the northern Gulf of Mexico UME, bottlenose dolphins were particularly susceptible to late-term pregnancy failures and development of in utero infections including brucellosis.
C1 [Colegrove, Kathleen M.] Univ Illinois, Coll Vet Med, Zool Pathol Program, Maywood, IL 60153 USA.
[Venn-Watson, Stephanie; Kinsel, Michael J.; Terio, Karen A.] Natl Marine Mammal Fdn, San Diego, CA 92016 USA.
[Litz, Jenny; Ewing, Ruth] Natl Marine Fisheries Serv, Southeast Fisheries Sci Ctr, Miami, FL 33149 USA.
[Fougeres, Erin] Natl Marine Fisheries Serv, Southeast Reg Off, St Petersburg, FL USA.
[Pabst, D. Ann; McLellan, William A.; Costidis, Alex] Univ N Carolina, Dept Biol & Marine Biol, Wilmington, NC 28403 USA.
[Raverty, Stephen] Anim Hlth Ctr, 1787 Angus Campbell Rd, Abbotsford, BC V3G 2M3, Canada.
[Saliki, Jeremiah] Univ Georgia, Athens Vet Diagnost Lab, Coll Vet Med, Athens, GA 30602 USA.
[Fire, Spencer; Mcfee, Wayne] NOAA, Natl Ocean Serv, Charleston, SC 29412 USA.
[Rappucci, Gina; Bowen-Stevens, Sabrina] NOAA, Southeast Fisheries Sci Ctr, Miami, FL 33149 USA.
[Noble, Lauren] NOAA, Southeast Fisheries Sci Ctr, Pascagoula, MS 39567 USA.
[Barbieri, Michelle; Rowles, Teresa K.] Natl Marine Fisheries Serv, Silver Spring, MD 20910 USA.
[Field, Cara; Smith, Suzanne] Audubon Aquarium Amer, New Orleans, LA 70130 USA.
[Carmichael, Ruth H.] Dauphin Isl Sea Lab, Dauphin Isl, AL USA.
[Carmichael, Ruth H.] Univ S Alabama, Dauphin Isl, AL USA.
[Chevis, Connie; Hatchett, Wendy; Shannon, Delphine] Inst Marine Mammal Studies, Gulfport, MS 39503 USA.
[Tumlin, Mandy] Louisiana Dept Wildlife & Fisheries, Baton Rouge, LA 70898 USA.
[Lovewell, Gretchen] Mote Marine Lab, Sarasota, FL 34236 USA.
[Fire, Spencer] Florida Inst Technol, Dept Biol Sci, Melbourne, FL 32901 USA.
[Barbieri, Michelle; Field, Cara] Marine Mammal Ctr, Sausalito, CA 94965 USA.
RP Colegrove, KM (reprint author), Univ Illinois, Coll Vet Med, Zool Pathol Program, Maywood, IL 60153 USA.
EM katie.colegrove@gmail.com
FU NMFS UME contingency fund; NOAA Marine Mammal Health and Stranding
Response Program; Deepwater Horizon oil spill Natural Resource Damage
Assessment
FX This work could not have been conducted without the efforts of the
Marine Mammal Stranding Network, including additional personnel from
those agencies working on the northern GoM UME: Louisiana Department of
Wildlife and Fisheries (especially staff from the Fisheries Research Lab
in Grand Isle), Audubon Aquarium of the Americas, Institute for Marine
Mammal Studies, Dauphin Island Sea Lab, Emerald Coast Wildlife Refuge,
and Gulf World Marine Park, particularly M. Brodsky, J. Hartley, M.
Kelley, C. N. Seely, N. Wingers, M. Stolen, D. Boyd, B. MacLean, and S.
Maillian. The authors acknowledge the northern GoM UME Investigative
Team and the past and present members of the Working Group for Marine
Mammal Unusual Mortality Events. We thank E. Stratton and L. Aichinger
Dias for their integral roles in the perinate necropsy session. We thank
B. Mase-Guthrie and E. Stratton for coordination of the SER Marine
Mammal Stranding Network. We thank N. Ahmed and J. Landolfi for their
integral work in completing the PCR assays and B. Thomsen for completion
of immunohistochemistry. M. Broadwater is acknowledged for her
assistance in biotoxin analysis. The biotoxin analysis was conducted
through the National Centers for Coastal Ocean Science (NCCOS) Harmful
Algal Bloom Analytical Response Team. C. Quance and S. Robbe-Austerman
from National Veterinary Services Laboratories, Animal and Plant Health
Inspection Service are acknowledged for their work on Brucella culture.
We thank the following individuals who helped review or otherwise
contribute to portions of this manuscript: L. Engleby, S. Horton, L.
Schwacke, C. Smith, Z. Wang, and F. Van Dolah. Funding for this
investigation was provided in part by the NMFS UME contingency fund,
NOAA Marine Mammal Health and Stranding Response Program and as part of
the Deepwater Horizon oil spill Natural Resource Damage Assessment being
conducted cooperatively between NOAA, other federal and state trustees
and BP.
NR 54
TC 5
Z9 5
U1 12
U2 15
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 0177-5103
EI 1616-1580
J9 DIS AQUAT ORGAN
JI Dis. Aquat. Org.
PD APR 12
PY 2016
VL 119
IS 1
BP 1
EP 16
DI 10.3354/dao02969
PG 16
WC Fisheries; Veterinary Sciences
SC Fisheries; Veterinary Sciences
GA DK0AX
UT WOS:000374575900001
PM 27068499
ER
PT J
AU Raymundo, LJ
Work, TM
Miller, RL
Lozada-Misa, PL
AF Raymundo, L. J.
Work, T. M.
Miller, R. L.
Lozada-Misa, P. L.
TI Effects of Coralliophila violacea on tissue loss in the scleractinian
corals Porites spp. depend on host response
SO DISEASES OF AQUATIC ORGANISMS
LA English
DT Article
DE Coralliophila; Coral disease; White syndrome; Porites; Guam
ID GREAT-BARRIER-REEF; WHITE SYNDROME; BAND DISEASE; LESIONS; GROSS;
TRANSMISSION; CORALLIVORE; COMMUNITIES; ABBREVIATA; DRUPELLA
AB We investigated interactions between the corallivorous gastropod Coralliophila violacea and its preferred hosts Porites spp. Our objectives were to experimentally determine whether tissue loss could progress in Porites during or after Coralliophila predation on corals with and without tissue loss and to histologically document snail predation. In 64% of feeding scars, tissue regenerated within 3 wk, leaving no trace of predation. However, in roughly 28% of scars, lesions progressed to subacute tissue loss resembling white syndrome. In feeding experiments, scars from snails previously fed diseased tissue developed progressive tissue loss twice as frequently as scars from snails previously fed healthy tissue. Scars from previously healthy-fed snails were 3 times as likely to heal as those from previously diseased-fed snails. Histology revealed marked differences in host responses to snails; P. cylindrica manifested a robust inflammatory response with fewer secondary colonizing organisms such as algae, sponges, and helminths, whereas P. rus showed no evident inflammation and more secondary colonization. We conclude that lesion progression associated with Coralliophila may be associated with secondary colonization of coral tissues damaged by predator-induced trauma and necrosis. Importantly, variation at the cellular level should be considered when explaining interspecific differences in host responses in corals impacted by phenomena such as predation.
C1 [Raymundo, L. J.] Univ Guam, Marine Lab, Mangilao, GU 96923 USA.
[Work, T. M.] USGS Natl Wildlife Hlth Ctr, Honolulu Field Stn, Honolulu, HI 96850 USA.
[Miller, R. L.] Bur Stat & Plans, Guam Coral Reef Monitoring Program, Mangilao, GU 96923 USA.
[Lozada-Misa, P. L.] NOAA, Honolulu, HI 96818 USA.
RP Raymundo, LJ (reprint author), Univ Guam, Marine Lab, Mangilao, GU 96923 USA.
EM ljraymundo@gmail.com
FU NOAA Coral Reef Conservation Program
FX This work was supported by a grant from the NOAA Coral Reef Conservation
Program to L.J.R. and G. Aeby. A. Miller, T. Reynolds, and R. Diaz
assisted in laboratory experiments. Discussions with G. Aeby guided the
experimental set up. Mention of products or trade names does not imply
endorsement by the US Government. We thank the anonymous reviewers for
their comments, which greatly improved the paper.
NR 36
TC 1
Z9 1
U1 10
U2 10
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 0177-5103
EI 1616-1580
J9 DIS AQUAT ORGAN
JI Dis. Aquat. Org.
PD APR 12
PY 2016
VL 119
IS 1
BP 75
EP 83
DI 10.3354/dao02982
PG 9
WC Fisheries; Veterinary Sciences
SC Fisheries; Veterinary Sciences
GA DK0AX
UT WOS:000374575900007
PM 27068505
ER
PT J
AU Stutzman, PE
Feng, P
Bullard, JW
AF Stutzman, Paul E.
Feng, Pan
Bullard, Jeffrey W.
TI Phase Analysis of Portland Cement by Combined Quantitative X-Ray Powder
Diffraction and Scanning Electron Microscopy
SO JOURNAL OF RESEARCH OF THE NATIONAL INSTITUTE OF STANDARDS AND
TECHNOLOGY
LA English
DT Article
DE materials characterization; microstructure; portland cement; scanning
electron microscopy; X-ray diffraction
AB X-ray powder diffraction (XRD) has been used for several decades to identify and measure the mass fractions of various crystalline phases in portland cement. More recently, a combination of scanning electron microscopy with X-ray microanalysis (SEM/XMA) and image processing has been shown to enable the quantitative characterization of microstructural features in these materials. Each-technique can furnish some information that is not accessible from the other. For example, SEM/XMA can identify the microstructural location and morphology of calcium sulfate minerals, while only XRD can determine the relative abundance of the different forms of calcium sulfate, such as gypsum (CaSO4 center dot 2H(2)O), bassanite (CaSO4 center dot 1/2 H2O), and anhydrite (CaSO4). This document describes how XRD and SEM/XMA can be used together to establish and validate the portland cement phase composition and microstructure. Particular emphasis is laid on step-by-step procedures and best practices for XRD specimen preparation, data collection, and intepretation. Similar detail has been given recently for SEM/XMA [Stutzman et al., NIST Tech Note 1877, U.S. Department of Commerce, April 2015]. The methods are demonstrated for three portland cement powders, through which apparent discrepancies between the results of the two methods are identified and procedures are described for resolving the discrepancies and quantifying uncertainty.
C1 [Stutzman, Paul E.; Feng, Pan; Bullard, Jeffrey W.] NIST, Gaithersburg, MD 20899 USA.
[Feng, Pan] Southeast Univ, Nanjing 210096, Jiangsu, Peoples R China.
RP Stutzman, PE (reprint author), NIST, Gaithersburg, MD 20899 USA.
EM paul.stutzman@nist.gov; pan.feng@nist.gov; jeffrey.bullard@nist.gov
NR 35
TC 0
Z9 0
U1 5
U2 6
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 APR 11
PY 2016
VL 121
DI 10.6028/jres.121.004
PG 61
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA DQ5AZ
UT WOS:000379218100001
ER
PT J
AU Yao, ZZ
Zhang, ZJ
Liu, LZ
Li, ZY
Zhou, W
Zhao, YF
Han, Y
Chen, BL
Krishna, R
Xiang, SC
AF Yao, Zizhu
Zhang, Zhangjing
Liu, Lizhen
Li, Ziyin
Zhou, Wei
Zhao, Yunfeng
Han, Yu
Chen, Banglin
Krishna, Rajamani
Xiang, Shengchang
TI Extraordinary Separation of Acetylene-Containing Mixtures with
Microporous Metal-Organic Frameworks with Open O Donor Sites and Tunable
Robustness through Control of the Helical Chain Secondary Building Units
SO CHEMISTRY-A EUROPEAN JOURNAL
LA English
DT Article
DE column breakthrough; metal-organic frameworks; open O donors; selective
gas adsorption; structural diversity
ID SELECTIVE C2H2/C2H4 SEPARATION; ROOM-TEMPERATURE; CO2/CH4 SEPARATION;
AMBIENT CONDITIONS; BINDING-ENERGY; GAS SEPARATION; NATURAL-GAS; CO2
CAPTURE; STORAGE; HYDROGENATION
AB Acetylene separation is a very important but challenging industrial separation task. Here, through the solvothermal reaction of CuI and 5-triazole isophthalic acid in different solvents, two metal-organic frameworks (MOFs, FJU-21 and FJU-22) with open O donor sites and controllable robustness have been obtained for acetylene separation. They contain the same paddle-wheel {Cu-2(COO2)(4)} nodes and metal-ligand connection modes, but with different helical chains as secondary building units (SBUs), leading to different structural robustness for the MOFs. FJU-21 and FJU-22 are the first examples in which the MOFs' robustness is controlled by adjusting the helical chain SBUs. Good robustness gives the activated FJU-22a, which has higher surface area and gas uptakes than the flexible FJU-21a. Importantly, FJU-22a shows extraordinary separation of acetylene mixtures under ambient conditions. The separation capacity of FJU-22a for 50:50 C2H2/CO2 mixtures is about twice that of the high-capacity HOF-3, and its actual separation selectivity for C2H2/C2H4 mixtures containing 1% acetylene is the highest among reported porous materials. Based on first-principles calculations, the extraordinary separation performance of C2H2 for FJU-22a was attributed to hydrogen-bonding interactions between the C2H2 molecules with the open O donors on the wall, which provide better recognition ability for C2H2 than other functional sites, including open metal sites and amino groups.
C1 [Yao, Zizhu; Zhang, Zhangjing; Liu, Lizhen; Li, Ziyin; Xiang, Shengchang] Fujian Normal Univ, Fujian Prov Key Lab Polymer Mat, 32 Shangsan Rd, Fuzhou 350007, Peoples R China.
[Zhou, Wei] NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Zhao, Yunfeng; Han, Yu] King Abdullah Univ Sci & Technol, Adv Membranes & Porous Mat Ctr, Phys Sci & Engn Div, Thuwal 239556900, Saudi Arabia.
[Chen, Banglin] Univ Texas San Antonio, Dept Chem, One UTSA Circle, San Antonio, TX 78249 USA.
[Krishna, Rajamani] Univ Amsterdam, Vant Hoff Inst Mol Sci, Sci Pk 904, NL-1098 XH Amsterdam, Netherlands.
[Zhao, Yunfeng] Tianjin Univ Technol, Sch Mat Sci & Engn, Inst New Energy Mat & Low Carbon Technol, Tianjin 300384, Peoples R China.
RP Xiang, SC (reprint author), Fujian Normal Univ, Fujian Prov Key Lab Polymer Mat, 32 Shangsan Rd, Fuzhou 350007, Peoples R China.; Krishna, R (reprint author), Univ Amsterdam, Vant Hoff Inst Mol Sci, Sci Pk 904, NL-1098 XH Amsterdam, Netherlands.
EM scxiang@fjnu.edu.cn
RI Chen, Banglin/F-5461-2010; Xiang, Shengchang/F-9210-2010; Zhao,
Yunfeng/H-1380-2011; Zhou, Wei/C-6504-2008; Krishna,
Rajamani/A-1098-2012
OI Chen, Banglin/0000-0001-8707-8115; Xiang,
Shengchang/0000-0001-6016-2587; Zhao, Yunfeng/0000-0002-1442-992X; Zhou,
Wei/0000-0002-5461-3617; Krishna, Rajamani/0000-0002-4784-8530
FU National Natural Science Foundation of China [21207018, 21273033,
21203024, 21573042]; Fujian Science and Technology Department
[2014J06003, 2014H6007]; Recruitment Program of Global Young Experts,
Program for New Century Excellent Talents in University [NCET-10-0108];
Award 'MinJiang Scholar Program' in Fujian Province
FX This work was financially supported by the National Natural Science
Foundation of China (21207018, 21273033, 21203024, and 21573042) and the
Fujian Science and Technology Department (2014J06003 and 2014H6007).
S.X. gratefully acknowledges the support of the Recruitment Program of
Global Young Experts, Program for New Century Excellent Talents in
University (NCET-10-0108), and the Award 'MinJiang Scholar Program' in
Fujian Province.
NR 80
TC 6
Z9 6
U1 21
U2 57
PU WILEY-V C H VERLAG GMBH
PI WEINHEIM
PA POSTFACH 101161, 69451 WEINHEIM, GERMANY
SN 0947-6539
EI 1521-3765
J9 CHEM-EUR J
JI Chem.-Eur. J.
PD APR 11
PY 2016
VL 22
IS 16
BP 5676
EP 5683
DI 10.1002/chem.201505107
PG 8
WC Chemistry, Multidisciplinary
SC Chemistry
GA DJ2EW
UT WOS:000374017500032
PM 26934040
ER
PT J
AU Schaan, E
Ferraro, S
Vargas-Magana, M
Smith, KM
Ho, S
Aiola, S
Battaglia, N
Bond, JR
De Bernardis, F
Calabrese, E
Cho, HM
Devlin, MJ
Dunkley, J
Gallardo, PA
Hasselfield, M
Henderson, S
Hill, JC
Hincks, AD
Hlozek, R
Hubmayr, J
Hughes, JP
Irwin, KD
Koopman, B
Kosowsky, A
Li, D
Louis, T
Lungu, M
Madhavacheri, M
Maurin, L
McMahon, JJ
Moodley, K
Naess, S
Nati, F
Newburgh, L
Niemack, MD
Page, LA
Pappas, CG
Partridge, B
Schmitt, BL
Sehga, N
Sherwin, BD
Sievers, JL
Spergel, DN
Staggs, ST
van Engelen, A
Wollack, EJ
AF Schaan, Emmanuel
Ferraro, Simone
Vargas-Magana, Mariana
Smith, Kendrick M.
Ho, Shirley
Aiola, Simone
Battaglia, Nicholas
Bond, J. Richard
De Bernardis, Francesco
Calabrese, Erminia
Cho, Hsiao-Mei
Devlin, Mark J.
Dunkley, Joanna
Gallardo, Patricio A.
Hasselfield, Matthew
Henderson, Shawn
Hill, J. Colin
Hincks, Adam D.
Hlozek, Renee
Hubmayr, Johannes
Hughes, John P.
Irwin, Kent D.
Koopman, Brian
Kosowsky, Arthur
Li, Dale
Louis, Thibaut
Lungu, Marius
Madhavacheri, Mathew
Maurin, Loic
McMahon, Jeffrey John
Moodley, Kavilan
Naess, Sigurd
Nati, Federico
Newburgh, Laura
Niemack, Michael D.
Page, Lyman A.
Pappas, Christine G.
Partridge, Bruce
Schmitt, Benjamin L.
Sehga, Neelima
Sherwin, Blake D.
Sievers, Jonathan L.
Spergel, David N.
Staggs, Suzanne T.
van Engelen, Alexander
Wollack, Edward J.
CA ACTPol Collaboration
TI Evidence for the kinematic Sunyaev-Zel'dovich effect with the Atacama
Cosmology Telescope and velocity reconstruction from the Baryon
Oscillation Spectroscopic Survey
SO PHYSICAL REVIEW D
LA English
DT Article
ID LOCALLY BRIGHTEST GALAXIES; WEAK LENSING SIGNAL; DIGITAL SKY SURVEY;
ACOUSTIC-OSCILLATIONS; POWER SPECTRUM; DATA RELEASE; BULK FLOW;
CONSTRAINTS; CLUSTERS; FEEDBACK
AB We use microwave temperature maps from two seasons of data from the Atacama Cosmology Telescope at 146 GHz, together with the "Constant Mass" CMASS galaxy sample from the Baryon Oscillation Spectroscopic Survey to measure the kinematic Sunyaev-Zel'dovich (kSZ) effect over the redshift range z = 0.4-0.7. We use galaxy positions and the continuity equation to obtain a reconstruction of the line-of-sight velocity field. We stack the microwave temperature at the location of each halo, weighted by the corresponding reconstructed velocity. We vary the size of the aperture photometry filter used, thus probing the free electron profile of these halos from within the virial radius out to three virial radii, on the scales relevant for investigating the missing baryons problem. The resulting best fit kSZ model is preferred over the no-kSZ hypothesis at 3.3 and 2.9 sigma for two independent velocity reconstruction methods, using 25,537 galaxies over 660 square degrees. The data suggest that the baryon profile is shallower than the dark matter in the inner regions of the halos probed here, potentially due to energy injection from active galactic nucleus or supernovae. Thus, by constraining the gas profile on a wide range of scales, this technique will be useful for understanding the role of feedback in galaxy groups and clusters. The effect of foregrounds that are uncorrelated with the galaxy velocities is expected to be well below our signal, and residual thermal Sunyaev-Zel'dovich contamination is controlled by masking the most massive clusters. Finally, we discuss the systematics involved in converting our measurement of the kSZ amplitude into the mean free electron fraction of the halos in our sample.
C1 [Schaan, Emmanuel; Ferraro, Simone; Battaglia, Nicholas; Calabrese, Erminia; Hasselfield, Matthew; Hlozek, Renee; Spergel, David N.] Princeton Univ, Dept Astrophys Sci, Peyton Hall, Princeton, NJ 08544 USA.
[Ferraro, Simone; Sherwin, Blake D.] Univ Calif Berkeley, Miller Inst Basic Res Sci, Berkeley, CA 94720 USA.
[Vargas-Magana, Mariana] Univ Nacl Autonoma Mexico, Inst Fis, Apartado Postal 20-364, Mexico City 04510, DF, Mexico.
[Smith, Kendrick M.] Perimeter Inst Theoret Phys, Waterloo, ON N2L 2Y5, Canada.
[Ho, Shirley] Carnegie Mellon Univ, Dept Phys, 5000 Forbes Ave, Pittsburgh, PA 15213 USA.
[Aiola, Simone; Kosowsky, Arthur] Univ Pittsburgh, Dept Phys & Astron, Pittsburgh, PA 15260 USA.
[Aiola, Simone; Kosowsky, Arthur] Univ Pittsburgh, Pittsburgh Particle Phys Astrophys & Cosmol Ctr, Pittsburgh, PA 15260 USA.
[Bond, J. Richard; van Engelen, Alexander] Univ Toronto, Canadian Inst Theoret Astrophys, Toronto, ON M5S 3H8, Canada.
[De Bernardis, Francesco; Gallardo, Patricio A.; Henderson, Shawn; Koopman, Brian; Maurin, Loic; Niemack, Michael D.] Cornell Univ, Dept Phys, Ithaca, NY 14853 USA.
[Calabrese, Erminia; Dunkley, Joanna; Louis, Thibaut; Naess, Sigurd] Univ Oxford, Subdept Astrophys, Keble Rd, Oxford OX1 3RH, England.
[Cho, Hsiao-Mei; Irwin, Kent D.; Li, Dale] SLAC Natl Accelerator Lab, 2575 Sandhill Hill Rd, Menlo Pk, CA 94025 USA.
[Devlin, Mark J.; Lungu, Marius; Nati, Federico; Schmitt, Benjamin L.] Univ Penn, Dept Phys & Astron, 209 South 33rd St, Philadelphia, PA 19104 USA.
[Hill, J. Colin] Columbia Univ, Dept Astron, Pupin Hall, New York, NY 10027 USA.
[Hincks, Adam D.] Univ British Columbia, Dept Phys & Astron, 6224 Agr Rd, Vancouver, BC V6T 1Z1, Canada.
[Hubmayr, Johannes] NIST, Boulder, CO 80305 USA.
[Hughes, John P.] Rutgers State Univ, Dept Phys & Astron, 136 Frelinghuysen Rd, Piscataway, NJ 08854 USA.
[Irwin, Kent D.] Stanford Univ, Dept Phys, Stanford, CA 94305 USA.
[Madhavacheri, Mathew; Sehga, Neelima] SUNY Stony Brook, Dept Phys & Astron, Stony Brook, NY 11794 USA.
[Maurin, Loic] Pontificia Univ Catolica Chile, Inst Astrofis, Santiago 7820436, Chile.
[McMahon, Jeffrey John] Univ Michigan, Dept Phys, Ann Arbor, MI 48103 USA.
[Moodley, Kavilan] Univ KwaZulu Natal, Sch Math Stat & Comp Sci, Astrophys & Cosmol Res Unit, ZA-4041 Durban, South Africa.
[Newburgh, Laura] Univ Toronto, Dunlap Inst, 50 St George St, Toronto, ON M5S 3H4, Canada.
[Page, Lyman A.; Pappas, Christine G.; Staggs, Suzanne T.] Princeton Univ, Joseph Henry Labs Phys, Jadwin Hall, Princeton, NJ 08544 USA.
[Partridge, Bruce] Haverford Coll, Dept Phys & Astron, Haverford, PA 19041 USA.
[Sherwin, Blake D.] Univ Calif Berkeley, LBL, Berkeley Ctr Cosmol Phys, Berkeley, CA 94720 USA.
[Sherwin, Blake D.] Univ Calif Berkeley, LBL, Dept Phys, Berkeley, CA 94720 USA.
[Sievers, Jonathan L.] Univ KwaZulu Natal, Sch Chem & Phys, Astrophys & Cosmol Res Unit, ZA-4041 Durban, South Africa.
[Sievers, Jonathan L.] Univ KwaZulu Natal, NITheP, Private Bag X54001, ZA-4000 Durban, South Africa.
[Wollack, Edward J.] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
RP Schaan, E (reprint author), Princeton Univ, Dept Astrophys Sci, Peyton Hall, Princeton, NJ 08544 USA.
EM eschaan@astro.princeton.edu
RI Wollack, Edward/D-4467-2012; Nati, Federico/I-4469-2016;
OI Wollack, Edward/0000-0002-7567-4451; Nati, Federico/0000-0002-8307-5088;
Aiola, Simone/0000-0002-1035-1854
FU U.S. National Science Foundation (NSF) [AST-0408698, AST-0965625,
PHY-0855887, PHY-1214379]; Princeton University; University of
Pennsylvania; Cornell University; Canada Foundation for Innovation
(CFI); Comision Nacional de Investigacion Cientifica y Tecnologica de
Chile (CONICYT); CFI under the auspices of Compute Canada; Government of
Ontario; Ontario Research Fund Research Excellence; University of
Toronto; Mishrahi Fund; Wilkinson Fund; NSF [AST1311756, AST1517593,
AST1412966, AST-1454881, AST-1517049]; NASA [NNXI2AG72G,
12-EUCLID11-0004, NNX13AE56G, NNX14AB58G, NNX12AM32H, ATP NNX14AB57G];
Government of Canada through Industry Canada; Province of Ontario
through the Ministry of Research and Innovation; NSERC Discovery grant;
DOE-ASC [DOE-DESC001114]; Lyman Spitzer fellowship; ERC [259505]; DOE
[DE-SC0011114]; NASA Space Technology research fellowships; CONICYT
[QUIMAL-120001, FONDECYT-1141113]; Office of Science of the U.S.
Department of Energy [DE-AC02-05CH11231]; Alfred P. Sloan Foundation;
National Science Foundation; U.S. Department of Energy Office of
Science; University of Arizona; Brazilian Participation Group;
Brookhaven National Laboratory; Carnegie Mellon University; University
of Florida; French Participation Group; German Participation Group;
Harvard University; Institute de Astrofisica de Canarias; Michigan
State/Notre Dame/JINA Participation Group; Johns Hopkins University;
Lawrence Berkeley National Laboratory; Max Planck Institute for
Astrophysics; Max Planck Institute for Extraterrestrial Physics; New
Mexico State University; New York University; Ohio State University;
Pennsylvania State University; University of Portsmouth; Spanish
Participation Group; University of Tokyo; University of Utah; Vanderbilt
University; University of Virginia; University of Washington; Yale
University; [AST-1312991]
FX We thank Marcelo Alvarez, Neal Dalal, Tommaso Giannantonio, Oliver Hahn,
Andrey Kravtsov, Guilhem Lavaux, Hironao Miyatake, Hyunbae Park, Hiranya
Peiris, Ue-Li Pen, Bjoern Soergel, Naonori Sugiyama and Simon White for
very useful discussions. This work was supported by the U.S. National
Science Foundation (NSF) through Grants No. AST-0408698 and No.
AST-0965625 for the ACT project, as well as Grants No. PHY-0855887 and
No. PHY-1214379. Funding was also provided by Princeton University, the
University of Pennsylvania, Cornell University and a Canada Foundation
for Innovation (CFI) award to the University of British Columbia.
ACToperates in the Parque Astronomico Atacama in northern Chile under
the auspices of the Comision Nacional de Investigacion Cientifica y
Tecnologica de Chile (CONICYT). Computations were performed on the GPC
supercomputer at the SciNet HPC Consortium. SciNet is funded by the CFI
under the auspices of Compute Canada, the Government of Ontario, the
Ontario Research Fund Research Excellence; and the University of
Toronto. Colleagues at RadioSky provide logistical support and keep
operations in Chile running smoothly. We also thank the Mishrahi Fund
and the Wilkinson Fund for their generous support of the project. E. S.,
S. F. and D. N. S. are supported by NSF Grant No. AST1311756 and NASA
Grant No. NNXI2AG72G. Research at Perimeter Institute is supported by
the Government of Canada through Industry Canada and by the Province of
Ontario through the Ministry of Research and Innovation. K. M. S. was
supported by an NSERC Discovery grant. S. H. is supported in part by
DOE-ASC Award No. DOE-DESC001114, NASA Grant No. 12-EUCLID11-0004, and
NSF Grants No. AST1517593 and No. AST1412966. N. B. acknowledges support
from the Lyman Spitzer fellowship. M. N. and F. D. B. acknowledge
support from NSF Grants No. AST-1454881 and No. AST-1517049. The
development of multichroic detectors and lenses was supported by NASA
Grants No. NNX13AE56G and No. NNX14AB58G. C. M. acknowledges support
from NASA Grant No. NNX12AM32H. Funding from ERC Grant No. 259505
supports S. N., J. D., E. C., and T. L. H. T. is supported by NASA Grant
No. ATP NNX14AB57G, DOE Award No. DE-SC0011114, and NSF Grant No.
AST-1312991. B. S. and B. K. are funded by NASA Space Technology
research fellowships. R. D. received funding from the CONICYT Grants No.
QUIMAL-120001 and No. FONDECYT-1141113. This research used resources of
the National Energy Research Scientific Computing Center, a DOE Office
of Science User Facility supported by the Office of Science of the U.S.
Department of Energy under Award No. DE-AC02-05CH11231. Funding for
SDSS-III has been provided by the Alfred P. Sloan Foundation, the
Participating Institutions, the National Science Foundation, and the
U.S. Department of Energy Office of Science. The SDSS-III web site is
http://www.sdss3.org/.; SDSS-III is managed by the Astrophysical
Research Consortium for the Participating Institutions of the SDSS-III
Collaboration including the University of Arizona, the Brazilian
Participation Group, Brookhaven National Laboratory, Carnegie Mellon
University, University of Florida, the French Participation Group, the
German Participation Group, Harvard University, the Institute de
Astrofisica de Canarias, the Michigan State/Notre Dame/JINA
Participation Group, Johns Hopkins University, Lawrence Berkeley
National Laboratory, Max Planck Institute for Astrophysics; Max Planck
Institute for Extraterrestrial Physics, New Mexico State University, New
York University, Ohio State University, Pennsylvania State University,
University of Portsmouth; Princeton University, the Spanish
Participation Group, University of Tokyo, University of Utah, Vanderbilt
University, University of Virginia; University of Washington, and Yale
University.
NR 51
TC 6
Z9 6
U1 4
U2 9
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 2470-0010
EI 2470-0029
J9 PHYS REV D
JI Phys. Rev. D
PD APR 11
PY 2016
VL 93
IS 8
AR 082002
DI 10.1103/PhysRevD.93.082002
PG 8
WC Astronomy & Astrophysics; Physics, Particles & Fields
SC Astronomy & Astrophysics; Physics
GA DI8SF
UT WOS:000373770800001
ER
PT J
AU Cheung, WWL
Jones, MC
Reygondeau, G
Stock, CA
Lam, VWY
Frolicher, TL
AF Cheung, William W. L.
Jones, Miranda C.
Reygondeau, Gabriel
Stock, Charles A.
Lam, Vicky W. Y.
Froelicher, Thomas L.
TI Structural uncertainty in projecting global fisheries catches under
climate change
SO ECOLOGICAL MODELLING
LA English
DT Article
DE Dynamic Bioclimate Envelope Model; Climate change; Uncertainty; Habitat
suitability; MAXENT; AquaMaps
ID TROPHIC AMPLIFICATION; DISTRIBUTION MODELS; LARVAL DISPERSAL; MARINE;
DISTRIBUTIONS; OCEAN; FISH; IMPACTS; GROWTH; SCALE
AB The global ocean is projected to be warmer, less oxygenated and more acidic in the 21st century relative to the present day, resulting in changes in the biogeography and productivity of marine organisms and ecosystems. Previous studies using a Dynamic Bioclimate Envelope Model (DBEM) projected increases in potential catch in high latitude regions and decreases in tropical regions over the next few decades. A major structural uncertainty of the projected redistribution of species and fisheries catches can be attributed to the habitat suitability algorithms used. Here, we compare the DBEM projections of potential catches of 500 species of exploited marine fishes and invertebrates from 1971 to 2060 using three versions of DBEM that differ by the algorithm used to predict relative habitat suitability: DBEM-Basic, DBEM-Maxent and DBEM-Aquamaps. All the DBEM models have similar skill in predicting the occurrence of exploited species and distribution of observed fisheries production. Globally, the models project a decrease in catch potential of 3% to 13% by 2050 under a high emissions scenario (Representative Concentration Pathway 8.5). For the majority, of the modelled species, projections by DBEM-Maxent are less sensitive to changes in ocean properties than those by DBEM-Aquamaps. The mean magnitude of projected changes relative to differences between projections differ between regions, being highest (>1 times the standard deviation) in the tropical regions and Arctic Ocean and lowest in three of the main Eastern Boundary Upwelling regions, the eastern Indian Ocean and the Southern Ocean. These results suggest that the qualitative patterns of changes in catch potential reported in previous studies are not affected by the structural uncertainty of DBEM, particularly in areas where catch potential was projected to be most sensitive to climate change. However, when making projections of fish stocks and their potential catches using DBEM in the future, multiple versions of DBEM should be used to quantify the uncertainty associated with structural uncertainty of the models. Overall, this study contributes to improving projection of future changes in living marine resources by exploring one aspect of the cascade of uncertainty associated with such projections. (C) 2016 Published by Elsevier B.V.
C1 [Cheung, William W. L.; Jones, Miranda C.; Reygondeau, Gabriel; Lam, Vicky W. Y.] Univ British Columbia, Inst Oceans & Fisheries, Nippon Fdn Nereus Program, Vancouver, BC V6T 1Z4, Canada.
[Jones, Miranda C.] Univ Cambridge, Dept Zool, Downing St, Cambridge CB2 3EJ, England.
[Stock, Charles A.] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA.
[Lam, Vicky W. Y.] Univ British Columbia, Inst Oceans & Fisheries, Sea Us, Vancouver, BC V6T 1Z4, Canada.
[Froelicher, Thomas L.] ETH, Inst Biogeochem & Pollutant Dynam, Environm Phys, Zurich, Switzerland.
RP Cheung, WWL (reprint author), Univ British Columbia, Inst Oceans & Fisheries, Nippon Fdn Nereus Program, Vancouver, BC V6T 1Z4, Canada.
EM w.cheung@oceans.ubc.ca
RI Frolicher, Thomas/E-5137-2015;
OI Frolicher, Thomas/0000-0003-2348-7854; Stock,
Charles/0000-0001-9549-8013
FU Natural Sciences and Engineering Research Council of Canada [22R68146];
SNSF (Ambizione grant) [PZ00P2_142573]
FX This study is a contribution from the Nippon Foundation-The University
of British Columbia Nereus Program. WWLC also acknowledges funding
support from Natural Sciences and Engineering Research Council of Canada
(22R68146). T. L. Frolicher acknowledges financial support from the SNSF
(Ambizione grant PZ00P2_142573).
NR 56
TC 8
Z9 8
U1 18
U2 62
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0304-3800
EI 1872-7026
J9 ECOL MODEL
JI Ecol. Model.
PD APR 10
PY 2016
VL 325
BP 57
EP 66
DI 10.1016/j.ecolmodel.2015.12.018
PG 10
WC Ecology
SC Environmental Sciences & Ecology
GA DG3BL
UT WOS:000371944400006
ER
PT J
AU Ong, TH
Romanova, EV
Roberts-Galbraith, RH
Yang, N
Zimmerman, TA
Collins, JJ
Lee, JE
Kelleher, NL
Newmark, PA
Sweedler, JV
AF Ong, Ta-Hsuan
Romanova, Elena V.
Roberts-Galbraith, Rachel H.
Yang, Ning
Zimmerman, Tyler A.
Collins, James J., III
Lee, Ji Eun
Kelleher, Neil L.
Newmark, Phillip A.
Sweedler, Jonathan V.
TI Mass Spectrometry Imaging and Identification of Peptides Associated with
Cephalic Ganglia Regeneration in Schmidtea mediterranea
SO JOURNAL OF BIOLOGICAL CHEMISTRY
LA English
DT Article
DE imaging; mass spectrometry (MS); neurogenesis; neuropeptide;
regeneration
ID PLURIPOTENT STEM-CELLS; HEAD-REGENERATION; PLANARIAN BRAIN; ANIMAL
REGENERATION; MOLECULAR ANALYSIS; NEUROPEPTIDES; PEPTIDOMICS;
EXPRESSION; DISCOVERY; SYSTEM
AB Tissue regeneration is a complex process that involves a mosaic of molecules that vary spatially and temporally. Insights into the chemical signaling underlying this process can be achieved with a multiplex and untargeted chemical imaging method such as mass spectrometry imaging (MSI), which can enable de novo studies of nervous system regeneration. A combination of MSI and multivariate statistics was used to differentiate peptide dynamics in the freshwater planarian flatworm Schmidtea mediterranea at different time points during cephalic ganglia regeneration. A protocol was developed to make S. mediterranea tissues amenable for MSI. MS ion images of planarian tissue sections allow changes in peptides and unknown compounds to be followed as a function of cephalic ganglia regeneration. In conjunction with fluorescence imaging, our results suggest that even though the cephalic ganglia structure is visible after 6 days of regeneration, the original chemical composition of these regenerated structures is regained only after 12 days. Differences were observed in many peptides, such as those derived from secreted peptide 4 and EYE53-1. Peptidomic analysis further identified multiple peptides from various known prohormones, histone proteins, and DNA- and RNA-binding proteins as being associated with the regeneration process. Mass spectrometry data also facilitated the identification of a new prohormone, which we have named secreted peptide prohormone 20 (SPP-20), and is up-regulated during regeneration in planarians.
C1 [Ong, Ta-Hsuan; Romanova, Elena V.; Yang, Ning; Zimmerman, Tyler A.; Lee, Ji Eun; Sweedler, Jonathan V.] Univ Illinois, Dept Chem, Urbana, IL 61801 USA.
[Ong, Ta-Hsuan; Romanova, Elena V.; Yang, Ning; Zimmerman, Tyler A.; Lee, Ji Eun; Sweedler, Jonathan V.] Univ Illinois, Beckman Inst, Urbana, IL 61801 USA.
[Roberts-Galbraith, Rachel H.; Collins, James J., III; Newmark, Phillip A.] Univ Illinois, Dept Cell & Dev Biol, Howard Hughes Med Inst, Urbana, IL 61801 USA.
[Kelleher, Neil L.] Northwestern Univ, Prote Ctr Excellence, Dept Chem, Evanston, IL 60611 USA.
[Kelleher, Neil L.] Northwestern Univ, Prote Ctr Excellence, Dept Mol Biosci, Evanston, IL 60611 USA.
[Zimmerman, Tyler A.] NIST, Mass Spectrometry Data Ctr Grp, Gaithersburg, MD 20899 USA.
[Collins, James J., III] Univ Texas SW Med Ctr Dallas, Dept Pharmacol, Dallas, TX 75390 USA.
[Lee, Ji Eun] Korea Inst Sci & Technol, Biomed Res Inst, Ctr Theragnosis, Seoul 136791, South Korea.
RP Sweedler, JV (reprint author), Univ Illinois, Dept Chem, Urbana, IL 61801 USA.
EM jsweedle@illinois.edu
RI Sweedler, Jonathan/A-9405-2009;
OI Sweedler, Jonathan/0000-0003-3107-9922; Zimmerman,
Tyler/0000-0002-5408-9771; Newmark, Phillip/0000-0003-0793-022X
FU National Institutes of Health NINDS [RO1 NS031609]; NICHD [R01
HD043403]; National Institute on Drug Abuse [P30 DA018310]
FX The work was supported by the National Institutes of Health NINDS Grant
RO1 NS031609, NICHD Grant R01 HD043403, and National Institute on Drug
Abuse Grant P30 DA018310. The content is solely the responsibility of
the authors and does not necessarily represent the official views of the
funding agencies. The authors have no conflicts of interest to declare.
NR 71
TC 0
Z9 0
U1 3
U2 8
PU AMER SOC BIOCHEMISTRY MOLECULAR BIOLOGY INC
PI BETHESDA
PA 9650 ROCKVILLE PIKE, BETHESDA, MD 20814-3996 USA
SN 0021-9258
EI 1083-351X
J9 J BIOL CHEM
JI J. Biol. Chem.
PD APR 8
PY 2016
VL 291
IS 15
BP 8109
EP 8120
DI 10.1074/jbc.M115.709196
PG 12
WC Biochemistry & Molecular Biology
SC Biochemistry & Molecular Biology
GA DJ2SZ
UT WOS:000374056700028
PM 26884331
ER
PT J
AU Perron, JK
Stewart, MD
Zimmerman, NM
AF Perron, Justin K.
Stewart, M. D., Jr.
Zimmerman, Neil M.
TI A new regime of Pauli-spin blockade
SO JOURNAL OF APPLIED PHYSICS
LA English
DT Article
ID DOUBLE-QUANTUM DOT; SINGLE-ELECTRON SPIN
AB Pauli-spin blockade (PSB) is a transport phenomenon in double quantum dots that allows for a type of spin to charge conversion often used to probe fundamental physics such as spin relaxation and singlet-triplet coupling. In this paper, we theoretically explore Pauli-spin blockade as a function of magnetic field B applied parallel to the substrate. In the well-studied low magnetic field regime, where PSB occurs in the forward (1, 1) -> (0, 2) tunneling direction, we highlight some aspects of PSB that are not discussed in detail in existing literature, including the change in size of both bias triangles measured in the forward and reverse biasing directions as a function of B. At higher fields, we predict a crossover to "reverse PSB" in which current is blockaded in the reverse direction due to the occupation of a spin singlet as opposed to the traditional triplet blockade that occurs at low fields. The onset of reverse PSB coincides with the development of a tail like feature in the measured bias triangles and occurs when the Zeeman energy of the polarized triplet equals the exchange energy in the (0, 2) charge configuration. In Si quantum dots, these fields are experimentally accessible; thus, this work suggests a way to observe a crossover in magnetic field to qualitatively different behavior. (C) 2016 AIP Publishing LLC.
C1 [Perron, Justin K.] Calif State Univ San Marcos, Dept Phys, San Marcos, CA 92096 USA.
[Perron, Justin K.] Natl Inst Stand & Technol, Joint Quantum Inst, Gaithersburg, MD 20899 USA.
[Perron, Justin K.; Stewart, M. D., Jr.; Zimmerman, Neil M.] Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
RP Perron, JK (reprint author), Calif State Univ San Marcos, Dept Phys, San Marcos, CA 92096 USA.; Perron, JK (reprint author), Natl Inst Stand & Technol, Joint Quantum Inst, Gaithersburg, MD 20899 USA.; Perron, JK; Zimmerman, NM (reprint author), Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
EM jperron@csusm.edu; Neil.Zimmerman@nist.gov
NR 23
TC 1
Z9 1
U1 2
U2 4
PU AMER INST PHYSICS
PI MELVILLE
PA 1305 WALT WHITMAN RD, STE 300, MELVILLE, NY 11747-4501 USA
SN 0021-8979
EI 1089-7550
J9 J APPL PHYS
JI J. Appl. Phys.
PD APR 7
PY 2016
VL 119
IS 13
AR 134307
DI 10.1063/1.4945393
PG 5
WC Physics, Applied
SC Physics
GA DJ4BK
UT WOS:000374150200020
ER
PT J
AU Tarling, GA
Hill, S
Peat, H
Fielding, S
Reiss, C
Atkinson, A
AF Tarling, G. A.
Hill, S.
Peat, H.
Fielding, S.
Reiss, C.
Atkinson, A.
TI Growth and shrinkage in Antarctic krill Euphausia superba is
sex-dependent
SO MARINE ECOLOGY PROGRESS SERIES
LA English
DT Article
DE Southern Ocean; Population dynamics; Production; Life cycle; Fishery
ID SOUTH GEORGIA; MEGANYCTIPHANES-NORVEGICA; MODELING GROWTH; BODY
SHRINKAGE; FREQUENCY DATA; LIPID-CONTENT; LARVAL KRILL; DANA; AGE;
LENGTH
AB The ability of Antarctic krill Euphausia superba Dana to withstand the overwintering period is critical to their success. Laboratory evidence suggests that krill may shrink in body length during this time in response to the low availability of food. Nevertheless, verification that krill can shrink in the natural environment is lacking because winter data are difficult to obtain. One of the few sources of winter krill population data is from commercial vessels. We examined length-frequency data of adult krill (> 35 mm total body length) obtained from commercial vessels in the Scotia-Weddell region and compared our results with those obtained from a combination of science and commercial sampling operations carried out in this region at other times of the year. Our analyses revealed body-length shrinkage in adult females but not males during winter, based on both the tracking of modal size classes over seasons and sex-ratio patterns. Other explanatory factors, such as differential mortality, immigration and emigration, could not explain the observed differences. The same pattern was also observed at South Georgia and in the Western Antarctic Peninsula. Fitted seasonally modulated von Bertalanffy growth functions predicted a pattern of overwintering shrinkage in all body-length classes of females, but only stagnation in growth in males. This shrinkage most likely reflects morphometric changes resulting from the contraction of the ovaries and is not necessarily an outcome of winter hardship. The sex-dependent changes that we observed need to be incorporated into life cycle and population dynamic models of this species, particularly those used in managing the fishery.
C1 [Tarling, G. A.; Hill, S.; Peat, H.; Fielding, S.] British Antarctic Survey, Nat Environm Res Council, Madingley Rd, Cambridge CB3 0ET, England.
[Reiss, C.] SW Fisheries Sci Ctr, 8604 La Jolla Shores Dr, La Jolla, CA 92037 USA.
[Atkinson, A.] Plymouth Marine Lab, Prospect Pl, Plymouth PL1 3DH, Devon, England.
RP Tarling, GA (reprint author), British Antarctic Survey, Nat Environm Res Council, Madingley Rd, Cambridge CB3 0ET, England.
EM gant@bas.ac.uk
RI Simeon, Hill/B-2307-2008
NR 73
TC 3
Z9 3
U1 5
U2 14
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 0171-8630
EI 1616-1599
J9 MAR ECOL PROG SER
JI Mar. Ecol.-Prog. Ser.
PD APR 7
PY 2016
VL 547
BP 61
EP 78
DI 10.3354/meps11634
PG 18
WC Ecology; Marine & Freshwater Biology; Oceanography
SC Environmental Sciences & Ecology; Marine & Freshwater Biology;
Oceanography
GA DJ5IT
UT WOS:000374241200005
ER
PT J
AU Thompson, AR
Hyde, JR
Watson, W
Chen, DC
Guo, LW
AF Thompson, Andrew R.
Hyde, John R.
Watson, William
Chen, Dustin C.
Guo, Lian W.
TI Rockfish assemblage structure and spawning locations in southern
California identified through larval sampling
SO MARINE ECOLOGY PROGRESS SERIES
LA English
DT Article
DE Sebastes; Southern California; Ecosystem based management; Conservation;
Biogeography
ID SARDINE SARDINOPS-SAGAX; COWCOD SEBASTES-LEVIS; COD GADUS-MORHUA; FISH
ASSEMBLAGES; ENGRAULIS-MORDAX; MARINE RESERVES; BIGHT; ECOSYSTEM;
HABITAT; PATTERNS
AB Differences in oceanographic conditions over short distances can dramatically affect the distribution of marine organisms over small spatial scales. In southern California, oceanographic conditions vary widely from east to west as the offshore region is impacted by cool, southern flowing California Current water, while the inshore is typically warmer and more productive. We investigated how patterns of distribution and abundance of larval, genetically identified rockfishes related to environmental conditions off southern California, the world's center of rockfish Sebastes spp. species diversity. The rockfish assemblage was dominated by small and short-lived species not typically targeted by recreational or commercial fishing (i.e. shortbelly S. jordani and squarespot S. hopkinsi rockfishes), but also contained moderate abundances of a few larger, targeted species (bank S. rufus and bocaccio S. paucispinis rockfishes). Spawning locations of many species were affected by environmental variability, as abundances of young (0 to 2 d old), targeted larvae were mainly found offshore in the cool, low primary production waters that also were relatively shallow and contained hard substrate. In contrast, untargeted species were more widespread and correlated positively only with hard substrate. Hotspots of species richness and targeted species were high within a large managed region, the Cowcod Conservation Area, indicating that it is effectively protecting important rockfish spawning habitat. This research highlights the need to account for environmental variation in habitat and assemblage structure when conducting marine spatial planning.
C1 [Thompson, Andrew R.; Hyde, John R.; Watson, William; Guo, Lian W.] NOAA, Fisheries Serv, Southwest Fisheries Sci Ctr, 8901 La Jolla Shores Dr, La Jolla, CA 92037 USA.
[Chen, Dustin C.] Univ San Diego, Dept Environm & Ocean Sci, San Diego, CA 92110 USA.
[Guo, Lian W.] Univ Massachusetts, Organism & Evolutionary Biol, 611 N Pleasant St, Amherst, MA 01003 USA.
RP Thompson, AR (reprint author), NOAA, Fisheries Serv, Southwest Fisheries Sci Ctr, 8901 La Jolla Shores Dr, La Jolla, CA 92037 USA.
EM andrew.thompson@noaa.gov
FU NOAA Fisheries and the Environment (FATE) grant
FX We express our deep gratitude to the crews of the RVs 'David Star
Jordan' and 'New Horizon' for collecting the samples, including, but not
limited to, David Ambrose, Noelle Bowlin, Sherri Charter, Dave Griffith,
Amy Hays and Sue Manion. We also appreciate the efforts of Amanda
Barker, Alice Brown, Brittany Idrizaj, Hannah Scholes, and Aryana
Sepassi who helped sort rockfish larvae from the plankton samples. The
manuscript was greatly improved by insightful comments from John Field,
Kevin Stierhoff and 3 anonymous reviewers. The habitat data used in this
study were acquired, processed, archived, and distributed by the
Seafloor Mapping Lab of California State University Monterey Bay with
help from Carrie Bretz. This work was partially funded by a NOAA
Fisheries and the Environment (FATE) grant.
NR 77
TC 0
Z9 0
U1 9
U2 10
PU INTER-RESEARCH
PI OLDENDORF LUHE
PA NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY
SN 0171-8630
EI 1616-1599
J9 MAR ECOL PROG SER
JI Mar. Ecol.-Prog. Ser.
PD APR 7
PY 2016
VL 547
BP 177
EP 192
DI 10.3354/meps11633
PG 16
WC Ecology; Marine & Freshwater Biology; Oceanography
SC Environmental Sciences & Ecology; Marine & Freshwater Biology;
Oceanography
GA DJ5IT
UT WOS:000374241200013
ER
PT J
AU Syzranov, SV
Ostrovsky, PM
Gurarie, V
Radzihovsky, L
AF Syzranov, S. V.
Ostrovsky, P. M.
Gurarie, V.
Radzihovsky, L.
TI Critical exponents at the unconventional disorder-driven transition in a
Weyl semimetal
SO PHYSICAL REVIEW B
LA English
DT Article
ID GROSS-NEVEU MODEL; CRITICAL-BEHAVIOR; BETA-FUNCTION; DEGENERATE
SEMICONDUCTORS; FERMION SEMIMETAL; ARCS
AB Disordered noninteracting systems in sufficiently high dimensions have been predicted to display a non-Anderson disorder-driven transition that manifests itself in the critical behavior of the density of states and other physical observables. Recently, the critical properties of this transition have been extensively studied for the specific case of Weyl semimetals by means of numerical and renormalisation-group approaches. Despite this, the values of the critical exponents at such a transition in a Weyl semimetal are currently under debate. We present an independent calculation of the critical exponents using a two-loop renormalization-group approach for Weyl fermions in 2 - epsilon dimensions and resolve controversies currently existing in the literature.
C1 [Syzranov, S. V.; Gurarie, V.; Radzihovsky, L.] Univ Colorado, Dept Phys, Boulder, CO 80309 USA.
[Syzranov, S. V.; Gurarie, V.; Radzihovsky, L.] Univ Colorado, Ctr Theory Quantum Matter, Boulder, CO 80309 USA.
[Ostrovsky, P. M.] Max Planck Inst Solid State Res, Heisenbergstr 1, D-70569 Stuttgart, Germany.
[Ostrovsky, P. M.] RAS, LD Landau Theoret Phys Inst, Moscow 119334, Russia.
[Radzihovsky, L.] Univ Colorado, JILA, NIST, Boulder, CO 80309 USA.
RP Syzranov, SV (reprint author), Univ Colorado, Dept Phys, Boulder, CO 80309 USA.; Syzranov, SV (reprint author), Univ Colorado, Ctr Theory Quantum Matter, Boulder, CO 80309 USA.
FU Alexander von Humboldt Foundation; NSF [DMR-1001240, DMR-1205303,
PHY-1211914, PHY-1125844]; Simons Foundation
FX We appreciate useful discussions with A. W. W. Ludwig. Our work was
supported by the Alexander von Humboldt Foundation through the Feodor
Lynen Research Fellowship (S.V.S.) and by the NSF grants DMR-1001240
(L.R. and S.V.S.), DMR-1205303(V.G. and S.V.S.), PHY-1211914 (V.G. and
S.V.S.), and PHY-1125844 (S.V.S.). L.R. also acknowledges support by the
Simons Investigator award from the Simons Foundation.
NR 39
TC 8
Z9 8
U1 3
U2 6
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 2469-9950
EI 2469-9969
J9 PHYS REV B
JI Phys. Rev. B
PD APR 7
PY 2016
VL 93
IS 15
AR 155113
DI 10.1103/PhysRevB.93.155113
PG 10
WC Physics, Condensed Matter
SC Physics
GA DI5WD
UT WOS:000373570300002
ER
PT J
AU Chaloupka, JL
Hickstein, DD
AF Chaloupka, Jan L.
Hickstein, Daniel D.
TI Dynamics of Strong-Field Double Ionization in Two-Color Counterrotating
Fields
SO PHYSICAL REVIEW LETTERS
LA English
DT Article
ID HIGH-HARMONIC-GENERATION; MULTIPHOTON IONIZATION; HELIUM; POLARIZATION;
DIFFRACTION
AB The double ionization of helium in bichromatic, circularly polarized intense laser fields is analyzed with a classical ensemble approach. It is found that counterrotating fields produce significant nonsequential double-ion yield and drive novel ionization dynamics. It is shown that distinct pathways to ionization can be modified by altering the relative intensities of the two colors, allowing for unique control of strong-field processes. Electrons are observed to return to the ion at different angles from the angle of ionization, opening new possibilities for probing electronic and molecular structure on the ultrafast time scale.
C1 [Chaloupka, Jan L.] Univ No Colorado, Dept Phys & Astron, Greeley, CO 80639 USA.
[Hickstein, Daniel D.] Univ Colorado, JILA, Dept Phys, Boulder, CO 80309 USA.
[Hickstein, Daniel D.] NIST, Boulder, CO 80309 USA.
RP Chaloupka, JL (reprint author), Univ No Colorado, Dept Phys & Astron, Greeley, CO 80639 USA.
FU US Department of Energy Office of Basic Energy Sciences Atomic Molecular
and Optical Sciences program
FX The work presented here represents an important departure from typical
strong-field double-ionization phenomena. The electron trajectories
driven by two-color counterrotating fields are complex and their shape
varies significantly depending on the makeup of the driving field. The
resulting electron momenta are spread throughout the transverse plane,
enabling sophisticated analysis of both the tunnel ionization and
rescattering processes. The angle of electron impact is shown to be very
different from the angle of release, and the excursion time exhibits a
remarkable diversity, from subcycle to single-cycle to multicycle time
scales. Understanding the details of this behavior represents a
significant opportunity for future theoretical and experimental study,
and provides a promising avenue for the tunable control of strong-field
processes. We are grateful for helpful discussions with Margaret
Murnane, Henry Kapteyn, Chris Mancuso, Jennifer Ellis, Franklin Dollar,
and Kevin Dorney. D. H. acknowledges support from the US Department of
Energy Office of Basic Energy Sciences Atomic Molecular and Optical
Sciences program.
NR 30
TC 10
Z9 10
U1 5
U2 14
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 0031-9007
EI 1079-7114
J9 PHYS REV LETT
JI Phys. Rev. Lett.
PD APR 7
PY 2016
VL 116
IS 14
AR 143005
DI 10.1103/PhysRevLett.116.143005
PG 5
WC Physics, Multidisciplinary
SC Physics
GA DI6CT
UT WOS:000373587500008
PM 27104705
ER
PT J
AU Hung, L
Guedj, C
Bernier, N
Blaise, P
Olevano, V
Sottile, F
AF Hung, L.
Guedj, C.
Bernier, N.
Blaise, P.
Olevano, V.
Sottile, F.
TI Interpretation of monoclinic hafnia valence electron energy-loss spectra
by time-dependent density functional theory
SO PHYSICAL REVIEW B
LA English
DT Article
ID MICROSCOPY; SILICON; SYSTEMS; HFO2; SI
AB We present the valence electron energy-loss spectrum and the dielectric function of monoclinic hafnia (m-HfO2) obtained from time-dependent density-functional theory (TDDFT) predictions and compared to energy-filtered spectroscopic imaging measurements in a high-resolution transmission-electron microscope. Fermi's golden rule density-functional theory (DFT) calculations can capture the qualitative features of the energy-loss spectrum, but we find that TDDFT, which accounts for local-field effects, provides nearly quantitative agreement with experiment. Using the DFT density of states and TDDFT dielectric functions, we characterize the excitations that result in the m-HfO2 energy-loss spectrum. The sole plasmon occurs between 13 and 16 eV, although the peaks similar to 28 and above 40 eV are also due to collective excitations. We furthermore elaborate on the first-principles techniques used, their accuracy, and remaining discrepancies among spectra. More specifically, we assess the influence of Hf semicore electrons (5p and 4f) on the energy-loss spectrum, and find that the inclusion of transitions from the 4f band damps the energy-loss intensity in the region above 13 eV. We study the impact of many-body effects in a DFT framework using the adiabatic local-density approximation (ALDA) exchange-correlation kernel, as well as from a many-body perspective using "scissors operators" matched to an ab initio GW calculation to account for self-energy corrections. These results demonstrate some cancellation of errors between self-energy and excitonic effects, even for excitations from the Hf 4f shell. We also simulate the dispersion with increasing momentum transfer for plasmon and collective excitation peaks.
C1 [Hung, L.; Sottile, F.] Univ Paris Saclay, CEA, CNRS, Lab Solides Irradies,Ecole Polytech, F-91128 Palaiseau, France.
[Hung, L.; Blaise, P.; Olevano, V.; Sottile, F.] ETSF, Liege, Belgium.
[Guedj, C.; Bernier, N.; Blaise, P.; Olevano, V.] Univ Grenoble Alpes, F-38000 Grenoble, France.
[Guedj, C.; Bernier, N.; Blaise, P.] CEA, LETI, MINATEC Campus, F-38054 Grenoble, France.
[Olevano, V.] CNRS, Inst Neel, F-38042 Grenoble, France.
[Hung, L.] Natl Inst Stand & Technol, NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA.
RP Hung, L (reprint author), Univ Paris Saclay, CEA, CNRS, Lab Solides Irradies,Ecole Polytech, F-91128 Palaiseau, France.; Hung, L (reprint author), ETSF, Liege, Belgium.; Hung, L (reprint author), Natl Inst Stand & Technol, NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA.
FU nanocharacterization platform (PFNC)
FX We acknowledge support from the nanocharacterization platform (PFNC)
(http://www.minatec.org/pfnc-plateforme-nanocaracterisation) for
experiment. This work was granted access to the HPC resources of IDRIS
under the allocations 2015096-655 and -544 made by GENCI (Grand
Equipement National de Calcul Intensif).
NR 37
TC 1
Z9 1
U1 5
U2 11
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 2469-9950
EI 2469-9969
J9 PHYS REV B
JI Phys. Rev. B
PD APR 6
PY 2016
VL 93
IS 16
AR 165105
DI 10.1103/PhysRevB.93.165105
PG 8
WC Physics, Condensed Matter
SC Physics
GA DI5WS
UT WOS:000373571800003
ER
PT J
AU Harder, G
Bartley, TJ
Lita, AE
Nam, SW
Gerrits, T
Silberhorn, C
AF Harder, Georg
Bartley, Tim J.
Lita, Adriana E.
Nam, Sae Woo
Gerrits, Thomas
Silberhorn, Christine
TI Single-Mode Parametric-Down-Conversion States with 50 Photons as a
Source for Mesoscopic Quantum Optics
SO PHYSICAL REVIEW LETTERS
LA English
DT Article
ID NUMBER-RESOLVING DETECTORS; KTP WAVE-GUIDES; TWIN BEAMS; EFFICIENCY;
LIGHT; ENTANGLEMENT; GENERATION; MECHANICS; CRYSTALS; PULSES
AB We generate pulsed, two-mode squeezed states in a single spatiotemporal mode with mean photon numbers up to 20. We directly measure photon-number correlations between the two modes with transition edge sensors up to 80 photons per mode. This corresponds roughly to a state dimensionality of 6400. We achieve detection efficiencies of 64% in the technologically crucial telecom regime and demonstrate the high quality of our measurements by heralded nonclassical distributions up to 50 photons per pulse and calculated correlation functions up to 40th order.
C1 [Harder, Georg; Bartley, Tim J.; Silberhorn, Christine] Univ Paderborn, Integrated Quantum Opt Grp, Appl Phys, D-33098 Paderborn, Germany.
[Bartley, Tim J.; Lita, Adriana E.; Nam, Sae Woo; Gerrits, Thomas] NIST, 325 Broadway, Boulder, CO 80305 USA.
RP Harder, G (reprint author), Univ Paderborn, Integrated Quantum Opt Grp, Appl Phys, D-33098 Paderborn, Germany.
EM georg.harder@uni-paderborn.de
FU Quantum Information Science Initiative (QISI); Deutsche
Forschungsgemeinschaft (DFG) [TRR142]; Deutscher Akademischer Austausch
Dienst (DAAD); Deutsche Forschungsgemeinschaft (DFG) via the Gottfried
Wilhelm Leibniz-Preis
FX This work was supported by the Quantum Information Science Initiative
(QISI) and the Deutsche Forschungsgemeinschaft (DFG) via TRR142 and via
the Gottfried Wilhelm Leibniz-Preis. T. J. B. acknowledges funding from
the Deutscher Akademischer Austausch Dienst (DAAD), and L. K. Shalm for
discussions. This work is a contribution of NIST, an agency of the U.S.
Government, and not subject to U.S. copyright.
NR 59
TC 8
Z9 8
U1 3
U2 10
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 0031-9007
EI 1079-7114
J9 PHYS REV LETT
JI Phys. Rev. Lett.
PD APR 6
PY 2016
VL 116
IS 14
AR 143601
DI 10.1103/PhysRevLett.116.143601
PG 5
WC Physics, Multidisciplinary
SC Physics
GA DI6CS
UT WOS:000373587400005
ER
PT J
AU Du, ZM
Domanski, PA
Payne, WV
AF Du, Zhimin
Domanski, Piotr A.
Payne, W. Vance
TI Effect of common faults on the performance of different types of vapor
compression systems
SO APPLIED THERMAL ENGINEERING
LA English
DT Article
DE Diagnostic efficiency; Fault detection; Fault diagnosis; Normalized
fault effect; Vapor compression system
ID AIR-HANDLING UNITS; VAV TERMINALS; DIAGNOSIS; SENSITIVITY; EQUIPMENT;
CHILLERS; CHARGE; IMPACT; FLOW
AB The effect of faults on the cooling capacity, coefficient of performance, and sensible heat ratio, was analyzed and compared for five split and rooftop systems, which use different types of expansion devices, compressors and refrigerants. The study applied multivariable polynomial and normalized performance models, which were developed for the studied systems for both fault-free and faulty conditions based on measurements obtained in a laboratory under controlled conditions. The analysis indicated differences in responses and trends between the studied systems, which underscores the challenge to devise a universal FDD algorithm for all vapor compression systems and the difficulty to develop a methodology for rating the performance of different FDD algorithms. Published by Elsevier Ltd.
C1 [Du, Zhimin] Shanghai Jiao Tong Univ, Sch Mech Engn, Shanghai 200030, Peoples R China.
[Du, Zhimin; Domanski, Piotr A.; Payne, W. Vance] NIST, HVAC&R Equipment Performance Grp, 100 Bur Dr,MS 8631, Gaithersburg, MD 20899 USA.
RP Domanski, PA (reprint author), NIST, HVAC&R Equipment Performance Grp, 100 Bur Dr,MS 8631, Gaithersburg, MD 20899 USA.
EM piotr.domanski@nist.gov
FU Intramural NIST DOC [9999-NIST]
NR 32
TC 2
Z9 2
U1 4
U2 6
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 1359-4311
J9 APPL THERM ENG
JI Appl. Therm. Eng.
PD APR 5
PY 2016
VL 98
BP 61
EP 72
DI 10.1016/j.applthermaleng.2015.11.108
PG 12
WC Thermodynamics; Energy & Fuels; Engineering, Mechanical; Mechanics
SC Thermodynamics; Energy & Fuels; Engineering; Mechanics
GA DJ0AE
UT WOS:000373863000006
PM 26929732
ER
PT J
AU Xiang, FM
Parviz, D
Givens, TM
Tzeng, P
Davis, EM
Stafford, CM
Green, MJ
Grunlan, JC
AF Xiang, Fangming
Parviz, Dorsa
Givens, Tara M.
Tzeng, Ping
Davis, Eric M.
Stafford, Christopher M.
Green, Micah J.
Grunlan, Jaime C.
TI Stiff and Transparent Multilayer Thin Films Prepared Through
Hydrogen-Bonding Layer-by-Layer Assembly of Graphene and Polymer
SO ADVANCED FUNCTIONAL MATERIALS
LA English
DT Article
DE elastic modulus; graphene; hydrogen bonding; layer-by-layer assembly;
light transmittance
ID FUNCTIONALIZED GRAPHENE; ELASTIC PROPERTIES; ORGANIC-SOLVENTS; OXYGEN
BARRIER; GAS BARRIER; NANOCOMPOSITES; CONDUCTIVITY; DISPERSIONS; SHEETS;
COMPOSITES
AB Due to their exceptional orientation of 2D nanofillers, layer-by-layer (LbL) assembled polymer/graphene oxide thin films exhibit unmatched mechanical performance relative to any conventionally produced counterparts with similar composition. Unprecedented mechanical property improvement, by replacing graphene oxide with pristine graphene, is demonstrated in this work. Polyvinylpyrrolidone-stabilized graphene platelets are alternately deposited with poly(acrylic acid) using hydrogen bonding assisted LbL assembly. Transmission electron microscopy imaging and the Halpin-Tsai model are used to demonstrate, for the first time, that intact graphene can be processed from water to generate polymer nanocomposite thin films with simultaneous parallel-alignment, high packing density, and exfoliation. A multilayer thin film with only 3.9 vol% of highly exfoliated, and structurally intact graphene, increases the elastic modulus (E) of a polymer multilayer thin film by 322% (from 1.41 to 4.81 GPa), while maintaining visible light transmittance of approximate to 90%. This is one of the greatest improvements in elastic modulus ever reported for a graphene-filled polymer nanocomposite with a glassy (E > 1 GPa) matrix. The technique described here provides a powerful new tool to improve nanocomposite properties (mechanical, gas transport, etc.) that can be universally applied to a variety of polymer matrices and 2D nanoplatelets.
C1 [Xiang, Fangming; Givens, Tara M.; Grunlan, Jaime C.] Texas A&M Univ, Dept Mech Engn, College Stn, TX 77843 USA.
[Parviz, Dorsa; Tzeng, Ping; Green, Micah J.] Texas A&M Univ, Artie McFerrin Dept Chem Engn, College Stn, TX 77843 USA.
[Davis, Eric M.; Stafford, Christopher M.] NIST, Mat Sci & Engn Div, 100 Bur Dr, Gaithersburg, MD 20899 USA.
[Xiang, Fangming] Natl Energy Technol Lab, 626 Cochrans Mill Rd, Pittsburgh, PA 15236 USA.
[Davis, Eric M.] Clemson Univ, Dept Chem & Biomol Engn, Clemson, SC 29634 USA.
RP Grunlan, JC (reprint author), Texas A&M Univ, Dept Mech Engn, College Stn, TX 77843 USA.
EM jgrunlan@tamu.edu
RI Grunlan, Jaime/K-3242-2016; Xiang, Fangming/L-4289-2014
OI Grunlan, Jaime/0000-0001-5241-9741; Xiang, Fangming/0000-0002-2022-8163
NR 48
TC 2
Z9 2
U1 33
U2 95
PU WILEY-V C H VERLAG GMBH
PI WEINHEIM
PA POSTFACH 101161, 69451 WEINHEIM, GERMANY
SN 1616-301X
EI 1616-3028
J9 ADV FUNCT MATER
JI Adv. Funct. Mater.
PD APR 5
PY 2016
VL 26
IS 13
BP 2143
EP 2149
DI 10.1002/adfm.201504758
PG 7
WC Chemistry, Multidisciplinary; Chemistry, Physical; Nanoscience &
Nanotechnology; Materials Science, Multidisciplinary; Physics, Applied;
Physics, Condensed Matter
SC Chemistry; Science & Technology - Other Topics; Materials Science;
Physics
GA DI8FX
UT WOS:000373738000010
ER
PT J
AU Adams, PD
Aertgeerts, K
Bauer, C
Bell, JA
Berman, HM
Bhat, TN
Blaney, JM
Bolton, E
Bricogne, G
Brown, D
Burley, SK
Case, DA
Clark, KL
Darden, T
Emsley, P
Feher, VA
Feng, ZK
Groom, CR
Harris, SF
Hendle, J
Holder, T
Joachimiak, A
Kleywegt, GJ
Krojer, T
Marcotrigiano, J
Mark, AE
Markley, JL
Miller, M
Minor, W
Montelione, GT
Murshudov, G
Nakagawa, A
Nakamura, H
Nicholls, A
Nicklaus, M
Nolte, RT
Padyana, AK
Peishoff, CE
Pieniazek, S
Read, RJ
Shao, CH
Sheriff, S
Smart, O
Soisson, S
Spurlino, J
Stouch, T
Svobodova, R
Tempel, W
Terwilliger, TC
Tronrud, D
Velankar, S
Ward, SC
Warren, GL
Westbrook, JD
Williams, P
Yang, HW
Young, J
AF Adams, Paul D.
Aertgeerts, Kathleen
Bauer, Cary
Bell, Jeffrey A.
Berman, Helen M.
Bhat, Talapady N.
Blaney, Jeff M.
Bolton, Evan
Bricogne, Gerard
Brown, David
Burley, Stephen K.
Case, David A.
Clark, Kirk L.
Darden, Tom
Emsley, Paul
Feher, Victoria A.
Feng, Zukang
Groom, Colin R.
Harris, Seth F.
Hendle, Jorg
Holder, Thomas
Joachimiak, Andrzej
Kleywegt, Gerard J.
Krojer, Tobias
Marcotrigiano, Joseph
Mark, Alan E.
Markley, John L.
Miller, Matthew
Minor, Wladek
Montelione, Gaetano T.
Murshudov, Garib
Nakagawa, Atsushi
Nakamura, Haruki
Nicholls, Anthony
Nicklaus, Marc
Nolte, Robert T.
Padyana, Anil K.
Peishoff, Catherine E.
Pieniazek, Susan
Read, Randy J.
Shao, Chenghua
Sheriff, Steven
Smart, Oliver
Soisson, Stephen
Spurlino, John
Stouch, Terry
Svobodova, Radka
Tempel, Wolfram
Terwilliger, Thomas C.
Tronrud, Dale
Velankar, Sameer
Ward, Suzanna C.
Warren, Gregory L.
Westbrook, John D.
Williams, Pamela
Yang, Huanwang
Young, Jasmine
TI Outcome of the First wwPDB/CCDC/D3R Ligand Validation Workshop
SO STRUCTURE
LA English
DT Article
ID PROTEIN DATA-BANK; CAMBRIDGE STRUCTURAL DATABASE; ELECTRON-DENSITY;
TASK-FORCE; INFORMATION; MACROMOLECULES; GENERATION; MOLECULES; TOOLS;
PDB
AB Crystallographic studies of ligands bound to biological macromolecules (proteins and nucleic acids) represent an important source of information concerning drug-target interactions, providing atomic level insights into the physical chemistry of complex formation between macromolecules and ligands. Of the more than 115,000 entries extant in the Protein Data Bank (PDB) archive, similar to 75% include at least one non-polymeric ligand. Ligand geometrical and stereochemical quality, the suitability of ligand models for in silico drug discovery and design, and the goodness-of-fit of ligand models to electron-density maps vary widely across the archive. We describe the proceedings and conclusions from the first Worldwide PDB/Cambridge Crystallographic Data Center/Drug Design Data Resource (wwPDB/CCDC/D3R) Ligand Validation Workshop held at the Research Collaboratory for Structural Bioinformatics at Rutgers University on July 30-31, 2015. Experts in protein crystallography from academe and industry came together with non-profit and for-profit software providers for crystallography and with experts in computational chemistry and data archiving to discuss and make recommendations on best practices, as framed by a series of questions central to structural studies of macromolecule-ligand complexes. What data concerning bound ligands should be archived in the PDB? How should the ligands be best represented? How should structural models of macromolecule-ligand complexes be validated? What supplementary information should accompany publications of structural studies of biological macromolecules? Consensus recommendations on best practices developed in response to each of these questions are provided, together with some details regarding implementation. Important issues addressed but not resolved at the workshop are also enumerated.
C1 [Adams, Paul D.] Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Mol Biophys & Integrated Bioimaging Div, Berkeley, CA 94720 USA.
[Aertgeerts, Kathleen] LLC, DART NeuroSci, San Diego, CA 92131 USA.
[Bauer, Cary] Bruker AXS Inc, Madison, WI 53711 USA.
[Bell, Jeffrey A.; Holder, Thomas] Schrodinger Inc, New York, NY 10036 USA.
[Berman, Helen M.; Burley, Stephen K.; Feng, Zukang; Shao, Chenghua; Westbrook, John D.; Yang, Huanwang; Young, Jasmine] State Univ New Jersey, Ctr Integrat Prote Res, Res Collaboratory Struct Bioinformat Prot D, Piscataway, NJ 08854 USA.
[Berman, Helen M.; Burley, Stephen K.; Feng, Zukang; Marcotrigiano, Joseph; Westbrook, John D.; Yang, Huanwang; Young, Jasmine] State Univ New Jersey, Dept Chem & Chem Biol Rutgers, Piscataway, NJ 08854 USA.
[Bhat, Talapady N.] NIST, Biosyst & Biomat Div, Gaithersburg, MD 20899 USA.
[Blaney, Jeff M.; Harris, Seth F.] South San Francisco, Genentech Inc, San Francisco, CA 94080 USA.
[Bolton, Evan] US Natl Lib Med, Natl Ctr Biotechnol Informat, Bethesda, MD 20894 USA.
[Bricogne, Gerard] Global Phasing Ltd, Cambridge CB3 0AX, England.
[Brown, David] Charles River Ltd, Struct Biol & Biophys, Cambridge CB10 1XL, England.
[Burley, Stephen K.] Univ Calif San Diego, San Diego Supercomputer Ctr, Skaggs Sch Pharm & Pharmaceut Sci, La Jolla, CA 92093 USA.
[Clark, Kirk L.] Novartis Inst BioMed Res, Cambridge, MA 02139 USA.
[Darden, Tom] OpenEye Sci, Cambridge, MA 02142 USA.
[Emsley, Paul; Nicholls, Anthony; Warren, Gregory L.] MRC Lab Mol Biol, Cambridge CB2 0QH, England.
[Feher, Victoria A.; Murshudov, Garib] Univ Calif San Diego, Dept Chem & Biochem, Drug Design Data Resource, La Jolla, CA 92093 USA.
[Groom, Colin R.] Cambridge Crystallog Data Ctr, Cambridge CB2 1EZ, England.
[Hendle, Jorg; Ward, Suzanna C.] Lilly Biotechnol Ctr, Structural Biol, San Diego, CA 92121 USA.
[Joachimiak, Andrzej] Argonne Natl Lab, Biosci, Structural Biol Ctr, Argonne, IL 60439 USA.
[Kleywegt, Gerard J.] European Bioinformat Inst, European Mol Biol Lab, Protein Data Bank Europe, Cambridge CB10 1SD, England.
[Krojer, Tobias; Velankar, Sameer] Univ Oxford, Structural Genom Consortium, Oxford OX3 7DQ, England.
[Marcotrigiano, Joseph; Montelione, Gaetano T.; Smart, Oliver] State Univ New Jersey, Ctr Adv Biotechnol & Med, Piscataway, NJ 08854 USA.
[Mark, Alan E.; Miller, Matthew] Univ Queensland, Sch Chem & Mol Biosci, St Lucia, Qld 4072, Australia.
[Markley, John L.] Univ Wisconsin, Dept Biochem, BioMagResBank, Madison, WI 53706 USA.
[Minor, Wladek] Univ Virginia, Dept Mol Physiol & Biol Phys, Charlottesville, VA 22908 USA.
[Montelione, Gaetano T.] State Univ New Jersey, Dept Mol Biol & Biochem, Piscataway, NJ 08854 USA.
[Nakagawa, Atsushi; Nakamura, Haruki] Osaka Univ, Inst Prot Res, Protein Data Bank Japan, Osaka 5650871, Japan.
[Nicklaus, Marc] Natl Inst Hlth, Natl Canc Inst, Ctr Canc Res, Computer Aided Drug Design Grp, Frederick, MD 21702 USA.
[Nolte, Robert T.; Peishoff, Catherine E.] Collegeville, GlaxoSmithKline, Collegeville, PA 19426 USA.
[Padyana, Anil K.] Agios Pharmaceut Inc, Cambridge, MA 02139 USA.
[Pieniazek, Susan] Bristol Myers Squibb Res & Dev, Pennington, NJ 08534 USA.
[Read, Randy J.] Univ Cambridge, Cambridge Inst Med Res, Dept Haematol, Cambridge CB2 0XY, England.
[Soisson, Stephen] Bristol Myers Squibb Res & Dev, Princeton, NJ 08543 USA.
[Soisson, Stephen] Merck Res Labs, West Point, PA 19486 USA.
[Spurlino, John] Janssen Pharmaceut Inc, Spring House, PA 19002 USA.
[Stouch, Terry] Sci Solut LLC, West Windsor, NJ 08550 USA.
[Svobodova, Radka] Masaryk Univ, Natl Ctr Biomol Res, CEITEC Cent European Inst Technol, Brno 62500, Czech Republic.
[Tempel, Wolfram] Univ Toronto, Structural Genom Consortium, Toronto, ON M5G IL7, Canada.
[Terwilliger, Thomas C.] Alamos Natl Lab, Biosci Div, Los Alamos, NM 87545 USA.
[Tronrud, Dale] Oregon State Univ, Dept Biochem & Biophys, Corvallis, OR 97331 USA.
[Williams, Pamela] Atex Pharmaceut, Cambridge CB4 0QA, England.
RP Burley, SK (reprint author), State Univ New Jersey, Ctr Integrat Prote Res, Res Collaboratory Struct Bioinformat Prot D, Piscataway, NJ 08854 USA.; Burley, SK (reprint author), State Univ New Jersey, Dept Chem & Chem Biol Rutgers, Piscataway, NJ 08854 USA.; Burley, SK (reprint author), Univ Calif San Diego, San Diego Supercomputer Ctr, Skaggs Sch Pharm & Pharmaceut Sci, La Jolla, CA 92093 USA.; Feher, VA (reprint author), Univ Calif San Diego, Dept Chem & Biochem, Drug Design Data Resource, La Jolla, CA 92093 USA.; Groom, CR (reprint author), Cambridge Crystallog Data Ctr, Cambridge CB2 1EZ, England.
EM stephen.burley@rcsb.org; vfeher@ucsd.edu; groom@ccdc.cam.ac.uk
RI Svobodova Varekova, Radka/E-2867-2012; Terwilliger, Thomas/K-4109-2012;
Marcotrigiano, Joseph /K-6697-2016; Read, Randy/L-1418-2013; Mark,
Alan/A-8799-2011;
OI Minor, Wladek/0000-0001-7075-7090; Terwilliger,
Thomas/0000-0001-6384-0320; Marcotrigiano, Joseph /0000-0003-0346-3353;
Read, Randy/0000-0001-8273-0047; Mark, Alan/0000-0001-5880-4798; Smart,
Oliver/0000-0002-9669-1998; Kleywegt, Gerard J./0000-0002-4670-0331;
Velankar, Sameer/0000-0002-8439-5964; Nicklaus, Marc/0000-0002-4775-7030
FU National Science Foundation [DBI 1338415]; Wellcome Trust [104948];
JST-NBDC; National Institute of General Medical Sciences [GM109046,
GM111528]
FX The workshop was supported by funding to RCSB PDB by the National
Science Foundation (DBI 1338415); PDBe by the Wellcome Trust (104948);
PDBj by JST-NBDC; BMRB by the National Institute of General Medical
Sciences (GM109046); D3R by the National Institute of General Medical
Sciences (GM111528); registration fees from industrial participants; and
a tax-deductible donation to the wwPDB Foundation by the Bristol-Myers
Squibb Foundation.
NR 38
TC 11
Z9 11
U1 6
U2 13
PU CELL PRESS
PI CAMBRIDGE
PA 600 TECHNOLOGY SQUARE, 5TH FLOOR, CAMBRIDGE, MA 02139 USA
SN 0969-2126
EI 1878-4186
J9 STRUCTURE
JI Structure
PD APR 5
PY 2016
VL 24
IS 4
BP 502
EP 508
DI 10.1016/j.str.2016.02.017
PG 7
WC Biochemistry & Molecular Biology; Biophysics; Cell Biology
SC Biochemistry & Molecular Biology; Biophysics; Cell Biology
GA DI5VN
UT WOS:000373568700005
PM 27050687
ER
PT J
AU Loh, W
Becker, J
Cole, DC
Coillet, A
Baynes, FN
Papp, SB
Diddams, SA
AF Loh, William
Becker, Joe
Cole, Daniel C.
Coillet, Aurelien
Baynes, Fred N.
Papp, Scott B.
Diddams, Scott A.
TI A microrod-resonator Brillouin laser with 240Hz absolute linewidth
SO NEW JOURNAL OF PHYSICS
LA English
DT Article
DE microresonators; lasers; stimulated Brillouin scattering; narrow
linewidth
ID MICRORESONATOR FREQUENCY COMBS; FIBER LASER; SEMICONDUCTOR-LASER;
MICROCAVITY; CHIP; GENERATION; SILICON
AB We demonstrate an ultralow-noise microrod-resonator based laser that oscillates on the gain supplied by the stimulated Brillouin scattering optical nonlinearity. Microresonator Brillouin lasers are known to offer an outstanding frequency noise floor, which is limited by fundamental thermal fluctuations. Here, we show experimental evidence that thermal effects also dominate the close-to-carrier frequency fluctuations. The 6 mm diameter microrod resonator used in our experiments has a large optical mode area of similar to 100 mu m(2), and hence its 10 ms thermal time constant filters the close-to-carrier optical frequency noise. The result is an absolute laser linewidth of 240 Hz with a corresponding white-frequency noise floor of 0.1 Hz(2) Hz(-1). We explain the steady-state performance of this laser by measurements of its operation state and of its mode detuning and lineshape. Our results highlight a mechanism for noise that is common to many microresonator devices due to the inherent coupling between intracavity power and mode frequency. We demonstrate the ability to reduce this noise through a feedback loop that stabilizes the intracavity power.
C1 [Loh, William; Becker, Joe; Cole, Daniel C.; Coillet, Aurelien; Baynes, Fred N.; Papp, Scott B.; Diddams, Scott A.] NIST, 325 Broadway, Boulder, CO 80305 USA.
RP Loh, W (reprint author), NIST, 325 Broadway, Boulder, CO 80305 USA.
EM William.Loh@nist.gov
FU NIST; DARPA PULSE Program; NRC/NAS; NSF GRFP [DGE 1144083]
FX We thank Dr Marco Schioppo, Dr Gabe Ycas, and Professor Kerry J Vahala
for their valuable comments on this manuscript. This work was funded by
NIST and the DARPA PULSE Program. WL acknowledges support from the
NRC/NAS. DC acknowledges support from the NSF GRFP under Grant No. DGE
1144083. This work is a contribution of the US Government and is not
subject to copyright in the US.
NR 36
TC 2
Z9 2
U1 5
U2 13
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 APR 4
PY 2016
VL 18
AR 045001
DI 10.1088/1367-2630/18/4/045001
PG 9
WC Physics, Multidisciplinary
SC Physics
GA DL2NN
UT WOS:000375472200001
ER
PT J
AU Kim, YS
Davis, R
Uddin, N
Nyden, M
Rabb, SA
AF Kim, Yeon Seok
Davis, Rick
Uddin, Nasir
Nyden, Marc
Rabb, Savelas A.
TI Quantification of nanoparticle release from polymer nanocomposite
coatings due to environmental stressing
SO JOURNAL OF OCCUPATIONAL AND ENVIRONMENTAL HYGIENE
LA English
DT Article
DE simulated chewing; ICP-OES; UV-Vis; Engineered nanoparticle; simulated
wear and tear; layer-by-layer assembly
ID WALL CARBON NANOTUBES; POLYURETHANE FOAM FLAMMABILITY; FILLED COATINGS;
REDUCE; NANOARCHITECTURES; PURIFICATION; NANOCOATINGS; DISPERSIONS;
COMPOSITES; ASSEMBLIES
AB Certain engineered nanoparticles (ENP) reduce the flammability of components used in soft furnishings (mattresses and upholstered furniture). However, because of the ENP's small size and ability to interact with biological molecules, these fire retardant ENPs may pose a health and environmental risks, if they are released sometime during the life cycle of the soft furnishing. Quantifying the released amount of these ENPs under normal end-use circumstances provides a basis for assessing their potential health and environmental impact. In this article, we report on efforts to identify suitable methodologies for quantifying the release of carbon nanofibers, carbon nanotubes, and sodium montmorillonites from coatings applied to the surfaces of barrier fabric and polyurethane foam. The ENPs released in simulated chewing and mechanical stressing experiments were collected in aqueous solution and quantified using Ultraviolet-Visible and inductively coupled plasma-optical emission spectroscopy. The microstructures of the released ENPs were characterized using scanning electron microscopy. The reported methodology and results provide important milestones to estimate the impact and toxicity of the ENP release during the life cycle of the nanocomposites. To our knowledge, this is the first study of ENP release from the soft furnishing coating, something that can be important application area for fire safety.
C1 [Kim, Yeon Seok; Davis, Rick; Uddin, Nasir; Nyden, Marc; Rabb, Savelas A.] NIST, 100 Bur Dr MS-8665, Gaithersburg, MD 20899 USA.
RP Kim, YS (reprint author), NIST, 100 Bur Dr MS-8665, Gaithersburg, MD 20899 USA.
EM yeonkim@nist.gov
FU Consumer Product Safety Commission
FX This work was partially supported by the Consumer Product Safety
Commission.
NR 44
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Z9 0
U1 7
U2 25
PU TAYLOR & FRANCIS INC
PI PHILADELPHIA
PA 530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA
SN 1545-9624
EI 1545-9632
J9 J OCCUP ENVIRON HYG
JI J. Occup. Environ. Hyg.
PD APR 2
PY 2016
VL 13
IS 4
BP 307
EP 317
DI 10.1080/15459624.2015.1116696
PG 11
WC Environmental Sciences; Public, Environmental & Occupational Health
SC Environmental Sciences & Ecology; Public, Environmental & Occupational
Health
GA DE2VW
UT WOS:000370486300006
PM 26647208
ER
PT J
AU Marvel, JA
Bostelman, R
AF Marvel, Jeremy A.
Bostelman, Roger
TI Test Methods for the Evaluation of Manufacturing Mobile Manipulator
Safety
SO JOURNAL OF ROBOTICS AND MECHATRONICS
LA English
DT Article
DE mobile manipulators; AGV safety; robot safety
AB This paper presents a test methodology for evaluating the safety of mobile manipulators (robot arms mounted on mobile bases). This methodology addresses the safety concerns relevant to modern, agile, manufacturing practices in which mobile manipulators will play a significant role. We consider 1) the unique capabilities and anticipated uses of mobile manipulators and 2) the potential exemptions and special cases in which their behavior may be unpredictable or otherwise contrary to the safety requirements. Finally, we define metrics for assessing compliance with functional safety requirements and anticipated performance.
C1 [Marvel, Jeremy A.; Bostelman, Roger] Natl Inst Stand & Technol, 100 Bur Dr,Stop 8230, Gaithersburg, MD 20899 USA.
[Bostelman, Roger] Univ Bourgogne, IEM, Le2i, BP 47870, F-21078 Dijon, France.
RP Marvel, JA (reprint author), Natl Inst Stand & Technol, 100 Bur Dr,Stop 8230, Gaithersburg, MD 20899 USA.
EM jeremy.marvel@nist.gov; roger.bostelman@nist.gov
NR 24
TC 0
Z9 0
U1 1
U2 1
PU FUJI TECHNOLOGY PRESS LTD
PI TOKYO
PA 4F TORANOMON SANGYO BLDG, 2-29, TORANOMON 1-CHOME, MINATO-KU, TOKYO,
105-0001, JAPAN
SN 0915-3942
EI 1883-8049
J9 J ROBOT MECHATRON
JI J. Robot. Mechatron.
PD APR
PY 2016
VL 28
IS 2
BP 199
EP 214
PG 16
WC Robotics
SC Robotics
GA EJ8DH
UT WOS:000393454500012
ER
PT J
AU Ding, YN
Carton, JA
Chepurin, GA
Steele, M
Hakkinen, S
AF Ding, Yanni
Carton, James A.
Chepurin, Gennady A.
Steele, Michael
Hakkinen, Sirpa
TI Seasonal heat and freshwater cycles in the Arctic Ocean in CMIP5 coupled
models
SO JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
LA English
DT Article
ID INTERCOMPARISON PROJECT; CLIMATE; ICE; VARIABILITY; REANALYSIS;
ATLANTIC; REGIMES; SYSTEM
AB This study examines the processes governing the seasonal response of the Arctic Ocean and sea ice to surface forcings as they appear in historical simulations of 14 Coupled Model Intercomparison Project Phase 5 coupled climate models. In both models and observations, the seasonal heat budget is dominated by a local balance between net surface heating and storage in the heat content of the ocean and in melting/freezing of sea ice. Observations suggest ocean heat storage is more important than sea ice melt, while in most of these models, sea ice melt dominates. Seasonal horizontal heat flux divergence driven by the seasonal cycle of volume transport is only important locally. In models and observations, the dominant terms in the basin-average seasonal freshwater budget are the storages of freshwater between the ocean and sea ice, and the exchange between the two. The largest external source term is continental discharge in early summer, which is an order of magnitude smaller. The appearance of sea ice (extent and volume) and also ocean stratification in both the heat and freshwater budgets provides two links between the budgets and provides two mechanisms for feedback. One consequence of such an interaction is the fact that models with strong/weak seasonal surface heating also have strong/weak seasonal haline and temperature stratification.
C1 [Ding, Yanni; Carton, James A.; Chepurin, Gennady A.] Univ Maryland, Dept Atmospher & Ocean Sci, College Pk, MD 20742 USA.
[Steele, Michael] Univ Washington, Appl Phys Lab, Polar Sci Ctr, Seattle, WA 98105 USA.
[Hakkinen, Sirpa] NOAA, Goddard Space Flight Ctr, Greenbelt, MD USA.
RP Carton, JA (reprint author), Univ Maryland, Dept Atmospher & Ocean Sci, College Pk, MD 20742 USA.
EM carton@atmos.umd.edu
FU National Science Foundation [OCE1233942]; NSF [OCE1233255]; Forum for
Arctic Modeling and Observational Synthesis (FAMOS)
FX Y.D., G.A.C., and J.A.C. gratefully acknowledge support from the
National Science Foundation (OCE1233942). Support for M.S. was provided
by NSF grant OCE1233255. We thank the World Climate Research Program's
Working Group on Coupled Modeling, which is responsible for CMIP, and
the climate modeling groups for producing and making available their
model output. For CMIP, the U.S. Department of Energy's Program for
Climate Model Diagnosis and Intercomparison (www-pcmdi.llnl.gov)
provides coordinating support and led development of software
infrastructure in partnership with the Global Organization for Earth
System Science Portals. We thank the Geophysical Fluid Dynamics
Laboratory for providing output from the two GFDL-ESM models used here.
We thank the ECMWF, NSIDC, and PSC teams for the ERA-40 atmospheric
fluxes, sea ice extent, PHC3.0 ocean climatology, and PIOMAS sea ice
volume data. ERA-40 data were downloaded from
http://apps.ecmwf.int/datasets/data/era40-moda/in 2014. The sea ice
extent was downloaded from http://nsidc.org/data/on February 2014. The
PHC3.0 ocean climatology was downloaded from
http://psc.apl.washington.edu/nonwp_projects/PHC/ on October 2013. The
PIOMAS data were downloaded from
http://psc.apl.uw.edu/research/projects/arctic-sea-ice-volume-anomaly/da
ta/on May 2015. We thank the support from Forum for Arctic Modeling and
Observational Synthesis (FAMOS).
NR 42
TC 1
Z9 1
U1 0
U2 0
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 APR
PY 2016
VL 121
IS 4
BP 2043
EP 2057
DI 10.1002/2015JC011124
PG 15
WC Oceanography
SC Oceanography
GA DW2HA
UT WOS:000383462300001
ER
PT J
AU Dmitrenko, IA
Kirillov, SA
Forest, A
Gratton, Y
Volkov, DL
Williams, WJ
Lukovich, JV
Belanger, C
Barber, DG
AF Dmitrenko, Igor A.
Kirillov, Sergei A.
Forest, Alexandre
Gratton, Yves
Volkov, Denis L.
Williams, William J.
Lukovich, Jennifer V.
Belanger, Claude
Barber, David G.
TI Shelfbreak current over the Canadian Beaufort Sea continental slope:
Wind-driven events in January 2005
SO JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
LA English
DT Article
ID ARCTIC-OCEAN SURFACE; HALOCLINE WATERS; MACKENZIE SHELF; PACIFIC WATER;
VARIABILITY; ATLANTIC; BASIN; CIRCULATION; WINTER; GRACE
AB The shelfbreak current over the Beaufort Sea continental slope is known to be one of the most energetic features of the Beaufort Sea hydrography. In January 2005, three oceanographic moorings deployed over the Canadian (eastern) Beaufort Sea continental slope simultaneously recorded two consecutive shelfbreak current events with along-slope eastward bottom-intensified flow up to 120 cm s(-1). Both events were generated by the local wind forcing associated with two Pacific-born cyclones passing north of the Beaufort Sea continental slope toward the Canadian Archipelago. Over the mooring array, the associated westerly wind exceeded 15 m s(-1). These two cyclones generated storm surges along the Beaufort Sea coast with sea surface height (SSH) rising up to 1.4 m following the two westerly wind maxima. We suggest that the westerly along-slope wind generated a surface Ekman onshore transport. The associated SSH increase over the shelf produced a cross-slope pressure gradient that drove an along-slope eastward geostrophic current, in the same direction as the wind. This wind-driven barotropic flow was superimposed on the background baroclinic bottom-intensified shelfbreak current that consequently amplified. Summer-fall satellite altimetry data for 1992-2013 show that the SSH gradient in the southeastern Beaufort Sea is enhanced over the upper continental slope in response to frequent storm surge events. Because the local wind forcing and/or sea-ice drift could not explain the reduction of sea-ice concentration over the Beaufort Sea continental slope in January 2005, we speculate that wind-driven sea level fluctuations may impact the sea-ice cover in winter.
C1 [Dmitrenko, Igor A.; Kirillov, Sergei A.; Lukovich, Jennifer V.; Barber, David G.] Univ Manitoba, Ctr Earth Observat Sci, Winnipeg, MB, Canada.
[Forest, Alexandre] Golder Associates, Quebec City, PQ, Canada.
[Gratton, Yves; Belanger, Claude] Inst Natl Rech Sci Eau Terre Environm, Quebec City, PQ, Canada.
[Volkov, Denis L.] Univ Miami, Cooperat Inst Marine & Atmospher Studies, Miami, FL USA.
[Volkov, Denis L.] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
[Williams, William J.] Fisheries & Oceans Canada, Inst Ocean Sci, Sidney, BC, Canada.
RP Dmitrenko, IA (reprint author), Univ Manitoba, Ctr Earth Observat Sci, Winnipeg, MB, Canada.
EM igor.dmitrenko@umanitoba.ca
RI Volkov, Denis/A-6079-2011;
OI Volkov, Denis/0000-0002-9290-0502; Forest, Alexandre/0000-0001-9002-947X
FU National Sciences and Engineering Research Council of Canada (NSERC)
[RGPIN-2014-03606]; NOAA Atlantic Oceanographic and Meteorological
Laboratory; CNES
FX The data used for this research were collected under the ArcticNet
framework, project Long-Term Oceanic Observatories in the Canadian
Arctic. We gratefully acknowledge the support by the Canada Excellence
Research Chair (CERC) and the Canada Research Chairs (CRC) programs.
This work is a contribution to the joint Canadian-Danish-Greenland ASP
cooperation. The research was also partly supported by National Sciences
and Engineering Research Council of Canada (NSERC, grant
RGPIN-2014-03606) and the base funds of NOAA Atlantic Oceanographic and
Meteorological Laboratory. The CTD and velocity data are available
through the Polar Data Catalogue at https://www.polardata.ca/pdcsearch/,
CCIN Reference #11653 and #11792. The SSH data were produced by
Ssalto/Duacs and distributed by Aviso (www.aviso.oceanobs.com) with
support from CNES.
NR 53
TC 0
Z9 0
U1 5
U2 5
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 APR
PY 2016
VL 121
IS 4
BP 2447
EP 2468
DI 10.1002/2015JC011514
PG 22
WC Oceanography
SC Oceanography
GA DW2HA
UT WOS:000383462300020
ER
PT J
AU Fedchak, JA
Scherschligt, J
Sefa, M
AF Fedchak, James A.
Scherschligt, Julia
Sefa, Makfir
TI How to Build a Vacuum Spring-transport Package for Spinning Rotor Gauges
SO JOVE-JOURNAL OF VISUALIZED EXPERIMENTS
LA English
DT Article
DE Engineering; Issue 110; Spinning Rotor Gauge; Spring-Transport
Mechanism; High-Vacuum Calibrations; Vacuum Metrology; Key Comparison;
Vacuum Gauge; Gauge Stability
AB The spinning rotor gauge (SRG) is a high-vacuum gauge often used as a secondary or transfer standard for vacuum pressures in the range of 1.0 x 10(-4) Pa to 1.0 Pa. In this application, the SRGs are frequently transported to laboratories for calibration. Events can occur during transportation that change the rotor surface conditions, thus changing the calibration factor. To assure calibration stability, a spring-transport mechanism is often used to immobilize the rotor and keep it under vacuum during transport. It is also important to transport the spring-transport mechanism using packaging designed to minimize the risk of damage during shipping. In this manuscript, a detailed description is given on how to build a robust spring-transport mechanism and shipping container. Together these form a spring-transport package. The spring-transport package design was tested using drop-tests and the performance was found to be excellent. The present spring-transport mechanism design keeps the rotor immobilized when experiencing shocks of several hundred g (g = 9.8 m/sec(2) and is the acceleration due to gravity), while the shipping container assures that the mechanism will not experience shocks greater than about 100 g during common shipping mishaps (as defined by industry standards).
C1 [Fedchak, James A.; Scherschligt, Julia; Sefa, Makfir] NIST, Thermodynam Metrol Grp, Sensor Sci Div, Gaithersburg, MD 20899 USA.
RP Fedchak, JA (reprint author), NIST, Thermodynam Metrol Grp, Sensor Sci Div, Gaithersburg, MD 20899 USA.
EM james.fedchak@nist.gov
NR 13
TC 0
Z9 0
U1 0
U2 0
PU JOURNAL OF VISUALIZED EXPERIMENTS
PI CAMBRIDGE
PA 1 ALEWIFE CENTER, STE 200, CAMBRIDGE, MA 02140 USA
SN 1940-087X
J9 JOVE-J VIS EXP
JI J. Vis. Exp.
PD APR
PY 2016
IS 110
AR e53937
DI 10.3791/53937
PG 12
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DR9ZX
UT WOS:000380256000065
PM 27078575
ER
PT J
AU Chan, PW
Zhang, P
Doviak, R
AF Chan, P. W.
Zhang, P.
Doviak, R.
TI Calculation and application of eddy dissipation rate map based on
spectrum width data of a S-band radar in Hong Kong
SO MAUSAM
LA English
DT Article
DE Weather radar; Eddy dissipation rate; Severe turbulence
ID DOPPLER LIDAR; TURBULENCE
AB The spectrum width data of an S-band radar in Hong Kong are used to calculate the map of eddy dissipation rate (EDR) with the objective of providing turbulence alerting service for the en-route aircraft in the Pearl River Delta region. The calculation methodology is different from that reported in the existing literature by also removing the wind shear contribution in determining the radar-based EDR. The performance of the EDR maps obtained from the conical scans of the radar is illustrated in two examples of moderate to severe turbulence reported by the aircraft. In both cases, based on the EDR values and windshear hazard factors determined from the aircraft data, the airflow disturbances could adversely affect the operation of the aircraft. By overlaying the flight route on the radar's reflectivity imageries, it appears that, in both cases, the disturbed airflow is associated with rather intense rain cells, though they are rather small and isolated. The EDR values calculated from the radar's spectrum width data at the locations of the rain cells are generally consistent with those determined using the aircraft's wind measurements. From the selected cases, it seems that the radar-based EDR values have generally satisfactory quality. If such data could be available at the cockpit through data uplinking, they could be useful hints for the pilots not to fly through the rain cells but rather going around them. The methodology may be applied to the radars in the Pearl River Delta region in order to construct a three-dimensional mosaic of turbulence intensity for the assurance of aviation safety.
C1 [Chan, P. W.] Hong Kong Observ, Hong Kong, Hong Kong, Peoples R China.
[Zhang, P.] Univ Oklahoma, CIMMS, Norman, OK 73019 USA.
[Doviak, R.] NOAA, Natl Severe Storms Lab, Norman, OK 73069 USA.
RP Chan, PW (reprint author), Hong Kong Observ, Hong Kong, Hong Kong, Peoples R China.
EM pwchan@hko.gov.hk
RI Chan, Pak Wai/C-8447-2011
OI Chan, Pak Wai/0000-0003-2289-0609
NR 17
TC 0
Z9 0
U1 4
U2 4
PU INDIA METEOROLOGICAL DEPT
PI NEW DELHI
PA MAUSAM BHAWAN, LODI RD, NEW DELHI, 110 003, INDIA
SN 0252-9416
J9 MAUSAM
JI Mausam
PD APR
PY 2016
VL 67
IS 2
BP 411
EP 422
PG 12
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DS0PI
UT WOS:000380298800008
ER
PT J
AU Berkelhammer, M
Noone, DC
Steen-Larsen, HC
Bailey, A
Cox, CJ
O'Neill, MS
Schneider, D
Steffen, K
White, JWC
AF Berkelhammer, Max
Noone, David C.
Steen-Larsen, Hans Christian
Bailey, Adriana
Cox, Christopher J.
O'Neill, Michael S.
Schneider, David
Steffen, Konrad
White, James W. C.
TI Surface-atmosphere decoupling limits accumulation at Summit, Greenland
SO SCIENCE ADVANCES
LA English
DT Article
ID ICE-SHEET; SNOW ACCUMULATION; WATER-VAPOR; ISOTOPIC COMPOSITION;
HYDROGEN ISOTOPES; ANTARCTIC PLATEAU; CLIMATE-CHANGE; SEA-ICE; OXYGEN;
TEMPERATURE
AB Despite rapid melting in the coastal regions of the Greenland Ice Sheet, a significant area (similar to 40%) of the ice sheet rarely experiences surface melting. In these regions, the controls on annual accumulation are poorly constrained owing to surface conditions (for example, surface clouds, blowing snow, and surface inversions), which render moisture flux estimates from myriad approaches (that is, eddy covariance, remote sensing, and direct observations) highly uncertain. Accumulation is partially determined by the temperature dependence of saturation vapor pressure, which influences the maximum humidity of air parcels reaching the ice sheet interior. However, independent proxies for surface temperature and accumulation from ice cores show that the response of accumulation to temperature is variable and not generally consistent with a purely thermodynamic control. Using three years of stable water vapor isotope profiles from a high altitude site on the Greenland Ice Sheet, we show that as the boundary layer becomes increasingly stable, a decoupling between the ice sheet and atmosphere occurs. The limited interaction between the ice sheet surface and free tropospheric air reduces the capacity for surface condensation to achieve the rate set by the humidity of the air parcels reaching interior Greenland. The isolation of the surface also acts to recycle sublimated moisture by recondensing it onto fog particles, which returns the moisture back to the surface through gravitational settling. The observations highlight a unique mechanism by which ice sheet mass is conserved, which has implications for understanding both past and future changes in accumulation rate and the isotopic signal in ice cores from Greenland.
C1 [Berkelhammer, Max] Univ Illinois, Dept Earth & Environm Sci, Chicago, IL 60607 USA.
[Berkelhammer, Max; Noone, David C.; Steen-Larsen, Hans Christian; Bailey, Adriana; Cox, Christopher J.; O'Neill, Michael S.; Schneider, David; Steffen, Konrad] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Berkelhammer, Max; Noone, David C.; Bailey, Adriana; Cox, Christopher J.] Univ Colorado, Dept Atmospher & Ocean Sci, Boulder, CO 80309 USA.
[Noone, David C.] Oregon State Univ, Coll Earth Ocean & Atmospher Sci, Corvallis, OR 97331 USA.
[Steen-Larsen, Hans Christian] UMR CEA CNRS UVSQ IPSL 8212, Lab Sci Climat & Environm, Gif Sur Yvette, France.
[Steen-Larsen, Hans Christian] Univ Copenhagen, Ctr Ice & Climate, Copenhagen, Denmark.
[Bailey, Adriana] Univ Washington, Joint Inst Study Atmosphere & Ocean, Seattle, WA 98195 USA.
[Cox, Christopher J.; O'Neill, Michael S.] NOAA, Boulder, CO 80305 USA.
[Schneider, David] Natl Ctr Atmospher Res, Boulder, CO 80305 USA.
[Steffen, Konrad] Swiss Fed Res Inst WSL, Birmensdorf, Switzerland.
[White, James W. C.] Univ Colorado, Dept Geol Sci, Boulder, CO 80309 USA.
[White, James W. C.] Univ Colorado, Environm Studies Program, Boulder, CO 80309 USA.
[White, James W. C.] Univ Colorado, Inst Arctic & Alpine Res, Boulder, CO 80309 USA.
RP Berkelhammer, M (reprint author), Univ Illinois, Dept Earth & Environm Sci, Chicago, IL 60607 USA.; Berkelhammer, M (reprint author), Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.; Berkelhammer, M (reprint author), Univ Colorado, Dept Atmospher & Ocean Sci, Boulder, CO 80309 USA.
EM berkelha@uic.edu
RI White, James/A-7845-2009; Steen-Larsen, Hans Christian/F-9927-2013; Cox,
Christopher/O-4276-2016
OI White, James/0000-0001-6041-4684; Steen-Larsen, Hans
Christian/0000-0002-7202-5907; Cox, Christopher/0000-0003-2203-7173
NR 48
TC 1
Z9 1
U1 7
U2 11
PU AMER ASSOC ADVANCEMENT SCIENCE
PI WASHINGTON
PA 1200 NEW YORK AVE, NW, WASHINGTON, DC 20005 USA
SN 2375-2548
J9 SCI ADV
JI Sci. Adv.
PD APR
PY 2016
VL 2
IS 4
AR e1501704
DI 10.1126/sciadv.1501704
PG 9
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DR7IB
UT WOS:000380072100033
PM 27386509
ER
PT J
AU Denton, RE
Takahashi, K
Amoh, J
Singer, HJ
AF Denton, R. E.
Takahashi, Kazue
Amoh, Justice, Jr.
Singer, H. J.
TI Mass density at geostationary orbit and apparent mass refilling
SO JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
LA English
DT Article
ID O PLUS CONCENTRATION; ELECTRON-DENSITIES; MAGNETOSPHERE; EVOLUTION;
WAVES; STORM; MODEL
AB We used the inferred equatorial mass density rho(m,eq) based on measurements of Alfven wave frequencies measured by the GOES satellites during 1980-1991 in order to construct a number of different models of varying complexity for the equatorial mass density at geostationary orbit. The most complicated models are able to account for 66% of the variance with a typical variation from actual values of a factor of 1.56. The factors that influenced rho(m,eq) in the models were, in order of decreasing importance, the F-10.7 EUV index, magnetic local time, the solar wind dynamic pressure P-dyn, the phase of the year, and the solar wind B-Z (GSM Z direction). During some intervals, some of which were especially geomagnetically quiet, rho(m,eq) rose to values that were significantly higher than those predicted by our models. For 10 especially quiet intervals, we examined long-term (>1 day) apparent refilling, the increase in rho(m,eq) at a fixed location. We found that the behavior of rho(m,eq) varies for different events. In some cases, there is significant apparent refilling, whereas in other cases rho(m,eq) stays the same or even decreases slightly. Nevertheless, we showed that on average, rho(m,eq) increases exponentially during quiet intervals. There is variation of apparent refilling with respect to the phase of the solar cycle. On the third day of apparent refilling, rho(m,eq) has on average a similar value at solar maximum or solar minimum, but at solar maximum, rho(m,eq) begins with a larger value and rises relatively less than at solar minimum.
C1 [Denton, R. E.; Amoh, Justice, Jr.] Dartmouth Coll, Dept Phys & Astron, Hanover, NH 03755 USA.
[Denton, R. E.; Amoh, Justice, Jr.] Dartmouth Coll, Thayer Sch Engn, Hanover, NH 03755 USA.
[Takahashi, Kazue] Johns Hopkins Univ, Appl Phys Lab, Johns Hopkins Rd, Laurel, MD 20723 USA.
[Singer, H. J.] NOAA, Space Weather Predict Ctr, Boulder, CO USA.
RP Denton, RE (reprint author), Dartmouth Coll, Dept Phys & Astron, Hanover, NH 03755 USA.; Denton, RE (reprint author), Dartmouth Coll, Thayer Sch Engn, Hanover, NH 03755 USA.
EM richard.e.denton@dartmouth.edu
FU NSF [AGS-1105790, AGS-1106427]; NASA [NNX10AQ60G]
FX Work at Dartmouth was supported by NSF grant AGS-1105790 and NASA grant
NNX10AQ60G. Work at JHU APL was supported by NSF grant AGS-1106427.
Solar wind parameters and geomagnetic indices were obtained from the
GSFC/SPDF OMNIWeb interface at http://omniweb.gsfc.nasa.gov. The
Kondrashov et al. [2014] database was used to fill in missing values
during data gaps
(http://onlinelibrary.wiley.com/doi/10.1002/2014GL059741/full). Values
of F10.7 come originally from NOAA's National Geophysical
Data Center. Numerical data shown in this paper are available from the
lead author upon request.
NR 21
TC 1
Z9 1
U1 0
U2 0
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 APR
PY 2016
VL 121
IS 4
BP 2962
EP 2975
DI 10.1002/2015JA022167
PG 14
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA DR5RO
UT WOS:000379960300010
ER
PT J
AU Zabotin, NA
Godin, OA
Bullett, TW
AF Zabotin, Nikolay A.
Godin, Oleg A.
Bullett, Terence W.
TI Oceans are a major source of waves in the thermosphere
SO JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
LA English
DT Article
DE A link between waves in the ocean; and in the thermosphere has been;
revealed; Power levels of gravity waves in both; media are significantly
correlated; The ocean is an important source of; background
thermospheric waves
ID TIME DATA ACQUISITION; INFRAGRAVITY WAVES; DEEP-OCEAN; GRAVITY-WAVES;
INTERPRETATION CAPABILITIES; SPACED DATA; DYNASONDE
AB Recent theoretical analysis by Godin et al. (2015) led to the suggestion that infragravity waves (IGWs, i.e., surface gravity waves in the ocean with periods longer than 30 s) can radiate acoustic-gravity waves (AGWs) and account for a significant part of the wave activity observed in the thermosphere with periods between about 5min and 3 h. In this paper, we report a strong experimental demonstration of thermospheric waves being driven by the ocean using data from two Deep-ocean Assessment and Reporting of Tsunamis stations located off the US East Coast and Dynasonde radar system located at Wallops Island, Virginia. Over a 9month observation period, variations of IGW and AGW spectral amplitudes demonstrate large, statistically significant correlation in a broad range of frequencies (0.2-3.2mHz) and altitudes (140-190 km). Peak correlation values (similar to 0.43) indicate that waves radiated by the ocean represent a major constituent of thermospheric wave activity.
C1 [Zabotin, Nikolay A.] Univ Colorado Boulder, Dept Elect Comp & Energy Engn, Boulder, CO 80309 USA.
[Zabotin, Nikolay A.; Godin, Oleg A.; Bullett, Terence W.] Univ Colorado Boulder, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Godin, Oleg A.] NOAA, Earth Syst Res Lab, Boulder, CO USA.
[Bullett, Terence W.] NOAA, Natl Ctr Environm Informat, Boulder, CO USA.
RP Zabotin, NA (reprint author), Univ Colorado Boulder, Dept Elect Comp & Energy Engn, Boulder, CO 80309 USA.; Zabotin, NA (reprint author), Univ Colorado Boulder, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
EM nikolay.zabotin@colorado.edu
RI Godin, Oleg/E-6554-2011; Zabotin, Nikolay/A-9639-2015
OI Godin, Oleg/0000-0003-4599-2149; Zabotin, Nikolay/0000-0003-0715-1082
FU Office of Naval Research Basic Research Challenge program
[N000141310348]; National Science Foundation [CNS-0821794]
FX This work was supported by the Office of Naval Research Basic Research
Challenge program, award N000141310348. Field support of the Wallops
Dynasonde operation has been provided, in part, by the staff of the
NASA's Wallops Flight Facility. The Dynasonde data are accessible
through the project's website (http://surf.colorado.edu) upon request to
the authors (N.Z. or T.B.) as well as through NCEI's MIRRION server
(ftp://ftp.ngdc.noaa.gov/ionosonde/data/WI937/). The collection of DART
data was performed by NDBC as a part of their standard operations. The
authors are grateful to J.W. Wright for comments that led to substantial
improvements in presentation and to G. Mungov for help with accessing
and preprocessing of the DART data provided by NDBC. We thank L.
Zabotina for help with developing tools for graphical display and
handling the Dynasonde analysis results. This work utilized the
University of Colorado Boulder research computing facility, which is
supported by the National Science Foundation (award CNS-0821794).
NR 36
TC 3
Z9 3
U1 4
U2 7
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 APR
PY 2016
VL 121
IS 4
BP 3452
EP 3463
DI 10.1002/2016JA022357
PG 12
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA DR5RO
UT WOS:000379960300044
ER
PT J
AU Negrea, C
Zabotin, N
Bullett, T
Fuller-Rowell, T
Fang, TW
Codrescu, M
AF Negrea, Catalin
Zabotin, Nikolay
Bullett, Terrence
Fuller-Rowell, Tim
Fang, Tzu-Wei
Codrescu, Mihail
TI Characteristics of acoustic gravity waves obtained from Dynasonde data
SO JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
LA English
DT Article
DE Characteristics of acoustic gravity; waves at Wallops Island; Comparison
with theoretical; dispersion relation; Propagation characteristics of;
traveling ionospheric disturbances
ID ATMOSPHERE RADAR OBSERVATIONS; UNEVENLY SAMPLED-DATA; TIME-SERIES
ANALYSIS; SPACED DATA; SPECTRAL-ANALYSIS; DISSIPATION; MIDDLE
AB Traveling ionospheric disturbances (TIDs) are ubiquitous in the thermosphere-ionosphere and are often assumed to be caused by acoustic gravity waves (AGWs). This study performs an analysis of the TID and AGW activity above Wallops Island, VA, during October 2013. The variations in electron density and ionospheric tilts obtained with the Dynasonde technique are used as primary indicators of wave activity. The temporal and spectral characteristics of the data are discussed in detail, using also results of the Whole Atmosphere Model (WAM) and the Global Ionosphere Plasmasphere Model (GIP). The full set of propagation parameters (frequency, and the vertical, zonal and meridional wave vector components) of the TIDs is determined over the 160-220 km height range. A test of the self-consistency of these results within the confines of the theoretical AGW dispersion relation is devised. This is applied to a sample data set of 24 October 2013. A remarkable agreement has been achieved for wave periods between 52 and 21 min, for which we can rigorously claim the TIDs are caused by underlying acoustic gravity waves. The Wallops Island Dynasonde can operate for extended periods at a 2 min cadence, allowing determination of the statistical distributions of propagation parameters. A dominant population of TIDs is identified in the frequency band below 1 mHz, and for it, the distributions of the horizontal wavelengths, vertical wavelengths, and horizontal phase speeds are obtained.
C1 [Negrea, Catalin; Zabotin, Nikolay] Univ Colorado, Dept Elect Comp & Energy Engn, Boulder, CO 80309 USA.
[Negrea, Catalin; Zabotin, Nikolay; Bullett, Terrence; Fuller-Rowell, Tim; Fang, Tzu-Wei] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Negrea, Catalin; Fuller-Rowell, Tim; Fang, Tzu-Wei; Codrescu, Mihail] NOAA, Space Weather Predict Ctr, Boulder, CO 80305 USA.
[Negrea, Catalin] Inst Space Sci, Magurele, Romania.
[Bullett, Terrence] NOAA, Natl Ctr Environm Informat, Boulder, CO USA.
RP Negrea, C (reprint author), Univ Colorado, Dept Elect Comp & Energy Engn, Boulder, CO 80309 USA.; Negrea, C (reprint author), Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.; Negrea, C (reprint author), NOAA, Space Weather Predict Ctr, Boulder, CO 80305 USA.; Negrea, C (reprint author), Inst Space Sci, Magurele, Romania.
EM Catalin.Negrea@noaa.gov
RI Zabotin, Nikolay/A-9639-2015; Negrea, Catalin/A-4321-2017
OI Zabotin, Nikolay/0000-0003-0715-1082;
FU Office of Naval Research Basic Research Challenge program
[N000141310348]; National Science Foundation [CNS-0821794]
FX Authors thank O. A. Godin for stimulating discussions and helpful
comments. This work was supported by the Office of Naval Research Basic
Research Challenge program through award N000141310348. Field support of
Wallops Dynasonde operation has been provided, in part, by the staff of
the NASA's Wallops Flight Facility. The Dynasonde data are accessible
through the project's web site (http://surf.colorado.edu) upon request
to the author (N.Z. or T.B.) as well as through NGDC's MIRRION server
(ftp://ftp.ngdc.noaa.gov/ionosonde/data/WI937/). This work utilized the
University of Colorado Boulder research computing facility, which is
supported by the National Science Foundation (award number CNS-0821794).
NR 40
TC 0
Z9 0
U1 5
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 APR
PY 2016
VL 121
IS 4
BP 3665
EP 3680
DI 10.1002/2016JA022495
PG 16
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA DR5RO
UT WOS:000379960300059
ER
PT J
AU Harnos, DS
Nesbitt, SW
AF Harnos, Daniel S.
Nesbitt, Stephen W.
TI Varied pathways for simulated tropical cyclone rapid intensification.
PartI: Precipitation and environment
SO QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY
LA English
DT Article
DE tropical cyclone; hurricane; typhoon; rapid intensification; radius of
maximum wind; convective processes; mesoscale processes
ID HURRICANE EARL 2010; STRUCTURAL-CHANGES; CONVECTIVE BURSTS;
UNITED-STATES; WARM-CORE; EVOLUTION; SHEAR; MODEL; DISTRIBUTIONS; RADAR
AB Two 1-km Weather Research and Forecasting model simulations of the rapid intensification (RI) periods of hurricanes Ike(2008) and Earl(2010), under low and high wind shear respectively, are performed to evaluate mechanisms linked to the initiation and maintenance of RI. Despite similar simulated intensification time series, the exhibited hydrometeor characteristics differ between the two cases since Ike possesses less asymmetry and less vigorous convection than Earl. An objective method to quantitatively estimate the radius of maximum wind (RMW) with respect to height is introduced for quantifying the primary circulation character of each storm, permitting analysis of where heating is most efficient for driving warm core growth and subsequent intensification. Following eye development in each, diabatic heating remains embedded within the RMW. Earl's RI onset coincides with an absolute maximum in diabatic heating occurring within the RMW, while Ike possesses relatively less diabatic heating inside the RMW throughout and lacks an absolute peak associated with RI. The majority of diabatic heating within the RMW of both cases occurs at subfreezing temperatures, indicative of the importance of clouds associated with ice processes in these RI simulations. Earl's diabatic heating peak is tied to a maximum in convective burst activity residing within the RMW. Earl's preference for more sparse but intense convection is associated with increased sea surface temperatures, surface heat fluxes, moisture convergence, and near-surface equivalent potential temperature relative to the broader, weaker convective character in Ike.
C1 [Harnos, Daniel S.] NOAA NWS NCEP, Climate Predict Ctr, College Pk, MD USA.
[Nesbitt, Stephen W.] Univ Illinois, Dept Atmospher Sci, Urbana, IL USA.
RP Harnos, DS (reprint author), NCWCP, Climate Predict Ctr, 5830 Univ Res Court,Room 3040, College Pk, MD 20740 USA.
EM daniel.harnos@noaa.gov
FU NASA Hurricane Science Research Project [NNX09AB82G]; NASA ESS
Fellowship [NNX10AP50H]
FX The authors thank Zhuo Wang, Greg McFarquhar, Ryan Sriver, and Brian
Jewett for discussions in developing this research. Constructive reviews
from Dr Robert Rogers and another anonymous reviewer are appreciated for
further refining the manuscript. DH and SN were supported by Ramesh
Kakar under NASA Hurricane Science Research Project grant NNX09AB82G; DH
was supported by NASA ESS Fellowship NNX10AP50H. Computing resources
were provided by the NASA Center for Climate Simulation. ERA-Interim and
MERRA reanalyses were provided by ECMWF and NASA respectively.
NR 55
TC 1
Z9 1
U1 9
U2 10
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0035-9009
EI 1477-870X
J9 Q J ROY METEOR SOC
JI Q. J. R. Meteorol. Soc.
PD APR
PY 2016
VL 142
IS 697
BP 1816
EP 1831
DI 10.1002/qj.2780
PN B
PG 16
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DP3LR
UT WOS:000378395500021
ER
PT J
AU Harnos, DS
Nesbitt, SW
AF Harnos, Daniel S.
Nesbitt, Stephen W.
TI Varied pathways for simulated tropical cyclone rapid intensification.
PartII: Vertical motion and cloud populations
SO QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY
LA English
DT Article
DE tropical cyclone; hurricane; typhoon; rapid intensification; convective
processes; mesoscale processes; precipitation; vertical motion
ID HIGH-RESOLUTION SIMULATION; HURRICANE EARL 2010; WIND SHEAR; CONVECTIVE
BURSTS; STORM STRUCTURE; HOT TOWERS; INTENSITY; RADAR; EVOLUTION; TRMM
AB Differences in the vertical velocity characteristics associated with various cloud populations are evaluated for two simulated cases of tropical cyclone (TC) rapid intensification (RI) under varying wind shear. Within the radius of maximum wind (RMW), preceding RI in the low-shear TC (hurricane Ike of 2008) increased updraught magnitudes for the top 1% of the distribution at 7km occur, while in the high-shear scenario (hurricane Earl of 2010) RI is led by increased updraught magnitudes of the top 1% of the distribution at 12km. Three-dimensional analyses of individual updraughts relative to their peak altitude enables direct quantification of processes associated with shallow cumuli, cumulus congestus, deep convection failing to penetrate the tropopause, and convective bursts (CBs). Mean profiles for each convective regime reveal positive contributions in certain variables of each updraught variety towards RI with positive diabatic heating, absolute vorticity, and moisture convergence roles. Within the RMW, CBs are shown to be the primary diabatic heating and vertical mass and vapour flux contributors in both simulations, while Ike includes secondary contributions from deep convection and congestus in addition to noteworthy diabatic heating from apparent stratiform processes that act to spin up the mid-level vortex. Inner-core moisture convergence has divided contributions from shallow cumuli, cumulus congestus, and CBs. CBs act to enhance potential vorticity to the greatest amount and over the deepest vertical layer at low levels. The simulation results overwhelmingly support the aggregate importance of vertically developed deep convection and its associated ice processes to the initiation and maintenance of RI.
C1 [Harnos, Daniel S.] NOAA NWS NCEP, Climate Predict Ctr, College Pk, MD USA.
[Nesbitt, Stephen W.] Univ Illinois, Dept Atmospher Sci, Urbana, IL USA.
RP Harnos, DS (reprint author), NCWCP, Climate Predict Ctr, 5830 Univ Res Court,Room 3040, College Pk, MD 20740 USA.
EM daniel.harnos@noaa.gov
FU NASA Hurricane Science Research Project [NNX09AB82G]; NASA ESS
Fellowship [NNX10AP50H]
FX The authors thank Zhuo Wang, Greg McFarquhar, Ryan Sriver, and Brian
Jewett for discussions that improved the quality of this work.
Constructive reviews from Robert Rogers and another anonymous reviewer
are appreciated for further improving this project. DH and SN were
supported by Ramesh Kakar under NASA Hurricane Science Research Project
grant NNX09AB82G; DH was supported by NASA ESS Fellowship NNX10AP50H.
Computing resources were provided by the NASA Center for Climate
Simulation.
NR 58
TC 1
Z9 1
U1 5
U2 7
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0035-9009
EI 1477-870X
J9 Q J ROY METEOR SOC
JI Q. J. R. Meteorol. Soc.
PD APR
PY 2016
VL 142
IS 697
BP 1832
EP 1846
DI 10.1002/qj.2778
PN B
PG 15
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DP3LR
UT WOS:000378395500022
ER
PT J
AU Kuchler, N
Turner, DD
Lohnert, U
Crewell, S
AF Kuechler, N.
Turner, D. D.
Loehnert, U.
Crewell, S.
TI Calibrating ground-based microwave radiometers: Uncertainty and drifts
SO RADIO SCIENCE
LA English
DT Article
ID LIQUID-NITROGEN; WATER-VAPOR; PROFILES; ACCURACY; TEMPERATURE; LOADS
AB The quality of microwave radiometer (MWR) calibrations, including both the absolute radiometric accuracy and the spectral consistency, determines the accuracy of geophysical retrievals. The Microwave Radiometer Calibration Experiment (MiRaCalE) was conducted to evaluate the performance of MWR calibration techniques, especially of the so-called Tipping Curve Calibrations (TCC) and Liquid Nitrogen Calibrations (LN2cal), by repeatedly calibrating a fourth-generation Humidity and Temperature Profiler (HATPRO-G4) that measures downwelling radiance between 20 GHz and 60 GHz. MiRaCalE revealed two major points to improve MWR calibrations: (i) the necessary repetition frequency for MWR calibration techniques to correct drifts, which ensures stable long-term measurements; and (ii) the spectral consistency of control measurements of a well known reference is useful to estimate calibration accuracy. Besides, we determined the accuracy of the HATPRO's liquid nitrogen-cooled blackbody's temperature. TCCs and LN2cals were found to agree within 0.5 K when observing the liquid nitrogen-cooled blackbody with a physical temperature of 77 K. This agreement of two different calibration techniques suggests that the brightness temperature of the LN2 cooled blackbody is accurate within at least 0.5 K, which is a significant reduction of the uncertainties that have been assumed to vary between 0.6 K and 1.5 K when calibrating the HATPRO-G4. The error propagation of both techniques was found to behave almost linearly, leading to maximum uncertainties of 0.7 K when observing a scene that is associated with a brightness temperature of 15 K.
C1 [Kuechler, N.; Loehnert, U.; Crewell, S.] Univ Cologne, Inst Geophys & Meteorol, D-50931 Cologne, Germany.
[Turner, D. D.] NOAA, Natl Severe Storms Lab, Forecast Res & Dev Div, Norman, OK 73069 USA.
RP Kuchler, N (reprint author), Univ Cologne, Inst Geophys & Meteorol, D-50931 Cologne, Germany.
EM nkuech@meteo.uni-koeln.de
RI Lohnert, Ulrich/C-3303-2013; Crewell, Susanne/O-1640-2013
OI Lohnert, Ulrich/0000-0002-9023-0269; Crewell,
Susanne/0000-0003-1251-5805
FU U.S. Department of Energy [DE-SC0008830]
FX MiRaCalE was hosted by the National Severe Storms Laboratory and the
School of Meteorology of the University of Oklahoma in cooperation of
the University of Cologne. Radio sounding data from the Southern Great
Plains was provided by the ARM research facility. We would like to thank
Rainer Haseneder-Lind, Doug Kennedy, and Birger Bohn for their
assistance in the field. We would like to thank also Radiometer Physics
GmbH for technical support. Comments from three anonymous reviewers were
greatly appreciated and improved the quality of this paper. This work
was supported in part by grant DE-SC0008830 from the U.S. Department of
Energy as part of the Atmospheric System Research program. The data used
are not available on the Internet, but free access is possible
contacting nkuech@meteo.uni-koeln.de.
NR 32
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U1 2
U2 8
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0048-6604
EI 1944-799X
J9 RADIO SCI
JI Radio Sci.
PD APR
PY 2016
VL 51
IS 4
BP 311
EP 327
DI 10.1002/2015RS005826
PG 17
WC Astronomy & Astrophysics; Geochemistry & Geophysics; Meteorology &
Atmospheric Sciences; Remote Sensing; Telecommunications
SC Astronomy & Astrophysics; Geochemistry & Geophysics; Meteorology &
Atmospheric Sciences; Remote Sensing; Telecommunications
GA DP0IL
UT WOS:000378173300006
ER
PT J
AU Davis, TW
Gobler, CJ
AF Davis, Timothy W.
Gobler, Christopher J.
TI Preface for Special Issue on "Global expansion of harmful cyanobacterial
blooms: Diversity, ecology, causes, and controls"
SO HARMFUL ALGAE
LA English
DT Editorial Material
ID LAKE-ERIE; EUTROPHICATION; CLIMATE
C1 [Davis, Timothy W.] NOAA, Great Lakes Environm Res Lab, 4840 South State Rd, Ann Arbor, MI 48108 USA.
[Gobler, Christopher J.] SUNY Stony Brook, Sch Marine & Atmospher Sci, 239 Montauk Hwy, Southampton, NY 11968 USA.
RP Gobler, CJ (reprint author), SUNY Stony Brook, Sch Marine & Atmospher Sci, 239 Montauk Hwy, Southampton, NY 11968 USA.
EM christopher.gobler@stonybrook.edu
NR 23
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U1 2
U2 4
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1568-9883
EI 1878-1470
J9 HARMFUL ALGAE
JI Harmful Algae
PD APR
PY 2016
VL 54
SI SI
BP 1
EP 3
DI 10.1016/j.hal.2016.02.003
PG 3
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA DN8HK
UT WOS:000377319600001
PM 28073470
ER
PT J
AU Gobler, CJ
Burkholder, JM
Davis, TW
Harke, MJ
Johengen, T
Stow, CA
Van de Waal, DB
AF Gobler, Christopher J.
Burkholder, JoAnn M.
Davis, Timothy W.
Harke, Matthew J.
Johengen, Tom
Stow, Craig A.
Van de Waal, Dedmer B.
TI The dual role of nitrogen supply in controlling the growth and toxicity
of cyanobacterial blooms
SO HARMFUL ALGAE
LA English
DT Review
DE Nitrogen; Phosphorus; Cyanobacteria; Microcystis; Diazotrophy; Nutrients
ID WESTERN LAKE-ERIE; ALKALINE-PHOSPHATASE ACTIVITY; MICROCYSTIS-AERUGINOSA
CULTURES; HARMFUL ALGAL BLOOMS; FRESH-WATER LAKES; BLUE-GREEN-ALGAE;
PHOSPHORUS LIMITATION; CYLINDROSPERMOPSIS-RACIBORSKII; ORGANIC
PHOSPHORUS; SHALLOW LAKES
AB Historically, phosphorus (P) has been considered the primary limiting nutrient for phytoplankton assemblages in freshwater ecosystems. This review, supported by new findings from Lake Erie, highlights recent molecular, laboratory, and field evidence that the growth and toxicity of some non-diazotrophic blooms of cyanobacteria can be controlled by nitrogen (N). Cyanobacteria such as Microcystis possess physiological adaptations that allow them to dominate low-P surface waters, and in temperate lakes, cyanobacterial densities can be controlled by N availability. Beyond total cyanobacterial biomass, N loading has been shown to selectively promote the abundance of Microcystis and Planktothrix strains capable of synthesizing microcystins over strains that do not possess this ability. Among strains of cyanobacteria capable of synthesizing the N-rich microcystins, cellular toxin quotas have been found to depend upon exogenous N supplies. Herein, multi-year observations from western Lake Erie are presented demonstrating that microcystin concentrations peak in parallel with inorganic N, but not orthophosphate, concentrations and are significantly lower (p < 0.01) during years of reduced inorganic nitrogen loading and concentrations. Collectively, this information underscores the importance of N as well as P in controlling toxic cyanobacteria blooms. Furthermore, it supports the premise that management actions to reduce P in the absence of concurrent restrictions on N loading may not effectively control the growth and/or toxicity of non-diazotrophic toxic cyanobacteria such as the cosmopolitan, toxin-producing genus, Microcystis. (C) 2016 Elsevier B.V. All rights reserved.
C1 SUNY Stony Brook, Sch Marine & Atmospher Sci, Stony Brook, NY 11968 USA.
N Carolina State Univ, Ctr Appl Aquat Ecol, Raleigh, NC 27606 USA.
NOAA, Great Lakes Environm Res Lab, Ann Arbor, MI 48108 USA.
Univ Michigan, Cooperat Inst Limnol & Ecosyst Res, Ann Arbor, MI 48109 USA.
Netherlands Inst Ecol NIOO KNAW, Dept Aquat Ecol, POB 50, NL-6700 AB Wageningen, Netherlands.
EM christopher.gobler@stonybrook.edu
RI Van de Waal, Dedmer/B-8002-2012;
OI Van de Waal, Dedmer/0000-0001-8803-1247; KNAW,
NIOO-KNAW/0000-0002-3835-159X
FU Chicago Community Fund grant NOAA-ECOHAB program - National Oceanic and
Atmospheric Center for Sponsored Coastal Ocean Research [NA10NOS4780140]
FX This work was supported by a Chicago Community Fund grant NOAA-ECOHAB
program being funded by the National Oceanic and Atmospheric Center for
Sponsored Coastal Ocean Research under award no. NA10NOS4780140 to
C.J.G. This is GLERL contribution number 1809 and ECOHAB contribution
number 844.[SS]
NR 157
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PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1568-9883
EI 1878-1470
J9 HARMFUL ALGAE
JI Harmful Algae
PD APR
PY 2016
VL 54
SI SI
BP 87
EP 97
DI 10.1016/j.hal.2016.01.010
PG 11
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA DN8HK
UT WOS:000377319600007
PM 28073483
ER
PT J
AU Visser, PM
Verspagen, JMH
Sandrini, G
Stal, LJ
Matthijs, HCP
Davis, TW
Paerl, HW
Huisman, J
AF Visser, Petra M.
Verspagen, Jolanda M. H.
Sandrini, Giovanni
Stal, Lucas J.
Matthijs, Hans C. P.
Davis, Timothy W.
Paerl, Hans W.
Huisman, Jef
TI How rising CO2 and global warming may stimulate harmful cyanobacterial
blooms
SO HARMFUL ALGAE
LA English
DT Review
DE Climate change; Cyanobacteria; Harmful algal blooms; Lakes; Rising CO2;
Temperature
ID CARBON-DIOXIDE SUPERSATURATION; APHANIZOMENON-OVALISPORUM NOSTOCALES;
MICROCYSTIS-AERUGINOSA KUTZ; SYNECHOCOCCUS SP PCC7942; INORGANIC CARBON;
CLIMATE-CHANGE; ELEVATED CO2; CONCENTRATING MECHANISM;
NITROGEN-FIXATION; N-2 FIXATION
AB Climate change is likely to stimulate the development of harmful cyanobacterial blooms in eutrophic waters, with negative consequences for water quality of many lakes, reservoirs and brackish ecosystems across the globe. In addition to effects of temperature and eutrophication, recent research has shed new light on the possible implications of rising atmospheric CO2 concentrations. Depletion of dissolved CO2 by dense cyanobacterial blooms creates a concentration gradient across the air-water interface. A steeper gradient at elevated atmospheric CO2 concentrations will lead to a greater influx of CO2, which can be intercepted by surface-dwelling blooms, thus intensifying cyanobacterial blooms in eutrophic waters. Bloom-forming cyanobacteria display an unexpected diversity in CO2 responses, because different strains combine their uptake systems for CO2 and bicarbonate in different ways. The genetic composition of cyanobacterial blooms may therefore shift. In particular, strains with high-flux carbon uptake systems may benefit from the anticipated rise in inorganic carbon availability. Increasing temperatures also stimulate cyanobacterial growth. Many bloom-forming cyanobacteria and also green algae have temperature optima above 25 degrees C, often exceeding the temperature optima of diatoms and dinoflagellates. Analysis of published data suggests that the temperature dependence of the growth rate of cyanobacteria exceeds that of green algae. Indirect effects of elevated temperature, like an earlier onset and longer duration of thermal stratification, may also shift the competitive balance in favor of buoyant cyanobacteria while eukaryotic algae are impaired by higher sedimentation losses. Furthermore, cyanobacteria differ from eukaryotic algae in that they can fix dinitrogen, and new insights show that the nitrogen-fixation activity of heterocystous cyanobacteria can be strongly stimulated at elevated temperatures. Models and lake studies indicate that the response of cyanobacterial growth to rising CO2 concentrations and elevated temperatures can be suppressed by nutrient limitation. The greatest response of cyanobacterial blooms to climate change is therefore expected to occur in eutrophic and hypertrophic lakes. (C) 2015 Elsevier B.V. All rights reserved.
C1 [Visser, Petra M.; Verspagen, Jolanda M. H.; Sandrini, Giovanni; Stal, Lucas J.; Matthijs, Hans C. P.; Huisman, Jef] Univ Amsterdam, Dept Aquat Microbiol, Inst Biodivers & Ecosyst Dynam, POB 94248, NL-1090 GE Amsterdam, Netherlands.
[Stal, Lucas J.] Royal Netherlands Inst Sea Res NIOZ, Dept Marine Microbiol, POB 140, NL-4400 AC Yerseke, Netherlands.
[Davis, Timothy W.] NOAA, Great Lakes Environm Res Lab, Ann Arbor, MI 48108 USA.
[Paerl, Hans W.] Univ North Carolina Chapel Hill, Inst Marine Sci, 3431 Arendell St, Morehead City, NC 28557 USA.
RP Visser, PM (reprint author), Univ Amsterdam, Dept Aquat Microbiol, Inst Biodivers & Ecosyst Dynam, POB 94248, NL-1090 GE Amsterdam, Netherlands.
EM P.M.Visser@uva.nl
FU Amsterdam Water Science program of the Amsterdam Academic Alliance;
Division of Earth and Life Sciences (ALW) of the Netherlands
Organization for Scientific Research (NWO); US National Science
Foundation [CBET 0826819, 1230543]; Dimensions of Biodiversity [1240851]
FX We thank the two reviewers for their constructive comments. J.M.H.
Verspagen was supported by the Amsterdam Water Science program of the
Amsterdam Academic Alliance; G. Sandrini was supported by the Division
of Earth and Life Sciences (ALW) of the Netherlands Organization for
Scientific Research (NWO); H.W. Paerl was supported by US National
Science Foundation Grants CBET 0826819, 1230543, and Dimensions of
Biodiversity (1240851). We acknowledge the COST Action ES 1105
'CYANO-COST-Cyanobacterial blooms and toxins in water resources:
Occurrence, impacts and management' for the opportunity to exchange
ideas with co-authors and other scientists. This manuscript is
NOAA-GLERL publication number 1802. [SS]
NR 171
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PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1568-9883
EI 1878-1470
J9 HARMFUL ALGAE
JI Harmful Algae
PD APR
PY 2016
VL 54
SI SI
BP 145
EP 159
DI 10.1016/j.hal.2015.12.006
PG 15
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA DN8HK
UT WOS:000377319600011
PM 28073473
ER
PT J
AU Stumpf, RP
Davis, TW
Wynne, TT
Graham, JL
Loftin, KA
Johengen, TH
Gossiaux, D
Palladino, D
Burtner, A
AF Stumpf, Richard P.
Davis, Timothy W.
Wynne, Timothy T.
Graham, Jennifer L.
Loftin, Keith A.
Johengen, Thomas H.
Gossiaux, Duane
Palladino, Danna
Burtner, Ashley
TI Challenges for mapping cyanotoxin patterns from remote sensing of
cyanobacteria
SO HARMFUL ALGAE
LA English
DT Review
DE Microcystins; Satellite; MERIS; Chlorophyll; Phycocyanin
ID LAURENTIAN GREAT-LAKES; CHLOROPHYLL-A; MICROCYSTIS-AERUGINOSA; COASTAL
WATERS; INLAND WATERS; TIME-SERIES; SATELLITE-OBSERVATIONS; IMAGING
SPECTROMETER; MERIS OBSERVATIONS; NONTOXIC STRAINS
AB Using satellite imagery to quantify the spatial patterns of cyanobacterial toxins has several challenges. These challenges include the need for surrogate pigments - since cyanotoxins cannot be directly detected by remote sensing, the-variability in the relationship between the pigments and cyanotoxins especially microcystins (MC), and the lack of standardization of the various measurement methods. A dual-model strategy can provide an approach to address these challenges. One model uses either chlorophyll-a (Chl-a) or phycocyanin (PC) collected in situ as a surrogate to estimate the MC concentration. The other uses a remote sensing algorithm to estimate the concentration of the surrogate pigment. Where blooms are mixtures of cyanobacteria and eukaryotic algae, PC should be the preferred surrogate to Chl-a. Where cyanobacteria dominate, Chl-a is a better surrogate than PC for remote sensing. Phycocyanin is less sensitive to detection by optical remote sensing, it is less frequently measured, PC laboratory methods are still not standardized, and PC has greater intracellular variability. Either pigment should not be presumed to have a fixed relationship with MC for any water body. The MC pigment relationship can be valid over weeks, but have considerable intra- and inter-annual variability due to changes in the amount of MC produced relative to cyanobacterial biomass. To detect pigments by satellite, three classes of algorithms (analytic, semi-analytic, and derivative) have been used. Analytical and semi-analytical algorithms are more sensitive but less robust than derivatives because they depend on accurate atmospheric correction; as a result derivatives are more commonly used. Derivatives can estimate Chl-a concentration, and research suggests they can detect and possibly quantify PC. Derivative algorithms, however, need to be standardized in order to evaluate the reproducibility of parameterizations between lakes. A strategy for producing useful estimates of microcystins from cyanobacterial biomass is described, provided cyanotoxin variability is addressed. Published by Elsevier B.V.
C1 [Stumpf, Richard P.; Wynne, Timothy T.] NOAA, Natl Ctr Coastal Ocean Sci, Silver Spring, MD 20910 USA.
[Davis, Timothy W.; Gossiaux, Duane] NOAA, Great Lakes Environm Res Lab, 2205 Commonwealth Blvd, Ann Arbor, MI 48105 USA.
[Graham, Jennifer L.; Loftin, Keith A.] US Geol Survey, Kansas Water Sci Ctr, Lawrence, KS USA.
[Johengen, Thomas H.; Palladino, Danna; Burtner, Ashley] CILER, Ann Arbor, MI USA.
RP Stumpf, RP (reprint author), NOAA, Natl Ctr Coastal Ocean Sci, Silver Spring, MD 20910 USA.
EM richard.stumpf@noaa.gov
FU NASA [NNH08ZDA001N, NNH09AL53I, 14-SMDUNSOL14-0001]; U.S. Geological
Survey's Toxic Substances Hydrology Program; Environmental Protection
Agency's Great Lake Research Initiative
FX This work was partially funded by the NASA Public Health and Water
Quality Program (NNH08ZDA001N) under contract NNH09AL53I, the NASA Ocean
Biology and Biochemistry Programs under proposal 14-SMDUNSOL14-0001, the
U.S. Geological Survey's Toxic Substances Hydrology Program, and the
Environmental Protection Agency's Great Lake Research Initiative. This
is NOAA GLERL publication number 1804. Steve Ruberg and the captains and
crew of NOAA GLERL's research vessels provided invaluable support. Any
use of trade, product, or firm names is for descriptive purposes only
and does not imply endorsement by the U.S. Government. The paper
benefitted from the insightful comments of the reviewers.
NR 104
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PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1568-9883
EI 1878-1470
J9 HARMFUL ALGAE
JI Harmful Algae
PD APR
PY 2016
VL 54
SI SI
BP 160
EP 173
DI 10.1016/j.hal.2016.01.005
PG 14
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA DN8HK
UT WOS:000377319600012
PM 28073474
ER
PT J
AU Bullerjahn, GS
Mckay, RM
Davis, TW
Baker, DB
Boyer, GL
D'Anglada, LV
Doucette, GJ
Ho, JC
Irwin, EG
Kling, CL
Kudela, RM
Kurmayer, R
Michalak, AM
Ortiz, JD
Otten, TG
Paerl, HW
Qin, BQ
Sohngen, BL
Stumpf, RP
Visser, PM
Wilhelm, SW
AF Bullerjahn, George S.
McKay, Robert M.
Davis, Timothy W.
Baker, David B.
Boyer, Gregory L.
D'Anglada, Lesley V.
Doucette, Gregory J.
Ho, Jeff C.
Irwin, Elena G.
Kling, Catherine L.
Kudela, Raphael M.
Kurmayer, Rainer
Michalak, Anna M.
Ortiz, Joseph D.
Otten, Timothy G.
Paerl, Hans W.
Qin, Boqiang
Sohngen, Brent L.
Stumpf, Richard P.
Visser, Petra M.
Wilhelm, Steven W.
TI Global solutions to regional problems: Collecting global expertise to
address the problem of harmful cyanobacterial blooms. A Lake Erie case
study
SO HARMFUL ALGAE
LA English
DT Review
DE Cyanobacteria; CHAB; Lake Erie; Microcystin; Phosphorus; Nitrogen
ID CO2 CONCENTRATING MECHANISMS; WATER-QUALITY; TOXIC CYANOBACTERIA; ALGAL
BLOOMS; AGRICULTURAL PHOSPHORUS; RE-EUTROPHICATION; CLIMATE-CHANGE;
SHALLOW LAKES; MAUMEE RIVER; GREAT-LAKES
AB In early August 2014, the municipality of Toledo, OH (USA) issued a 'do not drink' advisory on their water supply directly affecting over 400,000 residential customers and hundreds of businesses (Wilson, 2014). This order was attributable to levels of microcystin, a potent liver toxin, which rose to 2.5 mu g L-1 in finished drinking water. The Toledo crisis afforded an opportunity to bring together scientists from around the world to share ideas regarding factors that contribute to bloom formation and toxigenicity, bloom and toxin detection as well as prevention and remediation of bloom events. These discussions took place at an NSF- and NOAA-sponsored workshop at Bowling Green State University on April 13 and 14, 2015. In all, more than 100 attendees from six countries and 15 US states gathered together to share their perspectives. The purpose of this review is to present the consensus summary of these issues that emerged from discussions at the Workshop. As additional reports in this special issue provide detailed reviews on many major CHAB species, this paper focuses on the general themes common to all blooms, such as bloom detection, modeling, nutrient loading, and strategies to reduce nutrients. (C) 2016 Elsevier B.V. All rights reserved.
C1 [Bullerjahn, George S.; McKay, Robert M.] Bowling Green State Univ, Dept Biol Sci, Life Sci Bldg, Bowling Green, OH 43403 USA.
[Davis, Timothy W.] NOAA, GLERL, 4840 South State Rd, Ann Arbor, MI 48108 USA.
[Baker, David B.] Heidelberg Univ, Natl Ctr Water Qual Res, Tiffin, OH 44883 USA.
[Boyer, Gregory L.] SUNY Coll Environm Sci & Forestry, Dept Chem, 1 Forestry Dr, Syracuse, NY 13210 USA.
[D'Anglada, Lesley V.] US EPA, Agcy Off Sci & Technol, 1200 Penn Ave NW, Washington, DC 20460 USA.
[Doucette, Gregory J.] NOAA, Natl Ocean Serv, 219 Ft Johnson Rd, Charleston, SC 29412 USA.
[Ho, Jeff C.] Stanford Univ, Dept Civil & Environm Engn, 473 Via Ortega, Stanford, CA 94305 USA.
[Ho, Jeff C.; Michalak, Anna M.] Carnegie Inst Sci, Dept Global Ecol, 260 Panama St, Stanford, CA 94305 USA.
[Irwin, Elena G.; Sohngen, Brent L.] Ohio State Univ, Dept Agr Environm & Dev Econ, 2120 Fyffe Rd, Columbus, OH 43210 USA.
[Kling, Catherine L.] Iowa State Univ Sci & Technol, Dept Econ, 578 Heady Hall, Ames, IA 50011 USA.
[Kudela, Raphael M.] Univ Calif Santa Cruz, Ocean Sci, 1156 High St, Santa Cruz, CA 95064 USA.
[Kurmayer, Rainer] Univ Innsbruck, Res Inst Limnol, Mondseestr 9, A-5310 Mondsee, Austria.
[Ortiz, Joseph D.] Kent State Univ, Dept Geol, 336 McGilvrey Hall, Kent, OH 44242 USA.
[Otten, Timothy G.] Oregon State Univ, Dept Microbiol, 226 Nash Hall, Corvallis, OR 97331 USA.
[Paerl, Hans W.] Univ N Carolina, Inst Marine Sci, 3431 Arendell St, Morehead City, NC 28557 USA.
[Qin, Boqiang] Nanjing Inst Geog & Limnol, 73 East Beijing Rd, Nanjing 210008, Peoples R China.
[Stumpf, Richard P.] NOAA, Natl Ctr Coastal Ocean Sci, 1305 East West Highway Code N SCI1, Silver Spring, MD 20910 USA.
[Visser, Petra M.] Univ Amsterdam, Inst Biodivers & Ecosyst Dynam, Dept Aquat Microbiol, POB 94248, NL-1090 GE Amsterdam, Netherlands.
[Wilhelm, Steven W.] Univ Tennessee, Dept Microbiol, 1414 West Cumberland Ave, Knoxville, TN 37996 USA.
RP Bullerjahn, GS (reprint author), Bowling Green State Univ, Dept Biol Sci, Life Sci Bldg, Bowling Green, OH 43403 USA.
EM bullerj@bgsu.edu
RI Wilhelm, Steven/B-8963-2008
OI Wilhelm, Steven/0000-0001-6283-8077
FU National Science Foundation [CBET-1515671]; NOAA Great Lakes
Environmental Research Laboratory; University of Michigan Water Center;
Office of the Vice President for Research AMP; Economic Development at
Bowling Green State University; Ohio Department of Education
[R/HAB-2-BOR]
FX The CHAB Workshop was supported by the National Science Foundation under
grant no. CBET-1515671 (GSB). Additional support was provided by the
NOAA Great Lakes Environmental Research Laboratory, the University of
Michigan Water Center and by the Office of the Vice President for
Research & Economic Development at Bowling Green State University.
Additional research support was provided by Ohio Department of Education
grant R/HAB-2-BOR to GSB, RMM and JDO. GSB, RMM and SWW thank Mr. Jason
Isakovic (Senior Legislative Assistant, office of US Rep. Robert Latta)
for helpful discussions on the legislative process. The authors also
thank the many staff and students at BGSU who provided assistance prior
and during the Workshop.[SS]
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PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 1568-9883
EI 1878-1470
J9 HARMFUL ALGAE
JI Harmful Algae
PD APR
PY 2016
VL 54
SI SI
BP 223
EP 238
DI 10.1016/j.hal.2016.01.003
PG 16
WC Marine & Freshwater Biology
SC Marine & Freshwater Biology
GA DN8HK
UT WOS:000377319600016
PM 28073479
ER
PT J
AU Ohlberger, J
Scheuerell, MD
Schindler, DE
AF Ohlberger, Jan
Scheuerell, Mark D.
Schindler, Daniel E.
TI Population coherence and environmental impacts across spatial scales: a
case study of Chinook salmon
SO ECOSPHERE
LA English
DT Article
DE coherence; environment; multivariate analysis; productivity dynamics;
spatial scale
ID NORTH PACIFIC-OCEAN; DYNAMIC FACTOR-ANALYSIS; SOCKEYE-SALMON; SURVIVAL
RATES; ONCORHYNCHUS SPP.; CLIMATE-CHANGE; TIME-SERIES; PINK SALMON;
COMMON TRENDS; ABUNDANCE
AB A central problem in understanding how species respond to global change is in parsing the effects of local drivers of population dynamics from regional and global drivers that are shared among populations. Management and conservation efforts that typically focus on a particular population would benefit greatly from being able to separate the effects of environmental processes at local, regional, and global scales. One way of addressing this challenge is to integrate data across multiple populations and use multivariate time series approaches to estimate shared and independent components of dynamics among neighboring populations. Here, we use a data set of 15 populations of Chinook salmon (Oncorhynchus tshawytscha) covering a broad geographical range in the eastern North Pacific Ocean to show how Dynamic Factor Analysis (DFA) can be used to estimate temporal coherence in population dynamics and to detect environmental drivers across spatial scales. Our results show that productivity dynamics of Chinook salmon populations strongly covary at the regional scale, but to a lesser degree at larger spatial scales. The timing of river ice break-up in spring was identified as an important driver of regional productivity dynamics. In addition, broad-scale variability in population productivity was linked to the North Pacific Gyre Oscillation, a dominant pattern of sea surface height variability. These broad-scale patterns in productivity dynamics may be associated with recent regime shifts in the Northeast Pacific Ocean. However, our results also demonstrate that populations within regions do not always respond consistently to the same environmental drivers, thus suggesting location-specific impacts. Overall, this study illustrates the use of DFA for quantifying the spatial and temporal complexity of multiple population responses to environmental change, thereby providing insights to processes that affect populations across large geographic areas, but that might be filtered by local habitat conditions.
C1 [Ohlberger, Jan; Schindler, Daniel E.] Univ Washington, Sch Aquat & Fishery Sci, Seattle, WA 98195 USA.
[Scheuerell, Mark D.] NOAA, Fish Ecol Div, Northwest Fisheries Sci Ctr, Natl Marine Fisheries Serv, Seattle, WA 98112 USA.
RP Ohlberger, J (reprint author), Univ Washington, Sch Aquat & Fishery Sci, Seattle, WA 98195 USA.
EM janohl@uw.edu
RI Scheuerell, Mark/N-6683-2016;
OI Scheuerell, Mark/0000-0002-8284-1254; Ohlberger, Jan/0000-0001-6795-240X
FU Arctic-Yukon-Kuskokwim Sustainable Salmon Initiative
FX We thank S. Fleischman and M. Catalano for providing run reconstructions
of spawning escapement and recruitment for the populations used in this
analysis. We also thank K. Myers and M. Bradford who provided additional
time series data on environmental indicators, and M. Stachura for
helpful discussions. Input from S. Fleischman, R. Clark, E. Volk, and J.
Linderman from the Alaska Department of Fish and Game was invaluable to
this project. This work was funded by the Arctic-Yukon-Kuskokwim
Sustainable Salmon Initiative, and we thank J. Spaeder for his insights
on this effort.
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U1 8
U2 15
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 2150-8925
J9 ECOSPHERE
JI Ecosphere
PD APR
PY 2016
VL 7
IS 4
AR e01333
DI 10.1002/ecs2.1333
PG 14
WC Ecology
SC Environmental Sciences & Ecology
GA DN6VA
UT WOS:000377213400016
ER
PT J
AU Ruzicka, JJ
Daly, EA
Brodeur, RD
AF Ruzicka, James J.
Daly, Elizabeth A.
Brodeur, Richard D.
TI Evidence that summer jellyfish blooms impact Pacific Northwest salmon
production
SO ECOSPHERE
LA English
DT Article
DE Chinook salmon; Chrysaora fuscescens; coho salmon; Columbia River;
competition; ecosystem model; food web; jellyfish; Northern California
Current; Oncorhynchus kisutch; Oncorhynchus tshawytscha; sea nettles
ID NORTHERN CALIFORNIA CURRENT; JUVENILE COHO SALMON; EARLY MARINE
RESIDENCE; SPRING CHINOOK SALMON; ONCORHYNCHUS-KISUTCH; SURFACE WATERS;
OCEANOGRAPHIC CONDITIONS; CHRYSAORA-FUSCESCENS; CURRENT ECOSYSTEM;
SPATIAL OVERLAP
AB Interannual variability in salmon (Oncorhynchus spp.) production in the northeast Pacific is understood to be driven by oceanographic variability and bottom-up processes affecting prey availability to juvenile salmon. Scyphozoan jellyfish have an important role in shaping the pathways of energy flow through pelagic food webs. While jellyfish obtain high production rates and biomasses as major consumers of zooplankton production, they have few predators and may divert plankton production away from higher trophic levels. Although jellyfish are planktivorous and juvenile coho (O. kisutch) and Chinook (O. tshawytscha) salmon are mainly piscivorous, they may be indirect competitors for plankton production. Ecosystem model simulations suggested that among all trophic interactions within the Pacific Northwest coastal food web, juvenile salmon are particularly sensitive to jellyfish blooms, and that salmon production will be suppressed in years of high summer jellyfish biomass. Pelagic surveys off Oregon and Washington (1999-2012) were used to examine the interannual relationship between salmon production and the dominant jellyfish species, the sea nettle Chrysaora fuscescens, off the Pacific Northwest coast. There was a significant, negative correlation between sea nettle biomass and the strength of adult coho and Chinook salmon returns to the Columbia River. Examination of spatial distributions across years showed a positive association between sea nettles and salmon. Within individual years, significant differences between the distribution of sea nettles and yearling coho and Chinook salmon generally occurred during cooler ocean summers, perhaps due to the greater expanse of optimal salmon habitat resulting from more upwelling. Whether the association is behavioral or a product of oceanographic processes, association enhances the opportunity for indirect competition. Examination of feeding incidence in September showed that salmon stomachs were less full at locations with higher sea nettle biomass.
C1 [Ruzicka, James J.; Daly, Elizabeth A.] Oregon State Univ, Cooperat Inst Marine Resources Studies, Newport, OR 97366 USA.
[Brodeur, Richard D.] NOAA, Fish Ecol Div, NOAA Fisheries, Northwest Fisheries Sci Ctr,Natl Marine Fisheries, Newport, OR 97366 USA.
RP Ruzicka, JJ (reprint author), Oregon State Univ, Cooperat Inst Marine Resources Studies, Newport, OR 97366 USA.
EM jim.ruzicka@oregonstate.edu
FU Bonneville Power Administration (BPA) [00053808]; North Pacific Research
Board [F6405-03, P1405]; Lenfest Ocean Program from the Pew Charitable
Trusts [00025535]
FX We thank P. Lawson (NWFSC), C. Rice (NWFSC), K. Robinson (OSU), L.
Weitkamp (NWFSC), and two anonymous reviewers for their comments on
earlier versions of this manuscript. S. Ruzicka (USDAFS) created the
maps. Support for this research came from the Bonneville Power
Administration (BPA Contract No. 00053808 to Oregon State University and
to NOAA), from the North Pacific Research Board to J. Ruzicka (F6405-03)
and R. Brodeur (P1405), and from the Lenfest Ocean Program (Grant No.
00025535) from the Pew Charitable Trusts.
NR 60
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Z9 2
U1 16
U2 22
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 2150-8925
J9 ECOSPHERE
JI Ecosphere
PD APR
PY 2016
VL 7
IS 4
AR e01324
DI 10.1002/ecs2.1324
PG 22
WC Ecology
SC Environmental Sciences & Ecology
GA DN6VA
UT WOS:000377213400013
ER
PT J
AU Kumar, S
Zwiers, F
Dirmeyer, PA
Lawrence, DM
Shrestha, R
Werner, AT
AF Kumar, Sanjiv
Zwiers, Francis
Dirmeyer, Paul A.
Lawrence, David M.
Shrestha, Rajesh
Werner, Arelia T.
TI Terrestrial contribution to the heterogeneity in hydrological changes
under global warming
SO WATER RESOURCES RESEARCH
LA English
DT Article
ID MEAN ANNUAL EVAPOTRANSPIRATION; NORTH-AMERICAN CLIMATE; LONG-TERM
PERSISTENCE; BUDYKO FRAMEWORK; UNITED-STATES; PRECIPITATION TRENDS;
WATER AVAILABILITY; STREAMFLOW TRENDS; CARBON-DIOXIDE; RUNOFF
AB This study investigates a physical basis for heterogeneity in hydrological changes, which suggests a greater detectability in wet than dry regions. Wet regions are those where atmospheric demand is less than precipitation (energy limited), and dry regions are those where atmospheric demand is greater than precipitation (water limited). Long-term streamflow trends in western North America and an analysis of Coupled Model Intercomparison Project Phase 5 (CMIP5) climate models at global scales show geographically heterogeneous detectability of hydrological changes. We apply the Budyko framework and state-of-the-art climate model data from CMIP5 to quantify the sensitivity and detectability of terrestrial hydrological changes. The Budyko framework quantifies the partitioning of precipitation into evapotranspiration and runoff components. We find that the terrestrial hydrological sensitivity is 3 times greater in regions where the hydrological cycle is energy limited rather than water limited. This additional source (the terrestrial part) contributes to 30-40% greater detectability in energy-limited regions. We also quantified the contribution of changes in the catchment efficiency parameter that oppose the effects of increasing evaporative demand in global warming scenarios. Incorporating changes to the catchment efficiency parameter in the Budyko framework reduces dry biases in global runoff change projections by 88% in the 21st century.
C1 [Kumar, Sanjiv; Zwiers, Francis; Shrestha, Rajesh; Werner, Arelia T.] Univ Victoria, Pacific Climate Impacts Consortium, Victoria, BC, Canada.
[Kumar, Sanjiv] NOAA, ESRL Phys Sci Div, Boulder, CO USA.
[Dirmeyer, Paul A.] George Mason Univ, Ctr Ocean Land Atmosphere Studies, Fairfax, VA 22030 USA.
[Lawrence, David M.] Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA.
RP Kumar, S (reprint author), Univ Victoria, Pacific Climate Impacts Consortium, Victoria, BC, Canada.; Kumar, S (reprint author), NOAA, ESRL Phys Sci Div, Boulder, CO USA.
EM Sanjiv.Kumar@noaa.gov
FU NSERC Canadian Sea Ice and snow Evaluation (CanSISE) Network
FX S.K. and F.Z. were supported by NSERC Canadian Sea Ice and snow
Evaluation (CanSISE) Network. The first author thanks Markus Schnorbus
and Faron Anslow (both from PCIC) for providing hydrology data for
watersheds in British Columbia. The first author also thanks Justin
Sheffield (Princeton University) for providing Princeton Hydrology data.
We acknowledge the World Climate Research Programme's Working Group on
Coupled Modelling, which is responsible for CMIP, and we thank the
climate modeling groups (listed in supporting information Table S1) for
producing and making available their model output. CMIP5 climate model
data were obtained from following website:
https://pcmdi9.llnl.gov/projects/esgf-llnl/. Streamflow data were
obtained from United States Geological Survey
(http://waterdata.usgs.gov/nwis/uv/?referred_module=sw) and Environment
Canada HYDAT database
(https://ec.gc.ca/rhc-wsc/default.asp?lang=En&n=9018B5EC-1) for western
United States and Western Canada, respectively. High-resolution PRISM
climate data were provided by PRISM Climate Group, Oregon State
University, http://prism.oregonstate.edu, created 4 February 2004. We
also thank Michael L. Roderick and one anonymous reviewer for their
constructive comments on earlier versions of this manuscript.
NR 70
TC 3
Z9 3
U1 12
U2 18
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0043-1397
EI 1944-7973
J9 WATER RESOUR RES
JI Water Resour. Res.
PD APR
PY 2016
VL 52
IS 4
BP 3127
EP 3142
DI 10.1002/2016WR018607
PG 16
WC Environmental Sciences; Limnology; Water Resources
SC Environmental Sciences & Ecology; Marine & Freshwater Biology; Water
Resources
GA DN9XA
UT WOS:000377432800044
ER
PT J
AU Bert, TM
Geiger, SP
Gerhart, SD
Mccarthy, KJ
AF Bert, Theresa M.
Geiger, Stephen P.
Gerhart, Susan D.
Mccarthy, Kevin J.
TI FACTORS INFLUENCING REPRODUCTIVE ATTRIBUTES OF STONE CRABS (MENIPPE) IN
TAMPA BAY, FLORIDA
SO JOURNAL OF SHELLFISH RESEARCH
LA English
DT Article
DE clutch size; egg size; egg weight; fishery; Florida; Gulf of Mexico;
Menippe; missing appendage; Octolasmis mulleri; reproduction; stone
crab; temperature
ID HELICE-CRASSA GRAPSIDAE; FRESH-WATER CRAYFISH; GULF-OF-MEXICO; EGG SIZE;
CALLINECTES-SAPIDUS; BRACHYURAN CRABS; BLUE-CRAB; CHIONOECETES-OPILIO;
MERCENARIA SAY; MUD CRAB
AB Understanding aspects of reproduction is important for studies of life history strategy and for resource management. The influences of nine factors (five intrinsic, four extrinsic) on the reproductive attributes egg diameter, egg dry weight, and clutch size (i.e., number of eggs in egg mass) of female stone crabs (genus Menippe (Say)) from Tampa Bay, FL, waters were investigated. Two intrinsic factors influenced reproductive attributes: carapace width was positively correlated with clutch size, and egg stage was positively related to egg size. Three intrinsic factors-genotype class, damaged or missing pleopods, and missing claws or legs-had no influence on any reproductive attribute. The four extrinsic factors each influenced at least two reproductive attributes. Egg diameter and weight were significantly larger and clutch size was significantly smaller (1) in females uninfested by Octolasmis mulleri; (2) during the early part of the spawning season, when water temperature was 27 degrees C or less; and (3) during the first year of the 3-y study. In addition, egg diameter varied significantly among season/year combinations. In all cases, when egg diameter and weight decreased, clutch size increased; suggesting that, in female stone crabs, selection for filling the available abdominal space with eggs is strong. Large eggs are known to produce larvae of high fitness in crabs. Because the largest eggs are produced during the early part of the spawning season, females should be protected from harvest during that time. Shortening the harvest season in spring would eliminate those females from vulnerability to the fishery.
C1 [Bert, Theresa M.; Geiger, Stephen P.] Florida Fish & Wildlife Conservat Commiss, Fish & Wildlife Res Inst, 100 Eighth Ave SE, St Petersburg, FL 33701 USA.
[Gerhart, Susan D.] Natl Marine Fisheries Serv, Southeast Reg Off, 263 13th Ave South, St Petersburg, FL 33701 USA.
[Mccarthy, Kevin J.] Natl Marine Fisheries Serv, Southeast Fisheries Sci Ctr, 75 Virginia Beach Dr, Key Biscayne, FL 33149 USA.
RP Bert, TM (reprint author), Florida Fish & Wildlife Conservat Commiss, Fish & Wildlife Res Inst, 100 Eighth Ave SE, St Petersburg, FL 33701 USA.
EM theresa.bert@myfwc.com
FU Department of Commerce; National Oceanic and Atmospheric Administration;
Interjurisdictional Fisheries grants; state of Florida
FX We are grateful to numerous Fish and Wildlife Research Institute staff
members who helped with the field work; and to T. Jones, who assisted
with the laboratory work involved in analyzing the reproductive
attributes. We thank Z. Boudreau, C. Crowley, R. Gandy, and D. Wilber
for providing valuable reviews of the manuscript. This work was
supported by Department of Commerce, National Oceanic and Atmospheric
Administration, Interjurisdictional Fisheries grants and by the state of
Florida.
NR 106
TC 1
Z9 1
U1 7
U2 7
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
EI 1943-6319
J9 J SHELLFISH RES
JI J. Shellfish Res.
PD APR
PY 2016
VL 35
IS 1
BP 241
EP 257
DI 10.2983/035.035.0127
PG 17
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA DN0HA
UT WOS:000376743800027
ER
PT J
AU Ryer, CH
Ottmar, M
Spencer, M
Anderson, JD
Cooper, D
AF Ryer, Clifford H.
Ottmar, Michele
Spencer, Mara
Anderson, Janet Duffy
Cooper, Daniel
TI TEMPERATURE-DEPENDENT GROWTH OF EARLY JUVENILE SOUTHERN TANNER CRAB
CHIONOECETES BAIRDI: IMPLICATIONS FOR COLD POOL EFFECTS AND CLIMATE
CHANGE IN THE SOUTHEASTERN BERING SEA
SO JOURNAL OF SHELLFISH RESEARCH
LA English
DT Article
DE temperature-dependent growth; survival; recruitment; intermolt period;
Chionoecetes bairdi; crab
ID RED KING CRAB; CALLINECTES-SAPIDUS; BLUE-CRAB; OPILIO; RECRUITMENT;
SIZE; ECOSYSTEM; DYNAMICS; ALASKAN; MOLT
AB Temperature strongly influences the growth of crustaceans and directly controls distribution. Despite being commercially important, there are no data on temperature effects upon growth in newly settled southern Tanner crab Chionoecetes bairdi. Recently settled crabs were reared through three consecutive molts, both individually and in groups, at four different temperatures; 2 degrees C, 6 degrees C, 9 degrees C, and 12 degrees C. Survival was higher for crabs grown individually (92%) than those in groups (66%) owing to cannibalism, particularly during molting. There were no temperature effects on survival. Growth rate (mm/day) increased linearly with temperature, a product of exponential decline in intermolt period with increasing temperature and a molt increment that was relatively constant across temperatures. Growth rate, intermolt period, and growth increment did not differ between crabs grown singly or in groups. These data suggest that growth in 0 y aged southern Tanner crabs is strongly inhibited at temperatures less than 2 degrees C. A small mesh beam trawl survey was conducted in the southeast Bering Sea during September 2012, a year when a cold pool (<2 degrees C bottom water) dominated the middle shelf. Southern Tanner crab less than 12mm(carapace width) were concentrated just north of the Alaska Peninsula and along the outer shelf where bottom water was more than 2 degrees C, but largely absent from the middle shelf. In contrast, adult southern Tanner crabs were widely distributed across the middle and outer shelves. It was hypothesized that early juvenile southern Tanner growth is inhibited by cold pool conditions, prolonging vulnerability to predation, and reducing survival. In the future, if sea temperature rises and sea ice is diminished, less frequent and less intense cold pool events may lead to increased persistence of thermally suitable juvenile southern Tanner crab habitat across the southeastern Bering Sea middle shelf region.
C1 [Ryer, Clifford H.; Ottmar, Michele; Spencer, Mara] Oregon State Univ, Hatfield Marine Sci Ctr, Fisheries Behav Ecol Program, RACE Div,Natl Marine Fisheries Serv,Alaska Fisher, 2030 Marine Sci Dr, Newport, OR 97365 USA.
[Anderson, Janet Duffy; Cooper, Daniel] Alaska Fisheries Sci Ctr, Recruitment Proc Program, RACE Div, Alaska Fisheries Sci Ctr, 7600 Sand Point Way NE, Seattle, WA 98115 USA.
RP Ryer, CH (reprint author), Oregon State Univ, Hatfield Marine Sci Ctr, Fisheries Behav Ecol Program, RACE Div,Natl Marine Fisheries Serv,Alaska Fisher, 2030 Marine Sci Dr, Newport, OR 97365 USA.
EM cliff.ryer@noaa.gov
FU Essential Fish Habitat grant from the Alaska Fisheries Science Center's
Regional Habitat Division
FX We would like to thank Paul Iseri and Scott Haines for assistance with
the laboratory experiments, as well as Ben Laurel and Brian Knoth for
assistance with live collections. Cynthia Sweitzer provided help with
procurement of permits and assisted with manuscript preparation. Helpful
comments on an early manuscript were provided by Dan Urban and Ben Daly.
This research was funded in part by an Essential Fish Habitat grant from
the Alaska Fisheries Science Center's Regional Habitat Division.
NR 46
TC 0
Z9 0
U1 10
U2 14
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
EI 1943-6319
J9 J SHELLFISH RES
JI J. Shellfish Res.
PD APR
PY 2016
VL 35
IS 1
BP 259
EP 267
DI 10.2983/035.035.0128
PG 9
WC Fisheries; Marine & Freshwater Biology
SC Fisheries; Marine & Freshwater Biology
GA DN0HA
UT WOS:000376743800028
ER
PT J
AU Suarez-Moo, PD
Gilbert-Horvath, EA
Vadopalas, B
Calderon-Aguilera, LE
Garza, JC
Rocha-Olivares, A
AF de Jesus Suarez-Moo, Pablo
Gilbert-Horvath, Elizabeth A.
Vadopalas, Brent
Eduardo Calderon-Aguilera, Luis
Carlos Garza, John
Rocha-Olivares, Axayacatl
TI Genetic homogeneity of the geoduck clam Panopea generosa in the
northeast Pacific
SO BIOCHEMICAL SYSTEMATICS AND ECOLOGY
LA English
DT Article
DE Panopea generosa; Mitochondrial genes; Microsatellite loci; Genetic
homogeneity; Washington; Baja California
ID TETRANUCLEOTIDE MICROSATELLITE LOCI; MULTILOCUS GENOTYPE DATA;
POPULATION-STRUCTURE; STRONGYLOCENTROTUS-FRANCISCANUS; BAJA-CALIFORNIA;
SOFTWARE; ABRUPTA; CIRCULATION; PATCHINESS; SEQUENCES
AB Geoduck clams are a valuable natural resource along the northeast Pacific, which makes the assessment of the biological and genetic status of their populations a key element to provide a basis for their proper management and conservation. In the present study, we assess the genetic variability and connectivity of Panopea generosa Gould, 1850 among four localities in the northeast Pacific using mitochondrial (DNA sequences from COI and COIII) and nuclear (five microsatellite loci) data. We found no evidence of genetic differentiation among localities encompassing scales of 100s to 1000s of kilometers along the northeast Pacific, which is consistent with a large effective population size and extensive gene flow in the absence of significant barriers acting on the larval stages. Our genetic findings and phenotypic evidence are consistent with the existence of a single management unit shared by Canada, the United States and Mexico, but further studies with increased geographic and genetic sampling are warranted to better estimate the extent and direction of gene flow to help in international management and conservation measures of this valuable resource. (C) 2016 Elsevier Ltd. All rights reserved.
C1 [de Jesus Suarez-Moo, Pablo; Rocha-Olivares, Axayacatl] CICESE, Dept Biol Oceanog, Mol Ecol Lab, Carretera Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico.
[Gilbert-Horvath, Elizabeth A.; Carlos Garza, John] NOAA, SW Fisheries Sci Ctr, 110 Shaffer Rd, Santa Cruz, CA 95060 USA.
[Vadopalas, Brent] Univ Washington, Sch Aquat & Fishery Sci, 1122 NE Boat St,Box 355020, Seattle, WA 98105 USA.
[Eduardo Calderon-Aguilera, Luis] CICESE, Dept Marine Ecol, Fisheries & Coastal Ecol Lab, Carretera Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico.
RP Rocha-Olivares, A (reprint author), CICESE, Dept Biol Oceanog, Mol Ecol Lab, Carretera Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico.
EM arocha@cicese.mx
RI Calderon-Aguilera, Luis Eduardo/E-1522-2015;
OI Calderon-Aguilera, Luis Eduardo/0000-0001-5427-6043; Rocha-Olivares,
Axayacatl/0000-0002-2700-9086
FU CICESE [625112]
FX We thank Alex Bradbury, Robert Sizemore, Don Rothaus, and Michael Ulrich
of the Washington Department of Fish and Wildlife (a.k.a. The Fab Four)
and Victor M. Moreno Rivera for help in sample collection and
processing. Vanessa Apkenas assisted with the genotyping of samples in
the laboratory. This research was supported by CICESE grant 625112 to
A.R.O.
NR 45
TC 0
Z9 0
U1 8
U2 12
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0305-1978
EI 1873-2925
J9 BIOCHEM SYST ECOL
JI Biochem. Syst. Ecol.
PD APR
PY 2016
VL 65
BP 66
EP 71
DI 10.1016/j.bse.2016.02.003
PG 6
WC Biochemistry & Molecular Biology; Ecology; Evolutionary Biology
SC Biochemistry & Molecular Biology; Environmental Sciences & Ecology;
Evolutionary Biology
GA DK0JN
UT WOS:000374599200009
ER
PT J
AU Carter, BR
Frolicher, TL
Dunne, JP
Rodgers, KB
Slater, RD
Sarmiento, JL
AF Carter, B. R.
Frolicher, T. L.
Dunne, J. P.
Rodgers, K. B.
Slater, R. D.
Sarmiento, J. L.
TI When can ocean acidification impacts be detected from decadal alkalinity
measurements?
SO GLOBAL BIOGEOCHEMICAL CYCLES
LA English
DT Article
DE alkalinity; ocean acidification; trend detection; repeat hydrography;
carbon cycle; carbonate system
ID LINE SIMULATION CHARACTERISTICS; CLIMATE; 21ST-CENTURY; VARIABILITY;
FORMULATION; EMERGENCE; MODELS; CYCLE; TIME
AB We use a large initial condition suite of simulations (30 runs) with an Earth system model to assess the detectability of biogeochemical impacts of ocean acidification (OA) on the marine alkalinity distribution from decadally repeated hydrographic measurements such as those produced by the Global Ship-Based Hydrographic Investigations Program (GO-SHIP). Detection of these impacts is complicated by alkalinity changes from variability and long-term trends in freshwater and organic matter cycling and ocean circulation. In our ensemble simulation, variability in freshwater cycling generates large changes in alkalinity that obscure the changes of interest and prevent the attribution of observed alkalinity redistribution to OA. These complications from freshwater cycling can be mostly avoided through salinity normalization of alkalinity. With the salinity-normalized alkalinity, modeled OA impacts are broadly detectable in the surface of the subtropical gyres by 2030. Discrepancies between this finding and the finding of an earlier analysis suggest that these estimates are strongly sensitive to the patterns of calcium carbonate export simulated by the model. OA impacts are detectable later in the subpolar and equatorial regions due to slower responses of alkalinity to OA in these regions and greater seasonal equatorial alkalinity variability. OA impacts are detectable later at depth despite lower variability due to smaller rates of change and consistent measurement uncertainty.
C1 [Carter, B. R.] Univ Washington, Joint Inst Study Atmosphere & Oceans, Seattle, WA 98195 USA.
[Carter, B. R.] NOAA, Pacific Marine Environm Lab, 7600 Sand Point Way Ne, Seattle, WA 98115 USA.
[Frolicher, T. L.] ETH, Inst Biogeochem & Pollutant Dynam, Environm Phys, Zurich, Switzerland.
[Dunne, J. P.] Princeton Univ, NOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08544 USA.
[Rodgers, K. B.; Slater, R. D.; Sarmiento, J. L.] Princeton Univ, Atmospher & Ocean Sci Program, Princeton, NJ 08544 USA.
RP Carter, BR (reprint author), Univ Washington, Joint Inst Study Atmosphere & Oceans, Seattle, WA 98195 USA.; Carter, BR (reprint author), NOAA, Pacific Marine Environm Lab, 7600 Sand Point Way Ne, Seattle, WA 98115 USA.
EM brendan.carter@noaa.gov
RI Frolicher, Thomas/E-5137-2015
OI Frolicher, Thomas/0000-0003-2348-7854
FU Climate Observation Division of the NOAA Climate Program Office; U.S.
National Science Foundation [ANT-1040957]; Carbon Data Management and
Synthesis NOAA grant [N8R1SE3-PGC]; SNSF [PZ00P2_142573]; NOAA Office of
Climate Observations (OCO) [NA17RJ2612, NA08OAR4320752]; NOAA
[NA11OAR4310066]
FX We thank Swarthmore undergraduate researcher Jeong Do Ahn for his
helpful explorations of carbonate cycling in ESM2M. Anonymous reviewers
provided appreciated helpful feedback on the manuscript content and
presentation. We are grateful to Kathy Tedesco of the Climate
Observation Division of the NOAA Climate Program Office for funding for
this research. B.R.C. was supported by the U.S. National Science
Foundation (ANT-1040957) and the Carbon Data Management and Synthesis
NOAA grant (N8R1SE3-PGC). T.L.F. acknowledges financial support from the
SNSF (Ambizione grant PZ00P2_142573). The contribution of KBR came
through awards NA17RJ2612 and NA08OAR4320752, which includes support
through the NOAA Office of Climate Observations (OCO), and NOAA award
NA11OAR4310066. ESM2M data output can be obtained from the Coupled Model
Intercomparison Project data portal
(http://cmippcmdi.llnl.gov/cmip5/data_portal.html), and the processed
ensemble model output required to reproduce our figures is included as
supporting information. This is PMEL contribution 4392 and JISAO
contribution 2504.
NR 45
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Z9 1
U1 6
U2 9
PU AMER GEOPHYSICAL UNION
PI WASHINGTON
PA 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
SN 0886-6236
EI 1944-9224
J9 GLOBAL BIOGEOCHEM CY
JI Glob. Biogeochem. Cycle
PD APR
PY 2016
VL 30
IS 4
BP 595
EP 612
DI 10.1002/2015GB005308
PG 18
WC Environmental Sciences; Geosciences, Multidisciplinary; Meteorology &
Atmospheric Sciences
SC Environmental Sciences & Ecology; Geology; Meteorology & Atmospheric
Sciences
GA DM3SY
UT WOS:000376268000004
ER
PT J
AU Scott, JD
Alexander, MA
Murray, DR
Swales, D
Eischeid, J
AF Scott, James D.
Alexander, Michael A.
Murray, Donald R.
Swales, Dustin
Eischeid, Jon
TI THE CLIMATE CHANGE WEB PORTAL A System to Access and Display Climate and
Earth System Model Output from the CMIP5 Archive
SO BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY
LA English
DT Editorial Material
C1 [Scott, James D.; Murray, Donald R.; Swales, Dustin; Eischeid, Jon] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Scott, James D.; Alexander, Michael A.; Murray, Donald R.; Swales, Dustin; Eischeid, Jon] NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA.
RP Scott, JD (reprint author), NOAA, Earth Syst Res Lab, R PSD1, 325 Broadway, Boulder, CO 80305 USA.
EM james.d.scott@noaa.gov
RI Alexander, Michael/A-7097-2013
OI Alexander, Michael/0000-0001-9646-6427
NR 6
TC 1
Z9 1
U1 0
U2 4
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 APR
PY 2016
VL 97
IS 4
BP 523
EP 530
DI 10.1175/BAMS-D-15-00035.1
PG 8
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DL9HE
UT WOS:000375951600003
ER
PT J
AU Clifford, D
Alegre, R
Bennett, V
Blower, J
Deluca, C
Kershaw, P
Lynnes, C
Mattmann, C
Phipps, R
Rozum, I
AF Clifford, Debbie
Alegre, Raquel
Bennett, Victoria
Blower, Jon
Deluca, Cecelia
Kershaw, Philip
Lynnes, Christopher
Mattmann, Chris
Phipps, Rhona
Rozum, Iryna
TI Capturing and Sharing Our Collective Expertise on Climate Data The
CHARMe Project
SO BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY
LA English
DT Editorial Material
C1 [Clifford, Debbie; Blower, Jon; Phipps, Rhona] Univ Reading, Reading RG6 6BB, Berks, England.
[Alegre, Raquel] UCL, London, England.
[Bennett, Victoria; Kershaw, Philip] Sci & Technol Facil Council, Swindon, Wilts, England.
[Deluca, Cecelia] NOAA, NESII, CIRES, Earth Syst Res Lab, Boulder, CO USA.
[Lynnes, Christopher] NASA, Goddard Space Flight Ctr, Greenbelt, MD USA.
[Mattmann, Chris] NASA, Jet Prop Lab, Pasadena, CA USA.
[Rozum, Iryna] European Ctr Medium Range Weather Forecasts, Shinfield Pk, Reading RG2 9AX, Berks, England.
RP Clifford, D (reprint author), Univ Reading, Dept Meteorol, Reading RG6 6BB, Berks, England.
EM d.j.clifford@reading.ac.uk
OI Kershaw, Philip/0000-0002-7646-291X
NR 6
TC 0
Z9 0
U1 0
U2 1
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 APR
PY 2016
VL 97
IS 4
BP 531
EP 539
DI 10.1175/BAMS-D-14-00189.1
PG 9
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DL9HE
UT WOS:000375951600004
ER
PT J
AU Zhang, J
Howard, K
Langston, C
Kaney, B
Qi, YC
Tang, L
Grams, H
Wang, YD
Cocks, S
Martinaitis, S
Arthur, A
Cooper, K
Brogden, J
Kitzmiller, D
AF Zhang, Jian
Howard, Kenneth
Langston, Carrie
Kaney, Brian
Qi, Youcun
Tang, Lin
Grams, Heather
Wang, Yadong
Cocks, Stephen
Martinaitis, Steven
Arthur, Ami
Cooper, Karen
Brogden, Jeff
Kitzmiller, David
TI MULTI-RADAR MULTI-SENSOR (MRMS) QUANTITATIVE PRECIPITATION ESTIMATION
Initial Operating Capabilities
SO BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY
LA English
DT Article
ID REAL-TIME ALGORITHM; UNITED-STATES; BEAM BLOCKAGE; NETWORK; SYSTEM;
RAIN; CLASSIFICATION; IDENTIFICATION; TERRAIN; QPES
C1 [Zhang, Jian; Howard, Kenneth; Langston, Carrie; Kaney, Brian; Qi, Youcun; Tang, Lin; Grams, Heather; Wang, Yadong; Cocks, Stephen; Martinaitis, Steven; Arthur, Ami; Cooper, Karen; Brogden, Jeff] NOAA OAR NSSL, Norman, OK USA.
[Langston, Carrie; Kaney, Brian; Qi, Youcun; Tang, Lin; Grams, Heather; Wang, Yadong; Cocks, Stephen; Martinaitis, Steven; Arthur, Ami; Cooper, Karen; Brogden, Jeff] Univ Oklahoma, Cooperat Inst Mesoscale Meteorol Studies, Norman, OK 73019 USA.
[Kitzmiller, David] NOAA NWS OHD, Silver Spring, MD USA.
RP Zhang, J (reprint author), Natl Weather Ctr, NSSL, 120 David L Boren Blvd, Norman, OK 73072 USA.
EM jian.zhang@noaa.gov
FU National Oceanic and Atmospheric Administration (NOAA); American
Institute in Taiwan (AIT); NOAA; Salt River Project; NOAA-University of
Oklahoma [NA17RJ1227, NA13OAR4830236]; NOAA Integrated Dissemination
Program; National Weather Service's Office of Science and Technology
program
FX Major funding for this research was provided under the agreement between
the National Oceanic and Atmospheric Administration (NOAA) and the
American Institute in Taiwan (AIT) and the agreement between NOAA and
the Salt River Project. Partial funding was provided under
NOAA-University of Oklahoma Cooperative Agreements NA17RJ1227 and
NA13OAR4830236. The NOAA Integrated Dissemination Program and the
National Weather Service's Office of Science and Technology program
provided additional support and computational resources.
NR 48
TC 20
Z9 20
U1 1
U2 4
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 APR
PY 2016
VL 97
IS 4
BP 621
EP 637
DI 10.1175/BAMS-D-14-00174.1
PG 17
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DL9HE
UT WOS:000375951600011
ER
PT J
AU Goessling, HF
Jung, T
Klebe, S
Baeseman, J
Bauer, P
Chen, P
Chevallier, M
Dole, R
Gordon, N
Ruti, P
Bradley, A
Bromwich, DH
Casati, B
Chechin, D
Day, JJ
Massonnet, F
Mills, B
Renfrew, I
Smith, G
Tatusko, R
AF Goessling, Helge F.
Jung, Thomas
Klebe, Stefanie
Baeseman, Jenny
Bauer, Peter
Chen, Peter
Chevallier, Matthieu
Dole, Randall
Gordon, Neil
Ruti, Paolo
Bradley, Alice
Bromwich, David H.
Casati, Barbara
Chechin, Dmitry
Day, Jonathan J.
Massonnet, Francois
Mills, Brian
Renfrew, Ian
Smith, Gregory
Tatusko, Renee
TI PAVING THE WAY FOR THE YEAR OF POLAR PREDICTION
SO BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY
LA English
DT Editorial Material
C1 [Goessling, Helge F.; Jung, Thomas; Klebe, Stefanie] Alfred Wegener Inst, Bremerhaven, Germany.
[Jung, Thomas] Univ Bremen, D-28359 Bremen, Germany.
[Baeseman, Jenny] Sci Comm Antarctic Res, Cambridge, England.
[Baeseman, Jenny] Univ Alaska Fairbanks, Int Arctic Res Ctr, Fairbanks, AK USA.
[Bauer, Peter] European Ctr Medium Range Weather Forecasts, Shinfield Pk, Reading RG2 9AX, Berks, England.
[Chevallier, Matthieu] CNRS UMR 3589, CNRM, Meteo France, Toulouse, France.
[Dole, Randall] NOAA, Earth Syst Res Lab, Boulder, CO USA.
[Ruti, Paolo] World Meteorol Org, Geneva, Switzerland.
[Bradley, Alice] Univ Colorado, Boulder, CO 80309 USA.
[Bromwich, David H.] Ohio State Univ, Byrd Polar & Climate Res Ctr, Columbus, OH 43210 USA.
[Casati, Barbara; Mills, Brian; Smith, Gregory] Environm & Climate Change Canada, Meteorol Res Div, Dorval, PQ, Canada.
[Chechin, Dmitry] Russian Acad Sci, AM Obukhov Inst Atmospher Phys, Moscow, Russia.
[Day, Jonathan J.] Univ Reading, Dept Meteorol, NCAS Climate, Reading, Berks, England.
[Massonnet, Francois] Catholic Univ Louvain, Georges Lematre Ctr Earth & Climate Res, Earth & Life Inst, Louvain La Neuve, Belgium.
[Massonnet, Francois] Catalan Inst Climate Sci, Climate Forecasting Unit, Barcelona, Spain.
[Renfrew, Ian] Univ E Anglia, Sch Environm Sci, Norwich NR4 7TJ, Norfolk, England.
[Tatusko, Renee] Natl Weather Serv, NOAA, Anchorage, AK USA.
RP Goessling, HF (reprint author), Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Bussestr 24, D-27570 Bremerhaven, Germany.
EM helge.goessling@awi.de
RI Jung, Thomas/J-5239-2012; Chechin, Dmitry/J-9923-2016; Renfrew,
Ian/E-4057-2010;
OI Jung, Thomas/0000-0002-2651-1293; Chechin, Dmitry/0000-0003-0021-9945;
Renfrew, Ian/0000-0001-9379-8215; Massonnet,
Francois/0000-0002-4697-5781; Chevallier, Matthieu/0000-0003-2033-166X
NR 0
TC 3
Z9 3
U1 1
U2 3
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 APR
PY 2016
VL 97
IS 4
BP ES85
EP ES88
DI 10.1175/BAMS-D-15-00270.1
PG 4
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DL9HE
UT WOS:000375951600001
ER
PT J
AU Faverzani, M
Becker, D
Bennett, D
Day, P
Falferi, P
Ferri, E
Fowler, J
Gard, J
Giachero, A
Giordano, C
Hays-Wehle, J
Hilton, G
Maino, M
Margesin, B
Mates, J
Mezzena, R
Nizzolo, R
Nucciotti, A
Puiu, A
Reintsema, C
Schmidt, D
Swetz, D
Ullom, J
Vale, L
Zanetti, L
AF Faverzani, M.
Becker, D.
Bennett, D.
Day, P.
Falferi, P.
Ferri, E.
Fowler, J.
Gard, J.
Giachero, A.
Giordano, C.
Hays-Wehle, J.
Hilton, G.
Maino, M.
Margesin, B.
Mates, J.
Mezzena, R.
Nizzolo, R.
Nucciotti, A.
Puiu, A.
Reintsema, C.
Schmidt, D.
Swetz, D.
Ullom, J.
Vale, L.
Zanetti, L.
TI Superconducting Detectors for Neutrino Mass Measurement
SO IEEE TRANSACTIONS ON APPLIED SUPERCONDUCTIVITY
LA English
DT Article
DE Holmium 163; kinetic inductance detectors; neutrino mass; transition
edge sensors
ID ELECTRON-CAPTURE; SEARCH; DECAY
AB Assessing the absolute neutrino mass scale is one of the major challenges in particle physics and astrophysics nowadays. A powerful tool to directly estimate the effective electron neutrino mass consists in the calorimetric measurement of the energy released within a nu cl ear bet a decay. The progresses made over the last few decades on low-temperature detector technologies have permitted to design experiments with expected sensitivities on the neutrino mass below 1 eV/c(2) with the calorimetric approach. Despite the remarkable performances in both energy (similar to eV at keV) and time resolutions (similar to 1 mu s) on the single channel, a large number of detectors working in parallel is required to reach a sub-eV sensitivity. Microwave frequency-domain readout provides a powerful technique to read out large arrays of low-temperature detectors, such as transition edge sensors (TESs) or microwave kinetic inductanced etectors (MKIDs). In this way, the multiplex factor is only limited by the bandwidth of the available commercial fast digitizers. The microwave multiplexing system will be used to readout the TES array of the HOLMES experiment, which is made of 1000 Ho-163-implanted microcalorimeters. HOLMES is a new experiment that aims to measure the electron neutrino mass by means of the electron capture decay of Ho-163 with an expected sensitivity of the order of the eV/c(2).
C1 [Faverzani, M.; Ferri, E.; Giachero, A.; Maino, M.; Nizzolo, R.; Nucciotti, A.; Puiu, A.; Zanetti, L.] Univ Milano Bicocca, I-20126 Milan, Italy.
[Faverzani, M.; Ferri, E.; Giachero, A.; Maino, M.; Nizzolo, R.; Nucciotti, A.; Puiu, A.; Zanetti, L.] INFN Milano Bicocca, I-20126 Milan, Italy.
[Becker, D.; Bennett, D.; Fowler, J.; Gard, J.; Hays-Wehle, J.; Hilton, G.; Mates, J.; Reintsema, C.; Schmidt, D.; Swetz, D.; Ullom, J.; Vale, L.] NIST, Boulder, CO 80305 USA.
[Day, P.] CALTECH, Pasadena, CA 91125 USA.
[Day, P.] CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91125 USA.
[Falferi, P.] CNR Fdn Bruno Kessler, Ist Foton & Nanotecnol, I-38122 Trento, Trento, Italy.
[Giordano, C.; Margesin, B.] Fdn Bruno Kessler, I-38122 Trento, Trento, Italy.
[Mezzena, R.] Univ Trento, I-38122 Trento, Trento, Italy.
RP Faverzani, M (reprint author), Univ Milano Bicocca, I-20126 Milan, Italy.; Faverzani, M (reprint author), INFN Milano Bicocca, I-20126 Milan, Italy.
EM marco.faverzani@mib.infn.it; dan.becker@nist.gov;
douglas.bennet@nist.gov; peter.k.day@jpl.nasa.gov; falferi@fbk.eu;
elena.ferri@mib.infn.it; joe.fowler@nist.gov; johnathon.gard@nist.gov;
andrea.giachero@mib.infn.it; cgiordano@fbk.eu;
james.hays-wehle@nist.gov; gene.hilton@nist.gov;
matteo.maino@mib.infn.it; margesin@fbk.eu; john.mates@nist.gov;
mezzena@science.unitn.it; riccardo.nizzolo@mib.infn.it;
angelo.nucciotti@mib.infn.it; andrei.puiu@mib.infn.it;
carl.reintsema@nist.gov; dan.schmidt@nist.gov; daniel.swetz@nist.gov;
ullom@boulder.nist.gov; leila.vale@nist.gov; lorenzo.zanetti@mib.infn.it
RI Giachero, Andrea/I-1081-2013; Ferri, Elena/L-8531-2014
OI Giachero, Andrea/0000-0003-0493-695X; Ferri, Elena/0000-0003-1425-3669
FU Fondazione Cariplo through the project "Development of Microresonator
Detectors for Neutrino Physics" [2010-2351]
FX The work on microwave kinetic inductance detectors was supported by the
Fondazione Cariplo through the project "Development of Microresonator
Detectors for Neutrino Physics" under Grant 2010-2351. (Corresponding
author : M. Faverzani.)
NR 19
TC 0
Z9 0
U1 2
U2 4
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 1051-8223
EI 1558-2515
J9 IEEE T APPL SUPERCON
JI IEEE Trans. Appl. Supercond.
PD APR
PY 2016
VL 26
IS 3
AR 2100204
DI 10.1109/TASC.2016.2540242
PG 4
WC Engineering, Electrical & Electronic; Physics, Applied
SC Engineering; Physics
GA DM2PR
UT WOS:000376189300001
ER
PT J
AU Hao, ZC
Hao, FH
Xia, YL
Singh, VP
Hong, Y
Shen, XY
Ouyang, W
AF Hao, Zengchao
Hao, Fanghua
Xia, Youlong
Singh, Vijay P.
Hong, Yang
Shen, Xinyi
Ouyang, Wei
TI A Statistical Method for Categorical Drought Prediction Based on NLDAS-2
SO JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY
LA English
DT Article
ID AMERICAN MULTIMODEL ENSEMBLE; UNITED-STATES; METEOROLOGICAL DROUGHT;
SEASONAL PREDICTION; MODEL; INDEX; INFORMATION; REGRESSION; FORECASTS;
MONITOR
AB Drought is a slowly varying natural phenomenon and may have wide impacts on a range of sectors. Tremendous efforts have therefore been devoted to drought monitoring and prediction to reduce potential impacts of drought. Reliable drought prediction is critically important to provide information ahead of time for early warning to facilitate drought-preparedness plans. The U.S. Drought Monitor (USDM) is a composite drought product that depicts drought conditions in categorical forms, and it has been widely used to track drought and its impacts for operational and research purposes. The USDM is an assessment of drought condition but does not provide drought prediction information. Given the wide application of USDM, drought prediction in a categorical form similar to that of USDM would be of considerable importance, but it has not been explored thus far. This study proposes a statistical method for categorical drought prediction by integrating the USDM drought category as an initial condition with drought information from other sources such as drought indices from land surface simulation or statistical prediction. Incorporating USDM drought categories and drought indices from phase 2 of the North American Land Data Assimilation System (NLDAS-2), the proposed method is tested in Texas for 2001-14. Results show satisfactory performance of the proposed method for categorical drought prediction, which provides useful information to aid early warning for drought-preparedness plans.
C1 [Hao, Zengchao; Hao, Fanghua; Ouyang, Wei] Beijing Normal Univ, Sch Environm, Green Dev Inst, Beijing 100875, Peoples R China.
[Xia, Youlong] Natl Ctr Environm Predict, Environm Modeling Ctr, College Pk, MD USA.
[Xia, Youlong] IM Syst Grp, College Pk, MD USA.
[Singh, Vijay P.] Texas A&M Univ, Dept Biol & Agr Engn, College Stn, TX USA.
[Singh, Vijay P.] Texas A&M Univ, Zachry Dept Civil Engn, College Stn, TX USA.
[Hong, Yang] Univ Oklahoma, Hydrometeorol & Remote Sensing Lab, Norman, OK 73019 USA.
[Hong, Yang] Univ Oklahoma, Adv Radar Res Ctr, Norman, OK 73019 USA.
[Hong, Yang] Univ Oklahoma, Sch Civil Engn & Environm Sci, Norman, OK 73019 USA.
[Shen, Xinyi] Univ Connecticut, Sch Engn, Dept Civil & Environm Engn, Storrs, CT USA.
RP Hao, ZC (reprint author), 19 XinJieKouWai St, Beijing 100875, Peoples R China.
EM haozc@bnu.edu.cn
RI Hong, Yang/D-5132-2009
OI Hong, Yang/0000-0001-8720-242X
FU program of the "Twelfth Five-Year Plan" for Science and Technology
Research of China [2012BAD15B05]; Youth Scholars Program of Beijing
Normal University [2015NT02]
FX The authors are grateful to the editor and anonymous reviewers for their
valuable comments and suggestions. This work is supported by the program
of the "Twelfth Five-Year Plan" for Science and Technology Research of
China (2012BAD15B05) and Youth Scholars Program of Beijing Normal
University (Grant 2015NT02). We thank the Environmental Modeling Center
of the National Oceanic and Atmospheric Administration National Centers
for Environmental Prediction for providing the NLDAS-2 datasets.
NR 60
TC 1
Z9 1
U1 4
U2 10
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 APR
PY 2016
VL 55
IS 4
BP 1049
EP 1061
DI 10.1175/JAMC-D-15-0200.1
PG 13
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DM3GF
UT WOS:000376234100002
ER
PT J
AU Dong, S
Li, JJ
Li, X
Wei, Y
AF Dong Sheng
Li Jingjing
Li Xue
Wei Yong
TI Study of Vertical Breakwater Reliability Based on Copulas
SO JOURNAL OF OCEAN UNIVERSITY OF CHINA
LA English
DT Article
DE vertical breakwater; reliability; Archimedean copula; goodness of fit;
bivariate logistic Gumbel distribution; bivariate Lognormal
distribution; multivariate distribution
ID CAISSON BREAKWATERS; CLIMATE-CHANGE; DESIGN METHOD; STABILITY
AB The reliability of a vertical breakwater is calculated using direct integration methods based on joint density functions. The horizontal and uplifting wave forces on the vertical breakwater can be well fitted by the lognormal and the Gumbel distributions, respectively. The joint distribution of the horizontal and uplifting wave forces is analyzed using different probabilistic distributions, including the bivariate logistic Gumbel distribution, the bivariate lognormal distribution, and three bivariate Archimedean copulas functions constructed with different marginal distributions simultaneously. We use the fully nested copulas to construct multivariate distributions taking into account related variables. Different goodness fitting tests are carried out to determine the best bivariate copula model for wave forces on a vertical breakwater. We show that a bivariate model constructed by Frank copula gives the best reliability analysis, using marginal distributions of Gumbel and lognormal to account for uplifting pressure and horizontal wave force on a vertical breakwater, respectively. The results show that failure probability of the vertical breakwater calculated by multivariate density function is comparable to those by the Joint Committee on Structural Safety methods. As copulas are suitable for constructing a bivariate or multivariate joint distribution, they have great potential in reliability analysis for other coastal structures.
C1 [Dong Sheng; Li Jingjing; Li Xue] Ocean Univ China, Coll Engn, Qingdao 266100, Peoples R China.
[Wei Yong] NOAA, Pacific Marine Environm Lab, 7600 Sand Point Way Ne, Seattle, WA 98115 USA.
[Wei Yong] Univ Washington, Joint Inst Study Atmosphere & Ocean, Seattle, WA 98105 USA.
RP Dong, S (reprint author), Ocean Univ China, Coll Engn, Qingdao 266100, Peoples R China.
EM dongsh@ouc.edu.cn
FU National Natural Science Foundation of China [51279186, 51479183]; 111
Project [B14028]; Chinese Scholarship Council
FX The study is supported by the National Natural Science Foundation of
China (51279186, 51479183) and the 111 Project (B14028). The first
author thanks the Chinese Scholarship Council for funding his research
in University of Washington. The authors thank the anonymous reviewers
for their constructive comments for the improvement of the manuscript.
NR 37
TC 0
Z9 0
U1 4
U2 4
PU OCEAN UNIV CHINA
PI QINGDAO
PA 5 YUSHAN RD, QINGDAO, 266003, PEOPLES R CHINA
SN 1672-5182
EI 1993-5021
J9 J OCEAN U CHINA
JI J. OCEAN UNIV.
PD APR
PY 2016
VL 15
IS 2
BP 232
EP 240
DI 10.1007/s11802-016-2692-7
PG 9
WC Oceanography
SC Oceanography
GA DM0HE
UT WOS:000376023500005
ER
PT J
AU Maghrebi, MF
AF Maghrebi, Mohammad F.
TI Renyi information from entropic effects in one higher dimension
SO JOURNAL OF STATISTICAL MECHANICS-THEORY AND EXPERIMENT
LA English
DT Article
DE entanglement in extended quantum systems (theory); Casimir effect
(theory)
ID ENTANGLEMENT ENTROPY; CASIMIR FORCE; FIELD-THEORY; SYSTEMS
AB Computing entanglement entropy and its cousins is often challenging even in the simplest continuum and lattice models, partly because such entropies depend nontrivially on all geometric characteristics of the entangling region. Quantum information measures between two or more regions are even more complicated, but contain more, and universal, information. In this paper, we focus on Renyi entropy and information of the order n = 2. For a free field theory, we show that these quantities are mapped to the change of the thermodynamic free energy by introducing boundaries subject to Dirichlet and Neumann boundary conditions in one higher dimension. This mapping allows us to exploit the powerful tools available in the context of thermal Casimir effect, specifically a multipole expansion suited for computing the Renyi information between arbitrarily-shaped regions. In particular, we compute the Renyi information between two disk-shaped regions at an arbitrary separation distance. We provide an alternative representation of the Renyi information as a sum over closed-loop polymers, which establishes a connection to purely entropic effects, and proves useful in deriving information inequalities. Finally, we discuss extensions of our results beyond free field theories.
C1 [Maghrebi, Mohammad F.] Univ Maryland, NIST, Joint Quantum Inst, College Pk, MD 20742 USA.
[Maghrebi, Mohammad F.] Univ Maryland, NIST, Joint Ctr Quantum Informat & Comp Sci, College Pk, MD 20742 USA.
RP Maghrebi, MF (reprint author), Univ Maryland, NIST, Joint Quantum Inst, College Pk, MD 20742 USA.; Maghrebi, MF (reprint author), Univ Maryland, NIST, Joint Ctr Quantum Informat & Comp Sci, College Pk, MD 20742 USA.
EM magrebi@umd.edu
FU NSF PIF; AFOSR; ARO; ARL; NSF PFC at the JQI; AFOSR MURI
FX I am grateful to N Graham for useful discussions regarding spheroidal
functions, and to R L Jaffe for his unpublished notes on multiple
reflections with capacitance matrices. I also acknowledge useful
correspondence with H J Schnitzer. This work was supported by the NSF
PIF, AFOSR, ARO, ARL, NSF PFC at the JQI, and AFOSR MURI.
NR 60
TC 0
Z9 0
U1 1
U2 1
PU IOP PUBLISHING LTD
PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 1742-5468
J9 J STAT MECH-THEORY E
JI J. Stat. Mech.-Theory Exp.
PD APR
PY 2016
AR 043102
DI 10.1088/1742-5468/2016/04/043102
PG 29
WC Mechanics; Physics, Mathematical
SC Mechanics; Physics
GA DL5VO
UT WOS:000375705300002
ER
PT J
AU Hodyss, D
Satterfield, E
McLay, J
Hamill, TM
Scheuerer, M
AF Hodyss, Daniel
Satterfield, Elizabeth
McLay, Justin
Hamill, Thomas M.
Scheuerer, Michael
TI Inaccuracies with Multimodel Postprocessing Methods Involving Weighted,
Regression-Corrected Forecasts
SO MONTHLY WEATHER REVIEW
LA English
DT Article
ID SURFACE-TEMPERATURE FORECASTS; PREDICTION SYSTEM; PROBABILISTIC
FORECASTS; ENSEMBLES; SCHEMES
AB Ensemble postprocessing is frequently applied to correct biases and deficiencies in the spread of ensemble forecasts. Methods involving weighted, regression-corrected forecasts address the typical biases and under-dispersion of ensembles through a regression correction of ensemble members followed by the generation of a probability density function (PDF) from the weighted sum of kernels fit around each corrected member. The weighting step accounts for the situation where the ensemble is constructed from different model forecasts or generated in some way that creates ensemble members that do not represent equally likely states. In the present work, it is shown that an overweighting of climatology in weighted, regression-corrected forecasts can occur when one first performs a regression-based correction before weighting each member. This overweighting of climatology results in an increase in the mean-squared error of the mean of the predicted PDF. The overweighting of climatology is illustrated in a simulation study and a real-data study, where the reference is generated through a direct application of Bayes's rule. The real-data example is a comparison of a particular method referred to as Bayesian model averaging (BMA) and a direct application of Bayes's rule for ocean wave heights using U.S. Navy and National Weather Service global deterministic forecasts. This direct application of Bayes's rule is shown to not overweight climatology and may be a low-cost replacement for the generally more expensive weighted, regression-correction methods.
C1 [Hodyss, Daniel; Satterfield, Elizabeth; McLay, Justin] Naval Res Lab, Monterey, CA 93943 USA.
[Hamill, Thomas M.] NOAA, Div Phys Sci, Earth Syst Res Lab, Boulder, CO USA.
[Scheuerer, Michael] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
RP Hodyss, D (reprint author), Naval Res Lab, Marine Meteorol Div, 7 Grace Hopper Ave,Stop 2, Monterey, CA 93943 USA.
EM daniel.hodyss@nrlmry.navy.mil
RI Scheuerer, Michael/D-5472-2015
OI Scheuerer, Michael/0000-0003-4540-9478
FU NRL Base Program [PE 0601153N]
FX This research is supported by the Chief of Naval Research through the
NRL Base Program, PE 0601153N. We thank three anonymous reviewers for
very conscientious critiques that have helped us greatly improve the
manuscript.
NR 33
TC 1
Z9 1
U1 6
U2 7
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0027-0644
EI 1520-0493
J9 MON WEATHER REV
JI Mon. Weather Rev.
PD APR
PY 2016
VL 144
IS 4
BP 1649
EP 1668
DI 10.1175/MWR-D-15-0204.1
PG 20
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DM1RY
UT WOS:000376125100001
ER
PT J
AU Benjamin, SG
Weygandt, SS
Brown, JM
Hu, M
Alexander, CR
Smirnova, TG
Olson, JB
James, EP
Dowell, DC
Grell, GA
Lin, HD
Peckham, SE
Smith, TL
Moninger, WR
Kenyon, JS
Manikin, GS
AF Benjamin, Stanley G.
Weygandt, Stephen S.
Brown, John M.
Hu, Ming
Alexander, Curtis R.
Smirnova, Tatiana G.
Olson, Joseph B.
James, Eric P.
Dowell, David C.
Grell, Georg A.
Lin, Haidao
Peckham, Steven E.
Smith, Tracy Lorraine
Moninger, William R.
Kenyon, Jaymes S.
Manikin, Geoffrey S.
TI A North American Hourly Assimilation and Model Forecast Cycle: The Rapid
Refresh
SO MONTHLY WEATHER REVIEW
LA English
DT Article
ID TURBULENCE CLOSURE-MODEL; ATMOSPHERIC BOUNDARY-LAYER; STABLY STRATIFIED
FLOWS; LARGE-EDDY SIMULATION; CASES-97 OBSERVATIONS; VARIATIONAL
ANALYSIS; EXPLICIT FORECASTS; WEATHER PREDICTION; COORDINATE MODEL;
DIURNAL-CYCLE
AB The Rapid Refresh (RAP), an hourly updated assimilation and model forecast system, replaced the Rapid Update Cycle (RUC) as an operational regional analysis and forecast system among the suite of models at the NOAA/National Centers for Environmental Prediction (NCEP) in 2012. The need for an effective hourly updated assimilation and modeling system for the United States for situational awareness and related decision-making has continued to increase for various applications including aviation (and transportation in general), severe weather, and energy. The RAP is distinct from the previous RUC in three primary aspects: a larger geographical domain (covering North America), use of the community-based Advanced Research version of the Weather Research and Forecasting (WRF) Model (ARW) replacing the RUC forecast model, and use of the Gridpoint Statistical Interpolation analysis system (GSI) instead of the RUC three-dimensional variational data assimilation (3DVar). As part of the RAP development, modifications have been made to the community ARW model (especially in model physics) and GSI assimilation systems, some based on previous model and assimilation design innovations developed initially with the RUC. Upper-air comparison is included for forecast verification against both rawinsondes and aircraft reports, the latter allowing hourly verification. In general, the RAP produces superior forecasts to those from the RUC, and its skill has continued to increase from 2012 up to RAP version 3 as of 2015. In addition, the RAP can improve on persistence forecasts for the 1-3-h forecast range for surface, upper-air, and ceiling forecasts.
C1 [Benjamin, Stanley G.; Weygandt, Stephen S.; Brown, John M.; Hu, Ming; Alexander, Curtis R.; Smirnova, Tatiana G.; Olson, Joseph B.; James, Eric P.; Dowell, David C.; Grell, Georg A.; Lin, Haidao; Peckham, Steven E.; Smith, Tracy Lorraine; Moninger, William R.; Kenyon, Jaymes S.] NOAA, Earth Syst Res Lab, R GSD1,325 Broadway, Boulder, CO 80305 USA.
[Manikin, Geoffrey S.] NOAA, NWS, NCEP, Environm Modeling Ctr, College Pk, MD USA.
[Hu, Ming; Alexander, Curtis R.; Smirnova, Tatiana G.; Olson, Joseph B.; James, Eric P.; Peckham, Steven E.; Moninger, William R.; Kenyon, Jaymes S.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Lin, Haidao; Smith, Tracy Lorraine] Colorado State Univ, Cooperat Inst Res Atmosphere, Ft Collins, CO 80523 USA.
RP Benjamin, SG (reprint author), NOAA, Earth Syst Res Lab, R GSD1,325 Broadway, Boulder, CO 80305 USA.
EM stan.benjamin@noaa.gov
RI Benjamin, Stan/C-5818-2015
OI Benjamin, Stan/0000-0002-5751-8236
FU NOAA; Federal Aviation Administration (FAA); Department of Energy
FX The RAP was developed under significant support from NOAA, the Federal
Aviation Administration (FAA), and the Department of Energy. We thank
Isidora Jankov, Hongli Jiang, and John Osborn of NOAA/ESRL for helpful
reviews. We also thank three anonymous reviewers and the journal editor
for extremely thorough and very thoughtful reviews of the manuscript.
NR 66
TC 17
Z9 17
U1 2
U2 2
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0027-0644
EI 1520-0493
J9 MON WEATHER REV
JI Mon. Weather Rev.
PD APR
PY 2016
VL 144
IS 4
BP 1669
EP 1694
DI 10.1175/MWR-D-15-0242.1
PG 26
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DM1RY
UT WOS:000376125100002
ER
PT J
AU Sakaeda, N
Roundy, PE
AF Sakaeda, Naoko
Roundy, Paul E.
TI The intraseasonal atmospheric angular momentum associated with MJO
convective initiations
SO QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY
LA English
DT Article
DE Madden-Julian oscillation; atmospheric angular momentum; momentum
budget; intraseasonal convective initiation
ID MADDEN-JULIAN OSCILLATION; VARYING BASIC STATE; VERTICAL STRUCTURE;
CIRCULATION; PROPAGATION; VARIABILITY; TROPICS; 40-DAY; MODEL; FLOW
AB The first part of this study examines the driving mechanisms of the equatorial intraseasonal relative atmospheric angular momentum (AAM) and its dynamical relationship to the upper-tropospheric zonal wind over the Western Hemisphere (WH) during the convective initiation of the Madden-Julian Oscillation (MJO) over the Indian Ocean. The budget analysis shows that the main driver of the equatorial intraseasonal AAM anomaly is the meridional transport of momentum induced by the modulation of the background subtropical eddies by the intraseasonal eddies. While the subtropical eddies over the central Pacific basin partly drive the equatorial AAM by meridionally transporting the momentum, the equatorial zonal wind associated with the same subtropical eddies is zonally advected and locally amplified over the east Pacific and Atlantic basins. The common source phenomena that transport momentum result in simultaneous evolution of the WH upper-tropospheric zonal wind and the AAM on intraseasonal time-scales, but their main driving mechanisms are different. The second part of the study investigates the influence of the equatorial intraseasonal AAM state on the subsequent development of initiating MJO convection over the Indian Ocean. In the presence of the WH upper-tropospheric easterly wind, MJO convection tends to develop a stronger enhanced convective envelope when the initiation occurs during the negative intraseasonal AAM state, which strengthens and extends the upper-tropospheric easterly wind in the WH. When the AAM anomaly is positive, it tends to induce stronger mid-tropospheric convergence above the region of convective initiation, thereby suppressing the lower-tropospheric updraught and suppressing the further growth of convection. The results show that the combined effects of the WH circumnavigating circulation and the AAM can influence the subsequent development of MJO convection over the Indian Ocean.
C1 [Sakaeda, Naoko] NOAA, Earth Syst Res Lab, Div Phys Sci, 325 Broadway, Boulder, CO 80305 USA.
[Roundy, Paul E.] SUNY Albany, Dept Atmospher & Environm Sci, Albany, NY USA.
RP Sakaeda, N (reprint author), NOAA, Earth Syst Res Lab, Div Phys Sci, 325 Broadway, Boulder, CO 80305 USA.
EM naoko.sakaeda@noaa.gov
FU NSF [AGS1358214, AGS1128779]
FX We thank two anomalous reviewers for their helpful comments. This work
was supported by NSF grant numbers AGS1358214 and AGS1128779.
NR 50
TC 1
Z9 1
U1 3
U2 3
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0035-9009
EI 1477-870X
J9 Q J ROY METEOR SOC
JI Q. J. R. Meteorol. Soc.
PD APR
PY 2016
VL 142
IS 696
BP 1371
EP 1384
DI 10.1002/qj.2740
PN A
PG 14
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DL9BF
UT WOS:000375935600016
ER
PT J
AU Butler, AH
Arribas, A
Athanassiadou, M
Baehr, J
Calvo, N
Charlton-Perez, A
Deque, M
Domeisen, DIV
Frohlich, K
Hendon, H
Imada, Y
Ishii, M
Iza, M
Karpechko, AY
Kumar, A
MacLachlan, C
Merryfield, WJ
Muller, WA
O'Neill, A
Scaife, AA
Scinocca, J
Sigmond, M
Stockdale, TN
Yasuda, T
AF Butler, Amy H.
Arribas, Alberto
Athanassiadou, Maria
Baehr, Johanna
Calvo, Natalia
Charlton-Perez, Andrew
Deque, Michel
Domeisen, Daniela I. V.
Froehlich, Kristina
Hendon, Harry
Imada, Yukiko
Ishii, Masayoshi
Iza, Maddalen
Karpechko, Alexey Yu.
Kumar, Arun
MacLachlan, Craig
Merryfield, William J.
Mueller, Wolfgang A.
O'Neill, Alan
Scaife, Adam A.
Scinocca, John
Sigmond, Michael
Stockdale, Timothy N.
Yasuda, Tamaki
TI The Climate-system Historical Forecast Project: do
stratosphere-resolving models make better seasonal climate predictions
in boreal winter?
SO QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY
LA English
DT Article
DE seasonal prediction; stratosphere-troposphere coupling; stratosphere; El
Nino/Southern Oscillation; Quasi-Biennial Oscillation; North Atlantic
Oscillation
ID QUASI-BIENNIAL OSCILLATION; NORTH-ATLANTIC OSCILLATION; LOW-TOP
VERSIONS; CMIP5 MODELS; EL-NINO; ARCTIC OSCILLATION; HEMISPHERE WINTER;
GRAVITY-WAVES; SKILL; PREDICTABILITY
AB Using an international, multi-model suite of historical forecasts from the World Climate Research Programme (WCRP) Climate-system Historical Forecast Project (CHFP), we compare the seasonal prediction skill in boreal wintertime between models that resolve the stratosphere and its dynamics (high-top') and models that do not (low-top'). We evaluate hindcasts that are initialized in November, and examine the model biases in the stratosphere and how they relate to boreal wintertime (December-March) seasonal forecast skill. We are unable to detect more skill in the high-top ensemble-mean than the low-top ensemble-mean in forecasting the wintertime North Atlantic Oscillation, but model performance varies widely. Increasing the ensemble size clearly increases the skill for a given model. We then examine two major processes involving stratosphere-troposphere interactions (the El Nino/Southern Oscillation (ENSO) and the Quasi-Biennial Oscillation (QBO)) and how they relate to predictive skill on intraseasonal to seasonal time-scales, particularly over the North Atlantic and Eurasia regions. High-top models tend to have a more realistic stratospheric response to El Nino and the QBO compared to low-top models. Enhanced conditional wintertime skill over high latitudes and the North Atlantic region during winters with El Nino conditions suggests a possible role for a stratospheric pathway.
C1 [Butler, Amy H.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Butler, Amy H.] NOAA, ESRL, CSD, 325 Broadway, Boulder, CO 80305 USA.
[Arribas, Alberto; Athanassiadou, Maria; MacLachlan, Craig; Scaife, Adam A.] Hadley Ctr, Met Off, Exeter, Devon, England.
[Baehr, Johanna] Univ Hamburg, Ctr Earth Syst Res & Sustainabil CEN, Inst Oceanog, Hamburg, Germany.
[Calvo, Natalia; Iza, Maddalen] Univ Complutense Madrid, Fac Ciencias Fis, Dept Fis Tierra 2, E-28040 Madrid, Spain.
[Charlton-Perez, Andrew; O'Neill, Alan] Univ Reading, Dept Meteorol, Reading RG6 2AH, Berks, England.
[Deque, Michel] CNRS GAME, Meteo France Ctr Natl Rech Meteorol, Toulouse, France.
[Domeisen, Daniela I. V.] Univ Kiel, GEOMAR Helmholtz Ctr Ocean Res Kiel, Kiel, Germany.
[Froehlich, Kristina] Deutsch Wetterdienst DWD, Offenbach, Germany.
[Hendon, Harry] Bur Meteorol, Melbourne, Vic, Australia.
[Imada, Yukiko; Ishii, Masayoshi] Japan Meteorol Agcy, Meteorol Res Inst, Ibaraki, Japan.
[Karpechko, Alexey Yu.] Finnish Meteorol Inst, FIN-00101 Helsinki, Finland.
[Kumar, Arun] NOAA, Natl Weather Serv, Climate Predict Ctr, College Pk, MD USA.
[Merryfield, William J.; Scinocca, John; Sigmond, Michael] Environm Canada, Canadian Ctr Climate Modelling & Anal, Victoria, BC, Canada.
[Mueller, Wolfgang A.] Max Planck Inst Meteorol, Bundesstr 55, D-20146 Hamburg, Germany.
[Stockdale, Timothy N.] European Ctr Medium Range Weather Forecasts, Shinfield Pk, Reading RG2 9AX, Berks, England.
[Yasuda, Tamaki] Japan Meteorol Agcy, Tokyo, Japan.
RP Butler, AH (reprint author), NOAA, ESRL, CSD, 325 Broadway, Boulder, CO 80305 USA.
EM amy.butler@noaa.gov
RI Butler, Amy/K-6190-2012; Manager, CSD Publications/B-2789-2015; Sigmond,
Michael /K-3169-2012;
OI Butler, Amy/0000-0002-3632-0925; Sigmond, Michael /0000-0003-2191-9756;
IZA, MADDALEN/0000-0002-6162-5501; Domeisen, Daniela/0000-0002-1463-929X
FU Academy of Finland [286298]
FX We acknowledge the WCRP/CLIVAR Working Group on Seasonal to Interannual
Prediction (WGSIP) for establishing the Climate-system Historical
Forecast Project (CHFP: Kirtman and Pirani, 2009) and the Centro de
Investigaciones del Mar y la Atmosfera (CIMA) for providing the model
output. We also thank the data providers for making the model output
available through CHFP. We have no potential sources of conflict of
interest. The contribution of AYK is funded by the Academy of Finland,
project no. 286298.
NR 91
TC 6
Z9 6
U1 11
U2 24
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0035-9009
EI 1477-870X
J9 Q J ROY METEOR SOC
JI Q. J. R. Meteorol. Soc.
PD APR
PY 2016
VL 142
IS 696
BP 1413
EP 1427
DI 10.1002/qj.2743
PN A
PG 15
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DL9BF
UT WOS:000375935600019
ER
PT J
AU Bernier, NB
Alves, JHGM
Tolman, H
Chawla, A
Peel, S
Pouliot, B
Belanger, JM
Pellerin, P
Lepine, M
Roch, M
AF Bernier, Natacha B.
Alves, Jose-Henrique G. M.
Tolman, Hendrik
Chawla, Arun
Peel, Syd
Pouliot, Benoit
Belanger, Jean-Marc
Pellerin, Pierre
Lepine, Mario
Roch, Michel
TI Operational Wave Prediction System at Environment Canada: Going Global
to Improve Regional Forecast Skill
SO WEATHER AND FORECASTING
LA English
DT Article
ID MULTISCALE GEM MODEL; VARIATIONAL DATA ASSIMILATION; PART I; BUOY DATA;
IMPLEMENTATION; SWELL
AB A global deterministic wave prediction system (GDWPS) is used to improve regional forecasts of waves off the Canadian coastline and help support the practice of safe marine activities in Canadian waters. The wave model has a grid spacing of 1/4 degrees with spectral resolution of 36 frequency bins and 36 directional bins. The wave model is driven with hourly 10-m winds generated by the operational global atmospheric prediction system. Ice conditions are updated every three hours using the ice concentration forecasts generated by the Global Ice-Ocean Prediction System. Wave forecasts are evaluated over two periods from 15 August to 31 October 2014 and from 15 December 2014 to 28 February 2015, as well as over select cases during the fall of 2012. The global system is shown to improve wave forecast skill over regions where forecasts were previously produced using limited-area models only. The usefulness of a global expansion is demonstrated for large swell events affecting the northeast Pacific. The first validation of a Canadian operational wave forecast system in the Arctic is presented. Improvements in the representation of forecast wave fields associated with tropical cyclones are also demonstrated. Finally, the GDWPS is shown to result in gains of at least 12 h of lead time.
C1 [Bernier, Natacha B.; Peel, Syd; Pouliot, Benoit; Belanger, Jean-Marc; Pellerin, Pierre; Roch, Michel] Environm Canada, Rech Previs Numer Environm, 2121 Route Trans Canadienne, Dorval, PQ H9P 1J3, Canada.
[Alves, Jose-Henrique G. M.; Tolman, Hendrik; Chawla, Arun] NOAA, Ctr Weather & Climate Predict, College Pk, MD USA.
[Lepine, Mario] Environm Canada, Serv Informat Rech, Dorval, PQ, Canada.
RP Bernier, NB (reprint author), Environm Canada, Rech Previs Numer Environm, 2121 Route Trans Canadienne, Dorval, PQ H9P 1J3, Canada.
EM natacha.bernier@ec.gc.ca
FU PERD [B11.001]; SARNif [SN201222]
FX The authors thank reviewers whose comments were very valuable. NBB also
thanks PERD B11.001 and SARNif SN201222 for financial support.
NR 46
TC 2
Z9 2
U1 1
U2 5
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0882-8156
EI 1520-0434
J9 WEATHER FORECAST
JI Weather Forecast.
PD APR
PY 2016
VL 31
IS 2
BP 353
EP 370
DI 10.1175/WAF-D-15-0087.1
PG 18
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DM2ZJ
UT WOS:000376216300001
ER
PT J
AU Nelson, BR
Prat, OP
Seo, DJ
Habib, E
AF Nelson, Brian R.
Prat, Olivier P.
Seo, D. -J.
Habib, Emad
TI Assessment and Implications of NCEP Stage IV Quantitative Precipitation
Estimates for Product Intercomparisons
SO WEATHER AND FORECASTING
LA English
DT Article
ID SOUTHEASTERN UNITED-STATES; OBJECT-BASED VERIFICATION; RAIN-GAUGE DATA;
TROPICAL CYCLONES; WSR-88D DATA; RIVER-BASIN; PART II; SATELLITE; RADAR;
FORECASTS
AB The National Centers for Environmental Prediction (NCEP) stage IV quantitative precipitation estimates (QPEs) are used in many studies for intercomparisons including those for satellite QPEs. An overview of the National Weather Service precipitation processing system is provided here so as to set the stage IV product in context and to provide users with some knowledge as to how it is developed. Then, an assessment of the stage IV product over the period 2002-12 is provided. The assessment shows that the stage IV product can be useful for conditional comparisons of moderate-to-heavy rainfall for select seasons and locations. When evaluating the product at the daily scale, there are many discontinuities due to the operational processing at the radar site as well as discontinuities due to the merging of data from different River Forecast Centers (RFCs) that use much different processing algorithms for generating their precipitation estimates. An assessment of the daily precipitation estimates is provided based on the cumulative distribution function for all of the daily estimates for each RFC by season. In addition it is found that the hourly estimates at certain RFCs suffer from lack of manual quality control and caution should be used.
C1 [Nelson, Brian R.; Prat, Olivier P.] NOAA, Natl Ctr Environm Informat, 151 Patton Ave, Asheville, NC 28801 USA.
[Prat, Olivier P.] N Carolina State Univ, Cooperat Inst Climate & Satellites, Asheville, NC USA.
[Seo, D. -J.] Univ Texas Arlington, Arlington, TX 76019 USA.
[Habib, Emad] Univ Louisiana Lafayette, Lafayette, LA 70504 USA.
RP Nelson, BR (reprint author), NOAA, Natl Ctr Environm Informat, 151 Patton Ave, Asheville, NC 28801 USA.
EM brian.nelson@noaa.gov
RI Prat, Olivier/B-7016-2009; Nelson, Brian/D-6432-2014
OI Prat, Olivier/0000-0002-9289-5723;
FU NOAA through the Cooperative Institute for Climate and Satellites-North
Carolina [NA14NES432003]
FX The second author is supported by NOAA through the Cooperative Institute
for Climate and Satellites-North Carolina under Cooperative Agreement
NA14NES432003. In addition the authors would like to express their
gratitude to the reviewers for the in-depth reviews.
NR 68
TC 1
Z9 1
U1 5
U2 6
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0882-8156
EI 1520-0434
J9 WEATHER FORECAST
JI Weather Forecast.
PD APR
PY 2016
VL 31
IS 2
BP 371
EP 394
DI 10.1175/WAF-D-14-00112.1
PG 24
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DM2ZJ
UT WOS:000376216300002
ER
PT J
AU Line, WE
Schmit, TJ
Lindsey, DT
Goodman, SJ
AF Line, William E.
Schmit, Timothy J.
Lindsey, Daniel T.
Goodman, Steven J.
TI Use of Geostationary Super Rapid Scan Satellite Imagery by the Storm
Prediction Center
SO WEATHER AND FORECASTING
LA English
DT Article
ID GOES-R; INITIATION
AB The Geostationary Operational Environmental Satellite-14 (GOES-14) Imager was operated by the National Oceanic and Atmospheric Administration (NOAA) in an experimental rapid scan 1-min mode during parts of 2012, 2013, 2014, and 2015. This scan mode, known as the Super Rapid Scan Operations for GOES-R (SRSOR), emulates the high-temporal-resolution sampling that will be provided by the Advanced Baseline Imager on the next-generation GOES-R series. NOAA/National Weather Service/Storm Prediction Center (SPC) forecasters utilized the 1-min imagery extensively in operations when available over convectively active regions. They found it provided them with unique insight into relevant features and processes before, during, and after convective initiation. This paper introduces how the SRSOR datasets from GOES-14 were used by SPC forecasters and how these data are likely to be applied when available operationally from GOES-R. Several animations, included as supplemental material, showcase the rapid change of severe weather related phenomena observed during the 2014 and 2015 SRSOR campaigns from the GOES-14 Imager.
C1 [Line, William E.] Univ Oklahoma, Cooperat Inst Mesoscale Meteorol Studies, Norman, OK 73019 USA.
[Line, William E.] NOAA, NWS, NCEP, Storm Predict Ctr, 120 David L Boren Blvd, Norman, OK 73072 USA.
[Schmit, Timothy J.] NOAA, NESDIS, Ctr Satellite Applicat & Res, Adv Satellite Prod Branch, Madison, WI USA.
[Lindsey, Daniel T.] NOAA, NESDIS, Ctr Satellite Applicat & Res, Reg & Mesoscale Meteorol Branch, Ft Collins, CO USA.
[Goodman, Steven J.] NOAA, NESDIS, GOES R Program Off, Greenbelt, MD USA.
RP Line, WE (reprint author), NOAA, NWS, NCEP, Storm Predict Ctr, 120 David L Boren Blvd, Norman, OK 73072 USA.
EM bill.line@noaa.gov
RI Schmit, Timothy/F-5624-2010; Lindsey, Dan/F-5607-2010
OI Lindsey, Dan/0000-0002-0967-5683
FU NOAA/Office of Oceanic and Atmospheric Research under NOAA-University of
Oklahoma [NA11OAR4320072]; U.S. Department of Commerce
FX More information about the GOES-R series can be found online
(http://www.goes-r.gov). More information about the SRSOR campaigns in
2012, 2013 2014, and 2015 is also available online
(http://cimss.ssec.wisc.edu/goes/srsor/overview_training.html).
Additional information on many of these cases can be found in the CIMSS
Satellite blog, under the GOES-14 category
(http://cimss.ssec.wisc.edu/goes/blog/archives/category/goes-14) and in
the Satellite Liaison blog, under the SPC category
(https://satelliteliaisonblog.wordpress.com/category/spc/). Thanks are
given to NOAA/NESDIS for the operation of GOES-14 in the SRSOR mode; to
CIRA/NESDIS/RAMMB, the SSEC Data Center, and NOAA CLASS for ingesting,
delivering, and archiving the data; and to the SPC forecasters for
providing detailed feedback on their use of the GOES-14 SRSOR data in
SPC operations. Thanks are also given to Robert Rabin (National Severe
Storms Laboratory), Israel Jirak (NOAA/NWS/NCEP/SPC), and Steven Weiss
(NOAA/NWS/NCEP/SPC). Funding was provided by the NOAA/Office of Oceanic
and Atmospheric Research under NOAA-University of Oklahoma Cooperative
Agreement NA11OAR4320072, U.S. Department of Commerce. The views,
opinions, and findings contained in this report 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.
NR 21
TC 2
Z9 2
U1 4
U2 6
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0882-8156
EI 1520-0434
J9 WEATHER FORECAST
JI Weather Forecast.
PD APR
PY 2016
VL 31
IS 2
BP 483
EP 494
DI 10.1175/WAF-D-15-0135.1
PG 12
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DM2ZJ
UT WOS:000376216300008
ER
PT J
AU Garraffo, ZD
Kim, HC
Mehra, A
Spindler, T
Rivin, I
Tolman, HL
AF Garraffo, Zulema D.
Kim, Hae-Cheol
Mehra, Avichal
Spindler, Todd
Rivin, Ilya
Tolman, Hendrik L.
TI Modeling of Cs-137 as a Tracer in a Regional Model for the Western
Pacific, after the Fukushima-Daiichi Nuclear Power Plant Accident of
March 2011
SO WEATHER AND FORECASTING
LA English
DT Article
ID DAI-ICHI; OCEAN MODEL; INTERMEDIATE WATER; VERTICAL COORDINATE; DATA
ASSIMILATION; KUROSHIO; CIRCULATION; DISPERSION; SYSTEM; TRANSPORT
AB In this study, results are presented from the first operational ocean tracer dispersion model operated by the National Oceanic and Atmospheric Administration/National Weather Service/National Centers for Environmental Prediction (NOAA/NWS/NCEP). This study addresses the dispersion of radionuclide contaminants after the Fukushima-Daiichi nuclear accident that was triggered by the 11 March 2011 earthquake and tsunami. The tracer capabilities of the Hybrid Coordinate Ocean Model (HYCOM) were used in a regional domain for the northwestern Pacific, with nesting lateral boundary conditions using daily nowcast-forecast fields from the global operational Real-Time Ocean Forecast System (RTOFS-Global), a 1/12 degrees HYCOM global forecast from NCEP, based on data-assimilative 1/12 degrees HYCOM Global Ocean Forecast System (GOFS) analyses from the Naval Research Laboratory/Naval Oceanographic Office (NRL/NAVOCEANO). This regional model, RTOFS Episodic Tracers for a region of the North West Pacific (RTOFS-ET_WPA), was in operation until the beginning of 2014, when the simulated Cs-137 concentration was very close to the background level in the Pacific before the accident, which was about 2 Becquerel m(-3) [Bq; 1 Becquerel = 1 (nuclear decay) s(-1)].
C1 [Garraffo, Zulema D.; Kim, Hae-Cheol; Spindler, Todd; Rivin, Ilya] NOAA, NCEP, IMSG, Environm Modeling Ctr, 5830 Univ Res Ct, College Pk, MD 20740 USA.
[Mehra, Avichal; Tolman, Hendrik L.] NOAA, NCEP, Environm Modeling Ctr, 5830 Univ Res Ct, College Pk, MD 20740 USA.
RP Garraffo, ZD (reprint author), NOAA, NCEP, IMSG, Environm Modeling Ctr, 5830 Univ Res Ct, College Pk, MD 20740 USA.
EM zulema.garraffo@noaa.gov
NR 53
TC 1
Z9 1
U1 4
U2 4
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0882-8156
EI 1520-0434
J9 WEATHER FORECAST
JI Weather Forecast.
PD APR
PY 2016
VL 31
IS 2
BP 553
EP 579
DI 10.1175/WAF-D-13-00101.1
PG 27
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DM2ZJ
UT WOS:000376216300012
ER
PT J
AU Kossin, JP
DeMaria, M
AF Kossin, James P.
DeMaria, Mark
TI Reducing Operational Hurricane Intensity Forecast Errors during Eyewall
Replacement Cycles
SO WEATHER AND FORECASTING
LA English
DT Article
AB Eyewall replacement cycles (ERCs) are fairly common events in tropical cyclones (TCs) of hurricane intensity or greater and typically cause large and sometimes rapid changes in the intensity evolution of the TC. Although the details of the intensity evolution associated with ERCs appear to have some dependence on the ambient environmental conditions that the TCs move through, these dependencies can also be quite different than those of TCs that are not undergoing an ERC. For example, the Statistical Hurricane Prediction Scheme (SHIPS), which is used in National Hurricane Center operations and provides intensity forecast skill that is, on average, equal to or greater than deterministic numerical model skill, typically identifies an environment that is not indicative of weakening during the onset and subsequent evolution of an ERC. Contrarily, a period of substantial weakening does typically begin near the onset of an ERC, and this disparity can cause large SHIPS intensity forecast errors. Here, a simple model based on a climatology of ERC intensity change is introduced and tested against SHIPS. It is found that the application of the model can reduce intensity forecast error substantially when applied at, or shortly after, the onset of ERC weakening.
C1 [Kossin, James P.] NOAA, Natl Ctr Environm Informat, Ctr Weather & Climate, Asheville, NC USA.
[DeMaria, Mark] NOAA, Natl Hurricane Ctr, Miami, FL USA.
RP Kossin, JP (reprint author), NOAA, Cooperat Inst Meteorol Satellite Studies, 1225 W Dayton St, Madison, WI 53706 USA.
EM james.kossin@noaa.gov
RI Kossin, James/C-2022-2016
OI Kossin, James/0000-0003-0461-9794
FU Joint Hurricane Testbed Project within NOAA's U.S. Weather Research
Program (USWRP)
FX Funding and support for the development of this statistical intensity
forecast model was provided by the Joint Hurricane Testbed Project
within NOAA's U.S. Weather Research Program (USWRP). We are especially
grateful to Chris Landsea and a number of National Hurricane Center
specialists for their input and guidance.
NR 12
TC 0
Z9 0
U1 1
U2 1
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0882-8156
EI 1520-0434
J9 WEATHER FORECAST
JI Weather Forecast.
PD APR
PY 2016
VL 31
IS 2
BP 601
EP 608
DI 10.1175/WAF-D-15-0123.1
PG 8
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DM2ZJ
UT WOS:000376216300014
ER
PT J
AU Benjamin, SG
Brown, JM
Smirnova, TG
AF Benjamin, Stanley G.
Brown, John M.
Smirnova, Tatiana G.
TI Explicit Precipitation-Type Diagnosis from a Model Using a Mixed-Phase
Bulk Cloud-Precipitation Microphysics Parameterization
SO WEATHER AND FORECASTING
LA English
DT Article
ID WINTER PRECIPITATION; OPERATIONAL SYSTEM; OBJECTIVE USE; FORECASTS
AB The Rapid Refresh (RAP) and High-Resolution Rapid Refresh (HRRR), both operational at NOAA's National Centers for Environmental Prediction (NCEP) use the Thompson et al. mixed-phase bulk cloud microphysics scheme. This scheme permits predicted surface precipitation to simultaneously consist of rain, snow, and graupel at the same location under certain conditions. Here, the explicit precipitation-type diagnostic method is described as used in conjunction with the Thompson et al. scheme in the RAP and HRRR models. The postprocessing logic combines the explicitly predicted multispecies hydrometeor data and other information from the model forecasts to produce fields of surface precipitation type that distinguish between rain and freezing rain, and to also portray areas of mixed precipitation. This explicit precipitation-type diagnostic method is used with the NOAA operational RAP and HRRR models. Verification from two winter seasons from 2013 to 2015 is provided against METAR surface observations. An example of this product from a January 2015 south-central United States winter storm is also shown.
C1 [Benjamin, Stanley G.; Brown, John M.; Smirnova, Tatiana G.] NOAA, ESRL, R GSD1,325 Broadway, Boulder, CO 80305 USA.
RP Smirnova, TG (reprint author), NOAA, ESRL, R GSD1,325 Broadway, Boulder, CO 80305 USA.
EM stan.benjamin@noaa.gov
RI Benjamin, Stan/C-5818-2015
OI Benjamin, Stan/0000-0002-5751-8236
FU Federal Aviation Administration
FX We thank Joseph Koval at The Weather Company and Kyoko Ikeda and her
NCAR colleagues for their help in identifying problems with the
precipitation-type diagnosis that led to improvements in the scheme now
documented in this article. We also thank Greg Thompson at the National
Center for Atmospheric Research for ongoing collaboration, and
colleagues at NOAA/ESRL, especially Curtis Alexander and Brian Jamison,
for their help on evaluation of the precipitation type algorithm
described here. We thank Kim Elmore and his colleagues at NSSL for
prompting identification of need for the IP criterion resetting. Ongoing
changes in the precipitation-type diagnostic described in this paper are
tracked online (http://ruc.noaa.gov/rr/RAP_var_diagnosis.html#ptype).
Finally, we thank Trevor Alcott, David Dowell, and John Osborn
(NOAA/ESRL) for very helpful reviews. The Federal Aviation
Administration has partially supported some of this work.
NR 24
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U1 1
U2 2
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0882-8156
EI 1520-0434
J9 WEATHER FORECAST
JI Weather Forecast.
PD APR
PY 2016
VL 31
IS 2
BP 609
EP 619
DI 10.1175/WAF-D-15-0136.1
PG 11
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DM2ZJ
UT WOS:000376216300015
ER
PT J
AU Iyer, ER
Clark, AJ
Xue, M
Kong, FY
AF Iyer, Eswar R.
Clark, Adam J.
Xue, Ming
Kong, Fanyou
TI A Comparison of 36-60-h Precipitation Forecasts from Convection-Allowing
and Convection-Parameterizing Ensembles
SO WEATHER AND FORECASTING
LA English
DT Article
ID NUMERICAL WEATHER PREDICTION; ATMOSPHERIC BOUNDARY-LAYER; TURBULENCE
CLOSURE-MODEL; LARGE-EDDY SIMULATION; YAMADA LEVEL-3 MODEL; PART I;
HIGH-RESOLUTION; WRF MODEL; MICROPHYSICS PARAMETERIZATION; REGIONAL
PREDICTION
AB Previous studies examining convection-allowing models (CAMs), as well as NOAA/Hazardous Weather Testbed Spring Forecasting Experiments (SFEs) have typically emphasized "day 1" (12-36 h) forecast guidance. These studies find a distinct advantage in CAMs relative to models that parameterize convection, especially for fields strongly tied to convection like precipitation. During the 2014 SFE, "day 2" (36-60 h) forecast products from a CAM ensemble provided by the Center for Analysis and Prediction of Storms (CAPS) at the University of Oklahoma were examined. Quantitative precipitation forecasts (QPFs) from the CAPS ensemble, known as the Storm Scale Ensemble Forecast (SSEF) system, are compared to NCEP's operational Short Range Ensemble Forecast (SREF) system, which provides lateral boundary conditions for the SSEF, to see if the CAM ensemble outperforms the SREF through forecast hours 36-60. Equitable threat scores (ETSs) were computed for precipitation thresholds ranging from 0.10 to 0.75 in. for each SSEF and SREF member, as well as ensemble means, for 3-h accumulation periods. The ETS difference between the SSEF and SREF peaked during hours 36-42. Probabilistic forecasts were evaluated using the area under the receiver operating characteristic curve (ROC area). The SSEF had higher values of ROC area, especially at thresholds >= 0.50 in. Additionally, time longitude diagrams of diurnally averaged rainfall were constructed for each SSEF/SREF ensemble member. Spatial correlation coefficients between forecasts and observations in time longitude space indicated that the SSEF depicted the diurnal cycle much better than the SREF, which underforecasted precipitation with a peak that had a 3-h phase lag. A minority of SREF members performed well.
C1 [Iyer, Eswar R.; Xue, Ming] Univ Oklahoma, Sch Meteorol, 120 David L Boren Blvd, Norman, OK 73072 USA.
[Clark, Adam J.] Univ Oklahoma, Cooperat Inst Mesoscale Meteorol Studies, 120 David L Boren Blvd, Norman, OK 73072 USA.
[Iyer, Eswar R.; Clark, Adam J.] NOAA, Natl Severe Storms Lab, OAR, Norman, OK 73069 USA.
[Xue, Ming; Kong, Fanyou] Univ Oklahoma, Ctr Anal & Predict Storms, 120 David L Boren Blvd, Norman, OK 73072 USA.
RP Iyer, ER (reprint author), Univ Oklahoma, NWC, Sch Meteorol, 120 David L Boren Blvd, Norman, OK 73072 USA.
EM eswar.iyer@noaa.gov
RI Xue, Ming/F-8073-2011
OI Xue, Ming/0000-0003-1976-3238
FU NOAA/Office of Oceanic and Atmospheric Research under NOAA University of
Oklahoma, U.S. Department of Commerce [NA11OAR4320072]; NOAA
Collaborative Science, Technology, and Applied Research (CSTAR) program;
NSF [AGS-0802888]
FX This work was made possible by a Presidential Early Career Award for
Scientists and Engineers (PECASE). Additional support was provided by
NOAA/Office of Oceanic and Atmospheric Research under NOAA-University of
Oklahoma Cooperative Agreement NA11OAR4320072, U.S. Department of
Commerce. CAPS SSEF forecasts were supported by the NOAA Collaborative
Science, Technology, and Applied Research (CSTAR) program with
supplementary support from NSF Grant AGS-0802888, using computing
resources at the National Science Foundation XSEDE National Institute of
Computational Science (NICS) at the University of Tennessee.
NR 68
TC 1
Z9 1
U1 1
U2 1
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0882-8156
EI 1520-0434
J9 WEATHER FORECAST
JI Weather Forecast.
PD APR
PY 2016
VL 31
IS 2
BP 647
EP 661
DI 10.1175/WAF-D-15-0143.1
PG 15
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DM2ZJ
UT WOS:000376216300018
ER
PT J
AU Kalina, EA
Friedrich, K
Motta, BC
Deierling, W
Stano, GT
Rydell, NN
AF Kalina, Evan A.
Friedrich, Katja
Motta, Brian C.
Deierling, Wiebke
Stano, Geoffrey T.
Rydell, Nezette N.
TI Colorado Plowable Hailstorms: Synoptic Weather, Radar, and Lightning
Characteristics
SO WEATHER AND FORECASTING
LA English
DT Article
ID LINEAR-POLARIZATION RADAR; 24 JUNE 2006; POLARIMETRIC RADAR; CONVECTIVE
STORMS; HAIL GROWTH; PART II; HYDROMETEOR CLASSIFICATION; SOUTHWESTERN
FRANCE; 3-BODY SCATTERING; MAPPING ARRAY
AB Synoptic weather, S-band dual-polarization radar, and total lightning observations are analyzed from four thunderstorms that produced "plowable" hail accumulations of 15-60 cm in localized areas of the Colorado Front Range. Results indicate that moist, relatively slow (5-15 m s(-1)) southwesterly-to-westerly flow at 500 hPa and postfrontal low-level upslope flow, with 2-m dewpoint temperatures of 11 degrees-19 degrees C at 1200 LST, were present on each plowable hail day. This pattern resulted in column-integrated precipitable water values that were 132 %-184% of the monthly means and freezing-level heights that were 100-700 m higher than average. Radar data indicate that between one and three maxima in reflectivity Z (68-75 dBZ) and 50-dBZ echo-top height (11-15 km MSL) occurred over the lifetime of each hailstorm. These maxima, which imply an enhancement in updraft strength, resulted in increased graupel and hail production and accumulating hail at the surface within 30 min of the highest echo tops. The hail core had Z similar to 70 dBZ, differential reflectivity ZDR from 0 to -4 dB, and correlation coefficient rho(HV) of 0.80-0.95. Time-height plots reveal that these minima in ZDR and rho(HV) gradually descended to the surface after originating at heights of 6-10 km MSL similar to 15-60 min prior to accumulating hailfall. Hail accumulations estimated from the radar data pinpoint the times and locations of plowable hail, with depths greater than 5 cm collocated with the plowable hail reports. Three of the four hail events were accompanied by lightning flash rates near the maximum observed thus far within the thunderstorm.
C1 [Kalina, Evan A.] NOAA, Earth Syst Res Lab, Div Phys Sci, 325 Broadway St, Boulder, CO 80305 USA.
[Kalina, Evan A.] NOAA, Atlantic Oceanog & Meteorol Lab, Hurricane Res Div, Miami, FL 33149 USA.
[Friedrich, Katja] Univ Colorado, Dept Atmospher & Ocean Sci, Boulder, CO 80309 USA.
[Motta, Brian C.] NOAA, NWS, Off Chief Learning Officer Boulder, Boulder, CO USA.
[Deierling, Wiebke] Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA.
[Stano, Geoffrey T.] NASA, Shortterm Predict Res & Transit Ctr SPoRT ENSCO I, Huntsville, AL USA.
[Rydell, Nezette N.] NOAA, NWS, Boulder, CO USA.
RP Kalina, EA (reprint author), NOAA, Earth Syst Res Lab, Div Phys Sci, 325 Broadway St, Boulder, CO 80305 USA.
EM evan.kalina@noaa.gov
FU National Science Foundation [DGE-1144083]
FX We thank the employees of the National Weather Service Forecast Office
in Boulder for providing valuable feedback on this study. We also thank
Mike Dixon (NCAR) for his assistance in using the Radx C++ software
package for radar data processing, and Scott Ellis (NCAR) for his help
in using Solo II to view and edit the radar data. Feedback from three
anonymous reviewers greatly improved an earlier version of this
manuscript. This material is based upon work supported by the National
Science Foundation Graduate Research Fellowship program under
DGE-1144083. A portion of this research was performed while EAK held a
National Research Council Research Associateship Award at the Earth
System Research Laboratory and the Atlantic Oceanographic and
Meteorological Laboratory.
NR 87
TC 0
Z9 0
U1 10
U2 11
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0882-8156
EI 1520-0434
J9 WEATHER FORECAST
JI Weather Forecast.
PD APR
PY 2016
VL 31
IS 2
BP 663
EP 693
DI 10.1175/WAF-D-15-0037.1
PG 31
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DM2ZJ
UT WOS:000376216300019
ER
PT J
AU Van Houtan, KS
Francke, DL
Alessi, S
Jones, TT
Martin, SL
Kurpita, L
King, CS
Baird, RW
AF Van Houtan, Kyle S.
Francke, Devon L.
Alessi, Sarah
Jones, T. Todd
Martin, Summer L.
Kurpita, Lauren
King, Cheryl S.
Baird, Robin W.
TI The developmental biogeography of hawksbill sea turtles in the North
Pacific
SO ECOLOGY AND EVOLUTION
LA English
DT Article
DE Bycatch; coastal ecology; natal dispersal; ocean plastics; pollution;
spatial structure
ID ANTHROPOGENIC DEBRIS INGESTION; ERETMOCHELYS-IMBRICATA; CARETTA-CARETTA;
MARINE DEBRIS; HAWAIIAN-ISLANDS; LOGGERHEAD TURTLES; GREEN TURTLES;
HABITAT USE; LOST YEARS; STRANDINGS
AB High seas oceanic ecosystems are considered important habitat for juvenile sea turtles, yet much remains cryptic about this important life-history period. Recent progress on climate and fishery impacts in these so-called lost years is promising, but the developmental biogeography of hawksbill sea turtles (Eretmochelys imbricata) has not been widely described in the Pacific Ocean. This knowledge gap limits the effectiveness of conservation management for this globally endangered species. We address this with 30 years of stranding observations, 20 years of bycatch records, and recent simulations of natal dispersal trajectories in the Hawaiian Archipelago. We synthesize the analyses of these data in the context of direct empirical observations, anecdotal sightings, and historical commercial harvests from the insular Pacific. We find hawksbills 04 years of age, measuring 8-34 cm straight carapace length, are found predominantly in the coastal pelagic waters of Hawaii. Unlike other species, we find no direct evidence of a prolonged presence in oceanic habitats, yet satellite tracks of passive drifters (simulating natal dispersal) and our small sample sizes suggest that an oceanic phase for hawksbills cannot be dismissed. Importantly, despite over 600 million hooks deployed and nearly 6000 turtle interactions, longline fisheries have never recorded a single hawksbill take. We address whether the patterns we observe are due to population size and gear selectivity. Although most sea turtle species demonstrate clear patterns of oceanic development, hawksbills in the North Pacific may by contrast occupy a variety of ecosystems including coastal pelagic waters and shallow reefs in remote atolls. This focuses attention on hazards in these ecosystems - entanglement and ingestion of marine debris - and perhaps away from longline bycatch and decadal climate regimes that affect sea turtle development in oceanic regions.
C1 [Van Houtan, Kyle S.; Jones, T. Todd] Pacific Isl Fisheries Sci Ctr, NOAA Fisheries, Honolulu, HI 96818 USA.
[Van Houtan, Kyle S.] Duke Univ, Nicholas Sch Environm, Durham, NC 27708 USA.
[Francke, Devon L.; Alessi, Sarah] Univ Hawaii, Joint Inst Marine & Atmospher Res, Honolulu, HI 96822 USA.
[Martin, Summer L.] Natl Acad Sci, Natl Res Council, Washington, DC 20001 USA.
[Kurpita, Lauren] Univ Hawaii, Pacific Cooperat Studies Unit, Honolulu, HI 96822 USA.
[Kurpita, Lauren] World Turtle Trust, Kailua, HI 96734 USA.
[King, Cheryl S.] Hawaii Wildlife Fund, Paia, HI 96779 USA.
[Baird, Robin W.] Cascadia Res Collect, Olympia, WA 98501 USA.
[Van Houtan, Kyle S.] Monterey Bay Aquarium, Monterey, CA 93940 USA.
RP Van Houtan, KS (reprint author), Pacific Isl Fisheries Sci Ctr, NOAA Fisheries, Honolulu, HI 96818 USA.
EM kyle.vanhoutan@gmail.com
OI Van Houtan, Kyle/0000-0001-5725-1773
FU Presidential Early Career Award in Science and Engineering
FX This study was supported by a Presidential Early Career Award in Science
and Engineering to KV.
NR 73
TC 2
Z9 2
U1 19
U2 37
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 2045-7758
J9 ECOL EVOL
JI Ecol. Evol.
PD APR
PY 2016
VL 6
IS 8
BP 2378
EP 2389
DI 10.1002/ece3.2034
PG 12
WC Ecology; Evolutionary Biology
SC Environmental Sciences & Ecology; Evolutionary Biology
GA DJ9YD
UT WOS:000374568300012
PM 27110350
ER
PT J
AU Jorgensen, JC
Ward, EJ
Scheuerell, MD
Zabel, RW
AF Jorgensen, Jeffrey C.
Ward, Eric J.
Scheuerell, Mark D.
Zabel, Richard W.
TI Assessing spatial covariance among time series of abundance
SO ECOLOGY AND EVOLUTION
LA English
DT Article
DE Chinook salmon; Columbia River; dynamic factor analysis; metapopulation;
multivariate autoregressive state-space models; population spatial
structure; species diversity
ID SALMON ONCORHYNCHUS-TSHAWYTSCHA; THREATENED PACIFIC SALMON; STATE-SPACE
MODELS; CHINOOK SALMON; POPULATION-STRUCTURE; MARINE SURVIVAL;
SOCKEYE-SALMON; COHO SALMON; CLIMATE; VARIABILITY
AB For species of conservation concern, an essential part of the recovery planning process is identifying discrete population units and their location with respect to one another. A common feature among geographically proximate populations is that the number of organisms tends to covary through time as a consequence of similar responses to exogenous influences. In turn, high covariation among populations can threaten the persistence of the larger metapopulation. Historically, explorations of the covariance in population size of species with many (>10) time series have been computationally difficult. Here, we illustrate how dynamic factor analysis (DFA) can be used to characterize diversity among time series of population abundances and the degree to which all populations can be represented by a few common signals. Our application focuses on anadromous Chinook salmon (Oncorhynchus tshawytscha), a species listed under the US Endangered Species Act, that is impacted by a variety of natural and anthropogenic factors. Specifically, we fit DFA models to 24 time series of population abundance and used model selection to identify the minimum number of latent variables that explained the most temporal variation after accounting for the effects of environmental covariates. We found support for grouping the time series according to 5 common latent variables. The top model included two covariates: the Pacific Decadal Oscillation in spring and summer. The assignment of populations to the latent variables matched the currently established population structure at a broad spatial scale. At a finer scale, there was more population grouping complexity. Some relatively distant populations were grouped together, and some relatively close populations - considered to be more aligned with each other - were more associated with populations further away. These coarse-and fine-grained examinations of spatial structure are important because they reveal different structural patterns not evident in other analyses.
C1 [Jorgensen, Jeffrey C.; Ward, Eric J.] NOAA, Natl Marine Fisheries Serv, NW Fisheries Sci Ctr, Conservat Biol Div, 2725 Montlake Blvd E, Seattle, WA 98112 USA.
[Scheuerell, Mark D.; Zabel, Richard W.] NOAA, Natl Marine Fisheries Serv, NW Fisheries Sci Ctr, Fish Ecol Div, 2725 Montlake Blvd E, Seattle, WA 98112 USA.
[Jorgensen, Jeffrey C.] NOAA, NW Fisheries Sci Ctr, 2725 Montlake Blvd E, Seattle, WA 98112 USA.
RP Jorgensen, JC (reprint author), NOAA, Natl Marine Fisheries Serv, NW Fisheries Sci Ctr, Conservat Biol Div, 2725 Montlake Blvd E, Seattle, WA 98112 USA.; Jorgensen, JC (reprint author), NOAA, NW Fisheries Sci Ctr, 2725 Montlake Blvd E, Seattle, WA 98112 USA.
EM jeff.jorgensen@noaa.gov
RI Scheuerell, Mark/N-6683-2016
OI Scheuerell, Mark/0000-0002-8284-1254
FU Bonneville Power Administration; U.S. Army Corps of Engineers
FX This work was funded in part from grants to the Northwest Fisheries
Science Center from the Bonneville Power Administration and the U.S.
Army Corps of Engineers.
NR 61
TC 0
Z9 0
U1 12
U2 19
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 2045-7758
J9 ECOL EVOL
JI Ecol. Evol.
PD APR
PY 2016
VL 6
IS 8
BP 2472
EP 2485
DI 10.1002/ece3.2031
PG 14
WC Ecology; Evolutionary Biology
SC Environmental Sciences & Ecology; Evolutionary Biology
GA DJ9YD
UT WOS:000374568300019
PM 27066234
ER
PT J
AU Lee, SK
Wittenberg, AT
Enfield, DB
Weaver, SJ
Wang, CZ
Atlas, R
AF Lee, Sang-Ki
Wittenberg, Andrew T.
Enfield, David B.
Weaver, Scott J.
Wang, Chunzai
Atlas, Robert
TI US regional tornado outbreaks and their links to spring ENSO phases and
North Atlantic SST variability
SO ENVIRONMENTAL RESEARCH LETTERS
LA English
DT Article
DE US tornado outbreaks; springtime ENSO phases; North Atlantic SST
tripole; ENSO teleconnections; ENSO diversity; ENSO flavors
ID MADDEN-JULIAN OSCILLATION; CENTRAL UNITED-STATES; LOW-LEVEL JET;
EL-NINO; REANALYSIS PROJECT; CLIMATE RESPONSE; GREAT-PLAINS; LA-NINA;
PRECIPITATION; EVOLUTION
AB Recent violent and widespread tornado outbreaks in the US, such as occurred in the spring of 2011, have caused devastating societal impact with significant loss of life and property. At present, our capacity to predict US tornado and other severe weather risk does not extend beyond seven days. In an effort to advance our capability for developing a skillful long-range outlook for US tornado outbreaks, here we investigate the spring probability patterns of US regional tornado outbreaks during 1950-2014. Weshow that the four dominant springtime El Nino-Southern Oscillation (ENSO) phases (persistent versus early-terminating El Nino and resurgent versus transitioning La Nina) and the North Atlantic sea surface temperature tripole variability are linked to distinct and significant US regional patterns of outbreak probability. These changes in the probability of outbreaks are shown to be largely consistent with remotely forced regional changes in the large-scale atmospheric processes conducive to tornado outbreaks. An implication of these findings is that the springtime ENSO phases and the North Atlantic SST tripole variability may provide seasonal predictability of US regional tornado outbreaks.
C1 [Lee, Sang-Ki; Enfield, David B.] Univ Miami, Cooperat Inst Marine & Atmospher Studies, Miami, FL USA.
[Lee, Sang-Ki; Wang, Chunzai; Atlas, Robert] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
[Wittenberg, Andrew T.] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA.
[Weaver, Scott J.] NOAA, Climate Predict Ctr, College Pk, MD USA.
RP Lee, SK (reprint author), Univ Miami, Cooperat Inst Marine & Atmospher Studies, Miami, FL USA.; Lee, SK (reprint author), NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
EM Sang-Ki.Lee@noaa.gov
RI Wittenberg, Andrew/G-9619-2013; Lee, Sang-Ki/A-5703-2011; Enfield,
David/I-2112-2013; Atlas, Robert/A-5963-2011
OI Wittenberg, Andrew/0000-0003-1680-8963; Lee,
Sang-Ki/0000-0002-4047-3545; Enfield, David/0000-0001-8107-5079; Atlas,
Robert/0000-0002-0706-3560
FU NOAA CPO through its MAPP program [NA12OAR4310083]; NOAA CPC
[N8R1MP1P00]; NOAA AOML
FX We would like to thank Ghassan Alaka and Hua Chen for their thoughtful
comments and careful reviews. S-K Lee acknowledge James Elsner, Hosmay
Lopez and Jeff Trapp for helpful comments and suggestions on the
statistical methods used in this study, and John Allen, Gerry Bell,
Ashton Cook, Kirstin Harnos, Arun Kumar and Hui Wang for useful
discussions during CPC seasonal severe weather outlook teleconferences.
This work was supported by NOAA CPO through its MAPP program
NA12OAR4310083, and by NOAA CPC (N8R1MP1P00) and NOAA AOML.
NR 48
TC 2
Z9 2
U1 1
U2 3
PU IOP PUBLISHING LTD
PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 1748-9326
J9 ENVIRON RES LETT
JI Environ. Res. Lett.
PD APR
PY 2016
VL 11
IS 4
AR 044008
DI 10.1088/1748-9326/11/4/044008
PG 10
WC Environmental Sciences; Meteorology & Atmospheric Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA DL6JZ
UT WOS:000375746800012
ER
PT J
AU Xue, YK
Oaida, CM
Diallo, I
Neelin, JD
Li, SS
De Sales, F
Gu, Y
Robinson, DA
Vasic, R
Yi, L
AF Xue, Yongkang
Oaida, Catalina M.
Diallo, Ismaila
Neelin, J. David
Li, Suosuo
De Sales, Fernando
Gu, Yu
Robinson, David A.
Vasic, Ratko
Yi, Lan
TI Spring land temperature anomalies in northwestern US and the summer
drought over Southern Plains and adjacent areas
SO ENVIRONMENTAL RESEARCH LETTERS
LA English
DT Article
DE land temperature; US drought and heat; regional climate model; southern
great plains; sea surface temperature
ID CONTERMINOUS UNITED-STATES; NORTH-AMERICAN DROUGHT; SOIL-MOISTURE;
GLOBAL CLIMATE; HEAT-WAVE; VARIABILITY; PRECIPITATION; MODEL; ENSO;
20TH-CENTURY
AB Recurrent drought and associated heatwave episodes are important features of the US climate. Many studies have examined the connection between ocean surface temperature changes and conterminous US droughts. However, remote effects of large-scale land surface temperature variability, over shorter but still considerable distances, on US regional droughts have been largely ignored. The present study combines two types of evidence to address these effects: climate observations and model simulations. Our analysis of observational data shows that springtime land temperature in northwest US is significantly correlated with summer rainfall and surface temperature changes in the US Southern Plains and its adjacent areas. Our model simulations of the 2011 Southern Plains drought using a general circulation model and a regional climate model confirm the observed relationship between land temperature anomaly and drought, and suggest that the long-distance effect of land temperature changes in the northwest US on Southern Plains droughts is probably as large as the more familiar effects of ocean surface temperatures and atmospheric internal variability. We conclude that the cool 2011 springtime climate conditions in the northwest US increased the probability of summer drought and abnormal heat in the Southern Plains. The present study suggests a strong potential for more skillful intra-seasonal predictions of US Southern Plains droughts when such facts as ones presented here are considered.
C1 [Xue, Yongkang; Diallo, Ismaila; Li, Suosuo; De Sales, Fernando] Univ Calif Los Angeles, Dept Geog, Los Angeles, CA 90095 USA.
[Xue, Yongkang; Oaida, Catalina M.; Neelin, J. David; Gu, Yu] Univ Calif Los Angeles, Dept Atmospher & Ocean Sci, Los Angeles, CA 90095 USA.
[Li, Suosuo] Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Peoples R China.
[De Sales, Fernando] San Diego State Univ, San Diego, CA 92182 USA.
[Robinson, David A.] Rutgers State Univ, Dept Geog, Piscataway, NJ 08854 USA.
[Vasic, Ratko] Natl Ctr Environm Predict, College Pk, MD 20740 USA.
[Yi, Lan] Chinese Acad Meteorol Sci, Beijing 10081, Peoples R China.
RP Xue, YK (reprint author), Univ Calif Los Angeles, Dept Geog, Los Angeles, CA 90095 USA.; Xue, YK (reprint author), Univ Calif Los Angeles, Dept Atmospher & Ocean Sci, Los Angeles, CA 90095 USA.
EM yxue@geog.ucla.edu
FU National Science Foundation [AGS-1346813, AGS-1115506, AGS-1540518]
FX This work was supported by National Science Foundation grants
AGS-1346813, AGS-1115506, and AGS-1540518. We thank Mr John Mioduszewski
and Mr Thomas Estilow of Rutgers University for the snow data. The
authors also thank Professor Jared Diamond and Professor David Rigby of
UCLA for their comments and contributions to the manuscript revisions,
as well as two anonymous reviewers' very constructive
comments/suggestions to help improve the paper. The model runs were
conducted at the National Center for Atmospheric Research Bluefire
Supercomputer and the Texas Advanced Computer Center Stampede
Supercomputer.
NR 54
TC 0
Z9 0
U1 4
U2 4
PU IOP PUBLISHING LTD
PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 1748-9326
J9 ENVIRON RES LETT
JI Environ. Res. Lett.
PD APR
PY 2016
VL 11
IS 4
AR 044018
DI 10.1088/1748-9326/11/4/044018
PG 12
WC Environmental Sciences; Meteorology & Atmospheric Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA DL6JZ
UT WOS:000375746800022
ER
PT J
AU Levine, J
AF Levine, Judah
TI The history of time and frequency from antiquity to the present day
SO EUROPEAN PHYSICAL JOURNAL H
LA English
DT Article
ID INTERNATIONAL ATOMIC TIME; BLACKBODY RADIATION; OPTICAL FREQUENCIES;
CESIUM; STANDARD; BEAM; UNCERTAINTY; ALGORITHMS; SIGNALS; BUREAU
AB I will discuss the evolution of the definitions of time, time interval, and frequency from antiquity to the present day. The earliest definitions of these parameters were based on a time interval defined by widely observed apparent astronomical phenomena, so that techniques of time distribution were not necessary. With this definition, both time, as measured by clocks, and frequency, as realized by some device, were derived quantities. On the other hand, the fundamental parameter today is a frequency based on the properties of atoms, so that the situation is reversed and time and time interval are now derived quantities. I will discuss the evolution of this transition and its consequences. In addition, the international standards of both time and frequency are currently realized by combining the data from a large number of devices located at many different laboratories, and this combination depends on (and is often limited by) measurements of the times of clocks located at widely-separated laboratories. I will discuss how these measurements are performed and how the techniques have evolved over time.
C1 [Levine, Judah] Natl Inst Stand & Technol, Div Time & Frequency, Boulder, CO 80305 USA.
[Levine, Judah] Natl Inst Stand & Technol, JILA, Boulder, CO 80305 USA.
[Levine, Judah] Univ Colorado, Boulder, CO 80305 USA.
RP Levine, J (reprint author), Natl Inst Stand & Technol, Div Time & Frequency, Boulder, CO 80305 USA.; Levine, J (reprint author), Natl Inst Stand & Technol, JILA, Boulder, CO 80305 USA.; Levine, J (reprint author), Univ Colorado, Boulder, CO 80305 USA.
EM judah.levine@colorado.edu
NR 80
TC 0
Z9 0
U1 8
U2 8
PU SPRINGER HEIDELBERG
PI HEIDELBERG
PA TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY
SN 2102-6459
EI 2102-6467
J9 EUR PHYS J H
JI Eur. Phys. J. H
PD APR
PY 2016
VL 41
IS 1
BP 1
EP 67
DI 10.1140/epjh/e2016-70004-3
PG 67
WC History & Philosophy Of Science; Physics, Multidisciplinary
SC History & Philosophy of Science; Physics
GA DK6JY
UT WOS:000375030900001
ER
PT J
AU Watson, W
Charter, SR
Lawley, CAT
AF Watson, William
Charter, Sharon R.
Lawley, Cynthia A. Taylor
TI Early larvae of the swordspine rockfish (Sebastes ensifer) identified by
molecular methods
SO FISHERY BULLETIN
LA English
DT Article
ID SOUTHERN CALIFORNIA BIGHT; GENUS SEBASTES; JUVENILES; LENGTH;
REPRODUCTION; PRESERVATION; SCORPAENIDAE; PAUCISPINIS; ATLANTIC; PCR
AB About 56 rockfish (Sebastes) species occur in Southern California, but the larvae of most of them are undescribed. Larval rockfishes collected off Southern. California during the California Cooperative Oceanic Fisheries Investigations (CalCOFI) cruise in April 1999 and the Baseline Cowcod Conservation Area (CCA) cruise in February 2002 were identified by using mitochondrial cytochrome b genomic DNA to determine the abundances of individual species. About 27% of the larvae from the CalCOFI cruise and 16% of the larvae from the CCA cruise were Sebastes ensifer. Larval S. ensifer were undescribed for most of the size range identified here (2.6-8.4 mm, early preflexion through early postflexion. stage). Larval S. ensifer are moderately deep-bodied and robust and have melanophores dorsally and ventrally on the gut, in a single ventral row on the tail, and on the pectoral fins. Starting at about 3.8 mm, melanophores form on the anterior part of the mandible. Larvae >= 6 mm have pigment in the mid- and hindbrain areas. Preflexion-stage larval S. ensifer are indistinguishable from the described larvae of sympatric species in the Sebastes subgenus Sebastomus, except perhaps Sebastes rosaceus and S. umbrosus. In later stages, S. ensifer may be distinguishable from S. constellatus and S. helvomaculatus.
C1 [Watson, William; Charter, Sharon R.; Lawley, Cynthia A. Taylor] NOAA, Southwest Fisheries Sci Ctr, Natl Marine Fisheries Serv, 8901 La Jolla Shores Dr, La Jolla, CA 92037 USA.
[Lawley, Cynthia A. Taylor] Univ Calif San Diego, Scripps Inst Oceanog, 9500 Gilman Dr,Mail Code 0203, La Jolla, CA 92093 USA.
RP Watson, W (reprint author), NOAA, Southwest Fisheries Sci Ctr, Natl Marine Fisheries Serv, 8901 La Jolla Shores Dr, La Jolla, CA 92037 USA.
EM william.watson@noaa.gov
FU Oceanids Foundation; Frieda Daum Urey scholarship committee
FX We wish to thank the scientific and ship's crews of the NOAA Ship David
Starr Jordan and Scripps Institution of Oceanography RV New Horizon. Our
appreciation goes to A. Hays, D. Griffith, and R. Charter, who
especially assisted in obtaining samples; L. Dunn for sorting the fish
larvae from the plankton samples; H. Timms and A. Brooks for their
assistance in the laboratory; and H. Moser, who contributed pertinent
information during review. For his tutelage and review of this article,
S. Charter is especially grateful to J. Hyde. We also thank the Oceanids
Foundation and the Frieda Daum Urey scholarship committee for their
endowment to CATL.
NR 36
TC 0
Z9 0
U1 1
U2 1
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
EI 1937-4518
J9 FISH B-NOAA
JI Fish. Bull.
PD APR
PY 2016
VL 114
IS 2
BP 135
EP 143
DI 10.7755/FB.114.2.1
PG 9
WC Fisheries
SC Fisheries
GA DK2DF
UT WOS:000374724100001
ER
PT J
AU Lewis, LA
Richardson, DE
Zakharov, EV
Hanner, R
AF Lewis, Leah A.
Richardson, David E.
Zakharov, Evgeny V.
Hanner, Robert
TI Integrating DNA barcoding of fish eggs into ichthyoplankton monitoring
programs
SO FISHERY BULLETIN
LA English
DT Article
ID COD GADUS-MORHUA; ATLANTIC COD; MARINE FISHES; ESTIMATING BIOMASS; IRISH
SEA; IDENTIFICATION; STOCK; LIFE; LARVAE; GULF
AB The data collected through ichthyoplankton monitoring surveys provide valuable insight into the spawning dynamics of multiple species. Fish eggs, more than larvae, offer a more precise evaluation of species-specific spawning characteristics; however, egg collections are greatly underused because of the limitations associated with morphology-based identifications. In recent years, a new means of molecular identification, termed DNA barcoding, has made species identification readily available across a broad range of taxa. We used DNA barcoding to identify ethanol-preserved fish eggs collected during 2002-2012 along the northeastern U.S. continental shelf A subsampling protocol was used to select 1603 unidentified eggs for analysis. DNA sequences were successfully obtained from 1495 (93.26%) of these eggs, representing 50 species many of which have either never before been identified to the species-level as eggs or have been identified previously only to a higher taxonomic level or during specific developmental egg stages. In comparison with past attempts at morphological identification, our molecular identifications comprise a broader diversity of eggs and provide a technique with high success rates of unambiguous identifications that is not sensitive to egg stage. Overall, this work shows that DNA barcoding of fish eggs is sufficiently advanced to be incorporated into long-term, regional-scale ichthyoplankton. monitoring programs.
C1 [Lewis, Leah A.; Richardson, David E.] NOAA, Natl Marine Fisheries Serv, Northeast Fisheries Sci Ctr, 28 Tarzwell Dr, Narragansett, RI 02882 USA.
[Zakharov, Evgeny V.; Hanner, Robert] Univ Guelph, Biodivers Inst Ontario, Guelph, ON N1G 2W1, Canada.
RP Richardson, DE (reprint author), NOAA, Natl Marine Fisheries Serv, Northeast Fisheries Sci Ctr, 28 Tarzwell Dr, Narragansett, RI 02882 USA.
EM david.richardson@noaa.gov
NR 38
TC 0
Z9 0
U1 3
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
EI 1937-4518
J9 FISH B-NOAA
JI Fish. Bull.
PD APR
PY 2016
VL 114
IS 2
BP 153
EP 165
DI 10.7755/FB.114.2.3
PG 13
WC Fisheries
SC Fisheries
GA DK2DF
UT WOS:000374724100003
ER
PT J
AU Demetras, NJ
Huff, DD
Michel, CJ
Smith, JM
Cutter, GR
Hayes, SA
Lindley, ST
AF Demetras, Nicholas J.
Huff, David D.
Michel, Cyril J.
Smith, Joseph M.
Cutter, George R.
Hayes, Sean A.
Lindley, Steven T.
TI Development of underwater recorders to quantify predation of juvenile
Chinook salmon (Oncorhynchus tshawytscha) in a river environment
SO FISHERY BULLETIN
LA English
DT Article
ID SURVIVAL; FISH; MIGRATION; HABITATS; DELTA; BASS
AB Recent acoustic tagging of juvenile Chinook salmon (Oncorhynchus tshawytscha) in the southern portion of California's Sacramento San Joaquin Delta has revealed extremely low survival rates (<1%), possibly due to predation by piscivorous fishes. We evaluated predation as a cause of low survival by designing and testing freely floating GPS-enabled predation.-event recorders (PERs) baited with juvenile Chinook salmon. We estimated predation rates and identified predation locations within. a 1-kilometer reach of the Lower San Joaquin River. We modeled the relationship between time to predation and environmental variables with a Cox proportional hazards analysis that accounts for censored data. Our results indicated that an increase of 1 m/s in water velocity elevated the minute-by-minute hazard of predation by a factor of 9.6. Similarly, each increase in median depth decreased the predation hazard by a factor of 0.5. The mean relative predation rate in the study area was 15.3% over 9 sampling events between March and May 2014. Waterproof video cameras attached to a subset (48 of 216) of PERs successfully identified predator species 25% of the time. Our GPS-enabled PERs proved to be an inexpensive and reliable tool, which quantified predation, identified predation locations, and provided complementary information for acoustic telemetry and predator diet studies.
C1 [Demetras, Nicholas J.; Michel, Cyril J.] Univ Calif Santa Cruz, Southwest Fisheries Sci Ctr, NOAA, Natl Marine Fisheries Serv, 110 Shaffer Rd, Santa Cruz, CA 95060 USA.
[Huff, David D.] NOAA, Point Adams Res Stn, Fish Ecol Div, NW Fisheries Sci Ctr, POB 155, Hammond, OR 97121 USA.
[Smith, Joseph M.] Univ Washington, Sch Aquat & Fishery Sci, 1122 NE Boat St, Seattle, WA 98105 USA.
[Cutter, George R.] NOAA, Fisheries Resource Div, Southwest Fisheries Sci Ctr, Natl Marine Fisheries Serv, 8901 La Jolla Shores Dr, La Jolla, CA 92037 USA.
[Hayes, Sean A.; Lindley, Steven T.] NOAA, Fisheries Resource Div, Southwest Fisheries Sci Ctr, Natl Marine Fisheries Serv, 110 Shaffer Rd, Santa Cruz, CA 95060 USA.
RP Demetras, NJ (reprint author), Univ Calif Santa Cruz, Southwest Fisheries Sci Ctr, NOAA, Natl Marine Fisheries Serv, 110 Shaffer Rd, Santa Cruz, CA 95060 USA.
EM nicholas.demetras@noaa.gov
OI Huff, David/0000-0001-9061-7685
FU California Department of Water Resources [46-10100]; National Marine
Fisheries Service
FX We would like to thank the many people who assisted with fieldwork,
particularly M. Sabal, V. Lo, T. Brown, B. Lehman, and M. Miller. In
addition, M. Henderson and F. Cordoleani provided insightful comments on
early drafts and three anonymous reviewers provided helpful suggestions
during the review process. The California Department of Water Resources
funded this work under agreement no. 46-10100 with the National Marine
Fisheries Service. Material and logistical support was also provided by
The National Marine Fisheries Service Southwest Fisheries Science
Center, Santa Cruz, CA.
NR 24
TC 0
Z9 0
U1 10
U2 11
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
EI 1937-4518
J9 FISH B-NOAA
JI Fish. Bull.
PD APR
PY 2016
VL 114
IS 2
BP 179
EP 185
DI 10.7755/FB.114.2.5
PG 7
WC Fisheries
SC Fisheries
GA DK2DF
UT WOS:000374724100005
ER
PT J
AU Yasumiishi, EM
Criddle, KR
Helle, JH
Hillgruber, N
Mueter, FJ
AF Yasumiishi, Ellen M.
Criddle, Keith R.
Helle, John H.
Hillgruber, Nicola
Mueter, Franz J.
TI Effect of population abundance and climate on the growth of 2
populations of chum salmon (Oncorhynchus keta) in the eastern North
Pacific Ocean
SO FISHERY BULLETIN
LA English
DT Article
ID PINK SALMON; SOCKEYE-SALMON; BERING-SEA; BODY-SIZE; HATCHERY PROGRAMS;
BRITISH-COLUMBIA; MARINE SURVIVAL; ALASKA; RIVER; GORBUSCHA
AB Seasonal and annual marine growth of chum salmon (Oncorhynchus keta) from Fish Creek, Alaska, during 1972-2004 and from Quilcene River, Washington., during 1973-2004 were examined in relation to abundances of chum salmon and pink salmon (O. gorbuscha) and climate indices from that period. Pink salmon abundance indices were included in the analysis because of evidence for density-dependent effects on chum salmon growth and survival. In linear regression models, growth was negatively related to abundance of chum salmon or to the combined abundance of pink and chum salmon during the middle juvenile (July-Sept), 1st immature, 2nd immature, and maturing stages for the Fish Creek chum salmon and the 1st immature, 2nd immature, and maturing stages for Quilcene River chum salmon, indicating possible density-dependent effects on growth. Mid-juvenile and maturing growth models for the Fish Creek chum salmon and the maturing growth model for Quilcene River chum salmon performed well in model validation, when model predictions were tested against 20% of the data that were not used for model specification, and provided insight into the effects of climate and abundance on growth of chum salmon from 1972 to 2004.
C1 [Yasumiishi, Ellen M.; Criddle, Keith R.; Helle, John H.; Hillgruber, Nicola; Mueter, Franz J.] Univ Alaska Fairbanks, Sch Fisheries & Ocean Sci, 17101 Point Lena Loop Rd, Juneau, AK 99801 USA.
[Yasumiishi, Ellen M.] NOAA, Auke Bay Labs, Alaska Fisheries Sci Ctr, Natl Marine Fisheries Serv,Ted Stevens Marine Res, 17109 Point Lena Loop Rd, Juneau, AK 99801 USA.
[Helle, John H.] 2427 ODay Dr, Juneau, AK 99801 USA.
[Hillgruber, Nicola] Thunen Inst Fisheries Ecol, Wulfsdorfer Weg 204, D-22926 Ahrensburg, Germany.
RP Yasumiishi, EM (reprint author), Univ Alaska Fairbanks, Sch Fisheries & Ocean Sci, 17101 Point Lena Loop Rd, Juneau, AK 99801 USA.; Yasumiishi, EM (reprint author), NOAA, Auke Bay Labs, Alaska Fisheries Sci Ctr, Natl Marine Fisheries Serv,Ted Stevens Marine Res, 17109 Point Lena Loop Rd, Juneau, AK 99801 USA.
EM ellen.yasumiishi@noaa.gov
FU Alaska Fisheries Science Center in Juneau, Alaska; Advanced Studies
Program, Professional Development program of the National Oceanic and
Atmospheric Administration
FX Funding and support for this project was received from the Alaska
Fisheries Science Center in Juneau, Alaska and the Advanced Studies
Program, Professional Development program of the National Oceanic and
Atmospheric Administration. We greatly appreciate the assistance of all
the people that helped with field collection throughout the years and
the assistance of the Alaska Department of Fish and Game in Ketchikan
and the U.S. Fish and Wildlife Service at the Quilcene National Fish
Hatchery in Quilcene, Washington. We appreciate the constructive
comments from Phil Mundy, Ed Farley, and Lisa Eisner. We also thank the
anonymous reviewers for their thoughtful suggestions that greatly
improved the manuscript.
NR 74
TC 0
Z9 0
U1 5
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
EI 1937-4518
J9 FISH B-NOAA
JI Fish. Bull.
PD APR
PY 2016
VL 114
IS 2
BP 203
EP 219
DI 10.7755/FB.114.2.7
PG 17
WC Fisheries
SC Fisheries
GA DK2DF
UT WOS:000374724100007
ER
PT J
AU Weijerman, M
Williams, I
Gutierrez, J
Grafeld, S
Tibbatts, B
Davis, G
AF Weijerman, Mariska
Williams, Ivor
Gutierrez, Jay
Grafeld, Shanna
Tibbatts, Brent
Davis, Gerry
TI Trends in biomass of coral reef fishes, derived from shore-based creel
surveys in Guam
SO FISHERY BULLETIN
LA English
DT Article
ID MANAGEMENT; PACIFIC; RESILIENCE; MICRONESIA; ECOSYSTEMS; ISLANDS; TRADE
AB Coral reef fisheries have a cultural, economic, and ecological importance and sustain the societal well-being of many coastal communities. However, the complexities of the multigear, multispecies fisheries that target coral reef species pose challenges for fisheries management. We focus on the Guam shore-based coral reef fishery 1) to evaluate the characteristics of the past and recent fishery in terms of catch composition and effort per gear type and 2) to reconstruct the reef-fish population in shallow (depths <= 30 m) water during 1985-2012. To accomplish this, we used the results from a detailed creel survey conducted by the Guam Division of Aquatic and Wildlife Resources. The total estimated effort has stayed more or less stable; however, the estimated total catch has dropped from an annual mean of 100 metric tons (t) during the period 1985-1990 to 37 t during the period 2007-2012. Catch per unit of effort (CPUE) declined for most gear types between the 2 time periods. Reconstruction. of historical targeted fish biomass, based on CPUE, showed a general decrease in biomass from 1985 to 2012. Biomass quickly dropped to about half of the 1985 values, then leveled off for a decade before declining again beginning in 2003 and continuing through 2012.
C1 [Weijerman, Mariska] Univ Hawaii Manoa, Joint Inst Marine & Atmospher Res, Sch Ocean & Earth Sci & Technol, Marine Sci Bldg 312,1000 Pope Rd, Honolulu, HI 96822 USA.
[Weijerman, Mariska] Wageningen Univ, Environm Syst Anal Grp, POB 47, NL-6700 AA Wageningen, Netherlands.
[Williams, Ivor] NOAA, Coral Reef Ecosyst Program, Pacific Isl Fisheries Sci Ctr, Natl Mariner Fisheries Serv, 1845 Wasp Blvd,Bldg 176, Honolulu, HI 96818 USA.
[Gutierrez, Jay; Tibbatts, Brent] Guam Dept Agr, Div Aquat & Wildlife Resources, 163 Dairy Rd, Mangilao, GU 96913 USA.
[Grafeld, Shanna] Univ Hawaii Manoa, Dept Nat Resources & Environm Management, 1910 East West Rd,Sherman Lab 101, Honolulu, HI 96822 USA.
[Davis, Gerry] NOAA, Habitat Conservat Div, Pacific Isl Reg Off, Natl Marine Fisheries Serv, 1845 Wasp Blvd,Bldg 176, Honolulu, HI 96818 USA.
RP Weijerman, M (reprint author), Univ Hawaii Manoa, Joint Inst Marine & Atmospher Res, Sch Ocean & Earth Sci & Technol, Marine Sci Bldg 312,1000 Pope Rd, Honolulu, HI 96822 USA.; Weijerman, M (reprint author), Wageningen Univ, Environm Syst Anal Grp, POB 47, NL-6700 AA Wageningen, Netherlands.
EM mariska.weijerman@noaa.gov
FU NOAA Coral Reef Conservation Program
FX Funding for the senior author and S. Grafeld was obtained from the NOAA
Coral Reef Conservation Program. We would like to acknowledge the staff
at the Division of Aquatic and Wildlife Resources, Guam Department of
Agriculture, for data collection and the following people at the NOAA
Pacific Islands Fisheries Science Center: K. Low, M. Quack, and P. Tao
for extracting and helping to interpret data, M. Nadon for advice on
data analyses, and C. Boggs and J. Wetherall for their valuable comments
on the draft manuscript.
NR 40
TC 0
Z9 0
U1 2
U2 5
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
EI 1937-4518
J9 FISH B-NOAA
JI Fish. Bull.
PD APR
PY 2016
VL 114
IS 2
BP 237
EP 256
DI 10.7755/FB.114.2.9
PG 20
WC Fisheries
SC Fisheries
GA DK2DF
UT WOS:000374724100009
ER
PT J
AU Chen, XF
Yan, RQ
Liu, YM
AF Chen, Xuefeng
Yan, Ruqiang
Liu, Yanmeng
TI Wind Turbine Condition Monitoring and Fault Diagnosis in China
SO IEEE INSTRUMENTATION & MEASUREMENT MAGAZINE
LA English
DT Article
C1 [Chen, Xuefeng] Xi An Jiao Tong Univ, Mech Engn, Xian, Peoples R China.
[Chen, Xuefeng] IEEE Xian & Chengdu Joint Sect Instrumentat & Mea, Xian, Peoples R China.
[Yan, Ruqiang] NIST, Gaithersburg, MD 20899 USA.
[Yan, Ruqiang] Southeast Univ, Sch Instrument Sci, Xian, Peoples R China.
[Yan, Ruqiang; Liu, Yanmeng] Xi An Jiao Tong Univ, Collaborat Innovat Ctr High End Mfg Equipment, Xian, Peoples R China.
RP Chen, XF (reprint author), Xi An Jiao Tong Univ, Mech Engn, Xian, Peoples R China.; Chen, XF (reprint author), IEEE Xian & Chengdu Joint Sect Instrumentat & Mea, Xian, Peoples R China.; Yan, RQ (reprint author), NIST, Gaithersburg, MD 20899 USA.; Yan, RQ (reprint author), Southeast Univ, Sch Instrument Sci, Xian, Peoples R China.; Yan, RQ (reprint author), Xi An Jiao Tong Univ, Collaborat Innovat Ctr High End Mfg Equipment, Xian, Peoples R China.
EM chenxf@mail.xjtu.edu.cn; ruqiang@seu.edu.cn
RI Yan, Ruqiang/A-9776-2012
OI Yan, Ruqiang/0000-0003-4341-6535
NR 4
TC 2
Z9 2
U1 1
U2 6
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 1094-6969
EI 1941-0123
J9 IEEE INSTRU MEAS MAG
JI IEEE Instrum. Meas. Mag.
PD APR
PY 2016
VL 19
IS 2
BP 22
EP 28
PG 7
WC Engineering, Electrical & Electronic; Instruments & Instrumentation
SC Engineering; Instruments & Instrumentation
GA DL3ZE
UT WOS:000375571400007
ER
PT J
AU Lumpkin, R
Centurioni, L
Perez, RC
AF Lumpkin, Rick
Centurioni, Luca
Perez, Renellys C.
TI Fulfilling Observing System Implementation Requirements with the Global
Drifter Array
SO JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY
LA English
DT Article
ID EQUATORIAL ATLANTIC
AB The Global Ocean Observing System (GOOS) requirements for in situ surface temperature and velocity measurements call for observations at 5 degrees x 5 degrees resolution. A key component of the GOOS that measures these essential climate variables is the global array of surface drifters. In this study, statistical observing system sampling experiments are performed to evaluate how many drifters are required to achieve the GOOS requirements, both with and without the presence of a completed global tropical moored buoy array at 5 degrees S-5 degrees N. The statistics for these simulations are derived from the evolution of the actual global drifter array. It is concluded that drifters should be deployed within the near-equatorial band even though that band is also in principle covered by the tropical moored array, as the benefits of not doing so are marginal. It is also concluded that an optimal design half-life for the drifters is similar to 450 days, neglecting external sources of death, such as running aground or being picked up. Finally, it is concluded that comparing the drifter array size to the number of static 5 degrees x 5 degrees open-ocean bins is not an ideal performance indicator for system evaluation; a better performance indicator is the fraction of 5 degrees x 5 degrees open-ocean bins sampled, neglecting bins with high drifter death rates.
C1 [Lumpkin, Rick; Perez, Renellys C.] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
[Centurioni, Luca] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA.
[Perez, Renellys C.] Univ Miami, Cooperat Inst Marine & Atmospher Studies, Miami, FL USA.
RP Lumpkin, R (reprint author), NOAA, Atlantic Oceanog & Meteorol Lab, Phys Oceanog Div, 4301 Rickenbacker Causeway, Miami, FL 33149 USA.
EM rick.lumpkin@noaa.gov
RI Perez, Renellys/D-1976-2012; Lumpkin, Rick/C-9615-2009
OI Perez, Renellys/0000-0002-4401-3853; Lumpkin, Rick/0000-0002-6690-1704
FU Atlantic Oceanographic and Meteorological Laboratory of the National
Oceanic and Atmospheric Administration, U.S. Department of Commerce;
Climate Observation Division of the Climate Program Office of the
National Oceanic and Atmospheric Administration, U.S. Department of
Commerce; NOAA [NA10OAR4320156, NA10OAR4320143]; Cooperative Institute
for Marine and Atmospheric Studies (CIMAS), a cooperative institute of
the University of Miami
FX Conversations and exchanges with Diane Stanitski, Champika Gallage, and
Cristina Lumpkin provided valuable input for this study. We thank Hosmay
Lopez and Libby Johns for the reviews and editorial suggestions. R.
Lumpkin and R. Perez were funded by the Atlantic Oceanographic and
Meteorological Laboratory and the Climate Observation Division of the
Climate Program Office, both of the National Oceanic and Atmospheric
Administration, U.S. Department of Commerce. L. Centurioni was funded by
NOAA Grant NA10OAR4320156, "The Global Drifter Program." This research
was carried out in part under the auspices of the Cooperative Institute
for Marine and Atmospheric Studies (CIMAS), a cooperative institute of
the University of Miami and NOAA, Cooperative Agreement NA10OAR4320143.
NR 20
TC 2
Z9 2
U1 1
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 APR
PY 2016
VL 33
IS 4
BP 685
EP 695
DI 10.1175/JTECH-D-15-0255.1
PG 11
WC Engineering, Ocean; Meteorology & Atmospheric Sciences
SC Engineering; Meteorology & Atmospheric Sciences
GA DL6FV
UT WOS:000375736000005
ER
PT J
AU Zhang, C
Zhang, Z
Li, GQ
AF Zhang, Chao
Zhang, Zhe
Li, Guo-Qiang
TI Simple vs. sophisticated fire models to predict performance of SHS
column in localized fire
SO JOURNAL OF CONSTRUCTIONAL STEEL RESEARCH
LA English
DT Article
DE Localized fire; Buckling temperature; Square hollow steel column; Simple
fire model; Comparative study; Thermo-mechanical analyses
ID THERMAL CALCULATION; STEEL COLUMNS; BEHAVIOR; BEAMS
AB This paper presents a comparative study on fire models to predict the performance of an axially loaded square hollow steel (SHS) column exposed to a localized fire. A simple fire model based on the classic fire plume theory and a sophisticated computational fluid dynamics (CFD) model named Fire Dynamics Simulator (FDS) were investigated and used to predict the heat fluxes from the localized fire to the column. Thermo-mechanical analyses using finite element software were conducted to obtain the temperature and structural responses of the column exposed to the predicted heat fluxes. A total of 22 cases were considered and the variable parameters included heat release rate, fire source diameter, location of the fire source and load ratio. The steel temperatures predicted using the simple fire model were higher than those predicted using the sophisticated fire model. The buckling temperatures predicted using the simple fire model were generally lower than those predicted using the sophisticated fire model, and the average difference of the predicted buckling temperatures was within 40 degrees C Buckling temperature is defined here as the maximum temperature in a steel column on onset of buckling. Comparing with the sophisticated fire model, the simple fire model is computationally efficient and yields conservative results, which may be used in structural fire engineering design. (C) 2015 Elsevier Ltd. All rights reserved.
C1 [Zhang, Chao] Tongji Univ, Coll Civil Engn, 1239 Siping Rd, Shanghai 200092, Peoples R China.
[Zhang, Chao] NIST, 100 Bur Dr,Stop 8666, Gaithersburg, MD 20899 USA.
[Zhang, Zhe] Zhengzhou Univ, Dept Civil Engn, Zhengzhou 450001, Henan, Peoples R China.
[Li, Guo-Qiang] Sate Key Lab Disaster Reduct Civil Engn, 1239 Siping Rd, Shanghai, Peoples R China.
RP Zhang, Z (reprint author), Zhengzhou Univ, Dept Civil Engn, Zhengzhou 450001, Henan, Peoples R China.
EM chao.zhang@nist.gov; zhangzhe_77@163.com
FU National Natural Science Foundation of China [51508399]
FX The work reported hereinabove is partially supported by the National
Natural Science Foundation of China through the contract 51508399. The
support is gratefully acknowledged.
NR 27
TC 0
Z9 0
U1 2
U2 6
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0143-974X
EI 1873-5983
J9 J CONSTR STEEL RES
JI J. Constr. Steel. Res.
PD APR
PY 2016
VL 120
BP 62
EP 69
DI 10.1016/j.jcsr.2015.12.026
PG 8
WC Construction & Building Technology; Engineering, Civil
SC Construction & Building Technology; Engineering
GA DK0LB
UT WOS:000374603200007
ER
PT J
AU Mazumdar, D
Knut, R
Thole, F
Gorgoi, M
Faleev, S
Mryasov, ON
Shelke, V
Ederer, C
Spaldin, NA
Gupta, A
Karis, O
AF Mazumdar, Dipanjan
Knut, R.
Thoele, F.
Gorgoi, M.
Faleev, Sergei
Mryasov, O. N.
Shelke, Vilas
Ederer, C.
Spaldin, N. A.
Gupta, A.
Karis, O.
TI The valence band electronic structure of rhombohedral-like and
tetragonal-like BiFeO3 thin films from hard X-ray photoelectron
spectroscopy and first-principles theory
SO JOURNAL OF ELECTRON SPECTROSCOPY AND RELATED PHENOMENA
LA English
DT Article
DE Hard X-ray photoelectron spectroscopy; Multifunctional materials;
Multiferroics; Electronic structure; Density functional theory; Bismuth
ferrite
ID ANGULAR-DISTRIBUTION PARAMETERS; RANGE 100-5000 EV; DOMAIN-WALLS;
ENERGY; POLARIZATION; TEMPERATURE; OXIDE
AB We investigate the electronic structure of rhombohedral-like (R) and tetragonal-like (T) BiFeO3 thin films using high energy X-ray photoelectron spectroscopy and first-principles electronic structure calculations. By exploiting the relative elemental cross sections to selectively probe the elemental composition of the valence band, we identify a strong Bi 6p contribution at the top of the valence band in both phases, overlapping in energy range with the O 2p states; this assignment is confirmed by our electronic structure calculations. We find that the measured occupied Bi 6p signal lies closer to the top of the valence band in the T phase than in the R phase, which we attribute, using our electronic structure calculations, to lower Bi-O hybridization in the T phase. We note, however, that our calculations of the corresponding densities of states underestimate the difference between the phases, suggesting that matrix element effects resulting from the different effective symmetries also contribute. Our results shed light on the chemical nature of the stereochemically active Bi lone pairs, which are responsible for the large ferroelectric polarization of BiFeO3. (C) 2015 Published by Elsevier B.V.
C1 [Mazumdar, Dipanjan] So Illinois Univ, Dept Phys, Carbondale, IL 62901 USA.
[Knut, R.] Univ Colorado, JILA, Boulder, CO 80309 USA.
[Knut, R.] Univ Colorado, Dept Phys, Boulder, CO 80309 USA.
[Knut, R.] NIST, Boulder, CO 80309 USA.
[Karis, O.] Uppsala Univ, Dept Phys & Astron, Uppsala, Sweden.
[Thoele, F.; Ederer, C.; Spaldin, N. A.] ETH, Mat Theory, Wolfgang Pauli Str 27, Zurich, Switzerland.
[Gorgoi, M.] BESSY II, Helmholtz Zentrum Berlin Mat & Energie GmbH, Berlin, Germany.
[Faleev, Sergei; Mryasov, O. N.; Gupta, A.] Univ Alabama, Ctr Mat Informat Technol, Tuscaloosa, AL 35487 USA.
RP Karis, O (reprint author), Uppsala Univ, Dept Phys & Astron, Uppsala, Sweden.
EM olof.karis@physics.uu.se
OI Thole, Florian/0000-0001-6006-9876
FU ETH Zurich; Southern Illinois University; Swedish Research Council (VR);
European Community [312284]
FX This work was supported financially by the ETH Zurich (N.A.S., C.E. and
F.T.) and by the Max Rossler Prize of the ETH Zurich (N.A.S.). DM
acknowledges start-up funds from Southern Illinois University. RK and OK
gratefully acknowledge the support of the Swedish Research Council (VR).
We thank HZB for the allocation of synchrotron radiation beamtime. The
research leading to these results has received funding from the European
Community's Seventh Framework Programme (FP7/2007-2013) under grant
agreement no. 312284.
NR 31
TC 2
Z9 2
U1 12
U2 21
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0368-2048
EI 1873-2526
J9 J ELECTRON SPECTROSC
JI J. Electron Spectrosc. Relat. Phenom.
PD APR
PY 2016
VL 208
SI SI
BP 63
EP 66
DI 10.1016/j.elspec.2015.10.002
PG 4
WC Spectroscopy
SC Spectroscopy
GA DL6GY
UT WOS:000375738900011
ER
PT J
AU Li, SS
Ma, ZW
Xiong, XZ
Christiani, DC
Wang, ZX
Liu, Y
AF Li, Shenshen
Ma, Zongwei
Xiong, Xiaozhen
Christiani, David C.
Wang, Zhaoxi
Liu, Yang
TI Satellite and Ground Observations of Severe Air Pollution Episodes in
the Winter of 2013 in Beijing, China
SO AEROSOL AND AIR QUALITY RESEARCH
LA English
DT Article
DE Smog; MODIS; Aerosol optical depth; PM2.5; HYSPLIT
ID LEVEL PM2.5 CONCENTRATIONS; AEROSOL OPTICAL DEPTH; EASTERN CHINA; LAND;
PRODUCTS; CITIES; STATES; REGRESSION; MODEL; FOG
AB Beginning in early January 2013, Beijing experienced multiple prolonged and severe smog events that were characterized by very high levels of PM2.5, with peak daily PM2.5 over 400 mu g m(-3). With PM2.5 concentration contours created from ground observations and satellite remote sensing data, we describe the spatial and temporal characteristics of these episodes and further investigated the factors that contributed to these episodes. Our results indicated that these smog episodes affected a much larger geographic region, far beyond Beijing metropolitan area, corresponding to a total area of similar to 550,000 km(2) and similar to 180 million people. The extremely cold weather in December 2012 and regional pollution transport were likely the main causes of these severe PM pollutions. In addition to aggressive emission control measures for Beijing, coordinated regional policy must be put in place to achieve more blue-sky days. Although the configuration of the current ground monitoring network may be sufficient to record PM2.5 levels in urban centers, these monitors alone cannot fully characterize the spatial pattern and track the transport of air pollution on a regional scale. Satellite remote sensing data can provide valuable information to fill the gaps left by ground monitors to create a more comprehensive picture of PM2.5.
C1 [Li, Shenshen] Chinese Acad Sci, Inst Remote Sensing & Digital Earth, State Key Lab Remote Sensing Sci, Beijing 100101, Peoples R China.
[Ma, Zongwei; Liu, Yang] Emory Univ, Rollins Sch Publ Hlth, 1518 Clifton Rd NE, Atlanta, GA 30322 USA.
[Xiong, Xiaozhen] NOAA, Ctr Satellite Applicat & Res, 5830 Univ Res Ct, College Pk, MD 20740 USA.
[Christiani, David C.; Wang, Zhaoxi] Harvard Univ, TH Chan Sch Publ Hlth, 655 Huntington Ave, Boston, MA 02115 USA.
RP Liu, Y (reprint author), Emory Univ, Rollins Sch Publ Hlth, 1518 Clifton Rd NE, Atlanta, GA 30322 USA.; Wang, ZX (reprint author), Harvard Univ, TH Chan Sch Publ Hlth, 655 Huntington Ave, Boston, MA 02115 USA.
EM mikewang@hohp.harvard.edu; yang.liu@emory.edu
RI Xiong, Xiaozhen/F-6591-2010;
OI Ma, Zongwei/0000-0003-0257-5695
FU National Natural Science Foundation of China [41471367]; Foundation of
Institute of Remote Sensing and Digital Earth, the Chinese Academy of
Sciences [Y3SJ5900CX]
FX This work was supported by the National Natural Science Foundation of
China (Grant No. 41471367), and the Foundation of Institute of Remote
Sensing and Digital Earth, the Chinese Academy of Sciences (Y3SJ5900CX).
NR 40
TC 1
Z9 1
U1 16
U2 32
PU TAIWAN ASSOC AEROSOL RES-TAAR
PI TAICHUNG COUNTY
PA CHAOYANG UNIV TECH, DEPT ENV ENG & MGMT, PROD CTR AAQR, NO 168, JIFONG E
RD, WUFONG TOWNSHIP, TAICHUNG COUNTY, 41349, TAIWAN
SN 1680-8584
EI 2071-1409
J9 AEROSOL AIR QUAL RES
JI Aerosol Air Qual. Res.
PD APR
PY 2016
VL 16
IS 4
BP 977
EP 989
DI 10.4209/aaqr.2015.01.0057
PG 13
WC Environmental Sciences
SC Environmental Sciences & Ecology
GA DK2UV
UT WOS:000374770800005
ER
PT J
AU Ronchi, E
Reneke, PA
Peacock, RD
AF Ronchi, Enrico
Reneke, Paul A.
Peacock, Richard D.
TI A conceptual fatigue-motivation model to represent pedestrian movement
during stair evacuation
SO APPLIED MATHEMATICAL MODELLING
LA English
DT Article
DE Evacuation; Egress; Stair; Fatigue; Modelling; Pedestrian
ID DYNAMICS; DESIGN; AFFORDANCES; PERFORMANCE; PERCEPTION; SIMULATION;
BEHAVIOR; HUMANS; PEOPLE; CHOICE
AB Evacuation models often neglect the impact of fatigue on pedestrian movement during stair evacuation. While a limited number of sub-models are available in the literature to represent fatigue during evacuations, they mostly refer to simple, fixed walking speed reductions due to physical fatigue. This paper introduces a more comprehensive conceptual model for the representation of the impact of fatigue on the performance of evacuees during building stair evacuation. The model is presented considering its conceptual formulation and the issues associated with its implementation. First, a comprehensive conceptual representation of the factors concerning fatigue affecting human behaviour is discussed. The model takes into account (1) physical factors (i.e., physical fatigue), and (2) psychological factors (i.e., motivation, intended as the variable balancing the perceived risk and the perceived fatigue). Second, the application of the proposed fatigue-motivation model to a hydraulic or Newtonian based evacuation modelling tool is discussed at various levels of sophistication. (C) 2015 Elsevier Inc. All rights reserved.
C1 [Ronchi, Enrico] Lund Univ, Dept Fire Safety Engn, Lund, Sweden.
[Reneke, Paul A.; Peacock, Richard D.] NIST, Fire Res Div, Gaithersburg, MD 20899 USA.
RP Ronchi, E (reprint author), Lund Univ, Dept Fire Safety Engn, Lund, Sweden.
EM enrico.ronchi@brand.lth.se
OI Ronchi, Enrico/0000-0002-2789-6359
NR 69
TC 3
Z9 3
U1 5
U2 10
PU ELSEVIER SCIENCE INC
PI NEW YORK
PA 360 PARK AVE SOUTH, NEW YORK, NY 10010-1710 USA
SN 0307-904X
EI 1872-8480
J9 APPL MATH MODEL
JI Appl. Math. Model.
PD APR
PY 2016
VL 40
IS 7-8
BP 4380
EP 4396
DI 10.1016/j.apm.2015.11.040
PG 17
WC Engineering, Multidisciplinary; Mathematics, Interdisciplinary
Applications; Mechanics
SC Engineering; Mathematics; Mechanics
GA DJ7BS
UT WOS:000374367500008
ER
PT J
AU Lee, TN
Melo, N
Smith, N
Johns, EM
Kelble, CR
Smith, RH
Ortner, PB
AF Lee, Thomas N.
Melo, Nelson
Smith, Ned
Johns, Elizabeth M.
Kelble, Christopher R.
Smith, Ryan H.
Ortner, Peter B.
TI Circulation and water renewal of Florida Bay, USA
SO BULLETIN OF MARINE SCIENCE
LA English
DT Article
ID CONTINENTAL-SHELF; VARIABILITY; SALINITY; EXCHANGE; QUALITY; KEYS
AB The circulation and exchange processes controlling transport and water renewal within the western subregion of Florida Bay, USA, are presented and compared to our previous findings for the north-central and northeast subregions of the bay. We find there is a common bank/basin flow response to wind forcing that is the primary driver of water renewal for each of the regions studied. Florida Bay is a patchwork of shallow basins surrounded by very shallow banks that are cut through with deeper channels connecting to nearby basins. We observed that, for each subregion studied, there was a net downwind basin outflow through the larger channels that was approximately balanced by a net basin inflow over the surrounding shallow banks. The resulting basin throughflows are used to estimate exchange times for renewal of western basin waters of approximately 1 mo. This exchange time is sufficient to prevent hypersalinity and degradation of water quality in the western basin, in contrast to the north-central subregion, where hypersalinity development is an annual occurrence. Our results highlight the importance of wind induced water renewal in shallow coastal bays with weak to moderate tidal exchange. In addition, we have discovered a significant clockwise circulation pattern through the western basins from strong inflows of coastal waters through Flamingo Channel that turn southward through the western basins before rejoining the coastal flow toward the Florida Keys tidal passages and Atlantic coastal zone. A practical solution to control hypersalinity, sea grass die-off, and water quality degradation of Florida Bay is proposed.
C1 [Lee, Thomas N.] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Dept Atmospher Sci, 4600 Rickenbacker Causeway, Miami, FL 33149 USA.
[Lee, Thomas N.] 880 Catfish Ave, New Smyrna Beach, FL 32169 USA.
[Melo, Nelson] Florida Int Univ, 11200 SW 8th St, Miami, FL 33199 USA.
[Smith, Ned] Florida Atlantic Univ, Harbor Branch Oceanog Inst, Dept Biol Sci, 5775 Old Dixie Highway, Ft Pierce, FL 34946 USA.
[Johns, Elizabeth M.; Smith, Ryan H.] NOAA, Atlantic Oceanog & Meteorol Lab, Phys Oceanog Div, 4301 Rickenbacker Causeway, Miami, FL 33149 USA.
[Kelble, Christopher R.] NOAA, Atlantic Oceanog & Meteorol Lab, Ocean Chem & Ecosyst Div, 4301 Rickenbacker Causeway, Miami, FL 33149 USA.
[Ortner, Peter B.] Univ Miami, Cooperat Inst Marine & Atmospher Studies, Rosenstiel Sch Marine & Atmospher Sci, 4600 Rickenbacker Causeway, Miami, FL 33149 USA.
RP Lee, TN (reprint author), Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Dept Atmospher Sci, 4600 Rickenbacker Causeway, Miami, FL 33149 USA.; Lee, TN (reprint author), 880 Catfish Ave, New Smyrna Beach, FL 32169 USA.
EM tlee8@cfl.rr.com
RI Johns, Elizabeth/I-3547-2013; Kelble, Christopher/A-8511-2008; Smith,
Ryan/A-5706-2011
OI Johns, Elizabeth/0000-0002-2181-5052; Kelble,
Christopher/0000-0003-0914-4134; Smith, Ryan/0000-0001-9824-6989
FU NOAA/CIMAS through the South Florida Program [NA17RJ1226]; NOAA's
Atlantic Oceanographic and Meteorological Laboratory
FX Our present understanding of the circulation and exchange processes of
Florida Bay was made possible by the dedicated service of marine
technicians M Graham and R Jones in maintaining the instrumentation,
constructing the specialized shallow moorings, and taking part in the
field work. We also thank B Roddy and G Rawson for their help with
instrumentation and field observations. Our interior basin study
benefited from continuity of the monthly Florida Bay surveys of the R/V
VIRGINIA K maintained by C Kelble and J Judas. The CMAN wind data were
collected as part of a cooperative agreement between FIO and NOAA/NDBC
through the SEAKEYS Program. Support for our Florida Bay circulation
studies was provided by NOAA/CIMAS through the South Florida Program
2004, Contract NA17RJ1226. Partial support for N Melo, EM Johns, CR
Kelble, and RH Smith was provided by NOAA's Atlantic Oceanographic and
Meteorological Laboratory.
NR 20
TC 1
Z9 1
U1 2
U2 7
PU ROSENSTIEL SCH MAR ATMOS SCI
PI MIAMI
PA 4600 RICKENBACKER CAUSEWAY, MIAMI, FL 33149 USA
SN 0007-4977
EI 1553-6955
J9 B MAR SCI
JI Bull. Mar. Sci.
PD APR
PY 2016
VL 92
IS 2
BP 153
EP 180
DI 10.5343/bms.2015.1019
PG 28
WC Marine & Freshwater Biology; Oceanography
SC Marine & Freshwater Biology; Oceanography
GA DL0XS
UT WOS:000375356500001
ER
PT J
AU Dixon, KW
Lanzante, JR
Nath, MJ
Hayhoe, K
Stoner, A
Radhakrishnan, A
Balaji, V
Gaitan, CF
AF Dixon, Keith W.
Lanzante, John R.
Nath, Mary Jo
Hayhoe, Katharine
Stoner, Anne
Radhakrishnan, Aparna
Balaji, V.
Gaitan, Carlos F.
TI Evaluating the stationarity assumption in statistically downscaled
climate projections: is past performance an indicator of future results?
SO CLIMATIC CHANGE
LA English
DT Article
ID CIRCULATION MODEL OUTPUT; DAILY VARIABILITY; BIAS CORRECTION;
PRECIPITATION; ASSESSMENTS; SIMULATION; INDEXES; TERMS
AB Empirical statistical downscaling (ESD) methods seek to refine global climate model (GCM) outputs via processes that glean information from a combination of observations and GCM simulations. They aim to create value-added climate projections by reducing biases and adding finer spatial detail. Analysis techniques, such as cross-validation, allow assessments of how well ESD methods meet these goals during observational periods. However, the extent to which an ESD method's skill might differ when applied to future climate projections cannot be assessed readily in the same manner. Here we present a "perfect model" experimental design that quantifies aspects of ESD method performance for both historical and late 21st century time periods. The experimental design tests a key stationarity assumption inherent to ESD methods - namely, that ESD performance when applied to future projections is similar to that during the observational training period. Case study results employing a single ESD method (an Asynchronous Regional Regression Model variant) and climate variable (daily maximum temperature) demonstrate that violations of the stationarity assumption can vary geographically, seasonally, and with the amount of projected climate change. For the ESD method tested, the greatest challenges in downscaling daily maximum temperature projections are revealed to occur along coasts, in summer, and under conditions of greater projected warming. We conclude with a discussion of the potential use and expansion of the perfect model experimental design, both to inform the development of improved ESD methods and to provide guidance on the use of ESD products in climate impacts analyses and decision-support applications.
C1 [Dixon, Keith W.; Lanzante, John R.; Nath, Mary Jo] NOAA, Geophys Fluid Dynam Lab, 201 Forrestal Rd, Princeton, NJ 08540 USA.
[Hayhoe, Katharine; Stoner, Anne] Texas Tech Univ, Climate Sci Ctr, Lubbock, TX 79409 USA.
[Radhakrishnan, Aparna] Engility, Chantilly, VA 20151 USA.
[Balaji, V.] Princeton Univ, Princeton, NJ 08544 USA.
[Gaitan, Carlos F.] Univ Oklahoma, Norman, OK 73072 USA.
RP Dixon, KW (reprint author), NOAA, Geophys Fluid Dynam Lab, 201 Forrestal Rd, Princeton, NJ 08540 USA.
EM Keith.Dixon@noaa.gov
RI Dixon, Keith/L-7120-2015;
OI Dixon, Keith/0000-0003-3044-326X; Gaitan, Carlos/0000-0003-3592-5196
FU U.S. Geologic Survey's South Central Climate Science Center [G12AC20512,
G13AC00387]; National Oceanic and Atmospheric Administration's (NOAA)
Climate Program Office; Cooperative Institute for Climate Science,
Princeton University under NOAA [NA08OAR4320752]
FX Our work benefitted from discussions with several National Climate
Predictions and Projections Platform workshop participants, Claudia
Tebaldi, and Isaac Held. We thank Vaishali Naik, Gabriel Vecchi, and two
anonymous reviewers for their constructive comments. The effort to
develop and implement this perfect model evaluation framework received
funding from the U.S. Geologic Survey's South Central Climate Science
Center (cooperative agreements G12AC20512 and G13AC00387) and the
National Oceanic and Atmospheric Administration's (NOAA) Climate Program
Office. V. Balaji is supported by the Cooperative Institute for Climate
Science, Princeton University, under NOAA award NA08OAR4320752.
NR 24
TC 4
Z9 4
U1 3
U2 7
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0165-0009
EI 1573-1480
J9 CLIMATIC CHANGE
JI Clim. Change
PD APR
PY 2016
VL 135
IS 3-4
BP 395
EP 408
DI 10.1007/s10584-016-1598-0
PG 14
WC Environmental Sciences; Meteorology & Atmospheric Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA DL2LQ
UT WOS:000375466700003
ER
PT J
AU Larson, JH
Richardson, WB
Evans, MA
Schaeffer, J
Wynne, T
Bartsch, M
Bartsch, L
Nelson, JC
Vallazza, J
AF Larson, James H.
Richardson, Wiliam B.
Evans, Mary Anne
Schaeffer, Jeff
Wynne, Timothy
Bartsch, Michelle
Bartsch, Lynn
Nelson, John. C.
Vallazza, Jon
TI Measuring spatial variation in secondary production and food quality
using a common consumer approach in Lake Erie
SO ECOLOGICAL APPLICATIONS
LA English
DT Article
DE ecosystem process; fatty acids; Lake Erie; Lampsilis siliquoidea;
nearshore; river mouths
ID FRESH-WATER MUSSELS; GREAT-LAKES; CYANOBACTERIAL BLOOM; ZEBRA MUSSELS;
FATTY-ACIDS; TRENDS; RIVER; FISH; PROFILES; INVASION
AB Lake Erie is a large lake straddling the border of the USA and Canada that has become increasingly eutrophic in recent years. Eutrophication is particularly focused in the shallow western basin. The western basin of Lake Erie is hydrodynamically similar to a large estuary, with riverine inputs from the Detroit and Maumee Rivers mixing together and creating gradients in chemical and physical conditions. This study was driven by two questions: (1) How does secondary production and food quality for consumers vary across this large mixing zone? and (2) Are there correlations between cyanobacterial abundance and secondary production or food quality for consumers? Measuring spatial and temporal variation in secondary production and food quality is difficult for a variety of logistical reasons, so here a common consumer approach was used. In a common consumer approach, individuals of a single species are raised under similar conditions until placed in the field across environmental gradients of interest. After some period of exposure, the response of that common consumer is measured to provide an index of spatial variation in conditions. Here, a freshwater mussel (Lampsilis siliquoidea) was deployed at 32 locations that spanned habitat types and a gradient in cyanobacterial abundance in the western basin of Lake Erie to measure spatial variation in growth (an index of secondary production) and fatty acid (FA) content (an index of food quality). We found secondary production was highest within the Maumee river mouth and lowest in the open waters of the lake. Mussel tissues in the Maumee river mouth also included more eicosapentaenoic and docosapentaenoic fatty acids (EPA and DPA, respectively), but fewer bacterial FAs, suggesting more algae at the base of the food web in the Maumee river mouth compared to open lake sites. The satellite-derived estimate of cyanobacterial abundance was not correlated to secondary production, but was positively related to EPA and DPA content in the mussels, suggesting more of these important FAs in locations with more cyanobacteria. These results suggest that growth of secondary consumers and the availability of important fatty acids in the western basin are centered on the Maumee river mouth.
C1 [Larson, James H.; Richardson, Wiliam B.; Bartsch, Michelle; Bartsch, Lynn; Nelson, John. C.; Vallazza, Jon] US Geol Survey, Upper Midwest Environm Sci Ctr, La Crosse, WI USA.
[Evans, Mary Anne; Schaeffer, Jeff] US Geol Survey, Great Lakes Sci Ctr, Ann Arbor, MI USA.
[Wynne, Timothy] NOAA, Natl Ocean Serv, Natl Ctr Coastal Ocean Sci, Ctr Coastal Monitoring & Assessment, 1305 East West Highway, Silver Spring, MD 20910 USA.
RP Larson, JH (reprint author), US Geol Survey, Upper Midwest Environm Sci Ctr, La Crosse, WI USA.
EM jhlarson@usgs.gov
OI Nelson, John/0000-0002-7105-0107; Bartsch, Michelle/0000-0002-9571-5564
NR 58
TC 2
Z9 2
U1 12
U2 16
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 1051-0761
EI 1939-5582
J9 ECOL APPL
JI Ecol. Appl.
PD APR
PY 2016
VL 26
IS 3
BP 873
EP 885
DI 10.1890/15-0440
PG 13
WC Ecology; Environmental Sciences
SC Environmental Sciences & Ecology
GA DK3TO
UT WOS:000374840500018
PM 27411257
ER
PT J
AU Burger, JL
Harries, ME
Bruno, TJ
AF Burger, Jessica L.
Harries, Megan E.
Bruno, Thomas J.
TI Characterization of Four Diesel Fuel Surrogates by the Advanced
Distillation Curve Method
SO ENERGY & FUELS
LA English
DT Article
ID THERMOPHYSICAL PROPERTIES; PHYSICOCHEMICAL AUTHENTICITY; MIXTURE-MODELS;
JET-A; GASOLINE; IMPROVEMENTS; IGNITION; COMBUSTION; RP-1; S-8
AB The development of surrogate fuels with measured and predicted thermophysical properties similar to their authentic refinery stream counterparts is critical for the development of alternative fuels and the optimization of engines to increase efficiency and decrease emissions. In this work, four diesel fuel surrogates, formulated according to a reliable and proven procedure, were characterized by the advanced distillation curve (ADC) method to determine the composition and enthalpy of combustion in various distillate volume fractions. Tracking the composition and enthalpy of distillate fractions provides valuable information for determining structure property relationships and also provides the basis for the development of equations of state that can describe the thermodynamic properties of these complex or simplified mixtures. This comparison showed that the volatility characteristic of the four surrogates is quite similar not only to the target diesel fuel but also to a number of other prototype alternative diesel fuels. The number of components in the surrogates affected how closely their volatility profiles resembled diesel fuel, as might be expected. The surrogate labeled V0a, consisting of just four components, was the most dissimilar to the target diesel fuel with respect to the initial boiling point and volatility curve shape. This suggests that, although minimizing the number of components greatly eases modeling and formulation efforts, caution should be used to avoid oversimplifying the surrogate mixtures.
C1 [Burger, Jessica L.; Harries, Megan E.; Bruno, Thomas J.] NIST, Appl Chem & Mat Div, Boulder, CO 80305 USA.
RP Bruno, TJ (reprint author), NIST, Appl Chem & Mat Div, Boulder, CO 80305 USA.
EM bruno@boulder.nist.gov
FU PREP postdoctoral associateship program; PREP graduate fellowship
program
FX J.B. acknowledges the PREP postdoctoral associateship program support
for research performed at NIST-Boulder for this work. M.H. acknowledges
the PREP graduate fellowship program support for research performed at
NIST-Boulder for this work.
NR 62
TC 2
Z9 2
U1 7
U2 10
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 APR
PY 2016
VL 30
IS 4
BP 2813
EP 2820
DI 10.1021/acs.energyfuels.6b00107
PG 8
WC Energy & Fuels; Engineering, Chemical
SC Energy & Fuels; Engineering
GA DK3GF
UT WOS:000374804400029
ER
PT J
AU Delgado, JP
Elliott, K
Cantelas, F
Schwemmer, RV
AF Delgado, James P.
Elliott, Kelley
Cantelas, Frank
Schwemmer, Robert V.
TI Initial Archaeological Survey of the ex-USS Independence (CVL-22)
SO JOURNAL OF MARITIME ARCHAEOLOGY
LA English
DT Article
DE Survey; Autonomous underwater vehicles; Nuclear; Deep-water; Cold War
AB The Boeing Company, collaborating with NOAA to address innovative ways to make ocean observations, provided their autonomous underwater vehicle, Echo Ranger, to conduct the first deep-water archaeological survey of the scuttled aircraft carrier USS Independence in the waters of Monterey Bay National Marine Sanctuary in March 2015. While a preliminary effort, and not comprehensive, the survey confirmed that a sonar feature (previously not proven to be an archaeological feature) charted at the location was Independence, and provided details on the condition of the wreck. At the same time, new information from declassified government reports provided more detail on Independence's use as a naval test craft for radiological decontamination as well as its use as a repository for radioactive materials at the time of its scuttling in 1951. The wreck is historically significant, but also of archaeological significance as an artifact of the early years of the atomic age and of the Cold War. This article summarizes Independence's contexts, its nuclear history, and the results of the survey of the wreck site.
C1 [Delgado, James P.; Schwemmer, Robert V.] NOAAs Off Natl Marine Sanctuaries, Maritime Heritage Program, 1305 East West Highway,SSMC4,11th Floor, Silver Spring, MD 20901 USA.
[Elliott, Kelley; Cantelas, Frank] NOAA, Off Ocean Explorat & Res, 1315 East West Highway,SSMC3,10th Floor, Silver Spring, MD USA.
[Schwemmer, Robert V.] Univ Calif Santa Barbara, West Coast Reg, Ocean Sci Educ Bldg 514,MC 6155, Santa Barbara, CA 93106 USA.
RP Delgado, JP (reprint author), NOAAs Off Natl Marine Sanctuaries, Maritime Heritage Program, 1305 East West Highway,SSMC4,11th Floor, Silver Spring, MD 20901 USA.
EM james.delgado@noaa.gov; Kelley.elliott@noaa.gov;
frank.cantelas@noaa.gov; robert.schwemmer@noaa.gov
NR 20
TC 0
Z9 0
U1 0
U2 0
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1557-2285
EI 1557-2293
J9 J MARIT ARCHAEOL
JI J. Marit. Archaeol.
PD APR
PY 2016
VL 11
IS 1
BP 9
EP 24
DI 10.1007/s11457-016-9152-9
PG 16
WC Archaeology
SC Archaeology
GA DK5IW
UT WOS:000374954600003
ER
PT J
AU Delgado, JP
AF Delgado, James P.
TI After Crossroads: The Fate of the Atomic Bomb Target Fleet
SO JOURNAL OF MARITIME ARCHAEOLOGY
LA English
DT Article
DE Naval; Atomic weapons; Cold War
AB The atomic tests at Bikini Atoll left a submerged archaeological legacy in the form of sixty-one shipwrecks at or near Bikini, Kwajalein, the California coast, and in two other lesser cases off Oahu and the coast of Washington State. Together they comprise a unique maritime cultural landscape of the Cold War, and the naval aspects of that conflict.
C1 [Delgado, James P.] NOAA, Silver Spring, MD USA.
RP Delgado, JP (reprint author), NOAA, Silver Spring, MD USA.
EM james.delgado@noaa.gov
NR 2
TC 0
Z9 0
U1 0
U2 0
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1557-2285
EI 1557-2293
J9 J MARIT ARCHAEOL
JI J. Marit. Archaeol.
PD APR
PY 2016
VL 11
IS 1
BP 25
EP 31
DI 10.1007/s11457-016-9154-7
PG 7
WC Archaeology
SC Archaeology
GA DK5IW
UT WOS:000374954600004
ER
PT J
AU Delgado, JP
AF Delgado, James P.
TI The Atomic Bomb, Operation Crossroads, the Cold War and Cold War Naval
Archaeology: A Suggested Reading List
SO JOURNAL OF MARITIME ARCHAEOLOGY
LA English
DT Article
C1 [Delgado, James P.] NOAA, Silver Spring, MD USA.
RP Delgado, JP (reprint author), NOAA, Silver Spring, MD USA.
EM james.delgado@noaa.gov
NR 34
TC 0
Z9 0
U1 1
U2 1
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 1557-2285
EI 1557-2293
J9 J MARIT ARCHAEOL
JI J. Marit. Archaeol.
PD APR
PY 2016
VL 11
IS 1
BP 33
EP 34
DI 10.1007/s11457-016-9155-6
PG 2
WC Archaeology
SC Archaeology
GA DK5IW
UT WOS:000374954600005
ER
PT J
AU Carter, BR
Williams, NL
Gray, AR
Feely, RA
AF Carter, B. R.
Williams, N. L.
Gray, A. R.
Feely, R. A.
TI Locally interpolated alkalinity regression for global alkalinity
estimation
SO LIMNOLOGY AND OCEANOGRAPHY-METHODS
LA English
DT Article
ID SATURATION STATE; SURFACE WATERS; OCEAN; CARBON; DEEP
AB We introduce methods and software for estimating total seawater alkalinity from salinity and any combination of up to four other parameters (potential temperature, apparent oxygen utilization, total dissolved nitrate, and total silicate). The methods return estimates anywhere in the global ocean with comparable accuracy to other published alkalinity estimation techniques. The software interpolates between a predetermined grid of coefficients for linear regressions onto arbitrary latitude, longitude, and depth coordinates, and thereby avoids the estimate discontinuities many similar methods return when transitioning from one regression constant set to another. The software can also return uncertainty estimates scaled by user-provided input parameter uncertainties. The methods have been optimized for the open ocean, for which we estimate globally averaged errors of 5.8-10.4 mol kg(-1) depending on which combination of regression parameters is used. We expect these methods to be especially useful for better constraining the carbonate system from measurement platformssuch as biogeochemical Argo floatsthat are only capable of measuring one carbonate system parameter (e.g., pH). It may also provide a useful way of simulating alkalinity for Earth system models that do not resolve the tracer prognostically.
C1 [Carter, B. R.] Univ Washington, Joint Inst Study Atmosphere & Ocean, Seattle, WA 98195 USA.
[Carter, B. R.; Feely, R. A.] NOAA, Pacific Marine Environm Lab, 7600 Sand Point Way Ne, Seattle, WA 98115 USA.
[Williams, N. L.] Oregon State Univ, Coll Earth Ocean & Atmospher Sci, Corvallis, OR 97331 USA.
[Gray, A. R.] Princeton Univ, Program Atmospher & Ocean Sci, Princeton, NJ 08544 USA.
RP Carter, BR (reprint author), Univ Washington, Joint Inst Study Atmosphere & Ocean, Seattle, WA 98195 USA.; Carter, BR (reprint author), NOAA, Pacific Marine Environm Lab, 7600 Sand Point Way Ne, Seattle, WA 98115 USA.
EM Brendan.carter@noaa.gov
RI Williams, Nancy/I-3472-2015;
OI Williams, Nancy/0000-0002-6541-9385; Gray, Alison/0000-0002-1644-7654;
Carter, Brendan/0000-0003-2445-0711
FU Global Ocean Ship-based Hydrographic Investigations Program (GO-SHIP)
[N8R1SE3-PRF]; US Global Carbon Data Management and Synthesis Project
[N8R3CEA-PDM]; National Oceanic and Atmospheric Administration (NOAA)
FX We would like to thank Dr. Robert Key for helpful comments early in the
process and Dr. Kelly Kearney for help with code optimization. Datasets
were acquired from the Carbon Dioxide Information and Analysis Center
(CDIAC) webpage, from the HOT-DOGS data portal
(http://hahana.soest.hawaii.edu/hot/hot-dogs/), and from the BATS data
portal (http://bats.bios.edu/). We are grateful to Kathy Tedesco of the
Climate Observation Division of the NOAA Climate Program Office for
funding for this research. Funding was provided by the Global Ocean
Ship-based Hydrographic Investigations Program (GO-SHIP) (N8R1SE3-PRF)
and the US Global Carbon Data Management and Synthesis Project
(N8R3CEA-PDM). A. R. Gray was supported by a National Oceanic and
Atmospheric Administration (NOAA) Climate and Global Change Postdoctoral
Fellowship. This is PMEL contribution number 4390 and JISAO contribution
number 2503.
NR 29
TC 2
Z9 2
U1 8
U2 8
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 1541-5856
J9 LIMNOL OCEANOGR-METH
JI Limnol. Oceanogr. Meth.
PD APR
PY 2016
VL 14
IS 4
BP 268
EP 277
DI 10.1002/lom3.10087
PG 10
WC Limnology; Oceanography
SC Marine & Freshwater Biology; Oceanography
GA DK2WE
UT WOS:000374774300004
ER
PT J
AU Baerwald, MR
Meek, MH
Stephens, MR
Nagarajan, RP
Goodbla, AM
Tomalty, KMH
Thorgaard, GH
May, B
Nichols, KM
AF Baerwald, Melinda R.
Meek, Mariah H.
Stephens, Molly R.
Nagarajan, Raman P.
Goodbla, Alisha M.
Tomalty, Katharine M. H.
Thorgaard, Gary H.
May, Bernie
Nichols, Krista M.
TI Migration-related phenotypic divergence is associated with epigenetic
modifications in rainbow trout
SO MOLECULAR ECOLOGY
LA English
DT Article
DE epigenetics; life history variation; Oncorhynchus mykiss; plasticity;
smoltification
ID PROTEIN-COUPLED RECEPTORS; ARYL-HYDROCARBON RECEPTOR; PARR-SMOLT
TRANSFORMATION; LONG-DISTANCE MIGRATION; SALMON SALMO-SALAR;
ONCORHYNCHUS-MYKISS; DNA METHYLATION; CIRCADIAN CLOCK; ATLANTIC SALMON;
STEELHEAD TROUT
AB Migration is essential for the reproduction and survival of many animals, yet little is understood about its underlying molecular mechanisms. We used the salmonid Oncorhynchus mykiss to gain mechanistic insight into smoltification, which is a morphological, physiological and behavioural transition undertaken by juveniles in preparation for seaward migration. O. mykiss is experimentally tractable and displays intra- and interpopulation variation in migration propensity. Migratory individuals can produce nonmigratory progeny and vice versa, indicating a high degree of phenotypic plasticity. One potential way that phenotypic plasticity might be linked to variation in migration-related life history tactics is through epigenetic regulation of gene expression. To explore this, we quantitatively measured genome-scale DNA methylation in fin tissue using reduced representation bisulphite sequencing of F-2 siblings produced from a cross between steelhead (migratory) and rainbow trout (nonmigratory) lines. We identified 57 differentially methylated regions (DMRs) between smolt and resident O. mykiss juveniles. DMRs were high in magnitude, with up to 62% differential methylation between life history types, and over half of the gene-associated DMRs were in transcriptional regulatory regions. Many of the DMRs encode proteins with activity relevant to migration-related transitions (e.g. circadian rhythm pathway, nervous system development, protein kinase activity). This study provides the first evidence of a relationship between epigenetic variation and life history divergence associated with migration-related traits in any species.
C1 [Baerwald, Melinda R.; Meek, Mariah H.; Goodbla, Alisha M.; Tomalty, Katharine M. H.; May, Bernie] Univ Calif Davis, Dept Anim Sci, Davis, CA 95616 USA.
[Stephens, Molly R.] Univ Calif Merced, Sch Nat Sci, Merced, CA 95343 USA.
[Nagarajan, Raman P.] GlaxoSmithKline, Canc Epigenet Discovery Performance Unit, Collegeville, PA 19426 USA.
[Thorgaard, Gary H.] Washington State Univ, Sch Biol Sci, Pullman, WA 99164 USA.
[Thorgaard, Gary H.] Washington State Univ, Ctr Reprod Biol, Pullman, WA 99164 USA.
[Nichols, Krista M.] NOAA, Conservat Biol Div, NW Fisheries Sci Ctr, Natl Marine Fisheries Serv, 2725 Montlake Blvd E, Seattle, WA 98112 USA.
RP Baerwald, MR (reprint author), Univ Calif Davis, Dept Anim Sci, Davis, CA 95616 USA.
EM mrbaerwald@ucdavis.edu
OI Meek, Mariah/0000-0002-3219-4888
FU California Department of Fish and Wildlife [P0740017]; NIH [S10RR029668,
S10RR027303]
FX This work was made possible by funding from the California Department of
Fish and Wildlife, contract number P0740017. We thank Michael Miller at
University of California, Davis, for assistance with data processing
scripts for using the U.S. O. mykiss draft genome assembly. We are
grateful to Paul Wheeler at Washington State University for his
instrumental role in producing original clonal lines and F2
doubled haploid individuals. We thank Jessica Petersen and three
anonymous reviewers for their helpful comments. This work used the
Vincent J. Coates Genomics Sequencing Laboratory at UC Berkeley,
supported by NIH S10 Instrumentation Grants S10RR029668 and S10RR027303.
NR 118
TC 12
Z9 12
U1 26
U2 48
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0962-1083
EI 1365-294X
J9 MOL ECOL
JI Mol. Ecol.
PD APR
PY 2016
VL 25
IS 8
BP 1785
EP 1800
DI 10.1111/mec.13231
PG 16
WC Biochemistry & Molecular Biology; Ecology; Evolutionary Biology
SC Biochemistry & Molecular Biology; Environmental Sciences & Ecology;
Evolutionary Biology
GA DK2WY
UT WOS:000374776300012
PM 25958780
ER
PT J
AU Weng, FZ
Yang, H
AF Weng, Fuzhong
Yang, Hu
TI Validation of ATMS Calibration Accuracy Using Suomi NPP Pitch Maneuver
Observations
SO REMOTE SENSING
LA English
DT Article
DE ATMS; Calibration; Pitch-Maneuver
ID GRIDPOINT TEMPERATURE ANOMALIES; RADIOSONDE VALIDATION; MSU CHANNEL-2;
CONSTRUCTION; PRECISION
AB The Suomi National Polar-orbiting Partnership (SNPP) satellite was launched on 28 October, 2011, and carries the Advanced Technology Microwave Sounder (ATMS) onboard. Currently, ATMS performance in orbit is very stable and the calibration parameters (e.g., noise and accuracy) meet specifications. This study documents an ATMS calibration error budget model and its results for community reference. The calibration accuracy is also verified with the ATMS pitch maneuver observations of cold space. It is shown that the ATMS pitch maneuver cold space observations at center positions are inconsistent with the values predicted by the instrument calibration error budget model. The biases also depend on scan angle. This scan-angle dependence may be caused by the ATMS plane reflector emission. Thus, a physical model is developed to simulate the radiation emitted from the reflector and is recommended as part of ATMS radiance calibration to further improve the sensor data record (SDR) data quality.
C1 [Weng, Fuzhong] NOAA, Ctr Satellite Applicat & Res, College Pk, MD 20740 USA.
[Yang, Hu] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20740 USA.
RP Weng, FZ (reprint author), NOAA, Ctr Satellite Applicat & Res, College Pk, MD 20740 USA.
EM Fuzhong.Weng@noaa.gov; huyang@umd.edu
RI Weng, Fuzhong/F-5633-2010
OI Weng, Fuzhong/0000-0003-0150-2179
FU NOAA Joint Polar Satellite System (JPSS) Program Office
FX The views expressed in this publication are those of the authors and do
not necessarily represent those of NOAA. The research is supported by
NOAA Joint Polar Satellite System (JPSS) Program Office.
NR 17
TC 0
Z9 0
U1 1
U2 2
PU MDPI AG
PI BASEL
PA POSTFACH, CH-4005 BASEL, SWITZERLAND
SN 2072-4292
J9 REMOTE SENS-BASEL
JI Remote Sens.
PD APR
PY 2016
VL 8
IS 4
AR 332
DI 10.3390/rs8040332
PG 14
WC Remote Sensing
SC Remote Sensing
GA DK8DD
UT WOS:000375156500065
ER
PT J
AU Zhao, XP
Heidinger, AK
Walther, A
AF Zhao, Xuepeng
Heidinger, Andrew K.
Walther, Andi
TI Climatology Analysis of Aerosol Effect on Marine Water Cloud from
Long-Term Satellite Climate Data Records
SO REMOTE SENSING
LA English
DT Article
DE aerosol; cloud; climate data record; aerosol indirect effect; satellite
ID MOMENT MICROPHYSICS PARAMETERIZATION; CHARACTERIZATION EXPERIMENT ACE-2;
BOUNDARY-LAYER CLOUDS; PART I; ANTHROPOGENIC AEROSOLS; NUMBER
CONCENTRATION; RADIATIVE PROPERTIES; CONDENSATION NUCLEI; POLLUTION
AEROSOL; OPTICAL-THICKNESS
AB Satellite aerosol and cloud climate data records (CDRs) have been used successfully to study the aerosol indirect effect (AIE). Data from the Advanced Very High Resolution Radiometer (AVHRR) now span more than 30 years and allow these studies to be conducted from a climatology perspective. In this paper, AVHRR data are used to study the AIE on water clouds over the global oceans. Correlation analysis between aerosol optical thickness (AOT) and cloud parameters, including cloud droplet effective radius (CDER), cloud optical depth (COD), cloud water path (CWP), and cloud cover fraction (CCF), is performed. For the first time from satellite observations, the long-term trend in AIE over the global oceans is also examined. Three regimes have been identified: (1) AOT < 0.08, where CDER increases with AOT; (2) 0.08 < AOT < 0.3, where CDER generally decreases when AOT increases; and (3) AOT > 0.3, where CDER first increases with AOT and then levels off. AIE is easy to manifest in the CDER reduction in the second regime (named Regime 2), which is identified as the AIE sensitive/effective regime. The AIE manifested in the consistent changes of all four cloud variables (CDER, COD, CWP, and CCF) together is located only in limited areas and with evident seasonal variations. The long-term trend of CDER changes due to the AIE of AOT changes is detected and falls into three scenarios: Evident CDER decreasing (increasing) with significant AOT increasing (decreasing) and evident CDER decreasing with limited AOT increasing but AOT values fall in the AIE sensitive Regime 2.
C1 [Zhao, Xuepeng] NOAA, NCEI, NESDIS, Asheville, NC 28801 USA.
[Heidinger, Andrew K.] NOAA, Ctr Satellite Applicat & Res STAR, NESDIS, Madison, WI 53706 USA.
[Walther, Andi] UW Madison, CIMSS, Madison, WI 53706 USA.
RP Zhao, XP (reprint author), NOAA, NCEI, NESDIS, Asheville, NC 28801 USA.
EM xuepeng.zhao@noaa.gov; andrew.heidinger@noaa.gov;
andi.walther@ssec.wisc.edu
RI Heidinger, Andrew/F-5591-2010;
OI Heidinger, Andrew/0000-0001-7631-109X; Zhao, Xuepeng/0000-0001-6491-3907
FU NOAA CDR program
FX This work is supported by the NOAA CDR program managed at the National
Centers of Environment Information (NCEI) of NOAA/NESDIS. NCEI internal
reviewers helped improve the paper. The constructive comments and
suggestions provided by four anonymous reviewers were very helpful for
improving the paper. The views, opinions, and findings contained in this
paper are those of the author(s) and should not be construed as an
official National Oceanic and Atmospheric Administration or U.S.
Government position, policy, or decision.
NR 85
TC 0
Z9 0
U1 3
U2 5
PU MDPI AG
PI BASEL
PA POSTFACH, CH-4005 BASEL, SWITZERLAND
SN 2072-4292
J9 REMOTE SENS-BASEL
JI Remote Sens.
PD APR
PY 2016
VL 8
IS 4
AR 300
DI 10.3390/rs8040300
PG 22
WC Remote Sensing
SC Remote Sensing
GA DK8DD
UT WOS:000375156500033
ER
PT J
AU Castro, JM
Beavers, A
AF Castro, Janine M.
Beavers, Aaron
TI Providing Aquatic Organism Passage in Vertically Unstable Streams
SO WATER
LA English
DT Article
DE fish passage; barriers; culverts; incision; grade stabilization; stream
evolution
ID FISH PASSAGE; WASHINGTON; ROADS
AB Aquatic organism passage barriers have been identified as one of the key impediments to recovery of salmonids and other migratory aquatic organisms in the Pacific Northwest of the United States. As such, state and federal agencies invest millions of dollars annually to address passage barriers. Because many barriers function as ad hoc grade control structures, their removal and/or replacement can unwittingly set off a cascade of effects that can negatively impact the very habitat and passage that project proponents seek to improve. The resultant vertical instability can result in a suite of effects that range from floodplain disconnection and loss of backwater and side channel habitat, to increased levels of turbidity. Risk assessment, including an evaluation of both the stage of stream evolution and a longitudinal profile analysis, provides a framework for determining if grade control is warranted, and if so, what type of structure is most geomorphically appropriate. Potential structures include placement of large wood and roughness elements, and constructed riffles, step-pools, and cascades. The use of structure types that mimic natural reach scale geomorphic analogues should result in improved aquatic organism passage, increased structural resilience, and reduced maintenance.
C1 [Castro, Janine M.] US Fish & Wildlife Serv, 2600 SE 98th Ave,Suite 100, Portland, OR 97266 USA.
[Beavers, Aaron] Natl Marine Fisheries Serv, 1201 Lloyd Blvd, Portland, OR 97232 USA.
RP Castro, JM (reprint author), US Fish & Wildlife Serv, 2600 SE 98th Ave,Suite 100, Portland, OR 97266 USA.
EM Janine_M_Castro@fws.gov; Aaron.Beavers@noaa.gov
OI Castro, Janine/0000-0002-1951-7507
FU United States Fish and Wildlife Service; Oregon Fish and Wildlife
Office; National Oceanic and Atmospheric Administration, National Marine
Fisheries Service, Portland Oregon Office
FX The development of this manuscript was supported solely by the authors'
employers, the United States Fish and Wildlife Service, Oregon Fish and
Wildlife Office, and the National Oceanic and Atmospheric
Administration, National Marine Fisheries Service, Portland Oregon
Office.
NR 40
TC 0
Z9 0
U1 4
U2 6
PU MDPI AG
PI BASEL
PA POSTFACH, CH-4005 BASEL, SWITZERLAND
SN 2073-4441
J9 WATER-SUI
JI Water
PD APR
PY 2016
VL 8
IS 4
AR 133
DI 10.3390/w8040133
PG 20
WC Water Resources
SC Water Resources
GA DK8DK
UT WOS:000375157200024
ER
PT J
AU Orbach, DN
Marshall, CD
Wursig, B
Mesnick, SL
AF Orbach, Dara N.
Marshall, Christopher D.
Wuersig, Bernd
Mesnick, Sarah L.
TI Variation in Female Reproductive Tract Morphology of the Common
Bottlenose Dolphin (Tursiops truncatus)
SO ANATOMICAL RECORD-ADVANCES IN INTEGRATIVE ANATOMY AND EVOLUTIONARY
BIOLOGY
LA English
DT Article
DE genital diversity; reproductive tract morphology; reproductive biology;
vaginal fold; common bottlenose dolphin
ID SPERM COMPETITION; AGE; GROWTH; RAT; SPERMATOZOA; EVOLUTION; PORPOISE;
EJECTION; MUSCLES; OVARIAN
AB Cetaceans exhibit vaginal folds, unusual protrusions of the vaginal wall into the vaginal lumen. Inconsistent terminology and a lack of anatomical landmarks in the literature have hindered comparative studies of the form and function of vaginal folds. Our objectives are to: (1) develop a standardized measurement protocol for the reproductive tracts of female cetaceans, (2) assess variation in morphometrics within the common bottlenose dolphin (Tursiops truncatus), and (3) determine if vaginal muscle is skeletal, and therefore of somatic origin in this species. We selected 15 measurements to characterize female reproductive tracts and evaluated variability using fresh or frozen-thawed specimens from southeastern USA representing a range of sexual maturity states and reproductive states (n=18 specimens). Presence of skeletal muscle and variation in the density of muscle banding were assessed using 90 histological samples (n=5 specimens). Analyses of the gross morphological data revealed that the dolphins generally had one large vaginal fold that bisected the vaginal lumen. Vaginal morphology was similar for sexually mature and immature specimens and across reproductive states. The histological data revealed that the vaginal musculature consisted of smooth muscle, consistent with other mammals, leading us to conclude that vaginal contractions are likely under autonomic rather than somatic control. No differences were found in the density of smooth muscle banding among vaginal regions or sexual maturity states. Our systematic protocol lays the foundation for evaluating the function (e.g., sexual selection, natural selection) and evolution of vaginal folds. (C) 2016 Wiley Periodicals, Inc.
C1 [Orbach, Dara N.; Marshall, Christopher D.; Wuersig, Bernd] Texas A&M Univ, Dept Marine Biol, 200 Seawolf Pkwy, Galveston, TX 77553 USA.
[Marshall, Christopher D.; Wuersig, Bernd] Texas A&M Univ, Dept Wildlife & Fisheries Sci, College Stn, TX 77843 USA.
[Mesnick, Sarah L.] NOAA, Natl Marine Fisheries Serv, SW Fisheries Sci Ctr, 8901 La Jolla Shores Dr, La Jolla, CA 92037 USA.
RP Orbach, DN (reprint author), Texas A&M Univ, Dept Marine Biol, 200 Seawolf Pkwy, Galveston, TX 77553 USA.; Mesnick, SL (reprint author), NOAA, Natl Marine Fisheries Serv, SW Fisheries Sci Ctr, 8901 La Jolla Shores Dr, La Jolla, CA 92037 USA.
EM dnorbach@gmail.com; sarah.mesnick@noaa.gov
FU Natural Science and Engineering Research Council of Canada
[PGSD2-420080-2012]; American Museum of Natural History Lerner Gray
Memorial Fund; Texas Sea Grant; Texas Institute of Oceanography Graduate
Research Fellowship
FX Grant sponsor: Natural Science and Engineering Research Council of
Canada Postgraduate Scholarship-Doctoral (to D. N. O.); Grant number:
PGSD2-420080-2012; Grant sponsors: American Museum of Natural History
Lerner Gray Memorial Fund (to D. N. O.), Texas Sea Grant Grants-In-Aid
of Graduate Student Research (to D. N. O.), Texas Institute of
Oceanography Graduate Research Fellowship (to D. N. O.).
NR 77
TC 1
Z9 1
U1 5
U2 7
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 1932-8486
EI 1932-8494
J9 ANAT REC
JI Anat. Rec.
PD APR
PY 2016
VL 299
IS 4
BP 520
EP 537
DI 10.1002/ar.23318
PG 18
WC Anatomy & Morphology
SC Anatomy & Morphology
GA DJ7FU
UT WOS:000374378100012
PM 26788790
ER
PT J
AU Kartalev, M
Keremidarska, V
Dryer, M
AF Kartalev, M.
Keremidarska, V.
Dryer, M.
TI Revisiting the Single-Fluid Modeling of the Solar Wind-Comet
Interaction: Closer Look at the Cometosheath
SO EARTH MOON AND PLANETS
LA English
DT Article
DE Solar wind-comet interaction; Single-fluid model; Mystery region; Comet
67P/C-G; Magnetic cavity boundary
ID PLASMA ENVIRONMENT; FLOW; 67P/CHURYUMOV-GERASIMENKO; MHD; PREDICTIONS;
SKJELLERUP; ATMOSPHERE; P/HALLEY
AB Earlier developed single fluid gas-dynamic model of solar wind-comet ionosphere interaction is applied to reveal some specifics in the morphology of the shocked "contaminated" solar wind region (cometosheath). The model is based on the Euler equations with added mass-loading, mass-loss and frictional force terms. Numerous reactions are taken into account in these terms including photoionization, charge transfer, dissociative recombination and ion-neutral frictional force. The electromagnetic terms are omitted, thus reducing the MHD single-fluid system of equations to gas-dynamic one. The used shock-fitting numerical scheme allows the separation of distinct areas formed by the considered interaction and exploration of their properties in detail. Attention is focused on the region between the shock wave and the contact surface as well as on the positions of these boundaries. Accurate examination of the distribution of density, temperature and velocity reveals spatial variations that resemble the variations registered by a number of spacecraft in the vicinity of comets. No specific comparisons with data are made at this stage. Two very first events of the Rosetta spacecraft's crossing of the magnetic cavity boundary around Comet 67P/Churyumov-Gerasimenko are discussed using a "faux-transient" application of our steady-state model.
C1 [Kartalev, M.; Keremidarska, V.] Bulgarian Acad Sci, Inst Mech, Sofia, Bulgaria.
[Keremidarska, V.] Microsoft Inc, Seattle, WA USA.
[Dryer, M.] NOAA, Space Weather Predict Ctr, Boulder, CO 80305 USA.
[Dryer, M.] Carmel Res Ctr, Santa Monica, CA 90406 USA.
RP Kartalev, M (reprint author), Bulgarian Acad Sci, Inst Mech, Sofia, Bulgaria.
EM m.kartalev@yahoo.com
FU International Space Science Institute (ISSI) in Bern
FX The authors are members of an International Team in Space Science on
modeling cometary environments sponsored by the International Space
Science Institute (ISSI) in Bern, and we thank ISSI for hospitality
during part of this work. The authors thank Prof. M. Lebedev from Moscow
State University for a very useful discussion and recommendations and
Prof. Susan McKenna-Lawlor of Space Technology Ireland, Ltd., for her
suggestion concerning the existence of the important "mystery" boundary
discussed herein. We thank the Teams of Rosetta Plasma Consortium
(RPC)-IGEP/IC, Rosetta Orbiter Spectrometer for Ion and Neutral Analysis
(ROSINA)-UBern/ BIRA/LATMOS/LMM/ IRAP/MPS/SwRI/TUB/Umich and Optical,
Spectroscopic, and Infrared Remote Imaging System (OSIRIS)-MPS/UPD/LAM/
IAA/SSO/INTA/UPM/ DASP/IDA for providing preliminary information about
the 29 July comet outburst event in ESA Internet sites.
NR 49
TC 0
Z9 0
U1 0
U2 0
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0167-9295
EI 1573-0794
J9 EARTH MOON PLANETS
JI Earth Moon Planets
PD APR
PY 2016
VL 117
IS 2-3
BP 109
EP 132
DI 10.1007/s11038-016-9485-2
PG 24
WC Astronomy & Astrophysics; Geosciences, Multidisciplinary
SC Astronomy & Astrophysics; Geology
GA DK1LB
UT WOS:000374672700005
ER
PT J
AU Deary, AL
Metscher, B
Brill, RW
Hilton, EJ
AF Deary, Alison L.
Metscher, Brian
Brill, Richard W.
Hilton, Eric J.
TI Shifts of sensory modalities in early life history stage estuarine
fishes (Sciaenidae) from the Chesapeake Bay using X-ray micro computed
tomography
SO ENVIRONMENTAL BIOLOGY OF FISHES
LA English
DT Article
DE Drums; Ecomorphology; Ontogeny; Larvae; Foraging habitat; Brain
ID BRAIN-AREAS; FIBER-CONNECTIONS; INNER-EAR; SEBASTISCUS-MARMORATUS;
NAVODON-MODESTUS; MORPHOLOGY; TELEOST; TELENCEPHALON; ORGANIZATION;
PATTERNS
AB Increases in human populations along coasts have altered the estuarine nursery habitats that are important for many aquatic organisms. These perturbations include changes to the sensory environment due to increased turbidity resulting from runoff and nutrient loading; these changes are occurring faster than fish species can become adapted to the new prevailing conditions. However, understanding how modifications to the sensory environment impacts fishes during early life history stages (ELHS) requires understanding the senses used to locate food and evade predators and how they change during ontogeny. The drums (Sciaenidae) exhibit substantial morphological diversity in their peripheral sense organs as adults. We, therefore, used the relative volumes of their brain structures to assess ontogenetic changes in the sensory modalities of sciaenid species from different foraging guilds. Early stage sciaenids were imaged using X-ray micro computed tomography. The optic tract was the largest sensory region, suggesting that vision is the primary sensory modality in sciaenids, regardless of size, species, or foraging habitat. There were differences in the relative proportions of the other sensory areas according to foraging guild. These differences suggest that Cynoscion nebulosus (a pelagic forager) relies on audition and mechanoreception through ontogeny to augment vision, whereas Sciaenops ocellatus (a generalist forager) uses olfaction, audition, and mechanoreception. In contrast, Leiostomus xanthurus (a benthic forager) relies on olfaction and gustation. We propose that the ontogenetic trends in sensory modality described in sciaenids from the Chesapeake Bay (USA) can be used in future research to ascertain the potential species-specific impacts of water quality change on ELHS fishes.
C1 [Deary, Alison L.; Hilton, Eric J.] Virginia Inst Marine Sci, Coll William & Mary, POB 1346,1375 Greate Rd, Gloucester Point, VA 23690 USA.
[Metscher, Brian] Univ Vienna, Dept Theoret Biol, Althanstr 14, A-1090 Vienna, Austria.
[Brill, Richard W.] Natl Marine Fisheries Serv, Northeast Fisheries Sci Ctr, James J Howard Marine Sci Lab, 74 Magruder Rd, Highlands, NJ 07732 USA.
[Deary, Alison L.] Univ So Mississippi, Gulf Coast Res Lab, Dept Coastal Sci, 703 East Beach Dr, Ocean Springs, MS 39564 USA.
RP Deary, AL (reprint author), Univ So Mississippi, Gulf Coast Res Lab, Dept Coastal Sci, 703 East Beach Dr, Ocean Springs, MS 39564 USA.
EM al.deary15@gmail.com
NR 52
TC 1
Z9 1
U1 2
U2 7
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0378-1909
EI 1573-5133
J9 ENVIRON BIOL FISH
JI Environ. Biol. Fishes
PD APR
PY 2016
VL 99
IS 4
BP 361
EP 375
DI 10.1007/s10641-016-0479-8
PG 15
WC Ecology; Marine & Freshwater Biology
SC Environmental Sciences & Ecology; Marine & Freshwater Biology
GA DK1KH
UT WOS:000374670500004
ER
PT J
AU Becker, E
van den Dool, H
AF Becker, Emily
van den Dool, Huug
TI Probabilistic Seasonal Forecasts in the North American Multimodel
Ensemble: A Baseline Skill Assessment
SO JOURNAL OF CLIMATE
LA English
DT Article
ID TO-INTERANNUAL PREDICTION; CLIMATE; SYSTEM; SIZE; RATIONALE; SUCCESS;
SCORE
AB The North American Multimodel Ensemble (NMME) forecasting system has been continuously producing seasonal forecasts since August 2011. The NMME, with its suite of diverse models, provides a valuable opportunity for characterizing forecast confidence using probabilistic forecasts. The current experimental probabilistic forecast product (in map format) presents the most likely tercile for the seasonal mean value, chosen out of above normal, near normal, or below normal categories, using a nonparametric counting method to determine the probability of each class. The skill of the 3 -month -mean probabilistic forecasts of 2-m surface temperature (T2m), precipitation rate, and sea surface temperature is assessed using forecasts from the 29-yr (1982-2010) NMME hindcast database. Three forecast configurations are considered: a full six model NMME; a "mini-NMME" with 24 members, four each from six models; and the 24 -member CFSv2 alone. Skill is assessed on the cross -validated hindcasts using the Brier skill score (BSS); forecast reliability and resolution are also assessed. This study provides a baseline skill assessment of the current method of creating probabilistic forecasts from the NMME system.
For forecasts in the above- and below -normal terciles for all variables and geographical regions examined in this study, BSS for NMME forecasts is higher than BSS for CFSv2 forecasts. Nitio-3.4 forecasts from the full NMME and the mini-NMME receive nearly identical BSS that are higher than BSS for CFSv2 forecasts. Even systems with modest BSS, such as T2m in the Northern Hemisphere, have generally high reliability, as shown in reliability diagrams.
C1 [Becker, Emily; van den Dool, Huug] NOAA, Climate Predict Ctr, NCEP, NWS, College Pk, MD 20740 USA.
RP Becker, E (reprint author), NOAA, Ctr Weather & Climate Predict, 5830 Univ Res Court, College Pk, MD 20740 USA.
EM emily.becker@noaa.gov
FU MAPP program award; NOAA; NSF; NASA; DOE
FX The authors thank the three anonymous reviewers whose comments greatly
improved this manuscript. This study was supported by a MAPP program
award. NMME project and data dissemination is supported by NOAA, NSF,
NASA, and DOE. The NMME forecasts and data archive are created, updated,
and maintained by NCEP, IRI, and NCAR personnel.
NR 29
TC 1
Z9 1
U1 4
U2 9
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 APR
PY 2016
VL 29
IS 8
BP 3015
EP 3026
DI 10.1175/JCLI-D-14-00862.1
PG 12
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DK7ZN
UT WOS:000375146100008
ER
PT J
AU Wilson, C
Sastre, AV
Hoffmeyer, M
Rowntree, VJ
Fire, SE
Santinelli, NH
Ovejero, SD
D'Agostino, V
Maron, CF
Doucette, GJ
Broadwater, MH
Wang, ZH
Montoya, N
Seger, J
Adler, FR
Sironi, M
Uhart, MM
AF Wilson, Cara
Viviana Sastre, A.
Hoffmeyer, Monica
Rowntree, Victoria J.
Fire, Spencer E.
Santinelli, Norma H.
Diaz Ovejero, Soledad
D'Agostino, Valeria
Maron, Carina F.
Doucette, Gregory J.
Broadwater, Margaret H.
Wang, Zhihong
Montoya, Nora
Seger, Jon
Adler, Frederick R.
Sironi, Mariano
Uhart, Marcela M.
TI Southern right whale (Eubalaena australis) calf mortality at Peninsula
Valdes, Argentina: Are harmful algal blooms to blame?
SO MARINE MAMMAL SCIENCE
LA English
DT Article
DE Eubalaena australis; Peninsula Valdes; calf mortality; Pseudo-nitzschia
spp; Alexandrium tamarense; PSTs; DA; SeaWiFS; MODIS; toxins; harmful
algal blooms
ID PARALYTIC SHELLFISH TOXINS; TAMARENSE LEBOUR BALECH; SAN MATIAS GULF;
DOMOIC ACID; ALEXANDRIUM-TAMARENSE; KARENIA-BREVIS; GOLFO-NUEVO;
OF-MEXICO; RED-TIDE; DINOFLAGELLATE
AB Peninsula Valdes (PV) in Argentina is an important calving ground for southern right whales (SRWs, Eubalaena australis). Since 2005, right whale mortality has increased at PV, with most of the deaths (similar to 90%) being calves <3 mo old. We investigated the potential involvement of harmful algal blooms (HABs) in these deaths by examining data that include: timing of the SRW deaths, biotoxins in samples from dead SRWs, abundances of the diatom, Pseudo-nitzschia spp., and the dinoflagellate, Alexandrium tamarense, shellfish harvesting closure dates, seasonal availability of whale prey at PV and satellite chlorophyll data. Evidence of the whales' exposure to HAB toxins includes trace levels of paralytic shellfish toxins (PSTs) and domoic acid (DA) in tissues of some dead whales, and fragments of Pseudo-nitzschia spp. frustules in whale feces. Additionally, whales are present at PV during both closures of the shellfish industry (due to high levels of PSTs) and periods with high levels of Pseudo-nitzschia spp. and A. tamarense. There is a positive statistical relationship between monthly Pseudo-nitzschia densities (but not A. tamarense) and calf deaths in both gulfs of PV.
C1 [Wilson, Cara] NOAA, Div Environm Res, Southwest Fisheries Sci Ctr, NMFS, 99 Pacific St,Suite 255A, Monterey, CA 93940 USA.
[Viviana Sastre, A.; Santinelli, Norma H.; Diaz Ovejero, Soledad] Univ Nacl Patagonia San Juan Bosco, FCN, Lab Hidrobiol, Trelew, Chubut, Argentina.
[Hoffmeyer, Monica] CCTBB CONICET, Inst Argentino Oceanog, B8000FWB, Bahia Blanca, Buenos Aires, Argentina.
[Hoffmeyer, Monica] Univ Tecnol Nacl, Fac Reg Bahia Blanca, 11 Abril 461,B8000MLI, Bahia Blanca, Buenos Aires, Argentina.
[Rowntree, Victoria J.; Maron, Carina F.; Sironi, Mariano; Uhart, Marcela M.] Southern Right Whale Hlth Monitoring Program, RA-9120 Puerto Madryn, Chubut, Argentina.
[Rowntree, Victoria J.; Maron, Carina F.; Seger, Jon; Adler, Frederick R.] Univ Utah, Dept Biol, Salt Lake City, UT 84112 USA.
[Fire, Spencer E.; Doucette, Gregory J.; Broadwater, Margaret H.; Wang, Zhihong] NOAA, NOS, Natl Ctr Coastal Ocean Sci, Ctr Coastal Environm Hlth & Biomol Res, 219 Ft Johnson Rd, Charleston, SC 29412 USA.
[Fire, Spencer E.] Florida Inst Technol, 150 W Univ Blvd, Melbourne, FL 32901 USA.
[D'Agostino, Valeria] Consejo Nacl Invest Cient & Tecn, Ctr Nacl Patagon CENPAT, Puerto Madryn, Chubut, Argentina.
[Montoya, Nora] Inst Nacl Invest & Desarrollo Pesquero INIDEP, 7602HSA, Mar Del Plata, Buenos Aires, Argentina.
[Adler, Frederick R.] Univ Utah, Dept Math, Salt Lake City, UT 84112 USA.
[Sironi, Mariano] Univ Nacl Cordoba, Diversidad Anim 2, RA-5000 Cordoba, Argentina.
[Uhart, Marcela M.] Univ Calif Davis, Sch Vet Med, Hlth Inst 1, 1089 Vet Med Dr, Davis, CA 95616 USA.
RP Wilson, C (reprint author), NOAA, Div Environm Res, Southwest Fisheries Sci Ctr, NMFS, 99 Pacific St,Suite 255A, Monterey, CA 93940 USA.
EM cara.wilson@noaa.gov
FU Office of Protected Resources of the US National Marine Fisheries
Service; National Ocean and Atmospheric Administration (NOAA)
[DG133F-02-SE-0901, DG-133F-06-SE-5823, DG133F07SE4651]; U.S. Marine
Mammal Commission [E4047315, E4061768]; National Agency for Science and
Technology Promotion of Argentina (ANPCYT) [2096, 3091]; Ocean
Foundation; Island Foundation Inc.; Pacific Life Foundation; Lawrence
Foundation; Research and Education Opportunities International (CREOI)
grant; Wildlife Conservation Society; Ocean Alliance
FX We are grateful to the Office of Protected Resources of the US National
Marine Fisheries Service, National Ocean and Atmospheric Administration
(NOAA) (Orders DG133F-02-SE-0901, DG-133F-06-SE-5823 and
DG133F07SE4651), the U.S. Marine Mammal Commission (Grants E4047315 and
E4061768), the National Agency for Science and Technology Promotion of
Argentina (ANPCYT) (Grants 2011-No 2096 and 2014-No 3091) the Ocean
Foundation, the Island Foundation Inc., the Pacific Life Foundation, the
Lawrence Foundation, Research and Education Opportunities International
(CREOI) grant to CFM, the Wildlife Conservation Society, and Ocean
Alliance for funding this research. We specially thank T. Rowles for her
support. Thanks to the divers and helmsmen of the Provincial Plan for
Prevention and Control of Red Tide (Chubut Province) for the collection
of phytoplankton samples. Thanks to all volunteers and members of
Southern Right Whale Health Monitoring Program team for their long hours
in the field and lab collecting and curating samples particularly, V.
Rago, L. La Sala, L. Pozzi, L. Musmeci, A. Chirife, M. Di Martino, and
L. Beltramino; the invaluable support of many kinds by D. Taboada, R.
Schteinbarg, M. Ricciardi, and volunteers of the Instituto de
Conservacion de Ballenas (ICB). Thanks to T. Knott and B. Haynes at
NOAA/NOS for assistance with biotoxin extractions and analyses. Thanks
to the Ministry of Fisheries of Chubut province for providing data on
timing of shell fishery closures and the data management group at the
NOAA/NMFS Environmental Research Division for making satellite data
easily accessible through the ERDDAP server developed by R. Simons.
Thanks to R. Brownell and L. DeWitt for their comments on earlier
versions of the manuscript. Research permits for this work were issued
annually by the Direccion de Fauna y Flora Silvestre and the
Subsecretaria de Turismo y Areas Protegidas of Chubut Province,
Argentina. Contribution INIDEP No. 1940.
NR 87
TC 2
Z9 2
U1 8
U2 16
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0824-0469
EI 1748-7692
J9 MAR MAMMAL SCI
JI Mar. Mamm. Sci.
PD APR
PY 2016
VL 32
IS 2
BP 423
EP 451
DI 10.1111/mms.12263
PG 29
WC Marine & Freshwater Biology; Zoology
SC Marine & Freshwater Biology; Zoology
GA DJ6UR
UT WOS:000374349200001
ER
PT J
AU Gruden, P
White, PR
Oswald, JN
Barkley, Y
Cerchio, S
Lammers, M
Baumann-Pickering, S
AF Gruden, Pina
White, Paul R.
Oswald, Julie N.
Barkley, Yvonne
Cerchio, Salvatore
Lammers, Marc
Baumann-Pickering, Simone
TI Differences in oscillatory whistles produced by spinner(Stenella
longirostris) and pantropical spotted (Stenella attenuata) dolphins
SO MARINE MAMMAL SCIENCE
LA English
DT Article
DE oscillatory whistles; whistle; global features; decision rule; dolphin;
spinner dolphin; pantropical spotted dolphin; Stenella longirostris;
Stenella attenuata; towed hydrophone array
ID BOTTLE-NOSED DOLPHINS; EASTERN TROPICAL PACIFIC; TURSIOPS-TRUNCATUS;
SPINNER DOLPHINS; GEOGRAPHIC-VARIATION; ECHOLOCATION CLICKS; AUTOMATIC
DETECTION; CLASSIFICATION; BEHAVIOR; WHALES
AB Acoustic recordings of two closely related species, spinner dolphin (Stenella longirostris) and pantropical spotted dolphin (Stenella attenuata), were investigated from four different geographic locations: two in the Central Tropical Pacific, one in the Eastern Tropical Pacific and one in the Indian Ocean. The two delphinid species occur in tropical and warm temperate waters, with overlapping ranges. They produce very similar vocalizations, but at the same time their calls exhibit a certain degree of intraspecific variation among different geographic locations as has been observed in other delphinid species. Oscillatory whistles (whistles with at least two oscillations in their frequency contours) were identified and manually extracted from the recordings. Whistles with four or more maxima (oscillations) occurred only in spinner dolphins and they were present in all geographic regions investigated. In addition, the oscillatory whistles with two and three maxima were significantly more frequent in spinner than in spotted dolphins. The differences in oscillatory whistles for these two species seem to be consistent across study areas and therefore, could be used in addition to other whistle features to help distinguish between them.
C1 [Gruden, Pina; White, Paul R.] Univ Southampton, Inst Sound & Vibrat Res, Highfield SO17 1BJ, Hants, England.
[Oswald, Julie N.] Biowaves Inc, 364 2nd St,Suite 3, Encinitas, CA 92024 USA.
[Barkley, Yvonne] NOAA, Pacific Isl Fisheries Sci Ctr, 1845 Wasp Blvd,Bldg 176, Honolulu, HI 96818 USA.
[Cerchio, Salvatore] New England Aquarium, 1 Cent Wharf, Boston, MA 02110 USA.
[Lammers, Marc] Hawaii Inst Marine Biol, POB 1346, Kaneohe, HI 96744 USA.
[Baumann-Pickering, Simone] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA.
RP Gruden, P (reprint author), Univ Southampton, Inst Sound & Vibrat Res, Highfield SO17 1BJ, Hants, England.
EM pg3g12@soton.ac.uk
NR 39
TC 0
Z9 0
U1 1
U2 3
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0824-0469
EI 1748-7692
J9 MAR MAMMAL SCI
JI Mar. Mamm. Sci.
PD APR
PY 2016
VL 32
IS 2
BP 520
EP 534
DI 10.1111/mms.12280
PG 15
WC Marine & Freshwater Biology; Zoology
SC Marine & Freshwater Biology; Zoology
GA DJ6UR
UT WOS:000374349200006
ER
PT J
AU van der Hoop, JM
Corkeron, P
Kenney, J
Landry, S
Morin, D
Smith, J
Moore, MJ
AF van der Hoop, Julie M.
Corkeron, Peter
Kenney, John
Landry, Scott
Morin, David
Smith, Jamison
Moore, Michael J.
TI Drag from fishing gear entangling North Atlantic rightwhales
SO MARINE MAMMAL SCIENCE
LA English
DT Article
DE whale; fisheries; rope; thrust; line; drag coefficient; energetics
ID WHALES EUBALAENA-GLACIALIS; DOLPHINS TURSIOPS-TRUNCATUS; ENTANGLEMENT
INJURIES; POWER OUTPUT; FUR SEALS; DISENTANGLEMENT; SURVIVAL; BEHAVIOR;
HEALTH
AB Lethal and sublethal fishing gear entanglement is pervasive in North Atlantic right whales (Eubalaena glacialis). Entanglement can lead to direct injury and is likely to incur substantial energetic costs. This study (1) evaluates drag characteristics of entangled right whales, (2) contextualizes gear drag measurements for individual whales, and (3) quantifies the benefits of partial disentanglement. A load cell measured drag forces on 15 sets of fishing gear removed from entangled right whales, a towed satellite telemetry buoy, and 200 m of polypropylene line as it was shortened to 25 m, as they were towed behind a vessel at similar to 0.77, 1.3, and 2.1 m/s (similar to 1.5, 2.5, and 4 knots) and similar to 0, 3, and 6 m depth. Mean drag ranges from 8.5 N to 315 N, and can be predicted from the dry weight or length of the gear. Combining gear drag measurements with theoretical estimates of drag on whales' bodies suggests that on average, entanglement increases drag and propulsive power by 1.47 fold. Reducing trailing line length by 75% can reduce parasitic gear drag by 85%, reinforcing current disentanglement response practices. These drag measurements can be incorporated into disentanglement response, serious injury determination, and evaluation of sublethal effects on population dynamics.
C1 [van der Hoop, Julie M.] MIT, Woods Hole Oceanog Inst Joint Program Oceanog App, 77 Massachusetts Ave, Cambridge, MA 02139 USA.
[van der Hoop, Julie M.; Moore, Michael J.] Woods Hole Oceanog Inst, 266 Woods Hole Rd MS 50, Woods Hole, MA 02543 USA.
[Corkeron, Peter] NOAA Fisheries, Northeast Fisheries Sci Ctr, Woods Hole, MA 02543 USA.
[Kenney, John] NOAA Fisheries, Greater Atlantic Reg Off, Saunderstown, RI 02874 USA.
[Landry, Scott] Ctr Coastal Studies, 5 Holway Ave, Provincetown, MA 02657 USA.
[Morin, David; Smith, Jamison] NOAA Fisheries, Greater Atlantic Reg Off, 55 Great Republ Dr, Gloucester, MA 01930 USA.
RP van der Hoop, JM (reprint author), MIT, Woods Hole Oceanog Inst Joint Program Oceanog App, 77 Massachusetts Ave, Cambridge, MA 02139 USA.; van der Hoop, JM (reprint author), Woods Hole Oceanog Inst, 266 Woods Hole Rd MS 50, Woods Hole, MA 02543 USA.
EM jvanderhoop@whoi.edu
OI van der Hoop, Julie/0000-0003-2327-9000
FU Herrington-Fitch Family Foundation; M.S. Worthington Foundation;
Cooperative Institute for the North Atlantic Region [CINAR]
[NA14OAR4320158]; Natural Sciences and Engineering Research Council of
Canada; MIT
FX This work was supported by grants from the Herrington-Fitch Family
Foundation, the M.S. Worthington Foundation, and the Cooperative
Institute for the North Atlantic Region [CINAR; NA14OAR4320158] to MJM
and JvdH. JvdH was supported by a Postgraduate Scholarship from the
Natural Sciences and Engineering Research Council of Canada, and an MIT
Martin Family for Sustainability Fellowship.
NR 62
TC 2
Z9 2
U1 12
U2 17
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0824-0469
EI 1748-7692
J9 MAR MAMMAL SCI
JI Mar. Mamm. Sci.
PD APR
PY 2016
VL 32
IS 2
BP 619
EP 642
DI 10.1111/mms.12292
PG 24
WC Marine & Freshwater Biology; Zoology
SC Marine & Freshwater Biology; Zoology
GA DJ6UR
UT WOS:000374349200012
ER
PT J
AU Thomas, PO
Reeves, RR
Brownell, RL
AF Thomas, Peter O.
Reeves, Randall R.
Brownell, Robert L., Jr.
TI Status of the world's baleen whales
SO MARINE MAMMAL SCIENCE
LA English
DT Article
DE status; cetaceans; baleen whales; blue whales; whaling; ship strike;
entanglement; bycatch; anthropogenic noise; climate change; ocean
acidification; endangered species; IUCN; Red List
ID ATLANTIC RIGHT WHALE; EASTERN NORTH PACIFIC; ARCTIC MARINE MAMMALS;
SOUTHERN RIGHT WHALES; CHILEAN BLUE WHALES; HUMPBACK WHALES;
MEGAPTERA-NOVAEANGLIAE; CLIMATE-CHANGE; BALAENOPTERA-MUSCULUS; BOWHEAD
WHALES
AB No global synthesis of the status of baleen whales has been published since the 2008 IUCN Red List assessments. Many populations remain at low numbers from historical commercial whaling, which had ceased for all but a few by 1989. Fishing gear entanglement and ship strikes are the most severe current threats. The acute and long-term effects of anthropogenic noise and the cumulative effects of multiple stressors are of concern but poorly understood. The looming consequences of climate change and ocean acidification remain difficult to characterize. North Atlantic and North Pacific right whales are among the species listed as Endangered. Southern right, bowhead, and gray whales have been assessed as Least Concern but some subpopulations of these species - western North Pacific gray whales, Chile-Peru right whales, and Svalbard/Barents Sea and Sea of Okhotsk bowhead whales - remain at low levels and are either Endangered or Critically Endangered. Eastern North Pacific blue whales have reportedly recovered, but Antarctic blue whales remain at about 1% of pre-exploitation levels. Small isolated subspecies or subpopulations, such as northern Indian Ocean blue whales, Arabian Sea humpback whales, and Mediterranean Sea fin whales are threatened while most subpopulations of sei, Bryde's, and Omura's whales are inadequately monitored and difficult to assess.
C1 [Thomas, Peter O.; Reeves, Randall R.] Marine Mammal Commiss, 4340 East West Highway,Room 700, Bethesda, MD 20814 USA.
[Reeves, Randall R.] Okapi Wildlife Associates, 27 Chandler Lane, Hudson, PQ J0P 1H0, Canada.
[Brownell, Robert L., Jr.] NOAA, Southwest Fisheries Sci Ctr, Natl Marine Fisheries Serv, 34500 Highway 1, Monterey, CA 93940 USA.
RP Thomas, PO (reprint author), Marine Mammal Commiss, 4340 East West Highway,Room 700, Bethesda, MD 20814 USA.
EM pthomas@mmc.gov
FU Marine Mammal Commission
FX We thank the Marine Mammal Commission for supporting this review. In
particular, we thank former Executive Director Tim Ragen for initiating
and championing the idea of such a global synthesis and current
Executive Director Rebecca Lent for supporting its conclusion. We thank
Daryl Boness, Frances Gulland, Michael Tillman, and David Laist for
their reviews of earlier versions. William Perrin, Brian Smith, and Mark
Richardson provided guidance at the outset of this effort. We thank Phil
Clapham, Peter Corkeron, and other reviewers whose comments greatly
improved the quality and content of the manuscript.
NR 312
TC 5
Z9 5
U1 45
U2 78
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0824-0469
EI 1748-7692
J9 MAR MAMMAL SCI
JI Mar. Mamm. Sci.
PD APR
PY 2016
VL 32
IS 2
BP 682
EP 734
DI 10.1111/mms.12281
PG 53
WC Marine & Freshwater Biology; Zoology
SC Marine & Freshwater Biology; Zoology
GA DJ6UR
UT WOS:000374349200015
ER
PT J
AU Kato, S
Inaba, K
Sugawa, S
Shibata, K
Yamamoto, R
Yamashita, M
Takahashi, Y
AF Kato, Shinya
Inaba, Kensuke
Sugawa, Seiji
Shibata, Kosuke
Yamamoto, Ryuta
Yamashita, Makoto
Takahashi, Yoshiro
TI Laser spectroscopic probing of coexisting superfluid and insulating
states of an atomic Bose-Hubbard system
SO NATURE COMMUNICATIONS
LA English
DT Article
ID MOTT INSULATOR; TRANSITION; GASES
AB A system of ultracold atoms in an optical lattice has been regarded as an ideal quantum simulator for a Hubbard model with extremely high controllability of the system parameters. While making use of the controllability, a comprehensive measurement across the weakly to strongly interacting regimes in the Hubbard model to discuss the quantum many-body state is still limited. Here we observe a great change in the excitation energy spectra across the two regimes in an atomic Bose-Hubbard system by using a spectroscopic technique, which can resolve the site occupancy in the lattice. By quantitatively comparing the observed spectra and numerical simulations based on sum rule relations and a binary fluid treatment under a finite temperature Gutzwiller approximation, we show that the spectra reflect the coexistence of a delocalized superfluid state and a localized insulating state across the two regimes.
C1 [Kato, Shinya; Sugawa, Seiji; Shibata, Kosuke; Yamamoto, Ryuta; Takahashi, Yoshiro] Kyoto Univ, Grad Sch Sci, Dept Phys, Kyoto 6068502, Japan.
[Inaba, Kensuke; Yamashita, Makoto] NTT Corp, NTT Basic Res Labs, Atsugi, Kanagawa 2430198, Japan.
[Kato, Shinya] Waseda Univ, Dept Appl Phys, 3-4-1 Okubo, Tokyo 1698555, Japan.
[Sugawa, Seiji] Univ Maryland, NIST, Joint Quantum Inst, Gaithersburg, MD 20899 USA.
[Shibata, Kosuke] Chuo Univ, Dept Phys, Tokyo 1128551, Japan.
RP Kato, S (reprint author), Kyoto Univ, Grad Sch Sci, Dept Phys, Kyoto 6068502, Japan.; Kato, S (reprint author), Waseda Univ, Dept Appl Phys, 3-4-1 Okubo, Tokyo 1698555, Japan.
EM s.kato2@kurenai.waseda.jp
OI Yamamoto, Ryuta/0000-0003-0913-9853
FU JSPS [18204035, 21102005C01, 22684022, 14J02311, 25220711, 26247064];
GCOE Program The Next Generation of Physics; Spun from Universality;
Emergence from MEXT of Japan; FIRST program; JST CREST; Impulsing
Paradigm Change through Disruptive Technologies (ImPACT) program
FX We thank Y. Nakamura for valuable discussions. This work is supported by
Grants-in-Aid for Scientific Research of JSPS (Nos. 18204035,
21102005C01 (Quantum Cybernetics), 22684022, 14J02311, 25220711, and
26247064), the GCOE Program The Next Generation of Physics, Spun from
Universality and Emergence from MEXT of Japan, FIRST program, JST CREST,
and the Impulsing Paradigm Change through Disruptive Technologies
(ImPACT) program.
NR 36
TC 1
Z9 1
U1 4
U2 6
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 2041-1723
J9 NAT COMMUN
JI Nat. Commun.
PD APR
PY 2016
VL 7
AR 11341
DI 10.1038/ncomms11341
PG 8
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DJ9WS
UT WOS:000374564600001
PM 27094083
ER
PT J
AU Rivnay, J
Inal, S
Collins, BA
Sessolo, M
Stavrinidou, E
Strakosas, X
Tassone, C
Delongchamp, DM
Malliaras, GG
AF Rivnay, Jonathan
Inal, Sahika
Collins, Brian A.
Sessolo, Michele
Stavrinidou, Eleni
Strakosas, Xenofon
Tassone, Christopher
Delongchamp, Dean M.
Malliaras, George G.
TI Structural control of mixed ionic and electronic transport in conducting
polymers
SO NATURE COMMUNICATIONS
LA English
DT Article
ID ORGANIC ELECTROCHEMICAL TRANSISTORS; PEDOT-PSS FILMS; THIN-FILMS;
CONJUGATED POLYMERS; SOLAR-CELLS; X-RAY; MORPHOLOGY;
POLY(3,4-ETHYLENEDIOXYTHIOPHENE); SPECTROSCOPY; EFFICIENCY
AB Poly(3,4-ethylenedioxythiophene) doped with poly(styrenesulfonate), PEDOT: PSS, has been utilized for over two decades as a stable, solution-processable hole conductor. While its hole transport properties have been the subject of intense investigation, recent work has turned to PEDOT: PSS as a mixed ionic/electronic conductor in applications including bioelectronics, energy storage and management, and soft robotics. Conducting polymers can efficiently transport both holes and ions when sufficiently hydrated, however, little is known about the role of morphology on mixed conduction. Here, we show that bulk ionic and electronic mobilities are simultaneously affected by processing-induced changes in nano- and meso-scale structure in PEDOT: PSS films. We quantify domain composition, and find that domain purification on addition of dispersion co-solvents limits ion mobility, even while electronic conductivity improves. We show that an optimal morphology allows for the balanced ionic and electronic transport that is critical for prototypical mixed conductor devices. These findings may pave the way for the rational design of polymeric materials and processing routes to enhance devices reliant on mixed conduction.
C1 [Rivnay, Jonathan; Inal, Sahika; Stavrinidou, Eleni; Strakosas, Xenofon; Malliaras, George G.] MOC, EMSE, CMP, Dept Bioelect, F-13541 Gardanne, France.
[Collins, Brian A.; Delongchamp, Dean M.] NIST, Mat Sci & Engn Div, Gaithersburg, MD 20899 USA.
[Collins, Brian A.] Washington State Univ, Dept Phys & Astron, Pullman, WA 99164 USA.
[Sessolo, Michele] Univ Valencia, Inst Ciencia Mol, Paterna 46980, Spain.
[Tassone, Christopher] SLAC Natl Accelerator Lab, SSRL, Menlo Pk, CA 94025 USA.
[Rivnay, Jonathan] PARC, 3333 Coyote Hill Rd, Palo Alto, CA 94304 USA.
RP Rivnay, J (reprint author), MOC, EMSE, CMP, Dept Bioelect, F-13541 Gardanne, France.
EM rivnay@gmail.com
RI Stavrinidou, Eleni/I-8526-2016;
OI Stavrinidou, Eleni/0000-0002-9357-776X; Sessolo,
Michele/0000-0002-9189-3005
FU Marie Curie post-doctoral fellowship (FP7); Fundacion BBVA, Spain
FX J.R. acknowledges support from a Marie Curie post-doctoral fellowship
(FP7). M.S. acknowledges the support by the Fundacion BBVA, Spain. We
acknowledge Prof. B. Winther-Jensen (Monash) for providing vapour-phase
polymerized PEDOT:Cl films, Dr E. Gann (Monash) for NEXAFS measurements,
Dr M. Ramuz (EMSE) for 3D printing efforts and I. Uguz (EMSE) for film
thickness measurements. We additionally thank Prof. C. Silva (Montreal)
for fruitful discussions. Portions of this research were carried out at
the Stanford Synchrotron Radiation Laboratory (SSRL), a national user
facility operated by the Stanford University on behalf of the US
Department of Energy, Office of Basic Energy Sciences.
NR 54
TC 15
Z9 15
U1 36
U2 111
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 2041-1723
J9 NAT COMMUN
JI Nat. Commun.
PD APR
PY 2016
VL 7
AR 11287
DI 10.1038/ncomms11287
PG 9
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DJ6AC
UT WOS:000374291300001
PM 27090156
ER
PT J
AU Levine, J
Tavella, P
Santarelli, G
AF Levine, Judah
Tavella, Patrizia
Santarelli, Giorgio
TI Introduction to the Special Issue on Celebrating the 50th Anniversary of
the Allan Variance
SO IEEE TRANSACTIONS ON ULTRASONICS FERROELECTRICS AND FREQUENCY CONTROL
LA English
DT Biographical-Item
C1 [Levine, Judah] Natl Inst Stand & Technol, Div Time & Frequency, Boulder, CO 80305 USA.
[Tavella, Patrizia] Ist Nazl Ric Metrol, INRIM, I-10135 Turin, Italy.
[Santarelli, Giorgio] Univ Bordeaux, CNRS, IOGS, Lab Photon Numer & Nanosci LP2N, F-33400 Talence, France.
RP Levine, J (reprint author), Natl Inst Stand & Technol, Div Time & Frequency, Boulder, CO 80305 USA.
NR 0
TC 0
Z9 0
U1 1
U2 4
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 0885-3010
EI 1525-8955
J9 IEEE T ULTRASON FERR
JI IEEE Trans. Ultrason. Ferroelectr. Freq. Control
PD APR
PY 2016
VL 63
IS 4
BP 511
EP 512
DI 10.1109/TUFFC.2016.2545823
PG 2
WC Acoustics; Engineering, Electrical & Electronic
SC Acoustics; Engineering
GA DJ4HB
UT WOS:000374164900001
PM 27504513
ER
PT J
AU Allan, DW
Levine, J
AF Allan, David W.
Levine, Judah
TI A Historical Perspective on the Development of the Allan Variances and
Their Strengths and Weaknesses
SO IEEE TRANSACTIONS ON ULTRASONICS FERROELECTRICS AND FREQUENCY CONTROL
LA English
DT Article
DE Allan variances (AVARs); atomic clocks; nonstationary processes;
precision analysis; time series analysis
AB Over the past 50 years, variances have been developed for characterizing the instabilities of precision clocks and oscillators. These instabilities are often modeled as nonstationary processes, and the variances have been shown to be well-behaved and to be unbiased, efficient descriptors of these types of processes. This paper presents a historical overview of the development of these variances. The time-domain and frequency-domain formulations are presented and their development is described. The strengths and weaknesses of these characterization metrics are discussed. These variances are also shown to be useful in other applications, such as in telecommunication.
C1 [Allan, David W.] Allans TIME, Fountain Green, UT 84632 USA.
[Levine, Judah] Natl Inst Stand & Technol, Div Time & Frequency, Boulder, CO 80305 USA.
RP Allan, DW (reprint author), Allans TIME, Fountain Green, UT 84632 USA.; Levine, J (reprint author), Natl Inst Stand & Technol, Div Time & Frequency, Boulder, CO 80305 USA.
EM david@allanstime.com; Judah.Levine@nist.gov
NR 18
TC 0
Z9 0
U1 1
U2 2
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 0885-3010
EI 1525-8955
J9 IEEE T ULTRASON FERR
JI IEEE Trans. Ultrason. Ferroelectr. Freq. Control
PD APR
PY 2016
VL 63
IS 4
BP 513
EP 519
DI 10.1109/TUFFC.2016.2524687
PG 7
WC Acoustics; Engineering, Electrical & Electronic
SC Acoustics; Engineering
GA DJ4HB
UT WOS:000374164900002
PM 26890729
ER
PT J
AU Weiss, MA
Shenoi, K
AF Weiss, M. A.
Shenoi, Kishan
TI The Time Deviation in Packet-Based Synchronization
SO IEEE TRANSACTIONS ON ULTRASONICS FERROELECTRICS AND FREQUENCY CONTROL
LA English
DT Article
DE Allan variance; packet networks; synchronous digital hierarchy (SDH);
synchronous optical network (SONET); time deviation (TDEV); time
variance (TVAR)
AB The telecommunications industry has used the time deviation (TDEV) very effectively for specifying network equipment clock performance as well as the performance of timing signals generated by Central Office equipment such as primary reference clocks and building integrated timing supplies (BITS) and synchronization supply units (SSUs). We discuss here the development of TDEV, and the variations of TDEV motivated by the advent of packet-switching and the steady transformation of the telecom network from circuit-switched-based to packet-switched-based. We illustrate these with simulation of the performance of the precise time protocol (PTP) across a packet-switched network. We then apply published methods to automatically determine noise types, and use these to predict time dispersion from a master clock for a slave clock using these PTP packets to stay synchronized. The result shows how TDEV and the other deviations provide an extensive array of tools for telecom networks, as well as for general time and frequency applications.
C1 [Weiss, M. A.] Natl Inst Stand & Technol, Boulder, CO 80305 USA.
[Shenoi, Kishan] Qulsar Inc, San Jose, CA 95110 USA.
RP Weiss, MA (reprint author), Natl Inst Stand & Technol, Boulder, CO 80305 USA.
EM mweiss@nist.gov
NR 8
TC 0
Z9 0
U1 1
U2 1
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 0885-3010
EI 1525-8955
J9 IEEE T ULTRASON FERR
JI IEEE Trans. Ultrason. Ferroelectr. Freq. Control
PD APR
PY 2016
VL 63
IS 4
BP 531
EP 537
DI 10.1109/TUFFC.2015.2495011
PG 7
WC Acoustics; Engineering, Electrical & Electronic
SC Acoustics; Engineering
GA DJ4HB
UT WOS:000374164900004
PM 26529756
ER
PT J
AU Levine, J
AF Levine, Judah
TI An Algorithm for Synchronizing a Clock When the Data Are Received Over a
Network With an Unstable Delay
SO IEEE TRANSACTIONS ON ULTRASONICS FERROELECTRICS AND FREQUENCY CONTROL
LA English
DT Article
DE Analysis of variance; frequency control; frequency locked loops;
low-frequency noise; phase noise; statistical distribution functions;
timing jitter
ID TIME SYNCHRONIZATION; COMPUTER; INTERNET
AB A method is presented for synchronizing the time of a clock to a remote time standard when the channel connecting the two has significant delay variation that can be described only statistically. The method compares the Allan deviation of the channel fluctuations to the free-running stability of the local clock, and computes the optimum interval between requests based on one of the three selectable requirements: 1) choosing the highest possible accuracy; 2) choosing the best tradeoff of cost versus accuracy; or 3) minimizing the number of requests to realize a specific accuracy. Once the interval between requests is chosen, the final step is to steer the local clock based on the received data. A typical adjustment algorithm, which supports both the statistical considerations based on the Allan deviation comparison and the timely detection of errors, is included as an example.
C1 [Levine, Judah] NIST, Div Time & Frequency, Boulder, CO 80305 USA.
RP Levine, J (reprint author), NIST, Div Time & Frequency, Boulder, CO 80305 USA.
EM Judah.Levine@nist.gov
FU Intramural NIST DOC [9999-NIST]
NR 12
TC 1
Z9 2
U1 0
U2 0
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 0885-3010
EI 1525-8955
J9 IEEE T ULTRASON FERR
JI IEEE Trans. Ultrason. Ferroelectr. Freq. Control
PD APR
PY 2016
VL 63
IS 4
BP 561
EP 570
DI 10.1109/TUFFC.2015.2495014
PG 10
WC Acoustics; Engineering, Electrical & Electronic
SC Acoustics; Engineering
GA DJ4HB
UT WOS:000374164900007
PM 26529759
ER
PT J
AU Ashby, N
Patla, B
AF Ashby, Neil
Patla, Bijunath
TI Simulations of the Hadamard Variance: Probability Distributions and
Confidence Intervals
SO IEEE TRANSACTIONS ON ULTRASONICS FERROELECTRICS AND FREQUENCY CONTROL
LA English
DT Article
DE Analysis of variance; digital simulation; time series analysis
ID POWER-LAW NOISE; FREQUENCY STABILITY
AB Power-law noise in clocks and oscillators can be simulated by Fourier transforming a modified spectrum of white phase noise. This approach has been applied successfully to simulation of the Allan variance and the modified Allan variance in both overlapping and nonoverlapping forms. When significant frequency drift is present in an oscillator, at large sampling times the Allan variance overestimates the intrinsic noise, while the Hadamard variance is insensitive to frequency drift. The simulation method is extended in this paper to predict the Hadamard variance for the common types of power-law noise. Symmetric real matrices are introduced whose traces-the sums of their eigenvalues-are equal to the Hadamard variances, in overlapping or nonoverlapping forms, as well as for the corresponding forms of the modified Hadamard variance. We show that the standard relations between spectral densities and Hadamard variance are obtained with this method. The matrix eigenvalues determine probability distributions for observing a variance at an arbitrary value of the sampling interval tau, and hence for estimating confidence in the measurements.
C1 [Ashby, Neil; Patla, Bijunath] NIST, Boulder, CO 80305 USA.
RP Ashby, N; Patla, B (reprint author), NIST, Boulder, CO 80305 USA.
EM ashby@boulder.nist.gov; bijunath.patla@boulder.nist.gov
FU NASA, Division of Planetary Science [NNH12AT81I]
FX This work was supported in part by NASA, Division of Planetary Science,
under Grant NNH12AT81I.
NR 24
TC 0
Z9 0
U1 1
U2 1
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 0885-3010
EI 1525-8955
J9 IEEE T ULTRASON FERR
JI IEEE Trans. Ultrason. Ferroelectr. Freq. Control
PD APR
PY 2016
VL 63
IS 4
BP 636
EP 645
DI 10.1109/TUFFC.2015.2507441
PG 10
WC Acoustics; Engineering, Electrical & Electronic
SC Acoustics; Engineering
GA DJ4HB
UT WOS:000374164900014
PM 26672035
ER
PT J
AU Camp, CH
Lee, YJ
Cicerone, MT
AF Camp, Charles H., Jr.
Lee, Young Jong
Cicerone, Marcus T.
TI Quantitative, comparable coherent anti-Stokes Raman scattering (CARS)
spectroscopy: correcting errors in phase retrieval
SO JOURNAL OF RAMAN SPECTROSCOPY
LA English
DT Article
DE coherent Raman spectroscopy; coherent anti-Stokes Raman scattering;
phase retrieval; Kramers-Kronig; baseline detrending
ID HUMAN CORONARY ATHEROSCLEROSIS; MAXIMUM-ENTROPY; MICROSCOPY;
MICROSPECTROSCOPY
AB Coherent anti-Stokes Raman scattering (CARS) microspectroscopy has demonstrated significant potential for biological and materials imaging. To date, however, the primary mechanism of disseminating CARS spectroscopic information is through pseudocolor imagery, which explicitly neglects a vast majority of the hyperspectral data. Furthermore, current paradigms in CARS spectral processing do not lend themselves to quantitative sample-to-sample comparability. The primary limitation stems from the need to accurately measure the so-called nonresonant background (NRB) that is used to extract the chemically sensitive Raman information from the raw spectra. Measurement of the NRB on a pixel-by-pixel basis is a nontrivial task; thus, surrogate NRB from glass or water is typically utilized, resulting in error between the actual and estimated amplitude and phase. In this paper, we present a new methodology for extracting the Raman spectral features that significantly suppresses these errors through phase detrending and scaling. Classic methods of error correction, such as baseline detrending, are demonstrated to be inaccurate and to simply mask the underlying errors. The theoretical justification is presented by re-developing the theory of phase retrieval via the Kramers-Kronig relation, and we demonstrate that these results are also applicable to maximum entropy method-based phase retrieval. This new error-correction approach is experimentally applied to glycerol spectra and tissue images, demonstrating marked consistency between spectra obtained using different NRB estimates and between spectra obtained on different instruments. Additionally, in order to facilitate implementation of these approaches, we have made many of the tools described herein available free for download. Published 2015. This article is a U.S. Government work and is in the public domain in the USA.
C1 [Camp, Charles H., Jr.; Lee, Young Jong; Cicerone, Marcus T.] NIST, Biosyst & Biomat Div, 100 Bur Dr, Gaithersburg, MD 20899 USA.
RP Camp, CH (reprint author), NIST, Biosyst & Biomat Div, 100 Bur Dr, Gaithersburg, MD 20899 USA.
EM charles.camp@nist.gov
RI Lee, Young Jong/B-7129-2008;
OI Lee, Young Jong/0000-0001-7754-3001; Camp Jr,
Charles/0000-0002-5805-1842
NR 34
TC 5
Z9 5
U1 16
U2 30
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0377-0486
EI 1097-4555
J9 J RAMAN SPECTROSC
JI J. Raman Spectrosc.
PD APR
PY 2016
VL 47
IS 4
BP 408
EP 415
DI 10.1002/jrs.4824
PG 8
WC Spectroscopy
SC Spectroscopy
GA DJ3XK
UT WOS:000374139800006
ER
PT J
AU Sikora, M
Rutkowski, M
Begelman, MC
AF Sikora, Marek
Rutkowski, Mieszko
Begelman, Mitchell C.
TI A spine-sheath model for strong-line blazars
SO MONTHLY NOTICES OF THE ROYAL ASTRONOMICAL SOCIETY
LA English
DT Article
DE acceleration of particles; radiation mechanisms: non-thermal; galaxies:
jets
ID RELATIVISTIC MAGNETOHYDRODYNAMIC SIMULATIONS; ACTIVE GALACTIC NUCLEI;
GAMMA-RAY ACTIVITY; LARGE-SCALE JETS; MULTIWAVELENGTH OBSERVATIONS; 3C
279; X-RAY; MAGNETIC COLLIMATION; LUMINOUS BLAZARS; RADIO-GALAXIES
AB We have developed a quasi-analytical model for the production of radiation in strong-line blazars, assuming a spine-sheath jet structure. The model allows us to study how the spine and sheath spectral components depend on parameters describing the geometrical and physical structure of 'the blazar zone'. We show that typical broad-band spectra of strong-line blazars can be reproduced by assuming the magnetization parameter to be of order unity and reconnection to be the dominant dissipation mechanism. Furthermore, we demonstrate that the spine-sheath model can explain why gamma-ray variations are often observed to have much larger amplitudes than the corresponding optical variations. The model is also less demanding of jet power than one-zone models, and can reproduce the basic features of extreme gamma-ray events.
C1 [Sikora, Marek] Nicolaus Copernicus Astron Ctr, Bartycka 18, PL-00716 Warsaw, Poland.
[Rutkowski, Mieszko] Jagiellonian Univ, Marian Smoluchowski Inst Phys, Lojasiewicza 11, PL-30348 Krakow, Poland.
[Begelman, Mitchell C.] Univ Colorado, JILA, 440 UCB, Boulder, CO 80309 USA.
[Begelman, Mitchell C.] Natl Inst Stand & Technol, 440 UCB, Boulder, CO 80309 USA.
[Begelman, Mitchell C.] Univ Colorado, Dept Astrophys & Planetary Sci, 391 UCB, Boulder, CO 80309 USA.
RP Sikora, M (reprint author), Nicolaus Copernicus Astron Ctr, Bartycka 18, PL-00716 Warsaw, Poland.
EM sikora@camk.edu.pl
FU Polish NCN [UMO-2013/08/A/ST9/00795]; NSF [AST-1411879]; NASA
Astrophysics Theory Program [NNX14AB37G]
FX The research was supported in part by the Polish NCN grant
UMO-2013/08/A/ST9/00795. MCB acknowledges support from NSF grant
AST-1411879 and NASA Astrophysics Theory Program grant NNX14AB37G.
NR 53
TC 4
Z9 4
U1 0
U2 0
PU OXFORD UNIV PRESS
PI OXFORD
PA GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND
SN 0035-8711
EI 1365-2966
J9 MON NOT R ASTRON SOC
JI Mon. Not. Roy. Astron. Soc.
PD APR 1
PY 2016
VL 457
IS 2
BP 1352
EP 1358
DI 10.1093/mnras/stw107
PG 7
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA DI6AB
UT WOS:000373580500019
ER
PT J
AU Olson, ND
Zook, JM
Samarov, DV
Jackson, SA
Salit, ML
AF Olson, Nathan D.
Zook, Justin M.
Samarov, Daniel V.
Jackson, Scott A.
Salit, Marc L.
TI PEPR: pipelines for evaluating prokaryotic references
SO ANALYTICAL AND BIOANALYTICAL CHEMISTRY
LA English
DT Article
DE Microbiology; Whole genome sequencing; Bioinformatics
ID DNA-SEQUENCING DATA; GENOME; FRAMEWORK; TOOLKIT
AB The rapid adoption of microbial whole genome sequencing in public health, clinical testing, and forensic laboratories requires the use of validated measurement processes. Well-characterized, homogeneous, and stable microbial genomic reference materials can be used to evaluate measurement processes, improving confidence in microbial whole genome sequencing results. We have developed a reproducible and transparent bioinformatics tool, PEPR, Pipelines for Evaluating Prokaryotic References, for characterizing the reference genome of prokaryotic genomic materials. PEPR evaluates the quality, purity, and homogeneity of the reference material genome, and purity of the genomic material. The quality of the genome is evaluated using high coverage paired-end sequence data; coverage, paired-end read size and direction, as well as soft-clipping rates, are used to identify mis-assemblies. The homogeneity and purity of the material relative to the reference genome are characterized by comparing base calls from replicate datasets generated using multiple sequencing technologies. Genomic purity of the material is assessed by checking for DNA contaminants. We demonstrate the tool and its output using sequencing data while developing a Staphylococcus aureus candidate genomic reference material. PEPR is open source and available at https://github.com/usnistgov/pepr.
C1 [Olson, Nathan D.; Zook, Justin M.; Jackson, Scott A.; Salit, Marc L.] NIST, Biosyst & Biomat Div, Mat Measurement Lab, Gaithersburg, MD 20899 USA.
[Samarov, Daniel V.] NIST, Stat Engn Div, Informat Technol Lab, Gaithersburg, MD 20899 USA.
[Salit, Marc L.] Stanford Univ, Dept Bioengn, Stanford, CA 94305 USA.
RP Olson, ND (reprint author), NIST, Biosyst & Biomat Div, Mat Measurement Lab, Gaithersburg, MD 20899 USA.
EM nolson@nist.gov
OI Olson, Nathanael/0000-0003-2585-3037
FU Department of Homeland Security (DHS) Science and Technology Directorate
[HSHQPM-14-X-00078]; NIST; FDA
FX The authors would like to thank Jenny McDaniel, Lindsay Vang, and David
Catoe for performing the MiSeq and PGM sequencing, and Tim Muruvanda for
performing the PacBio sequencing. Additionally, we would like to thank
Drs. Nancy Lin and Steven Lund for conversations and suggestions while
developing PEPR and drafting the manuscript. Department of Homeland
Security (DHS) Science and Technology Directorate funded this project
under Interagency Agreement HSHQPM-14-X-00078 with NIST. This work was
additionally supported by two interagency agreements between NIST and
the FDA. Opinions expressed in this paper are the author's and do not
necessarily reflect the policies and views of the DHS, NIST, or
affiliated venues. Certain commercial equipment, instruments, or
materials are identified in this paper only to specify the experimental
procedure adequately. Such identification is not intended to imply
recommendation or endorsement by the NIST, nor is it intended to imply
that the materials or equipment identified are necessarily the best
available for the purpose. Official contribution of NIST; not subject to
copyrights in USA.
NR 26
TC 0
Z9 0
U1 1
U2 2
PU SPRINGER HEIDELBERG
PI HEIDELBERG
PA TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY
SN 1618-2642
EI 1618-2650
J9 ANAL BIOANAL CHEM
JI Anal. Bioanal. Chem.
PD APR
PY 2016
VL 408
IS 11
BP 2975
EP 2983
DI 10.1007/s00216-015-9299-5
PG 9
WC Biochemical Research Methods; Chemistry, Analytical
SC Biochemistry & Molecular Biology; Chemistry
GA DJ3MX
UT WOS:000374110700028
PM 26935931
ER
PT J
AU France, K
Loyd, ROP
Youngblood, A
Brown, A
Schneider, PC
Hawley, SL
Froning, CS
Linsky, JL
Roberge, A
Buccino, AP
Davenport, JRA
Fontenla, JM
Kaltenegger, L
Kowalski, AF
Mauas, PJD
Miguel, Y
Redfield, S
Rugheimer, S
Tian, F
Vieytes, MC
Walkowicz, LM
Weisenburger, KL
AF France, Kevin
Loyd, R. O. Parke
Youngblood, Allison
Brown, Alexander
Schneider, P. Christian
Hawley, Suzanne L.
Froning, Cynthia S.
Linsky, Jeffrey L.
Roberge, Aki
Buccino, Andrea P.
Davenport, James R. A.
Fontenla, Juan M.
Kaltenegger, Lisa
Kowalski, Adam F.
Mauas, Pablo J. D.
Miguel, Yamila
Redfield, Seth
Rugheimer, Sarah
Tian, Feng
Vieytes, Mariela C.
Walkowicz, Lucianne M.
Weisenburger, Kolby L.
TI THE MUSCLES TREASURY SURVEY. I. MOTIVATION AND OVERVIEW
SO ASTROPHYSICAL JOURNAL
LA English
DT Article
DE planetary systems; stars: activity; stars: low-mass
ID LOCAL INTERSTELLAR-MEDIUM; HUBBLE-SPACE-TELESCOPE; LOW-MASS STAR;
POTENTIALLY HABITABLE PLANETS; EXTRASOLAR GIANT PLANETS; EXOPLANET HOST
STARS; MAIN-SEQUENCE STARS; EARTH-LIKE PLANETS; GJ 436 SYSTEM; M-DWARF
STARS
AB Ground-and space-based planet searches employing radial velocity techniques and transit photometry have detected thousands of planet-hosting stars in the Milky Way. With so many planets discovered, the next step toward identifying potentially habitable planets is atmospheric characterization. While the Sun-Earth system provides a good framework for understanding the atmospheric chemistry of Earth-like planets around solar-type stars, the observational and theoretical constraints on the atmospheres of rocky planets in the habitable zones (HZs) around low-mass stars (K and M dwarfs) are relatively few. The chemistry of these atmospheres is controlled by the shape and absolute flux of the stellar spectral energy distribution (SED), however, flux distributions of relatively inactive low-mass stars are poorly understood at present. To address this issue, we have executed a panchromatic (X-ray to mid-IR) study of the SEDs of 11 nearby planet-hosting stars, the Measurements of the Ultraviolet Spectral Characteristics of Low-mass Exoplanetary Systems (MUSCLES) Treasury Survey. The MUSCLES program consists visible observations from Hubble and ground-based observatories. Infrared and astrophysically inaccessible wavelengths (EUV and Ly alpha) are reconstructed using stellar model spectra to fill in gaps in the observational data. In this overview and the companion papers describing the MUSCLES survey, we show that energetic radiation (X-ray and ultraviolet) is present from magnetically active stellar atmospheres at all times for stars as late as M6. The emission line luminosities of C IV and Mg II are strongly correlated with band-integrated luminosities and we present empirical relations that can be used to estimate broadband FUV and XUV (equivalent to X-ray + EUV) fluxes from individual stellar emission line measurements. We find that while the slope of the SED, FUV/NUV, increases by approximately two orders of magnitude form early K to late M dwarfs (approximate to 0.01-1), the absolute FUV and XUV flux levels at their corresponding HZ distances are constant to within factors of a few, spanning the range 10-70 erg cm(-2) s(-1) in the HZ. Despite the lack of strong stellar activity indicators in their optical spectra, several of the M dwarfs in our sample show spectacular UV flare emission in their light curves. We present an example with flare/quiescent ultraviolet flux ratios of the order of 100:1 where the transition region energy output during the flare is comparable to the total quiescent luminosity of the star E-flare(UV) similar to 0.3 L-*Delta t (Delta t = 1 s). Finally, we interpret enhanced L(line)/L-Bol ratios for C IV and N V as tentative observational evidence for the interaction of planets with large planetary mass-to-orbital distance ratios (M-plan/a(plan)) with the transition regions of their host stars.
C1 [France, Kevin; Loyd, R. O. Parke; Youngblood, Allison] Univ Colorado, Lab Atmospher & Space Phys, 600 UCB, Boulder, CO 80309 USA.
[Brown, Alexander] Univ Colorado, Ctr Astrophys & Space Astron, 389 UCB, Boulder, CO 80309 USA.
[Schneider, P. Christian] European Space Res & Technol Ctr ESA ESTEC, Keplerlaan 1, NL-2201 AZ Noordwijk, Netherlands.
[Hawley, Suzanne L.; Weisenburger, Kolby L.] Univ Washington, Dept Astron, Box 351580, Seattle, WA 98195 USA.
[Froning, Cynthia S.] Univ Texas Austin, Dept Astron, C1400, Austin, TX 78712 USA.
[Linsky, Jeffrey L.] Univ Colorado, JILA, 440 UCB, Boulder, CO 80309 USA.
[Linsky, Jeffrey L.] NIST, 440 UCB, Boulder, CO 80309 USA.
[Roberge, Aki] NASA, Goddard Space Flight Ctr, Exoplanets & Stellar Astrophys Lab, Greenbelt, MD 20771 USA.
[Buccino, Andrea P.; Mauas, Pablo J. D.; Vieytes, Mariela C.] Inst Astron & Fis Espacio UBA CONICET, CC 67,Suc 28, RA-1428 Buenos Aires, DF, Argentina.
[Buccino, Andrea P.; Mauas, Pablo J. D.] Dept Fis UBA, CC 67,Suc 28, RA-1428 Buenos Aires, DF, Argentina.
[Davenport, James R. A.] Western Washington Univ, Dept Phys & Astron, Bellingham, WA 98225 USA.
[Fontenla, Juan M.] North West Res Associates, 3380 Mitchell Lane, Boulder, CO 80301 USA.
[Kaltenegger, Lisa] Cornell Univ, Carl Sagan Inst, Ithaca, NY 14850 USA.
[Kowalski, Adam F.] Univ Maryland, Dept Astron, College Pk, MD 20742 USA.
[Miguel, Yamila] Univ Nice Sophia Antipolis, Observ Cote Azur, CNRS, Lab Lagrange, Blvd Observ,CS 34229, F-06304 Nice 4, France.
[Redfield, Seth] Wesleyan Univ, Dept Astron, Middletown, CT 06459 USA.
[Redfield, Seth] Wesleyan Univ, Van Vleck Observ, Middletown, CT 06459 USA.
[Rugheimer, Sarah] Univ St Andrews, Dept Earth & Environm Sci, Irvine Bldg, St Andrews KY16 9AL, Fife, Scotland.
[Tian, Feng] Tsinghua Univ, Ctr Earth Syst Sci, Key Lab Earth Syst Modeling, Minist Educ, Beijing 100084, Peoples R China.
[Vieytes, Mariela C.] UNTREF, CC 67,Suc 28, RA-1428 Buenos Aires, DF, Argentina.
[Walkowicz, Lucianne M.] Adler Planetarium, 1300 S Lakeshore Dr, Chicago, IL 60605 USA.
RP France, K (reprint author), Univ Colorado, Lab Atmospher & Space Phys, 600 UCB, Boulder, CO 80309 USA.
EM kevin.france@colorado.edu
RI Tian, Feng/C-1344-2015;
OI Tian, Feng/0000-0002-9607-560X; Rugheimer, Sarah/0000-0003-1620-7658;
Redfield, Seth/0000-0003-3786-3486; FRANCE, KEVIN/0000-0002-1002-3674;
Roberge, Aki/0000-0002-2989-3725
FU HST Guest Observing programs [12464, 13650]; COS Science Team Guaranteed
Time programs [12034, 12035]; STScI [HST-GO-12464.01, HST-GO-13650.01];
Smithsonian Astrophysical Observatory [GO4-15014X, GO5-16155X]; NASA
[NNX16AC09G]; NSF [AST 13-11678]; National Natural Science Foundation of
China [41175039]; Ministry of Education of China [20131029170]; Tsinghua
University Initiative Scientific Research Program; ESA Research
Fellowship
FX The data presented here were obtained as part of the HST Guest Observing
programs #12464 and #13650 as well as the COS Science Team Guaranteed
Time programs # 12034 and # 12035. This work was supported by STScI
grants HST-GO-12464.01 and HST-GO-13650.01 to the University of Colorado
at Boulder. Data for the MUSCLES Treasury Survey were also acquired as
part of Chandra and XMM guest observing programs, supported by Chandra
grants GO4-15014X and GO5-16155X from the Smithsonian Astrophysical
Observatory and NASA XMM grant NNX16AC09G to the University of Colorado
at Boulder. This work is based in part upon observations obtained with
the Apache Point Observatory 3.5 m and 0.5 m telescopes, which are owned
and operated by the Astrophysical Research Consortium. K.F. thanks
Evgenya Shkolnik for enjoyable discussions about low-mass stars and
Jorge Sanz-Forcada for assistance with the absolute flux levels of the
X-exoplanets model spectra. The MUSCLES team also thanks STScI program
coordinator Amber Armstrong for her long hours spent scheduling these
complicated coordinated observations. P.C.S. gratefully acknowledges an
ESA Research Fellowship. S.L.H. acknowledges support from NSF grant AST
13-11678. F.T. is supported by the National Natural Science Foundation
of China (41175039), the Startup Fund of the Ministry of Education of
China (20131029170), and the Tsinghua University Initiative Scientific
Research Program.
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PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0004-637X
EI 1538-4357
J9 ASTROPHYS J
JI Astrophys. J.
PD APR 1
PY 2016
VL 820
IS 2
AR 89
DI 10.3847/0004-637X/820/2/89
PG 24
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA DI8HE
UT WOS:000373741300008
ER
PT J
AU Sayers, J
Zemcov, M
Glenn, J
Golwala, SR
Maloney, PR
Siegel, SR
Wheeler, J
Bockstiegel, C
Brugger, S
Czakon, NG
Day, PK
Downes, TP
Duan, RP
Gao, JS
Hollister, MI
Lam, A
LeDuc, HG
Mazin, BA
McHugh, SG
Miller, DA
Mroczkowski, TK
Noroozian, O
Nguyen, HT
Radford, SJE
Schlaerth, JA
Vayonakis, A
Wilson, PR
Zmuidzinas, J
AF Sayers, Jack
Zemcov, Michael
Glenn, Jason
Golwala, Sunil R.
Maloney, Philip R.
Siegel, Seth R.
Wheeler, Jordan
Bockstiegel, Clint
Brugger, Spencer
Czakon, Nicole G.
Day, Peter K.
Downes, Thomas P.
Duan, Ran P.
Gao, Jiansong
Hollister, Matthew I.
Lam, Albert
LeDuc, Henry G.
Mazin, Benjamin A.
McHugh, Sean G.
Miller, David A.
Mroczkowski, Tony K.
Noroozian, Omid
Nguyen, Hien T.
Radford, Simon J. E.
Schlaerth, James A.
Vayonakis, Anastasios
Wilson, Philip R.
Zmuidzinas, Jonas
TI PECULIAR VELOCITY CONSTRAINTS FROM FIVE-BAND SZ EFFECT MEASUREMENTS
TOWARD RX J1347.5-1145 WITH MUSIC AND BOLOCAM FROM THE CSO
SO ASTROPHYSICAL JOURNAL
LA English
DT Article
DE galaxies: clusters: individual: (RX. J1347.5-1145); galaxies: clusters:
intracluster medium
ID SUNYAEV-ZELDOVICH SIGNAL; RELAXED GALAXY CLUSTERS; X-RAY-CLUSTER;
SCALING RELATIONS; MACS J0717.5+3745; PRESSURE PROFILES; SAMPLE; GHZ;
J1347-1145; COSMOLOGY
AB We present Sunyaev-Zel'dovich (SZ) effect measurements from wide-field images toward the galaxy cluster RX. J1347.5-1145 obtained from the Caltech Submillimeter Observatory with the Multiwavelength Submillimeter Inductance Camera at 147, 213, 281, and 337 GHz and with Bolocam at 140 GHz. As part of our analysis, we have used higher frequency data from Herschel-SPIRE and previously published lower frequency radio data to subtract the signal from the brightest dusty star-forming galaxies behind RX. J1347.5-1145 and from the AGN in RX. J1347.5-1145's BCG. Using these five-band SZ effect images, combined with X-ray spectroscopic measurements of the temperature of the intra-cluster medium (ICM) from Chandra, we constrain the ICM optical depth to be tau(e) = 7.33(-0.97)(+0.96) x 10(-3) and the ICM line of sight peculiar velocity to be v(pec) = 1040(-840)(+870) km s(-1). The errors for both quantities are limited by measurement noise rather than calibration uncertainties or astrophysical contamination, and significant improvements are possible with deeper observations. Our best-fit velocity is in good agreement with one previously published SZ effect analysis and in mild tension with the other, although some or all of that tension may be because that measurement samples a much smaller cluster volume. Furthermore, our best-fit optical depth implies a gas mass slightly larger than the Chandra-derived value, implying the cluster is elongated along the line of sight.
C1 [Sayers, Jack; Golwala, Sunil R.; Siegel, Seth R.; Hollister, Matthew I.; Lam, Albert; Miller, David A.; Radford, Simon J. E.; Schlaerth, James A.; Vayonakis, Anastasios; Zmuidzinas, Jonas] CALTECH, Div Phys Math & Astron, Pasadena, CA 91125 USA.
[Zemcov, Michael] Rochester Inst Technol, Rochester, NY 14623 USA.
[Glenn, Jason; Maloney, Philip R.; Wheeler, Jordan; Brugger, Spencer; Schlaerth, James A.] Univ Colorado, Dept Astrophys & Planetary Sci, Boulder, CO 80309 USA.
[Bockstiegel, Clint; Mazin, Benjamin A.; McHugh, Sean G.] Univ Calif Santa Barbara, Dept Phys, Santa Barbara, CA 93106 USA.
[Czakon, Nicole G.] Acad Sinica, Inst Astron & Astrophys, Taipei 115, Taiwan.
[Day, Peter K.; LeDuc, Henry G.; Nguyen, Hien T.; Wilson, Philip R.] CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91109 USA.
[Downes, Thomas P.] Univ Wisconsin, Dept Phys, Milwaukee, WI 53201 USA.
[Duan, Ran P.] Chinese Acad Sci, Natl Astron Observ, Beijing, Peoples R China.
[Gao, Jiansong] NIST, Boulder, CO 80305 USA.
[Mroczkowski, Tony K.] US Naval Res Lab, Washington, DC 20375 USA.
[Noroozian, Omid] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
RP Sayers, J (reprint author), CALTECH, Div Phys Math & Astron, Pasadena, CA 91125 USA.
EM jack@caltech.edu
OI radford, simon/0000-0001-9113-1660; Mroczkowski,
Tony/0000-0003-3816-5372
FU Norris Foundation Fellowship; NASA Graduate Student Research Fellowship;
NASA Earth and Space Science Fellowship; Gordon and Betty Moore
Foundation; JPL internal funds; NSF; NASA
FX We thank the anonymous referee for his or her extensive suggestions to
improve this manuscript. We acknowledge the assistance of: the day crew
and Hilo staff of the Caltech Submillimeter Observatory, who provided
invaluable assistance during data-taking for this data set; Kathy
Deniston and Diana Bisel, who provided effective administrative support
at Caltech and in Hilo; J.S. was partially supported by a Norris
Foundation Fellowship; N.G.C. was partially supported by a NASA Graduate
Student Research Fellowship; S.R.S. was supported by a NASA Earth and
Space Science Fellowship; MUSIC was constructed and commissioned with
funding provided by the Gordon and Betty Moore Foundation, JPL internal
funds, and the NSF Advanced Technologies and Instrumentation (ATI) and
Astronomy and Astrophysics Grants (AAG) Programs. This work is based in
part on observations made with Herschel, a European Space Agency
Cornerstone Mission with a significant participation by NASA. Partial
support for this work was provided by NASA through an award issued by
JPL/Caltech. This research was performed while TM held a National
Research Council Research Associateship Award at the Naval Research
Laboratory.
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PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0004-637X
EI 1538-4357
J9 ASTROPHYS J
JI Astrophys. J.
PD APR 1
PY 2016
VL 820
IS 2
AR 101
DI 10.3847/0004-637X/820/2/101
PG 13
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA DI8HE
UT WOS:000373741300020
ER
PT J
AU Mahboubi, H
Aghdam, AG
Sayrafian-Pour, K
AF Mahboubi, Hamid
Aghdam, Amir G.
Sayrafian-Pour, Kamran
TI Toward Autonomous Mobile Sensor Networks Technology
SO IEEE TRANSACTIONS ON INDUSTRIAL INFORMATICS
LA English
DT Article
DE Coverage; lifetime; energy; mobile sensor network
ID DISTRIBUTED DEPLOYMENT ALGORITHMS; ENERGY-CONSUMPTION; IMPROVED
COVERAGE; WIRELESS; LIFETIME; SYSTEM; OPTIMIZATION; STRATEGIES; SCHEME
AB Mobile sensor networking technology has attracted considerable attention in various research communities in recent years due to their widespread applications in civilian and military environments. One objective when using mobile sensors is to obtain maximum field coverage by properly deploying sensor nodes. In many real-world applications, a priori knowledge about the best deployment position for the sensors is not available. However, the motion capability of the sensors could allow each node to adjust its position (i.e., relocate) so that a better (and ultimately maximal) coverage is achieved. In this paper, a novel autonomous joint sensing range and relocation control algorithm is presented that achieves improved coverage and network lifetime at the same time. In the proposed algorithm, the sensing range of each sensor is adjusted iteratively based on its residual energy. At the same time, the sensor is directed to move within its corresponding multiplicatively weighted Voronoi region to ultimately increase sensing coverage in the field. Simulation results demonstrate the efficacy of the technique.
C1 [Mahboubi, Hamid] McGill Univ, Dept Elect & Comp Engn, Montreal, PQ H3A 0G4, Canada.
[Aghdam, Amir G.] Concordia Univ, Dept Elect & Comp Engn, Montreal, PQ H3G 1M8, Canada.
[Sayrafian-Pour, Kamran] NIST, Informat Technol Lab, Gaithersburg, MD 20899 USA.
RP Mahboubi, H (reprint author), McGill Univ, Dept Elect & Comp Engn, Montreal, PQ H3A 0G4, Canada.; Aghdam, AG (reprint author), Concordia Univ, Dept Elect & Comp Engn, Montreal, PQ H3G 1M8, Canada.; Sayrafian-Pour, K (reprint author), NIST, Informat Technol Lab, Gaithersburg, MD 20899 USA.
EM hamid.mahboobi@mail.mcgill.ca; aghdam@ece.concordia.ca;
ksayrafian@nist.gov
FU National Institute of Standards and Technology (NIST) [70NANB8H8146]
FX This work was supported by the National Institute of Standards and
Technology (NIST) under Grant 70NANB8H8146. Paper no. TII-15-0383.
NR 41
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PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 1551-3203
EI 1941-0050
J9 IEEE T IND INFORM
JI IEEE Trans. Ind. Inform.
PD APR
PY 2016
VL 12
IS 2
BP 576
EP 586
DI 10.1109/TII.2016.2521710
PG 11
WC Automation & Control Systems; Computer Science, Interdisciplinary
Applications; Engineering, Industrial
SC Automation & Control Systems; Computer Science; Engineering
GA DJ1FQ
UT WOS:000373949100013
ER
PT J
AU Li, SS
Schlamminger, S
Haddad, D
Seifert, F
Chao, L
Pratt, JR
AF Li, Shisong
Schlamminger, Stephan
Haddad, Darine
Seifert, Frank
Chao, Leon
Pratt, Jon R.
TI Coil motion effects in watt balances: a theoretical check
SO METROLOGIA
LA English
DT Article
DE watt balance; magnetic field measurement; the Planck constant;
systematic error
ID PLANCK CONSTANT; MAGNET SYSTEM; MARK II; REDEFINITION; KILOGRAM; DESIGN;
FIELD
AB A watt balance is a precision apparatus for the measurement of the Planck constant that has been proposed as a primary method for realizing the unit of mass in a revised International System of Units. In contrast to an ampere balance, which was historically used to realize the unit of current in terms of the kilogram, the watt balance relates electrical and mechanical units through a virtual power measurement and has far greater precision. However, because the virtual power measurement requires the execution of a prescribed motion of a coil in a fixed magnetic field, systematic errors introduced by horizontal and rotational deviations of the coil from its prescribed path will compromise the accuracy. We model these potential errors using an analysis that accounts for the fringing field in the magnet, creating a framework for assessing the impact of this class of errors on the uncertainty of watt balance results.
C1 [Li, Shisong] Tsinghua Univ, Dept Elect Engn, Beijing 100084, Peoples R China.
[Li, Shisong; Schlamminger, Stephan; Haddad, Darine; Seifert, Frank; Chao, Leon; Pratt, Jon R.] NIST, Gaithersburg, MD 20899 USA.
RP Li, SS (reprint author), Tsinghua Univ, Dept Elect Engn, Beijing 100084, Peoples R China.; Li, SS; Schlamminger, S (reprint author), NIST, Gaithersburg, MD 20899 USA.
EM leeshisong@sina.com; stephan.schlamminger@nist.gov
OI Li, Shisong/0000-0002-2509-5523
FU National Natural Science Foundation of China [51507088]
FX S Li acknowledges support from the National Natural Science Foundation
of China, grant #51507088.
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PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0026-1394
EI 1681-7575
J9 METROLOGIA
JI Metrologia
PD APR
PY 2016
VL 53
IS 2
BP 817
EP 828
DI 10.1088/0026-1394/53/2/817
PG 12
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA DI3CR
UT WOS:000373376300012
ER
PT J
AU Chalermsongsak, T
Hall, ED
Cole, GD
Follman, D
Seifert, F
Arai, K
Gustafson, EK
Smith, JR
Aspelmeyer, M
Adhikari, RX
AF Chalermsongsak, Tara
Hall, Evan D.
Cole, Garrett D.
Follman, David
Seifert, Frank
Arai, Koji
Gustafson, Eric K.
Smith, Joshua R.
Aspelmeyer, Markus
Adhikari, Rana X.
TI Coherent cancellation of photothermal noise in GaAs/Al0.92Ga0.08As Bragg
mirrors
SO METROLOGIA
LA English
DT Article
DE photothermal noise; AlGaAs; laser frequency stabilization; Fabry-Perot
cavities; gravitational waves
ID LASER STABILIZATION; THERMAL-NOISE; COATINGS; CAVITY; DISSIPATION;
REDUCTION; PHASE; LIGHT; GAAS
AB Thermal noise is a limiting factor in many high-precision optical experiments. A search is underway for novel optical materials with reduced thermal noise. One such pair of materials, gallium arsenide and aluminum-alloyed gallium arsenide (collectively referred to as AlGaAs), shows promise for its low Brownian noise when compared to conventional materials such as silica and tantala. However, AlGaAs has the potential to produce a high level of thermo-optic noise. We have fabricated a set of AlGaAs crystalline coatings, transferred to fused silica substrates, whose layer structure has been optimized to reduce thermo-optic noise by inducing coherent cancellation of the thermoelastic and thermorefractive effects. By measuring the photothermal transfer function of these mirrors, we find evidence that this optimization has been successful.
C1 [Chalermsongsak, Tara; Hall, Evan D.; Arai, Koji; Gustafson, Eric K.; Adhikari, Rana X.] CALTECH, LIGO Lab, MS 100-36, Pasadena, CA 91125 USA.
[Cole, Garrett D.; Follman, David] Crystalline Mirror Solut LLC, 114 E Haley,Suite G, Santa Barbara, CA 93101 USA.
[Cole, Garrett D.] Crystalline Mirror Solut GmbH, Parkring 10, A-1220 Vienna, Austria.
[Seifert, Frank] NIST, Joint Quantum Inst, 100 Bur Dr, Gaithersburg, MD 20899 USA.
[Seifert, Frank] Univ Maryland, 100 Bur Dr, Gaithersburg, MD 20899 USA.
[Smith, Joshua R.] Calif State Univ Fullerton, Dept Phys, Fullerton, CA 92831 USA.
[Aspelmeyer, Markus] Univ Vienna, Fac Phys, Vienna Ctr Quantum Sci & Technol VCQ, A-1090 Vienna, Austria.
RP Hall, ED (reprint author), CALTECH, LIGO Lab, MS 100-36, Pasadena, CA 91125 USA.
EM ehall@caltech.edu
RI Aspelmeyer, Markus/C-4098-2017
OI Aspelmeyer, Markus/0000-0003-4499-7335
FU National Science Foundation [PHY-0757058]; EURAMET/EMRP (QESOCAS);
Austrian Science Fund (FWF) [AI0090921]; AWS Seed program; Institute for
Quantum Information and Matter, an NSF Physics Frontiers Center; Gordon
and Betty Moore Foundation; NSF [PHY-1255650]
FX We gratefully acknowledge the informative discussions we have had
regarding thermal noise with the Optics and Advanced Interferometer
working groups of the LIGO Scientific Collaboration. In particular, we
appreciate the input from Y Levin, M Evans, J Eichholz, A Gretarsson and
K Yamamoto. We thank G Lovelace for pointing out an error in an earlier
version of this manuscript. TC, EDH, FS, KA, EKG, and RXA acknowledge
support from the National Science Foundation under PHY-0757058. GDC
acknowledges support from EURAMET/EMRP (QESOCAS). GDC and MA acknowledge
support by the Austrian Science Fund (FWF) through project AI0090921, as
well as funding by an AWS Seed program. A portion of this work was
performed in the UCSB Nanofabrication Facility. RXA gratefully
acknowledges funding provided by the Institute for Quantum Information
and Matter, an NSF Physics Frontiers Center with support of the Gordon
and Betty Moore Foundation. JRS is supported by NSF award PHY-1255650.
This article has the internal project designation LIGO-P1500054.
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PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0026-1394
EI 1681-7575
J9 METROLOGIA
JI Metrologia
PD APR
PY 2016
VL 53
IS 2
BP 860
EP 868
DI 10.1088/0026-1394/53/2/860
PG 9
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA DI3CR
UT WOS:000373376300018
ER
PT J
AU Wei, HY
Pomeroy, J
AF Wei, Haoyan
Pomeroy, Joshua
TI Application of the double paddle oscillator for quantifying
environmental, surface mass variation
SO METROLOGIA
LA English
DT Article
DE double paddle oscillator; microbalance; instability of mass artefacts;
gas adsorption and desorption
ID SINGLE-CRYSTAL SILICON; STAINLESS-STEEL; WATT BALANCE; PRECISION
DETERMINATION; ADSORPTION LAYERS; PLANCK CONSTANT; NOBLE-GAS; STANDARDS;
KILOGRAM; STABILITY
AB Sub-monolayer sensitivity to controlled gas adsorption and desorption is demonstrated using a double paddle oscillator (DPO) installed within an ultra-high vacuum (UHV) environmental chamber equipped with in situ film deposition, (multi) gas admission and temperature control. This effort is intended to establish a robust framework for quantitatively comparing mass changes due to gas loading and unloading on different materials systems selected or considered for use as mass artefacts. Our apparatus is composed of a UHV chamber with gas introduction and temperature control and in situ materials deposition for future materials testing enabling in situ preparation of virgin surfaces that can be monitored during initial exposure to gasses of interest. These tools are designed to allow us to comparatively evaluate how different materials gain or lose mass due to precisely controlled environmental excursions, with a long term goal of measuring changes in absolute mass. Herein, we provide a detailed experimental description of the apparatus, an evaluation of the initial performance, and demonstration measurements using nitrogen adsorption and desorption directly on the DPO.
C1 [Wei, Haoyan; Pomeroy, Joshua] NIST, Quantum Measurement Div, Gaithersburg, MD 20899 USA.
[Wei, Haoyan] Univ Maryland, Joint Quantum Inst, College Pk, MD 20742 USA.
RP Pomeroy, J (reprint author), NIST, Quantum Measurement Div, Gaithersburg, MD 20899 USA.
EM joshua.pomeroy@nist.gov
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PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0026-1394
EI 1681-7575
J9 METROLOGIA
JI Metrologia
PD APR
PY 2016
VL 53
IS 2
BP 869
EP 880
DI 10.1088/0026-1394/53/2/869
PG 12
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA DI3CR
UT WOS:000373376300019
ER
PT J
AU Covey, JP
Moses, SA
Gaerttner, M
Safavi-Naini, A
Miecnikowski, MT
Fu, ZK
Schachenmayer, J
Julienne, PS
Rey, AM
Jin, DS
Ye, J
AF Covey, Jacob P.
Moses, Steven A.
Gaerttner, Martin
Safavi-Naini, Arghavan
Miecnikowski, Matthew T.
Fu, Zhengkun
Schachenmayer, Johannes
Julienne, Paul S.
Rey, Ana Maria
Jin, Deborah S.
Ye, Jun
TI Doublon dynamics and polar molecule production in an optical lattice
SO NATURE COMMUNICATIONS
LA English
DT Article
ID ATOMS; GAS
AB Polar molecules in an optical lattice provide a versatile platform to study quantum many-body dynamics. Here we use such a system to prepare a density distribution where lattice sites are either empty or occupied by a doublon composed of an interacting Bose-Fermi pair. By letting this out-of-equilibrium system evolve from a well-defined, but disordered, initial condition, we observe clear effects on pairing that arise from inter-species interactions, a higher partial-wave Feshbach resonance and excited Bloch-band population. These observations facilitate a detailed understanding of molecule formation in the lattice. Moreover, the interplay of tunnelling and interaction of fermions and bosons provides a controllable platform to study Bose-Fermi Hubbard dynamics. Additionally, we can probe the distribution of the atomic gases in the lattice by measuring the inelastic loss of doublons. These techniques realize tools that are generically applicable to studying the complex dynamics of atomic mixtures in optical lattices.
C1 [Covey, Jacob P.; Moses, Steven A.; Gaerttner, Martin; Safavi-Naini, Arghavan; Miecnikowski, Matthew T.; Fu, Zhengkun; Schachenmayer, Johannes; Rey, Ana Maria; Jin, Deborah S.; Ye, Jun] NIST, JILA, Boulder, CO 80309 USA.
[Covey, Jacob P.; Moses, Steven A.; Gaerttner, Martin; Safavi-Naini, Arghavan; Miecnikowski, Matthew T.; Fu, Zhengkun; Schachenmayer, Johannes; Rey, Ana Maria; Jin, Deborah S.; Ye, Jun] Univ Colorado, Boulder, CO 80309 USA.
[Covey, Jacob P.; Moses, Steven A.; Gaerttner, Martin; Safavi-Naini, Arghavan; Miecnikowski, Matthew T.; Fu, Zhengkun; Schachenmayer, Johannes; Rey, Ana Maria; Jin, Deborah S.; Ye, Jun] Univ Colorado, Dept Phys, Boulder, CO 80309 USA.
[Julienne, Paul S.] Univ Maryland, Joint Quantum Inst, College Pk, MD 20702 USA.
[Julienne, Paul S.] NIST, College Pk, MD 20702 USA.
RP Jin, DS; Ye, J (reprint author), NIST, JILA, Boulder, CO 80309 USA.; Jin, DS; Ye, J (reprint author), Univ Colorado, Boulder, CO 80309 USA.; Jin, DS; Ye, J (reprint author), Univ Colorado, Dept Phys, Boulder, CO 80309 USA.
EM jin@jilau1.colorado.edu; ye@jila.colorado.edu
RI Ye, Jun/C-3312-2011
FU NIST; NSF [1125844]; AFOSR-MURI; ARO-MURI; ARO; NDSEG fellowship;
[NSF-PIF-1211914]
FX We thank M. Wall for useful discussions. We acknowledge funding for this
work from NIST, NSF grant number 1125844, NSF-PIF-1211914, AFOSR-MURI,
ARO-MURI, and ARO. J.P.C. acknowledges funding from the NDSEG
fellowship. Part of the computation for this work was performed at the
University of Oklahoma Supercomputing Center for Education and Research
(OSCER).
NR 38
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U1 5
U2 12
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 2041-1723
J9 NAT COMMUN
JI Nat. Commun.
PD APR
PY 2016
VL 7
AR 11279
DI 10.1038/ncomms11279
PG 8
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DJ3SL
UT WOS:000374126300001
PM 27075831
ER
PT J
AU Lootens, D
Bentz, DP
AF Lootens, Didier
Bentz, Dale P.
TI On the relation of setting and early-age strength development to
porosity and hydration in cement-based materials
SO CEMENT & CONCRETE COMPOSITES
LA English
DT Article
DE Calorimetry; Hydration; Percolation; Porosity; Setting; Strength;
Ultrasonic reflection
ID ULTRASONIC MEASUREMENTS; WATER; MICROSTRUCTURE; CONCRETE; RATIO;
BEHAVIOR; MORTAR; PASTE
AB Previous research has demonstrated a linear relationship between compressive strength (mortar cubes and concrete cylinders) and cumulative heat release normalized per unit volume of (mixing) water for a wide variety of cement-based mixtures at ages of 1 d and beyond. This paper utilizes concurrent ultrasonic reflection and calorimetry measurements to further explore this relationship from the time of specimen casting to 3 d. The ultrasonic measurements permit a continuous evaluation of thickening, setting, and strength development during this time period for comparison with the ongoing chemical reactions, as characterized by isothermal calorimetry measurements. Initially, the ultrasonic strength heat release relation depends strongly on water-to-cement ratio, as well as admixture additions, with no universal behavior. Still, each individual strength-heat release curve is consistent with a percolation based view of the cement setting process. However, beyond about 8 h for the systems investigated in the present study, the various strength-heat release curves merge towards a single relationship that broadly characterizes the development of strength as a function of heat released (fractional space filled), demonstrating that mortar and/or concrete strength at early ages can be effectively monitored using either ultrasonic or calorimetry measurements on small paste or mortar specimens. Published by Elsevier Ltd.
C1 [Lootens, Didier] Sika Technol AG, Tuffenwies 16, CH-8048 Zurich, Switzerland.
[Bentz, Dale P.] NIST, Engn Lab, 100Bur Dr,Stop 8615, Gaithersburg, MD 20899 USA.
RP Bentz, DP (reprint author), NIST, Engn Lab, 100Bur Dr,Stop 8615, Gaithersburg, MD 20899 USA.
EM lootens.didier@ch.sika.com; dale.bentz@nist.gov
FU Intramural NIST DOC [9999-NIST]
NR 27
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U1 5
U2 12
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0958-9465
EI 1873-393X
J9 CEMENT CONCRETE COMP
JI Cem. Concr. Compos.
PD APR
PY 2016
VL 68
BP 9
EP 14
DI 10.1016/j.cemconcomp.2016.02.010
PG 6
WC Construction & Building Technology; Materials Science, Composites
SC Construction & Building Technology; Materials Science
GA DI7AE
UT WOS:000373650700002
PM 27046956
ER
PT J
AU Rangwala, I
Sinsky, E
Miller, JR
AF Rangwala, Imtiaz
Sinsky, Eric
Miller, James R.
TI Variability in projected elevation dependent warming in boreal
midlatitude winter in CMIP5 climate models and its potential drivers
SO CLIMATE DYNAMICS
LA English
DT Article
DE Elevation dependent warming; Mountains; Rocky Mountains; Tibetan
Plateau; Water vapor; Snow albedo; Feedbacks; Temperature; EDW; Winter;
CMIP5; GCM
ID TEMPERATURE TRENDS; ROCKY-MOUNTAINS; FEEDBACK; SNOW; AIR
AB The future rate of climate change in mountains has many potential human impacts, including those related to water resources, ecosystem services, and recreation. Analysis of the ensemble mean response of CMIP5 global climate models (GCMs) shows amplified warming in high elevation regions during the cold season in boreal midlatitudes. We examine how the twenty-first century elevation-dependent response in the daily minimum surface air temperature [d(Delta Tmin)/dz] varies among 27 different GCMs during winter for the RCP 8.5 emissions scenario. The focus is on regions within the northern hemisphere mid-latitude band between 27.5A degrees N and 40A degrees N, which includes both the Rocky Mountains and the Tibetan Plateau/Himalayas. We find significant variability in d(Delta Tmin)/dz among the individual models ranging from 0.16 A degrees C/km (10th percentile) to 0.97 A degrees C/km (90th percentile), although nearly all of the GCMs (24 out of 27) show a significant positive value for d(Delta Tmin)/dz. To identify some of the important drivers associated with the variability in d(Delta Tmin)/dz during winter, we evaluate the co-variance between d(Delta Tmin)/dz and the differential response of elevation-based anomalies in different climate variables as well as the GCMs' spatial resolution, their global climate sensitivity, and their elevation-dependent free air temperature response. We find that d(Delta Tmin)/dz has the strongest correlation with elevation-dependent increases in surface water vapor, followed by elevation-dependent decreases in surface albedo, and a weak positive correlation with the GCMs' free air temperature response.
C1 [Rangwala, Imtiaz] Univ Colorado, Cooperat Inst Res Environm Sci, Western Water Assessment, Boulder, CO 80309 USA.
[Rangwala, Imtiaz] NOAA ESRL, Div Phys Sci, 325 Broadway, Boulder, CO USA.
[Sinsky, Eric] Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA.
[Miller, James R.] Rutgers State Univ, Dept Marine & Coastal Sci, New Brunswick, NJ 08903 USA.
RP Rangwala, I (reprint author), Univ Colorado, Cooperat Inst Res Environm Sci, Western Water Assessment, Boulder, CO 80309 USA.; Rangwala, I (reprint author), NOAA ESRL, Div Phys Sci, 325 Broadway, Boulder, CO USA.
EM imtiaz.rangwala@noaa.gov
FU National Science Foundation [AGS-1064326, AGS-1064281]
FX We thank the two anonymous reviewers for their time and helpful
suggestions. This research is supported by the National Science
Foundation Grants: AGS-1064326 and AGS-1064281. We acknowledge KNMI and
ESGF data portals for access to CMIP5 data. We thank C. Naud and J.
Barsugli for helpful comments.
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U1 5
U2 9
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0930-7575
EI 1432-0894
J9 CLIM DYNAM
JI Clim. Dyn.
PD APR
PY 2016
VL 46
IS 7-8
BP 2115
EP 2122
DI 10.1007/s00382-015-2692-0
PG 8
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DI4AR
UT WOS:000373442900006
ER
PT J
AU Krishnamurthy, L
Krishnamurthy, V
AF Krishnamurthy, Lakshmi
Krishnamurthy, V.
TI Teleconnections of Indian monsoon rainfall with AMO and Atlantic tripole
SO CLIMATE DYNAMICS
LA English
DT Article
DE Indian monsoon; AMO; Atlantic tripole; NAO; NCAR CCSM4; Decadal
variability
ID ASIAN SUMMER MONSOON; TROPICAL ATLANTIC; MULTIDECADAL OSCILLATION;
INTERANNUAL VARIABILITY; ENSO RELATIONSHIP; COLORED NOISE; OCEAN;
CLIMATE; FREQUENCY; PREDICTABILITY
AB The teleconnections between the decadal modes in the Indian monsoon rainfall (IMR) and the North Atlantic sea surface temperature are investigated. The two decadal modes of variability in the North Atlantic, the Atlantic multidecadal oscillation (AMO) and the Atlantic tripole, have opposite relation with the two decadal modes of IMR. The AMO has positive correlation with the monsoon rainfall while the Atlantic tripole has negative correlation. This study has put forward hypotheses for the mechanisms involved in the teleconnections of the AMO and the Atlantic tripole with the IMR. The warm phase of AMO may influence the monsoon through the summer North Atlantic Oscillation (SNAO) and further through the equatorial zonal winds which increase the moisture flow over India by enhancing the southwesterly flow. The warm phase of Atlantic tripole may impact the monsoon through the all-season NAO, leading to decreased moisture flow over India through the equatorial wind pattern. The observed relations between the decadal modes in the North Atlantic and the Indian monsoon are explored in the simulations of National Center for Atmospheric Research Community Climate System Model version 4 (CCSM4) model. Although the model supports the observed decadal teleconnection between the Atlantic Ocean and Indian monsoon, it has limitations in capturing the details of the spatial pattern associated with the teleconnection. The teleconnections of AMO and Atlantic tripole with the Indian monsoon is further demonstrated through an experiment with CCSM4 by decoupling the North Atlantic Ocean. The hypotheses for the mechanisms of the Atlantic teleconnections are also explored in the CCSM4 simulation.
C1 [Krishnamurthy, Lakshmi; Krishnamurthy, V.] George Mason Univ, Dept Atmospher Ocean & Earth Sci, Fairfax, VA 22030 USA.
[Krishnamurthy, V.] Inst Global Environm & Soc, Ctr Ocean Land Atmosphere Studies, Fairfax, VA USA.
[Krishnamurthy, Lakshmi] Princeton Univ, UCAR NOAA Geophys Fluid Dynam Lab, Forrestal Campus,201 Forrestal Rd, Princeton, NJ 08540 USA.
RP Krishnamurthy, L (reprint author), George Mason Univ, Dept Atmospher Ocean & Earth Sci, Fairfax, VA 22030 USA.; Krishnamurthy, L (reprint author), Princeton Univ, UCAR NOAA Geophys Fluid Dynam Lab, Forrestal Campus,201 Forrestal Rd, Princeton, NJ 08540 USA.
EM Lakshmi.Krishnamurthy@noaa.gov
FU National Science Foundation [ATM-0830062, ATM-0830068]; National Oceanic
and Atmospheric Administration [A09OAR4310058]; National Aeronautics and
Space Administration [NNX09AN50G]
FX This work was supported by grants from National Science Foundation
(ATM-0830062 and ATM-0830068), National Oceanic and Atmospheric
Administration (A09OAR4310058), and National Aeronautics and Space
Administration (NNX09AN50G). The authors thank National Center for
Atmospheric Research for computer time, the model control data and
technical help with model experiments, and Bohua Huang and Yohan
Ruprich-Robert for helpful discussions. We also thank two anonymous
reviewers for their insights which has helped to improve this
manuscript. This work formed a part of the Ph.D. thesis of Lakshmi
Krishnamurthy at George Mason University.
NR 43
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U1 7
U2 10
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0930-7575
EI 1432-0894
J9 CLIM DYNAM
JI Clim. Dyn.
PD APR
PY 2016
VL 46
IS 7-8
BP 2269
EP 2285
DI 10.1007/s00382-015-2701-3
PG 17
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DI4AR
UT WOS:000373442900015
ER
PT J
AU Wang, ZZ
Chiang, MYM
AF Wang, Zhengzhi
Chiang, Martin Y. M.
TI System compliance dictates the effect of composite filler content on
polymerization shrinkage stress
SO DENTAL MATERIALS
LA English
DT Article
DE Dental composites; Polymerization shrinkage stress; Filler content;
Curing kinetics; Compliance of constraint
ID DENTAL RESIN-COMPOSITES; LIGHT-CURED COMPOSITES; CONTRACTION STRESS;
INSTRUMENT COMPLIANCE; RESTORATIVE RESINS; PARTICLE-SIZE; C-FACTOR;
CONVERSION; PHOTOPOLYMERIZATION; KINETICS
AB Objective. The effect of filler content in dental restorative composites on the polymerization shrinkage stress (PS) is not straightforward and has caused much debate in the literature. Our objective in this study was to clarify the PS/filler content relationship based on analytical and experimental approaches, so that guidelines for materials comparison in terms of PS and clinical selection of dental composites with various filler content can be provided.
Methods. Analytically, a simplified model based on linear elasticity was utilized to predict PS as a function of filler content under various compliances of the testing system, a cantilever beam-based instrument used in this study. The predictions were validated by measuring PS of composites synthesized using 50/50 mixtures of two common dimethacrylate resins with a variety of filler contents.
Results. Both experiments and predictions indicated that the influence of filler content on the PS highly depended on the compliance of the testing system. Within the clinic-relevant range of compliances and for the specific sample configuration tested, the PS increased with increasing filler content at low compliance of instrument, while increasing the compliance caused the effect of filler content on the PS to gradually diminish. Eventually, at high compliance, the PS inverted and decreased with increasing filler content.
Significance. This compliance-dependent effect of filler content on PS suggests: (1) for materials comparison in terms of PS, the specific compliance at which the comparison being done should always be reported and (2) clinically, composites with relatively lower filler content could be selected for such cavities with relatively lower compliance (e.g. a Class-I cavity with thick tooth walls or the basal part in a cavity) and vice versa in order to reduce the final PS. Published by Elsevier Ltd on behalf of Academy of Dental Materials.
C1 [Wang, Zhengzhi; Chiang, Martin Y. M.] NIST, Biosyst & Biomat Div, Gaithersburg, MD 20899 USA.
[Wang, Zhengzhi] Wuhan Univ, Sch Civil Engn, Dept Engn Mech, Wuhan 430072, Peoples R China.
RP Chiang, MYM (reprint author), NIST, Biosyst & Biomat Div, Gaithersburg, MD 20899 USA.
EM martin.chiang@nist.gov
FU National Institute of Dental and Craniofacial Research (NIDCR)
[Y1-DE-7005-01]; NIST [Y1-DE-7005-01]
FX Financial support was provided through an Interagency Agreement between
the National Institute of Dental and Craniofacial Research (NIDCR) and
NIST (Y1-DE-7005-01). We thank Dr. Forrest A. Landis and Dr. Joseph M.
Antonucci for their help in preparing the composites, Dr. Jae Hyun Kim
and Mr. Anthony A.M. Giuseppetti for their help in the elastic modulus
measurement.
NR 55
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U1 5
U2 9
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0109-5641
EI 1879-0097
J9 DENT MATER
JI Dent. Mater.
PD APR
PY 2016
VL 32
IS 4
BP 551
EP 560
DI 10.1016/j.dental.2016.01.006
PG 10
WC Dentistry, Oral Surgery & Medicine; Materials Science, Biomaterials
SC Dentistry, Oral Surgery & Medicine; Materials Science
GA DI4TU
UT WOS:000373493100010
PM 26916062
ER
PT J
AU Guo, YW
Landis, FA
Wang, ZZ
Bai, D
Jiang, L
Chiang, MYM
AF Guo, Yongwen
Landis, Forrest A.
Wang, Zhengzhi
Bai, Ding
Jiang, Li
Chiang, Martin Y. M.
TI Polymerization stress evolution of a bulk-fill flowable composite under
different compliances
SO DENTAL MATERIALS
LA English
DT Article
DE Bulk-fill flowable composite; Polymerization stress; Exotherm; Degree of
conversion; Compliance
ID DENTAL RESIN-COMPOSITES; LIGHT-CURED COMPOSITES; SHRINKAGE-STRESS;
THERMAL-EXPANSION; CONTRACTION STRESS; INSTRUMENT COMPLIANCE; KINETICS;
CONVERSION; PHOTOPOLYMERIZATION; RESTORATIONS
AB Objective. To use a compliance-variable instrument to simultaneously measure and compare the polymerization stress (PS) evolution, degree of conversion (DC), and exotherm of a bulk fill flowable composite to a packable composite.
Methods. A bulk-fill flowable composite (Filtek Bulk-fill, FBF) and a conventional packable composite (Filtek Z250, Z250) purchased from 3 M ESPE were investigated. The composites were studied using a cantilever-beam based instrument equipped with an in situ near infrared (NIR) spectrometer and a microprobe thermocouple. The measurements were carried out under various instrumental compliances (ranging from 0.3327 mu m/N to 12.3215 mu m/N) that are comparable to the compliances of clinically prepared tooth cavities. Correlations between the PS and temperature change as well as the DC were interpreted.
Results. The maximum PS of both composites at 10 min after irradiation decreased with the increase in the compliance of the cantilever beam. The FBF composite generated a lower final stress than the Z250 sample under instrumental compliances less than ca. 4 mu m/N; however, both materials generated statistically similar PS values at higher compliances. The reaction exotherm and the DC of both materials were found to be independent of compliance. The DC of the FBF sample was slightly higher than that of the packable Z250 composite while the peak exotherm of FBF was almost double that of the Z250 composite. For FBF, a characteristic drop in the PS was observed during the early stage of polymerization for all compliances studied which was not observed in the Z250 sample. This drop was shown to relate to the greater exotherm of the less-filled FBF sample relative to the Z250 composite.
Significance. While the composites with lower filler content (low viscosity) are generally considered to have lower PS than the conventional packable composites, a bulk-fill flowable composite was shown to produce lower PS under a lower compliance of constraint as would be experienced if the composite was used as the base material in clinical procedures. Published by Elsevier Ltd on behalf of Academy of Dental Materials.
C1 [Guo, Yongwen; Bai, Ding; Jiang, Li] Sichuan Univ, West China Sch Stomatol, Dept Orthodont, State Key Lab Oral Dis, Chengdu 610041, Peoples R China.
[Guo, Yongwen; Wang, Zhengzhi; Bai, Ding; Jiang, Li; Chiang, Martin Y. M.] NIST, Biosyst & Biomat Div, Gaithersburg, MD 20899 USA.
[Landis, Forrest A.] Penn State Univ, Dept Chem, York Campus, York, PA 17403 USA.
RP Chiang, MYM (reprint author), NIST, Biosyst & Biomat Div, Gaithersburg, MD 20899 USA.
EM martin.chiang@nist.gov
FU China Scholarship Council; National Institute of Dental and Craniofacial
Research [Y1-DE-7005-01]; National Institute of Standards and
Technology, NIH/NIDCR [Y1-DE-7005-01]
FX This study is based on research that was funded through the China
Scholarship Council and an Interagency Agreement between the National
Institute of Dental and Craniofacial Research and the National Institute
of Standards and Technology, NIH/NIDCR [Y1-DE-7005-01].
NR 40
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U1 6
U2 15
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0109-5641
EI 1879-0097
J9 DENT MATER
JI Dent. Mater.
PD APR
PY 2016
VL 32
IS 4
BP 578
EP 586
DI 10.1016/j.dental.2016.01.009
PG 9
WC Dentistry, Oral Surgery & Medicine; Materials Science, Biomaterials
SC Dentistry, Oral Surgery & Medicine; Materials Science
GA DI4TU
UT WOS:000373493100013
PM 26861171
ER
PT J
AU Lee, WS
Monaghan, P
Metcalfe, NB
AF Lee, Who-Seung
Monaghan, Pat
Metcalfe, Neil B.
TI Perturbations in growth trajectory due to early diet affect age-related
deterioration in performance
SO FUNCTIONAL ECOLOGY
LA English
DT Article
DE ageing; compensatory growth; life history; nutrition; senescence;
trade-off
ID CATCH-UP GROWTH; JUVENILE BROWN TROUT; COMPENSATORY GROWTH; TRADE-OFF;
GASTEROSTEUS-ACULEATUS; SWIMMING PERFORMANCE; OXIDATIVE STRESS;
LIFE-SPAN; 3-SPINED STICKLEBACK; REPRODUCTIVE EFFORT
AB Fluctuations in early developmental conditions can cause changes in growth trajectories that subsequently affect the adult phenotype. Here, we investigated whether compensatory growth has long-term consequences for patterns of senescence. Using three-spined sticklebacks (Gasterosteus aculeatus), we show that a brief period of dietary manipulation in early life affected skeletal growth rate not only during the manipulation itself, but also during a subsequent compensatory phase when fish caught up in size with controls. However, this growth acceleration influenced swimming endurance and its decline over the course of the breeding season, with a faster decline in fish that had undergone faster growth compensation. Similarly, accelerated growth led to a more pronounced reduction in the breeding period (as indicated by the duration of sexual ornamentation) over the following two breeding seasons, suggesting faster reproductive senescence. Parallel experiments showed a heightened effect of accelerated growth on these age-related declines in performance if the fish were under greater time stress to complete their compensation prior to the breeding season. Compensatory growth led to a reduction in median life span of 12% compared to steadily growing controls. While life span was independent of the eventual adult size attained, it was negatively correlated with the age-related decline in swimming endurance and sexual ornamentation. These results, complementary to those found when growth trajectories were altered by temperature rather than dietary manipulations, show that the costs of accelerated growth can last well beyond the time over which growth rates differ and are affected by the time available until an approaching life-history event such as reproduction.
C1 [Lee, Who-Seung; Monaghan, Pat; Metcalfe, Neil B.] Univ Glasgow, Coll Med Vet & Life Sci, Inst Biodivers Anim Hlth & Comparat Med, Graham Kerr Bldg, Glasgow G12 8QQ, Lanark, Scotland.
[Lee, Who-Seung] Univ Calif Santa Cruz, Southwest Fisheries Sci Cente, NOAA Fisheries, Santa Cruz, CA 95064 USA.
[Lee, Who-Seung] Univ Calif Santa Cruz, Ctr Stock Assessment Res, Santa Cruz, CA 95064 USA.
RP Lee, WS (reprint author), Univ Glasgow, Coll Med Vet & Life Sci, Inst Biodivers Anim Hlth & Comparat Med, Graham Kerr Bldg, Glasgow G12 8QQ, Lanark, Scotland.; Lee, WS (reprint author), Univ Calif Santa Cruz, Southwest Fisheries Sci Cente, NOAA Fisheries, Santa Cruz, CA 95064 USA.; Lee, WS (reprint author), Univ Calif Santa Cruz, Ctr Stock Assessment Res, Santa Cruz, CA 95064 USA.
EM whoseung@gmail.com
RI Monaghan, Pat/E-6810-2015; Metcalfe, Neil/C-5997-2009
OI Metcalfe, Neil/0000-0002-1970-9349
FU University of Glasgow Postgraduate Scholarship; Overseas Research
Student Award; ERC Advanced grant [268926, 322784]; NERC [NE/K00400X/1]
FX We thank Graham Law, John Laurie and Alastair Kirk for help with fish
husbandry. WSL was funded by a University of Glasgow Postgraduate
Scholarship and an Overseas Research Student Award. PM was funded by ERC
Advanced grant 268926, and NBM was funded by ERC Advanced Grant 322784;
both PM and NBM were funded by NERC grant NE/K00400X/1.
NR 64
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U2 8
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0269-8463
EI 1365-2435
J9 FUNCT ECOL
JI Funct. Ecol.
PD APR
PY 2016
VL 30
IS 4
BP 625
EP 635
DI 10.1111/1365-2435.12538
PG 11
WC Ecology
SC Environmental Sciences & Ecology
GA DJ0UV
UT WOS:000373920800014
ER
PT J
AU Hull, RN
Luoma, SN
Bayne, BA
Iliff, J
Larkin, DJ
Paschke, MW
Victor, SL
Ward, SE
AF Hull, Ruth N.
Luoma, Samuel N.
Bayne, Bruce A.
Iliff, John
Larkin, Daniel J.
Paschke, Mark W.
Victor, Sasha L.
Ward, Sara E.
TI Opportunities and challenges of integrating ecological restoration into
assessment and management of contaminated ecosystems
SO INTEGRATED ENVIRONMENTAL ASSESSMENT AND MANAGEMENT
LA English
DT Article
DE Early integration; Ecosystem services; Monitoring; Restoration
ID GLOBAL CLIMATE-CHANGE; REMEDIATION; STREAMS
AB Ecosystem restoration planning near the beginning of the site assessment and management process (early integration) involves consideration of restoration goals from the outset in developing solutions for contaminated ecosystems. There are limitations to integration that stem from institutional barriers, few successful precedents, and limited availability of guidance. Challenges occur in integrating expertise from various disciplines and multiple, sometimes divergent interests and goals. The more complex process can result in timing, capacity, communication, and collaboration challenges. On the other hand, integrating the 2 approaches presents new and creative opportunities. For example, integration allows early planning for expanding ecosystem services on or near contaminated lands or waters that might otherwise have been unaddressed by remediation alone. Integrated plans can explicitly pursue ecosystem services that have market value, which can add to funds for long-term monitoring and management. Early integration presents opportunities for improved and productive collaboration and coordination between ecosystem restoration and contaminant assessment and management. Examples exist where early integration facilitates liability resolution and generates positive public relations. Restoration planning and implementation before the completion of the contaminated site assessment, remediation, or management process (early restoration) can facilitate coordination with offsite restoration options and a regional approach to restoration of contaminated environments. Integration of performance monitoring, for both remedial and restoration actions, can save resources and expand the interpretive power of results. Early integration may aid experimentation, which may be more feasible on contaminated lands than in many other situations. The potential application of concepts and tools from adaptive management is discussed as a way of avoiding pitfalls and achieving benefits in early integration. In any case, there will be challenges with early integration of restoration concepts for contaminated ecosystems, but the benefits are likely to outweigh them. Integr Environ Assess Manag 2016;12:296-305. (c) 2015 The Authors. Integrated Environmental Assessment and Management published by Wiley Periodicals, Inc. on behalf of Society of Environmental Toxicology & Chemistry (SETAC)
C1 [Hull, Ruth N.] Intrinsik Environm Sci, Mississauga, ON, Canada.
[Luoma, Samuel N.] Univ Calif Davis, John Muir Inst Environm, Davis, CA 95616 USA.
[Bayne, Bruce A.] AECOM, Conshohocken, PA USA.
[Iliff, John] NOAA, NMFS Off Habitat Conservat, Operat Management & Informat Div, Silver Spring, MD USA.
[Larkin, Daniel J.] Univ Minnesota, Dept Fisheries Wildlife & Conservat Biol, St Paul, MN 55108 USA.
[Paschke, Mark W.; Victor, Sasha L.] Colorado State Univ, Dept Forest & Rangeland Stewardship, Ft Collins, CO 80523 USA.
[Ward, Sara E.] US Fish & Wildlife Serv, Raleigh Ecol Serv Field Off, Raleigh, NC USA.
RP Hull, RN (reprint author), Intrinsik Environm Sci, Mississauga, ON, Canada.
EM rhull@intrinsik.com
FU Anchor QEA LLC; Chevron; CSIRO; DuPont; ExxonMobil; Honeywell;
Industrial Economics; Intrinsik Environmental Sciences; Integral
Consulting; Matrix New World Engineering; Newmont Mining; Rio Tinto;
Teck Metals; Conservation Fund; URS Corporation; US Department of the
Interior; Windward Environmental LLC.
FX We gratefully acknowledge the SETAC North America staff, in particular
Greg Schiefer and Nikki Mayo, who provided support to us before, during,
and after the workshop. We appreciate the funding support from the
following groups that made the workshop possible: Anchor QEA LLC,
Chevron, CSIRO, DuPont, ExxonMobil, Honeywell, Industrial Economics,
Intrinsik Environmental Sciences, Integral Consulting, Matrix New World
Engineering, Newmont Mining, Rio Tinto, Teck Metals, The Conservation
Fund, URS Corporation, US Department of the Interior, and Windward
Environmental LLC.
NR 41
TC 2
Z9 2
U1 7
U2 10
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 1551-3777
EI 1551-3793
J9 INTEGR ENVIRON ASSES
JI Integr. Environ. Assess. Manag.
PD APR
PY 2016
VL 12
IS 2
BP 296
EP 305
DI 10.1002/ieam.1714
PG 10
WC Environmental Sciences; Toxicology
SC Environmental Sciences & Ecology; Toxicology
GA DI3KG
UT WOS:000373396900010
PM 26419951
ER
PT J
AU Hao, ZC
Hong, Y
Xia, YL
Singh, VP
Hao, FH
Cheng, HG
AF Hao, Zengchao
Hong, Yang
Xia, Youlong
Singh, Vijay P.
Hao, Fanghua
Cheng, Hongguang
TI Probabilistic drought characterization in the categorical form using
ordinal regression
SO JOURNAL OF HYDROLOGY
LA English
DT Article
DE Drought; Drought indices; Drought category; US Drought Monitor
ID UNITED-STATES; INDEX; MODELS; MONITOR
AB Drought is an insidious natural hazard that may cause tremendous losses to different sectors, including agriculture and ecosystems. Reliable drought monitoring and early warning are of critical importance for drought preparedness planning and mitigation to reduce potential impacts. Traditional drought monitoring is generally based on drought indices, such as Standardized Precipitation Index (SPI), that are computed from hydro-climatic variables. The U.S. Drought Monitor (USDM) classifies drought conditions into different drought categories to provide composite drought information by integrating multiple drought indices, which has been commonly used to aid decision making at the federal, state, and local levels. Characterizing drought in categories similar to USDM would be important for decision making for both research and operational purposes. However, drought monitoring, based on a variety of drought indices, is challenged by the classification of drought into categories used by USDM. In this study, an ordinal regression model is proposed to characterize droughts in USDM drought categories based on several drought indices, in which the probability of each drought category can be estimated. The proposed method is assessed by comparing with USDM in Texas and a satisfactory performance for estimating drought categories is revealed. (C) 2016 Published by Elsevier B.V.
C1 [Hao, Zengchao; Hao, Fanghua; Cheng, Hongguang] Beijing Normal Univ, Sch Environm, Green Dev Inst, Beijing 100875, Peoples R China.
[Hao, Zengchao; Hong, Yang] Hydrometeorol & Remote Sensing Lab, Norman, OK USA.
[Hao, Zengchao; Hong, Yang] Adv Radar Res Ctr, Norman, OK USA.
[Hong, Yang] Univ Oklahoma, Sch Civil Engn & Environm Sci, Norman, OK 73019 USA.
[Xia, Youlong] Natl Ctr Environm Predict, IM Syst Grp Environm Modeling Ctr, College Pk, MD USA.
[Singh, Vijay P.] Texas A&M Univ, Dept Biol & Agr Engn, College Stn, TX USA.
[Singh, Vijay P.] Texas A&M Univ, Zachry Dept Civil Engn, College Stn, TX USA.
RP Hong, Y (reprint author), 120 David L Boren Blvd,Suite 4610, Norman, OK 73072 USA.
EM haozc@bnu.edu.cn; yanghong@ou.edu
RI Hong, Yang/D-5132-2009
OI Hong, Yang/0000-0001-8720-242X
FU Beijing Normal University [2015NT02]; National Natural Science
Foundation of China (NSFC)-CGIAR Project [71461010701]
FX This work is supported by Youth Scholars Program of Beijing Normal
University (Grant No. 2015NT02) and National Natural Science Foundation
of China (NSFC)-CGIAR Project (No. 71461010701). We thank the
Environmental Modeling Center (EMC) of the National Centers for
Environmental Prediction (NCEP), National Oceanic and Atmospheric
Administration (NOAA) for providing NLDAS-2 datasets.
NR 44
TC 1
Z9 1
U1 2
U2 9
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0022-1694
EI 1879-2707
J9 J HYDROL
JI J. Hydrol.
PD APR
PY 2016
VL 535
BP 331
EP 339
DI 10.1016/j.jhydrol.2016.01.074
PG 9
WC Engineering, Civil; Geosciences, Multidisciplinary; Water Resources
SC Engineering; Geology; Water Resources
GA DI3TN
UT WOS:000373421500028
ER
PT J
AU Haugland, RA
Siefring, S
Varma, M
Oshima, KH
Sivaganesan, M
Cao, YP
Raith, M
Griffith, J
Weisberg, SB
Noble, RT
Blackwood, AD
Kinzelman, J
Anan'eva, T
Bushon, RN
Stelzer, EA
Harwood, VJ
Gordon, KV
Sinigalliano, C
AF Haugland, Richard A.
Siefring, Shawn
Varma, Manju
Oshima, Kevin H.
Sivaganesan, Mano
Cao, Yiping
Raith, Meredith
Griffith, John
Weisberg, Stephen B.
Noble, Rachel T.
Blackwood, A. Denene
Kinzelman, Julie
Anan'eva, Tamara
Bushon, Rebecca N.
Stelzer, Erin A.
Harwood, Valarie J.
Gordon, Katrina V.
Sinigalliano, Christopher
TI Multi-laboratory survey of qPCR enterococci analysis method performance
in US coastal and inland surface waters
SO JOURNAL OF MICROBIOLOGICAL METHODS
LA English
DT Article
DE Enterococci; qPCR; Interference; Performance; EPA Method 1609; EPA
Method 1611
ID POLYMERASE-CHAIN-REACTION; CULTURE-BASED METHODS; QUANTITATIVE PCR;
ENVIRONMENTAL WATERS; MARINE BEACHES; ENUMERATION; QUALITY;
QUANTIFICATION; INDICATORS; ILLNESS
AB Quantitative polymerase chain reaction (qPCR) has become a frequently used technique for quantifying enterococci in recreational surface waters, but there are several methodological options. Here we evaluated how three method permutations, type of mastermix, sample extract dilution and use of controls in results calculation, affect method reliability among multiple laboratories with respect to sample interference. Multiple samples from each of 22 sites representing an array of habitat types were analyzed using EPA Method 1611 and 1609 reagents with full strength and five-fold diluted extracts. The presence of interference was assessed three ways: using sample processing and PCR amplifications controls; consistency of results across extract dilutions; and relative recovery of target genes from spiked enterococci in water sample compared to control matrices with acceptable recovery defined as 50 to 200%. Method 1609, which is based on an environmental mastermix, was found to be superior to Method 1611, which is based on a universal mastermix. Method 1611 had over a 40% control assay failure rate with undiluted extracts and a 6% failure rate with diluted extracts. Method 1609 failed in only 11% and 3% of undiluted and diluted extracts analyses. Use of sample processing control assay results in the delta-delta Ct method for calculating relative target gene recoveries increased the number of acceptable recovery results. Delta-delta tended to bias recoveries from apparent partially inhibitory samples on the high side which could help in avoiding potential underestimates of enterococci - an important consideration in a public health context. Control assay and delta-delta recovery results were largely consistent across the range of habitats sampled, and among laboratories. The methodological option that best balanced acceptable estimated target gene recoveries with method sensitivity and avoidance of underestimated enterococci densities was Method 1609 without extract dilution and using the delta-delta calculation method. The applicability of this method can be extended by the analysis of diluted extracts to sites where interference is indicated but, particularly in these instances, should be confirmed by augmenting the control assays with analyses for target gene recoveries from spiked target organisms. Published by Elsevier B.V.
C1 [Haugland, Richard A.; Siefring, Shawn; Varma, Manju; Oshima, Kevin H.] US EPA, Off Res & Dev, Natl Exposure Res Lab, Cincinnati, OH 45268 USA.
[Sivaganesan, Mano] US EPA, Off Res & Dev, Natl Risk Management Res Lab, Cincinnati, OH 45268 USA.
[Cao, Yiping; Raith, Meredith; Griffith, John; Weisberg, Stephen B.] Southern Calif Coastal Water Res Project Author, Costa Mesa, CA USA.
[Noble, Rachel T.; Blackwood, A. Denene] Univ North Carolina Chapel Hill, Inst Marine Sci, Morehead City, NC USA.
[Kinzelman, Julie; Anan'eva, Tamara] City Racine Hlth Dept, Racine, WI USA.
[Bushon, Rebecca N.; Stelzer, Erin A.] US Geol Survey, Columbus, OH USA.
[Harwood, Valarie J.; Gordon, Katrina V.] Univ S Florida, Dept Integrat Biol, Tampa, FL USA.
[Sinigalliano, Christopher] NOAA, Atlantic Oceanog & Meteorol Lab, Ocean Chem Div, Miami, FL 33149 USA.
RP Haugland, RA (reprint author), US EPA, Off Res & Dev, Natl Exposure Res Lab, Cincinnati, OH 45268 USA.
EM haugland.rich@epa.gov
RI Weisberg, Stephen/B-2477-2008; Sinigalliano, Christopher/A-8760-2014
OI Weisberg, Stephen/0000-0002-0655-9425; Sinigalliano,
Christopher/0000-0002-9942-238X
NR 32
TC 1
Z9 1
U1 2
U2 7
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0167-7012
EI 1872-8359
J9 J MICROBIOL METH
JI J. Microbiol. Methods
PD APR
PY 2016
VL 123
BP 114
EP 125
DI 10.1016/j.mimet.2016.01.017
PG 12
WC Biochemical Research Methods; Microbiology
SC Biochemistry & Molecular Biology; Microbiology
GA DI7BY
UT WOS:000373655300017
PM 26844886
ER
PT J
AU Bill, BD
Moore, SK
Hay, LR
Anderson, DM
Trainer, VL
AF Bill, Brian D.
Moore, Stephanie K.
Hay, Levi R.
Anderson, Donald M.
Trainer, Vera L.
TI Effects of temperature and salinity on the growth of Alexandrium
(Dinophyceae) isolates from the Salish Sea
SO JOURNAL OF PHYCOLOGY
LA English
DT Article
DE Alexandrium; growth rate; HAB; harmful algae; hindcast; Puget Sound;
salinity; Salish Sea; temperature
ID PARALYTIC SHELLFISH; PUGET-SOUND; GONYAULAX-TAMARENSIS; NARRAGANSETT
BAY; TOXICITY; ACCUMULATION; WASHINGTON; IRRADIANCE; PATTERNS; TOXINS
AB Toxin-producing blooms of dinoflagellates in the genus Alexandrium have plagued the inhabitants of the Salish Sea for centuries. Yet the environmental conditions that promote accelerated growth of this organism, a producer of paralytic shellfish toxins, is lacking. This study quantitatively determined the growth response of two Alexandrium isolates to a range of temperatures and salinities, factors that will strongly respond to future climate change scenarios. An empirical equation, derived from observed growth rates describing the temperature and salinity dependence of growth, was used to hindcast bloom risk. Hindcasting was achieved by comparing predicted growth rates, calculated from insitu temperature and salinity data from Quartermaster Harbor, with corresponding Alexandrium cell counts and shellfish toxin data. The greatest bloom risk, defined at >0.25d(-1), generally occurred from April through November annually; however, growth rates rarely fell below 0.10d(-1). Except for a few occasions, Alexandrium cells were only observed during the periods of highest bloom risk and paralytic shellfish toxins above the regulatory limit always fell within the periods of predicted bloom occurrence. While acknowledging that Alexandrium growth rates are affected by other abiotic and biotic factors, such as grazing pressure and nutrient availability, the use of this empirical growth function to predict higher risk time frames for blooms and toxic shellfish within the Salish Sea provides the groundwork for a more comprehensive biological model of Alexandrium bloom dynamics in the region and will enhance our ability to forecast blooms in the Salish Sea under future climate change scenarios.
C1 [Bill, Brian D.; Trainer, Vera L.] NW Fisheries Sci Ctr, Environm & Fisheries Sci Div, Marine Biotoxins Program, Seattle, WA USA.
[Moore, Stephanie K.] Univ Corp Atmospher Res, Joint Off Sci Support, Seattle, WA USA.
[Hay, Levi R.] Univ Washington, NW Fisheries Sci Ctr, Seattle, WA 98195 USA.
[Anderson, Donald M.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.
[Trainer, Vera L.] NW Fisheries Sci Ctr, Environm & Fisheries Sci Div, Marine Biotoxins Program, Seattle, WA USA.
RP Bill, BD (reprint author), NW Fisheries Sci Ctr, Environm & Fisheries Sci Div, Marine Biotoxins Program, Seattle, WA USA.
EM brian.d.bill@noaa.gov
FU NOAA Ecology and Oceanography of Harmful Algal Bloom (ECOHAB) Program;
Woods Hole Center for Oceans and Human Health, National Science
Foundation [OCE-1314642]; National Institute of Environmental Health
Sciences [1-P01-ES021923-01]
FX The authors thank K. Bright (American Gold Seafoods) and K. Rickerson
(SoundToxins program) for collecting the bloom water used for
Alexandrium isolation; J. A. Johnstone (Joint Institute for the Study of
the Atmosphere and Ocean) for modeling the growth responses; S. Brugger
for culture maintenance; and the Northwest Fisheries Science Center's
Pasco Research Station for building the temperature gradient bar. We
thank C. Greengrove and J. Masura (University of Washington Tacoma) for
providing in situ Quartermaster Harbor light data, K. Rickerson and the
SoundToxins partnership for Alexandrium cell counts, the King County
Department of Natural Resources and Parks for temperature and salinity
data and the Washington State Department of Health for shellfish
toxicity data. This research was supported in part by a grant from the
NOAA Ecology and Oceanography of Harmful Algal Bloom (ECOHAB) Program to
the NOAA Northwest Fisheries Science Center. Support for D. M. Anderson
was also provided through the NOAA Ecology and Oceanography of Harmful
Algal Bloom (ECOHAB) Program grant OCE-1314642 and National Institute of
Environmental Health Sciences grant 1-P01-ES021923-01. This is ECOHAB
publication number 808.
NR 35
TC 2
Z9 2
U1 7
U2 21
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0022-3646
EI 1529-8817
J9 J PHYCOL
JI J. Phycol.
PD APR
PY 2016
VL 52
IS 2
BP 230
EP 238
DI 10.1111/jpy.12386
PG 9
WC Plant Sciences; Marine & Freshwater Biology
SC Plant Sciences; Marine & Freshwater Biology
GA DI6OG
UT WOS:000373618400008
PM 27037588
ER
PT J
AU Saglamyurek, E
Puigibert, MG
Zhou, Q
Giner, L
Marsili, F
Verma, VB
Nam, SW
Oesterling, L
Nippa, D
Oblak, D
Tittel, W
AF Saglamyurek, Erhan
Puigibert, Marcelli Grimau
Zhou, Qiang
Giner, Lambert
Marsili, Francesco
Verma, Varun B.
Nam, Sae Woo
Oesterling, Lee
Nippa, David
Oblak, Daniel
Tittel, Wolfgang
TI A multiplexed light-matter interface for fibre-based quantum networks
SO NATURE COMMUNICATIONS
LA English
DT Article
ID MEMORY; STORAGE; PHOTONS
AB Processing and distributing quantum information using photons through fibre-optic or free-space links are essential for building future quantum networks. The scalability needed for such networks can be achieved by employing photonic quantum states that are multiplexed into time and/or frequency, and light-matter interfaces that are able to store and process such states with large time-bandwidth product and multimode capacities. Despite important progress in developing such devices, the demonstration of these capabilities using non-classical light remains challenging. Here, employing the atomic frequency comb quantum memory protocol in a cryogenically cooled erbium-doped optical fibre, we report the quantum storage of heralded single photons at a telecom-wavelength (1.53 mu m) with a time-bandwidth product approaching 800. Furthermore, we demonstrate frequency-multimode storage and memory-based spectral-temporal photon manipulation. Notably, our demonstrations rely on fully integrated quantum technologies operating at telecommunication wavelengths. With improved storage efficiency, our light-matter interface may become a useful tool in future quantum networks.
C1 [Saglamyurek, Erhan; Puigibert, Marcelli Grimau; Zhou, Qiang; Giner, Lambert; Oblak, Daniel; Tittel, Wolfgang] Univ Calgary, Inst Quantum Sci & Technol, 2500 Univ Dr NW, Calgary, AB T2N 1N4, Canada.
[Saglamyurek, Erhan; Puigibert, Marcelli Grimau; Zhou, Qiang; Giner, Lambert; Oblak, Daniel; Tittel, Wolfgang] Univ Calgary, Dept Phys & Astron, 2500 Univ Dr NW, Calgary, AB T2N 1N4, Canada.
[Marsili, Francesco] CALTECH, Jet Prop Lab, Div Appl Phys, 4800 Oak Grove Dr, Pasadena, CA 91109 USA.
[Verma, Varun B.; Nam, Sae Woo] NIST, Boulder, CO 80305 USA.
[Oesterling, Lee; Nippa, David] Battelle Mem Inst, 505 King Ave, Columbus, OH 43201 USA.
[Giner, Lambert] Univ Ottawa, Dept Phys, 150 Louis Pasteur, Ottawa, ON K1N 6N5, Canada.
RP Tittel, W (reprint author), Univ Calgary, Inst Quantum Sci & Technol, 2500 Univ Dr NW, Calgary, AB T2N 1N4, Canada.; Tittel, W (reprint author), Univ Calgary, Dept Phys & Astron, 2500 Univ Dr NW, Calgary, AB T2N 1N4, Canada.
EM wtittel@ucalgary.ca
RI Tittel, Wolfgang/A-1600-2011
FU Alberta Innovates Technology Futures; National Science and Engineering
Research Council of Canada; Canadian Institute for Advanced Research;
DARPA Information in a Photon (InPho) programme; National Aeronautics
and Space Administration
FX E.S., M.G., Q.Z., L.G., D.O. and W.T. thank Jeongwan Jin, Neil Sinclair,
Charles Thiel and Vladimir Kiselyov for discussions and technical
support, and acknowledge funding through the Alberta Innovates
Technology Futures and the National Science and Engineering Research
Council of Canada. Furthermore, W.T. acknowledges support as a Senior
Fellow of the Canadian Institute for Advanced Research, and V.B.V. and
S.W.N. partial funding for detector development from the DARPA
Information in a Photon (InPho) programme. Part of the research was
carried out at the Jet Propulsion Laboratory, California Institute of
Technology, under a contract with the National Aeronautics and Space
Administration. L.O. and D.N. acknowledge Srico Inc. for their
assistance with the fabrication of PPLN wafers.
NR 37
TC 1
Z9 1
U1 17
U2 30
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 2041-1723
J9 NAT COMMUN
JI Nat. Commun.
PD APR
PY 2016
VL 7
AR 11202
DI 10.1038/ncomms11202
PG 7
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DI6PK
UT WOS:000373621700001
PM 27046076
ER
PT J
AU Campbell, DL
Spielman, IB
AF Campbell, D. L.
Spielman, I. B.
TI Rashba realization: Raman with RF
SO NEW JOURNAL OF PHYSICS
LA English
DT Article
DE Rashba; spin-orbit; cold atoms; Bose-Einstein condensate; Floquet;
effective potential
ID OPTICAL LATTICES; PHASE; POTENTIALS; DYNAMICS
AB We theoretically explore a Rashba spin-orbit coupling scheme which operates entirely in the absolute ground state manifold of an alkali atom, thereby minimizing all inelastic processes. An energy gap between ground eigenstates of the proposed coupling can be continuously opened or closed by modifying laser polarizations. Our technique uses far-detuned 'Raman' laser coupling to create the Rashba potential, which has the benefit of low spontaneous emission rates. At these detunings, the Raman matrix elements that link m(F) magnetic sublevel quantum numbers separated by two are also suppressed. These matrix elements are necessary to produce the Rashba Hamiltonian within a single total angular momentum f manifold. However, the far-detuned Raman couplings can link the three XYZ states familiar to quantum chemistry, which possess the necessary connectivity to realize the Rashba potential. We show that these XYZ states are essentially the hyperfine spin eigenstates of Rb-87 dressed by a strong radio-frequency magnetic field.
C1 [Campbell, D. L.] Univ Maryland, Joint Quantum Inst, College Pk, MD 20742 USA.
NIST, College Pk, MD 20742 USA.
RP Campbell, DL (reprint author), Univ Maryland, Joint Quantum Inst, College Pk, MD 20742 USA.
EM dlcamp@mit.edu
FU ARO's atomtronics MURI; AFOSR's Quantum Matter MURI; NIST; NSF through
the PFC at the JQI
FX This work was partially supported by the ARO's atomtronics MURI, by the
AFOSR's Quantum Matter MURI, NIST, and the NSF through the PFC at the
JQI.
NR 33
TC 5
Z9 5
U1 5
U2 14
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 APR 1
PY 2016
VL 18
AR 033035
DI 10.1088/1367-2630/18/3/033035
PG 12
WC Physics, Multidisciplinary
SC Physics
GA DI8CE
UT WOS:000373727800001
ER
PT J
AU Ilicak, M
Drange, H
Wang, Q
Gerdes, R
Aksenov, Y
Bailey, D
Bentsen, M
Biastoch, A
Bozec, A
Boning, C
Cassou, C
Chassignet, E
Coward, AC
Curry, B
Danabasoglu, G
Danilov, S
Fernandez, E
Fogli, PG
Fujii, Y
Griffies, SM
Iovino, D
Jahn, A
Jung, T
Large, WG
Lee, C
Lique, C
Lu, JH
Masina, S
Nurser, AJG
Roth, C
Melia, DSY
Samuels, BL
Spence, P
Tsujino, H
Valcke, S
Voldoire, A
Wang, XZ
Yeager, SG
AF Ilicak, Mehmet
Drange, Helge
Wang, Qiang
Gerdes, Rudiger
Aksenov, Yevgeny
Bailey, David
Bentsen, Mats
Biastoch, Arne
Bozec, Alexandra
Boening, Claus
Cassou, Christophe
Chassignet, Eric
Coward, Andrew C.
Curry, Beth
Danabasoglu, Gokhan
Danilov, Sergey
Fernandez, Elodie
Fogli, Pier Giuseppe
Fujii, Yosuke
Griffies, Stephen M.
Iovino, Doroteaciro
Jahn, Alexandra
Jung, Thomas
Large, William G.
Lee, Craig
Lique, Camille
Lu, Jianhua
Masina, Simona
Nurser, A. J. George
Roth, Christina
Salas y Melia, David
Samuels, Bonita L.
Spence, Paul
Tsujino, Hiroyuki
Valcke, Sophie
Voldoire, Aurore
Wang, Xuezhu
Yeager, Steve G.
TI An assessment of the Arctic Ocean in a suite of interannual CORE-II
simulations. Part III: Hydrography and fluxes
SO OCEAN MODELLING
LA English
DT Article
DE Arctic Ocean; Atlantic Water; St. Anna Trough; Density currents; CORE-II
atmospheric forcing
ID NORTH-ATLANTIC SIMULATIONS; LIQUID FRESH-WATER; SEA-ICE; THERMOHALINE
CIRCULATION; SUBPOLAR GYRE; COLD WINTERS; MASSES; ADVECTION; WEATHER;
CLIMATOLOGY
AB In this paper we compare the simulated Arctic Ocean in 15 global ocean-sea ice models in the framework of the Coordinated Ocean-ice Reference Experiments, phase II (CORE-II). Most of these models are the ocean and sea-ice components of the coupled climate models used in the Coupled Model Intercomparison Project Phase 5 (CMIP5) experiments. We mainly focus on the hydrography of the Arctic interior, the state of Atlantic Water layer and heat and volume transports at the gateways of the Davis Strait, the Bering Strait, the Fram Strait and the Barents Sea Opening. We found that there is a large spread in temperature in the Arctic Ocean between the models, and generally large differences compared to the observed temperature at intermediate depths. Warm bias models have a strong temperature anomaly of inflow of the Atlantic Water entering the Arctic Ocean through the Fram Strait. Another process that is not represented accurately in the CORE-II models is the formation of cold and dense water, originating on the eastern shelves. In the cold bias models, excessive cold water forms in the Barents Sea and spreads into the Arctic Ocean through the St. Anna Through. There is a large spread in the simulated mean heat and volume transports through the Fram Strait and the Barents Sea Opening. The models agree more on the decadal variability, to a large degree dictated by the common atmospheric forcing. We conclude that the CORE-II model study helps us to understand the crucial biases in the Arctic Ocean. The current coarse resolution state-of-the-art ocean models need to be improved in accurate representation of the Atlantic Water inflow into the Arctic and density currents coming from the shelves. (C) 2016 The Authors. Published by Elsevier Ltd.
C1 [Ilicak, Mehmet; Bentsen, Mats] Bjerknes Ctr Climate Res, Uni Res Climate, Bergen, Norway.
[Drange, Helge] Univ Bergen, Inst Geophys, Bergen, Norway.
[Drange, Helge] Bjerknes Ctr Climate Res, Bergen, Norway.
[Wang, Qiang; Gerdes, Rudiger; Danilov, Sergey; Jung, Thomas; Wang, Xuezhu] Helmholtz Ctr Polar & Marine Res AWI, Alfred Wegener Inst, Bremerhaven, Germany.
[Aksenov, Yevgeny; Coward, Andrew C.; Nurser, A. J. George] NOC, Southampton SO14 3ZH, Hants, England.
[Bailey, David; Danabasoglu, Gokhan; Jahn, Alexandra; Large, William G.; Yeager, Steve G.] NCAR, Boulder, CO USA.
[Biastoch, Arne; Boening, Claus; Roth, Christina] GEOMAR Helmholtz Ctr Ocean Res, Kiel, Germany.
[Bozec, Alexandra; Chassignet, Eric; Lu, Jianhua] Florida State Univ, COAPS, Tallahassee, FL 32306 USA.
[Cassou, Christophe; Fernandez, Elodie; Valcke, Sophie] CNRS, Ctr Europeen Rech & Format Avancee Calcul Sci, Unite Rech Associee 1875, Toulouse, France.
[Curry, Beth; Lee, Craig] Univ Washington, Appl Phys Lab, Seattle, WA 98105 USA.
[Fogli, Pier Giuseppe; Iovino, Doroteaciro; Masina, Simona] Ctr Euromediterraneo Cambiamenti Climatici CMCC, Bologna, Italy.
[Fujii, Yosuke; Tsujino, Hiroyuki] Japan Meteorol Agcy, MRI, Tsukuba, Ibaraki, Japan.
[Griffies, Stephen M.; Samuels, Bonita L.] NOAA, GFDL, Princeton, NJ USA.
[Lique, Camille] Univ Oxford, Dept Earth Sci, Oxford OX1 3PR, England.
[Salas y Melia, David; Voldoire, Aurore] CNRM, Toulouse, France.
[Spence, Paul] Univ New S Wales, ARC Ctr Excellence Climate Syst Sci, Sydney, NSW, Australia.
[Spence, Paul] Univ New S Wales, Climate Change Res Ctr, Sydney, NSW, Australia.
[Masina, Simona] INGV, Bologna, Italy.
[Jahn, Alexandra] Univ Colorado, Inst Arctic & Alpine Res, Dept Atmopher & Ocean Sci, Boulder, CO 80309 USA.
IFREMER, Lab Phys Oceans, Brest, France.
RP Ilicak, M (reprint author), Bjerknes Ctr Climate Res, Uni Res Climate, Bergen, Norway.
EM mehmet.ilicak@noaa.gov
RI Lique, Camille/L-5543-2015; Jung, Thomas/J-5239-2012; Fogli, Pier
Giuseppe/E-9486-2015; Jahn, Alexandra/C-6545-2008; Boening,
Claus/B-1686-2012; Danilov, Sergey/S-6184-2016
OI Lique, Camille/0000-0002-8357-4928; Jung, Thomas/0000-0002-2651-1293;
Fogli, Pier Giuseppe/0000-0001-7997-6273; Jahn,
Alexandra/0000-0002-6580-2579; Boening, Claus/0000-0002-6251-5777;
FU European Research Council under the European Community's Seventh
Framework Programme [610055]; Research Council of Norway through the
project EVA [229771, nn2345k, ns2345k]; international CLIVAR; U.S.
CLIVAR project offices; Research Council of Norway through the EarthClim
[207711/E10]; NO-TUR/NorStore projects; Centre for Climate Dynamics at
the Bjerknes Centre for Climate Research; Helmholtz Climate Initiative
REKLIM (Regional Climate Change) project; Italian Ministry of Education;
Italian Ministry of Environment, Land, and Sea under the GEMINA project;
U.S. National Science Foundation (NSF); NOAA Climate Program Office
under Climate Variability and Predictability Program [NA09OAR4310163,
NA13OAR4310138]; NSF Collaborative Research EaSM2 grant [OCE-1243015];
"RACE-Regional Atlantic Circulation and Global Change" - German Federal
Ministry for Education and Research (BMBF) [03F0651B]; UK Natural
Environment Research Council (NERC) Marine Centres - Strategic Research
Programme; Arctic Research Programme TEA-COSI project [NE/I028947/1];
National Science Foundation Office of Polar Programs [PLR-1313614,
PLR-1203720]; Australian Research Council grant [DE150100223]
FX M. Ilicak is supported by Ice2Ice project that has received funding from
the European Research Council under the European Community's Seventh
Framework Programme (FP7/2007-2013)/ERC grant agreement no. 610055.; M.
Bentsen, H. Drange and M. Ilicak acknowledge support from the Research
Council of Norway through the project EVA (grants 229771, nn2345k,
ns2345k).; The WCRP/CLIVAR Ocean Model Development Panel (OMDP) is
responsible for organizing the Coordinated Ocean-sea ice Reference
Experiments, with support from the international CLIVAR and U.S. CLIVAR
project offices. We are grateful for the efforts of modelers who have
contributed to the simulation and processing of the CORE-II
experiments.; The BERGEN contribution is supported by the Research
Council of Norway through the EarthClim (207711/E10) and NO-TUR/NorStore
projects, as well as the Centre for Climate Dynamics at the Bjerknes
Centre for Climate Research.; AWI is a member of the Helmholtz
Association of German Research Centers. Q. Wang is funded by the
Helmholtz Climate Initiative REKLIM (Regional Climate Change) project.;
The CMCC contribution received funding from the Italian Ministry of
Education, University, and Research and the Italian Ministry of
Environment, Land, and Sea under the GEMINA project.; NCAR is sponsored
by the U.S. National Science Foundation (NSF). S.G. Yeager was supported
by the NOAA Climate Program Office under Climate Variability and
Predictability Program grants NA09OAR4310163 and NA13OAR4310138 and by
the NSF Collaborative Research EaSM2 grant OCE-1243015 to NCAR.; The
GEOMAR experiments were performed at the North-German Supercomputing
Alliance (HLRN). C. Roth was supported by the Co-Operative Project
"RACE-Regional Atlantic Circulation and Global Change" funded by the
German Federal Ministry for Education and Research (BMBF), grant no.
03F0651B.; The NOC contribution was partly supported by the UK Natural
Environment Research Council (NERC) Marine Centres - Strategic Research
Programme and partly by the Arctic Research Programme TEA-COSI project
(NE/I028947/1). We also acknowledge the annual meetings of the Forum for
Arctic Modeling and Observing Synthesis (FAMOS), funded by the National
Science Foundation Office of Polar Programs, awards PLR-1313614 and
PLR-1203720 being instrumental in conceiving ideas and in inspiring the
present study and are thankful to FAMOS for travel support to attend
these meetings. The NOC-ORCA simulations were performed using the NOC
local computing facilities and the cluster MOBILIS.; P. Spence is
supported by the Australian Research Council grant DE150100223.
NR 77
TC 6
Z9 6
U1 7
U2 18
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 1463-5003
EI 1463-5011
J9 OCEAN MODEL
JI Ocean Model.
PD APR
PY 2016
VL 100
BP 141
EP 161
DI 10.1016/j.ocemod.2016.02.004
PG 21
WC Meteorology & Atmospheric Sciences; Oceanography
SC Meteorology & Atmospheric Sciences; Oceanography
GA DI8BN
UT WOS:000373726000010
ER
PT J
AU Long, DA
Fleisher, AJ
Liu, Q
Hodges, JT
AF Long, D. A.
Fleisher, A. J.
Liu, Q.
Hodges, J. T.
TI Ultra-sensitive cavity ring-down spectroscopy in the mid-infrared
spectral region
SO OPTICS LETTERS
LA English
DT Article
ID LASER; STABILIZATION; SPECTROMETER
AB We describe an ultra-sensitive cavity ring-down spectrometer which operates in the mid-infrared spectral region near 4.5 mu m. With this instrument a noise-equivalent absorption coefficient of 2.6 x 10(-11) cm(-1) Hz(-1/2) was demonstrated with less than 150 nW of optical power incident on the photodetector. Quantum noise was observed in the individual ring-down decay events, leading to quantum-noise-limited short-time performance. We believe that this spectrometer's combination of high sensitivity and robustness make it well suited for measurements of ultra-trace gas species as well as applications in optics and fundamental physics.
C1 [Long, D. A.; Fleisher, A. J.; Liu, Q.; Hodges, J. T.] NIST, Mat Measurement Lab, Gaithersburg, MD 20899 USA.
RP Long, DA (reprint author), NIST, Mat Measurement Lab, Gaithersburg, MD 20899 USA.
EM david.long@nist.gov; adam.fleisher@nist.gov
RI Fleisher, Adam/A-4215-2012
OI Fleisher, Adam/0000-0001-9216-0607
FU National Institute of Standards and Technology (NIST)
FX National Institute of Standards and Technology (NIST) (Greenhouse Gas
Measurements and Climate Research, Innovation in Measurement Science
Grant).
NR 23
TC 1
Z9 1
U1 10
U2 25
PU OPTICAL SOC AMER
PI WASHINGTON
PA 2010 MASSACHUSETTS AVE NW, WASHINGTON, DC 20036 USA
SN 0146-9592
EI 1539-4794
J9 OPT LETT
JI Opt. Lett.
PD APR 1
PY 2016
VL 41
IS 7
BP 1612
EP 1615
DI 10.1364/OL.41.001612
PG 4
WC Optics
SC Optics
GA DI0ZI
UT WOS:000373225400078
PM 27192300
ER
PT J
AU Panthi, J
Aryal, S
Dahal, P
Bhandari, P
Krakauer, NY
Pandey, VP
AF Panthi, Jeeban
Aryal, Suman
Dahal, Piyush
Bhandari, Parashuram
Krakauer, Nir Y.
Pandey, Vishnu Prasad
TI Livelihood vulnerability approach to assessing climate change impacts on
mixed agro-livestock smallholders around the Gandaki River Basin in
Nepal
SO REGIONAL ENVIRONMENTAL CHANGE
LA English
DT Article
DE Climate change; Mixed agro-livestock; Nepal; Smallholders; Vulnerability
ID COMMUNITIES; ADAPTATION; VARIABILITY; ASSESSMENTS; FRAMEWORK; RAINFALL;
HIMALAYA; SYSTEMS; FLOODS
AB Climate change vulnerability depends upon various factors and differs between places, sectors and communities. People in developing countries whose subsistence livelihood depends mainly upon agriculture and livestock production are identified as particularly vulnerable. Nepal, where the majority of people are in a mixed agro-livestock system, is identified as the world's fourth most vulnerable country to climate change. However, there is limited knowledge on how vulnerable mixed agro-livestock smallholders are and how their vulnerability differs across different ecological regions in Nepal. This study aims to test two vulnerability assessment indices, livelihood vulnerability index and IPCC vulnerability index, around the Gandaki River Basin of central Nepal. A total of 543 households practicing mixed agro-livestock were surveyed from three districts, namely Dhading, Syangja and Kapilvastu representing three major ecological zones: mountain, mid-hill and Terai (lowland). Data on socio-demographics, livelihood determinants, social networks, health, food and water security, natural disasters and climate variability were collected and combined into the indices. Both indices differed for mixed agro-livestock smallholders across the three districts, with Dhading scoring as the most vulnerable and Syangja the least. Substantial variation across the districts was observed in components, sub-components and three dimensions (exposure, sensitivity and adaptive capacity) of vulnerability. The findings help in designing site-specific intervention strategies to reduce vulnerability of mixed agro-livestock smallholders to climate change.
C1 [Panthi, Jeeban; Dahal, Piyush] Small Earth Nepal, 626 Bhakti Thapa Sadak,POB 20533, Kathmandu, Nepal.
[Aryal, Suman] Univ So Queensland, Int Ctr Appl Climate Sci, Toowoomba, Qld 4350, Australia.
[Aryal, Suman] Univ So Queensland, Fac Business Educ Law & Arts, Toowoomba, Qld 4350, Australia.
[Bhandari, Parashuram] Tribhuvan Univ, Cent Dept Environm Sci, Kathmandu, Nepal.
[Krakauer, Nir Y.] CUNY City Coll, Dept Civil Engn, New York, NY 10031 USA.
[Krakauer, Nir Y.] CUNY City Coll, NOAA CREST, New York, NY 10031 USA.
[Pandey, Vishnu Prasad] Asian Inst Technol & Management, POB 25, Lalitpur Patan 44700, Spain.
[Pandey, Vishnu Prasad] Asian Inst Technol, POB 4, Klongluang 12120, Pathumthani, Thailand.
RP Panthi, J (reprint author), Small Earth Nepal, 626 Bhakti Thapa Sadak,POB 20533, Kathmandu, Nepal.
EM panthijeeban@gmail.com; aaryalsuman@gmail.com; Piyush.dahal@gmail.com;
Parashu.bhandari@gmail.com; nkrakauer@ccny.cuny.edu;
vishnu.pandey@gmail.com
FU USAID Feed the Future Innovation Lab for Collaborative Research on
Adapting Livestock Systems to Climate Change at Colorado State
University [9650-32]
FX Department of Hydrology and Meteorology (DHM), the government of Nepal
and the UNISDR are highly acknowledged for providing the observed
meteorological data and natural disaster events, respectively. Field
enumerators from The Small Earth Nepal (SEN) and Tribhuvan University
are thanked. This work is part of a collaborative research project
supported by the USAID Feed the Future Innovation Lab for Collaborative
Research on Adapting Livestock Systems to Climate Change at Colorado
State University under sub-award 9650-32. All statements made are the
views of the authors and not the opinions of the funders or the US
government.
NR 63
TC 3
Z9 3
U1 8
U2 26
PU SPRINGER HEIDELBERG
PI HEIDELBERG
PA TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY
SN 1436-3798
EI 1436-378X
J9 REG ENVIRON CHANGE
JI Reg. Envir. Chang.
PD APR
PY 2016
VL 16
IS 4
BP 1121
EP 1132
DI 10.1007/s10113-015-0833-y
PG 12
WC Environmental Sciences; Environmental Studies
SC Environmental Sciences & Ecology
GA DI2FH
UT WOS:000373310600017
ER
PT J
AU Hicks, CC
Levine, A
Agrawal, A
Basurto, X
Breslow, SJ
Carothers, C
Charnley, S
Coulthard, S
Dolsak, N
Donatuto, J
Garcia-Quijano, C
Mascia, MB
Norman, K
Poe, MR
Satterfield, T
Martin, KS
Levin, PS
AF Hicks, Christina C.
Levine, Arielle
Agrawal, Arun
Basurto, Xavier
Breslow, Sara J.
Carothers, Courtney
Charnley, Susan
Coulthard, Sarah
Dolsak, Nives
Donatuto, Jamie
Garcia-Quijano, Carlos
Mascia, Michael B.
Norman, Karma
Poe, Melissa R.
Satterfield, Terre
Martin, Kevin St.
Levin, Phillip S.
TI Engage key social concepts for sustainability
SO SCIENCE
LA English
DT Editorial Material
C1 [Hicks, Christina C.] Stanford Univ, Ctr Ocean Solut, Stanford, CA 94305 USA.
[Hicks, Christina C.] James Cook Univ, Australian Res Council Ctr Excellence Coral Reef, Sydney, NSW, Australia.
[Hicks, Christina C.] Univ Lancaster, Lancaster Environm Ctr, Lancaster LA1 4YW, England.
[Levine, Arielle] San Diego State Univ, Geog, San Diego, CA 92182 USA.
[Agrawal, Arun] Univ Michigan, Sch Nat Resources & Environm, Ann Arbor, MI 48109 USA.
[Basurto, Xavier] Duke Univ, Nicholas Sch Environm, Durham, NC 27706 USA.
[Breslow, Sara J.; Norman, Karma; Poe, Melissa R.; Levin, Phillip S.] NOAA, Northwest Fisheries Sci Ctr, Tacoma, WA USA.
[Carothers, Courtney] Univ Alaska Fairbanks, Sch Fisheries & Ocean Sci, Fairbanks, AK USA.
[Charnley, Susan] US Forest Serv, USDA, Washington, DC USA.
[Coulthard, Sarah] Northumbria Univ, Newcastle Upon Tyne NE1 8ST, Tyne & Wear, England.
[Dolsak, Nives] Univ Washington, Sch Marine & Environm airs, Seattle, WA 98195 USA.
[Donatuto, Jamie] Swinomish Indian Tribal Community, Tacoma, WA USA.
[Garcia-Quijano, Carlos] Univ Rhode Isl, Anthropol & Marine Affairs, Kingston, RI 02881 USA.
[Mascia, Michael B.] Conservat Int, Moore Ctr Sci, Arlington, VA USA.
[Poe, Melissa R.] Univ Washington, Washington Sea Grant, Seattle, WA 98195 USA.
[Satterfield, Terre] Univ British Columbia, Inst Resources Environm & Sustainabil, Vancouver, BC V5Z 1M9, Canada.
[Martin, Kevin St.] Rutgers State Univ, Dept Geog, Piscataway, NJ 08855 USA.
RP Hicks, CC (reprint author), Stanford Univ, Ctr Ocean Solut, Stanford, CA 94305 USA.; Hicks, CC (reprint author), James Cook Univ, Australian Res Council Ctr Excellence Coral Reef, Sydney, NSW, Australia.; Hicks, CC (reprint author), Univ Lancaster, Lancaster Environm Ctr, Lancaster LA1 4YW, England.
EM christina.hicks@lancaster.ac.uk
OI Hicks, Christina/0000-0002-7399-4603
NR 15
TC 11
Z9 11
U1 13
U2 33
PU AMER ASSOC ADVANCEMENT SCIENCE
PI WASHINGTON
PA 1200 NEW YORK AVE, NW, WASHINGTON, DC 20005 USA
SN 0036-8075
EI 1095-9203
J9 SCIENCE
JI Science
PD APR 1
PY 2016
VL 352
IS 6281
BP 38
EP 40
PG 3
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DH8JP
UT WOS:000373039600023
PM 27034361
ER
PT J
AU Schaefer, H
Fletcher, SEM
Veidt, C
Lassey, KR
Brailsford, GW
Bromley, TM
Dlugokencky, EJ
Michel, SE
Miller, JB
Levin, I
Lowe, DC
Martin, RJ
Vaughn, BH
White, JWC
AF Schaefer, Hinrich
Fletcher, Sara E. Mikaloff
Veidt, Cordelia
Lassey, Keith R.
Brailsford, Gordon W.
Bromley, Tony M.
Dlugokencky, Edward J.
Michel, Sylvia E.
Miller, John B.
Levin, Ingeborg
Lowe, Dave C.
Martin, Ross J.
Vaughn, Bruce H.
White, James W. C.
TI A 21st-century shift from fossil-fuel to biogenic methane emissions
indicated by (CH4)-C-13
SO SCIENCE
LA English
DT Article
ID ATMOSPHERIC METHANE; INTERANNUAL VARIABILITY; MIXING-RATIO; BUDGET;
ATTRIBUTION; HYDROXYL; DECADES; TREND; SINKS; STATE
AB Between 1999 and 2006, a plateau interrupted the otherwise continuous increase of atmospheric methane concentration [CH4] since preindustrial times. Causes could be sink variability or a temporary reduction in industrial or climate-sensitive sources. We reconstructed the global history of [CH4] and its stable carbon isotopes from ice cores, archived air, and a global network of monitoring stations. A box-model analysis suggests that diminishing thermogenic emissions, probably from the fossil-fuel industry, and/or variations in the hydroxyl CH4 sink caused the [CH4] plateau. Thermogenic emissions did not resume to cause the renewed [CH4] rise after 2006, which contradicts emission inventories. Post-2006 source increases are predominantly biogenic, outside the Arctic, and arguably more consistent with agriculture than wetlands. If so, mitigating CH4 emissions must be balanced with the need for food production.
C1 [Schaefer, Hinrich; Fletcher, Sara E. Mikaloff; Lassey, Keith R.; Brailsford, Gordon W.; Bromley, Tony M.; Lowe, Dave C.; Martin, Ross J.] Natl Inst Water & Atmospher Res NIWA, Climate & Atmosphere Ctr, 301 Evans Bay Parade, Wellington 6021, New Zealand.
[Veidt, Cordelia; Levin, Ingeborg] Heidelberg Univ, Inst Umweltphys, Neuenheimer Feld 229, D-69120 Heidelberg, Germany.
[Dlugokencky, Edward J.; Miller, John B.] NOAA, ESRL, Global Monitoring Div, 325 Broadway, Boulder, CO 80305 USA.
[Michel, Sylvia E.; Vaughn, Bruce H.; White, James W. C.] Univ Colorado, Inst Arctic & Alpine Res INSTAAR, Boulder, CO 80309 USA.
[Lassey, Keith R.] Lassey Res & Educ, 4 Witako St, Lower Hutt 5011, New Zealand.
[Lowe, Dave C.] LoweNZ, 31 Queen St, Lower Hutt 5012, New Zealand.
RP Schaefer, H (reprint author), Natl Inst Water & Atmospher Res NIWA, Climate & Atmosphere Ctr, 301 Evans Bay Parade, Wellington 6021, New Zealand.
EM hinrich.schaefer@niwa.co.nz
RI White, James/A-7845-2009
OI White, James/0000-0001-6041-4684
FU Marsden Fund Council from New Zealand Government; NIWA under Climate and
Atmosphere Research Programme [CAAC1504 (2014/15 SCI)]
FX We thank S. Montzka for supplying OH-reconstruction data. M. Harvey and
K. Steinkamp provided helpful discussions. Feedback from two anonymous
reviewers improved the manuscript. Antarctica NZ supports air sampling
at Arrival Heights, Antarctica (ARH). Raw data for individual stations
measured by INSTAAR and NIWA are available from the World Data Centre
for Greenhouse Gases
http://ds.data.jma.go.jp/gmd/wdcgg/introduction.html; data from INSTAAR
are also available from ftp://aftp.cmdl.noaa.gov/data/trace_gases. Data
from Heidelberg University are available from
http://www.iup.uni-heidelberg.de/institut/forschung/groups/kk/en/Data_ht
ml. Data measured by University of Washington and University of
California, Irvine, were taken from http://cdiac.ornl.gov/ndps/quay.html
and http://cdiac.ornl.gov/epubs/db/db1022/db1022.html, respectively.
Yearly delta13 C values for individual stations and global
annual averages are presented in tables S3 and S4. This research was
supported by the Marsden Fund Council from New Zealand Government
funding, administered by the Royal Society of New Zealand. Further
support came from NIWA under Climate and Atmosphere Research Programme
CAAC1504 (2014/15 SCI). The authors declare no competing interests. H.
S. designed the data analysis; G. W. B., T. M. B., R. J. M., J. B. M.,
D. C. L., B. H. V., C. V., and S. E. M. performed delta13C
measurements; C. V., J. B. M., I. L., D. C. L., and J. W. C. W. designed
sampling and analytical programmes and performed data quality control;
E. J. D. provided [CH4] data; K. R. L. and H. S. designed the
box model; S. E. M. F. and H. S. performed uncertainty analyses; and all
authors contributed to the interpretation and the writing of the
manuscript.
NR 32
TC 21
Z9 21
U1 33
U2 65
PU AMER ASSOC ADVANCEMENT SCIENCE
PI WASHINGTON
PA 1200 NEW YORK AVE, NW, WASHINGTON, DC 20005 USA
SN 0036-8075
EI 1095-9203
J9 SCIENCE
JI Science
PD APR 1
PY 2016
VL 352
IS 6281
BP 80
EP 84
DI 10.1126/science.aad2705
PG 5
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DH8JP
UT WOS:000373039600039
PM 26966190
ER
PT J
AU Nielsen, AAK
Der, BS
Shin, J
Vaidyanathan, P
Paralanov, V
Strychalski, EA
Ross, D
Densmore, D
Voigt, CA
AF Nielsen, Alec A. K.
Der, Bryan S.
Shin, Jonghyeon
Vaidyanathan, Prashant
Paralanov, Vanya
Strychalski, Elizabeth A.
Ross, David
Densmore, Douglas
Voigt, Christopher A.
TI Genetic circuit design automation
SO SCIENCE
LA English
DT Article
ID SYNTHETIC BIOLOGY; ESCHERICHIA-COLI; LOGIC GATES; COMPUTATIONAL DESIGN;
REGULATORY NETWORKS; LIVING CELLS; TRANSCRIPTION; EXPRESSION; SYSTEM;
PARTS
AB Computation can be performed in living cells by DNA-encoded circuits that process sensory information and control biological functions. Their construction is time-intensive, requiring manual part assembly and balancing of regulator expression. We describe a design environment, Cello, in which a user writes Verilog code that is automatically transformed into a DNA sequence. Algorithms build a circuit diagram, assign and connect gates, and simulate performance. Reliable circuit design requires the insulation of gates from genetic context, so that they function identically when used in different circuits. We used Cello to design 60 circuits for Escherichia coli (880,000 base pairs of DNA), for which each DNA sequence was built as predicted by the software with no additional tuning. Of these, 45 circuits performed correctly in every output state (up to 10 regulators and 55 parts), and across all circuits 92% of the output states functioned as predicted. Design automation simplifies the incorporation of genetic circuits into biotechnology projects that require decision-making, control, sensing, or spatial organization.
C1 [Nielsen, Alec A. K.; Der, Bryan S.; Shin, Jonghyeon; Voigt, Christopher A.] MIT, Dept Biol Engn, Synthet Biol Ctr, 77 Massachusetts Ave, Cambridge, MA 02139 USA.
[Der, Bryan S.; Vaidyanathan, Prashant; Densmore, Douglas] Boston Univ, Dept Biomed Engn, Biol Design Ctr, Dept Elect & Comp Engn, Boston, MA 02215 USA.
[Paralanov, Vanya; Strychalski, Elizabeth A.; Ross, David] NIST, Biosyst & Biomat Div, Mat Measurement Lab, Gaithersburg, MD 20817 USA.
RP Voigt, CA (reprint author), MIT, Dept Biol Engn, Synthet Biol Ctr, 77 Massachusetts Ave, Cambridge, MA 02139 USA.
EM cavoigt@gmail.com
FU Office of Naval Research, Multidisciplinary University Research
Initiative [N00014-13-1-0074]; Siebel Scholarship; Air Force Office of
Scientific Research; National Defense Science and Engineering Graduate
fellowship [FA9550-11-C-0028]; National Institute of General Medical
Sciences [P50 GMO98792]; NSF Synthetic Biology Engineering Research
Center [SynBERC EEC0540879]; NSF [1147158]; NIST Strategic and Emerging
Research Initiative; National Research Council postdoctoral program; AWS
in Education Grant; Thermo Fischer (Life Technologies) [A114510]
FX All data described in this paper are presented in the supplementary
materials. Cello can be accessed at www.cellocad.org; the code is open
source and maintained via the Nona Research Foundation
(www.nonasoftware.org). The insulated gates, circuits, and plasmids
defined in the UCF can be obtained via Addgene (www.addgene.org). The E.
coli strain used in this UCF is available from New England Biolabs
(C3019). D.D. is president and part owner of Lattice Automation, which
works on software for synthetic biology. Supported by Office of Naval
Research, Multidisciplinary University Research Initiative grant
N00014-13-1-0074 (C.A.V. and A.A.K.N.); a Siebel Scholarship (Class of
2015) and Air Force Office of Scientific Research, National Defense
Science and Engineering Graduate fellowship FA9550-11-C-0028 (A.A.K.N.);
National Institute of General Medical Sciences grant P50 GMO98792 and
NSF Synthetic Biology Engineering Research Center grant SynBERC
EEC0540879 (C.A.V. and J.S.); NSF grant 1147158 (D.D. and P.V.); the
NIST Strategic and Emerging Research Initiative (V.P., E.A.S., and
D.R.); the National Research Council postdoctoral program (V.P.); an AWS
in Education Grant; and Thermo Fischer (Life Technologies, A114510). We
thank S. Bhatia (Boston University) for his work to enumerate the
three-input, one-output logic motifs; R. Ghamari (Boston University) for
early work on the Cello software foundation and design approach; N.
Roehner for technical assistance with SBOL; and E. Oberortner for
technical assistance with Eugene. The National Institute of Standards
and Technology notes that certain commercial equipment, instruments, and
materials are identified in this paper to specify an experimental
procedure as completely as possible. In no case does the identification
of particular equipment or materials imply a recommendation or
endorsement by NIST, nor does it imply that the materials, instruments,
or equipment are necessarily the best available for the purpose. The
University of California, San Francisco, holds a patent application
associated with this work (US20130005590 A1). The set of insulated
gates, the plasmid backbones for the circuit and output plasmids (Fig.
1), and the standard RPU plasmid are available via Addgene
(www.addgene.org/Christopher_Voigt/). Cello can be accessed as a
web-based application (www.cellocad.org), the code for which will be
open source and provided on Github (https://github.com/CIDARLAB/cello).
NR 98
TC 37
Z9 37
U1 48
U2 103
PU AMER ASSOC ADVANCEMENT SCIENCE
PI WASHINGTON
PA 1200 NEW YORK AVE, NW, WASHINGTON, DC 20005 USA
SN 0036-8075
EI 1095-9203
J9 SCIENCE
JI Science
PD APR 1
PY 2016
VL 352
IS 6281
AR aac7341
DI 10.1126/science.aac7341
PG 11
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DH8JP
UT WOS:000373039600032
PM 27034378
ER
PT J
AU Friedman, LH
Vaudin, MD
Stranick, SJ
Stan, G
Gerbig, YB
Osborn, W
Cook, RF
AF Friedman, Lawrence H.
Vaudin, Mark D.
Stranick, Stephan J.
Stan, Gheorghe
Gerbig, Yvonne B.
Osborn, William
Cook, Robert F.
TI Assessing strain mapping by electron backscatter diffraction and
confocal Raman microscopy using wedge-indented Si
SO ULTRAMICROSCOPY
LA English
DT Article
DE EBSD; AFM; Confocal Raman Microscopy; FEA; Indentation; Strain
ID MONO-CRYSTALLINE SILICON; PHASE-TRANSFORMATIONS; HIGH-RESOLUTION; STRESS
MEASUREMENTS; NANO-INDENTATION; ELASTIC STRAINS; SIMULATION;
SPECTROSCOPY; NANOINDENTATION; MECHANICS
AB The accuracy of electron backscatter diffraction (EBSD) and confocal Raman microscopy (CRM) for smallscale strain mapping are assessed using the multi-axial strain field surrounding a wedge indentation in Si as a test vehicle. The strain field is modeled using finite element analysis (FEA) that is adapted to the near-indentation surface profile measured by atomic force microscopy (AFM). The assessment consists of (1) direct experimental comparisons of strain and deformation and (2) comparisons in which the modeled strain field is used as an intermediate step. Direct experimental methods (1) consist of comparisons of surface elevation and gradient measured by AFM and EBSD and of Raman shifts measured and predicted by CRM and EBSD, respectively. Comparisons that utilize the combined FEA-AFM model (2) consist of predictions of distortion, strain, and rotation for comparison with EBSD measurements and predictions of Raman shift for comparison with CRM measurements. For both EBSD and CRM, convolution of measurements in depth-varying strain fields is considered. The interconnected comparisons suggest that EBSD was able to provide an accurate assessment of the wedge indentation deformation field to within the precision of the measurements, approximately 2 x 10(-4) in strain. CRM was similarly precise, but was limited in accuracy to several times this value. Published by Elsevier B.V.
C1 [Friedman, Lawrence H.; Vaudin, Mark D.; Stranick, Stephan J.; Stan, Gheorghe; Gerbig, Yvonne B.; Osborn, William; Cook, Robert F.] NIST, Mat Measurement Sci Div, Gaithersburg, MD 20899 USA.
RP Cook, RF (reprint author), NIST, Mat Measurement Sci Div, Gaithersburg, MD 20899 USA.
EM robert.cook@nist.gov
RI Friedman, Lawrence/G-5650-2011
OI Friedman, Lawrence/0000-0003-2416-9903
FU Intramural NIST DOC [9999-NIST]
NR 52
TC 2
Z9 2
U1 5
U2 22
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0304-3991
EI 1879-2723
J9 ULTRAMICROSCOPY
JI Ultramicroscopy
PD APR
PY 2016
VL 163
BP 75
EP 86
DI 10.1016/j.ultramic.2016.02.001
PG 12
WC Microscopy
SC Microscopy
GA DI5GE
UT WOS:000373526100009
PM 26939030
ER
PT J
AU Obuchowski, NA
Buckler, A
Kinahan, P
-Mayer, HC
Petrick, N
Barboriak, DP
Bullen, J
Barnhart, H
Sullivan, DC
AF Obuchowski, Nancy A.
Buckler, Andrew
Kinahan, Paul
-Mayer, Heather Chen
Petrick, Nicholas
Barboriak, Daniel P.
Bullen, Jennifer
Barnhart, Huiman
Sullivan, Daniel C.
TI Statistical Issues in Testing Conformance with the Quantitative Imaging
Biomarker Alliance (QIBA) Profile Claims
SO ACADEMIC RADIOLOGY
LA English
DT Article
DE QIBA; quantitative imaging biomarker; precision; repeatability; bias;
total deviation index; linearity
ID TECHNICAL PERFORMANCE
AB A major initiative of the Quantitative Imaging Biomarker Alliance is to develop standards-based documents called "Profiles," which describe one or more technical performance claims for a given imaging modality. The term "actor" denotes any entity (device, software, or person) whose performance must meet certain specifications for the claim to be met. The objective of this paper is to present the statistical issues in testing actors' conformance with the specifications. In particular, we present the general rationale and interpretation of the claims, the minimum requirements for testing whether an actor achieves the performance requirements, the study designs used for testing conformity, and the statistical analysis plan. We use three examples to illustrate the process: apparent diffusion coefficient in solid tumors measured by MRI, change in Perc 15 as a biomarker for the progression of emphysema, and percent change in solid tumor volume by computed tomography as a biomarker for lung cancer progression.
C1 [Obuchowski, Nancy A.; Bullen, Jennifer] Cleveland Clin Fdn, Quantitat Hlth Sci, 9500 Euclid Ave, Cleveland, OH 44195 USA.
[Buckler, Andrew] Elucid Bioimaging Inc, Wenham, MA USA.
[Kinahan, Paul] Univ Washington, Dept Radiol, Seattle, WA 98195 USA.
[-Mayer, Heather Chen] NIST, Gaithersburg, MD 20899 USA.
[Petrick, Nicholas] US FDA, CDRH, Silver Spring, MD USA.
[Barboriak, Daniel P.; Barnhart, Huiman; Sullivan, Daniel C.] Duke Univ, Sch Med, Durham, NC USA.
RP Obuchowski, NA (reprint author), Cleveland Clin Fdn, Quantitat Hlth Sci, 9500 Euclid Ave, Cleveland, OH 44195 USA.
EM obuchon@ccf.org
RI Barboriak, Daniel/M-4414-2015;
OI Barboriak, Daniel/0000-0002-2536-6266; Buckler,
Andrew/0000-0002-0786-4835
FU NIBIB [HHSN268201300071C]
FX This work was supported by a grant from NIBIB (no. HHSN268201300071C).
QIBA is indebted to the many volunteers who participated in the QIBA
metrology workshops for their contributions to the statistical
groundwork for the claims.
NR 13
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Z9 0
U1 2
U2 3
PU ELSEVIER SCIENCE INC
PI NEW YORK
PA 360 PARK AVE SOUTH, NEW YORK, NY 10010-1710 USA
SN 1076-6332
EI 1878-4046
J9 ACAD RADIOL
JI Acad. Radiol.
PD APR
PY 2016
VL 23
IS 4
BP 496
EP 506
DI 10.1016/j.acra.2015.12.020
PG 11
WC Radiology, Nuclear Medicine & Medical Imaging
SC Radiology, Nuclear Medicine & Medical Imaging
GA DH8HM
UT WOS:000373034100014
PM 26898527
ER
PT J
AU Klose, A
Ycas, G
Cruz, FC
Maser, DL
Diddams, SA
AF Klose, Andrew
Ycas, Gabriel
Cruz, Flavio C.
Maser, Daniel L.
Diddams, Scott A.
TI Rapid, broadband spectroscopic temperature measurement of CO2 using VIPA
spectroscopy
SO APPLIED PHYSICS B-LASERS AND OPTICS
LA English
DT Article
ID FOURIER-TRANSFORM SPECTROSCOPY; FREQUENCY COMB SPECTROSCOPY;
DIODE-LASER; GAS; DATABASE
AB Time-resolved spectroscopic temperature measurements of a sealed carbon dioxide sample cell were realized with an optical frequency comb combined with a two-dimensional dispersive spectrometer. A supercontinuum laser source based on an erbium fiber mode-locked laser was employed to generate coherent light around 2000 nm (5000 cm(-1)). The laser was passed through a 12-cm-long cell containing CO2, and the transmitted light was analyzed in a virtually imaged phased array-based spectrometer. Broadband spectra spanning more than 100 cm(-1) with a spectral resolution of roughly 0.075 cm(-1) (2.2 GHz) were acquired with an integration period of 2 ms. The temperature of the CO2 sample was deduced from fitting a modeled spectrum to the line intensities of the experimentally acquired spectrum. Temperature dynamics on the timescale of milliseconds were observed with a temperature resolution of 2.6 K. The spectroscopically deduced temperatures agreed with temperatures of the sample cell measured with a thermistor. Potential applications of this technique include quantitative measurement of carbon dioxide concentration and temperature dynamics in gas-phase chemical reactions(e.g., combustion) and plasma diagnostics.
C1 [Klose, Andrew; Ycas, Gabriel; Cruz, Flavio C.; Maser, Daniel L.; Diddams, Scott A.] NIST, Boulder, CO 80305 USA.
[Cruz, Flavio C.] Univ Estadual Campinas, Inst Fis Gleb Wataghin, BR-13083859 Campinas, SP, Brazil.
[Maser, Daniel L.; Diddams, Scott A.] Univ Colorado, Dept Phys, Boulder, CO 80309 USA.
[Klose, Andrew] Augustana Univ, Dept Chem, Sioux Falls, SD 57197 USA.
RP Klose, A (reprint author), NIST, Boulder, CO 80305 USA.; Klose, A (reprint author), Augustana Univ, Dept Chem, Sioux Falls, SD 57197 USA.
EM aklose@augie.edu
FU NIST Greenhouse Gas and Climate Science Measurements Program; National
Research Council Postdoctoral Fellowship Program; CNPq; Fapesp; NIST
FX This work was supported in part by the NIST Greenhouse Gas and Climate
Science Measurements Program. The authors thank T.A. Johnson, L.
Nugent-Glandorf, F. Quinlan, and F. Giorgetta for useful discussions, J.
Ye for providing the VIPA etalon, and M. Hirano of Sumitomo for
providing the nonlinear fiber. A.K. acknowledges support from the
National Research Council Postdoctoral Fellowship Program, and F.C.C.
acknowledges support from CNPq, Fapesp and NIST. This work is a
contribution of the United States Government and is not subject to
copyright in the United States.
NR 17
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U1 10
U2 15
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0946-2171
EI 1432-0649
J9 APPL PHYS B-LASERS O
JI Appl. Phys. B-Lasers Opt.
PD APR
PY 2016
VL 122
IS 4
AR UNSP 78
DI 10.1007/s00340-016-6349-4
PG 8
WC Optics; Physics, Applied
SC Optics; Physics
GA DH6IQ
UT WOS:000372894600011
ER
PT J
AU Fang, SX
Tans, PP
Dong, F
Zhou, HG
Luan, T
AF Fang, Shuang-xi
Tans, Pieter P.
Dong, Fan
Zhou, Huaigang
Luan, Tian
TI Characteristics of atmospheric CO2 and CH4 at the Shangdianzi regional
background station in China
SO ATMOSPHERIC ENVIRONMENT
LA English
DT Article
DE Carbon dioxide; Methane; Observation; Back trajectory; Air mass
transport
ID CARBON-DIOXIDE; EAST-ASIA; WMO/GAW STATIONS; EMISSIONS; METHANE;
MONOXIDE; TRENDS; POLLUTANTS; GROWTH; SITE
AB Atmospheric CO2 and CH4 have been continuously measured at the Shangdianzi regional background station (SDZ) in China from 2009 to 2013. Based on the influences of local surface wind and long-distance transport, the observed records were flagged into locally influenced, Beijing-Tianjin-Hebei (BTH) influenced, and Russia, Mongolia, and Inner Mongolia autonomous region influenced (RMI). similar to 81.4% of CO2 and similar to 75.6% of CH4 mole fractions were flagged as locally representative, indicating that the atmospheric CO2 and CH4 at SDZ were strongly influenced by local sources and sinks. Cluster analysis of back trajectories proved that the atmospheric CO2 and CH4 were influenced by air masses from northwest (RMI) or from south and southeast (BTH). The CO2 and CH4 mole fractions in BTH are always higher than in RMI, with the largest difference of 11.5 +/- 0.3 ppm for CO2 and 102 +/- 1 ppb for CH4 in July. The annual growth rates of CO2 and CH4 in BTH are 3.8 +/- 0.01 ppm yr(-1) and 10 +/- 0.1 ppb yr(-1), respectively, which are apparently higher than those of the RMI and the global means. The long-term trends of CO2 and CH4 in BTH are deviating from those in RMI, with ratios of similar to 1.0 ppm yr(-1) for CO2 and similar to 2 ppb yr(-1) for CH4, indicating the strengths of CO2 and CH4 emission in Beijing-Tianjin-Hebei plain increased more than 20% every year. (C) 2016 Elsevier Ltd. All rights reserved.
C1 [Fang, Shuang-xi] China Meteorol Adm, MOC, Beijing, Peoples R China.
[Tans, Pieter P.] NOAA, ESRL, Boulder, CO USA.
[Dong, Fan; Zhou, Huaigang] CMA, Shangdianzi Reg Background Stn, Beijing, Peoples R China.
[Luan, Tian] Chinese Acad Meteorol Sci, CMA, Beijing, Peoples R China.
RP Fang, SX (reprint author), China Meteorol Adm, MOC, Beijing, Peoples R China.
EM fangsx@cma.gov.cn
FU National Natural Science Foundation of China [41375130, 41405129,
41303052]
FX We express our great thanks to the staff at Shangdianzi station, who
have contributed to the system installation and maintenance. This work
is supported by National Natural Science Foundation of China (No.
41375130, 41405129, 41303052).
NR 50
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U1 6
U2 22
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 1352-2310
EI 1873-2844
J9 ATMOS ENVIRON
JI Atmos. Environ.
PD APR
PY 2016
VL 131
BP 1
EP 8
DI 10.1016/j.atmosenv.2016.01.044
PG 8
WC Environmental Sciences; Meteorology & Atmospheric Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA DH4NT
UT WOS:000372763400001
ER
PT J
AU Kritzer, JP
Delucia, MB
Greene, E
Shumway, C
Topolski, MF
Thomas-Blate, J
Chiarella, LA
Davy, KB
Smith, K
AF Kritzer, Jacob P.
Delucia, Mari-Beth
Greene, Emily
Shumway, Caroly
Topolski, Marek F.
Thomas-Blate, Jessie
Chiarella, Louis A.
Davy, Kay B.
Smith, Kent
TI The Importance of Benthic Habitats for Coastal Fisheries
SO BIOSCIENCE
LA English
DT Article
DE coastal ecosystems; fisheries; marine biology; aquatic ecosystems;
conservation
ID ECOSYSTEM SERVICES; FISH COMMUNITIES; MANAGEMENT; ESTUARINE; JUVENILE;
IMPACTS; CONSERVATION; BIODIVERSITY; CONNECTIVITY; ASSEMBLAGES
AB Ecosystem-based management requires greater attention to habitat conservation. We evaluate the importance of benthic habitats as space for shelter, feeding, and breeding by coastal fishes and motile invertebrates in four biogeographic regions of the eastern United States. The importance of different habitats changed with latitude. Soft sediments and riverine systems scored higher in northern regions, and marshes and coral reefs scored higher in the south. The importance of soft sediments is notable because environmental assessments often assume their ecological value is lower. Submerged aquatic vegetation was a key nursery habitat coast-wide. An important consideration is that anthropogenic impacts have altered habitat availability and use, and climate change is causing ongoing disturbance. Furthermore, distinct habitats should not be managed in isolation but rather as interconnected mosaics. Our approach, combined with information on status, vulnerability, and other ecological functions, can be used to evaluate trade-offs and develop habitat-management strategies.
C1 [Kritzer, Jacob P.] Environm Def Fund, Boston, MA USA.
[Delucia, Mari-Beth] Nature Conservancy, Harrisburg, PA USA.
[Greene, Emily] Earth Resources Technol Inc, Laurel, MD USA.
[Shumway, Caroly] Merrimack River Watershed Council, Lawrence, MA USA.
[Topolski, Marek F.] Maryland Dept Nat Resources, Fisheries Serv, Annapolis, MD USA.
[Thomas-Blate, Jessie] Amer Rivers, Washington, DC USA.
[Chiarella, Louis A.] Natl Marine Fisheries Serv, Greater Atlant Reg Fisheries Off, Gloucester, MA USA.
[Davy, Kay B.] Natl Marine Fisheries Serv, Protected Resources Div, Dania, FL USA.
[Smith, Kent] Florida Fish & Wildlife Conservat Commiss, Aquat Habitat Conservat & Restorat Sect, Tallahassee, FL USA.
RP Kritzer, JP (reprint author), Environm Def Fund, Boston, MA USA.
EM jkritzer@edf.org
FU ASMFC; ACFHP [DC M-60-HM]; USFWS [F14AC00728]
FX We thank the many scientists at agencies, institutions, and
organizations along the Atlantic coast that completed - sections of the
matrix, participated in review meetings, or conducted independent
reviews (see the supplementary material for a full list). Funding for
the habitat evaluation was provided to ASMFC and ACFHP through the
Multistate Conservation Grant Program, grant no. DC M-60-HM,
administered by the U.S. Fish and Wildlife Agency (USFWS) and the
Association of Fish and Wildlife Agencies. Additional funding was
provided by USFWS cooperative agreement no. F14AC00728 to ASMFC.
Comments from three anonymous reviewers improved the quality of this
article, although the content remains the sole responsibility of the
authors. The habitat scores and supporting bibliography are archived by
ACFHP (www.atlanticfishhabitat.org). The authors claim no conflicts of
interest.
NR 64
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U1 7
U2 31
PU OXFORD UNIV PRESS
PI OXFORD
PA GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND
SN 0006-3568
EI 1525-3244
J9 BIOSCIENCE
JI Bioscience
PD APR
PY 2016
VL 66
IS 4
BP 274
EP 284
DI 10.1093/biosci/biw014
PG 11
WC Biology
SC Life Sciences & Biomedicine - Other Topics
GA DI0WK
UT WOS:000373217800004
ER
PT J
AU Wagner, R
Moon, RJ
Raman, A
AF Wagner, Ryan
Moon, Robert J.
Raman, Arvind
TI Mechanical properties of cellulose nanomaterials studied by contact
resonance atomic force microscopy
SO CELLULOSE
LA English
DT Article
DE Atomic force microscopy; Cellulose nanomaterials; Cellulose
nanocrystals; Cellulose nanofibrils; Contact resonance; Nanomechanics
ID ELASTIC-MODULI; WHISKERS; NANOCRYSTALS; CALIBRATION; SIZE
AB Quantification of the mechanical properties of cellulose nanomaterials is key to the development of new cellulose nanomaterial based products. Using contact resonance atomic force microscopy we measured and mapped the transverse elastic modulus of three types of cellulosic nanoparticles: tunicate cellulose nanocrystals, wood cellulose nanocrystals, and wood cellulose nanofibrils. These modulus values were calculated with different contact mechanics models exploring the effects of cellulose geometry and thickness on the interpretation of the data. While intra-particle variations in modulus are detected, we did not observe a measureable difference in modulus between the three types of cellulose particles. Improved practices and experimental complications for the characterization of cellulosic nanomaterials with atomic force microscopy are discussed.
C1 [Wagner, Ryan; Raman, Arvind] Purdue Univ, Birck Nanotechnol Ctr, W Lafayette, IN 47907 USA.
[Wagner, Ryan; Raman, Arvind] Purdue Univ, Sch Mech Engn, W Lafayette, IN 47907 USA.
[Moon, Robert J.] US Forest Serv, Forest Prod Lab, Madison, WI 53726 USA.
[Wagner, Ryan] NIST, Mat Measurement Lab, Boulder, CO 80305 USA.
RP Wagner, R (reprint author), NIST, Mat Measurement Lab, Boulder, CO 80305 USA.
EM rbwagner187@gmail.com; robertmoon@fs.fed.us; raman@purdue.edu
FU Forest Products laboratory (US Forest Service) [12-CR-11111129-076]
FX The authors would like to thank the Forest Products laboratory (US
Forest Service) Grant No. 12-CR-11111129-076 for funding this research.
We are grateful to the Forest Products laboratory for providing the wood
CN samples and Professor Christoph Weder (Universite de Fribourg) for
providing tunicate CN samples. We are also grateful for Jason Killgore
(NIST) for helpful discussions regarding the contact resonance AFM
technique.
NR 46
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U1 5
U2 27
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0969-0239
EI 1572-882X
J9 CELLULOSE
JI Cellulose
PD APR
PY 2016
VL 23
IS 2
BP 1031
EP 1041
DI 10.1007/s10570-016-0883-4
PG 11
WC Materials Science, Paper & Wood; Materials Science, Textiles; Polymer
Science
SC Materials Science; Polymer Science
GA DH9SO
UT WOS:000373136400002
ER
PT J
AU Gangodagamage, C
Foufoula-Georgiou, E
Brumby, SP
Chartrand, R
Koltunov, A
Liu, DS
Cai, M
Ustin, SL
AF Gangodagamage, Chandana
Foufoula-Georgiou, Efi
Brumby, Steven P.
Chartrand, Rick
Koltunov, Alexander
Liu, Desheng
Cai, Michael
Ustin, Susan L.
TI Wavelet-Compressed Representation of Landscapes for Hydrologic and
Geomorphologic Applications
SO IEEE GEOSCIENCE AND REMOTE SENSING LETTERS
LA English
DT Article
DE Biorthogonal modulation; biorthogonal wavelets; channel networks; data
compression; Digital Elevation models (DEMs); high spatial resolution
data; hydrology; image resolution; LiDAR; lossy compression; wavelets;
wavelet transforms
ID ORGANIZATION
AB The availability of high-resolution digital elevation data (submeter resolution) from LiDAR has increased dramatically over the past few years. As a result, the efficient storage and transmission of those large data sets and their use for geomorphic feature extraction and hydrologic/environmental modeling are becoming a scientific challenge. This letter explores the use of multiresolution wavelet analysis for compression of LiDAR digital elevation data sets. The compression takes advantage of the fact that, in most landscapes, neighboring pixels are correlated and thus contain some redundant information. The space-frequency localization of the wavelet filters allows one to preserve detailed high-resolution features where needed while representing the rest of the landscape at lower resolution. We explore a lossy compression methodology based on biorthogonal wavelets and demonstrate that, by keeping only approximately 10% of the original information (data compression ratio similar to 94%), the reconstructed landscapes retain most of the information of relevance to geomorphologic applications, such as the ability to accurately extract channel networks for environmental flux routing, as well as to identify geomorphic process transition from the curvature-slope and slope-distance relationships.
C1 [Gangodagamage, Chandana; Koltunov, Alexander; Ustin, Susan L.] Univ Calif Davis, Dept Land Air & Water Resources, Davis, CA 95616 USA.
[Gangodagamage, Chandana] Los Alamos Natl Lab, Earth & Environm Sci & Space Sci & Remote Sensing, POB 1663, Los Alamos, NM 87544 USA.
[Gangodagamage, Chandana] NOAA, Natl Water Ctr, Tuscaloosa, AL 35406 USA.
[Foufoula-Georgiou, Efi] Univ Minnesota, Dept Civil Engn, St Anthony Falls Lab, Minneapolis, MN 55414 USA.
[Foufoula-Georgiou, Efi] Univ Minnesota, Natl Ctr Earth Surface Dynam, Minneapolis, MN 55414 USA.
[Brumby, Steven P.; Chartrand, Rick] Los Alamos Natl Lab, POB 1663, Los Alamos, NM 87545 USA.
[Brumby, Steven P.; Chartrand, Rick] Descartes Labs, Los Alamos, NM 87544 USA.
[Liu, Desheng] Ohio State Univ, Dept Geog, Columbus, OH 43210 USA.
[Cai, Michael] Los Alamos Natl Lab, Space Data Syst, POB 1663, Los Alamos, NM 87545 USA.
RP Gangodagamage, C (reprint author), Univ Calif Davis, Dept Land Air & Water Resources, Davis, CA 95616 USA.; Gangodagamage, C (reprint author), Los Alamos Natl Lab, Earth & Environm Sci & Space Sci & Remote Sensing, POB 1663, Los Alamos, NM 87544 USA.; Gangodagamage, C (reprint author), NOAA, Natl Water Ctr, Tuscaloosa, AL 35406 USA.
EM chhandana@gmail.com
RI Liu, Desheng/A-9356-2011;
OI Gangodagamage, Chandana/0000-0001-6511-1711
NR 22
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U1 5
U2 12
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 APR
PY 2016
VL 13
IS 4
BP 480
EP 484
DI 10.1109/LGRS.2015.2513011
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 DH7YJ
UT WOS:000373009800002
ER
PT J
AU Yang, H
Weng, FZ
AF Yang, Hu
Weng, Fuzhong
TI Corrections for On-Orbit ATMS Lunar Contamination
SO IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING
LA English
DT Article
DE Advanced Technology Microwave Sounder (ATMS); calibration;
contamination; lunar intrusion (LI)
ID BRIGHTNESS TEMPERATURE
AB The cold calibration count from the Advanced Technology Microwave Sounder (ATMS) space view increases when the lunar radiation intrudes its antenna field of view (FOV). This increase is referred to as lunar contamination since the cold count is notmatched with the specified brightness temperature of 2.73 K. For ATMS, it is found that the elapse time of lunar intrusion (LI) and the magnitude of the cold count increase are channel dependent. If the lunar-affected calibration counts are rejected in the processing, a data gap can be shown in brightness temperature at all channels. At ATMS channels 1 and 2, which have a large FOV, the LI can result in an increase of 40 counts in cold calibration. At higher frequency channels which have a smaller FOV size, the LI intensity is much stronger and can be as large as a few hundred counts. The LI becomes significant when its radiation appears in the ATMS antenna main beam. In the current ATMS operational calibration algorithm, the cold count anomaly is detected when the intensity of LI exceeds a certain threshold. The lunar radiation can be also corrected in the ATMS calibration. In doing so, a lunar radiation term is derived as a function of antenna gain, the solid angle of the Moon, and the brightness temperature of the Moon disk. This algorithm is applied in an ATMS calibration system developed at NOAA and shows a successful removal of all the lunar contamination on the earth-scene brightness temperature.
C1 [Yang, Hu] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20740 USA.
[Weng, Fuzhong] NOAA, Ctr Satellite Applicat & Res, College Pk, MD 20740 USA.
RP Yang, H (reprint author), Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20740 USA.
EM huyang@umd.edu
RI Weng, Fuzhong/F-5633-2010
OI Weng, Fuzhong/0000-0003-0150-2179
FU National Oceanic and Atmospheric Administration's Joint Polar Satellite
System Program
FX This work was supported by the National Oceanic and Atmospheric
Administration's Joint Polar Satellite System Program. The views
expressed in this publication are those of the authors and do not
necessarily represent those of NOAA.
NR 9
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U1 2
U2 3
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 0196-2892
EI 1558-0644
J9 IEEE T GEOSCI REMOTE
JI IEEE Trans. Geosci. Remote Sensing
PD APR
PY 2016
VL 54
IS 4
BP 1918
EP 1924
DI 10.1109/TGRS.2015.2490198
PG 7
WC Geochemistry & Geophysics; Engineering, Electrical & Electronic; Remote
Sensing; Imaging Science & Photographic Technology
SC Geochemistry & Geophysics; Engineering; Remote Sensing; Imaging Science
& Photographic Technology
GA DH7WF
UT WOS:000373004000004
ER
PT J
AU Fu, SD
Cui, WL
Hu, M
Chang, RN
Donahue, MJ
Lomakin, V
AF Fu, Sidi
Cui, Weilong
Hu, Matthew
Chang, Ruinan
Donahue, Michael J.
Lomakin, Vitaliy
TI Finite-Difference Micromagnetic Solvers With the Object-Oriented
Micromagnetic Framework on Graphics Processing Units
SO IEEE TRANSACTIONS ON MAGNETICS
LA English
DT Article
DE Graphics processing unit (GPU); magnetostatics; micromagnetics;
object-oriented micromagnetic framework (OOMMF)
ID FIELD CALCULATION; SIMULATIONS; ALGORITHM
AB A micromagnetic solver using the finite-difference method on a graphics processing unit (GPU) and its integration with the object-oriented micromagnetic framework (OOMMF) are presented. Two approaches for computing the magnetostatic field accelerated by the fast Fourier transform are implemented. The first approach, referred to as the tensor approach, is based on the tensor spatial convolution to directly compute the magnetostatic field from magnetic moments. The second approach, referred to as the scalar potential approach, uses differential operator evaluation through finite differences (divergence for magnetic charge and gradient for magnetostatic field) and spatial convolution for magnetic scalar potential. Comparisons of implementation details, speed, memory consumption, and accuracy are provided. The GPU implementation of OOMMF shows up to 32x GPU-CPU speedup.
C1 [Fu, Sidi; Lomakin, Vitaliy] Univ Calif San Diego, Ctr Magnet Res, La Jolla, CA 92037 USA.
[Fu, Sidi; Lomakin, Vitaliy] Univ Calif San Diego, Dept Elect & Comp Engn, La Jolla, CA 92037 USA.
[Cui, Weilong] Univ Calif Santa Barbara, Dept Comp Sci, Santa Barbara, CA 93106 USA.
[Hu, Matthew] Stanford Univ, Dept Elect Engn, Stanford, CA 94305 USA.
[Chang, Ruinan] Oracle Corp, San Diego, CA 92121 USA.
[Donahue, Michael J.] NIST, Gaithersburg, MD 20899 USA.
RP Fu, SD (reprint author), Univ Calif San Diego, Ctr Magnet Res, La Jolla, CA 92037 USA.; Fu, SD (reprint author), Univ Calif San Diego, Dept Elect & Comp Engn, La Jolla, CA 92037 USA.
EM s6fu@ucsd.edu
FU National Institute of Standards and Technology
FX This work was supported by the National Institute of Standards and
Technology. The mention of specific products, trademarks, or brand names
is for the purposes of identification only. Such a mention is not to be
interpreted in any way as an endorsement or certification of such
products or brands by the National Institute of Standards and
Technology. All trademarks mentioned herein belong to their respective
owners.
NR 29
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PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 0018-9464
EI 1941-0069
J9 IEEE T MAGN
JI IEEE Trans. Magn.
PD APR
PY 2016
VL 52
IS 4
AR 7100109
DI 10.1109/TMAG.2015.2503262
PG 9
WC Engineering, Electrical & Electronic; Physics, Applied
SC Engineering; Physics
GA DH5PK
UT WOS:000372843500018
ER
PT J
AU Ortega, KL
Krause, JM
Ryzhkov, AV
AF Ortega, Kiel L.
Krause, John M.
Ryzhkov, Alexander V.
TI Polarimetric Radar Characteristics of Melting Hail. Part III: Validation
of the Algorithm for Hail Size Discrimination
SO JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY
LA English
DT Article
DE Algorithms; Convective storms; Remote sensing; Hail; Radars/Radar
observations
ID HYDROMETEOR CLASSIFICATION; POLARIZATION EXPERIMENT; DOPPLER RADAR;
INDICATOR; WSR-88D; MODEL; REFLECTIVITY; PERFORMANCE; SIGNATURES;
GRAUPEL
AB This study is the third part of a paper series investigating the polarimetric radar properties of melting hail and application of those properties for operational polarimetric hail detection and determination of its size. The results of theoretical simulations in Part I were used to develop a hail size discrimination algorithm (HSDA) described in Part II. The HSDA uses radar reflectivity Z, differential reflectivity Z(DR), and cross-correlation coefficient rho(hv) along with melting-level height within a fuzzy-logic scheme to distinguish among three hail size classes: small hail (with diameter D < 2.5 cm), large hail (2.5 < D < 5.0 cm), and giant hail (D > 5.0 cm). The HSDA validation is performed using radar data collected by numerous WSR-88D sites and more than 3000 surface hail reports obtained from the Severe Hazards Analysis and Verification Experiment (SHAVE). The original HSDA version was modified in the process of validation, and the modified algorithm demonstrates probability of detection of 0.594, false-alarm ratio of 0.136, and resulting critical success index (CSI) equal to 0.543. The HSDA outperformed the current operational single-polarization hail detection algorithm, which only provides a single hail size estimate per storm and is characterized by CSI equal to 0.324. It is shown that HSDA is particularly sensitive to the quality of Z(DR) measurements, which might be affected by possible radar miscalibration and anomalously high differential attenuation.
C1 Univ Oklahoma, Cooperat Inst Mesoscale Meteorol Studies, Norman, OK 73019 USA.
NOAA, OAR Natl Severe Storms Lab, Norman, OK USA.
RP Ortega, KL (reprint author), 120 David L Boren Blvd, Norman, OK 73072 USA.
EM kiel.ortega@noaa.gov
FU NOAA/Office of Oceanic and Atmospheric Research under NOAA-University of
Oklahoma, U.S. Department of Commerce [NA11OAR4320072]
FX The authors thank Terry Schuur, Jeff Snyder, and three anonymous
reviewers for their feedback, which helped clarify the text and figures.
Thanks also are given to the many students who worked for SHAVE and
collected this valuable dataset
(http://www.nssl.noaa.gov/projects/shave/team.php). Funding was provided
by NOAA/Office of Oceanic and Atmospheric Research under NOAA-University
of Oklahoma Cooperative Agreement NA11OAR4320072, U.S. Department of
Commerce.
NR 39
TC 3
Z9 3
U1 7
U2 13
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 APR
PY 2016
VL 55
IS 4
BP 829
EP 848
DI 10.1175/JAMC-D-15-0203.1
PG 20
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DH5OM
UT WOS:000372839700001
ER
PT J
AU Hoerling, M
Eischeid, J
Perlwitz, J
Quan, XW
Wolter, K
Cheng, LY
AF Hoerling, Martin
Eischeid, Jon
Perlwitz, Judith
Quan, Xiao-Wei
Wolter, Klaus
Cheng, Linyin
TI Characterizing Recent Trends in U.S. Heavy Precipitation
SO JOURNAL OF CLIMATE
LA English
DT Article
DE Atmosphere-ocean interaction; Trends; Climate variability; Physical
Meteorology and Climatology; Geographic location/entity; Variability;
North America; Climate change
ID UNITED-STATES; CLIMATE MODEL; SURFACE-TEMPERATURE; DAILY VARIABILITY;
EL-NINO; TRANSIENTS; FREQUENCY; EXTREMES; DATASET; EVENTS
AB Time series of U.S. daily heavy precipitation (95th percentile) are analyzed to determine factors responsible for regionality and seasonality in their 1979-2013 trends. For annual conditions, contiguous U.S. trends have been characterized by increases in precipitation associated with heavy daily events across the northern United States and decreases across the southern United States. Diagnosis of climate simulations (CCSM4 and CAM4) reveals that the evolution of observed sea surface temperatures (SSTs) was a more important factor influencing these trends than boundary condition changes linked to external radiative forcing alone. Since 1979, the latter induces widespread, but mostly weak, increases in precipitation associated with heavy daily events. The former induces a meridional pattern of northern U.S. increases and southern U.S. decreases as observed, the magnitude of which closely aligns with observed changes, especially over the south and far west. Analysis of model ensemble spread reveals that appreciable 35-yr trends in heavy daily precipitation can occur in the absence of forcing, thereby limiting detection of the weak anthropogenic influence at regional scales.
Analysis of the seasonality in heavy daily precipitation trends supports physical arguments that their changes during 1979-2013 have been intimately linked to internal decadal ocean variability and less so to human-induced climate change. Most of the southern U.S. decrease has occurred during the cold season that has been dynamically driven by an atmospheric circulation reminiscent of teleconnections linked to cold tropical eastern Pacific SSTs. Most of the northeastern U.S. increase has been a warm season phenomenon, the immediate cause for which remains unresolved.
C1 [Hoerling, Martin; Eischeid, Jon; Perlwitz, Judith; Quan, Xiao-Wei; Wolter, Klaus; Cheng, Linyin] NOAA, Earth Syst Res Lab, Boulder, CO 80303 USA.
[Eischeid, Jon; Perlwitz, Judith; Quan, Xiao-Wei; Wolter, Klaus; Cheng, Linyin] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
RP Hoerling, M (reprint author), NOAA, ESRL Phys Sci Div, R E PSD 325 Broadway, Boulder, CO 80303 USA.
EM Martin.hoerling@noaa.gov
RI Perlwitz, Judith/B-7201-2008
OI Perlwitz, Judith/0000-0003-4061-2442
FU NOAA Climate Program Office MAPP program; NASA MAP program
FX The authors thank the editor and three anonymous reviewers for their
helpful and constructive comments on the manuscript. We also acknowledge
the support provided by the NOAA Climate Program Office MAPP program and
by the NASA MAP program.
NR 37
TC 2
Z9 2
U1 5
U2 16
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 APR
PY 2016
VL 29
IS 7
BP 2313
EP 2332
DI 10.1175/JCLI-D-15-0441.1
PG 20
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DH5GG
UT WOS:000372813600001
ER
PT J
AU Zhang, T
Hoerling, MP
Perlwitz, J
Xu, TY
AF Zhang, Tao
Hoerling, Martin P.
Perlwitz, Judith
Xu, Taiyi
TI Forced Atmospheric Teleconnections during 1979-2014
SO JOURNAL OF CLIMATE
LA English
DT Article
DE Climate variability; Variability; Atmosphere-ocean interaction;
Atmospheric circulation; Circulation/ Dynamics; ENSO
ID SEA-SURFACE TEMPERATURE; SEASONAL FOOTPRINTING MECHANISM;
GENERAL-CIRCULATION MODEL; EL-NINO; SOUTHERN-OSCILLATION; CLIMATE
RESPONSE; ENSO ASYMMETRY; LA-NINA; ANOMALIES; VARIABILITY
AB Forced atmospheric teleconnections during 1979-2014 are examined using a 50-member ensemble of atmospheric general circulation model (AGCM) simulations subjected to observed variations in sea surface temperatures (SSTs), sea ice, and carbon dioxide. Three primary modes of forced variability are identified using empirical orthogonal function (EOF) analysis of the ensemble mean wintertime extratropical Northern Hemisphere 500-hPa heights. The principal component time series of the first and second modes are highly correlated with Nino-3.4 and trans-Nino (TNI) SST indices, respectively, indicating mostly tropical sources. Their impacts are largely confined to the Pacific-North American (PNA) sector. The leading mode describes the canonical atmospheric teleconnection associated with El Nino-Southern Oscillation (ENSO) resembling the tropical/Northern Hemisphere pattern. The second mode describes a wave train resembling the classic PNA pattern resulting from atmospheric sensitivity to ENSO asymmetry and from sensitivity to a tropical precursor SST for ENSO development. The third mode is characterized by a hemisphere-scale increasing trend in heights. Based on a comparison with 50-member coupled ocean-atmosphere model simulations, it is argued that this mode is strongly related to radiatively forced climate change, while the other two forced teleconnections are principally related to internal coupled variability. A trend in the leading forced mode is related to ENSO-like decadal variability and dominates the overall observed 500-hPa height trend since 1979. These model results indicate that the trend in the first mode is due to internal variability rather than external radiative forcing.
C1 [Zhang, Tao; Perlwitz, Judith; Xu, Taiyi] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Zhang, Tao; Hoerling, Martin P.; Perlwitz, Judith; Xu, Taiyi] NOAA, Earth Syst Res Lab, Div Phys Sci, Boulder, CO 80305 USA.
RP Zhang, T (reprint author), NOAA, ESRL, PSD, 325 Broadway,R PSD1, Boulder, CO 80305 USA.
EM tao.zhang@noaa.gov
RI Perlwitz, Judith/B-7201-2008
OI Perlwitz, Judith/0000-0003-4061-2442
FU NOAA's Climate Program Office
FX This work was supported by grants from NOAA's Climate Program Office. We
acknowledge NCAR's CESM1(CAM5) Large Ensemble Community Project for
carrying out the large CESM1 ensemble. We wish to thank Xiaowei Quan for
carrying out the large CCSM4 ensemble and Jon Eischeid for his technical
support. We also thank three anonymous reviewers for their constructive
comments that helped to improve the paper.
NR 60
TC 1
Z9 1
U1 3
U2 15
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 APR
PY 2016
VL 29
IS 7
BP 2333
EP 2357
DI 10.1175/JCLI-D-15-0226.1
PG 25
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DH5GG
UT WOS:000372813600002
ER
PT J
AU Krishnamurthy, L
Vecchi, GA
Msadek, R
Murakami, H
Wittenberg, A
Zeng, FR
AF Krishnamurthy, Lakshmi
Vecchi, Gabriel A.
Msadek, Rym
Murakami, Hiroyuki
Wittenberg, Andrew
Zeng, Fanrong
TI Impact of Strong ENSO on Regional Tropical Cyclone Activity in a
High-Resolution Climate Model in the North Pacific and North Atlantic
Oceans
SO JOURNAL OF CLIMATE
LA English
DT Article
DE Climate models; ENSO; Atm/Ocean Structure/ Phenomena; Models and
modeling; Tropical cyclones; Circulation/ Dynamics
ID SOUTH CHINA SEA; 1997-98 EL-NINO; INTERANNUAL VARIABILITY; STORM
FORMATION; LA-NINA; EVENTS; FREQUENCY; PRECIPITATION; MECHANISMS;
SIMULATION
AB Tropical cyclone (TC) activity in the North Pacific and North Atlantic Oceans is known to be affected by the El Nino-Southern Oscillation (ENSO). This study uses the GFDL Forecast Oriented Low Ocean Resolution Model (FLOR), which has relatively high resolution in the atmosphere, as a tool to investigate the sensitivity of TC activity to the strength of ENSO events. This study shows that TCs exhibit a nonlinear response to the strength of ENSO in the tropical eastern North Pacific (ENP) but a quasi-linear response in the tropical western North Pacific (WNP) and tropical North Atlantic. Specifically, a stronger El Nino results in disproportionate inhibition of TCs in the ENP and North Atlantic, and leads to an eastward shift in the location of TCs in the southeast of the WNP. However, the character of the response of TCs in the Pacific is insensitive to the amplitude of La Nina events. The eastward shift of TCs in the southeast of the WNP in response to a strong El Nino is due to an eastward shift of the convection and of the associated environmental conditions favorable for TCs. The inhibition of TC activity in the ENP and Atlantic during El Nino is attributed to the increase in the number of days with strong vertical wind shear during stronger El Nino events. These results are further substantiated with coupled model experiments. Understanding of the impact of strong ENSO on TC activity is important for present and future climate as the frequency of occurrence of extreme ENSO events is projected to increase in the future.
C1 [Krishnamurthy, Lakshmi; Vecchi, Gabriel A.; Msadek, Rym; Murakami, Hiroyuki; Wittenberg, Andrew; Zeng, Fanrong] NOAA, Geophys Fluid Dynam Lab, Princeton Univ Forrestal Campus,201 Forrestal Rd, Princeton, NJ 08540 USA.
[Krishnamurthy, Lakshmi; Msadek, Rym] Univ Corp Atmospher Res, Boulder, CO USA.
[Vecchi, Gabriel A.; Murakami, Hiroyuki] Princeton Univ, Atmospher & Ocean Sci Program, Princeton, NJ 08544 USA.
RP Krishnamurthy, L (reprint author), NOAA, Geophys Fluid Dynam Lab, Princeton Univ Forrestal Campus,201 Forrestal Rd, Princeton, NJ 08540 USA.
EM Lakshmi.Krishnamurthy@noaa.gov
RI Wittenberg, Andrew/G-9619-2013; Vecchi, Gabriel/A-2413-2008
OI Wittenberg, Andrew/0000-0003-1680-8963; Vecchi,
Gabriel/0000-0002-5085-224X
FU MAPP Intra Americas Seas proposal - NOAA/Climate Program Office
FX We thank Tom Delworth for his contribution to the FLOR flux adjusted run
and helpful comments, Wei Zhang and Baoqiang Xiang for their
suggestions, Seth Underwood for technical help with the model runs, and
Catherine Raphael for help with schematic diagram. We also thank the
anonymous reviewers for their constructive suggestions. This work is
supported by MAPP Intra Americas Seas proposal funded by the
NOAA/Climate Program Office.
NR 51
TC 7
Z9 7
U1 7
U2 19
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 APR
PY 2016
VL 29
IS 7
BP 2375
EP 2394
DI 10.1175/JCLI-D-15-0468.1
PG 20
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DH5GJ
UT WOS:000372813900001
ER
PT J
AU Mo, KC
Lettenmaier, DP
AF Mo, Kingtse C.
Lettenmaier, Dennis P.
TI Precipitation Deficit Flash Droughts over the United States
SO JOURNAL OF HYDROMETEOROLOGY
LA English
DT Article
DE Drought; Atm/Ocean Structure/ Phenomena; Agriculture; Extreme events;
Applications
ID CONVECTIVE INSTABILITY PATHWAY; HYDROLOGICALLY BASED DATASET;
EVAPORATIVE STRESS INDEX; WARM-SEASON DROUGHT; LAND-SURFACE FLUXES;
20TH-CENTURY DROUGHT; REANALYSIS PROJECT; SOIL-MOISTURE; INHIBITION;
MODULATION
AB Flash drought refers to relatively short periods of warm surface temperature and anomalously low and rapid decreasing soil moisture (SM). Based on the physical mechanisms associated with flash droughts, these events are classified into two categories: heat wave and precipitation P deficit flash droughts. In previous work, the authors have defined heat wave flash droughts as resulting from the confluence of severe warm air temperature T-air, which increases evapotranspiration (ET), and anomalously low and decreasing SM. Here, a second type of flash drought caused by precipitation deficits is explored. The authors term these events P-deficit flash droughts, which they associate with lack of P. Precipitation deficits cause ET to decrease and temperature to increase. The P-deficit flash droughts are analyzed based on observations of P, T-air, and SM and ET reconstructed using land surface models for the period 1916-2013. The authors find that P-deficit flash droughts are more common than heat wave flash droughts. They are about twice as likely to occur as heat wave flash droughts over the conterminous United States. They are most prevalent over the southern United States with maxima over the southern Great Plains and the Southwest, in contrast to heat wave flash droughts that are mostly likely to occur over the Midwest and the Pacific Northwest, where the vegetation cover is dense.
C1 [Mo, Kingtse C.] NOAA, NWS, NCEP, Climate Predict Ctr, 5830 Univ Res Ct, College Pk, MD 20740 USA.
[Lettenmaier, Dennis P.] Univ Calif Los Angeles, Dept Geog, Los Angeles, CA 90024 USA.
RP Mo, KC (reprint author), NOAA, NWS, NCEP, Climate Predict Ctr, 5830 Univ Res Ct, College Pk, MD 20740 USA.
EM kingtse.mo@noaa.gov
FU NOAA [GC14-168A, NA14OAR4310293]
FX This project was supported by NOAA Grant GC14-168A to the NOAA/Climate
Prediction Center and by NOAA Grant NA14OAR4310293 to the University of
California, Los Angeles.
NR 32
TC 0
Z9 0
U1 12
U2 21
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 1525-755X
EI 1525-7541
J9 J HYDROMETEOROL
JI J. Hydrometeorol.
PD APR
PY 2016
VL 17
IS 4
BP 1169
EP 1184
DI 10.1175/JHM-D-15-0158.1
PG 16
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DI2GM
UT WOS:000373313700001
ER
PT J
AU Kang, DJ
Curchitser, EN
Rosati, A
AF Kang, Dujuan
Curchitser, Enrique N.
Rosati, Anthony
TI Seasonal Variability of the Gulf Stream Kinetic Energy
SO JOURNAL OF PHYSICAL OCEANOGRAPHY
LA English
DT Article
DE Models and modeling; Currents; Geographic location/entity; Numerical
analysis/modeling; Variability; Atm/Ocean Structure/ Phenomena; North
Atlantic Ocean; Seasonal variability; Eddies; Circulation/ Dynamics
ID NORTH-ATLANTIC; OCEAN CIRCULATION; EDDY ENERGY; TRANSPORT; SURFACE;
EDDIES; MODULATION; ALTIMETRY; GEOSAT; MODEL
AB The seasonal variability of the mean kinetic energy (MKE) and eddy kinetic energy (EKE) of the Gulf Stream (GS) is examined using high-resolution regional ocean model simulations. A set of three numerical experiments with different surface wind and buoyancy forcing is analyzed to investigate the mechanisms governing the seasonal cycle of upper ocean energetics. In the GS along-coast region, MKE has a significant seasonal cycle that peaks in summer, while EKE has two comparable peaks in May and September near the surface; the May peak decays rapidly with depth. In the off-coast region, MKE has a weak seasonal cycle that peaks in summer, while EKE has a dominant peak in May and a secondary peak in September near the surface. The May peak also decays with depth leaving the September peak as the only seasonal signal below 100 m. An analysis of the three numerical experiments suggests that the seasonal variability in the local wind forcing significantly impacts the September peak of the along-coast EKE through a local-flow barotropic instability process. Alternatively, the seasonal buoyancy forcing primarily impacts the flow baroclinic instability and is consequently related to the May peak of the upper ocean EKE in both regions. The analysis results indicate that the seasonal cycle of the along-coast MKE is influenced by both local energy generation by wind and the advection of energy from upstream regions. Finally, the MKE cycle and the September peak of EKE in the off-coast region are mainly affected by advection of energy from remote regions, giving rise to correlations with the seasonal cycle of remote winds.
C1 [Kang, Dujuan; Curchitser, Enrique N.] Rutgers State Univ, Dept Environm Sci, 14 Coll Farm Rd, New Brunswick, NJ 08901 USA.
[Rosati, Anthony] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA.
RP Kang, DJ (reprint author), Rutgers State Univ, Dept Environm Sci, 14 Coll Farm Rd, New Brunswick, NJ 08901 USA.
EM dujuan@esm.rutgers.edu
FU National Science Foundation [OCE-1049088, OCE-1419584, OCE-0961545];
National Oceanic and Atmospheric Administration [NOAA-NA-13OAR4830233,
NOAA-NA-15OAR4310133]
FX The authors gratefully acknowledge the support of the National Science
Foundation through Awards OCE-1049088, OCE-1419584, and OCE-0961545; and
the National Oceanic and Atmospheric Administration through Awards
NOAA-NA-13OAR4830233 and NOAA-NA-15OAR4310133. Some of the computations
were carried out at the National Center for Atmospheric Research in
Boulder, Colorado. We also thank two anonymous reviewers for their
valuable comments and suggestions.
NR 38
TC 1
Z9 1
U1 2
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 APR
PY 2016
VL 46
IS 4
BP 1189
EP 1207
DI 10.1175/JPO-D-15-0235.1
PG 19
WC Oceanography
SC Oceanography
GA DH5FZ
UT WOS:000372812800001
ER
PT J
AU Knaff, JA
Slocum, CJ
Musgrave, KD
Sampson, CR
Strahl, BR
AF Knaff, John A.
Slocum, Christopher J.
Musgrave, Kate D.
Sampson, Charles R.
Strahl, Brian R.
TI Using Routinely Available Information to Estimate Tropical Cyclone Wind
Structure
SO MONTHLY WEATHER REVIEW
LA English
DT Article
DE Satellite observations; Hurricanes/typhoons; Observational techniques
and algorithms; Atm/Ocean Structure/ Phenomena; Hurricanes; Algorithms;
Models and modeling; Diagnostics; Circulation/ Dynamics
ID SIZE ESTIMATION ALGORITHMS; WESTERN NORTH PACIFIC; INERTIAL STABILITY;
INTENSITY; SYSTEM; SHEAR; FLOW; RECONNAISSANCE; IMPROVEMENTS;
CLIMATOLOGY
AB A relatively simple method to estimate tropical cyclone (TC) wind radii from routinely available information including storm data (location, motion, and intensity) and TC size is introduced. The method is based on a combination of techniques presented in previous works and makes an assumption that TCs are largely symmetric and that asymmetries are based solely on storm motion and location. The method was applied to TC size estimates from two sources: infrared satellite imagery and global model analyses. The validation shows that the methodology is comparable with other objective methods based on the error statistics. The technique has a variety of practical research and operational applications, some of which are also discussed.
C1 [Knaff, John A.] NOAA, Ctr Satellite Applicat & Res, Ft Collins, CO 80523 USA.
[Slocum, Christopher J.] Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA.
[Musgrave, Kate D.] Colorado State Univ, Cooperat Inst Res Atmosphere, Ft Collins, CO 80523 USA.
[Sampson, Charles R.] Naval Res Lab, Monterey, CA USA.
[Strahl, Brian R.] Joint Typhoon Warning Ctr, Honolulu, HI USA.
RP Knaff, JA (reprint author), NOAA, RAMMB, CIRA CSU, Campus Delivery 1375, Ft Collins, CO 80523 USA.
EM john.knaff@noaa.gov
RI Knaff, John /F-5599-2010
OI Knaff, John /0000-0003-0427-1409
FU NOAA programs, GOES-R Risk Reduction Program; Hurricane Forecast
Improvement Program under NOAA Grant [NA17RJ1228]; NRL Base Program [PE
0601153N]
FX This research was supported by NOAA programs including the GOES-R Risk
Reduction Program, and the Hurricane Forecast Improvement Program under
NOAA Grant NA17RJ1228, and by the Chief of Naval Research through the
NRL Base Program, PE 0601153N. In addition, this work made use of
techniques developed for the Joint Hurricane Testbed and the display
capabilities of ATCF. The methods developed here were also inspired by
recent recommendations made at the WMO's Eighth International Workshop
on Tropical Cyclones geared toward two goals including: 1) the
specification of the entire TC vortex in advisories and forecasts, and
2) the development of homogeneous long-term records of tropical
cyclones. We also recognize our work is only possible because of
best-tracked wind radii and would like to encourage this practice and
the standardization of wind radii types and formats worldwide. Finally,
we thank Megan Troutman for her assistance on earlier versions of the
manuscript. The views, opinions, and findings contained in this report
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.
NR 60
TC 2
Z9 3
U1 2
U2 4
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0027-0644
EI 1520-0493
J9 MON WEATHER REV
JI Mon. Weather Rev.
PD APR
PY 2016
VL 144
IS 4
BP 1233
EP 1247
DI 10.1175/MWR-D-15-0267.1
PG 15
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DI2FV
UT WOS:000373312000001
ER
PT J
AU Klotzbach, PJ
Oliver, ECJ
Leeper, RD
Schreck, CJ
AF Klotzbach, Philip J.
Oliver, Eric C. J.
Leeper, Ronald D.
Schreck, Carl J., III
TI The Relationship between the Madden-Julian Oscillation (MJO) and
Southeastern New England Snowfall
SO MONTHLY WEATHER REVIEW
LA English
DT Article
DE Snowfall; Snow; Atm/Ocean Structure/ Phenomena; Madden-Julian
oscillation; Extratropical cyclones
ID VARIABILITY; REANALYSIS; PRECIPITATION; CIRCULATION; RAINFALL
AB The winter of 2014/15 brought record snow totals to portions of southeastern New England. Additionally, over 90% of Boston Logan Airport snowfall during the winter fell during phases 7 and 8 of the Madden-Julian oscillation (MJO) index. This motivated the authors to investigate potential connections between intense southeastern New England snowstorms and the MJO in the historical record. It was found that southeastern New England snowfall, measured since the 1930s at several stations in the region, recorded higher than average winter snowfalls when enhanced MJO convection was located over the western Pacific and the Western Hemisphere (phases 7-8). Similarly, snowfall was suppressed when enhanced MJO convection was located over the Maritime Continent (phases 4-5). The MJO also modulates the frequency of nor'easters, which contribute the majority of New England's snowfall, as measured by reanalysis-derived cyclone tracks. These tracks were more numerous during the same MJO phases that lead to enhanced snowfall, and they were less common during phases with less snowfall.
C1 [Klotzbach, Philip J.] Colorado State Univ, Dept Atmospher Sci, West LaPorte Ave, Ft Collins, CO 80523 USA.
[Oliver, Eric C. J.] Univ Tasmania, Inst Marine & Antarctic Studies, Australian Res Council Ctr Climate Syst Sci, Hobart, Tas, Australia.
[Leeper, Ronald D.; Schreck, Carl J., III] N Carolina State Univ, NOAA, Natl Ctr Environm Informat, Cooperat Inst Climate & Satellites, Asheville, NC USA.
RP Klotzbach, PJ (reprint author), Colorado State Univ, Dept Atmospher Sci, West LaPorte Ave, Ft Collins, CO 80523 USA.
EM philk@atmos.colostate.edu
RI Oliver, Eric/G-5118-2014; Schreck, Carl/B-8711-2011
OI Oliver, Eric/0000-0002-4006-2826; Schreck, Carl/0000-0001-9331-5754
FU NOAA's Climate Program Office [NA09OAR4310104]; G. Unger Vetlesen
Foundation; NOAA through the Cooperative Institute for Climate and
Satellites, North Carolina [NA14NES432003]
FX We would like to acknowledge the efforts of Scott Applequist, David
Easterling, and Ken Kunkel in the development of the extratropical
cyclone (ETC) dataset used in this study, which was funded by the NOAA's
Climate Program Office by Grant NA09OAR4310104. Klotzbach would like to
thank the G. Unger Vetlesen Foundation for financial support that helped
fund this research. Schreck and Leeper were supported by NOAA through
the Cooperative Institute for Climate and Satellites, North Carolina,
under Cooperative Agreement NA14NES432003. This paper makes a
contribution to the objectives of the Australian Research Council Centre
of Excellence for Climate System Science (ARCCCS).
NR 26
TC 0
Z9 0
U1 3
U2 9
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0027-0644
EI 1520-0493
J9 MON WEATHER REV
JI Mon. Weather Rev.
PD APR
PY 2016
VL 144
IS 4
BP 1355
EP 1362
DI 10.1175/MWR-D-15-0434.1
PG 8
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DI2FY
UT WOS:000373312300002
ER
PT J
AU Bluestein, HB
French, MM
Snyder, JC
Houser, JB
AF Bluestein, Howard B.
French, Michael M.
Snyder, Jeffrey C.
Houser, Jana B.
TI Doppler Radar Observations of Anticyclonic Tornadoes in Cyclonically
Rotating, Right-Moving Supercells
SO MONTHLY WEATHER REVIEW
LA English
DT Article
DE Storm environments; Severe storms; Mesocyclones; Atm/Ocean Structure/
Phenomena; Supercells; Tornadoes
ID SEVERE CONVECTIVE STORMS; RAPID UPDATE CYCLE; X-BAND; DUAL-DOPPLER;
SEVERE THUNDERSTORMS; HIGH-RESOLUTION; EL RENO; PHOTOGRAMMETRIC
ANALYSIS; NUMERICAL-SIMULATION; POLARIMETRIC RADAR
AB Supercells dominated by mesocyclones, which tend to propagate to the right of the tropospheric pressure-weighted mean wind, on rare occasions produce anticyclonic tornadoes at the trailing end of the rear-flank gust front. More frequently, mesoanticyclones are found at this location, most of which do not spawn any tornadoes. In this paper, four cases are discussed in which the formation of anticyclonic tornadoes was documented in the plains by mobile or fixed-site Doppler radars. These brief case studies include the analysis of Doppler radar data for tornadoes at the following dates and locations: 1) 24 April 2006, near El Reno, Oklahoma; 2) 23 May 2008, near Ellis, Kansas; 3) 18 March 2012, near Willow, Oklahoma; and 4) 31 May 2013, near El Reno, Oklahoma. Three of these tornadoes were also documented photographically. In all of these cases, a strong mesocyclone (i.e., vortex signature characterized by azimuthal shear in excess of ~5 x 10(-3) s(-1) or a 20 m s(-1) change in Doppler velocity over 5 km) or tornado was observed ~10 km away from the anticyclonic tornado. In three of these cases, the evolution of the tornadic vortex signature in time and height is described. Other features common to all cases are noted and possible mechanisms for anticyclonic tornadogenesis are identified. In addition, a set of estimated environmental parameters for these and other similar cases are discussed.
C1 [Bluestein, Howard B.] Univ Oklahoma, Sch Meteorol, 120 David L Boren Blvd,Suite 5900, Norman, OK 73072 USA.
[French, Michael M.] SUNY Stony Brook, Sch Marine & Atmospher Sci, Stony Brook, NY 11794 USA.
[Snyder, Jeffrey C.] Univ Oklahoma, Cooperat Inst Mesoscale Meteorol Studies, Norman, OK 73072 USA.
[Snyder, Jeffrey C.] NOAA, Natl Severe Storms Lab, OAR, Norman, OK 73069 USA.
[Houser, Jana B.] Ohio Univ, Dept Geog, Athens, OH 45701 USA.
RP Bluestein, HB (reprint author), Univ Oklahoma, Sch Meteorol, 120 David L Boren Blvd,Suite 5900, Norman, OK 73072 USA.
EM hblue@ou.edu
FU NSF [AGS-0934307, AGS-1262048]; NOAA/Office of Oceanic and Atmospheric
Research under NOAA-University of Oklahoma [NA11OAR4320072]; U.S.
Department of Commerce; MRI
FX This study was supported by NSF Grants AGS-0934307 and AGS-1262048;
additional funding was provided by NOAA/Office of Oceanic and
Atmospheric Research under NOAA-University of Oklahoma Cooperative
Agreement NA11OAR4320072, U.S. Department of Commerce. Robert Bluth and
Paul Buczynski from the Naval Postgraduate School and Chad Baldi from
ProSensing, Inc. provided the MWR-05XP and support for its operation and
data processing. John Meier at the Advanced Radar Research Center at the
University of Oklahoma (OU) maintained RaXPol for use during our field
experiment and OU provided matching funds for the MRI grant that funded
the construction of the radar. Helicopter videos of the anticyclonic
tornado on 24 April 2006 were taken by Mason Dunn and made available by
Gary England at KWTV Channel 9 in Oklahoma City. NCEP reanalysis data
were provided by the NOAA/OAR/ESRL PSD, Boulder, Colorado, from their
website at http://www.esrl.noaa.gov/psd/, and hodographs presented
herein were created using code modified from a script available from
http://gradsaddict.blogspot.com/. The authors thank Corey Potvin for an
early review of the manuscript and three anonymous reviewers for their
constructive comments.
NR 84
TC 3
Z9 3
U1 3
U2 5
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0027-0644
EI 1520-0493
J9 MON WEATHER REV
JI Mon. Weather Rev.
PD APR
PY 2016
VL 144
IS 4
BP 1591
EP 1616
DI 10.1175/MWR-D-15-0304.1
PG 26
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DI2GJ
UT WOS:000373313400001
ER
PT J
AU Mahoney, K
Jackson, DL
Neiman, P
Hughes, M
Darby, L
Wick, G
White, A
Sukovich, E
Cifelli, R
AF Mahoney, Kelly
Jackson, Darren L.
Neiman, Paul
Hughes, Mimi
Darby, Lisa
Wick, Gary
White, Allen
Sukovich, Ellen
Cifelli, Rob
TI Understanding the Role of Atmospheric Rivers in Heavy Precipitation in
the Southeast United States
SO MONTHLY WEATHER REVIEW
LA English
DT Article
DE Precipitation; Forecasting; Rainfall; Operational forecasting; Atm/Ocean
Structure/ Phenomena; Flood events; Extratropical cyclones
ID MESOSCALE CONVECTIVE SYSTEMS; TROPICAL MOISTURE EXPORTS; PREDECESSOR
RAIN EVENTS; WATER-VAPOR SIGNATURE; WARM CONVEYOR BELTS; SYNOPTIC-SCALE;
INLAND PENETRATION; ROCKY-MOUNTAINS; WEST-COAST; CYCLONES
AB An analysis of atmospheric rivers (ARs) as defined by an automated AR detection tool based on integrated water vapor transport (IVT) and the connection to heavy precipitation in the southeast United States (SEUS) is performed. Climatological water vapor and water vapor transport fields are compared between the U.S. West Coast (WCUS) and the SEUS, highlighting stronger seasonal variation in integrated water vapor in the SEUS and stronger seasonal variation in IVT in the WCUS. The climatological analysis suggests that IVT values above ~500 kg m(-1) s(-1) (as incorporated into an objective identification tool such as the AR detection tool used here) may serve as a sensible threshold for defining ARs in the SEUS.
Atmospheric river impacts on heavy precipitation in the SEUS are shown to vary on an annual cycle, and a connection between ARs and heavy precipitation during the nonsummer months is demonstrated. When identified ARs are matched to heavy precipitation days (>100 mm day(-1)), an average match rate of ~41% is found.
Results suggest that some aspects of an AR identification framework in the SEUS may offer benefit in forecasting heavy precipitation, particularly at medium- to longer-range forecast lead times. However, the relatively high frequency of SEUS heavy precipitation cases in which an AR is not identified necessitates additional careful consideration and incorporation of other critical aspects of heavy precipitation environments such that significant predictive skill might eventually result.
C1 [Mahoney, Kelly; Neiman, Paul; Darby, Lisa; Wick, Gary; White, Allen; Cifelli, Rob] NOAA, Earth Syst Res Lab, Div Phys Sci, Mail Code R-PSD2,325 Broadway, Boulder, CO 80305 USA.
[Jackson, Darren L.; Hughes, Mimi; Sukovich, Ellen] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Jackson, Darren L.; Hughes, Mimi; Sukovich, Ellen] NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA.
RP Mahoney, K (reprint author), NOAA, Earth Syst Res Lab, Div Phys Sci, Mail Code R-PSD2,325 Broadway, Boulder, CO 80305 USA.
EM kelly.mahoney@noaa.gov
RI Darby, Lisa/A-8037-2009; Hughes, Mimi/C-3710-2009
OI Darby, Lisa/0000-0003-1271-0643; Hughes, Mimi/0000-0002-4554-9289
FU Hurricane Sandy Supplemental Funding Award [NA14OAR4830066]; U.S.
Weather Research Program-Hydrometeorology Testbed; NOAA/ESRL/Physical
Sciences Division (PSD)
FX We gratefully acknowledge support from Hurricane Sandy Supplemental
Funding Award NA14OAR4830066, the U.S. Weather Research
Program-Hydrometeorology Testbed, and NOAA/ESRL/Physical Sciences
Division (PSD). We also value the helpful input from three anonymous
reviewers, as well as the collaboration of Benjamin Moore (SUNY-Albany),
Tom Hamill (NOAA/ESRL/PSD), Michael Brennan (NOAA/National Hurricane
Center), and Sarah Perfator, Ben Albrecht, and David Novak
(NOAA/NCEP/Weather Prediction Center).
NR 53
TC 1
Z9 1
U1 1
U2 13
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 0027-0644
EI 1520-0493
J9 MON WEATHER REV
JI Mon. Weather Rev.
PD APR
PY 2016
VL 144
IS 4
BP 1617
EP 1632
DI 10.1175/MWR-D-15-0279.1
PG 16
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DI2GJ
UT WOS:000373313400002
ER
PT J
AU Gleckler, PJ
Durack, PJ
Stouffer, RJ
Johnson, GC
Forest, CE
AF Gleckler, Peter J.
Durack, Paul J.
Stouffer, Ronald J.
Johnson, Gregory C.
Forest, Chris E.
TI Industrial-era global ocean heat uptake doubles in recent decades
SO NATURE CLIMATE CHANGE
LA English
DT Article
ID SEA-LEVEL RISE; TEMPERATURE; ABYSSAL
AB Formal detection and attribution studies have used observations and climate models to identify an anthropogenic warming signature in the upper (0-700 m) ocean(1-4). Recently, as a result of the so-called surface warming hiatus, there has been considerable interest in global ocean heat content (OHC) changes in the deeper ocean, including natural and anthropogenically forced changes identified in observational(5-7), modelling(8,9) and data re-analysis(10,11) studies. Here, we examine OHC changes in the context of the Earth's global energy budget since early in the industrial era (circa 1865-2015) for a range of depths. We rely on OHC change estimates from a diverse collection of measurement systems including data from the nineteenth-century Challenger expedition(12), a multi-decadal record of ship-based in situ mostly upper-ocean measurements, the more recent near-global Argo floats profiling to intermediate (2,000 m) depths(13), and full-depth repeated transoceanic sections(5). We show that the multi-model mean constructed from the current generation of historically forced climate models is consistent with the OHC changes from this diverse collection of observational systems. Our model-based analysis suggests that nearly half of the industrial-era increases in global OHC have occurred in recent decades, with over a third of the accumulated heat occurring below 700m and steadily rising.
C1 [Gleckler, Peter J.; Durack, Paul J.] Lawrence Livermore Natl Lab, Program Climate Model Diag & Intercomparison, 7000 East Ave, Livermore, CA 94550 USA.
[Stouffer, Ronald J.] Princeton Univ, Geophys Fluid Dynam Lab, Forrestal Campus,201 Forrestal Rd, Princeton, NJ 08540 USA.
[Johnson, Gregory C.] NOAA, Pacific Marine Environm Lab, 7600 Sand Point Way NE, Seattle, WA 98115 USA.
[Forest, Chris E.] Penn State Univ, Dept Meteorol, State Coll, PA 16802 USA.
[Forest, Chris E.] Penn State Univ, Dept Geosci, State Coll, PA 16802 USA.
[Forest, Chris E.] Penn State Univ, Earth & Environm Syst Inst, State Coll, PA 16802 USA.
RP Gleckler, PJ (reprint author), Lawrence Livermore Natl Lab, Program Climate Model Diag & Intercomparison, 7000 East Ave, Livermore, CA 94550 USA.
EM gleckler1@llnl.gov
RI Johnson, Gregory/I-6559-2012; Forest, Chris/M-1993-2014; Durack,
Paul/A-8758-2010
OI Johnson, Gregory/0000-0002-8023-4020; Forest, Chris/0000-0002-2643-0186;
Durack, Paul/0000-0003-2835-1438
FU US Department of Energy, Office of Science, Office of Biological and
Environmental Research [DE-SC0004956, DEFG02-94ER61937]; National
Science Foundation through the Network for Sustainable Climate Risk
Management (SCRiM) under NSF [GEO-1240507]; NOAA; NOAA Ocean Climate
Observations Program; [DE-AC52-07NA27344]
FX The work of P.J.G. and P.J.D., from Lawrence Livermore National
Laboratory, is a contribution to the US Department of Energy, Office of
Science, Climate and Environmental Sciences Division, Regional and
Global Climate Modeling Program under contract DE-AC52-07NA27344. C.E.F.
was partially supported by the US Department of Energy, Office of
Science, Office of Biological and Environmental Research, grants
DE-SC0004956 (as a member of the International Detection and Attribution
Working Group (IDAG)) and DEFG02-94ER61937 and by the National Science
Foundation through the Network for Sustainable Climate Risk Management
(SCRiM) under NSF cooperative agreement GEO-1240507. G.C.J. is supported
by NOAA Research and the NOAA Ocean Climate Observations Program. We
thank K. Taylor, B. Santer and J. Gregory for their helpful suggestions
concerning our analysis. We acknowledge the sources of observed data
used in this study: C. M. Domingues, M. Ishii and M. Kimoto, S. Levitus
and T. Boyer, S. Purkey and G. Johnson, D. Roemmich and J. Gilson, S.
Hosoda, T. Ohira and T. Nakamura and the International Pacific Research
Center. We thank the climate modelling groups (listed in Supplementary
Table 1) for producing and making available their model output.
NR 37
TC 8
Z9 9
U1 12
U2 38
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 1758-678X
EI 1758-6798
J9 NAT CLIM CHANGE
JI Nat. Clim. Chang.
PD APR
PY 2016
VL 6
IS 4
BP 394
EP +
DI 10.1038/NCLIMATE2915
PG 6
WC Environmental Sciences; Environmental Studies; Meteorology & Atmospheric
Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA DH8QI
UT WOS:000373060000017
ER
PT J
AU Smith, NG
Malyshev, SL
Shevliakova, E
Kattge, J
Dukes, JS
AF Smith, Nicholas G.
Malyshev, Sergey L.
Shevliakova, Elena
Kattge, Jens
Dukes, Jeffrey S.
TI Foliar temperature acclimation reduces simulated carbon sensitivity to
climate
SO NATURE CLIMATE CHANGE
LA English
DT Article
ID NET ECOSYSTEM EXCHANGE; THERMAL-ACCLIMATION; BIOCHEMICAL-MODEL;
VEGETATION MODELS; PLANT RESPIRATION; PHOTOSYNTHESIS; ASSIMILATION;
FLUXES; CO2
AB Plant photosynthesis and respiration are the largest carbon fluxes between the terrestrial biosphere and the atmosphere(1), and their parameterizations represent large sources of uncertainty in projections of land carbon uptake in Earth system models(2,3) (ESMs). The incorporation of temperature acclimation of photosynthesis and foliar respiration, commonly observed processes, into ESMs has been proposed as a way to reduce this uncertainty(2). Here we show that, across 15 flux tower sites spanning multiple biomes at various locations worldwide (10 degrees S-67 degrees N), acclimation parameterizations(4,5) improve a model's ability to reproduce observed net ecosystem exchange of CO2. This improvement is most notable in tropical biomes, where photosynthetic acclimation increased model performance by 36%. The consequences of acclimation for simulated terrestrial carbon uptake depend on the process, region and time period evaluated. Globally, including acclimation has a net effect of increasing carbon assimilation and storage, an effect that diminishes with time, but persists well into the future. Our results suggest that land models omitting foliar temperature acclimation are likely to overestimate the temperature sensitivity of terrestrial carbon exchange, thus biasing projections of future carbon storage and estimates of policy indicators such as the transient climate response to cumulative carbon emissions(1).
C1 [Smith, Nicholas G.; Dukes, Jeffrey S.] Purdue Univ, Dept Biol Sci, W Lafayette, IN 47907 USA.
[Malyshev, Sergey L.; Shevliakova, Elena] Princeton Univ, Princeton, NJ 08540 USA.
[Malyshev, Sergey L.; Shevliakova, Elena] Cooperat Inst Climate Studies, Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA.
[Kattge, Jens] Max Planck Inst Biogeochem, D-07745 Jena, Germany.
[Kattge, Jens] German Ctr Integrat Biodivers Res Halle Jena Leip, D-04103 Leipzig, Germany.
[Dukes, Jeffrey S.] Purdue Univ, Dept Forestry & Nat Resources, W Lafayette, IN 47907 USA.
RP Smith, NG (reprint author), Purdue Univ, Dept Biol Sci, W Lafayette, IN 47907 USA.
EM ngsmith@purdue.edu
RI Dukes, Jeffrey/C-9765-2009; Kattge, Jens/J-8283-2016; Smith,
Nicholas/B-7126-2015
OI Dukes, Jeffrey/0000-0001-9482-7743; Kattge, Jens/0000-0002-1022-8469;
Smith, Nicholas/0000-0001-7048-4387
FU INTERFACE RCN (NSF) [DEB-0955771]; Purdue Climate Change Research
Center; NASA Earth and Space Science fellowship [NNX13AN65H]; National
Oceanic and Atmospheric (US Department of Commerce) [NAOSOAR4320752]; US
Department of Energy, Biological and Environmental Research, Terrestrial
Carbon Program [DE-FG02-04ER63917, DE-FG02-04ER63911]; CFCAS; NSERC;
BIOCAP; Environment Canada; NRCan; LBA; CarboEuropeIP; FAO-GTOS-TCO;
iLEAPS; Max Planck Institute for Biogeochemistry; National Science
Foundation; University of Tuscia; Universite Laval; US Department of
Energy
FX This project was supported by student exchange funding for N.G.S.
provided by the INTERFACE RCN (NSF DEB-0955771), a Purdue Climate Change
Research Center graduate fellowship to N.G.S., and a NASA Earth and
Space Science fellowship to N.G.S. (NNX13AN65H). S.L.M. acknowledges
support from the National Oceanic and Atmospheric (US Department of
Commerce) Grant NAOSOAR4320752. This work used eddy-covariance data
acquired by the FLUXNET community and in particular by the following
networks: AmeriFlux (US Department of Energy, Biological and
Environmental Research, Terrestrial Carbon Program (DE-FG02-04ER63917
and DE-FG02-04ER63911)), CarboEuropeIP, Fluxnet-Canada (supported by
CFCAS, NSERC, BIOCAP, Environment Canada, and NRCan), and LBA. We
acknowledge the financial support to the eddy-covariance data
harmonization provided by CarboEuropeIP, FAO-GTOS-TCO, iLEAPS, Max
Planck Institute for Biogeochemistry, National Science Foundation,
University of Tuscia, Universite Laval, Environment Canada and US
Department of Energy and the database development and technical support
from Berkeley Water Center, Lawrence Berkeley National Laboratory,
Microsoft Research eScience, Oak Ridge National Laboratory, University
of California-Berkeley and the University of Virginia. This is
publication 1605 of the Purdue Climate Change Research Center.
NR 33
TC 4
Z9 4
U1 8
U2 23
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 1758-678X
EI 1758-6798
J9 NAT CLIM CHANGE
JI Nat. Clim. Chang.
PD APR
PY 2016
VL 6
IS 4
BP 407
EP +
DI 10.1038/NCLIMATE2878
PG 7
WC Environmental Sciences; Environmental Studies; Meteorology & Atmospheric
Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA DH8QI
UT WOS:000373060000020
ER
PT J
AU Pan, LD
Laurita, NJ
Ross, KA
Gaulin, BD
Armitage, NP
AF Pan, LiDong
Laurita, N. J.
Ross, Kate A.
Gaulin, Bruce D.
Armitage, N. P.
TI A measure of monopole inertia in the quantum spin ice Yb2Ti2O7
SO NATURE PHYSICS
LA English
DT Article
ID FRUSTRATED MAGNETS; MODEL
AB An important and continuing theme of modern solid state physics is the realization of exotic excitations in materials, known as quasiparticles, that have no analogy in the actual physical vacuum of free space. Although they are not fundamental, such quasiparticles do constitute the most basic description of the excited states of the 'vacuum' in which they reside. In this regard the magnetic textures of the excited states of spin ices, magnetic pyrochlore oxides with dominant Ising interactions, have been proposed to behave as effective magnetic charge monopoles. Inelastic neutron scattering experiments have established the pyrochlore material Yb2Ti2O7 (YbTO) as a quantum spin ice, where, in addition to the Ising interactions, there are substantial transverse terms that may induce quantum dynamics and-in principle-coherent monopole motion. Here we report a combined time-domain terahertz spectroscopy (TDTS) and microwave cavity study of YbTO to probe its complex dynamic magnetic susceptibility. We find that the form of the susceptibility is consistent with that of a monopole gas, and a magnetic monopole conductivity can be defined and measured. Using the phase sensitive capabilities of these techniques, we observe a sign change in the reactive part of the magnetic response. In generic models of magnetic excitations this is possible only by introducing inertial effects, such as a mass-dependent term, to the equations of motion. Analogous to conventional electric charge systems, measurement of the conductivity's spectral weight allows us to derive a value for the magnetic monopole mass. Our results support the idea of magnetic monopoles of quantum spin ice as the true coherently propagating quasiparticles of this system.
C1 [Pan, LiDong; Laurita, N. J.; Ross, Kate A.; Armitage, N. P.] Johns Hopkins Univ, Dept Phys & Astron, Inst Quantum Matter, Baltimore, MD 21218 USA.
[Ross, Kate A.] NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Gaulin, Bruce D.] McMaster Univ, Dept Phys & Astron, Hamilton, ON L8S 4M1, Canada.
[Gaulin, Bruce D.] McMaster Univ, Brockhouse Inst Mat Res, Hamilton, ON L8S 4M1, Canada.
[Gaulin, Bruce D.] Canadian Inst Adv Res, 180 Dundas St W, Toronto, ON M5G 1Z8, Canada.
RP Armitage, NP (reprint author), Johns Hopkins Univ, Dept Phys & Astron, Inst Quantum Matter, Baltimore, MD 21218 USA.
EM npa@pha.jhu.edu
FU Gordon and Betty Moore Foundation [GBMF2628]; DOE [DE-FG02-08ER46544];
ARCS Foundation; NSERC
FX This work at JHU was supported by the Gordon and Betty Moore Foundation
through Grant GBMF2628 to N.P.A. The microwave cavity work was supported
by the DOE through DE-FG02-08ER46544. N.J.L. had additional support
through the ARCS Foundation. The crystal growth work at Mcmaster was
supported by NSERC. We would like to thank L. Balents, C. Broholm, N.
Drichko, M. Gingras, Z. Hao, S. M. Koohpayeh, J. Lynn, G. Luke, M.
Mourigal, M. Robbins, L. Savary, R Singh, O. Tchernyshyov, M. Valentine
and Y. Wan for helpful conversations and E. Kermarrec for help with the
crystal preparation.
NR 34
TC 9
Z9 9
U1 16
U2 41
PU NATURE PUBLISHING GROUP
PI LONDON
PA MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND
SN 1745-2473
EI 1745-2481
J9 NAT PHYS
JI Nat. Phys.
PD APR
PY 2016
VL 12
IS 4
BP 361
EP U97
DI 10.1038/NPHYS3608
PG 7
WC Physics, Multidisciplinary
SC Physics
GA DI1AB
UT WOS:000373227300023
ER
PT J
AU Lamouroux, J
Charria, G
De Mey, P
Raynaud, S
Heyraud, C
Craneguy, P
Dumas, F
Le Henaff, M
AF Lamouroux, Julien
Charria, Guillaume
De Mey, Pierre
Raynaud, Stephane
Heyraud, Catherine
Craneguy, Philippe
Dumas, Franck
Le Henaff, Matthieu
TI Objective assessment of the contribution of the RECOPESCA network to the
monitoring of 3D coastal ocean variables in the Bay of Biscay and the
English Channel
SO OCEAN DYNAMICS
LA English
DT Article
DE Design of in situ observation network; Bay of Biscay; English Channel;
Performance assessment; Model errors
ID DIURNAL INTERNAL TIDES; CONTINENTAL-SHELF; INVERSE METHODS; MODEL
ERRORS; DYNAMICS; UNCERTAINTIES; ASSIMILATION; CIRCULATION; CURRENTS;
SYSTEM
AB In the Bay of Biscay and the English Channel, in situ observations represent a key element to monitor and to understand the wide range of processes in the coastal ocean and their direct impacts on human activities. An efficient way to measure the hydrological content of the water column over the main part of the continental shelf is to consider ships of opportunity as the surface to cover is wide and could be far from the coast. In the French observation strategy, the RECOPESCA programme, as a component of the High frequency Observation network for the environment in coastal SEAs (HOSEA), aims to collect environmental observations from sensors attached to fishing nets. In the present study, we assess that network using the Array Modes (ArM) method (a stochastic implementation of Le H,naff et al. Ocean Dyn 59: 3-20. doi: 10.1007/s10236-008-0144-7, 2009). That model ensemble-based method is used here to compare model and observation errors and to quantitatively evaluate the performance of the observation network at detecting prior (model) uncertainties, based on hypotheses on error sources. A reference network, based on fishing vessel observations in 2008, is assessed using that method. Considering the various seasons, we show the efficiency of the network at detecting the main model uncertainties. Moreover, three scenarios, based on the reference network, a denser network in 2010 and a fictive network aggregated from a pluri-annual collection of profiles, are also analysed. Our sensitivity study shows the importance of the profile positions with respect to the sheer number of profiles for ensuring the ability of the network to describe the main error modes. More generally, we demonstrate the capacity of this method, with a low computational cost, to assess and to design new in situ observation networks.
C1 [Lamouroux, Julien] NOVELTIS, 153 Rue Lac, F-31670 Labege, France.
[Lamouroux, Julien] Mercator Ocean, 8-10 Rue Hermes, F-31520 Romainville St Agne, France.
[Charria, Guillaume] Univ Brest, IFREMER, CNRS, IRD,Lab Oceanog Phys & Spatiale,IUEM, F-29280 Brest, France.
[De Mey, Pierre] CNRS, LEGOS, UMR 5566, 18 Av Edouard Belin, F-31401 Toulouse 9, France.
[Raynaud, Stephane; Heyraud, Catherine; Craneguy, Philippe] ACTIMAR, 36 Quai Douane, F-29200 Brest, France.
[Dumas, Franck] SHOM, HOM, 13 Rue Chatellier, F-29200 Brest, France.
[Le Henaff, Matthieu] Univ Miami, Cooperat Inst Marine & Atmospher Studies, 4600 Rickenbacker Causeway, Miami, FL 33149 USA.
[Le Henaff, Matthieu] NOAA, Atlantic Oceanog & Meteorol Lab, 4301 Rickenbacker Causeway, Miami, FL 33149 USA.
RP Charria, G (reprint author), Univ Brest, IFREMER, CNRS, IRD,Lab Oceanog Phys & Spatiale,IUEM, F-29280 Brest, France.
EM Julien.Lamouroux@mercator-ocean.fr; Guillaume.Charria@ifremer.fr
OI Charria, Guillaume/0000-0001-5204-1654
FU PREVIMER project; FP7 JERICO (WP9) project; FP7 SANGOMA project
[FP7-SPACE-2011-283580]; base funds of NOAA Atlantic Oceanographic and
Meteorological Laboratory
FX This study has been undertaken in the frame and with the financial
support of the PREVIMER project, the FP7 JERICO (WP9) project, and the
FP7 SANGOMA project (FP7-SPACE-2011-283580). M. Le Henaff received
partial support for this work from the base funds of the NOAA Atlantic
Oceanographic and Meteorological Laboratory. It has also been conducted
as a contribution to the GODAE OceanView Coastal Ocean and Shelf Seas
Task Team (COSS-TT). We would like to thank Emilie Leblond and Patrick
Berthou for leading the RECOPESCA programme, Loic Quemener and Michel
Repecaud for operating the network, and the voluntary fishermen who have
accepted to join the RECOPESCA network. We also thank the technical team
of RECOPESCA, especially Matthieu Bourbigot, and the observers of the
Ifremer Fisheries Information System. The data from the EUMETSAT
Satellite Application Facility on Ocean and Sea Ice is accessible
through the SAF's homepage: http://www.osi-saf.org. We are grateful to
the two anonymous referees and the Associate Editor Emil Vassilev Stanev
for their very fruitful and constructive comments on this manuscript.
NR 35
TC 1
Z9 1
U1 1
U2 4
PU SPRINGER HEIDELBERG
PI HEIDELBERG
PA TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY
SN 1616-7341
EI 1616-7228
J9 OCEAN DYNAM
JI Ocean Dyn.
PD APR
PY 2016
VL 66
IS 4
BP 567
EP 588
DI 10.1007/s10236-016-0938-y
PG 22
WC Oceanography
SC Oceanography
GA DH9NQ
UT WOS:000373123300008
ER
PT J
AU Srivastava, PK
Han, DW
Islam, T
Petropoulos, GP
Gupta, M
Dai, Q
AF Srivastava, Prashant K.
Han, Dawei
Islam, Tanvir
Petropoulos, George P.
Gupta, Manika
Dai, Qiang
TI Seasonal evaluation of evapotranspiration fluxes from MODIS satellite
and mesoscale model downscaled global reanalysis datasets
SO THEORETICAL AND APPLIED CLIMATOLOGY
LA English
DT Article
ID SMOS SOIL-MOISTURE; CROP EVAPOTRANSPIRATION; INCREMENTAL APPROACH; WRF
MODEL; VALIDATION; PERFORMANCE; ALGORITHM; PRODUCTS; SURFACES; FUTURE
AB Reference evapotranspiration (ETo) is an important variable in hydrological modeling, which is not always available, especially for ungauged catchments. Satellite data, such as those available from the MODerate Resolution Imaging Spectroradiometer (MODIS), and global datasets via the European Centre for Medium Range Weather Forecasts (ECMWF) reanalysis (ERA) interim and National Centers for Environmental Prediction (NCEP) reanalysis are important sources of information for ETo. This study explored the seasonal performances of MODIS (MOD16) and Weather Research and Forecasting (WRF) model downscaled global reanalysis datasets, such as ERA interim and NCEP-derived ETo, against ground-based datasets. Overall, on the basis of the statistical metrics computed, ETo derived from ERA interim and MODIS were more accurate in comparison to the estimates from NCEP for all the seasons. The pooled datasets also revealed a similar performance to the seasonal assessment with higher agreement for the ERA interim (r = 0.96, RMSE = 2.76 mm/8 days; bias = 0.24 mm/8 days), followed by MODIS (r = 0.95, RMSE = 7.66 mm/8 days; bias = -7.17 mm/8 days) and NCEP (r = 0.76, RMSE = 11.81 mm/8 days; bias = -10.20 mm/8 days). The only limitation with downscaling ERA interim reanalysis datasets using WRF is that it is time-consuming in contrast to the readily available MODIS operational product for use in mesoscale studies and practical applications.
C1 [Srivastava, Prashant K.] NASA, Goddard Space Flight Ctr, Hydrol Sci, Greenbelt, MD 20771 USA.
[Srivastava, Prashant K.] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20742 USA.
[Srivastava, Prashant K.; Han, Dawei; Islam, Tanvir; Dai, Qiang] Univ Bristol, Dept Civil Engn, Bristol, Avon, England.
[Islam, Tanvir] NOAA, NESDIS, Ctr Satellite Applicat & Res, College Pk, MD 20740 USA.
[Islam, Tanvir] Colorado State Univ, Cooperat Inst Res Atmosphere, Ft Collins, CO 80523 USA.
[Petropoulos, George P.] Aberystwyth Univ, Dept Geog & Earth Sci, Aberystwyth SY23 3DB, Dyfed, Wales.
[Gupta, Manika] IIT, Dept Civil Engn, Water Resources, Delhi 110016, India.
RP Srivastava, PK (reprint author), NASA, Goddard Space Flight Ctr, Hydrol Sci, Greenbelt, MD 20771 USA.; Srivastava, PK (reprint author), Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20742 USA.; Srivastava, PK (reprint author), Univ Bristol, Dept Civil Engn, Bristol, Avon, England.
EM prashant.k.srivastava@nasa.gov
RI Petropoulos, George/F-2384-2013;
OI Petropoulos, George/0000-0003-1442-1423; Islam,
Tanvir/0000-0003-2429-3074
FU Commonwealth Scholarship Commission; British Council, UK; Ministry of
Human Resource Development, Government of India
FX The authors would like to thank the Commonwealth Scholarship Commission,
British Council, UK and the Ministry of Human Resource Development,
Government of India for providing the necessary support and funding for
this research. The authors would like to acknowledge the British
Atmospheric Data Centre, UK for providing the ground datasets. The
author also acknowledges the Advanced Computing Research Centre at
University of Bristol for providing the access to supercomputer facility
(The Blue Crystal) for some of the analysis. Dr. Petropoulos's
contribution was supported by the European Commission Marie Curie
Re-Integration Grant "TRANSFORM-EO" project. Authors would also like to
thank Gareth Ireland for the language proof reading of the manuscript.
The views expressed here are those of the authors solely and do not
constitute a statement of policy, decision, or position on behalf of
NOAA/NASA or the authors' affiliated institutions.
NR 52
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U1 5
U2 12
PU SPRINGER WIEN
PI WIEN
PA SACHSENPLATZ 4-6, PO BOX 89, A-1201 WIEN, AUSTRIA
SN 0177-798X
EI 1434-4483
J9 THEOR APPL CLIMATOL
JI Theor. Appl. Climatol.
PD APR
PY 2016
VL 124
IS 1-2
BP 461
EP 473
DI 10.1007/s00704-015-1430-1
PG 13
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DH9VH
UT WOS:000373143600035
ER
PT J
AU Ortiz-Montalvo, DL
Schwier, AN
Lim, YB
McNeill, VF
Turpin, BJ
AF Ortiz-Montalvo, Diana L.
Schwier, Allison N.
Lim, Yong B.
McNeill, V. Faye
Turpin, Barbara J.
TI Volatility of methylglyoxal cloud SOA formed through OH radical
oxidation and droplet evaporation
SO ATMOSPHERIC ENVIRONMENT
LA English
DT Article
DE Methylglyoxal; Secondary organic aerosol (SOA); Cloud processing; OH
radical oxidation; Droplet evaporation; Volatility
ID SECONDARY ORGANIC AEROSOL; AQUEOUS PARTICLES; INORGANIC SALTS; GLYOXAL;
CHEMISTRY; VAPORIZATION; PREDICTION; PHASE; ACIDS; PHOTOCHEMISTRY
AB The volatility of secondary organic aerosol (SOA) formed through cloud processing (aqueous hydroxyl radical (OH) oxidation and droplet evaporation) of methylglyoxal (MGly) was studied. Effective vapor pressure and effective enthalpy of vaporization (Delta H-vap,H-eff) were determined using 1) droplets containing MGly and its oxidation products, 2) a Vibrating Orifice Aerosol Generator (VOAG) system, and 3) Temperature Programmed Desorption Aerosol-Chemical Ionization Mass Spectrometry (TPD Aerosol-CIMS). Simulated in-cloud MGly oxidation (for 10-30 min) produces an organic mixture of higher and lower volatility components with an overall effective vapor pressure of (4 +/- 7) x 10(-7) atm at pH 3. The effective vapor pressure decreases by a factor of 2 with addition of ammonium hydroxide (pH 7). The fraction of organic material remaining in the particle-phase after drying was smaller than for similar experiments with glycolaldehyde and glyoxal SOA. The Delta H-vap,H-eff of pyruvic acid and oxalic acid + methylglyoxal in the mixture (from TPD Aerosol-CIMS) were smaller than the theoretical enthalpies of the pure compounds and smaller than that estimated for the entire precursor/product mix after droplet evaporation. After 10 (even neutralized) will volatilize during droplet evaporation; neutralization and at least 80 min of oxidation at 10(-12) M (OH)-O-center dot (or >12 h at 10(-14) M) is needed before low volatility ammonium oxalate exceeds pyruvate. (C) 2015 Elsevier Ltd. All rights reserved.
C1 [Ortiz-Montalvo, Diana L.; Lim, Yong B.] Rutgers State Univ, Environm Sci, New Brunswick, NJ 08903 USA.
[Schwier, Allison N.; McNeill, V. Faye] Columbia Univ, Chem Engn, New York, NY USA.
[Lim, Yong B.] Korea Inst Sci & Technol, Ctr Environm Hlth & Welf Res, Seoul 02792, South Korea.
[Turpin, Barbara J.] Univ N Carolina, Environm Sci & Engn, Chapel Hill, NC USA.
[Ortiz-Montalvo, Diana L.] NIST, Gaithersburg, MD 20899 USA.
RP Turpin, BJ (reprint author), Univ N Carolina, Environm Sci & Engn, Chapel Hill, NC USA.
EM bjturpin@email.unc.edu
RI Lim, Yong/A-5310-2013;
OI Lim, Yong/0000-0001-5000-5991; Ortiz-Montalvo, Diana/0000-0001-7293-4476
FU Ford Foundation Dissertation Fellowship Award; Air Pollution Educational
and Research Grant, Mid-Atlantic States Section of Air and Waste
Management Association; Department of Education, Graduate Assistance in
Areas of National Need [P200A060156]; National Science Foundation
[ATM-0630298]; National Oceanic and Atmospheric Association
[NA07OAR4310279]; US Environmental Protection Agency Science To Achieve
Results [RD-83375101-0]; New Jersey Agricultural Experiment Station;
USDA-NIFA; NASA Tropospheric Chemistry [NNX09AF26G]
FX This research was supported, in part, by a Ford Foundation Dissertation
Fellowship Award; Air Pollution Educational and Research Grant,
Mid-Atlantic States Section of Air and Waste Management Association;
Department of Education, Graduate Assistance in Areas of National Need
(P200A060156); National Science Foundation (ATM-0630298), National
Oceanic and Atmospheric Association (NA07OAR4310279), US Environmental
Protection Agency Science To Achieve Results (RD-83375101-0), New Jersey
Agricultural Experiment Station; USDA-NIFA. VFM and ANS acknowledge
support of NASA Tropospheric Chemistry (NNX09AF26G). This research was
not subjected to government agency review. It does not necessarily
reflect views of any government agency. No official endorsement should
be inferred.
NR 48
TC 1
Z9 1
U1 18
U2 25
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 1352-2310
EI 1873-2844
J9 ATMOS ENVIRON
JI Atmos. Environ.
PD APR
PY 2016
VL 130
SI SI
BP 145
EP 152
DI 10.1016/j.atmosenv.2015.12.013
PG 8
WC Environmental Sciences; Meteorology & Atmospheric Sciences
SC Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences
GA DG9CU
UT WOS:000372381200016
ER
PT J
AU DeLorenzo, ME
Brooker, J
Chung, KW
Kelly, M
Martinez, J
Moore, JG
Thomas, M
AF DeLorenzo, M. E.
Brooker, J.
Chung, K. W.
Kelly, M.
Martinez, J.
Moore, J. G.
Thomas, M.
TI Exposure of the grass shrimp, Palaemonetes pugio, to antimicrobial
compounds affects associated Vibrio bacterial density and development of
antibiotic resistance
SO ENVIRONMENTAL TOXICOLOGY
LA English
DT Article
DE antibiotics; triclosan; shrimp; Vibrio; toxicity; resistance
ID VETERINARY ANTIBIOTICS; AQUATIC ENVIRONMENT; HUMAN HEALTH; TRICLOSAN;
WATER; PHARMACEUTICALS; TOXICITY; OXYTETRACYCLINE; VULNIFICUS; MECHANISM
AB Antimicrobial compounds are widespread, emerging contaminants in the aquatic environment and may threaten ecosystem and human health. This study characterized effects of antimicrobial compounds common to human and veterinary medicine, aquaculture, and consumer personal care products [erythromycin (ERY), sulfamethoxazole (SMX), oxytetracycline (OTC), and triclosan (TCS)] in the grass shrimp Palaemonetes pugio. The effects of antimicrobial treatments on grass shrimp mortality and lipid peroxidation activity were measured. The effects of antimicrobial treatments on the bacterial community of the shrimp were then assessed by measuring Vibrio density and testing bacterial isolates for antibiotic resistance. TCS (0.33 mg/L) increased shrimp mortality by 37% and increased lipid peroxidation activity by 63%. A mixture of 0.33 mg/L TCS and 60 mg/L SMX caused a 47% increase in shrimp mortality and an 88% increase in lipid peroxidation activity. Exposure to SMX (30 mg/L or 60 mg/L) alone and to a mixture of SMX/ERY/OTC did not significantly affect shrimp survival or lipid peroxidation activity. Shrimp exposure to 0.33 mg/L TCS increased Vibrio density 350% as compared to the control whereas SMX, the SMX/TCS mixture, and the mixture of SMX/ERY/OTC decreased Vibrio density 78-94%. Increased Vibrio antibiotic resistance was observed for all shrimp antimicrobial treatments except for the mixture of SMX/ERY/OTC. Approximately 87% of grass shrimp Vibrio isolates displayed resistance to TCS in the control treatment suggesting a high level of TCS resistance in environmental Vibrio populations. The presence of TCS in coastal waters may preferentially increase the resistance and abundance of pathogenic bacteria. These results indicate the need for further study into the potential interactions between antimicrobials, aquatic organisms, and associated bacterial communities. (c) 2014 Wiley Periodicals, Inc. Environ Toxicol 31: 469-477, 2016.
C1 [DeLorenzo, M. E.; Chung, K. W.; Moore, J. G.] NOAA, Natl Ocean Serv, Natl Ctr Coastal Ocean Sci, Ctr Coastal Environm Hlth & Biomol Res, Charleston, SC 29412 USA.
[Brooker, J.; Kelly, M.; Martinez, J.; Thomas, M.] Coll Charleston, Dept Biol, Charleston, SC 29412 USA.
RP DeLorenzo, ME (reprint author), NOAA, Natl Ocean Serv, Natl Ctr Coastal Ocean Sci, Ctr Coastal Environm Hlth & Biomol Res, Charleston, SC 29412 USA.
EM marie.delorenzo@noaa.gov
FU National Science Foundation [DBI-1062990]; Medical University of South
Carolina MBES Program, NOAA
FX Contract grant sponsor: National Science Foundation.; Contract grant
number: DBI-1062990.; Contract grant sponsor: Medical University of
South Carolina MBES Program, NOAA.
NR 50
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Z9 0
U1 6
U2 11
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 1520-4081
EI 1522-7278
J9 ENVIRON TOXICOL
JI Environ. Toxicol.
PD APR
PY 2016
VL 31
IS 4
BP 469
EP 477
DI 10.1002/tox.22060
PG 9
WC Environmental Sciences; Toxicology; Water Resources
SC Environmental Sciences & Ecology; Toxicology; Water Resources
GA DG8FL
UT WOS:000372318300009
PM 25348372
ER
PT J
AU Chuang, MC
Hwang, JN
Williams, K
AF Chuang, Meng-Che
Hwang, Jenq-Neng
Williams, Kresimir
TI A Feature Learning and Object Recognition Framework for Underwater Fish
Images
SO IEEE TRANSACTIONS ON IMAGE PROCESSING
LA English
DT Article
DE Feature learning; fish species identification; object recognition;
underwater imagery; unsupervised learning
ID PARTIAL CLASSIFICATION; MEAN-SHIFT; TRACKING; SYSTEM; SPACE
AB Live fish recognition is one of the most crucial elements of fisheries survey applications where the vast amount of data is rapidly acquired. Different from general scenarios, challenges to underwater image recognition are posted by poor image quality, uncontrolled objects and environment, and difficulty in acquiring representative samples. In addition, most existing feature extraction techniques are hindered from automation due to involving human supervision. Toward this end, we propose an underwater fish recognition framework that consists of a fully unsupervised feature learning technique and an error-resilient classifier. Object parts are initialized based on saliency and relaxation labeling to match object parts correctly. A non-rigid part model is then learned based on fitness, separation, and discrimination criteria. For the classifier, an unsupervised clustering approach generates a binary class hierarchy, where each node is a classifier. To exploit information from ambiguous images, the notion of partial classification is introduced to assign coarse labels by optimizing the benefit of indecision made by the classifier. Experiments show that the proposed framework achieves high accuracy on both public and self-collected underwater fish images with high uncertainty and class imbalance.
C1 [Chuang, Meng-Che; Hwang, Jenq-Neng] Univ Washington, Dept Elect Engn, Seattle, WA 98195 USA.
[Williams, Kresimir] NOAA, Alaska Fisheries Sci Ctr, Seattle, WA 98115 USA.
RP Chuang, MC; Hwang, JN (reprint author), Univ Washington, Dept Elect Engn, Seattle, WA 98195 USA.; Williams, K (reprint author), NOAA, Alaska Fisheries Sci Ctr, Seattle, WA 98115 USA.
EM mengche@uw.edu; hwang@uw.edu; kresimir.williams@noaa.gov
FU National Marine Fisheries Services' Advanced Sampling Technology Working
Group; National Oceanic and Atmospheric Administration, Seattle, WA, USA
FX This work was supported in part by the National Marine Fisheries
Services' Advanced Sampling Technology Working Group and in part by the
National Oceanic and Atmospheric Administration, Seattle, WA, USA. The
associate editor coordinating the review of this manuscript and
approving it for publication was Prof. Peter Tay.
NR 37
TC 0
Z9 0
U1 7
U2 16
PU IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
PI PISCATAWAY
PA 445 HOES LANE, PISCATAWAY, NJ 08855-4141 USA
SN 1057-7149
EI 1941-0042
J9 IEEE T IMAGE PROCESS
JI IEEE Trans. Image Process.
PD APR
PY 2016
VL 25
IS 4
BP 1862
EP 1872
DI 10.1109/TIP.2016.2535342
PG 11
WC Computer Science, Artificial Intelligence; Engineering, Electrical &
Electronic
SC Computer Science; Engineering
GA DH2WN
UT WOS:000372648000009
PM 26930683
ER
PT J
AU Dirmeyer, PA
Wu, JX
Norton, HE
Dorigo, WA
Quiring, SM
Ford, TW
Santanello, JA
Bosilovich, MG
Ek, MB
Koster, RD
Balsamo, G
Lawrence, DM
AF Dirmeyer, Paul A.
Wu, Jiexia
Norton, Holly E.
Dorigo, Wouter A.
Quiring, Steven M.
Ford, Trenton W.
Santanello, Joseph A., Jr.
Bosilovich, Michael G.
Ek, Michael B.
Koster, Randal D.
Balsamo, Gianpaolo
Lawrence, David M.
TI Confronting Weather and Climate Models with Observational Data from Soil
Moisture Networks over the United States
SO JOURNAL OF HYDROMETEOROLOGY
LA English
DT Article
DE Reanalysis data; Land surface model; Geographic location/entity; Soil
moisture; Climate models; Instrumentation/sensors; Physical Meteorology
and Climatology; North America; Models and modeling; Observational
techniques and algorithms
ID DATA ASSIMILATION SYSTEM; LAND-SURFACE MODELS; REANALYSIS DATA SET;
SPATIAL VARIABILITY; TRIPLE COLLOCATION; COUPLING STRENGTH; OBSERVING
SYSTEM; PERFORMANCE; VALIDATION; MESONET
AB Four land surface models in uncoupled and coupled configurations are compared to observations of daily soil moisture from 19 networks in the conterminous United States to determine the viability of such comparisons and explore the characteristics of model and observational data. First, observations are analyzed for error characteristics and representation of spatial and temporal variability. Some networks have multiple stations within an area comparable to model grid boxes; for those it is found that aggregation of stations before calculation of statistics has little effect on estimates of variance, but soil moisture memory is sensitive to aggregation. Statistics for some networks stand out as unlike those of their neighbors, likely because of differences in instrumentation, calibration, and maintenance. Buried sensors appear to have less random error than near-field remote sensing techniques, and heat-dissipation sensors show less temporal variability than other types. Model soil moistures are evaluated using three metrics: standard deviation in time, temporal correlation (memory), and spatial correlation (length scale). Models do relatively well in capturing large-scale variability of metrics across climate regimes, but they poorly reproduce observed patterns at scales of hundreds of kilometers and smaller. Uncoupled land models do no better than coupled model configurations, nor do reanalyses outperform free-running models. Spatial decorrelation scales are found to be difficult to diagnose. Using data for model validation, calibration, or data assimilation from multiple soil moisture networks with different types of sensors and measurement techniques requires great caution. Data from models and observations should be put on the same spatial and temporal scales before comparison.
C1 [Dirmeyer, Paul A.; Wu, Jiexia; Norton, Holly E.] George Mason Univ, Fairfax, VA 22030 USA.
[Dorigo, Wouter A.] Vienna Univ Technol, A-1040 Vienna, Austria.
[Dorigo, Wouter A.] Univ Ghent, Lab Forest & Water Management, B-9000 Ghent, Belgium.
[Quiring, Steven M.] Texas A&M Univ, College Stn, TX USA.
[Ford, Trenton W.] So Illinois Univ, Carbondale, IL 62901 USA.
[Santanello, Joseph A., Jr.; Bosilovich, Michael G.; Koster, Randal D.] NASA, Goddard Space Flight Ctr, Greenbelt, MD USA.
[Ek, Michael B.] NOAA, Natl Ctr Environm Predict, College Pk, MD USA.
[Balsamo, Gianpaolo] European Ctr Medium Range Weather Forecasts, Shinfield Pk, Reading RG2 9AX, Berks, England.
[Lawrence, David M.] Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA.
RP Dirmeyer, PA (reprint author), George Mason Univ, Ctr Ocean Land Atmosphere Studies, 4400 Univ Dr,Mail Stop 6C5, Fairfax, VA 22030 USA.
EM pdirmeye@gmu.edu
RI Koster, Randal/F-5881-2012; Santanello, Joseph/D-4438-2012; Bosilovich,
Michael/F-8175-2012
OI Koster, Randal/0000-0001-6418-6383; Santanello,
Joseph/0000-0002-0807-6590;
FU National Aeronautics and Space Administration [NNX13AQ21G]; SMOS Soil
Moisture Network Study Operational Phase (ESA ESTEC) [4000102722/10]
FX This work has been primarily supported by National Aeronautics and Space
Administration Grant NNX13AQ21G. Funding for W.D. has come from SMOS
Soil Moisture Network Study Operational Phase (ESA ESTEC Contract
4000102722/10). Support for the Twentieth Century Reanalysis Project
dataset is provided by the U.S. Department of Energy, Office of Science
Innovative and Novel Computational Impact on Theory and Experiment (DOE
INCITE) program, and Office of Biological and Environmental Research
(BER), and by the National Oceanic and Atmospheric Administration
Climate Program Office. We thank G. Compo for making 20CR data available
to us.
NR 66
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Z9 4
U1 2
U2 10
PU AMER METEOROLOGICAL SOC
PI BOSTON
PA 45 BEACON ST, BOSTON, MA 02108-3693 USA
SN 1525-755X
EI 1525-7541
J9 J HYDROMETEOROL
JI J. Hydrometeorol.
PD APR
PY 2016
VL 17
IS 4
BP 1049
EP 1067
DI 10.1175/JHM-D-15-0196.1
PG 19
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DG9LY
UT WOS:000372405700001
ER
PT J
AU Colle, R
Colle, AM
AF Colle, R.
Colle, A. M.
TI On the Po-209 half-life error and its confirmation: a critique
SO JOURNAL OF RADIOANALYTICAL AND NUCLEAR CHEMISTRY
LA English
DT Article
DE Data analysis; Half-life; Measurement uncertainty; Po-209
ID PRIMARY STANDARDIZATION; ISOTOPES
AB A recent report on Po-209 claimed to have made a determination of the 125-a half-life from measurements made over 0.8 % of one half-life. A careful reanalysis of the original data with a more complete and rigorous consideration of the underlying uncertainties demonstrates that this claim cannot withstand critical scrutiny. More importantly, this critique examines the larger issue as to what constitutes a valid half-life determination, and highlights that a careful and realistic analysis beyond the mere fitting of decay data to an exponential function is required for the measurement and reporting of half-life values.
C1 [Colle, R.] NIST, Gaithersburg, MD 20899 USA.
[Colle, A. M.] Univ Maryland, Dept Comp Sci, College Pk, MD 20742 USA.
RP Colle, R (reprint author), NIST, Gaithersburg, MD 20899 USA.
EM rcolle@nist.gov
NR 22
TC 0
Z9 0
U1 2
U2 3
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0236-5731
EI 1588-2780
J9 J RADIOANAL NUCL CH
JI J. Radioanal. Nucl. Chem.
PD APR
PY 2016
VL 308
IS 1
BP 271
EP 278
DI 10.1007/s10967-015-4307-y
PG 8
WC Chemistry, Analytical; Chemistry, Inorganic & Nuclear; Nuclear Science &
Technology
SC Chemistry; Nuclear Science & Technology
GA DG7MQ
UT WOS:000372268800030
ER
PT J
AU Hershberger, PK
Gregg, JL
Hart, LM
Moffitt, S
Brenner, R
Stick, K
Coonradt, E
Otis, EO
Vollenweider, JJ
Garver, KA
Lovy, J
Meyers, TR
AF Hershberger, P. K.
Gregg, J. L.
Hart, L. M.
Moffitt, S.
Brenner, R.
Stick, K.
Coonradt, E.
Otis, E. O.
Vollenweider, J. J.
Garver, K. A.
Lovy, J.
Meyers, T. R.
TI The parasite Ichthyophonus sp in Pacific herring from the coastal NE
Pacific
SO JOURNAL OF FISH DISEASES
LA English
DT Article
DE Ichthyophonus; Pacific herring
ID SARDINOPS-SAGAX-NEOPILCHARDUS; FLOUNDER LIMANDA-FERRUGINEA;
CLUPEA-PALLASI POPULATION; NOVA-SCOTIA SHELF; PUGET-SOUND; EPIZOOTIC
MORTALITY; MASS MORTALITY; CHINOOK SALMON; HOFERI PLEHN; PILCHARD
AB The protistan parasite Ichthyophonus occurred in populations of Pacific herring Clupea pallasii Valenciennes throughout coastal areas of the NE Pacific, ranging from Puget Sound, WA north to the Gulf of Alaska, AK. Infection prevalence in local Pacific herring stocks varied seasonally and annually, and a general pattern of increasing prevalence with host size and/or age persisted throughout the NE Pacific. An exception to this zoographic pattern occurred among a group of juvenile, age 1+ year Pacific herring from Cordova Harbor, AK in June 2010, which demonstrated an unusually high infection prevalence of 35%. Reasons for this anomaly were hypothesized to involve anthropogenic influences that resulted in locally elevated infection pressures. Interannual declines in infection prevalence from some populations (e.g. Lower Cook Inlet, AK; from 20-32% in 2007 to 0-3% during 2009-13) or from the largest size cohorts of other populations (e.g. Sitka Sound, AK; from 62.5% in 2007 to 19.6% in 2013) were likely a reflection of selective mortality among the infected cohorts. All available information for Ichthyophonus in the NE Pacific, including broad geographic range, low host specificity and presence in archived Pacific herring tissue samples dating to the 1980s, indicate a long-standing host-pathogen relationship.
C1 [Hershberger, P. K.; Gregg, J. L.; Hart, L. M.] US Geol Survey, Western Fisheries Res Ctr, Marrowstone Marine Field Stn, 616 Marrowstone Point Rd, Nordland, WA 98358 USA.
[Moffitt, S.; Brenner, R.] Alaska Dept Fish & Game ADF&G Commercial Fisherie, Cordova, AK USA.
[Stick, K.] Reg 4 LaConner Dist Off, Fish Program, Washington Dept Fish & Wildlife, La Conner, WA USA.
[Coonradt, E.] ADF&G Commercial Fisheries, Sitka, AK USA.
[Otis, E. O.] ADF&G Commercial Fisheries, Homer, AK USA.
[Vollenweider, J. J.] Natl Ocean & Atmospher Adm, Alaska Fisheries Sci Ctr, Auke Bay Labs, Juneau, AK USA.
[Garver, K. A.] Fisheries & Oceans Canada, Pacific Biol Stn, Nanaimo, BC V9T 6N7, Canada.
[Lovy, J.] Off Fish & Wildlife Hlth & Forens, New Jersey Div Fish & Wildlife, Oxford, NJ USA.
[Meyers, T. R.] ADF&G Juneau Fish Pathol Lab, Juneau, AK USA.
RP Hershberger, PK (reprint author), US Geol Survey, Western Fisheries Res Ctr, Marrowstone Marine Field Stn, 616 Marrowstone Point Rd, Nordland, WA 98358 USA.
EM phershberger@usgs.gov
FU Exxon Valdez Oil Spill Trustee Council [10100132-I]; Herring
Conservation and Research Society; U.S. Geological Survey - Fisheries
Program, Ecosystems Mission Area
FX Funding was provided by the Exxon Valdez Oil Spill Trustee Council,
Project # 10100132-I, the Herring Conservation and Research Society, and
the U.S. Geological Survey - Fisheries Program, Ecosystems Mission Area.
Technical support was provided by C. Pacheco, C. Grady, J. Word, R.
Wade, S. Roon, S. Luis, C. Luk, N. Lewandowski, B. Tyler and M. Yanney
(USGS - Marrowstone Marine Field Station). Sample collection from Canada
was facilitated by L. Hammer (Herring Conservation and Research
Society). Insights into the overwintering structure of British Columbia
herring were provided by Dr. Doug Hay (DFO - Canada). Access to archived
Pacific herring at the University of Washington Fish Collection was
provided by Drs. T. Pietch and K. Pearson Maslenikov The use of trade,
firm or corporation names in this publication is for the information and
convenience of the reader. Such use does not constitute an official
endorsement or approval by the U.S. Department of Interior or the U.S.
Geological Survey of any product or service to the exclusion of others
that may be suitable.
NR 43
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Z9 4
U1 5
U2 11
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0140-7775
EI 1365-2761
J9 J FISH DIS
JI J. Fish Dis.
PD APR
PY 2016
VL 39
IS 4
BP 395
EP 410
DI 10.1111/jfd.12370
PG 16
WC Fisheries; Marine & Freshwater Biology; Veterinary Sciences
SC Fisheries; Marine & Freshwater Biology; Veterinary Sciences
GA DG8KZ
UT WOS:000372334000001
PM 25828232
ER
PT J
AU Muralikrishnan, B
Phillips, S
Sawyer, D
AF Muralikrishnan, Bala
Phillips, Steve
Sawyer, Daniel
TI Laser trackers for large-scale dimensional metrology: A review
SO PRECISION ENGINEERING-JOURNAL OF THE INTERNATIONAL SOCIETIES FOR
PRECISION ENGINEERING AND NANOTECHNOLOGY
LA English
DT Review
DE Laser tracker; Large-scale dimensional metrology; Error modeling;
Performance evaluation; Measurement uncertainty; Standardization
ID TRACKING INTERFEROMETER SYSTEM; CATS-EYE RETROREFLECTOR; UPDATED EDLEN
EQUATION; REFRACTIVE-INDEX; MACHINE-TOOLS; CALIBRATION SYSTEM;
COORDINATE DATA; ANGLE ENCODER; ERROR; UNCERTAINTY
AB Thirty years since their invention, laser trackers are now recognized as the measurement tool of choice in the manufacture and assembly of large components. The general design of laser trackers, i.e., a ranging unit on a two-axis gimbal, has not changed significantly over the years. However, innovations in ranging technology, for example, the emergence of increasingly accurate absolute distance meters (ADMs), are providing users with an alternative to interferometers (IFMs). Hand-held accessories such as touch probes and line scanners are expanding the scope and applicability of laser trackers. In this paper, we survey the literature in all areas of laser trackers as applied to large-scale dimensional metrology (LSDM), with emphasis on error modeling, measurement uncertainty, performance evaluation and standardization. Published by Elsevier Inc.
C1 [Muralikrishnan, Bala; Phillips, Steve; Sawyer, Daniel] NIST, Div Engn Phys, Gaithersburg, MD 20899 USA.
RP Muralikrishnan, B (reprint author), NIST, Div Engn Phys, Gaithersburg, MD 20899 USA.
EM balam@nist.gov
NR 150
TC 2
Z9 2
U1 15
U2 31
PU ELSEVIER SCIENCE INC
PI NEW YORK
PA 360 PARK AVE SOUTH, NEW YORK, NY 10010-1710 USA
SN 0141-6359
EI 1873-2372
J9 PRECIS ENG
JI Precis. Eng.-J. Int. Soc. Precis. Eng. Nanotechnol.
PD APR
PY 2016
VL 44
BP 13
EP 28
DI 10.1016/j.precisioneng.2015.12.001
PG 16
WC Engineering, Multidisciplinary; Engineering, Manufacturing; Nanoscience
& Nanotechnology; Instruments & Instrumentation
SC Engineering; Science & Technology - Other Topics; Instruments &
Instrumentation
GA DG3AX
UT WOS:000371943000002
ER
PT J
AU Johnsson, E
Yang, JC
AF Johnsson, Erik
Yang, Jiann C.
TI Experimental study on hardening a motorcoach against tire fire
penetration
SO FIRE AND MATERIALS
LA English
DT Article
DE transportation fires; fire growth; flame spread; vehicle fires; bus
fires; tire fires; fire penetration; fire hardening
AB Three full-scale fire experiments were conducted to assess methods of hardening the motorcoach against penetration of a tire fire. The first method was to replace the combustible fender and exterior side panel above the wheels with stainless steel sheet metal. The second method was to coat the plastic fender and side panel with an intumescent layer. The third method was to install a sheet steel fire plume deflector between the fender and side panel. A special burner was used that imitates the frictional heating of hub and wheel metal caused by failed axle bearings, locked brakes, or dragged blown tires. For each experiment, heating to obtain tire ignition was initiated on the exterior of the passenger side tag axle wheel. Measurements of interior and exterior temperatures, interior heat flux, and heat release rate were performed. Standard and infrared videos and still photographs were recorded. The experimental results were compared with those obtained with no fire hardening. The metal replacement method performed best and prevented fire penetration for over 30min longer than the nonhardened cases. The intumescent coating extended fire penetration by about 20min longer than the nonhardened cases. The steel plume deflector had no significant impact on the timing for fire penetration of the windows. Published 2015. This article is a U.S. Government work and is in the public domain in the USA.
C1 [Johnsson, Erik; Yang, Jiann C.] NIST, Engn Lab, 100 Bur Dr, Gaithersburg, MD 20899 USA.
RP Johnsson, E (reprint author), NIST, Engn Lab, 100 Bur Dr, Gaithersburg, MD 20899 USA.
EM erik.johnsson@nist.gov
OI Johnsson, Erik/0000-0003-1170-7370
FU NHTSA
FX This work was sponsored by the NHTSA. Thanks to Marco Fernandez of NIST
and the National Fire Research Laboratory staff for all the hard work
preparing for and running this challenging experimental project, to Ed
Hnetkovsky of NIST for help with the burner, and to the NIST Fire
Protection Group and the Fire Fighting Technology Group for providing
backup fire suppression. Also, the NIST Plant Division is appreciated
for providing crews to move our motorcoach. NIST thanks Randy Smith and
Alex Cook of Greyhound for their helpful technical advice.
NR 6
TC 1
Z9 1
U1 5
U2 6
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0308-0501
EI 1099-1018
J9 FIRE MATER
JI Fire Mater.
PD APR
PY 2016
VL 40
IS 3
BP 416
EP 426
DI 10.1002/fam.2295
PG 11
WC Materials Science, Multidisciplinary
SC Materials Science
GA DF9KG
UT WOS:000371679300005
ER
PT J
AU Kendall, MS
Poti, M
Karnauskas, KB
AF Kendall, Matthew S.
Poti, Matt
Karnauskas, Kristopher B.
TI Climate change and larval transport in the ocean: fractional effects
from physical and physiological factors
SO GLOBAL CHANGE BIOLOGY
LA English
DT Article
DE Caroline Archipelago; connectivity; coral reef; larvae; Marianas;
Micronesia; pelagic larval duration
ID EARLY-LIFE-HISTORY; REEF FISH LARVAE; CORAL-REEFS; TEMPERATURE;
DISPERSAL; CONNECTIVITY; CONSERVATION; MODEL; ACIDIFICATION;
REPRODUCTION
AB Changes in larval import, export, and self-seeding will affect the resilience of coral reef ecosystems. Climate change will alter the ocean currents that transport larvae and also increase sea surface temperatures (SST), hastening development, and shortening larval durations. Here, we use transport simulations to estimate future larval connectivity due to: (1) physical transport of larvae from altered circulation alone, and (2) the combined effects of altered currents plus physiological response to warming. Virtual larvae from islands throughout Micronesia were moved according to present-day and future ocean circulation models. The Hybrid Coordinate Ocean Model (HYCOM) spanning 2004-2012 represented present-day currents. For future currents, we altered HYCOM using analysis from the National Center for Atmospheric Research Community Earth System Model, version 1-Biogeochemistry, Representative Concentration Pathway 8.5 experiment. Based on the NCAR model, regional SST is estimated to rise 2.74 degrees C which corresponds to a similar to 17% decline in larval duration for some taxa. This reduction was the basis for a separate set of simulations. Results predict an increase in self-seeding in 100years such that 62-76% of islands experienced increased self-seeding, there was an average domainwide increase of similar to 1-3% points in self-seeding, and increases of up to 25% points for several individual islands. When changed currents alone were considered, approximately half (i.e., random) of all island pairs experienced decreased connectivity but when reduced PLD was added as an effect, similar to 65% of connections were weakened. Orientation of archipelagos relative to currents determined the directional bias in connectivity changes. There was no universal relationship between climate change and connectivity applicable to all taxa and settings. Islands that presently export large numbers of larvae but that also maintain or enhance this role into the future should be the focus of conservation measures that promote long-term resilience of larval supply.
C1 [Kendall, Matthew S.; Poti, Matt] NOAA, NCCOS, CCMA, Biogeog Branch, Silver Spring, MD USA.
[Poti, Matt] Consolidated Safety Serv Dynamac Inc, Fairfax, VA USA.
[Karnauskas, Kristopher B.] Univ Colorado, CIRES, Dept Atmospher & Ocean Sci, Boulder, CO 80309 USA.
RP Kendall, MS (reprint author), NOAA, NCCOS, CCMA, Biogeog Branch, Silver Spring, MD USA.
EM matt.kendall@noaa.gov
FU NOAA's Coral Reef Conservation Program; Alfred P. Sloan Foundation; WHOI
Oceans and Climate Change Institute; CSS-Dynamac, Fairfax VA under NOAA
[DG133C11CO0019]
FX This study was funded by NOAA's Coral Reef Conservation Program, Alfred
P. Sloan Foundation, and the WHOI Oceans and Climate Change Institute.
Chris Barker and Caitlin O'Conner provided assistance with running
transport simulations in GNOME. Brian Kinlan and Arliss Winship provided
guidance on Matlab and R code for processing data outputs. Dana Okano
and Adrienne Loerzel facilitated contact with many local experts in the
Mariana region. John Christensen and anonymous reviewers provided
constructive comments to improve the manuscript. Government contract
labor was provided by CSS-Dynamac, Fairfax VA under NOAA contract
DG133C11CO0019.
NR 67
TC 1
Z9 1
U1 10
U2 53
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 1354-1013
EI 1365-2486
J9 GLOBAL CHANGE BIOL
JI Glob. Change Biol.
PD APR
PY 2016
VL 22
IS 4
BP 1532
EP 1547
DI 10.1111/gcb.13159
PG 16
WC Biodiversity Conservation; Ecology; Environmental Sciences
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA DF7CN
UT WOS:000371515300018
PM 26554877
ER
PT J
AU Seung, CK
AF Seung, Chang K.
TI Identifying channels of economic impacts: An inter-regional structural
path analysis for Alaska fisheries
SO MARINE POLICY
LA English
DT Article
DE Alaska fisheries; Inter-regional economic impacts; Social accounting
matrix; Structural path analysis
ID SOCIAL ACCOUNTING MATRIX; FRAMEWORK; SHOCKS; MODEL
AB Alaska fisheries have strong spillover effects on economies of other states (especially the state of Washington) due to their dependence on imports from these other states. Several studies attempt to develop inter-regional or multi-regional economic impact models to investigate these spillover effects, and calculate the multipliers for Alaska fisheries. However, these multipliers measure only total economic impacts, failing to provide fishery managers with the information on how and along what channels these total economic impacts are generated and transmitted throughout the regions. This paper uses an inter-regional structural path analysis (IRSPA) to identify the various channels (paths) through which the economic impacts of an initial shock to a seafood sector are transmitted, amplified, and spilled over to other regions, within an inter-regional social accounting matrix (IRSAM) framework for two US regions Alaska and the rest of US (RUS). Published by Elsevier Ltd.
C1 [Seung, Chang K.] NOAA, Alaska Fisheries Sci Ctr, Natl Marine Fisheries Serv, 7600 Sand Point Way NE, Seattle, WA 98115 USA.
RP Seung, CK (reprint author), NOAA, Alaska Fisheries Sci Ctr, Natl Marine Fisheries Serv, 7600 Sand Point Way NE, Seattle, WA 98115 USA.
EM Chang.Seung@noaa.gov
NR 24
TC 0
Z9 0
U1 4
U2 4
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 0308-597X
EI 1872-9460
J9 MAR POLICY
JI Mar. Pol.
PD APR
PY 2016
VL 66
BP 39
EP 49
DI 10.1016/j.marpol.2016.01.015
PG 11
WC Environmental Studies; International Relations
SC Environmental Sciences & Ecology; International Relations
GA DF7QN
UT WOS:000371552800006
ER
PT J
AU Simiu, E
Shi, L
Yeo, D
AF Simiu, Emil
Shi, Liang
Yeo, DongHun
TI Planetary Boundary-Layer Modelling and Tall Building Design
SO BOUNDARY-LAYER METEOROLOGY
LA English
DT Article
DE Boundary-layer meteorology; Brunt; Vaisala frequency; Conventionally
neutral stratification; Planetary boundary layer; Tall structures
ID INTEGRAL MEASURES
AB Characteristics of flow in the planetary boundary layer (PBL) strongly affect the design of tall structures. PBL modelling in building codes, based as it is on empirical data from the 1960s and 1970s, differs significantly from contemporary PBL models, which account for both "neutral" flows, and "conventionally neutral" flows. PBL heights estimated in these relatively sophisticated models are typically approximately half as large as those obtained using the classical asymptotic similarity approach, and are one order of magnitude larger than those specified in North American and Japanese building codes. A simple method is proposed for estimating the friction velocity and PBL height as functions of specified surface roughness and geostrophic wind speed. Based on published results, it is tentatively determined that, even at elevations as high as 800 m above the surface, the contribution to the resultant mean flow velocity of the component V normal to the surface stress is negligible and the veering angle is of the order of only 5. This note aims to encourage dialogue between boundary-layer meteorologists and structural engineers.
C1 [Simiu, Emil; Shi, Liang; Yeo, DongHun] NIST, Engn Lab, Gaithersburg, MD 20899 USA.
RP Simiu, E (reprint author), NIST, Engn Lab, Gaithersburg, MD 20899 USA.
EM emil.simiu@nist.gov
NR 14
TC 0
Z9 0
U1 4
U2 4
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 0006-8314
EI 1573-1472
J9 BOUND-LAY METEOROL
JI Bound.-Layer Meteor.
PD APR
PY 2016
VL 159
IS 1
BP 173
EP 181
DI 10.1007/s10546-015-0106-9
PG 9
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DF3KW
UT WOS:000371243800010
ER
PT J
AU Smith, JP
Hunter, TS
Clites, AH
Stow, CA
Slawecki, T
Muhr, GC
Gronewold, AD
AF Smith, Joeseph P.
Hunter, Timothy S.
Clites, Anne H.
Stow, Craig A.
Slawecki, Tad
Muhr, Glenn C.
Gronewold, Andrew D.
TI An expandable web-based platform for visually analyzing basin-scale
hydro-climate time series data
SO ENVIRONMENTAL MODELLING & SOFTWARE
LA English
DT Article
DE Data visualization; Great lakes; Data access; Analytics; Software;
Object oriented
ID GREAT-LAKES; WATER; SYSTEM; MANAGEMENT; FUTURE
AB Growing demand from the general public for centralized points of data access and analytics tools coincides with similar, well-documented needs of regional and international hydrology research and resource management communities. To address this need within the Laurentian Great Lakes region, we introduce the Great Lakes Dashboard (GLD), a dynamic web data visualization platform that brings multiple time series data sets together for visual analysis and download. The platform's adaptable, robust, and expandable Time Series Core Object Model (GLD-TSCOM) separates the growing complexity and size of Great Lakes data sets from the web application interface. Although the GLD-TSCOM is currently applied exclusively to Great Lakes data sets, the concepts and methods discussed here can be applied in other geographical and topical areas of interest. (C) 2016 The Authors. Published by Elsevier Ltd.
C1 [Smith, Joeseph P.] Univ Michigan, Cooperat Inst Limnol & Ecosyst Res, Ann Arbor, MI 48109 USA.
[Hunter, Timothy S.; Clites, Anne H.; Stow, Craig A.; Muhr, Glenn C.; Gronewold, Andrew D.] NOAA, Great Lakes Environm Res Lab, Ann Arbor, MI 48108 USA.
[Slawecki, Tad] LimnoTech, Ann Arbor, MI 48108 USA.
[Gronewold, Andrew D.] Univ Michigan, Dept Civil & Environm Engn, Ann Arbor, MI 48109 USA.
RP Smith, JP (reprint author), Univ Michigan, Cooperat Inst Limnol & Ecosyst Res, Ann Arbor, MI 48109 USA.
EM joeseph@umich.edu
RI karanki, Archana/E-7014-2016;
OI Smith, Joeseph/0000-0002-1896-1390; Clites, Anne/0000-0002-2385-3802
FU CILER by NOAA; Great Lakes Restoration Initiative [DW1392377301-0];
International Joint Commission International Upper Great Lakes Study
[P14100186]; USACE [W56MES32262531]
FX Funding for this research and development was provided through CILER by
NOAA, the Great Lakes Restoration Initiative (No. DW1392377301-0,
administered by USEPA), the International Joint Commission International
Upper Great Lakes Study (No. P14100186), and the USACE (No.
W56MES32262531). The authors would like to thank NOAA's Climate.gov
dashboard team for initial advice, including Viviane Silva, David
Herring, and Mark Phillips. For technical and communication support, we
would like to thank NOAA-GLERL's Margaret Lansing and Cathy Darnell. For
general guidance and partnership, we thank the United States Army Corps
of Engineers - Detroit District, specifically Jim Lewis, John Allis, and
Keith Kompoltowicz, along with Heather Stirratt and Brandon Krumwiede at
NOAA's Office for Coastal Management. Special thanks to all who took
time to review this paper, including Brent Lofgren of NOAA-GLERL and
John Bratton of LimnoTech, and all anonymous reviewers.
NR 33
TC 0
Z9 0
U1 5
U2 22
PU ELSEVIER SCI LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND
SN 1364-8152
EI 1873-6726
J9 ENVIRON MODELL SOFTW
JI Environ. Modell. Softw.
PD APR
PY 2016
VL 78
BP 97
EP 105
DI 10.1016/j.envsoft.2015.12.005
PG 9
WC Computer Science, Interdisciplinary Applications; Engineering,
Environmental; Environmental Sciences
SC Computer Science; Engineering; Environmental Sciences & Ecology
GA DF5FS
UT WOS:000371377800008
ER
PT J
AU Srivastava, S
Kishore, S
Narayanan, S
Sandy, AR
Bhatia, SR
AF Srivastava, Sunita
Kishore, Suhasini
Narayanan, Suresh
Sandy, Alec R.
Bhatia, Surita R.
TI Multiple Dynamic Regimes in Colloid-Polymer Dispersions: New Insight
Using X-Ray Photon Correlation Spectroscopy
SO JOURNAL OF POLYMER SCIENCE PART B-POLYMER PHYSICS
LA English
DT Article
DE colloids; gels; nanoparticles
ID LAPONITE-PEO MIXTURES; POLY(ETHYLENE OXIDE); LIGHT-SCATTERING;
NANOCOMPOSITE HYDROGELS; AQUEOUS DISPERSIONS; GLASS-TRANSITION; AGING
BEHAVIOR; SHAKE-GELS; CLAY; SUSPENSIONS
AB We present an X-ray photon correlation spectroscopy (XPCS) study of dynamic transitions in an anisotropic colloid-polymer dispersion with multiple arrested states. The results provide insight into the mechanism for formation of repulsive glasses, attractive glasses, and networked gels of colloids with weakly adsorbing polymer chains. In the presence of adsorbing polymer chains, we observe three distinct regimes: a state with slow dynamics consisting of finite particles and clusters, for which interparticle interactions are predominantly repulsive; a second dynamic regime occurring above the saturation concentration of added polymer, in which small clusters of nanoparticles form via a short-range depletion attraction; and a third regime above the overlap concentration in which dynamics of clusters are independent of polymer chain length. The observed complex dynamic state diagram is primarily governed by the structural reorganization of a nanoparticle cluster and polymer chains at the nanoparticle-polymer surface and in the concentrated medium, which in turn controls the dynamics of the dispersion. (C) 2015 Wiley Periodicals, Inc.
C1 [Srivastava, Sunita; Kishore, Suhasini; Bhatia, Surita R.] SUNY Stony Brook, Dept Chem, Stony Brook, NY 11794 USA.
[Srivastava, Sunita] Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.
[Kishore, Suhasini] Univ Massachusetts, Dept Chem Engn, Amherst, MA 01003 USA.
[Narayanan, Suresh; Sandy, Alec R.] Argonne Natl Lab, Adv Photon Source, Argonne, IL 60439 USA.
[Bhatia, Surita R.] Brookhaven Natl Lab, Ctr Funct Nanomat, Upton, NY 11973 USA.
RP Srivastava, S; Bhatia, SR (reprint author), SUNY Stony Brook, Dept Chem, Stony Brook, NY 11794 USA.; Srivastava, S (reprint author), Natl Inst Stand & Technol, Gaithersburg, MD 20899 USA.; Bhatia, SR (reprint author), Brookhaven Natl Lab, Ctr Funct Nanomat, Upton, NY 11973 USA.
EM sunita.srivastava@nist.gov; surita.bhatia@stonybrook.edu
RI Bhatia, Surita/B-4536-2008
FU National Science Foundation [CBET-1335787]; U.S. Department of Energy
Office of Science [DE-AC02-06CH11357]; U.S. Department of Energy, Office
of Basic Energy Sciences [DE-AC02-98CH10886]
FX This work was supported by the National Science Foundation, Award No.
CBET-1335787. Use of the Advanced Photon Source at Argonne National
Laboratory was supported by the U.S. Department of Energy Office of
Science under contract DE-AC02-06CH11357. Research carried out in part
at the Center for Functional Nanomaterials, Brookhaven National
Laboratory, which is supported by the U.S. Department of Energy, Office
of Basic Energy Sciences, under Contract No. DE-AC02-98CH10886.
NR 65
TC 2
Z9 2
U1 5
U2 27
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0887-6266
EI 1099-0488
J9 J POLYM SCI POL PHYS
JI J. Polym. Sci. Pt. B-Polym. Phys.
PD APR 1
PY 2016
VL 54
IS 7
BP 752
EP 760
DI 10.1002/polb.23973
PG 9
WC Polymer Science
SC Polymer Science
GA DF6UQ
UT WOS:000371492800007
ER
PT J
AU Spromberg, JA
Baldwin, DH
Damm, SE
McIntyre, JK
Huff, M
Sloan, CA
Anulacion, BF
Davis, JW
Scholz, NL
AF Spromberg, Julann A.
Baldwin, David H.
Damm, Steven E.
McIntyre, Jenifer K.
Huff, Michael
Sloan, Catherine A.
Anulacion, Bernadita F.
Davis, Jay W.
Scholz, Nathaniel L.
TI Coho salmon spawner mortality in western US urban watersheds:
bioinfiltration prevents lethal storm water impacts
SO JOURNAL OF APPLIED ECOLOGY
LA English
DT Article
DE habitat restoration; non-point source pollution; Pacific salmon;
run-off; storm water; urban ecology; urban streams
ID POLYCYCLIC AROMATIC-HYDROCARBONS; EARLY-LIFE STAGES; CRUDE-OIL;
LAND-USE; ONCORHYNCHUS-KISUTCH; SOIL BIORETENTION; PUGET-SOUND; RUNOFF;
EXPOSURE; GROWTH
AB Adult coho salmon Oncorhynchus kisutch return each autumn to freshwater spawning habitats throughout western North America. The migration coincides with increasing seasonal rainfall, which in turn increases storm water run-off, particularly in urban watersheds with extensive impervious land cover. Previous field assessments in urban stream networks have shown that adult coho are dying prematurely at high rates (>50%). Despite significant management concerns for the long-term conservation of threatened wild coho populations, a causal role for toxic run-off in the mortality syndrome has not been demonstrated. We exposed otherwise healthy coho spawners to: (i) artificial storm water containing mixtures of metals and petroleum hydrocarbons, at or above concentrations previously measured in urban run-off; (ii) undiluted storm water collected from a high traffic volume urban arterial road (i.e. highway run-off); and (iii) highway run-off that was first pre-treated via bioinfiltration through experimental soil columns to remove pollutants. We find that mixtures of metals and petroleum hydrocarbons - conventional toxic constituents in urban storm water - are not sufficient to cause the spawner mortality syndrome. By contrast, untreated highway run-off collected during nine distinct storm events was universally lethal to adult coho relative to unexposed controls. Lastly, the mortality syndrome was prevented when highway run-off was pretreated by soil infiltration, a conventional green storm water infrastructure technology. Our results are the first direct evidence that: (i) toxic run-off is killing adult coho in urban watersheds, and (ii) inexpensive mitigation measures can improve water quality and promote salmon survival.Synthesis and applications. Coho salmon, an iconic species with exceptional economic and cultural significance, are an ecological sentinel for the harmful effects of untreated urban run-off. Wild coho populations cannot withstand the high rates of mortality that are now regularly occurring in urban spawning habitats. Green storm water infrastructure or similar pollution prevention methods should be incorporated to the maximal extent practicable, at the watershed scale, for all future development and redevelopment projects, particularly those involving transportation infrastructure.
Coho salmon, an iconic species with exceptional economic and cultural significance, are an ecological sentinel for the harmful effects of untreated urban run-off. Wild coho populations cannot withstand the high rates of mortality that are now regularly occurring in urban spawning habitats. Green storm water infrastructure or similar pollution prevention methods should be incorporated to the maximal extent practicable, at the watershed scale, for all future development and redevelopment projects, particularly those involving transportation infrastructure. Editor's Choice
C1 [Spromberg, Julann A.] Natl Marine Fisheries Serv, Ocean Associates, NW Fisheries Sci Ctr, NOAA, 2725 Montlake Blvd E, Seattle, WA 98112 USA.
[Baldwin, David H.; Sloan, Catherine A.; Anulacion, Bernadita F.; Scholz, Nathaniel L.] Natl Marine Fisheries Serv, Environm & Fisheries Sci Div, NW Fisheries Sci Ctr, NOAA, 2725 Montlake Blvd E, Seattle, WA 98112 USA.
[Damm, Steven E.; Davis, Jay W.] US Fish & Wildlife Serv, Washington Fish & Wildlife Off, 510 Desmond Dr S-E, Lacey, WA 98503 USA.
[McIntyre, Jenifer K.] Washington State Univ, Puyallup Res & Extens Ctr, 2606 W Pioneer Ave, Puyallup, WA 98371 USA.
[Huff, Michael] Suquamish Tribe, POB 498,18490 Suquamish Way, Suquamish, WA 98392 USA.
RP Scholz, NL (reprint author), Natl Marine Fisheries Serv, Environm & Fisheries Sci Div, NW Fisheries Sci Ctr, NOAA, 2725 Montlake Blvd E, Seattle, WA 98112 USA.
EM nathaniel.scholz@noaa.gov
RI feng, yongzhong/F-5090-2012;
OI feng, yongzhong/0000-0002-5202-4368; Scholz,
Nathaniel/0000-0001-6207-0272
FU NOAA Coastal Storms Program (National Ocean Service, Coastal Services
Center); U.S. Fish & Wildlife Service; Puget Sound's Regional Stormwater
Monitoring Programme (RSMP); U.S. Environmental Protection Agency,
Region 10
FX We appreciate the technical assistance of Allisan Beck, Richard Edmunds,
Tony Gill, Emma Mudrock, Tiffany Linbo, Kate Macneale, Jana Labenia,
Mark Tagal, Frank Sommers, Gina Ylitalo, Daryle Boyd, Barb French, Ann
England, Karen Peck, MaryJean Willis, Cathy Laetz, Sylvia Charles,
William Alexander, Ben Purser, Corey Oster, Luke Williams and the Kitsap
Poggie Club. This study received agency funding from the NOAA Coastal
Storms Program (National Ocean Service, Coastal Services Center), the
U.S. Fish & Wildlife Service, the Puget Sound's Regional Stormwater
Monitoring Programme (RSMP as administered by the WA State Dept. of
Ecology), and the U.S. Environmental Protection Agency, Region 10.
Lastly, we appreciate the helpful suggestions of two anonymous
reviewers. Findings and conclusions herein are those of the authors and
do not necessarily represent the views of the sponsoring organizations.
NR 36
TC 5
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U1 12
U2 38
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0021-8901
EI 1365-2664
J9 J APPL ECOL
JI J. Appl. Ecol.
PD APR
PY 2016
VL 53
IS 2
BP 398
EP 407
DI 10.1111/1365-2664.12534
PG 10
WC Biodiversity Conservation; Ecology
SC Biodiversity & Conservation; Environmental Sciences & Ecology
GA DE9LN
UT WOS:000370959100012
ER
PT J
AU Mitropoulos, S
Tsiantos, V
Ovaliadis, K
Kechrakos, D
Donahue, M
AF Mitropoulos, Spyridon
Tsiantos, Vassilis
Ovaliadis, Kyriakos
Kechrakos, Dimitris
Donahue, Michael
TI Stiff modes in spinvalve simulations with OOMMF
SO PHYSICA B-CONDENSED MATTER
LA English
DT Article; Proceedings Paper
CT 10th International Symposium on Hysteresis Modeling and Micromagnetics
(HMM)
CY MAY 18-20, 2015
CL Alexandru Ioan Cuza Univ, Iasi, ROMANIA
HO Alexandru Ioan Cuza Univ
DE Micromagnetic simulations; Spinvalve; ODEs; Stiffness
ID MICROMAGNETIC SOLVERS
AB Micromagnetic simulations are an important tool for the investigation of magnetic materials. Micro magnetic software uses various techniques to solve differential equations, partial or ordinary, involved in the dynamic simulations. Euler, Runge-Kutta, Adams, and BDF (Backward Differentiation Formulae) are some of the methods used for this purpose. In this paper, spinvalve simulations are investigated. Evidence is presented showing that these systems have stiff modes, and that implicit methods such as BDF are more effective than explicit methods in such cases. (C) 2015 Elsevier B.V. All rights reserved.
C1 [Mitropoulos, Spyridon] TEI Eastern Macedonia & Thrace, Dept Comp & Informat Engn, Kavala, Greece.
[Tsiantos, Vassilis; Ovaliadis, Kyriakos] TEI Eastern Macedonia & Thrace, Dept Elect Engn, Kavala 65404, Greece.
[Kechrakos, Dimitris] ASPETE, Dept Educ, Athens, Greece.
[Donahue, Michael] NIST, Appl & Computat Math Div, Gaithersburg, MD 20899 USA.
RP Tsiantos, V (reprint author), TEI Eastern Macedonia & Thrace, Dept Elect Engn, Kavala 65404, Greece.
EM tsianto@teikav.edu.gr
RI Kechrakos, Dimitris/H-7455-2014
NR 18
TC 0
Z9 0
U1 6
U2 10
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0921-4526
EI 1873-2135
J9 PHYSICA B
JI Physica B
PD APR 1
PY 2016
VL 486
BP 169
EP 172
DI 10.1016/j.physb.2015.10.010
PG 4
WC Physics, Condensed Matter
SC Physics
GA DE7YQ
UT WOS:000370853400038
ER
PT J
AU Zhu, HF
Sun, X
Kang, LM
Hong, MN
Liu, ML
Yu, ZH
Ouyang, J
AF Zhu, Hanfei
Sun, Xin
Kang, Limin
Hong, Mina
Liu, Menglin
Yu, Zhenghai
Ouyang, Jun
TI Charge transport behaviors in epitaxial BiFeO3 thick films sputtered
with different Ar/O-2 flow ratios
SO SCRIPTA MATERIALIA
LA English
DT Article
DE Ferroelectric materials; BiFeO3 films; Sputtering; Electrical
properties; Charge transport
ID MULTIFERROIC PROPERTIES; HETEROSTRUCTURES; POLARIZATION; TEMPERATURE;
PHASES; STRAIN
AB Heteroepitaxial BiFeO3 thick films were prepared on (100) LaAlO3 substrates using magnetron sputtering. The sputtering atmosphere, i.e. Ar/O-2 flow ratio, showed significant influence on the charge transport behaviors of BiFeO3 films. The distinct current density-electric field (J-E) characteristics of films were fitted to three charge transport models: ionic conduction, Schottky emission, and space-charge-limited-current (SCLC). These models were verified by an Auger depth profiling study, which revealed the chemical compositions of the films across their thicknesses. The apparent flow ratio dependence of charge transport in these films is well explained by the models with the supporting Auger data. (C) 2016 Elsevier Ltd. All rights reserved.
C1 [Zhu, Hanfei; Liu, Menglin; Yu, Zhenghai; Ouyang, Jun] Shandong Univ, Sch Mat Sci & Engn, Engn Ceram Key Lab Shandong Prov, Key Lab Liquid Solid Struct Evolut & Proc Mat,Min, Jinan 250061, Shandong, Peoples R China.
[Sun, Xin] Univ Missouri, Dept Mech & Aerosp Engn, Columbia, MO 65211 USA.
[Kang, Limin] Shandong Ind Ceram Res & Design Inst Co Ltd, Zibo 255031, Shandong, Peoples R China.
[Hong, Mina] George Washington Univ, Dept Chem, Washington, DC 20052 USA.
[Ouyang, Jun] NIST, Gaithersburg, MD 20899 USA.
RP Ouyang, J (reprint author), Shandong Univ, Sch Mat Sci & Engn, Engn Ceram Key Lab Shandong Prov, Key Lab Liquid Solid Struct Evolut & Proc Mat,Min, Jinan 250061, Shandong, Peoples R China.
EM ouyangjun@sdu.edu.cn
OI Ouyang, Jun/0000-0003-2446-2958
FU NSFC [91122024]; Program for New Century Excellent Talents in University
(State Education Ministry); State Key Laboratory of New Ceramics and
Fine Processing (Tsinghua University); Shandong University; Scientific
Research Foundation (SRF) for the Returned Overseas Chinese Scholars,
State Education Ministry (ROCS, SEM); Key Cultivating Projects of The
Interdisciplinary Research in Shandong University [2015JC034];
Nanotechnology Projects of Soochow City [ZXG201445]; Independent
Innovation Foundation of Shandong University [2015YQ009]
FX The authors acknowledge the financial support of the NSFC (Grant No.
91122024), Program for New Century Excellent Talents in University
(State Education Ministry), as well as the State Key Laboratory of New
Ceramics and Fine Processing (Tsinghua University). J. Ouyang would also
like to thank the "Qi-Lu Young Scholar Fund" of Shandong University, the
project sponsored by the Scientific Research Foundation (SRF) for the
Returned Overseas Chinese Scholars, State Education Ministry (ROCS,
SEM), and Key Cultivating Projects of The Interdisciplinary Research in
Shandong University (Grant No. 2015JC034). H. Zhu, Z. Yu, and J. Ouyang
acknowledge the financial support of the Nanotechnology Projects of
Soochow City (Grant # ZXG201445) and the Independent Innovation
Foundation of Shandong University (Grant No. 2015YQ009).
NR 29
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Z9 3
U1 7
U2 21
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 1359-6462
J9 SCRIPTA MATER
JI Scr. Mater.
PD APR 1
PY 2016
VL 115
BP 62
EP 65
DI 10.1016/j.scriptamat.2015.12.029
PG 4
WC Nanoscience & Nanotechnology; Materials Science, Multidisciplinary;
Metallurgy & Metallurgical Engineering
SC Science & Technology - Other Topics; Materials Science; Metallurgy &
Metallurgical Engineering
GA DE8NV
UT WOS:000370893800014
ER
PT J
AU Sisco, E
Forbes, TP
AF Sisco, Edward
Forbes, Thomas P.
TI Direct analysis in real time mass spectrometry of potential by-products
from homemade nitrate ester explosive synthesis
SO TALANTA
LA English
DT Article
DE Explosives; Nitrate esters; Direct analysis in real time; Mass
spectrometry; Forensic science
ID ELECTROSPRAY-IONIZATION; PENTAERYTHRITOL TETRANITRATE; TRACE DETECTION;
INSTRUMENTATION; IDENTIFICATION; MECHANISMS; CHEMISTRY; DESI; MS
AB This work demonstrates the coupling of direct analysis in real time (DART) ionization with time-of-flight mass spectrometry (MS) in an off-axis configuration for the trace detection and analysis of potential partially nitrated and dimerized by-products of homemade nitrate ester explosive synthesis. Five compounds relating to the synthesis of nitroglycerin (NG) and pentaerythritol tetranitrate (PETN) were examined. Deprotonated ions and adducts with molecular oxygen, nitrite, and nitrate were observed in the mass spectral responses of these compounds. A global optimum temperature of 350 degrees C for the by-products investigated here enabled single nanogram to sub nanogram trace detection. Matrix effects were examined through a series of mixtures containing one or more compounds (sugar alcohol precursors, by-products, and/or explosives) across a range of mass loadings. The explosives MS responses experienced competitive ionization in the presence of all by-products. The magnitude of this influence corresponded to both the degree of by-product nitration and the relative mass loading of the by-product to the explosive. This work provides a characterization of potential by-products from homemade nitrate ester synthesis, including matrix effects and potential challenges that might arise from the trace detection of homemade explosives (HMEs) containing impurities. Detection and understanding of HME impurities and complex mixtures may provide valuable information for the screening and sourcing of homemade nitrate ester explosives. Published by Elsevier B.V.
C1 [Sisco, Edward; Forbes, Thomas P.] NIST, Mat Measurement Sci Div, Gaithersburg, MD 20899 USA.
RP Sisco, E (reprint author), NIST, Mat Measurement Sci Div, Gaithersburg, MD 20899 USA.
EM edward.sisco@nist.gov
FU U.S. Department of Homeland Security Science and Technology Directorate
[IAA HSHQDC-12-X-00024]; National Institute of Standards and Technology
(NIST)
FX The U.S. Department of Homeland Security Science and Technology
Directorate sponsored a portion of the production of this material under
Interagency Agreement IAA HSHQDC-12-X-00024 with the National Institute
of Standards and Technology (NIST).
NR 22
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U1 10
U2 37
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0039-9140
EI 1873-3573
J9 TALANTA
JI Talanta
PD APR 1
PY 2016
VL 150
BP 177
EP 183
DI 10.1016/j.talanta.2015.12.013
PG 7
WC Chemistry, Analytical
SC Chemistry
GA DE6VA
UT WOS:000370770500024
PM 26838397
ER
PT J
AU Vico, F
Ferrando, M
Greengard, L
Gimbutas, Z
AF Vico, Felipe
Ferrando, Miguel
Greengard, Leslie
Gimbutas, Zydrunas
TI The Decoupled Potential Integral Equation for Time-Harmonic
Electromagnetic Scattering
SO COMMUNICATIONS ON PURE AND APPLIED MATHEMATICS
LA English
DT Article
ID EFIE; FREQUENCIES; OPERATORS
AB We present a new formulation for the problem of electromagnetic scattering from perfect electric conductors. While our representation for the electric and magnetic fields is based on the standard vector and scalar potentials A, phi in the Lorenz gauge, we establish boundary conditions on the potentials themselves rather than on the field quantities. This permits the development of a wellconditioned second-kind Fredholm integral equation that has no spurious resonances, avoids low-frequency breakdown, and is insensitive to the genus of the scatterer. The equations for the vector and scalar potentials are decoupled. That is, the unknown scalar potential defining the scattered field, phi(scat), is determined entirely by the incident scalar potential phi(inc). Likewise, the unknown vector potential defining the scattered field, A scat, is determined entirely by the incident vector potential A(inc). This decoupled formulation is valid not only in the static limit but for arbitrary omega >= 0. (C) 2016 Wiley Periodicals, Inc.
C1 [Vico, Felipe; Ferrando, Miguel] Univ Politecn Valencia, Inst Telecomunicac & Aplicac Multimedia ITEAM, E-46022 Valencia, Spain.
[Greengard, Leslie] NYU, Courant Inst, Simons Fdn, Simons Ctr Data Anal, 251 Mercer St, New York, NY 10012 USA.
[Gimbutas, Zydrunas] NIST, Informat Technol Lab, 325 Broadway,Mail Stop 891-01, Boulder, CO 80305 USA.
RP Vico, F; Ferrando, M (reprint author), Univ Politecn Valencia, Inst Telecomunicac & Aplicac Multimedia ITEAM, E-46022 Valencia, Spain.; Greengard, L (reprint author), NYU, Courant Inst, Simons Fdn, Simons Ctr Data Anal, 251 Mercer St, New York, NY 10012 USA.; Gimbutas, Z (reprint author), NIST, Informat Technol Lab, 325 Broadway,Mail Stop 891-01, Boulder, CO 80305 USA.
EM felipe.vico@gmail.com; mferrand@dcom.upv.es; greengard@cims.nyu.edu;
zydrunas.gimbutas@nist.gov
RI Ferrando Bataller, Miguel/O-2926-2013
OI Ferrando Bataller, Miguel/0000-0003-3561-5112
FU Applied Mathematical Sciences Program of the U.S. Department of Energy
[DE-FGO288ER25053]; Office of the Assistant Secretary of Defense for
Research and Engineering; AFOSR under NSSEFF Program [FA9550-10-1-0180];
Spanish Ministry of Science and Innovation (Ministerio de Ciencia e
Innovacion) [CSD2008-00068, TEC2010-20841-C04-01]
FX This work was supported in part by the Applied Mathematical Sciences
Program of the U.S. Department of Energy under Contract DE-FGO288ER25053
(L.G.), by the Office of the Assistant Secretary of Defense for Research
and Engineering and AFOSR under NSSEFF Program Award FA9550-10-1-0180
(L.G. and Z.G.), and in part by the Spanish Ministry of Science and
Innovation (Ministerio de Ciencia e Innovacion) under projects
CSD2008-00068 and TEC2010-20841-C04-01. The authors thank A. Klockner
and M. O'Neil for many useful discussions.
NR 37
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U1 0
U2 2
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0010-3640
EI 1097-0312
J9 COMMUN PUR APPL MATH
JI Commun. Pure Appl. Math.
PD APR
PY 2016
VL 69
IS 4
BP 771
EP 812
PG 42
WC Mathematics, Applied; Mathematics
SC Mathematics
GA DE5JS
UT WOS:000370667900007
ER
PT J
AU Deroba, JJ
Miller, TJ
AF Deroba, Jonathan J.
Miller, Timothy J.
TI Correct in theory but wrong in practice: Bias caused by using a
lognormal distribution to penalize annual recruitments in fish stock
assessment models
SO FISHERIES RESEARCH
LA English
DT Article
DE Likelihood; Recruitment; Assessment; Simulation; Fish
ID PRODUCTIVITY; SELECTIVITY
AB Penalties are widely used for a range of parameters while fitting fish stock assessment models. Penalizing annual recruitments for deviating from an underlying mean recruitment is probably the most common. Assuming that recruits are log-normally distributed for the purposes of this penalty is theoretically justifiable. In practice, however, bias may be induced because this distributional assumption includes a term equal to the summation of the log observed data, which in the case of recruitment equals the summation of the log recruitment parameters that are not data. Using simulation, the potential for bias caused by assuming that recruits were log-normally distributed was explored, and results were contrasted with the assumption that log-recruitment was normally distributed, an alternative that avoids the potentially troublesome summation term. Spawning stock biomass (SSB) and recruitment were negatively biased, while fishing mortality (F) was positively biased under the assumption of log-normally distributed recruitments, and the bias worsened closer to the terminal year. The bias also worsened when the true underlying F was low relative to natural mortality, and with domed fishery selectivity. Bias in SSB, recruitment, and F was nonexistent or relatively small under the assumption that log-recruitment was normally distributed. Distributional assumptions for penalties used in assessment models should be reviewed to reduce the potential for biased estimation. These results also provide further support for simulation testing to evaluate statistical behavior of assessment models. Published by Elsevier B.V.
C1 [Deroba, Jonathan J.; Miller, Timothy J.] NOAA Fisheries, Northeast Fisheries Sci Ctr, 166 Water St, Woods Hole, MA 02543 USA.
RP Deroba, JJ (reprint author), NOAA Fisheries, Northeast Fisheries Sci Ctr, 166 Water St, Woods Hole, MA 02543 USA.
EM jonathan.deroba@noaa.gov
NR 23
TC 1
Z9 1
U1 3
U2 9
PU ELSEVIER SCIENCE BV
PI AMSTERDAM
PA PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
SN 0165-7836
EI 1872-6763
J9 FISH RES
JI Fish Res.
PD APR
PY 2016
VL 176
BP 86
EP 93
DI 10.1016/j.fishres.2015.12.002
PG 8
WC Fisheries
SC Fisheries
GA DE0HZ
UT WOS:000370307000010
ER
PT J
AU Guzewich, SD
Newman, CE
Juarez, MD
Wilson, RJ
Lemmon, M
Smith, MD
Kahanpaa, H
Harri, AM
AF Guzewich, Scott D.
Newman, C. E.
Juarez, M. de la Torre
Wilson, R. J.
Lemmon, M.
Smith, M. D.
Kahanpaa, H.
Harri, A. -M.
CA REMS Sci Team
MSL Sci Team
TI Atmospheric tides in Gale Crater, Mars
SO ICARUS
LA English
DT Article
DE Mars, atmosphere; Atmospheres, dynamics; Meteorology
ID GENERAL-CIRCULATION MODEL; MARTIAN DUST CYCLE; WATER ICE CLOUDS; THERMAL
TIDES; INTERANNUAL VARIABILITY; OPTICAL DEPTH; STORMS; ROVER;
SIMULATION; CLIMATE
AB Atmospheric tides are the primary source of daily air pressure variation at the surface of Mars. These tides are forced by solar heating of the atmosphere and modulated by the presence of atmospheric dust, topography, and surface albedo and thermal inertia. This results in a complex mix of sun-synchronous and non sun-synchronous tides propagating both eastward and westward around the planet in periods that are integer fractions of a solar day. The Rover Environmental Monitoring Station on board the Mars Science Laboratory has observed air pressure at a regular cadence for over 1 Mars year and here we analyze and diagnose atmospheric tides in this pressure record. The diurnal tide amplitude varies from 26 to 63 Pa with an average phase of 0424 local true solar time, while the semidiurnal tide amplitude varies from 5 to 20 Pa with an average phase of 0929. We find that both the diurnal and semidiurnal tides in Gale Crater are highly correlated to atmospheric opacity variations at a value of 0.9 and to each other at a value of 0.77, with some key exceptions occurring during regional and local dust storms. We supplement our analysis with MarsWRF general circulation modeling to examine how a local dust storm impacts the diurnal tide in its vicinity. We find that both the diurnal tide amplitude enhancement and regional coverage of notable amplitude enhancement linearly scales with the size of the local dust storm. Our results provide the first long-term record of surface pressure tides near the martian equator. (C) 2015 Elsevier Inc. All rights reserved.
C1 [Guzewich, Scott D.] NASA GSFC, CRESST, Greenbelt, MD 20771 USA.
[Guzewich, Scott D.; Smith, M. D.] NASA GSFC, Planetary Syst Lab, Greenbelt, MD 20771 USA.
[Guzewich, Scott D.] Univ Space Res Assoc, 7178 Columbia Gateway Dr, Columbia, MD 21046 USA.
[Newman, C. E.] Ashima Res, Pasadena, CA 91106 USA.
[Juarez, M. de la Torre] CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91109 USA.
[Wilson, R. J.] Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA.
[Lemmon, M.] Texas A&M Univ, College Stn, TX 77843 USA.
[Kahanpaa, H.; Harri, A. -M.] Finnish Meteorol Inst, FIN-00101 Helsinki, Finland.
[Kahanpaa, H.] Aalto Univ, Espoo, Finland.
RP Guzewich, SD (reprint author), Univ Space Res Assoc, 7178 Columbia Gateway Dr, Columbia, MD 21046 USA.
RI Lemmon, Mark/E-9983-2010; Rodriguez-Manfredi, Jose/L-8001-2014;
Gonzalez, Rafael/D-1748-2009; Harri, Ari-Matti/C-7142-2012; Ramos,
Miguel/K-2230-2014;
OI Lemmon, Mark/0000-0002-4504-5136; Rodriguez-Manfredi,
Jose/0000-0003-0461-9815; Harri, Ari-Matti/0000-0001-8541-2802; Ramos,
Miguel/0000-0003-3648-6818; Guzewich, Scott/0000-0003-1149-7385
FU MSL Participating Scientist grant; MSL mission
FX This work was partially funded by a MSL Participating Scientist grant to
M.D. Smith. C.E. Newman, M. de la Torre Juarez, and M. Lemmon
acknowledge funding from the MSL mission, the REMS team, and the MastCam
team. MarsWRF simulations were conducted on the NASA Pleiades Advanced
Supercomputer system.
NR 46
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U1 4
U2 22
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 APR
PY 2016
VL 268
BP 37
EP 49
DI 10.1016/j.icarus.2015.12.028
PG 13
WC Astronomy & Astrophysics
SC Astronomy & Astrophysics
GA DD9AN
UT WOS:000370218100004
ER
PT J
AU Zhao, Q
Petersen, EJ
Cornelis, G
Wang, XL
Guo, XY
Tao, S
Xing, BS
AF Zhao, Qing
Petersen, Elijah J.
Cornelis, Geert
Wang, Xilong
Guo, Xiaoying
Tao, Shu
Xing, Baoshan
TI Retention of C-14-labeled multiwall carbon nanotubes by humic acid and
polymers: Roles of macromolecule properties
SO CARBON
LA English
DT Article
ID NATURAL ORGANIC-MATTER; COLLOIDAL STABILITY; ENVIRONMENTAL FATE;
ECOLOGICAL UPTAKE; SORPTION; WATER; NANOPARTICLES; SOILS; TRANSPORT;
IMPACT
AB Developing methods to measure interactions of carbon nanotubes (CNTs) with soils and sediments and understanding the impact of soil and sediment properties on CNT deposition are essential for assessing CNT environmental risks. In this study, we utilized functionalized carbon-14 labeled nanotubes to systematically investigate retention of multiwall CNTs (MWCNTs) by 3 humic acids, 3 natural biopolymers, and 10 model solid-phase polymers, collectively termed macromolecules. Surface properties, rather than bulk properties of macromolecules, greatly influenced MWCNT retention. As shown via multiple linear regression analysis and path analysis, aromaticity and surface polarity were the two most positive factors for retention, suggesting retention was regulated by pi-pi stacking and hydrogen bonding interactions. Moreover, MWCNT deposition was irreversible. These observations may explain the high retention of MWCNT in natural soils. Moreover, our findings on the relative contribution of each macromolecule property on CNT retention provide information on macromolecule selection for removal of MWCNTs from wastewater and provide a method for measuring CNT interactions with organic macromolecules. Published by Elsevier Ltd.
C1 [Zhao, Qing] Chinese Acad Sci, Inst Appl Ecol, Shenyang 110016, Peoples R China.
[Zhao, Qing; Xing, Baoshan] Univ Massachusetts, Stockbridge Sch Agr, Amherst, MA 01003 USA.
[Petersen, Elijah J.] NIST, Biosyst & Biomat Div, Gaithersburg, MD 20899 USA.
[Cornelis, Geert] Univ Gothenburg, Dept Chem & Mol Biol, S-41296 Gothenburg, Sweden.
[Wang, Xilong; Guo, Xiaoying; Tao, Shu] Peking Univ, Coll Urban & Environm Sci, Lab Earth Surface Proc, Beijing 100871, Peoples R China.
[Zhao, Qing] Chinese Acad Sci, Inst Appl Ecol, Key Lab Pollut Ecol & Environm Engn, Shenyang 110016, Peoples R China.
RP Xing, BS (reprint author), Univ Massachusetts, Stockbridge Sch Agr, Amherst, MA 01003 USA.; Petersen, EJ (reprint author), NIST, Biosyst & Biomat Div, Gaithersburg, MD 20899 USA.
EM Elijah.petersen@nist.gov; bx@umass.edu
RI Petersen, Elijah/E-3034-2013; Zhao, Qing/I-5749-2013; Zhao,
Qing/N-6541-2014; Cornelis, Geert/F-7044-2010;
OI Zhao, Qing/0000-0003-3192-3804; Zhao, Qing/0000-0003-2250-5571;
Cornelis, Geert/0000-0003-0078-6798; Petersen,
Elijah/0000-0001-8215-9127
FU Hundreds Talents Program of Chinese Academy of Sciences; CAS Pioneer
Hundred Talents Program; USDA-AFRI Hatch program [MAS 00475]; NSFC
[41328003]; 111 project [B14001]; Open Foundation of State Key
Laboratory of Environmental Criteria and Risk Assessment, Chinese
Research Academy of Environmental Sciences [SKLECRA2015OFP10]
FX This work was in part supported by the Hundreds Talents Program of
Chinese Academy of Sciences (2014-2019), CAS Pioneer Hundred Talents
Program (2015-2020), USDA-AFRI Hatch program (MAS 00475), NSFC
(41328003) and the 111 project (B14001) and Open Foundation of State Key
Laboratory of Environmental Criteria and Risk Assessment, Chinese
Research Academy of Environmental Sciences (SKLECRA2015OFP10). Certain
commercial equipment or materials are identified in this article in
order to specify adequately the experimental procedure. Such
identification does not imply recommendation or endorsement by the
National Institute of Standards and Technology, nor does it imply that
the materials or equipment identified are necessarily the best available
for the purpose.
NR 61
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U1 12
U2 41
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0008-6223
EI 1873-3891
J9 CARBON
JI Carbon
PD APR
PY 2016
VL 99
BP 229
EP 237
DI 10.1016/j.carbon.2015.12.024
PG 9
WC Chemistry, Physical; Materials Science, Multidisciplinary
SC Chemistry; Materials Science
GA DC2TP
UT WOS:000369069800027
PM 27458320
ER
PT J
AU Li, W
Cheng, GJ
Liang, YR
Tian, BY
Liang, XL
Peng, LM
Walker, ARH
Gundlach, DJ
Nguyen, NV
AF Li, Wei
Cheng, Guangjun
Liang, Yiran
Tian, Boyuan
Liang, Xuelei
Peng, Lianmao
Walker, A. R. Hight
Gundlach, David J.
Nguyen, Nhan V.
TI Broadband optical properties of graphene by spectroscopic ellipsometry
SO CARBON
LA English
DT Article
ID BILAYER GRAPHENE; FILMS
AB The optical properties of chemical vapor deposition grown graphene were measured with high accuracy by spectroscopy ellipsometry in the energy range of 0.7 eV-9.0 eV, which is spectrally broader compared with those reported in literature. The refractive index (n) and extinction coefficient (k) of graphene were accurately obtained and compared with directly measured transmittance data. The absorption of graphene follows the well-known fine structure constant in the visible range, becomes lower below 1 eV, and shows a strong absorption peak around 4.8 eV. The latter was attributed to the resonant excitons near the van Hove singularity at the M point of the Brillouin zone. A higher energy absorption peak was observed at 6.4 eV resulting from the excitonic effect of the sigma-to-sigma* transition at the Gamma point of the Brillouin zone. The multi-layer graphene, fabricated by repeated transfer, exhibit similar optical properties to mono-layer graphene and the 4.8 eV absorption peak exhibits a layer-number dependent peak shift, similar to the exfoliated AB-stacked multi-layer graphene. The broadband optical properties reported in this letter are believed to enhance the understanding of the optical properties of graphene and will benefit the development of graphene-based optoelectronic devices. (C) 2015 Elsevier Ltd. All rights reserved.
C1 [Li, Wei; Liang, Yiran; Tian, Boyuan; Liang, Xuelei; Peng, Lianmao] Peking Univ, Key Lab Phys & Chem Nanodevices, Beijing 100871, Peoples R China.
[Li, Wei; Liang, Yiran; Tian, Boyuan; Liang, Xuelei; Peng, Lianmao] Peking Univ, Dept Elect, Beijing 100871, Peoples R China.
[Li, Wei; Cheng, Guangjun; Walker, A. R. Hight; Gundlach, David J.; Nguyen, Nhan V.] NIST, Phys Measurement Lab, Gaithersburg, MD 20899 USA.
RP Liang, XL (reprint author), Peking Univ, Key Lab Phys & Chem Nanodevices, Beijing 100871, Peoples R China.; Liang, XL (reprint author), Peking Univ, Dept Elect, Beijing 100871, Peoples R China.; Nguyen, NV (reprint author), NIST, Phys Measurement Lab, Gaithersburg, MD 20899 USA.
EM liangxl@pku.edu.cn; Nhan.Nguyen@nist.gov
RI Liang, Xuelei/C-4690-2013; Peng, Lianmao/E-2089-2011; Hight Walker,
Angela/C-3373-2009
OI Hight Walker, Angela/0000-0003-1385-0672
FU Ministry of Science and Technology of China [2011CB921904]; Ministry of
education of China [113003A]; National Natural Science Foundation of
China [61321001]; Beijing Municipal Science & Technology Commission
[Z141100003814006]; National Institute of Standards and Technology
FX This work was supported by the Ministry of Science and Technology of
China (Grant No. 2011CB921904), the Ministry of education of China
(Grant No. 113003A), National Natural Science Foundation of China (Grant
No. 61321001) and Beijing Municipal Science & Technology Commission
(Grant No. Z141100003814006). Wei Li is partly supported by National
Institute of Standards and Technology. The authors are grateful to the
discussion with Alex Boosalis of University of Nebraska-Lincoln.
NR 38
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U1 15
U2 59
PU PERGAMON-ELSEVIER SCIENCE LTD
PI OXFORD
PA THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND
SN 0008-6223
EI 1873-3891
J9 CARBON
JI Carbon
PD APR
PY 2016
VL 99
BP 348
EP 353
DI 10.1016/j.carbon.2015.12.007
PG 6
WC Chemistry, Physical; Materials Science, Multidisciplinary
SC Chemistry; Materials Science
GA DC2TP
UT WOS:000369069800041
ER
PT J
AU Roberts, K
Simpson, M
Demner-Fushman, D
Voorhees, E
Hersh, W
AF Roberts, Kirk
Simpson, Matthew
Demner-Fushman, Dina
Voorhees, Ellen
Hersh, William
TI State-of-the-art in biomedical literature retrieval for clinical cases:
a survey of the TREC 2014 CDS track
SO INFORMATION RETRIEVAL
LA English
DT Article
DE Biomedical information retrieval; Clinical decision support; Information
retrieval evaluation
ID PERFORMANCE; INFORMATION; DISEASES; DATABASE; MEDLINE; CARE
AB Providing access to relevant biomedical literature in a clinical setting has the potential to bridge a critical gap in evidence-based medicine. Here, our goal is specifically to provide relevant articles to clinicians to improve their decision-making in diagnosing, treating, and testing patients. To this end, the TREC 2014 Clinical Decision Support Track evaluated a system's ability to retrieve relevant articles in one of three categories (Diagnosis, Treatment, Test) using an idealized form of a patient medical record . Over 100 submissions from over 25 participants were evaluated on 30 topics, resulting in over 37k relevance judgments. In this article, we provide an overview of the task, a survey of the information retrieval methods employed by the participants, an analysis of the results, and a discussion on the future directions for this challenging yet important task.
C1 [Roberts, Kirk; Simpson, Matthew; Demner-Fushman, Dina] Natl Lib Med, Lister Hill Natl Ctr Biomed Commun, NIH, Bethesda, MD USA.
[Voorhees, Ellen] NIST, Gaithersburg, MD 20899 USA.
[Hersh, William] Oregon Hlth & Sci Univ, Dept Med Informat & Clin Epidemiol, Portland, OR 97201 USA.
RP Roberts, K (reprint author), Natl Lib Med, Lister Hill Natl Ctr Biomed Commun, NIH, Bethesda, MD USA.
EM kirk.roberts@nih.gov
OI Hersh, William/0000-0002-4114-5148
FU intramural research program at U.S. National Library of Medicine,
National Institutes of Health
FX Kirk Roberts, Matthew Simpson, and Dina Demner-Fushman were supported by
the intramural research program at the U.S. National Library of
Medicine, National Institutes of Health. The authors would also like to
thank the following participants for providing feedback and
clarifications: Raymond Wan, Paul McNamee, Jean Garcia-Gathright, Joao
Palotti, Eva D'hondt, Dawit Girmay, Afshin Deroie, Sungbin Choi, Luca
Soldaini, Joe McCarthy, and Yi-Shu Wei.
NR 75
TC 3
Z9 3
U1 1
U2 2
PU SPRINGER
PI DORDRECHT
PA VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS
SN 1386-4564
EI 1573-7659
J9 INFORM RETRIEVAL
JI Inf. Retr.
PD APR
PY 2016
VL 19
IS 1-2
SI SI
BP 113
EP 148
DI 10.1007/s10791-015-9259-x
PG 36
WC Computer Science, Information Systems
SC Computer Science
GA DC1UM
UT WOS:000369002500006
ER
PT J
AU Muzzillo, CP
Campbell, CE
Anderson, TJ
AF Muzzillo, Christopher P.
Campbell, Carelyn E.
Anderson, Timothy J.
TI Cu-Ga-In thermodynamics: experimental study, modeling, and implications
for photovoltaics
SO JOURNAL OF MATERIALS SCIENCE
LA English
DT Article
ID CHALCOPYRITE THIN-FILMS; COPPER-INDIUM; SOLAR-CELLS; SELENIZATION
TECHNIQUE; LATTICE-PARAMETERS; PHASE-EQUILIBRIA; HEAT-CAPACITY;
BINARY-SYSTEM; AB-INITIO; ALLOYS
AB Both experimental measurements and assessment of phase equilibria are reported in the Cu-Ga-In material system, which is an important constituent in growth of the thin film photovoltaic absorber Cu(In,Ga)Se-2 (CIGS). Characterization of four different alloys using inductively coupled plasma atomic emission spectroscopy, X-ray diffraction, scanning electron microscopy, energy dispersive spectroscopy, differential thermal analysis, and differential scanning calorimetry has been conducted, and high-temperature equilibration studies have been performed on 2 of those. The new data are qualitatively consistent with the previous nonequilibrium thin film Cu-Ga-In observations. A thermodynamic assessment of the ternary system has also been performed using a CALPHAD approach after re-assessing the Cu-In constituent. The model fits the ternary data well in addition to the Cu-Ga, Cu-In, and Ga-In binary data. Practical applications of the model to metal precursors in a CIGS selenization process are discussed. Using the assessed parameters, the model predicts that at temperatures typically used in CIGS processes, Cu-Ga-In films should undergo equilibrium phase transformations. Slight changes in composition are found to determine whether or not these transitions occur, and at what temperature. Equilibrated precursor films are calculated to have high gamma-Cu-9(Ga,In)(4) phase content, where reducing equilibration and gamma-Cu-9(Ga,In)(4) formation have previously been found to improve photovoltaic performance.
C1 [Muzzillo, Christopher P.; Anderson, Timothy J.] Univ Florida, Dept Chem Engn, Gainesville, FL 32611 USA.
[Campbell, Carelyn E.] NIST, Gaithersburg, MD 20874 USA.
RP Muzzillo, CP (reprint author), Univ Florida, Dept Chem Engn, Gainesville, FL 32611 USA.
EM muzzillo@ufl.edu; tim@ufl.edu
FU U.S. Department of Energy under FPACE [DE-EE0005407]; Department of
Energy FPACE [DE-EE0005407]
FX The authors gratefully acknowledge funding from the U.S. Department of
Energy under FPACE contract DE-EE0005407. The authors would like to
thank GE for graciously providing bulk alloys and performing DSC, and
Thermo-Calc Software and CompuTherm LLC for providing software. This
study was funded by Department of Energy FPACE grant DE-EE0005407.
NR 87
TC 1
Z9 1
U1 6
U2 53
PU SPRINGER
PI NEW YORK
PA 233 SPRING ST, NEW YORK, NY 10013 USA
SN 0022-2461
EI 1573-4803
J9 J MATER SCI
JI J. Mater. Sci.
PD APR
PY 2016
VL 51
IS 7
BP 3362
EP 3379
DI 10.1007/s10853-015-9651-3
PG 18
WC Materials Science, Multidisciplinary
SC Materials Science
GA DA8KS
UT WOS:000368054100008
ER
PT J
AU Mamontov, E
Sharma, VK
Borreguero, JM
Tyagi, M
AF Mamontov, E.
Sharma, V. K.
Borreguero, J. M.
Tyagi, M.
TI Protein-Style Dynamical Transition in a Non-Biological Polymer and a
Non-Aqueous Solvent
SO JOURNAL OF PHYSICAL CHEMISTRY B
LA English
DT Article
ID ELASTIC NEUTRON-SCATTERING; AMORPHOUS POLYSTYRENE; HYDRATION WATER;
FLUCTUATIONS; MOTIONS
AB Temperature-dependent onset of apparent anharmonicity in the microscopic dynamics of hydrated proteins and other biomolecules has been known as protein dynamical transition for the last quarter of a century. Using neutron scattering and molecular dynamics simulation, techniques most often associated with protein dynamical transition studies, we have investigated the microscopic dynamics of one of the most common polymers, polystyrene, which was exposed to toluene vapor, mimicking the process of protein hydration from water vapor. Polystyrene with adsorbed toluene is an example of a solvent-solute system, which, unlike biopolymers, is anhydrous and lacks hydrogen bonding. Nevertheless, it exhibits the essential traits of the dynamical transition in biomolecules, such as a specific dependence of the microscopic dynamics of both solvent and host on the temperature and the amount of solvent adsorbed. We conclude that the protein dynamical transition is a manifestation of a universal solvent-solute dynamical relationship, which is not specific to either biomolecules as solute, or aqueous media as solvent, or even a particular type of interactions between solvent and solute.
C1 [Mamontov, E.] Oak Ridge Natl Lab, Neutron Sci Directorate, Chem & Engn Mat Div, Oak Ridge, TN 37831 USA.
[Sharma, V. K.] Oak Ridge Natl Lab, Neutron Sci Directorate, Biol & Soft Matter Div, Oak Ridge, TN 37831 USA.
[Sharma, V. K.] Bhabha Atom Res Ctr, Div Solid State Phys, Bombay 400085, Maharashtra, India.
[Borreguero, J. M.] Oak Ridge Natl Lab, Neutron Sci Directorate, Neutron Data Anal & Visualizat Div, Oak Ridge, TN 37831 USA.
[Tyagi, M.] NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Tyagi, M.] Univ Maryland, Dept Mat Sci & Engn, College Pk, MD 20742 USA.
RP Mamontov, E (reprint author), Oak Ridge Natl Lab, Neutron Sci Directorate, Chem & Engn Mat Div, Oak Ridge, TN 37831 USA.
EM mamontove@ornl.gov
RI Mamontov, Eugene/Q-1003-2015
OI Mamontov, Eugene/0000-0002-5684-2675
FU National Science Foundation [DMR-1508249]; Scientific User Facilities
Division, Office of Basic Energy Sciences, U.S. Department of Energy;
Center for Accelerating Materials Modeling (CAMM) - U.S. Department of
Energy, Basic Energy Sciences, Material Sciences and Engineering
Division [FWP-3ERKCSNL]; U.S. Department of Energy [DE-AC05-00OR22725]
FX The neutron scattering experiments on HFBS at NCNR were supported in
part by the National Science Foundation under Agreement No. DMR-1508249.
The neutron scattering experiments on BASIS at SNS were supported by the
Scientific User Facilities Division, Office of Basic Energy Sciences,
U.S. Department of Energy. J.M.B. is supported by the Center for
Accelerating Materials Modeling (CAMM) funded by the U.S. Department of
Energy, Basic Energy Sciences, Material Sciences and Engineering
Division under FWP-3ERKCSNL. This manuscript has been authored by
UT-Battelle, LLC under Contract No. DE-AC05-00OR22725 with the U.S.
Department of Energy. The United States Government retains and the
publisher, by accepting the article for publication, acknowledges that
the United States Government retains a nonexclusive, paid up,
irrevocable, worldwide license to publish or reproduce the published
form of this manuscript, or allow others to do so, for United States
Government purposes. The Department of Energy will provide public access
to these results of federally sponsored research in accordance with the
DOE Public Access Plan
(http://energy.gov/downloads/doe-public-access-plan). Certain commercial
material suppliers are identified in this paper to foster understanding.
Such identification does not imply recommendation or endorsement by the
National Institute of Standards and Technology, nor does it imply that
the materials or equipment identified are necessarily the best available
for the purpose. The authors declare no competing financial interests.
NR 36
TC 3
Z9 3
U1 0
U2 4
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 1520-6106
J9 J PHYS CHEM B
JI J. Phys. Chem. B
PD MAR 31
PY 2016
VL 120
IS 12
BP 3232
EP 3239
DI 10.1021/acs.jpcb.6b00866
PG 8
WC Chemistry, Physical
SC Chemistry
GA DI3RR
UT WOS:000373416700025
PM 26977709
ER
PT J
AU Osterberg, C
Fahlquist, H
Haussermann, U
Brown, CM
Udovic, TJ
Karlsson, M
AF Osterberg, Carin
Fahlquist, Henrik
Haussermann, Ulrich
Brown, Craig M.
Udovic, Terrence J.
Karlsson, Maths
TI Dynamics of Pyramidal SiH3- Ions in ASiH(3) (A = K and Rb) Investigated
with Quasielastic Neutron Scattering
SO JOURNAL OF PHYSICAL CHEMISTRY C
LA English
DT Article
ID HYDROGEN-STORAGE MATERIALS; BOROHYDRIDES MBH4 M; TETRAHYDROBORATE
ANIONS; POTASSIUM SILANIDE; CRYSTAL-STRUCTURES; ALUMINUM HYDRIDES;
LIBH4; SILYL; LITHIUM; KSIH3
AB The two alkali silanides ASiH(3) (A = K and Rb) were investigated by means of quasielastic neutron scattering, both below and above the order-disorder phase transition occurring at around 275-300 K. Measurements upon heating show that there is a large change in the dynamics on going through the phase transition, whereas measurements upon cooling reveal a strong hysteresis due to undercooling of the disordered phase. The results show that the dynamics is associated with rotational diffusion of SiH3- anions, adequately modeled by H-jumps among 24 different jump locations radially distributed around the Si atom. The average relaxation time between successive jumps is of the order of subpicoseconds and exhibits a weak temperature dependence with a small difference in activation energy between the two materials, 39(1) meV for KSiH3 and 33(1) meV for RbSiH3. The pronounced SiH3- dynamics explains the high entropy observed in the disordered phase resulting in the low entropy variation for hydrogen absorption/desorption and hence the origin of these materials' favorable hydrogen storage properties.
C1 [Osterberg, Carin; Karlsson, Maths] Chalmers, Dept Phys, SE-41296 Gothenburg, Sweden.
[Fahlquist, Henrik; Haussermann, Ulrich] Stockholm Univ, Dept Mat & Environm Chem, SE-10691 Stockholm, Sweden.
[Brown, Craig M.; Udovic, Terrence J.] NIST, Ctr Neutron Res, 100 Bur Dr, Gaithersburg, MD 20899 USA.
RP Karlsson, M (reprint author), Chalmers, Dept Phys, SE-41296 Gothenburg, Sweden.
EM maths.karlsson@chalmers.se
RI Brown, Craig/B-5430-2009
OI Brown, Craig/0000-0002-9637-9355
FU Swedish Foundation for Strategic Research [ICA10-0001]; Swedish Research
Council [2010-3519]; U.S. DOE EERE [DE-EE0002978]; Chalmers Area of
Advance in Materials Science; NSF [DMR-0944772]
FX This research was funded by the Swedish Foundation for Strategic
Research (Grant No. ICA10-0001), the Swedish Research Council (Grant No.
2010-3519), and the U.S. DOE EERE (Grant No. DE-EE0002978). A travel
grant by the Chalmers Area of Advance in Materials Science is also
gratefully acknowledged. The NIST Center for Neutron Research is thanked
for access to neutron beam facilities. This work utilized facilities
supported in part by the NSF under Agreement No. DMR-0944772.
NR 30
TC 6
Z9 6
U1 4
U2 16
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 MAR 31
PY 2016
VL 120
IS 12
BP 6369
EP 6376
DI 10.1021/acs.jpcc.6b00363
PG 8
WC Chemistry, Physical; Nanoscience & Nanotechnology; Materials Science,
Multidisciplinary
SC Chemistry; Science & Technology - Other Topics; Materials Science
GA DI3RP
UT WOS:000373416500009
ER
PT J
AU Turkovic, V
Engmann, S
Tsierkezos, N
Hoppe, H
Madsen, M
Rubahn, HG
Ritter, U
Gobsch, G
AF Turkovic, Vida
Engmann, Sebastian
Tsierkezos, Nikos
Hoppe, Harald
Madsen, Morten
Rubahn, Horst-Guenter
Ritter, Uwe
Gobsch, Gerhard
TI Long-term stabilization of organic solar cells using UV absorbers
SO JOURNAL OF PHYSICS D-APPLIED PHYSICS
LA English
DT Article
DE lifetime; degradation; stabilization; ternary blend; UV screening;
organic solar cells; Brazilian MRS
ID PHOTOVOLTAIC DEVICES; OXIDATION POTENTIALS; POLY(3-ALKYLTHIOPHENES);
ENCAPSULATION; STABILITY; LAYERS; PHOTOCHEMISTRY; PHOTOOXIDATION;
IONIZATION; MECHANISMS
AB We are reporting on the successful implementation of UV absorbers for the long-term stabilization of organic photovoltaic devices (OPV). A set of six commercially available representatives of main UV absorber classes, commonly used for insulating plastics, were ternary-blended into the active layer, and the OPV performances were recorded under International Summit on OPV Stability standards (ISOS-3) degradation conditions. An improvement in the long-term performance of the OPV devices, manifested in the accumulated power generation (APG) increase for over a factor of 3, was found for 2-(4,6-diphenyl-1,3,5-triazin-2-yl)-5-[(hexyl) oxy]phenol. This improvement is governed by a significantly decreased PCE loss during the burn-in period. Fourier transform infrared spectroscopy (FTIR) spectroscopy, used to trace chemical degradation over time, indicates that the stabilization of the active layer occurs due to a reduced formation of radicals facilitated by the UV screening properties of the additive.
C1 [Turkovic, Vida; Engmann, Sebastian; Hoppe, Harald; Gobsch, Gerhard] Ilmenau Univ Technol, Inst Phys, D-98683 Ilmenau, Germany.
[Turkovic, Vida; Engmann, Sebastian; Hoppe, Harald; Gobsch, Gerhard] Ilmenau Univ Technol, Inst Micro & Nanotechnol, D-98683 Ilmenau, Germany.
[Tsierkezos, Nikos; Ritter, Uwe] Ilmenau Univ Technol, Inst Chem & Biotechnol, D-98693 Ilmenau, Germany.
[Turkovic, Vida; Madsen, Morten; Rubahn, Horst-Guenter] Univ Southern Denmark, Mads Clausen Inst, DK-6400 Sonderborg, Denmark.
[Engmann, Sebastian] NIST, Mat Sci & Engn Div, Gaithersburg, MD 20899 USA.
RP Engmann, S (reprint author), Ilmenau Univ Technol, Inst Phys, D-98683 Ilmenau, Germany.; Engmann, S (reprint author), Ilmenau Univ Technol, Inst Micro & Nanotechnol, D-98683 Ilmenau, Germany.; Engmann, S (reprint author), NIST, Mat Sci & Engn Div, Gaithersburg, MD 20899 USA.
EM engmann@mci.sdu.dk
RI Hoppe, Harald/P-5293-2014; Madsen, Morten/K-8597-2012;
OI Engmann, Vida/0000-0001-5608-1362; Madsen, Morten/0000-0001-6503-0479
FU Federal State of Thuringia via the Landesgraduierten Stipendium; Federal
Ministry of Education and Research (BMBF) [03X3516F]; Interreg 4A
Syddanmark-Schleswig-K.E.R.N; Det Frie Forskningsrad
FX The authors would like to thank Katrin Risch for recording the FTIR
spectra and Doreen Schneider for additional CV measurements. We
thankfully acknowledge Dr Solon Economopoulos for his valuable
discussion on cyclic voltammetry. Financial support from the Federal
State of Thuringia via the Landesgraduierten Stipendium, from the
Federal Ministry of Education and Research (BMBF) for funding research
project EOS (Grant number 03X3516F), from Interreg 4A
Syddanmark-Schleswig-K.E.R.N. for funding project eMotion, and Det Frie
Forskningsrad for funding project StabilO is gratefully acknowledged.
NR 40
TC 0
Z9 0
U1 4
U2 33
PU IOP PUBLISHING LTD
PI BRISTOL
PA TEMPLE CIRCUS, TEMPLE WAY, BRISTOL BS1 6BE, ENGLAND
SN 0022-3727
EI 1361-6463
J9 J PHYS D APPL PHYS
JI J. Phys. D-Appl. Phys.
PD MAR 31
PY 2016
VL 49
IS 12
AR 125604
DI 10.1088/0022-3727/49/12/125604
PG 7
WC Physics, Applied
SC Physics
GA DF0QJ
UT WOS:000371043700027
ER
PT J
AU Contento, NM
Semancik, S
AF Contento, Nicholas M.
Semancik, Steve
TI Thermal characteristics of temperature-controlled electrochemical
microdevices
SO SENSORS AND ACTUATORS B-CHEMICAL
LA English
DT Article
DE Microheater; Temperature; Electrochemistry; Thermal imaging; Cyclic
voltammetry
ID GAS SENSOR ARRAY; HEATED ELECTRODES; MICROSENSORS; MICROELECTRODES;
AMPLIFICATION; VOLTAMMETRY; BACKGROUNDS; ACTIVATION; SYSTEMS; CHIP
AB The development of novel, miniaturized sensing systems is driven by the demand for better and faster chemical measurements with lower power consumption and smaller sample sizes. Emerging miniature sensors, or microsensors, also offer rapid thermal and diffusive transport characteristics. For instance, temperature changes, during both heating and cooling, can be achieved on micrometer-scale surfaces much more rapidly than on bulk, macro-scale surfaces. While these rapid thermal characteristics have been most successfully exploited to date in gas-phase sensing devices, the prospect of developing analogous microfabricated, temperature-controlled microsensors for use in aqueous, or solution-phase, environments has been less explored. In this work, electrodes with underlying microheaters were designed and fabricated, and thermal characterization was performed using temperature imaging, transient temperature measurements, and theoretical modeling to determine temperature distributions and thermal response times in both gas- and solution-phase environments. These results will guide the development of solution-phase electrochemical sensors. Temperature-controlled electrochemical characterization was performed using cyclic voltammetry of a model analyte, hexaamineruthenium(III) chloride, to demonstrate the use of the multilayer, microfabricated devices, which consisted of a gold disk electrode and an underlying microheater. Electrochemical signals were enhanced by up to a factor of three at elevated temperatures (up to 81 degrees C) compared to those measured at room temperature (21 degrees C). This improved signal at elevated temperatures was explained by finite element method calculations that accounted for both temperature-dependent diffusion and thermal convection near the heated electrode surface. Published by Elsevier B.V.
C1 [Contento, Nicholas M.; Semancik, Steve] NIST, Biomol Measurement Div, Gaithersburg, MD 20899 USA.
RP Contento, NM (reprint author), NIST, Biomol Measurement Div, Gaithersburg, MD 20899 USA.
EM nicholas.contento@nist.gov
FU National Research Council-National Institute of Standards and Technology
(NIST) Postdoctoral Associateship Program; Center for Nanoscale Science
and Technology's Nanofab at NIST
FX NMC acknowledges funding through an award from the National Research
Council-National Institute of Standards and Technology (NIST)
Postdoctoral Associateship Program. We thank M. Carrier and C.
Montgomery for helpful discussions and assistance with microfabrication
tools and techniques. We acknowledge technical support from the Center
for Nanoscale Science and Technology's Nanofab at NIST. We also thank B.
Lane of the NIST Intelligent Systems Division for assistance with IR
thermal imaging and suggestions about the IR temperature calibration
method used in this work.
NR 42
TC 0
Z9 1
U1 2
U2 30
PU ELSEVIER SCIENCE SA
PI LAUSANNE
PA PO BOX 564, 1001 LAUSANNE, SWITZERLAND
SN 0925-4005
J9 SENSOR ACTUAT B-CHEM
JI Sens. Actuator B-Chem.
PD MAR 31
PY 2016
VL 225
BP 279
EP 287
DI 10.1016/j.snb.2015.11.019
PG 9
WC Chemistry, Analytical; Electrochemistry; Instruments & Instrumentation
SC Chemistry; Electrochemistry; Instruments & Instrumentation
GA CY9XK
UT WOS:000366759500035
ER
PT J
AU Burgess, DR
AF Burgess, Donald R., Jr.
TI An Evaluation of Gas Phase Enthalpies of Formation for Hydrogen-Oxygen
(HxOy) Species
SO JOURNAL OF RESEARCH OF THE NATIONAL INSTITUTE OF STANDARDS AND
TECHNOLOGY
LA English
DT Article
DE ab initio thermochemistry; atomization energies; bond dissociation
energies; enthalpy of formation; hydrogen-oxygen species; thermochemical
network; thermodynamic properties
ID ACTIVE THERMOCHEMICAL TABLES; COMPLETE BASIS-SET; POTENTIAL-ENERGY
SURFACE; INFRARED ACTION SPECTROSCOPY; AB-INITIO THERMOCHEMISTRY;
BOND-DISSOCIATION ENERGY; ELECTRONIC GROUND-STATE; ROTATIONALLY RESOLVED
PHOTOIONIZATION; COUPLED-CLUSTER CALCULATIONS; ZERO-POINT ENERGIES
AB We have compiled gas phase enthalpies of formation for nine hydrogen-oxygen species (HxOy) and selected recommended values for H, O, OH, H2O, HO2, H2O2, O-3, HO3, and H2O3. The compilation consists of values derived from experimental measurements, quantum chemical calculations, and prior evaluations. This work updates the recommended values in the NIST-JANAF (1985) and Gurvich et al. (1989) thermochemical tables for seven species. For two species, HO3 and H2O3 (important in atmospheric chemistry) and not found in prior thermochemical evaluations, we also provide supplementary data consisting of molecular geometries, vibrational frequencies, and torsional potentials which can be used to compute thermochemical functions. For all species, we also provide supplementary data consisting of zero point energies, vibrational frequencies, and ion reaction energetics.
C1 [Burgess, Donald R., Jr.] NIST, Mat Measurement Lab, Div Chem Sci, Gaithersburg, MD 20899 USA.
RP Burgess, DR (reprint author), NIST, Mat Measurement Lab, Div Chem Sci, Gaithersburg, MD 20899 USA.
EM donald.burgess@nist.gov
NR 294
TC 0
Z9 0
U1 13
U2 16
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 MAR 30
PY 2016
VL 121
BP 108
EP 138
DI 10.6028/jres.121.005
PG 31
WC Instruments & Instrumentation; Physics, Applied
SC Instruments & Instrumentation; Physics
GA DQ5BB
UT WOS:000379218300001
ER
PT J
AU Samant, SP
Grabowski, CA
Kisslinger, K
Yager, KG
Yuan, GC
Satija, SK
Durstock, MF
Raghavan, D
Karim, A
AF Samant, Saumil P.
Grabowski, Christopher A.
Kisslinger, Kim
Yager, Kevin G.
Yuan, Guangcui
Satija, Sushil K.
Durstock, Michael F.
Raghavan, Dharmaraj
Karim, Alamgir
TI Directed Self-Assembly of Block Copolymers for High Breakdown Strength
Polymer Film Capacitors
SO ACS APPLIED MATERIALS & INTERFACES
LA English
DT Article
DE block copolymer; directed self-assembly; cold zone annealing soft-shear;
lamellae; breakdown strength; barrier effect; dielectric; capacitor
ID THIN-FILMS; DIELECTRIC-BREAKDOWN; SOLID DIELECTRICS; ELECTRIC-FIELD;
ENERGY; NANOCOMPOSITES; ORIENTATION; ALIGNMENT; NANOPARTICLES;
PERFORMANCE
AB Emerging needs for fast charge/discharge yet high-power, lightweight, and flexible electronics requires the use of polymer-film-based solid-state capacitors with high energy densities. Fast charge/discharge rates of film capacitors on the order of microseconds are not achievable with slower charging conventional batteries, supercapacitors and related hybrid technologies. However, the current energy densities of polymer film capacitors fall short of rising demand, and could be significantly enhanced by increasing the breakdown strength (E-BD) and dielectric permittivity (epsilon(r)) of the polymer films. Co-extruded two-homopolymer component multilayered films have demonstrated much promise in this regard showing higher E-BD over that of component polymers. Multilayered films can also help incorporate functional features besides energy storage, such as enhanced optical, mechanical, thermal and barrier properties. In this work, we report accomplishing multilayer, multicomponent block copolymer dielectric films (BCDF) with soft-shear driven highly oriented self-assembled lamellar diblock copolymers (BCP) as a novel application of this important class of self-assembling materials. Results of a model PS-b-PMMA system show similar to 50% enhancement in E-BD of self-assembled multilayer lamellar BCP films compared to unordered as-cast films, indicating that the breakdown is highly sensitive to the nanostructure of the BCP. The enhancement in E-BD is attributed to the "barrier effect", where the multiple interfaces between the lamellae block components act as barriers to the dielectric breakdown through the film. The increase in E-BD corresponds to more than doubling the energy storage capacity using a straightforward directed self-assembly strategy. This approach opens a new nanomaterial paradigm for designing high energy density dielectric materials.
C1 [Samant, Saumil P.; Karim, Alamgir] Univ Akron, Dept Polymer Engn, Akron, OH 44325 USA.
[Grabowski, Christopher A.; Durstock, Michael F.] Wright Patterson Air Force Base, Air Force Res Lab, Dayton, OH 45433 USA.
[Kisslinger, Kim; Yager, Kevin G.] Brookhaven Natl Lab, Ctr Funct Nanomat, Upton, NY 11973 USA.
[Yuan, Guangcui; Satija, Sushil K.] NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Raghavan, Dharmaraj] Howard Univ, Dept Chem, Washington, DC 20059 USA.
RP Karim, A (reprint author), Univ Akron, Dept Polymer Engn, Akron, OH 44325 USA.
EM alamgir@uakron.edu
FU Air Force Office of Scientific Research (AFOSR) [FA9550-12-1-0306];
National Science Foundation (NSF) [DMR-1006421]
FX This work was supported by Air Force Office of Scientific Research
(AFOSR) under contract No. FA9550-12-1-0306 and the National Science
Foundation (NSF) via Grant DMR-1006421.
NR 43
TC 7
Z9 7
U1 19
U2 59
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 MAR 30
PY 2016
VL 8
IS 12
BP 7966
EP 7976
DI 10.1021/acsami.5b11851
PG 11
WC Nanoscience & Nanotechnology; Materials Science, Multidisciplinary
SC Science & Technology - Other Topics; Materials Science
GA DI5DQ
UT WOS:000373519500043
PM 26942835
ER
PT J
AU Hume, DB
Leibrandt, DR
AF Hume, David B.
Leibrandt, David R.
TI Probing beyond the laser coherence time in optical clock comparisons
SO PHYSICAL REVIEW A
LA English
DT Article
ID ATOMIC CLOCKS; LATTICE CLOCKS; INSTABILITY; CONSTANTS; CAVITY; NOISE;
2ND
AB We develop differential measurement protocols that circumvent the laser noise limit in the stability of optical clock comparisons by synchronous probing of two clocks using phase-locked local oscillators. This allows for probe times longer than the laser coherence time, avoids the Dick effect, and supports Heisenberg-limited measurement precision. We present protocols for such frequency comparisons and develop numerical simulations of the protocols with realistic noise sources. These methods provide a route to reduce frequency ratio measurement durations by more than an order of magnitude.
C1 [Hume, David B.; Leibrandt, David R.] NIST, 325 Broadway, Boulder, CO 80305 USA.
RP Hume, DB (reprint author), NIST, 325 Broadway, Boulder, CO 80305 USA.
EM david.hume@nist.gov
FU Defense Advanced Research Projects Agency; Office of Naval Research
FX We thank T. Rosenband and D. Wineland for useful discussions related to
this work. We also thank K. Beloy and E. Knill for critical reading of
the manuscript. We acknowledge support from the Defense Advanced
Research Projects Agency and the Office of Naval Research. This work is
a contribution of the U.S. government, not subject to U.S. copyright.
NR 42
TC 1
Z9 1
U1 7
U2 11
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 2469-9926
EI 2469-9934
J9 PHYS REV A
JI Phys. Rev. A
PD MAR 30
PY 2016
VL 93
IS 3
AR 032138
DI 10.1103/PhysRevA.93.032138
PG 7
WC Optics; Physics, Atomic, Molecular & Chemical
SC Optics; Physics
GA DH9FH
UT WOS:000373101300003
ER
PT J
AU Docaj, A
Wall, ML
Mukherjee, R
Hazzard, KRA
AF Docaj, Andris
Wall, Michael L.
Mukherjee, Rick
Hazzard, Kaden R. A.
TI Ultracold Nonreactive Molecules in an Optical Lattice: Connecting
Chemistry to Many-Body Physics
SO PHYSICAL REVIEW LETTERS
LA English
DT Article
ID GROUND-STATE MOLECULES; POLAR-MOLECULES; QUANTUM GAS;
CHEMICAL-REACTIONS; ATOMS; COLD; TEMPERATURES
AB We derive effective lattice models for ultracold bosonic or fermionic nonreactive molecules (NRMs) in an optical lattice, analogous to the Hubbard model that describes ultracold atoms in a lattice. In stark contrast to the Hubbard model, which is commonly assumed to accurately describe NRMs, we find that the single on-site interaction parameter U is replaced by a multichannel interaction, whose properties we elucidate. Because this arises from complex short-range collisional physics, it requires no dipolar interactions and thus occurs even in the absence of an electric field or for homonuclear molecules. We find a crossover between coherent few-channel models and fully incoherent single-channel models as the lattice depth is increased. We show that the effective model parameters can be determined in lattice modulation experiments, which, consequently, measure molecular collision dynamics with a vastly sharper energy resolution than experiments in a free-space ultracold gas.
C1 [Docaj, Andris; Mukherjee, Rick; Hazzard, Kaden R. A.] Rice Univ, Dept Phys & Astron, Houston, TX 77005 USA.
[Docaj, Andris; Mukherjee, Rick; Hazzard, Kaden R. A.] Rice Univ, Rice Ctr Quantum Mat, Houston, TX 77005 USA.
[Wall, Michael L.] Univ Colorado, NIST, Joint Inst Lab Astrophys, Boulder, CO 80309 USA.
[Wall, Michael L.] Univ Colorado, Boulder, CO 80309 USA.
RP Hazzard, KRA (reprint author), Rice Univ, Dept Phys & Astron, Houston, TX 77005 USA.; Hazzard, KRA (reprint author), Rice Univ, Rice Ctr Quantum Mat, Houston, TX 77005 USA.
EM kaden.hazzard@gmail.com
FU Welch foundation [C-1872]; NRC
FX We thank John Bohn, Brandon Ruzic, Svetlana Kotochigova, Michael
Foss-Feig, Ana Maria Rey, Daniel Sheehy, Shah Alam, and Ian White for
useful discussions. K. R. A. H. acknowledges the Aspen Center for
Physics for its hospitality while part of this work was performed. This
work was supported with funds from the Welch foundation, Grant No.
C-1872. M. L. W. acknowledges support from the NRC postdoctoral
fellowship program.
NR 96
TC 1
Z9 1
U1 5
U2 9
PU AMER PHYSICAL SOC
PI COLLEGE PK
PA ONE PHYSICS ELLIPSE, COLLEGE PK, MD 20740-3844 USA
SN 0031-9007
EI 1079-7114
J9 PHYS REV LETT
JI Phys. Rev. Lett.
PD MAR 30
PY 2016
VL 116
IS 13
AR 135301
DI 10.1103/PhysRevLett.116.135301
PG 7
WC Physics, Multidisciplinary
SC Physics
GA DH9EP
UT WOS:000373099500010
PM 27081984
ER
PT J
AU Kim, G
Ahn, JB
Kryjov, VN
Sohn, SJ
Yun, WT
Graham, R
Kolli, RK
Kumar, A
Ceron, JP
AF Kim, Gayoung
Ahn, Joong-Bae
Kryjov, Vladimir N.
Sohn, Soo-Jin
Yun, Won-Tae
Graham, Richard
Kolli, Rupa K.
Kumar, Arun
Ceron, Jean-Pierre
TI Global and regional skill of the seasonal predictions by WMO Lead Centre
for Long-Range Forecast Multi-Model Ensemble
SO INTERNATIONAL JOURNAL OF CLIMATOLOGY
LA English
DT Article
DE WMO; long-range forecasts; Global Producing Centres; Lead Centre;
seasonal forecasts; multi-model ensemble; WMO LC-LRFMME
ID TO-INTERANNUAL PREDICTION; CLIMATE FILTER; SUPERENSEMBLE; IMPROVEMENT;
PRECIPITATION; DEMETER; WEATHER; SYSTEM
AB The World Meteorological Organization (WMO) Lead Centre for Long-Range Forecast Multi-Model Ensemble (WMO LC-LRFMME) has been established to collect and share long-range forecasts from the WMO designated Global Producing Centres (GPC). In this study, the seasonal skill of the deterministic multi-model prediction of GPCs in WMO LC-LRFMME is investigated. The GPC models included in the analysis cover 30 years of common hindcast period from 1981 to 2010 and real-time forecast for the period from DJF2011/2012 to SON2014. The equal-weighted multi-model ensemble (MME) method is used to produce the MME forecast. We show that the GPC models generally capture the observed climatological patterns and seasonal variations in temperature and precipitation. However, some systematic biases/errors in simulation of the climatological mean patterns and zonal mean profiles are also found, most of which are located in mid-latitudes or high latitudes. The temporal correlation coefficients both of 2 m temperature and precipitation in the tropical region (especially over the ocean) exceed 95%, but drop gradually towards high latitudes and are even negative in the polar region for precipitation. The prediction skills of individual models and the MME over 13 regional climate outlook forum (RCOF) regions for four calendar seasons are also assessed. The prediction skills vary with season and region, with the highest skill being demonstrated by the MME forecasts for the regions of the tropical RCOFs. These predictions are strongly affected by the ENSO over Pacific Islands, Southeast Asia and Central America. Additionally, Southeast of South America and North Eurasian regions show relatively low skills for all seasons when compared to other regions.
C1 [Kim, Gayoung; Kryjov, Vladimir N.; Sohn, Soo-Jin] APEC Climate Ctr, Climate Res Dept, 12 Centum 7 Ro, Busan 612020, South Korea.
[Kim, Gayoung; Ahn, Joong-Bae] Pusan Natl Univ, Div Earth Environm Syst, Pusan, South Korea.
[Yun, Won-Tae] Natl Typhoon Ctr, Korea Meteorol Adm, Seogwipo, South Korea.
[Graham, Richard] Met Off Hadley Ctr, Monthly Decadal Predict, Exeter, Devon, England.
[Kolli, Rupa K.] World Meteorol Org, World Climate Applicat & Serv Div, Geneva, Switzerland.
[Kumar, Arun] Natl Ctr Environm Predict, Climate Predict Ctr, College Pk, MD USA.
[Ceron, Jean-Pierre] Meteo France, Direct Climatol, Toulouse, France.
RP Kryjov, VN (reprint author), APEC Climate Ctr, Climate Res Dept, 12 Centum 7 Ro, Busan 612020, South Korea.
EM kryjov@yahoo.co.uk
FU APEC Climate Center; Rural Development Administration cooperative
Research Program for Agriculture and Technology Development [PJ009953];
Korea Meteorological Administration Research and Development
[KMIPA2015-2081]; Republic of Korea
FX The authors appreciate the participating institutes of the WMO LC-LRFMME
multi-model ensemble operational system for providing hindcast and
forecast experimental data. G. Kim, V. Kryjov and S.-J. Sohn received
support from the APEC Climate Center. The NCEP-DOE reanalysis 2 used in
the study was obtained from the NOAA/OAR/ESRL PSD, Boulder, CO, USA
(http://www.esrl.noaa.gov/psd/). The CAMS OPI monthly estimates were
acquired from the NOAA/CPC ftp site
(ftp://ftp.cpc.ncep.noaa.gov/precip/data-req/cams_opi_v0208). This work
was conducted with the support of the Rural Development Administration
cooperative Research Program for Agriculture and Technology Development
under Grant No. PJ009953, Republic of Korea, and the Korea
Meteorological Administration Research and Development Program under
Grant KMIPA2015-2081.
NR 27
TC 1
Z9 1
U1 2
U2 6
PU WILEY-BLACKWELL
PI HOBOKEN
PA 111 RIVER ST, HOBOKEN 07030-5774, NJ USA
SN 0899-8418
EI 1097-0088
J9 INT J CLIMATOL
JI Int. J. Climatol.
PD MAR 30
PY 2016
VL 36
IS 4
BP 1657
EP 1675
DI 10.1002/joc.4449
PG 19
WC Meteorology & Atmospheric Sciences
SC Meteorology & Atmospheric Sciences
GA DG4IV
UT WOS:000372036800007
ER
PT J
AU Weijerman, M
Fulton, EA
Brainard, RE
AF Weijerman, Mariska
Fulton, Elizabeth A.
Brainard, Russell E.
TI Management Strategy Evaluation Applied to Coral Reef Ecosystems in
Support of Ecosystem-Based Management
SO PLOS ONE
LA English
DT Article
ID GREAT-BARRIER-REEF; MARINE RESERVES; FISHERIES MANAGEMENT; BENEFITS;
DISTURBANCE; RESILIENCE; STRESSORS; DIVERSITY; SERVICES; DECLINE
AB Ecosystem modelling is increasingly used to explore ecosystem-level effects of changing environmental conditions and management actions. For coral reefs there has been increasing interest in recent decades in the use of ecosystem models for evaluating the effects of fishing and the efficacy of marine protected areas. However, ecosystem models that integrate physical forcings, biogeochemical and ecological dynamics, and human induced perturbations are still underdeveloped. We applied an ecosystem model (Atlantis) to the coral reef ecosystem of Guam using a suite of management scenarios prioritized in consultation with local resource managers to review the effects of each scenario on performance measures related to the ecosystem, the reef-fish fishery (e.g., fish landings) and coral habitat. Comparing tradeoffs across the selected scenarios showed that each scenario performed best for at least one of the selected performance indicators. The integrated 'full regulation' scenario outperformed other scenarios with four out of the six performance metrics at the cost of reef-fish landings. This model application quantifies the socio-ecological costs and benefits of alternative management scenarios. When the effects of climate change were taken into account, several scenarios performed equally well, but none prevented a collapse in coral biomass over the next few decades assuming a business-as-usual greenhouse gas emissions scenario.
C1 [Weijerman, Mariska] Univ Hawaii Manoa, Joint Inst Marine & Atmospher Res, Honolulu, HI 96822 USA.
[Weijerman, Mariska] Wageningen Univ, Environm Syst Anal Grp, NL-6700 AP Wageningen, Netherlands.
[Weijerman, Mariska; Brainard, Russell E.] NOAA, Coral Reef Ecosystem Program, Pacific Isl Fisheries Sci Ctr, Honolulu, HI USA.
[Fulton, Elizabeth A.] CSIRO Oceans & Atmosphere, Hobart, Tas, Australia.
[Fulton, Elizabeth A.] Univ Tasmania, Ctr Marine Socioecol, Hobart, Tas, Australia.
RP Weijerman, M (reprint author), Univ Hawaii Manoa, Joint Inst Marine & Atmospher Res, Honolulu, HI 96822 USA.; Weijerman, M (reprint author), Wageningen Univ, Environm Syst Anal Grp, NL-6700 AP Wageningen, Netherlands.; Weijerman, M (reprint author), NOAA, Coral Reef Ecosystem Program, Pacific Isl Fisheries Sci Ctr, Honolulu, HI USA.
EM mariska.weijerman@noaa.gov
RI Fulton, Elizabeth/A-2871-2008
OI Fulton, Elizabeth/0000-0002-5904-7917
FU National Oceanic and Atmospheric Administration; NOAA
FX Funding was provided to MW though the National Oceanic and Atmospheric
Administration. The funder had no role in study design, data collection
and analysis, decision to publish, or preparation of the manuscript.;
Funding was provided to MW through NOAA. We gratefully acknowledge the
staff of NOAA PIFSC CREP and PIRO Habitat Division, and staff of Guam
Division of Aquatic and Wildlife Resources, Coastal Management Program
and Guam University for their contributions in data and/or discussions.
We further would like to acknowledge Ivor Williams, Adel Heenan, John
Rooney, Brett Taylor for their improvements to the manuscript.
NR 54
TC 3
Z9 3
U1 14
U2 36
PU PUBLIC LIBRARY SCIENCE
PI SAN FRANCISCO
PA 1160 BATTERY STREET, STE 100, SAN FRANCISCO, CA 94111 USA
SN 1932-6203
J9 PLOS ONE
JI PLoS One
PD MAR 29
PY 2016
VL 11
IS 3
AR e0152577
DI 10.1371/journal.pone.0152577
PG 17
WC Multidisciplinary Sciences
SC Science & Technology - Other Topics
GA DH9KB
UT WOS:000373113900080
PM 27023183
ER
PT J
AU Sumino, Y
Yamada, NL
Nagao, M
Honda, T
Kitahata, H
Melnichenko, YB
Seto, H
AF Sumino, Yutaka
Yamada, Norifumi L.
Nagao, Michihiro
Honda, Takuya
Kitahata, Hiroyuki
Melnichenko, Yuri B.
Seto, Hideki
TI Mechanism of Spontaneous Blebbing Motion of an Oil-Water Interface:
Elastic Stress Generated by a Lamellar-Lamellar Transition
SO LANGMUIR
LA English
DT Article
ID ALCOHOL; SURFACTANT; CHLORIDE; SYSTEM
AB A quaternary system composed of surfactant, cosurfactant, oil, and water showing spontaneous motion of the oil-water interface-under far-from-equilibrium condition is studied in order to understand nanometer-scale structures and their roles in spontaneous motion. The interfacial motion is characterized by the repetitive. extension and retraction of spherical protrusions at the interface, i.e, blebbing motion. During, the, blebbing motion, elastic aggregates are accumulated, which were characterized as surfactant lamellar structures with mean repeat distances d of 25 to 40 nm. Still unclear is the relationship between the structure formation and, the dynamics of the interfacial motion. In the present study, we find that a new lamellar structure with d larger than. 80 run is formed at. the blebbing oil-water interface,. while the resultant elastic aggregates, which are the one reported before, have a lamellar structure with smaller d (25 to 40 nm). Such transition of lamellar structures from the larger d to smaller d is induced by a penetration of surfactants from an aqueous phase into the aggregates. We propose a model in which elastic stress generated by the transition-drives the blebbing motion at the interface. The present results explain the link between nanometer-scale transition of lamellar structure and millimeter-scale dynamics at an oil water interface.
C1 [Sumino, Yutaka] Tokyo Univ Sci, Fac Sci, Dept Appl Phys, Tokyo 1258585, Japan.
[Yamada, Norifumi L.; Seto, Hideki] High Energy Accelerator Res Org, Inst Mat Struct Sci, KENS&CMRC, Tokai, Ibaraki 3190016, Japan.
[Nagao, Michihiro] NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA.
[Nagao, Michihiro] Indiana Univ, Ctr Explorat Energy & Matter, Bloomington, IN 47408 USA.
[Honda, Takuya] Aichi Univ Educ, Dept Educ, Kariya, Aichi 4488542, Japan.
[Kitahata, Hiroyuki] Chiba Univ, Grad Sch Sci, Dept Phys, Chiba, Chiba 2638522, Japan.
[Melnichenko, Yuri B.] Oak Ridge Natl Lab, Biol & Soft Matter Div, Oak Ridge, TN 37831 USA.
RP Sumino, Y (reprint author), Tokyo Univ Sci, Fac Sci, Dept Appl Phys, Tokyo 1258585, Japan.
EM ysumino@rs.tus.ac.jp
RI Kitahata, Hiroyuki/E-8635-2015;
OI Kitahata, Hiroyuki/0000-0003-3453-9883; Seto, Hideki/0000-0002-1658-3576
FU JSPS [24740287]; U.S.-Japan Cooperative Program on Neutron Scattering;
NIST, U.S. Department of Commerce [70NANB10H255]; Scientific User
Facilities Division, office of Basic Energy Sciences, U.S. Department of
Energy
FX This work was supported in part by a Grant-in-Aid for Young Scientists B
by JSPS to Y.S. (No. 24740287) and by the U.S.-Japan Cooperative Program
on Neutron Scattering, and also performed under the Cooperative Research
Program of "Network Joint Research Center for Materials and Devices."
M.N. acknowledges the funding support of cooperative agreement
70NANB10H255 from NIST, U.S. Department of Commerce. The authors wish to
thank M. Hishida (University of Tsukuba) for helpful discussions. The
SAXS analyses were performed under the approval of the Photon Factory
Program Advisory Committee (Proposal Nos. 2013G530 and 2013G525). The
authors also extend special thanks to N. Igarashi and N. Shimizu (Photon
Factory, KEK) for their invaluable assistance in obtaining data from
beamline BL6A. The SANS analyses were performed under the approval of
the HFIR (Cycle 445 CG-2; IPTS-7094). The research at Oak Ridge National
Laboratory's High Flux Isotope Reactor was sponsored by the Scientific
User Facilities Division, office of Basic Energy Sciences, U.S.
Department of Energy.
NR 22
TC 0
Z9 0
U1 4
U2 9
PU AMER CHEMICAL SOC
PI WASHINGTON
PA 1155 16TH ST, NW, WASHINGTON, DC 20036 USA
SN 0743-7463
J9 LANGMUIR
JI Langmuir
PD MAR 29
PY 2016
VL 32
IS 12
BP 2891
EP 2899
DI 10.1021/acs.langmuir.6b00107
PG 9
WC Chemistry, Multidisciplinary; Chemistry, Physical; Materials Science,
Multidisciplinary
SC Chemistry; Materials Science
GA DI1HO
UT WOS:000373247400006
PM 26938640
ER
PT J
AU Le, G
Luhr, H
Anderson, BJ
Strangeway, RJ
Russell, CT
Singer, H
Slavin, JA
Zhang, Y
Huang, T
Bromund, K
Chi, PJ
Lu, G
Fischer, D
Kepko, EL
Leinweber, HK
Magnes, W
Nakamura, R
Plaschke, F
Park, J
Rauberg, J
Stolle, C
Torbert, RB
AF Le, G.
Luehr, H.
Anderson, B. J.
Strangeway, R. J.
Russell, C. T.
Singer, H.
Slavin, J. A.
Zhang, Y.
Huang, T.
Bromund, K.
Chi, P. J.
Lu, G.
Fischer, D.
Kepko, E. L.
Leinweber, H. K.
Magnes, W.
Nakamura, R.
Plaschke, F.
Park, J.
Rauberg, J.
Stolle, C.
Torbert, R. B.
TI Magnetopause erosion during the 17 March 2015 magnetic storm: Combined
field-aligned currents, auroral oval, and magnetopause observations
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
DE magnetopause erosion; magnetic reconnection; field-aligned currents;
Birkland currents; auroral oval; solar wind-magnetosphere interaction
ID SOLAR-WIND CONTROL; DAYSIDE MAGNETOSPHERE; BIRKELAND CURRENTS;
MAGNETOMETER DATA; FLUX TRANSFER; SHAPE; LOCATION; SYSTEM; MOTION; ANGLE
AB We present multimission observations of field-aligned currents, auroral oval, and magnetopause crossings during the 17 March 2015 magnetic storm. Dayside reconnection is expected to transport magnetic flux, strengthen field-aligned currents, lead to polar cap expansion and magnetopause erosion. Our multimission observations assemble evidence for all these manifestations. After a prolonged period of strongly southward interplanetary magnetic field, Swarm and AMPERE observe significant intensification of field-aligned currents. The dayside auroral oval, as seen by DMSP, appears as a thin arc associated with ongoing dayside reconnection. Both the field-aligned currents and the auroral arc move equatorward reaching as low as similar to 60 degrees magnetic latitude. Strong magnetopause erosion is evident in the in situ measurements of the magnetopause crossings by GOES 13/15 and MMS. The coordinated Swarm, AMPERE, DMSP, MMS and GOES observations, with both global and in situ coverage of the key regions, provide a clear demonstration of the effects of dayside reconnection on the entire magnetosphere.
C1 [Le, G.; Bromund, K.; Kepko, E. L.] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
[Luehr, H.; Huang, T.; Rauberg, J.; Stolle, C.] GFZ German Res Ctr Geosci, Potsdam, Germany.
[Anderson, B. J.; Zhang, Y.] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD USA.
[Strangeway, R. J.; Russell, C. T.; Chi, P. J.; Leinweber, H. K.] Univ Calif Los Angeles, Inst Geophys & Planetary Phys & Earth, Los Angeles, CA USA.
[Strangeway, R. J.; Russell, C. T.; Chi, P. J.; Leinweber, H. K.] Univ Calif Los Angeles, Dept Space Sci, Los Angeles, CA USA.
[Singer, H.] NOAA, Space Weather Predict Ctr, Boulder, CO USA.
[Slavin, J. A.] Univ Michigan, Dept Climate & Space Sci & Engn, Ann Arbor, MI 48109 USA.
[Lu, G.] UCAR, High Altitude Observ, Boulder, CO USA.
[Fischer, D.; Magnes, W.; Nakamura, R.; Plaschke, F.] Austrian Acad Sci, Space Res Inst, A-8010 Graz, Austria.
[Park, J.] Korea Astron & Space Sci Inst, Daejeon, South Korea.
[Torbert, R. B.] Univ New Hampshire, Dept Phys, Durham, NH 03824 USA.
RP Le, G (reprint author), NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.
EM Guan.Le@nasa.gov
RI Nakamura, Rumi/I-7712-2013; Le, Guan/C-9524-2012; NASA MMS, Science
Team/J-5393-2013; Slavin, James/H-3170-2012; Zhang,
Yongliang/C-2180-2016
OI Nakamura, Rumi/0000-0002-2620-9211; Le, Guan/0000-0002-9504-5214; NASA
MMS, Science Team/0000-0002-9504-5214; Slavin,
James/0000-0002-9206-724X; Zhang, Yongliang/0000-0003-4851-1662
FU NSF [ATM-0739864, ATM-1420184]
FX We thank O. Le Contel and S. Petrinec for useful discussions. AMPERE
development, data acquisition, and science processing were supported by
NSF awards ATM-0739864 and ATM-1420184 to JHU/APL, and all products used
here are available via http://ampere.jhuapl.edu. We thank the JHU/APL
SSUSI team for providing the DMSP F18 SSUSI auroral data. The European
Space Agency is acknowledged for providing the Swarm data. The Swarm
data used in this paper are freely accessible at
https://earth.esa.int/guest/swarm/data-access. We acknowledge use of
NASA/GSFC's Space Physics Data Facility's CDAWeb service for obtaining
the ACE interplanetary magnetic field data, ACE solar wind plasma data,
and the SYM-H index. We acknowledge use of NOAA Space Weather Prediction
Center for obtaining GOES magnetometer data. We thank the entire team of
NASA's MMS mission for the dedication and expertise in its successful
development and operations.
NR 41
TC 3
Z9 3
U1 4
U2 9
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 MAR 28
PY 2016
VL 43
IS 6
BP 2396
EP 2404
DI 10.1002/2016GL068257
PG 9
WC Geosciences, Multidisciplinary
SC Geology
GA DK1TM
UT WOS:000374697200008
ER
PT J
AU Maruyama, N
Sun, YY
Richards, PG
Middlecoff, J
Fang, TW
Fuller-Rowell, TJ
Akmaev, RA
Liu, JY
Valladares, CE
AF Maruyama, Naomi
Sun, Yang-Yi
Richards, Phillip G.
Middlecoff, Jacques
Fang, Tzu-Wei
Fuller-Rowell, Timothy J.
Akmaev, Rashid A.
Liu, Jaun-Yeng
Valladares, Cesar E.
TI A new source of the midlatitude ionospheric peak density structure
revealed by a new Ionosphere-Plasmasphere model
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
DE midlatitude ionosphere; new plasma density peak; new ionosphere model
ID EQUATORIAL F-REGION; ATMOSPHERE; WINDS
AB The newly developed Ionosphere-Plasmasphere (IP) model has revealed neutral winds as a primary source of the third-peak density structure in the daytime global ionosphere that has been observed by the low-latitude ionospheric sensor network GPS total electron content measurements over South America. This third peak is located near -30 degrees magnetic latitude and is clearly separate from the conventional twin equatorial ionization anomaly peaks. The IP model reproduces the global electron density structure as observed by the FORMOSAT-3/COSMIC mission. The model reveals that the third peak is mainly created by the prevailing neutral meridional wind, which flows from the summer hemisphere to the winter hemisphere lifting the plasma along magnetic field lines to higher altitudes where recombination is slower. The same prevailing wind that increases the midlatitude density decreases the low-latitude density in the summer hemisphere by counteracting the equatorial fountain flow. The longitudinal variation of the three-peak structure is explained by the displacement between the geographic and geomagnetic equators.
C1 [Maruyama, Naomi; Sun, Yang-Yi; Fang, Tzu-Wei; Fuller-Rowell, Timothy J.] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
[Maruyama, Naomi; Sun, Yang-Yi; Fang, Tzu-Wei; Fuller-Rowell, Timothy J.; Akmaev, Rashid A.] NOAA, Space Weather Predict Ctr, Boulder, CO USA.
[Sun, Yang-Yi; Liu, Jaun-Yeng] Natl Cent Univ, Inst Space Sci, Taoyuan, Taiwan.
[Richards, Phillip G.] George Mason Univ, Dept Phys & Astron, Fairfax, VA 22030 USA.
[Middlecoff, Jacques] Colorado State Univ, Cooperat Inst Res Atmosphere, Ft Collins, CO 80523 USA.
[Middlecoff, Jacques] NOAA, Global Syst Div, Boulder, CO USA.
[Valladares, Cesar E.] Boston Coll, Inst Sci Res, Chestnut Hill, MA 02167 USA.
RP Maruyama, N (reprint author), Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.; Maruyama, N (reprint author), NOAA, Space Weather Predict Ctr, Boulder, CO USA.
EM naomi.maruyama@noaa.gov
RI Liu, Jann-Yenq/Q-1668-2015
FU National Science Foundation (NSF) [ATM-1103149, ATM-1042258,
ATM-1452298]; NASA [NNX13AF77G, NNX16AB83G, NNX15AI90G]; Taiwan National
Science Council (NSC) [NSC 102-2628-M-008-001]; Air Force Research
Laboratory [FA8718-09-C-0041]; NSF [ATM-1135675, ATM-1242476]; NASA LWS
[NNX11AP02G]
FX This material is based upon work supported by the National Science
Foundation (NSF grant ATM-1103149, ATM-1042258, and ATM-1452298), NASA
awards NNX13AF77G and NNX16AB83G to the University of Colorado at
Boulder, and the Taiwan National Science Council (NSC) grant NSC
102-2628-M-008-001. The authors thank COSMIC Data Analysis and Archival
Center (CDAAC) and Taiwan Analysis Center for COSMIC (TACC) for making
the F3/C data available online. Cesar E. Valladares was partially
supported by Air Force Research Laboratory contract FA8718-09-C-0041,
NSF grants ATM-1135675 and ATM-1242476, and NASA LWS grant NNX11AP02G.
Phillip G. Richards was supported by NASA grant NNX15AI90G to George
Mason University.
NR 21
TC 1
Z9 1
U1 1
U2 4
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 MAR 28
PY 2016
VL 43
IS 6
BP 2429
EP 2435
DI 10.1002/2015GL067312
PG 7
WC Geosciences, Multidisciplinary
SC Geology
GA DK1TM
UT WOS:000374697200012
ER
PT J
AU Baddock, MC
Ginoux, P
Bullard, JE
Gill, TE
AF Baddock, Matthew C.
Ginoux, Paul
Bullard, Joanna E.
Gill, Thomas E.
TI Do MODIS-defined dust sources have a geomorphological signature?
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
DE aerosol; dust; MODIS; geomorphology
ID CHIHUAHUAN DESERT; MOJAVE DESERT; IMPACTS; COVER; USA; DEPOSITION;
CALIFORNIA; PARTICLES; SYSTEM; STORM
AB The preferential dust source (PDS) scheme enables large-scale mapping of geomorphology in terms of importance for dust emissions but has not been independently tested other than at local scales. We examine the PDS qualitative conceptual model of surface emissivity alongside a quantitative measurement of dust loading from Moderate Resolution Imaging Spectroradiometer (MODIS) Deep Blue Collection 6 for the Chihuahuan Desert. The predicted ranked importance of each geomorphic type for dust emissions is compared with the actual ranked importance as determined from the satellite-derived dust loading. For this region, the predicted variability and magnitude of dust emissions from most surface types present coincides with the observed characteristics demonstrating the significance of geomorphological controls on emission. The exception is for areas of low magnitude but persistent emissions such as alluvial surfaces where PDS overpredicts dustiness. As PDS is a good predictor of emissions and incorporates surface dynamics it could improve models of future dust emissions.
C1 [Baddock, Matthew C.; Bullard, Joanna E.] Univ Loughborough, Dept Geog, Loughborough, Leics, England.
[Ginoux, Paul] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA.
[Gill, Thomas E.] Univ Texas El Paso, Environm Sci & Engn Program, El Paso, TX 79968 USA.
[Gill, Thomas E.] Univ Texas El Paso, Dept Geol Sci, El Paso, TX 79968 USA.
RP Baddock, MC (reprint author), Univ Loughborough, Dept Geog, Loughborough, Leics, England.
EM m.c.baddock@lboro.ac.uk
RI Baddock, Matthew/A-5739-2012; Ginoux, Paul/C-2326-2008;
OI Baddock, Matthew/0000-0003-1490-7511; Ginoux, Paul/0000-0003-3642-2988;
Gill, Thomas E/0000-0001-9011-4105
FU NOAA R2O NGGPS grant; NOAA [NA17AE1623, NA17AE1625]
FX Partially supported by a NOAA R2O NGGPS grant (P.G.) and NOAA
cooperative agreements NA17AE1623 and NA17AE1625 (T.G.). The authors are
grateful to Miguel Dominguez Acosta for discussions. MODIS C6 Deep Blue
is available at the Level-1 and Atmosphere Archive and Distribution
System (LAADS) Distributed Active Archive Center
(https://ladsweb.nascom.nasa.gov). We thank Carlos Perez Garcia-Pando
and an anonymous reviewer for comments.
NR 40
TC 4
Z9 4
U1 6
U2 10
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 MAR 28
PY 2016
VL 43
IS 6
BP 2606
EP 2613
DI 10.1002/2015GL067327
PG 8
WC Geosciences, Multidisciplinary
SC Geology
GA DK1TM
UT WOS:000374697200034
ER
PT J
AU Kieber, DJ
Keene, WC
Frossard, AA
Long, MS
Maben, JR
Russell, LM
Kinsey, JD
Tyssebotn, IMB
Quinn, PK
Bates, TS
AF Kieber, David J.
Keene, William C.
Frossard, Amanda A.
Long, Michael S.
Maben, John R.
Russell, Lynn M.
Kinsey, Joanna D.
Tyssebotn, Inger Marie B.
Quinn, Patricia K.
Bates, Timothy S.
TI Coupled ocean-atmosphere loss of marine refractory dissolved organic
carbon
SO GEOPHYSICAL RESEARCH LETTERS
LA English
DT Article
DE photochemistry; Sargasso; marine aerosol; marine carbon cycle; marine
surfactant; DOC
ID SEA-SPRAY AEROSOL; SIDE-SCAN SONAR; PACIFIC-OCEAN; MATTER ENRICHMENT;
BOUNDARY-LAYER; BREAKING WAVES; SIZE; SALT; EMISSIONS; SEAWATER
AB The oceans hold a massive quantity of organic carbon, nearly all of which is dissolved and more than 95% is refractory, cycling through the oceans several times before complete removal. The vast reservoir of refractory dissolved organic carbon (RDOC) is a critical component of the global carbon cycle that is relevant to our understanding of fundamental marine biogeochemical processes and the role of the oceans in climate change with respect to long-term storage and sequestration of atmospheric carbon dioxide. Here we show that RDOC includes surface-active organic matter that can be incorporated into primary marine aerosol produced by bursting bubbles at the sea surface. We propose that this process will deliver RDOC from the sea surface to the atmosphere wherein its photochemical oxidation corresponds to a potentially important and hitherto unknown removal mechanism for marine RDOC.
C1 [Kieber, David J.; Kinsey, Joanna D.; Tyssebotn, Inger Marie B.] SUNY Syracuse, Coll Environm Sci & Forestry, Dept Chem, Syracuse, NY USA.
[Keene, William C.; Maben, John R.] Univ Virginia, Dept Environm Sci, Clark Hall, Charlottesville, VA 22903 USA.
[Frossard, Amanda A.; Russell, Lynn M.] Univ Calif San Diego, Scripps Inst Oceanog, San Diego, CA 92103 USA.
[Frossard, Amanda A.] Univ Calif Berkeley, Dept Chem, Berkeley, CA 94720 USA.
[Long, Michael S.] Harvard Univ, John A Paulson Sch Engn & Appl Sci, Cambridge, MA 02138 USA.
[Kinsey, Joanna D.] N Carolina State Univ, Dept Marine Earth & Atmospher Sci, Raleigh, NC USA.
[Quinn, Patricia K.; Bates, Timothy S.] NOAA, Pacific Marine Environm Lab, 7600 Sand Point Way Ne, Seattle, WA 98115 USA.
[Bates, Timothy S.] Univ Washington, Joint Inst Study Atmosphere & Ocean, Seattle, WA 98195 USA.
RP Kieber, DJ (reprint author), SUNY Syracuse, Coll Environm Sci & Forestry, Dept Chem, Syracuse, NY USA.
EM djkieber@esf.edu
RI Bates, Timothy/L-6080-2016; Quinn, Patricia/R-1493-2016
OI Quinn, Patricia/0000-0003-0337-4895
FU National Science Foundation [OCE-0948216, OCE-1129896]; University of
Virginia [OCE-0948420, OCE-1129836]; Scripps Institution of Oceanography
[OCE-1129580]; Harvard University [AGS-1252755]; NOAA Atmospheric
Composition and Climate Program
FX Data and analyses reported in this study are available upon request from
the authors. We thank G. Henderson, D. Coffman, K. Schulz, D. Hamilton,
J. Johnson, and M. Haserodt for their assistance in sample collection
and analysis; V. Trainer for the loan and calibration of the
fluorometer; X. Lopez-Yglesias and F. Brechtel of Brechtel Manufacturing
for their timely assistance