Glaciologist studies Greenland snow conditions and helps calibrate CryoSat instrument
Identifieur interne : 000465 ( Istex/Corpus ); précédent : 000464; suivant : 000466Glaciologist studies Greenland snow conditions and helps calibrate CryoSat instrument
Auteurs : Randy ShowstackSource :
- Eos, Transactions American Geophysical Union [ 0096-3941 ] ; 2011-07-02.
Abstract
GREENLAND—On a typically frigid mid‐July day at Summit Station, almost smack in the middle of Greenland, with the temperature hovering around −10°C, Elizabeth Morris and John Sweeny were bundled up against the cold atop their black Ski‐Doo snowmobiles, which Morris described as being similar to motorcycles on ski tracks. They drove the vehicles—without yet attaching three wooden sleds that would be pulled during their summer scientific traverse across part of central Greenland—on a practice spin along the perimeter of Summit's groomed, approximately 4600‐meter × 60‐meter snow runway. One of the longest runways in the world, it lies atop 3.2 kilometers of ice, with the horizon stretching in every direction. Morris, a glaciologist who is a senior associate at the Scott Polar Research Institute at Cambridge University, United Kingdom, and Sweeny, her polar guide, were taking advantage of an unexpected extra day at Summit, a scientific research station sponsored by the U.S. National Science Foundation (NSF), before the traverse began. They hoped that the socked‐in visibility just a few hours earlier that morning, 16 July, would not be repeated the following day so that a U.S. Air National Guard 109th Airlift Wing C‐130 cargo plane would be cleared to fly to Summit from Kangerlussuaq on Greenland's west coast with needed supplies. Morris and Sweeny would load up each sled with about 270 kilograms of gear.
Url:
DOI: 10.1029/2011EO310002
Links to Exploration step
ISTEX:8154B757AA73960087AE6FA724AD5EFB5C6A89B4Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Glaciologist studies Greenland snow conditions and helps calibrate CryoSat instrument</title><author><name sortKey="Showstack, Randy" sort="Showstack, Randy" uniqKey="Showstack R" first="Randy" last="Showstack">Randy Showstack</name><affiliation><mods:affiliation>American Geophysical Union,Washington, D. C., USA</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:8154B757AA73960087AE6FA724AD5EFB5C6A89B4</idno><date when="2011" year="2011">2011</date><idno type="doi">10.1029/2011EO310002</idno><idno type="url">https://api.istex.fr/document/8154B757AA73960087AE6FA724AD5EFB5C6A89B4/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000465</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Glaciologist studies Greenland snow conditions and helps calibrate CryoSat instrument</title><author><name sortKey="Showstack, Randy" sort="Showstack, Randy" uniqKey="Showstack R" first="Randy" last="Showstack">Randy Showstack</name><affiliation><mods:affiliation>American Geophysical Union,Washington, D. C., USA</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Eos, Transactions American Geophysical Union</title><title level="j" type="abbrev">Eos Trans. AGU</title><idno type="ISSN">0096-3941</idno><idno type="eISSN">2324-9250</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2011-07-02">2011-07-02</date><biblScope unit="volume">92</biblScope><biblScope unit="issue">31</biblScope><biblScope unit="page" from="258">258</biblScope><biblScope unit="page" to="259">259</biblScope></imprint><idno type="ISSN">0096-3941</idno></series><idno type="istex">8154B757AA73960087AE6FA724AD5EFB5C6A89B4</idno><idno type="DOI">10.1029/2011EO310002</idno><idno type="ArticleID">EOST17991</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0096-3941</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract">GREENLAND—On a typically frigid mid‐July day at Summit Station, almost smack in the middle of Greenland, with the temperature hovering around −10°C, Elizabeth Morris and John Sweeny were bundled up against the cold atop their black Ski‐Doo snowmobiles, which Morris described as being similar to motorcycles on ski tracks. They drove the vehicles—without yet attaching three wooden sleds that would be pulled during their summer scientific traverse across part of central Greenland—on a practice spin along the perimeter of Summit's groomed, approximately 4600‐meter × 60‐meter snow runway. One of the longest runways in the world, it lies atop 3.2 kilometers of ice, with the horizon stretching in every direction. Morris, a glaciologist who is a senior associate at the Scott Polar Research Institute at Cambridge University, United Kingdom, and Sweeny, her polar guide, were taking advantage of an unexpected extra day at Summit, a scientific research station sponsored by the U.S. National Science Foundation (NSF), before the traverse began. They hoped that the socked‐in visibility just a few hours earlier that morning, 16 July, would not be repeated the following day so that a U.S. Air National Guard 109th Airlift Wing C‐130 cargo plane would be cleared to fly to Summit from Kangerlussuaq on Greenland's west coast with needed supplies. Morris and Sweeny would load up each sled with about 270 kilograms of gear.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>Randy Showstack</name><affiliations><json:string>American Geophysical Union,Washington, D. C., USA</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>Greenland</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>glacier</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>ice sheet</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>climate change</value></json:item></subject><articleId><json:string>EOST17991</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>news</json:string></originalGenre><abstract>GREENLAND—On a typically frigid mid‐July day at Summit Station, almost smack in the middle of Greenland, with the temperature hovering around −10°C, Elizabeth Morris and John Sweeny were bundled up against the cold atop their black Ski‐Doo snowmobiles, which Morris described as being similar to motorcycles on ski tracks. They drove the vehicles—without yet attaching three wooden sleds that would be pulled during their summer scientific traverse across part of central Greenland—on a practice spin along the perimeter of Summit's groomed, approximately 4600‐meter × 60‐meter snow runway. One of the longest runways in the world, it lies atop 3.2 kilometers of ice, with the horizon stretching in every direction. Morris, a glaciologist who is a senior associate at the Scott Polar Research Institute at Cambridge University, United Kingdom, and Sweeny, her polar guide, were taking advantage of an unexpected extra day at Summit, a scientific research station sponsored by the U.S. National Science Foundation (NSF), before the traverse began. They hoped that the socked‐in visibility just a few hours earlier that morning, 16 July, would not be repeated the following day so that a U.S. Air National Guard 109th Airlift Wing C‐130 cargo plane would be cleared to fly to Summit from Kangerlussuaq on Greenland's west coast with needed supplies. Morris and Sweeny would load up each sled with about 270 kilograms of gear.</abstract><qualityIndicators><score>5.806</score><pdfVersion>1.4</pdfVersion><pdfPageSize>612 x 792 pts (letter)</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>4</keywordCount><abstractCharCount>1423</abstractCharCount><pdfWordCount>2618</pdfWordCount><pdfCharCount>16114</pdfCharCount><pdfPageCount>3</pdfPageCount><abstractWordCount>224</abstractWordCount></qualityIndicators><title>Glaciologist studies Greenland snow conditions and helps calibrate CryoSat instrument</title><genre><json:string>article</json:string></genre><host><volume>92</volume><publisherId><json:string>EOST</json:string></publisherId><pages><total>2</total><last>259</last><first>258</first></pages><issn><json:string>0096-3941</json:string></issn><issue>31</issue><subject><json:item><value>CRYOSPHERE</value></json:item><json:item><value>Glaciers</value></json:item><json:item><value>Glaciology</value></json:item><json:item><value>Tundra</value></json:item><json:item><value>GLOBAL CHANGE</value></json:item><json:item><value>Cryospheric change</value></json:item><json:item><value>OCEANOGRAPHY: GENERAL</value></json:item><json:item><value>Arctic and Antarctic oceanography</value></json:item><json:item><value>GEOGRAPHIC LOCATION</value></json:item><json:item><value>Arctic region</value></json:item><json:item><value>News</value></json:item></subject><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>2324-9250</json:string></eissn><title>Eos, Transactions American Geophysical Union</title><doi><json:string>10.1002/(ISSN)2324-9250</json:string></doi></host><publicationDate>2011</publicationDate><copyrightDate>2011</copyrightDate><doi><json:string>10.1029/2011EO310002</json:string></doi><id>8154B757AA73960087AE6FA724AD5EFB5C6A89B4</id><score>0.15769838</score><fulltext><json:item><original>true</original><mimetype>application/pdf</mimetype><extension>pdf</extension><uri>https://api.istex.fr/document/8154B757AA73960087AE6FA724AD5EFB5C6A89B4/fulltext/pdf</uri></json:item><json:item><original>false</original><mimetype>application/zip</mimetype><extension>zip</extension><uri>https://api.istex.fr/document/8154B757AA73960087AE6FA724AD5EFB5C6A89B4/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/8154B757AA73960087AE6FA724AD5EFB5C6A89B4/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Glaciologist studies Greenland snow conditions and helps calibrate CryoSat instrument</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Blackwell Publishing Ltd</publisher><availability><p>Copyright 2011 by the American Geophysical Union</p></availability><date>2011</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Glaciologist studies Greenland snow conditions and helps calibrate CryoSat instrument</title><author xml:id="author-1"><persName><forename type="first">Randy</forename><surname>Showstack</surname></persName><affiliation>American Geophysical Union,Washington, D. C., USA</affiliation></author></analytic><monogr><title level="j">Eos, Transactions American Geophysical Union</title><title level="j" type="abbrev">Eos Trans. AGU</title><idno type="pISSN">0096-3941</idno><idno type="eISSN">2324-9250</idno><idno type="DOI">10.1002/(ISSN)2324-9250</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2011-07-02"></date><biblScope unit="volume">92</biblScope><biblScope unit="issue">31</biblScope><biblScope unit="page" from="258">258</biblScope><biblScope unit="page" to="259">259</biblScope></imprint></monogr><idno type="istex">8154B757AA73960087AE6FA724AD5EFB5C6A89B4</idno><idno type="DOI">10.1029/2011EO310002</idno><idno type="ArticleID">EOST17991</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>2011</date></creation><langUsage><language ident="en">en</language></langUsage><abstract><p>GREENLAND—On a typically frigid mid‐July day at Summit Station, almost smack in the middle of Greenland, with the temperature hovering around −10°C, Elizabeth Morris and John Sweeny were bundled up against the cold atop their black Ski‐Doo snowmobiles, which Morris described as being similar to motorcycles on ski tracks. They drove the vehicles—without yet attaching three wooden sleds that would be pulled during their summer scientific traverse across part of central Greenland—on a practice spin along the perimeter of Summit's groomed, approximately 4600‐meter × 60‐meter snow runway. One of the longest runways in the world, it lies atop 3.2 kilometers of ice, with the horizon stretching in every direction. Morris, a glaciologist who is a senior associate at the Scott Polar Research Institute at Cambridge University, United Kingdom, and Sweeny, her polar guide, were taking advantage of an unexpected extra day at Summit, a scientific research station sponsored by the U.S. National Science Foundation (NSF), before the traverse began. They hoped that the socked‐in visibility just a few hours earlier that morning, 16 July, would not be repeated the following day so that a U.S. Air National Guard 109th Airlift Wing C‐130 cargo plane would be cleared to fly to Summit from Kangerlussuaq on Greenland's west coast with needed supplies. Morris and Sweeny would load up each sled with about 270 kilograms of gear.</p></abstract><textClass><keywords scheme="keyword"><list><head>keywords</head><item><term>Greenland</term></item><item><term>glacier</term></item><item><term>ice sheet</term></item><item><term>climate change</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>index-terms</head><item><term>CRYOSPHERE</term></item><item><term>Glaciers</term></item><item><term>Glaciology</term></item><item><term>Tundra</term></item><item><term>GLOBAL CHANGE</term></item><item><term>Cryospheric change</term></item><item><term>OCEANOGRAPHY: GENERAL</term></item><item><term>Arctic and Antarctic oceanography</term></item><item><term>GEOGRAPHIC LOCATION</term></item><item><term>Arctic region</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>article-category</head><item><term>News</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2011-07-02">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><original>false</original><mimetype>text/plain</mimetype><extension>txt</extension><uri>https://api.istex.fr/document/8154B757AA73960087AE6FA724AD5EFB5C6A89B4/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley component found"><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="eost17991"><header><publicationMeta level="product"><doi>10.1002/(ISSN)2324-9250</doi><issn type="print">0096-3941</issn><issn type="electronic">2324-9250</issn><idGroup><id type="product" value="EOST"></id><id type="coden" value="ETAGCT"></id></idGroup><titleGroup><title type="main" xml:lang="en" sort="EOS, TRANSACTIONS AMERICAN GEOPHYSICAL UNION">Eos, Transactions American Geophysical Union</title><title type="short">Eos Trans. AGU</title></titleGroup></publicationMeta><publicationMeta level="part" position="310"><doi>10.1002/eost.v92.31</doi><numberingGroup><numbering type="journalVolume" number="92">92</numbering><numbering type="journalIssue">31</numbering></numberingGroup><coverDate startDate="2011-07-02">2 August 2011</coverDate></publicationMeta><publicationMeta level="unit" type="news" position="30" status="forIssue"><doi>10.1029/2011EO310002</doi><idGroup><id type="unit" value="EOST17991"></id></idGroup><countGroup><count type="pageTotal" number="2"></count></countGroup><titleGroup><title type="articleCategory">News</title><title type="tocHeading1">News</title></titleGroup><copyright ownership="thirdParty">Copyright 2011 by the American Geophysical Union</copyright><eventGroup><event type="firstOnline" date="2011-08-02"></event><event type="publishedOnlineFinalForm" date="2011-08-02"></event><event type="xmlConverted" agent="SPi Global Converter:AGUv5.2_TO_WileyML3Gv1.0.3 version:1.2; WileyML 3G Packaging Tool v1.0" date="2013-01-11"></event><event type="xmlConverted" agent="Converter:WILEY_ML3G_TO_WILEY_ML3GV2 version:3.8.8" date="2014-01-25"></event><event type="xmlConverted" agent="Converter:WML3G_To_WML3G version:4.1.7 mode:FullText,remove_FC" date="2014-10-16"></event></eventGroup><numberingGroup><numbering type="pageFirst">258</numbering><numbering type="pageLast">259</numbering></numberingGroup><subjectInfo><subject href="http://psi.agu.org/taxonomy5/0700">CRYOSPHERE</subject><subjectInfo><subject href="http://psi.agu.org/taxonomy5/0720">Glaciers</subject><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/0776">Glaciology</subject><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/0718">Tundra</subject></subjectInfo><subject href="http://psi.agu.org/taxonomy5/1600">GLOBAL CHANGE</subject><subjectInfo><subject href="http://psi.agu.org/taxonomy5/1621">Cryospheric change</subject></subjectInfo><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/4200">OCEANOGRAPHY: GENERAL</subject><subjectInfo><subject role="crossTerm" href="http://psi.agu.org/taxonomy5/4207">Arctic and Antarctic oceanography</subject></subjectInfo><subject href="http://psi.agu.org/taxonomy5/9300">GEOGRAPHIC LOCATION</subject><subjectInfo><subject href="http://psi.agu.org/taxonomy5/9315">Arctic region</subject></subjectInfo></subjectInfo><selfCitationGroup><citation xml:id="eost17991-cit-0000" type="self"><author><familyName>Showstack</familyName>,<givenNames>R.</givenNames></author>, (<pubYear year="2011">2011</pubYear>),<articleTitle>Glaciologist studies Greenland snow conditions and helps calibrate CryoSat instrument</articleTitle>, <journalTitle>Eos Trans. AGU</journalTitle>, <vol>92</vol>(<issue>31</issue>), <pageFirst>258</pageFirst>.</citation></selfCitationGroup><linkGroup><link type="toTypesetVersion" href="file:EOST.EOST17991.pdf"></link></linkGroup></publicationMeta><contentMeta><countGroup><count type="wordTotal" number="12600"></count><count type="figureTotal" number="1"></count></countGroup><titleGroup><title type="main">Glaciologist studies Greenland snow conditions and helps calibrate CryoSat instrument</title><title type="shortAuthors">Showstack</title></titleGroup><creators><creator xml:id="eost17991-cr-0001" creatorRole="author" affiliationRef="#eost17991-aff-0001"><personName><givenNames>Randy</givenNames><familyName>Showstack</familyName></personName></creator></creators><affiliationGroup><affiliation xml:id="eost17991-aff-0001" countryCode="US" type="organization"><unparsedAffiliation>American Geophysical Union,Washington, D. C., USA</unparsedAffiliation></affiliation></affiliationGroup><keywordGroup type="author"><keyword xml:id="eost17991-kwd-0001">Greenland</keyword><keyword xml:id="eost17991-kwd-0002">glacier</keyword><keyword xml:id="eost17991-kwd-0003">ice sheet</keyword><keyword xml:id="eost17991-kwd-0004">climate change</keyword></keywordGroup><abstractGroup><abstract type="main"><p xml:id="eost17991-para-0001" label="1">GREENLAND—On a typically frigid mid‐July day at Summit Station, almost smack in the middle of Greenland, with the temperature hovering around −10°C, Elizabeth Morris and John Sweeny were bundled up against the cold atop their black Ski‐Doo snowmobiles, which Morris described as being similar to motorcycles on ski tracks. They drove the vehicles—without yet attaching three wooden sleds that would be pulled during their summer scientific traverse across part of central Greenland—on a practice spin along the perimeter of Summit's groomed, approximately 4600‐meter × 60‐meter snow runway. One of the longest runways in the world, it lies atop 3.2 kilometers of ice, with the horizon stretching in every direction. Morris, a glaciologist who is a senior associate at the Scott Polar Research Institute at Cambridge University, United Kingdom, and Sweeny, her polar guide, were taking advantage of an unexpected extra day at Summit, a scientific research station sponsored by the U.S. National Science Foundation (NSF), before the traverse began. They hoped that the socked‐in visibility just a few hours earlier that morning, 16 July, would not be repeated the following day so that a U.S. Air National Guard 109th Airlift Wing C‐130 cargo plane would be cleared to fly to Summit from Kangerlussuaq on Greenland's west coast with needed supplies. Morris and Sweeny would load up each sled with about 270 kilograms of gear.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Glaciologist studies Greenland snow conditions and helps calibrate CryoSat instrument</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Glaciologist studies Greenland snow conditions and helps calibrate CryoSat instrument</title></titleInfo><name type="personal"><namePart type="given">Randy</namePart><namePart type="family">Showstack</namePart><affiliation>American Geophysical Union,Washington, D. C., USA</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="news"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><dateIssued encoding="w3cdtf">2011-07-02</dateIssued><edition>Showstack,R., (2011),Glaciologist studies Greenland snow conditions and helps calibrate CryoSat instrument, Eos Trans. AGU, 92(31), 258.</edition><copyrightDate encoding="w3cdtf">2011</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">1</extent><extent unit="words">12600</extent></physicalDescription><abstract>GREENLAND—On a typically frigid mid‐July day at Summit Station, almost smack in the middle of Greenland, with the temperature hovering around −10°C, Elizabeth Morris and John Sweeny were bundled up against the cold atop their black Ski‐Doo snowmobiles, which Morris described as being similar to motorcycles on ski tracks. They drove the vehicles—without yet attaching three wooden sleds that would be pulled during their summer scientific traverse across part of central Greenland—on a practice spin along the perimeter of Summit's groomed, approximately 4600‐meter × 60‐meter snow runway. One of the longest runways in the world, it lies atop 3.2 kilometers of ice, with the horizon stretching in every direction. Morris, a glaciologist who is a senior associate at the Scott Polar Research Institute at Cambridge University, United Kingdom, and Sweeny, her polar guide, were taking advantage of an unexpected extra day at Summit, a scientific research station sponsored by the U.S. National Science Foundation (NSF), before the traverse began. They hoped that the socked‐in visibility just a few hours earlier that morning, 16 July, would not be repeated the following day so that a U.S. Air National Guard 109th Airlift Wing C‐130 cargo plane would be cleared to fly to Summit from Kangerlussuaq on Greenland's west coast with needed supplies. Morris and Sweeny would load up each sled with about 270 kilograms of gear.</abstract><subject><genre>keywords</genre><topic>Greenland</topic><topic>glacier</topic><topic>ice sheet</topic><topic>climate change</topic></subject><relatedItem type="host"><titleInfo><title>Eos, Transactions American Geophysical Union</title></titleInfo><titleInfo type="abbreviated"><title>Eos Trans. AGU</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/taxonomy5/0720">Glaciers</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0776">Glaciology</topic><topic authorityURI="http://psi.agu.org/taxonomy5/0718">Tundra</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1600">GLOBAL CHANGE</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1621">Cryospheric change</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/taxonomy5/9300">GEOGRAPHIC LOCATION</topic><topic authorityURI="http://psi.agu.org/taxonomy5/9315">Arctic region</topic></subject><subject><genre>article-category</genre><topic>News</topic></subject><identifier type="ISSN">0096-3941</identifier><identifier type="eISSN">2324-9250</identifier><identifier type="DOI">10.1002/(ISSN)2324-9250</identifier><identifier type="CODEN">ETAGCT</identifier><identifier type="PublisherID">EOST</identifier><part><date>2011</date><detail type="volume"><caption>vol.</caption><number>92</number></detail><detail type="issue"><caption>no.</caption><number>31</number></detail><extent unit="pages"><start>258</start><end>259</end><total>2</total></extent></part></relatedItem><identifier type="istex">8154B757AA73960087AE6FA724AD5EFB5C6A89B4</identifier><identifier type="DOI">10.1029/2011EO310002</identifier><identifier type="ArticleID">EOST17991</identifier><accessCondition type="use and reproduction" contentType="copyright">Copyright 2011 by the American Geophysical Union</accessCondition><recordInfo><recordContentSource>WILEY</recordContentSource></recordInfo></mods></metadata><enrichments><json:item><type>multicat</type><uri>https://api.istex.fr/document/8154B757AA73960087AE6FA724AD5EFB5C6A89B4/enrichments/multicat</uri></json:item><json:item><type>refBibs</type><uri>https://api.istex.fr/document/8154B757AA73960087AE6FA724AD5EFB5C6A89B4/enrichments/refBibs</uri></json:item></enrichments><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Ticri/CIDE/explor/CyberinfraV1/Data/Istex/Corpus
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000465 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Istex/Corpus/biblio.hfd -nk 000465 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= Ticri/CIDE
|area= CyberinfraV1
|flux= Istex
|étape= Corpus
|type= RBID
|clé= ISTEX:8154B757AA73960087AE6FA724AD5EFB5C6A89B4
|texte= Glaciologist studies Greenland snow conditions and helps calibrate CryoSat instrument
}}
| This area was generated with Dilib version V0.6.25. |  |