Sea‐ice production over the Laptev Sea shelf inferred from historical summer‐to‐winter hydrographic observations of 1960s–1990s
Identifieur interne : 000C47 ( Istex/Corpus ); précédent : 000C46; suivant : 000C48Sea‐ice production over the Laptev Sea shelf inferred from historical summer‐to‐winter hydrographic observations of 1960s–1990s
Auteurs : Igor A. Dmitrenko ; Sergey A. Kirillov ; L. Bruno Tremblay ; Dorothea Bauch ; Sascha WillmesSource :
- Geophysical Research Letters [ 0094-8276 ] ; 2009-07.
Abstract
The winter net sea‐ice production (NSIP) over the Laptev Sea shelf is inferred from continuous summer‐to‐winter historical salinity records of 1960s–1990s. While the NSIP strongly depends on the assumed salinity of newly formed ice, the NSIP quasi‐decadal variability can be linked to the wind‐driven circulation anomalies in the Laptev Sea region. The increased wind‐driven advection of ice away from the Laptev Sea coast when the Arctic Oscillation (AO) is positive implies enhanced coastal polynya sea‐ice production and brine release in the shelf water. When the AO is negative, the NSIP and seasonal salinity amplitude tends to weaken. These results are in reasonable agreement with sea‐ice observations and modeling.
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DOI: 10.1029/2009GL038775
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Dmitrenko</name><affiliation><mods:affiliation>Leibniz Institute of Marine Sciences, University of Kiel, Kiel, Germany</mods:affiliation></affiliation><affiliation><mods:affiliation>E-mail: idmitrenko@ifm-geomar.de</mods:affiliation></affiliation></author><author><name sortKey="Kirillov, Sergey A" sort="Kirillov, Sergey A" uniqKey="Kirillov S" first="Sergey A." last="Kirillov">Sergey A. Kirillov</name><affiliation><mods:affiliation>Arctic and Antarctic Research Institute, St. Petersburg, Russia</mods:affiliation></affiliation></author><author><name sortKey="Tremblay, L Bruno" sort="Tremblay, L Bruno" uniqKey="Tremblay L" first="L. Bruno" last="Tremblay">L. Bruno Tremblay</name><affiliation><mods:affiliation>Department of Atmospheric and Oceanic Sciences, McGill University, Montreal, Quebec, Canada</mods:affiliation></affiliation></author><author><name sortKey="Bauch, Dorothea" sort="Bauch, Dorothea" uniqKey="Bauch D" first="Dorothea" last="Bauch">Dorothea Bauch</name><affiliation><mods:affiliation>Leibniz Institute of Marine Sciences, University of Kiel, Kiel, Germany</mods:affiliation></affiliation></author><author><name sortKey="Willmes, Sascha" sort="Willmes, Sascha" uniqKey="Willmes S" first="Sascha" last="Willmes">Sascha Willmes</name><affiliation><mods:affiliation>Environmental Meteorology, University of Trier, Trier, Germany</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Geophysical Research Letters</title><title level="j" type="abbrev">Geophys. Res. Lett.</title><idno type="ISSN">0094-8276</idno><idno type="eISSN">1944-8007</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2009-07">2009-07</date><biblScope unit="volume">36</biblScope><biblScope unit="issue">13</biblScope><biblScope unit="page" from="/">n/a</biblScope><biblScope unit="page" to="/">n/a</biblScope></imprint><idno type="ISSN">0094-8276</idno></series><idno type="istex">D02CEA70C65C4BD5F59761522AA3E203336EDDCB</idno><idno type="DOI">10.1029/2009GL038775</idno><idno type="ArticleID">2009GL038775</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0094-8276</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract">The winter net sea‐ice production (NSIP) over the Laptev Sea shelf is inferred from continuous summer‐to‐winter historical salinity records of 1960s–1990s. While the NSIP strongly depends on the assumed salinity of newly formed ice, the NSIP quasi‐decadal variability can be linked to the wind‐driven circulation anomalies in the Laptev Sea region. The increased wind‐driven advection of ice away from the Laptev Sea coast when the Arctic Oscillation (AO) is positive implies enhanced coastal polynya sea‐ice production and brine release in the shelf water. When the AO is negative, the NSIP and seasonal salinity amplitude tends to weaken. These results are in reasonable agreement with sea‐ice observations and modeling.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>Igor A. Dmitrenko</name><affiliations><json:string>Leibniz Institute of Marine Sciences, University of Kiel, Kiel, Germany</json:string><json:string>E-mail: idmitrenko@ifm-geomar.de</json:string></affiliations></json:item><json:item><name>Sergey A. Kirillov</name><affiliations><json:string>Arctic and Antarctic Research Institute, St. Petersburg, Russia</json:string></affiliations></json:item><json:item><name>L. Bruno Tremblay</name><affiliations><json:string>Department of Atmospheric and Oceanic Sciences, McGill University, Montreal, Quebec, Canada</json:string></affiliations></json:item><json:item><name>Dorothea Bauch</name><affiliations><json:string>Leibniz Institute of Marine Sciences, University of Kiel, Kiel, Germany</json:string></affiliations></json:item><json:item><name>Sascha Willmes</name><affiliations><json:string>Environmental Meteorology, University of Trier, Trier, Germany</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>seasonal salinity difference</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>sea‐ice formation</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>coastal polynya</value></json:item></subject><articleId><json:string>2009GL038775</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>The winter net sea‐ice production (NSIP) over the Laptev Sea shelf is inferred from continuous summer‐to‐winter historical salinity records of 1960s–1990s. While the NSIP strongly depends on the assumed salinity of newly formed ice, the NSIP quasi‐decadal variability can be linked to the wind‐driven circulation anomalies in the Laptev Sea region. The increased wind‐driven advection of ice away from the Laptev Sea coast when the Arctic Oscillation (AO) is positive implies enhanced coastal polynya sea‐ice production and brine release in the shelf water. When the AO is negative, the NSIP and seasonal salinity amplitude tends to weaken. 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Bruno</forename><surname>Tremblay</surname></persName><affiliation>Department of Atmospheric and Oceanic Sciences, McGill University, Montreal, Quebec, Canada</affiliation></author><author xml:id="author-4"><persName><forename type="first">Dorothea</forename><surname>Bauch</surname></persName><affiliation>Leibniz Institute of Marine Sciences, University of Kiel, Kiel, Germany</affiliation></author><author xml:id="author-5"><persName><forename type="first">Sascha</forename><surname>Willmes</surname></persName><affiliation>Environmental Meteorology, University of Trier, Trier, Germany</affiliation></author></analytic><monogr><title level="j">Geophysical Research Letters</title><title level="j" type="abbrev">Geophys. Res. Lett.</title><idno type="pISSN">0094-8276</idno><idno type="eISSN">1944-8007</idno><idno type="DOI">10.1002/(ISSN)1944-8007</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2009-07"></date><biblScope unit="volume">36</biblScope><biblScope unit="issue">13</biblScope><biblScope unit="page" from="/">n/a</biblScope><biblScope unit="page" to="/">n/a</biblScope></imprint></monogr><idno type="istex">D02CEA70C65C4BD5F59761522AA3E203336EDDCB</idno><idno type="DOI">10.1029/2009GL038775</idno><idno type="ArticleID">2009GL038775</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>2009</date></creation><langUsage><language ident="en">en</language></langUsage><abstract><p>The winter net sea‐ice production (NSIP) over the Laptev Sea shelf is inferred from continuous summer‐to‐winter historical salinity records of 1960s–1990s. While the NSIP strongly depends on the assumed salinity of newly formed ice, the NSIP quasi‐decadal variability can be linked to the wind‐driven circulation anomalies in the Laptev Sea region. The increased wind‐driven advection of ice away from the Laptev Sea coast when the Arctic Oscillation (AO) is positive implies enhanced coastal polynya sea‐ice production and brine release in the shelf water. When the AO is negative, the NSIP and seasonal salinity amplitude tends to weaken. These results are in reasonable agreement with sea‐ice observations and modeling.</p></abstract><textClass><keywords scheme="keyword"><list><head>keywords</head><item><term>seasonal salinity difference</term></item><item><term>sea‐ice formation</term></item><item><term>coastal polynya</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>index-terms</head><item><term>CRYOSPHERE</term></item><item><term>Sea ice</term></item><item><term>Cryosphere</term></item><item><term>Sea ice</term></item><item><term>Polynas</term></item><item><term>Leads</term></item><item><term>GLOBAL CHANGE</term></item><item><term>Climate variability</term></item><item><term>Oceans</term></item><item><term>MARINE GEOLOGY AND GEOPHYSICS</term></item><item><term>Continental shelf and slope processes</term></item><item><term>ATMOSPHERIC PROCESSES</term></item><item><term>Climate change and variability</term></item><item><term>OCEANOGRAPHY: GENERAL</term></item><item><term>Arctic and Antarctic oceanography</term></item><item><term>Continental shelf and slope processes</term></item><item><term>Climate and interannual variability</term></item><item><term>OCEANOGRAPHY: PHYSICAL</term></item><item><term>Decadal ocean variability</term></item><item><term>Ice mechanics and air/sea/ice exchange processes</term></item><item><term>Ice mechanics and air/sea/ice exchange processes</term></item><item><term>GEOGRAPHIC LOCATION</term></item><item><term>Antarctica</term></item><item><term>Arctic region</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>article-category</head><item><term>Oceans</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2009-04-19">Received</change><change when="2009-06-10">Registration</change><change when="2009-07">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/D02CEA70C65C4BD5F59761522AA3E203336EDDCB/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley, elements deleted: body"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration><istex:document><component type="serialArticle" version="2.0" xml:lang="en" xml:id="grl26065"><header><publicationMeta level="product"><doi>10.1002/(ISSN)1944-8007</doi><issn type="print">0094-8276</issn><issn type="electronic">1944-8007</issn><idGroup><id type="product" value="GRL"></id><id type="coden" value="GPRLAJ"></id></idGroup><titleGroup><title type="main" xml:lang="en" sort="GEOPHYSICAL RESEARCH LETTERS">Geophysical Research Letters</title><title type="short">Geophys. Res. Lett.</title></titleGroup></publicationMeta><publicationMeta level="part" position="130"><doi>10.1002/grl.v36.13</doi><numberingGroup><numbering type="journalVolume" number="36">36</numbering><numbering type="journalIssue">13</numbering></numberingGroup><coverDate startDate="2009-07">July 2009</coverDate></publicationMeta><publicationMeta level="unit" position="300" type="article" status="forIssue"><doi>10.1029/2009GL038775</doi><idGroup><id type="editorialOffice" value="2009GL038775"></id><id type="society" value="L13605"></id><id type="unit" value="GRL26065"></id></idGroup><countGroup><count type="pageTotal" number="4"></count></countGroup><titleGroup><title type="articleCategory">Oceans</title><title type="tocHeading1">Oceans</title></titleGroup><copyright ownership="thirdParty">Copyright 2009 by the American Geophysical Union.</copyright><eventGroup><event type="manuscriptReceived" date="2009-04-19"></event><event type="manuscriptRevised" date="2009-05-27"></event><event type="manuscriptAccepted" date="2009-06-10"></event><event type="firstOnline" date="2009-07-07"></event><event type="publishedOnlineFinalForm" date="2009-07-07"></event><event type="xmlConverted" agent="SPi Global Converter:AGUv3.44_TO_WileyML3Gv1.0.3 version:1.3; WileyML 3G Packaging Tool v1.0; AGU2WileyML3G Final Clean Up v1.0" date="2012-12-17"></event><event type="xmlConverted" agent="Converter:WILEY_ML3G_TO_WILEY_ML3GV2 version:3.8.8" date="2014-01-26"></event><event type="xmlConverted" agent="Converter:WML3G_To_WML3G version:4.1.7 mode:FullText,remove_FC" date="2014-10-23"></event></eventGroup><numberingGroup><numbering type="pageFirst">n/a</numbering><numbering type="pageLast">n/a</numbering></numberingGroup><subjectInfo><subject href="http://psi.agu.org/taxonomy5/0700">CRYOSPHERE</subject><subjectInfo><subject href="http://psi.agu.org/taxonomy5/0750">Sea ice</subject><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/0700">Cryosphere</subject><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/0750">Sea ice</subject><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/0752">Polynas</subject><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/0754">Leads</subject></subjectInfo><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/1600">GLOBAL CHANGE</subject><subjectInfo><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/1616">Climate variability</subject><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/1635">Oceans</subject></subjectInfo><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/3000">MARINE GEOLOGY AND GEOPHYSICS</subject><subjectInfo><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/3002">Continental shelf and slope processes</subject></subjectInfo><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/3300">ATMOSPHERIC PROCESSES</subject><subjectInfo><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/3305">Climate change and variability</subject></subjectInfo><subject href="http://psi.agu.org/taxonomy5/4200">OCEANOGRAPHY: GENERAL</subject><subjectInfo><subject href="http://psi.agu.org/taxonomy5/4207">Arctic and Antarctic oceanography</subject><subject href="http://psi.agu.org/taxonomy5/4219">Continental shelf and slope processes</subject><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/4215">Climate and interannual variability</subject></subjectInfo><subject href="http://psi.agu.org/taxonomy5/4500">OCEANOGRAPHY: PHYSICAL</subject><subjectInfo><subject href="http://psi.agu.org/taxonomy5/4513">Decadal ocean variability</subject><subject href="http://psi.agu.org/taxonomy5/4540">Ice mechanics and air/sea/ice exchange processes</subject><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/4540">Ice mechanics and air/sea/ice exchange processes</subject></subjectInfo><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/9300">GEOGRAPHIC LOCATION</subject><subjectInfo><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/9310">Antarctica</subject><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/9315">Arctic region</subject></subjectInfo></subjectInfo><selfCitationGroup><citation xml:id="grl26065-cit-0000" type="self"><author><familyName>Dmitrenko</familyName>, <givenNames>I. A.</givenNames></author>, <author><givenNames>S. A.</givenNames> <familyName>Kirillov</familyName></author>, <author><givenNames>L. B.</givenNames> <familyName>Tremblay</familyName></author>, <author><givenNames>D.</givenNames> <familyName>Bauch</familyName></author>, and <author><givenNames>S.</givenNames> <familyName>Willmes</familyName></author> (<pubYear year="2009">2009</pubYear>), <articleTitle>Sea‐ice production over the Laptev Sea shelf inferred from historical summer‐to‐winter hydrographic observations of 1960s–1990s</articleTitle>, <journalTitle>Geophys. Res. Lett.</journalTitle>, <vol>36</vol>, L13605, doi:<accessionId ref="info:doi/10.1029/2009GL038775">10.1029/2009GL038775</accessionId>.</citation></selfCitationGroup><linkGroup><link type="toTypesetVersion" href="file:GRL.GRL26065.pdf"></link></linkGroup></publicationMeta><contentMeta><countGroup><count type="figureTotal" number="4"></count></countGroup><titleGroup><title type="main">Sea‐ice production over the Laptev Sea shelf inferred from historical summer‐to‐winter hydrographic observations of 1960s–1990s</title><title type="short">LAPTEV SEA SHELF SEA‐ICE PRODUCTION</title><title type="shortAuthors">Dmitrenko <i>et al</i>.</title></titleGroup><creators><creator creatorRole="author" xml:id="grl26065-cr-0001" affiliationRef="#grl26065-aff-0001"><personName><givenNames>Igor A.</givenNames> <familyName>Dmitrenko</familyName></personName><contactDetails><email normalForm="idmitrenko@ifm-geomar.de">idmitrenko@ifm-geomar.de</email></contactDetails></creator><creator creatorRole="author" xml:id="grl26065-cr-0002" affiliationRef="#grl26065-aff-0002"><personName><givenNames>Sergey A.</givenNames> <familyName>Kirillov</familyName></personName></creator><creator creatorRole="author" xml:id="grl26065-cr-0003" affiliationRef="#grl26065-aff-0003"><personName><givenNames>L. Bruno</givenNames> <familyName>Tremblay</familyName></personName></creator><creator creatorRole="author" xml:id="grl26065-cr-0004" affiliationRef="#grl26065-aff-0001"><personName><givenNames>Dorothea</givenNames> <familyName>Bauch</familyName></personName></creator><creator creatorRole="author" xml:id="grl26065-cr-0005" affiliationRef="#grl26065-aff-0004"><personName><givenNames>Sascha</givenNames> <familyName>Willmes</familyName></personName></creator></creators><affiliationGroup><affiliation countryCode="DE" type="organization" xml:id="grl26065-aff-0001"><orgDiv>Leibniz Institute of Marine Sciences</orgDiv><orgName>University of Kiel</orgName><address><city>Kiel</city><country>Germany</country></address></affiliation><affiliation type="organization" xml:id="grl26065-aff-0002"><orgName>Arctic and Antarctic Research Institute</orgName><address><city>St. Petersburg</city><country>Russia</country></address></affiliation><affiliation countryCode="CA" type="organization" xml:id="grl26065-aff-0003"><orgDiv>Department of Atmospheric and Oceanic Sciences</orgDiv><orgName>McGill University</orgName><address><city>Montreal, Quebec</city><country>Canada</country></address></affiliation><affiliation countryCode="DE" type="organization" xml:id="grl26065-aff-0004"><orgDiv>Environmental Meteorology</orgDiv><orgName>University of Trier</orgName><address><city>Trier</city><country>Germany</country></address></affiliation></affiliationGroup><keywordGroup type="author"><keyword xml:id="grl26065-kwd-0001">seasonal salinity difference</keyword><keyword xml:id="grl26065-kwd-0002">sea‐ice formation</keyword><keyword xml:id="grl26065-kwd-0003">coastal polynya</keyword></keywordGroup><abstractGroup><abstract type="main"><p xml:id="grl26065-para-0001" label="1">The winter net sea‐ice production (NSIP) over the Laptev Sea shelf is inferred from continuous summer‐to‐winter historical salinity records of 1960s–1990s. While the NSIP strongly depends on the assumed salinity of newly formed ice, the NSIP quasi‐decadal variability can be linked to the wind‐driven circulation anomalies in the Laptev Sea region. The increased wind‐driven advection of ice away from the Laptev Sea coast when the Arctic Oscillation (AO) is positive implies enhanced coastal polynya sea‐ice production and brine release in the shelf water. When the AO is negative, the NSIP and seasonal salinity amplitude tends to weaken. These results are in reasonable agreement with sea‐ice observations and modeling.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Sea‐ice production over the Laptev Sea shelf inferred from historical summer‐to‐winter hydrographic observations of 1960s–1990s</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>LAPTEV SEA SHELF SEA‐ICE PRODUCTION</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Sea‐ice production over the Laptev Sea shelf inferred from historical summer‐to‐winter hydrographic observations of 1960s–1990s</title></titleInfo><name type="personal"><namePart type="given">Igor A.</namePart><namePart type="family">Dmitrenko</namePart><affiliation>Leibniz Institute of Marine Sciences, University of Kiel, Kiel, Germany</affiliation><affiliation>E-mail: idmitrenko@ifm-geomar.de</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Sergey A.</namePart><namePart type="family">Kirillov</namePart><affiliation>Arctic and Antarctic Research Institute, St. Petersburg, Russia</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">L. Bruno</namePart><namePart type="family">Tremblay</namePart><affiliation>Department of Atmospheric and Oceanic Sciences, McGill University, Montreal, Quebec, Canada</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Dorothea</namePart><namePart type="family">Bauch</namePart><affiliation>Leibniz Institute of Marine Sciences, University of Kiel, Kiel, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Sascha</namePart><namePart type="family">Willmes</namePart><affiliation>Environmental Meteorology, University of Trier, Trier, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><dateIssued encoding="w3cdtf">2009-07</dateIssued><dateCaptured encoding="w3cdtf">2009-04-19</dateCaptured><dateValid encoding="w3cdtf">2009-06-10</dateValid><edition>Dmitrenko, I. A., S. A. Kirillov, L. B. Tremblay, D. Bauch, and S. Willmes (2009), Sea‐ice production over the Laptev Sea shelf inferred from historical summer‐to‐winter hydrographic observations of 1960s–1990s, Geophys. Res. Lett., 36, L13605, doi:10.1029/2009GL038775.</edition><copyrightDate encoding="w3cdtf">2009</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="figures">4</extent></physicalDescription><abstract>The winter net sea‐ice production (NSIP) over the Laptev Sea shelf is inferred from continuous summer‐to‐winter historical salinity records of 1960s–1990s. While the NSIP strongly depends on the assumed salinity of newly formed ice, the NSIP quasi‐decadal variability can be linked to the wind‐driven circulation anomalies in the Laptev Sea region. The increased wind‐driven advection of ice away from the Laptev Sea coast when the Arctic Oscillation (AO) is positive implies enhanced coastal polynya sea‐ice production and brine release in the shelf water. When the AO is negative, the NSIP and seasonal salinity amplitude tends to weaken. These results are in reasonable agreement with sea‐ice observations and modeling.</abstract><subject><genre>keywords</genre><topic>seasonal salinity difference</topic><topic>sea‐ice formation</topic><topic>coastal polynya</topic></subject><relatedItem type="host"><titleInfo><title>Geophysical Research Letters</title></titleInfo><titleInfo type="abbreviated"><title>Geophys. Res. Lett.</title></titleInfo><genre type="journal">journal</genre><subject><genre>index-terms</genre><topic authorityURI="http://psi.agu.org/taxonomy5/0700">CRYOSPHERE</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0750">Sea ice</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0700">Cryosphere</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0750">Sea ice</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0752">Polynas</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0754">Leads</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1600">GLOBAL CHANGE</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1616">Climate variability</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1635">Oceans</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3000">MARINE GEOLOGY AND GEOPHYSICS</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3002">Continental shelf and slope processes</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3300">ATMOSPHERIC PROCESSES</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3305">Climate change and variability</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4200">OCEANOGRAPHY: GENERAL</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4207">Arctic and Antarctic oceanography</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4219">Continental shelf and slope processes</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4215">Climate and interannual variability</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4500">OCEANOGRAPHY: PHYSICAL</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4513">Decadal ocean variability</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4540">Ice mechanics and air/sea/ice exchange processes</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4540">Ice mechanics and air/sea/ice exchange processes</topic><topic authorityURI="http://psi.agu.org/taxonomy5/9300">GEOGRAPHIC LOCATION</topic><topic authorityURI="http://psi.agu.org/taxonomy5/9310">Antarctica</topic><topic authorityURI="http://psi.agu.org/taxonomy5/9315">Arctic region</topic></subject><subject><genre>article-category</genre><topic>Oceans</topic></subject><identifier type="ISSN">0094-8276</identifier><identifier type="eISSN">1944-8007</identifier><identifier type="DOI">10.1002/(ISSN)1944-8007</identifier><identifier type="CODEN">GPRLAJ</identifier><identifier type="PublisherID">GRL</identifier><part><date>2009</date><detail type="volume"><caption>vol.</caption><number>36</number></detail><detail type="issue"><caption>no.</caption><number>13</number></detail><extent unit="pages"><start>n/a</start><end>n/a</end><total>4</total></extent></part></relatedItem><identifier type="istex">D02CEA70C65C4BD5F59761522AA3E203336EDDCB</identifier><identifier type="DOI">10.1029/2009GL038775</identifier><identifier type="ArticleID">2009GL038775</identifier><accessCondition type="use and reproduction" contentType="copyright">Copyright 2009 by the American Geophysical Union.</accessCondition><recordInfo><recordContentSource>WILEY</recordContentSource></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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