Observations of supercooling and frazil ice formation in the Laptev Sea coastal polynya
Identifieur interne : 001375 ( Istex/Corpus ); précédent : 001374; suivant : 001376Observations of supercooling and frazil ice formation in the Laptev Sea coastal polynya
Auteurs : Igor A. Dmitrenko ; Carolyn Wegner ; Heidemarie Kassens ; Sergey A. Kirillov ; Thomas Krumpen ; Günther Heinemann ; Alfred Helbig ; David Schröder ; Jens A. Hölemann ; Torben Klagge ; Konstantin P. Tyshko ; Thomas BuscheSource :
- Journal of Geophysical Research: Oceans [ 0148-0227 ] ; 2010-05.
Abstract
This paper examines a hydrographic response to the wind‐driven coastal polynya activity over the southeastern Laptev Sea shelf for April–May 2008, using a combination of Environmental Satellite (Envisat) advanced synthetic aperture radar (ASAR) and TerraSAR‐X satellite imagery, aerial photography, meteorological data, and SBE‐37 salinity‐temperature‐depth and acoustic Doppler current profiler land‐fast ice edge‐moored instruments. When ASAR observed the strongest end‐of‐April polynya event with frazil ice formation, the moored instruments showed maximal acoustical scattering within the surface mixed layer, and the seawater temperatures were either at or 0.02°C below freezing. We also find evidence of the persistent horizontal temperature and salinity gradients across the fast ice edge to have the signature of geostrophic flow adjustment as predicted by polynya models.
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DOI: 10.1029/2009JC005798
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Hölemann</name><affiliation><mods:affiliation>Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany</mods:affiliation></affiliation></author><author><name sortKey="Klagge, Torben" sort="Klagge, Torben" uniqKey="Klagge T" first="Torben" last="Klagge">Torben Klagge</name><affiliation><mods:affiliation>Leibniz Institute of Marine Sciences at, University of Kiel (IFM‐GEOMAR), Kiel, Germany</mods:affiliation></affiliation></author><author><name sortKey="Tyshko, Konstantin P" sort="Tyshko, Konstantin P" uniqKey="Tyshko K" first="Konstantin P." last="Tyshko">Konstantin P. Tyshko</name><affiliation><mods:affiliation>Arctic and Antarctic Research Institute, St. Petersburg, Russia</mods:affiliation></affiliation></author><author><name sortKey="Busche, Thomas" sort="Busche, Thomas" uniqKey="Busche T" first="Thomas" last="Busche">Thomas Busche</name><affiliation><mods:affiliation>German Aerospace Center, Microwaves and Radar Institute, Oberpfaffenhofen‐Wessling, Germany</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Journal of Geophysical Research: Oceans</title><title level="j" type="abbrev">J. Geophys. Res.</title><idno type="ISSN">0148-0227</idno><idno type="eISSN">2156-2202</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2010-05">2010-05</date><biblScope unit="volume">115</biblScope><biblScope unit="issue">C5</biblScope><biblScope unit="page" from="/">n/a</biblScope><biblScope unit="page" to="/">n/a</biblScope></imprint><idno type="ISSN">0148-0227</idno></series><idno type="istex">0FECA3C16BDFC799B30436D0ADF9DD11B4C7B5EC</idno><idno type="DOI">10.1029/2009JC005798</idno><idno type="ArticleID">2009JC005798</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0148-0227</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract">This paper examines a hydrographic response to the wind‐driven coastal polynya activity over the southeastern Laptev Sea shelf for April–May 2008, using a combination of Environmental Satellite (Envisat) advanced synthetic aperture radar (ASAR) and TerraSAR‐X satellite imagery, aerial photography, meteorological data, and SBE‐37 salinity‐temperature‐depth and acoustic Doppler current profiler land‐fast ice edge‐moored instruments. When ASAR observed the strongest end‐of‐April polynya event with frazil ice formation, the moored instruments showed maximal acoustical scattering within the surface mixed layer, and the seawater temperatures were either at or 0.02°C below freezing. We also find evidence of the persistent horizontal temperature and salinity gradients across the fast ice edge to have the signature of geostrophic flow adjustment as predicted by polynya models.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>Igor A. Dmitrenko</name><affiliations><json:string>Leibniz Institute of Marine Sciences at, University of Kiel (IFM‐GEOMAR), Kiel, Germany</json:string><json:string>E-mail: idmitrenko@ifm-geomar.de</json:string></affiliations></json:item><json:item><name>Carolyn Wegner</name><affiliations><json:string>Leibniz Institute of Marine Sciences at, University of Kiel (IFM‐GEOMAR), Kiel, Germany</json:string></affiliations></json:item><json:item><name>Heidemarie Kassens</name><affiliations><json:string>Leibniz Institute of Marine Sciences at, University of Kiel (IFM‐GEOMAR), Kiel, Germany</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>Thomas Krumpen</name><affiliations><json:string>Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany</json:string></affiliations></json:item><json:item><name>Günther Heinemann</name><affiliations><json:string>Department of Environmental Meteorology, University of Trier, Trier, Germany</json:string></affiliations></json:item><json:item><name>Alfred Helbig</name><affiliations><json:string>Department of Environmental Meteorology, University of Trier, Trier, Germany</json:string></affiliations></json:item><json:item><name>David Schröder</name><affiliations><json:string>Department of Environmental Meteorology, University of Trier, Trier, Germany</json:string></affiliations></json:item><json:item><name>Jens A. Hölemann</name><affiliations><json:string>Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany</json:string></affiliations></json:item><json:item><name>Torben Klagge</name><affiliations><json:string>Leibniz Institute of Marine Sciences at, University of Kiel (IFM‐GEOMAR), Kiel, Germany</json:string></affiliations></json:item><json:item><name>Konstantin P. Tyshko</name><affiliations><json:string>Arctic and Antarctic Research Institute, St. Petersburg, Russia</json:string></affiliations></json:item><json:item><name>Thomas Busche</name><affiliations><json:string>German Aerospace Center, Microwaves and Radar Institute, Oberpfaffenhofen‐Wessling, Germany</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>coastal polynya</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>supercooling</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>frazil ice</value></json:item></subject><articleId><json:string>2009JC005798</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>This paper examines a hydrographic response to the wind‐driven coastal polynya activity over the southeastern Laptev Sea shelf for April–May 2008, using a combination of Environmental Satellite (Envisat) advanced synthetic aperture radar (ASAR) and TerraSAR‐X satellite imagery, aerial photography, meteorological data, and SBE‐37 salinity‐temperature‐depth and acoustic Doppler current profiler land‐fast ice edge‐moored instruments. When ASAR observed the strongest end‐of‐April polynya event with frazil ice formation, the moored instruments showed maximal acoustical scattering within the surface mixed layer, and the seawater temperatures were either at or 0.02°C below freezing. We also find evidence of the persistent horizontal temperature and salinity gradients across the fast ice edge to have the signature of geostrophic flow adjustment as predicted by polynya models.</abstract><qualityIndicators><score>6.538</score><pdfVersion>1.4</pdfVersion><pdfPageSize>612 x 792 pts (letter)</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>880</abstractCharCount><pdfWordCount>4622</pdfWordCount><pdfCharCount>27785</pdfCharCount><pdfPageCount>9</pdfPageCount><abstractWordCount>118</abstractWordCount></qualityIndicators><title>Observations of supercooling and frazil ice formation in the Laptev Sea coastal polynya</title><refBibs><json:item><author><json:item><name>J. 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Res.</title><idno type="pISSN">0148-0227</idno><idno type="eISSN">2156-2202</idno><idno type="DOI">10.1002/(ISSN)2156-2202c</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2010-05"></date><biblScope unit="volume">115</biblScope><biblScope unit="issue">C5</biblScope><biblScope unit="page" from="/">n/a</biblScope><biblScope unit="page" to="/">n/a</biblScope></imprint></monogr><idno type="istex">0FECA3C16BDFC799B30436D0ADF9DD11B4C7B5EC</idno><idno type="DOI">10.1029/2009JC005798</idno><idno type="ArticleID">2009JC005798</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>2010</date></creation><langUsage><language ident="en">en</language></langUsage><abstract><p>This paper examines a hydrographic response to the wind‐driven coastal polynya activity over the southeastern Laptev Sea shelf for April–May 2008, using a combination of Environmental Satellite (Envisat) advanced synthetic aperture radar (ASAR) and TerraSAR‐X satellite imagery, aerial photography, meteorological data, and SBE‐37 salinity‐temperature‐depth and acoustic Doppler current profiler land‐fast ice edge‐moored instruments. When ASAR observed the strongest end‐of‐April polynya event with frazil ice formation, the moored instruments showed maximal acoustical scattering within the surface mixed layer, and the seawater temperatures were either at or 0.02°C below freezing. We also find evidence of the persistent horizontal temperature and salinity gradients across the fast ice edge to have the signature of geostrophic flow adjustment as predicted by polynya models.</p></abstract><textClass><keywords scheme="keyword"><list><head>keywords</head><item><term>coastal polynya</term></item><item><term>supercooling</term></item><item><term>frazil ice</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>index-terms</head><item><term>ATMOSPHERIC COMPOSITION AND STRUCTURE</term></item><item><term>Air/sea constituent fluxes</term></item><item><term>CRYOSPHERE</term></item><item><term>Polynas</term></item><item><term>Remote sensing</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>Ocean/atmosphere interactions</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>NATURAL HAZARDS</term></item><item><term>Atmospheric</term></item><item><term>OCEANOGRAPHY: PHYSICAL</term></item><item><term>Ice mechanics and air/sea/ice exchange processes</term></item><item><term>Air/sea interactions</term></item><item><term>GEOGRAPHIC LOCATION</term></item><item><term>Antarctica</term></item><item><term>Arctic region</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2009-09-10">Received</change><change when="2009-12-28">Registration</change><change when="2010-05">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/0FECA3C16BDFC799B30436D0ADF9DD11B4C7B5EC/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="jgrc11552"><header><publicationMeta level="product"><doi>10.1002/(ISSN)2156-2202c</doi><issn type="print">0148-0227</issn><issn type="electronic">2156-2202</issn><idGroup><id type="product" value="JGRC"></id><id type="coden" value="JGREA2"></id></idGroup><titleGroup><title type="main" xml:lang="en" sort="JOURNAL OF GEOPHYSICAL RESEARCH: OCEANS">Journal of Geophysical Research: Oceans</title><title type="short">J. 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A.</givenNames></author>, et al. (<pubYear year="2010">2010</pubYear>), <articleTitle>Observations of supercooling and frazil ice formation in the Laptev Sea coastal polynya</articleTitle>, <journalTitle>J. Geophys. 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affiliationRef="#jgrc11552-aff-0001"><personName><givenNames>Carolyn</givenNames> <familyName>Wegner</familyName></personName></creator><creator creatorRole="author" xml:id="jgrc11552-cr-0003" affiliationRef="#jgrc11552-aff-0001"><personName><givenNames>Heidemarie</givenNames> <familyName>Kassens</familyName></personName></creator><creator creatorRole="author" xml:id="jgrc11552-cr-0004" affiliationRef="#jgrc11552-aff-0002"><personName><givenNames>Sergey A.</givenNames> <familyName>Kirillov</familyName></personName></creator><creator creatorRole="author" xml:id="jgrc11552-cr-0005" affiliationRef="#jgrc11552-aff-0003"><personName><givenNames>Thomas</givenNames> <familyName>Krumpen</familyName></personName></creator><creator creatorRole="author" xml:id="jgrc11552-cr-0006" affiliationRef="#jgrc11552-aff-0004"><personName><givenNames>Günther</givenNames> <familyName>Heinemann</familyName></personName></creator><creator creatorRole="author" xml:id="jgrc11552-cr-0007" 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affiliationRef="#jgrc11552-aff-0005"><personName><givenNames>Thomas</givenNames> <familyName>Busche</familyName></personName></creator></creators><affiliationGroup><affiliation countryCode="DE" type="organization" xml:id="jgrc11552-aff-0001"><orgDiv>Leibniz Institute of Marine Sciences at</orgDiv><orgName>University of Kiel (IFM‐GEOMAR)</orgName><address><city>Kiel</city><country>Germany</country></address></affiliation><affiliation type="organization" xml:id="jgrc11552-aff-0002"><orgName>Arctic and Antarctic Research Institute</orgName><address><city>St. Petersburg</city><country>Russia</country></address></affiliation><affiliation countryCode="DE" type="organization" xml:id="jgrc11552-aff-0003"><orgName>Alfred Wegener Institute for Polar and Marine Research</orgName><address><city>Bremerhaven</city><country>Germany</country></address></affiliation><affiliation countryCode="DE" type="organization" xml:id="jgrc11552-aff-0004"><orgDiv>Department of Environmental Meteorology</orgDiv><orgName>University of Trier</orgName><address><city>Trier</city><country>Germany</country></address></affiliation><affiliation countryCode="DE" type="organization" xml:id="jgrc11552-aff-0005"><orgDiv>German Aerospace Center</orgDiv><orgName>Microwaves and Radar Institute</orgName><address><city>Oberpfaffenhofen‐Wessling</city><country>Germany</country></address></affiliation></affiliationGroup><keywordGroup type="author"><keyword xml:id="jgrc11552-kwd-0001">coastal polynya</keyword><keyword xml:id="jgrc11552-kwd-0002">supercooling</keyword><keyword xml:id="jgrc11552-kwd-0003">frazil ice</keyword></keywordGroup><abstractGroup><abstract type="main"><p xml:id="jgrc11552-para-0001" label="1">This paper examines a hydrographic response to the wind‐driven coastal polynya activity over the southeastern Laptev Sea shelf for April–May 2008, using a combination of Environmental Satellite (Envisat) advanced synthetic aperture radar (ASAR) and TerraSAR‐X satellite imagery, aerial photography, meteorological data, and SBE‐37 salinity‐temperature‐depth and acoustic Doppler current profiler land‐fast ice edge‐moored instruments. When ASAR observed the strongest end‐of‐April polynya event with frazil ice formation, the moored instruments showed maximal acoustical scattering within the surface mixed layer, and the seawater temperatures were either at or 0.02°C below freezing. We also find evidence of the persistent horizontal temperature and salinity gradients across the fast ice edge to have the signature of geostrophic flow adjustment as predicted by polynya models.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Observations of supercooling and frazil ice formation in the Laptev Sea coastal polynya</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>SUPERCOOLING AND FRAZIL ICE FORMATION</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Observations of supercooling and frazil ice formation in the Laptev Sea coastal polynya</title></titleInfo><name type="personal"><namePart type="given">Igor A.</namePart><namePart type="family">Dmitrenko</namePart><affiliation>Leibniz Institute of Marine Sciences at, University of Kiel (IFM‐GEOMAR), 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">Carolyn</namePart><namePart type="family">Wegner</namePart><affiliation>Leibniz Institute of Marine Sciences at, University of Kiel (IFM‐GEOMAR), Kiel, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Heidemarie</namePart><namePart type="family">Kassens</namePart><affiliation>Leibniz Institute of Marine Sciences at, University of Kiel (IFM‐GEOMAR), Kiel, Germany</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">Thomas</namePart><namePart type="family">Krumpen</namePart><affiliation>Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Günther</namePart><namePart type="family">Heinemann</namePart><affiliation>Department of Environmental Meteorology, University of Trier, Trier, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Alfred</namePart><namePart type="family">Helbig</namePart><affiliation>Department of Environmental Meteorology, University of Trier, Trier, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">David</namePart><namePart type="family">Schröder</namePart><affiliation>Department of Environmental Meteorology, University of Trier, Trier, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Jens A.</namePart><namePart type="family">Hölemann</namePart><affiliation>Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Torben</namePart><namePart type="family">Klagge</namePart><affiliation>Leibniz Institute of Marine Sciences at, University of Kiel (IFM‐GEOMAR), Kiel, Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Konstantin P.</namePart><namePart type="family">Tyshko</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">Thomas</namePart><namePart type="family">Busche</namePart><affiliation>German Aerospace Center, Microwaves and Radar Institute, Oberpfaffenhofen‐Wessling, 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">2010-05</dateIssued><dateCaptured encoding="w3cdtf">2009-09-10</dateCaptured><dateValid encoding="w3cdtf">2009-12-28</dateValid><edition>Dmitrenko, I. A., et al. (2010), Observations of supercooling and frazil ice formation in the Laptev Sea coastal polynya, J. Geophys. Res., 115, C05015, doi:10.1029/2009JC005798.</edition><copyrightDate encoding="w3cdtf">2010</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">7</extent></physicalDescription><abstract>This paper examines a hydrographic response to the wind‐driven coastal polynya activity over the southeastern Laptev Sea shelf for April–May 2008, using a combination of Environmental Satellite (Envisat) advanced synthetic aperture radar (ASAR) and TerraSAR‐X satellite imagery, aerial photography, meteorological data, and SBE‐37 salinity‐temperature‐depth and acoustic Doppler current profiler land‐fast ice edge‐moored instruments. When ASAR observed the strongest end‐of‐April polynya event with frazil ice formation, the moored instruments showed maximal acoustical scattering within the surface mixed layer, and the seawater temperatures were either at or 0.02°C below freezing. We also find evidence of the persistent horizontal temperature and salinity gradients across the fast ice edge to have the signature of geostrophic flow adjustment as predicted by polynya models.</abstract><subject><genre>keywords</genre><topic>coastal polynya</topic><topic>supercooling</topic><topic>frazil ice</topic></subject><relatedItem type="host"><titleInfo><title>Journal of Geophysical Research: Oceans</title></titleInfo><titleInfo type="abbreviated"><title>J. Geophys. Res.</title></titleInfo><genre type="journal">journal</genre><subject><genre>index-terms</genre><topic authorityURI="http://psi.agu.org/taxonomy5/0300">ATMOSPHERIC COMPOSITION AND STRUCTURE</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0312">Air/sea constituent fluxes</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0700">CRYOSPHERE</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0752">Polynas</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0758">Remote sensing</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/taxonomy5/3339">Ocean/atmosphere interactions</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/taxonomy5/4300">NATURAL HAZARDS</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4301">Atmospheric</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4500">OCEANOGRAPHY: PHYSICAL</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4540">Ice mechanics and air/sea/ice exchange processes</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4504">Air/sea interactions</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><identifier type="ISSN">0148-0227</identifier><identifier type="eISSN">2156-2202</identifier><identifier type="DOI">10.1002/(ISSN)2156-2202c</identifier><identifier type="CODEN">JGREA2</identifier><identifier type="PublisherID">JGRC</identifier><part><date>2010</date><detail type="volume"><caption>vol.</caption><number>115</number></detail><detail type="issue"><caption>no.</caption><number>C5</number></detail><extent unit="pages"><start>n/a</start><end>n/a</end><total>9</total></extent></part></relatedItem><identifier type="istex">0FECA3C16BDFC799B30436D0ADF9DD11B4C7B5EC</identifier><identifier type="DOI">10.1029/2009JC005798</identifier><identifier type="ArticleID">2009JC005798</identifier><accessCondition type="use and reproduction" contentType="copyright">Copyright 2010 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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|texte= Observations of supercooling and frazil ice formation in the Laptev Sea coastal polynya
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