Sea ice feedbacks observed in western Weddell Sea
Identifieur interne : 000E16 ( Istex/Corpus ); précédent : 000E15; suivant : 000E17Sea ice feedbacks observed in western Weddell Sea
Auteurs : Hartmut H. Hellmer ; Christian Haas ; Gerhard S. Dieckmann ; Michael SchröderSource :
- Eos, Transactions American Geophysical Union [ 0096-3941 ] ; 2006-05-02.
Abstract
The western Weddell Sea is the largest region of perennial sea ice in the Southern Ocean. Although poorly explored, earlier studies suggest that it hosts important sources for deep and bottom water ventilating of the global abyss. Ocean structure limits ice melt because the oceanic heat flux is only a few watts per square meter, and wind change in summer prevents the large‐scale northward movement of the pack ice [Hunke andAckley, 2001]. As the ice melts,the absence of melt ponds and the development of gap‐like porous internal layers with extremely high amounts of algal standing stocks have large implications for primary productivity and biogeochemical cycles.
Url:
DOI: 10.1029/2006EO180001
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Although poorly explored, earlier studies suggest that it hosts important sources for deep and bottom water ventilating of the global abyss. Ocean structure limits ice melt because the oceanic heat flux is only a few watts per square meter, and wind change in summer prevents the large‐scale northward movement of the pack ice [Hunke andAckley, 2001]. As the ice melts,the absence of melt ponds and the development of gap‐like porous internal layers with extremely high amounts of algal standing stocks have large implications for primary productivity and biogeochemical cycles.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>Hartmut H. 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Although poorly explored, earlier studies suggest that it hosts important sources for deep and bottom water ventilating of the global abyss. Ocean structure limits ice melt because the oceanic heat flux is only a few watts per square meter, and wind change in summer prevents the large‐scale northward movement of the pack ice [Hunke andAckley, 2001]. 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Sci.</title></host><title>On the differences in ablation seasons of Arctic and Antarctic sea ice</title></json:item><json:item><author><json:item><name>A. Gordon</name></json:item></author><host><volume>75</volume><pages><last>240</last><first>215</first></pages><author></author><title>Ocean, Ice, and Atmosphere: Interactions at the Antarctic Continental Margin, Antarct. Res. Ser</title></host><title>Western Weddell Sea thermo‐haline stratification</title></json:item><json:item><author><json:item><name>A. Gordon</name></json:item></author><host><volume>74</volume><pages><first>121</first></pages><issue>11</issue><author></author><title>Eos Trans. AGU</title></host><title>Weddell Sea exploration from ice station</title></json:item><json:item><author><json:item><name>C. Haas</name></json:item></author><host><volume>33</volume><pages><last>73</last><first>69</first></pages><author></author><title>Ann. Glaciol.</title></host><title>The seasonal cycle of ERS scatterometer signatures over perennial Antarctic Sea ice and associated surface ice properties and processes</title></json:item><json:item><author><json:item><name>C. Haas</name></json:item><json:item><name>D. N. Thomas</name></json:item><json:item><name>J. Bareiss</name></json:item></author><host><volume>47</volume><pages><last>625</last><first>613</first></pages><issue>159</issue><author></author><title>J. Glaciol.</title></host><title>Surface properties and processes of perennial Antarctic sea ice in summer</title></json:item><json:item><author><json:item><name>E. C. Hunke</name></json:item><json:item><name>S. F. Ackley</name></json:item></author><host><volume>106</volume><pages><last>22,382</last><first>22,373</first></pages><issue>C10</issue><author></author><title>J. Geophys. Res.</title></host><title>A numerical investigation of the 1997‐1998 Ronne polynya</title></json:item><json:item><author><json:item><name>S. Willmes</name></json:item><json:item><name>J. Bareiss</name></json:item><json:item><name>C. Haas</name></json:item></author><host><author></author><title>Ann. 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H.</givenNames></author>, <author><givenNames>C.</givenNames> <familyName>Haas</familyName></author>, <author><givenNames>G. S.</givenNames> <familyName>Dieckmann</familyName></author>, and <author><givenNames>M.</givenNames> <familyName>Schröder</familyName></author> (<pubYear year="2006">2006</pubYear>), <articleTitle>Sea ice feedbacks observed in western Weddell Sea</articleTitle>, <journalTitle>Eos Trans. AGU</journalTitle>, <vol>87</vol>(<issue>18</issue>), <pageFirst>173</pageFirst>–<pageLast>179</pageLast>, doi:<accessionId ref="info:doi/10.1029/2006EO180001">10.1029/2006EO180001</accessionId>.</citation></selfCitationGroup><linkGroup><link type="toTypesetVersion" href="file:EOST.EOST15477.pdf"></link></linkGroup></publicationMeta><contentMeta><titleGroup><title type="main">Sea ice feedbacks observed in western Weddell Sea</title><title type="shortAuthors">Hellmer ET AL.</title></titleGroup><creators><creator xml:id="eost15477-cr-0001" affiliationRef="#eost15477-aff-0001"><personName><givenNames>Hartmut H.</givenNames><familyName>Hellmer</familyName></personName></creator><creator xml:id="eost15477-cr-0002" affiliationRef="#eost15477-aff-0001"><personName><givenNames>Christian</givenNames><familyName>Haas</familyName></personName></creator><creator xml:id="eost15477-cr-0003" affiliationRef="#eost15477-aff-0001"><personName><givenNames>Gerhard S.</givenNames><familyName>Dieckmann</familyName></personName></creator><creator xml:id="eost15477-cr-0004" affiliationRef="#eost15477-aff-0001"><personName><givenNames>Michael</givenNames><familyName>Schröder</familyName></personName></creator></creators><affiliationGroup><affiliation xml:id="eost15477-aff-0001" type="organization"><unparsedAffiliation>Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany</unparsedAffiliation></affiliation></affiliationGroup><abstractGroup><abstract type="main"><p xml:id="eost15477-para-0001">The western Weddell Sea is the largest region of perennial sea ice in the Southern Ocean. Although poorly explored, earlier studies suggest that it hosts important sources for deep and bottom water ventilating of the global abyss. Ocean structure limits ice melt because the oceanic heat flux is only a few watts per square meter, and wind change in summer prevents the large‐scale northward movement of the pack ice [Hunke andAckley, 2001]. As the ice melts,the absence of melt ponds and the development of gap‐like porous internal layers with extremely high amounts of algal standing stocks have large implications for primary productivity and biogeochemical cycles.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Sea ice feedbacks observed in western Weddell Sea</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Sea ice feedbacks observed in western Weddell Sea</title></titleInfo><name type="personal"><namePart type="given">Hartmut H.</namePart><namePart type="family">Hellmer</namePart><affiliation>Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany</affiliation></name><name type="personal"><namePart type="given">Christian</namePart><namePart type="family">Haas</namePart><affiliation>Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany</affiliation></name><name type="personal"><namePart type="given">Gerhard S.</namePart><namePart type="family">Dieckmann</namePart><affiliation>Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany</affiliation></name><name type="personal"><namePart type="given">Michael</namePart><namePart type="family">Schröder</namePart><affiliation>Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany</affiliation></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><dateIssued encoding="w3cdtf">2006-05-02</dateIssued><edition>Hellmer, H. H., C. Haas, G. S. Dieckmann, and M. Schröder (2006), Sea ice feedbacks observed in western Weddell Sea, Eos Trans. AGU, 87(18), 173–179, doi:10.1029/2006EO180001.</edition><copyrightDate encoding="w3cdtf">2006</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract>The western Weddell Sea is the largest region of perennial sea ice in the Southern Ocean. Although poorly explored, earlier studies suggest that it hosts important sources for deep and bottom water ventilating of the global abyss. Ocean structure limits ice melt because the oceanic heat flux is only a few watts per square meter, and wind change in summer prevents the large‐scale northward movement of the pack ice [Hunke andAckley, 2001]. 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|clé= ISTEX:5280CF6601757BA6436C4E5AFBA17793F347A870
|texte= Sea ice feedbacks observed in western Weddell Sea
}}
| This area was generated with Dilib version V0.6.31. |  |