Understanding feedback mechanisms of the Indo‐Pacific Ocean climate system
Identifieur interne : 000318 ( Istex/Corpus ); précédent : 000317; suivant : 000319Understanding feedback mechanisms of the Indo‐Pacific Ocean climate system
Auteurs : Gary Meyers ; Wenju CaiSource :
- Eos, Transactions American Geophysical Union [ 0096-3941 ] ; 2011-07-02.
Abstract
Indo‐Pacific Climate Variability and Change Workshop; Cairns, Queensland, Australia, 7–8 April 2011; The latest in the Australian GREENHOUSE conference series, GREENHOUSE 2011, provided scientists and representatives from industry and all levels of government the opportunity to hear about the latest in climate change science from leading researchers from Australia and around the world. This year's conference included a workshop on Indo‐Pacific climate variability and change that focused on interactions between the two ocean basins, their teleconnections, and how these might change in the future. There were 16 presentations by participants, which are now available at http://www.greenhouse2011.com/page.aspx?docid=11. Several talks at the workshop identified feedback mechanisms that control the development and structure of climate modes, using both observations and Coupled Model Intercomparison Project Phase 3 (CMIP3) results for the twentieth and 21st centuries. For example, skewness in the Indian Ocean Dipole (IOD) was associated with nonlinear temperature advection, sea surface temperature (SST)‐cloud‐radiation feedback, and feedbacks among the thermocline, SST, and wind. Observations indicated that the frequency of the IOD has increased since 1950. However, there were varying interpretations on the relative strengths of the feedbacks, how they will change in the future, and whether the increased frequency of the IOD is induced by natural variation or human activity.
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DOI: 10.1029/2011EO310004
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This year's conference included a workshop on Indo‐Pacific climate variability and change that focused on interactions between the two ocean basins, their teleconnections, and how these might change in the future. There were 16 presentations by participants, which are now available at <url href="http://www.greenhouse2011.com/page.aspx?docid=11">http://www.greenhouse2011.com/page.aspx?docid=11</url>. Several talks at the workshop identified feedback mechanisms that control the development and structure of climate modes, using both observations and Coupled Model Intercomparison Project Phase 3 (CMIP3) results for the twentieth and 21st centuries. For example, skewness in the Indian Ocean Dipole (IOD) was associated with nonlinear temperature advection, sea surface temperature (SST)‐cloud‐radiation feedback, and feedbacks among the thermocline, SST, and wind. Observations indicated that the frequency of the IOD has increased since 1950. However, there were varying interpretations on the relative strengths of the feedbacks, how they will change in the future, and whether the increased frequency of the IOD is induced by natural variation or human activity.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Understanding feedback mechanisms of the Indo‐Pacific Ocean climate system</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Understanding feedback mechanisms of the Indo‐Pacific Ocean climate system</title></titleInfo><name type="personal"><namePart type="given">Gary</namePart><namePart type="family">Meyers</namePart><affiliation>Commonwealth Scientific and Industrial Research Organisation (CSIRO) Marine and Atmospheric Research, Australia</affiliation><affiliation>University of Tasmania, Hobart, Tasmania, Australia</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Wenju</namePart><namePart type="family">Cai</namePart><affiliation>CSIRO Marine and Atmospheric Research,Aspendale, Victoria, Australia</affiliation><affiliation>E-mail: wenju.cai@csiro.au</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="conference" displayLabel="meetingReport"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><dateIssued encoding="w3cdtf">2011-07-02</dateIssued><edition>Meyers, G., and W.Cai (2011), Understanding feedback mechanisms of the Indo‐Pacific Ocean climate system, Eos Trans. AGU, 92(31), 260.</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="words">3700</extent></physicalDescription><abstract>Indo‐Pacific Climate Variability and Change Workshop; Cairns, Queensland, Australia, 7–8 April 2011; The latest in the Australian GREENHOUSE conference series, GREENHOUSE 2011, provided scientists and representatives from industry and all levels of government the opportunity to hear about the latest in climate change science from leading researchers from Australia and around the world. This year's conference included a workshop on Indo‐Pacific climate variability and change that focused on interactions between the two ocean basins, their teleconnections, and how these might change in the future. There were 16 presentations by participants, which are now available at http://www.greenhouse2011.com/page.aspx?docid=11. Several talks at the workshop identified feedback mechanisms that control the development and structure of climate modes, using both observations and Coupled Model Intercomparison Project Phase 3 (CMIP3) results for the twentieth and 21st centuries. For example, skewness in the Indian Ocean Dipole (IOD) was associated with nonlinear temperature advection, sea surface temperature (SST)‐cloud‐radiation feedback, and feedbacks among the thermocline, SST, and wind. Observations indicated that the frequency of the IOD has increased since 1950. However, there were varying interpretations on the relative strengths of the feedbacks, how they will change in the future, and whether the increased frequency of the IOD is induced by natural variation or human activity.</abstract><subject><genre>keywords</genre><topic>Indo‐Pacific</topic><topic>the IOD and ENSO</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/taxonomy5/1600">GLOBAL CHANGE</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1616">Climate variability</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/taxonomy5/1616">Climate variability</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1635">Oceans</topic><topic authorityURI="http://psi.agu.org/taxonomy5/1635">Oceans</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/taxonomy5/3309">Climatology</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3305">Climate change and variability</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3309">Climatology</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3305">Climate change and variability</topic><topic authorityURI="http://psi.agu.org/taxonomy5/3309">Climatology</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4200">OCEANOGRAPHY: GENERAL</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4215">Climate and interannual variability</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4231">Equatorial oceanography</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4215">Climate and interannual variability</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/taxonomy5/4522">ENSO</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4513">Decadal ocean variability</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4513">Decadal ocean variability</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4513">Decadal ocean variability</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4900">PALEOCEANOGRAPHY</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4922">El Nino</topic></subject><subject><genre>article-category</genre><topic>Meetings</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>260</start><end>260</end><total>1</total></extent></part></relatedItem><identifier type="istex">C21666422B10484D36C3D08D046452ED35DE8587</identifier><identifier type="DOI">10.1029/2011EO310004</identifier><identifier type="ArticleID">EOST17993</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/C21666422B10484D36C3D08D046452ED35DE8587/enrichments/multicat</uri></json:item><json:item><type>refBibs</type><uri>https://api.istex.fr/document/C21666422B10484D36C3D08D046452ED35DE8587/enrichments/refBibs</uri></json:item></enrichments><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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