Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics
The ocean currents connecting the western tropical Pacific Ocean with the eastern tropical Pacific Ocean are driven by surface winds. The surface winds are in turn driven by the sea-surface temperature (SST) differences between these two regions. This dynamic coupling between the atmosphere and ocea...
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Veröffentlicht in: | Science 1996-05, Vol.272 (5265), p.1148-1150 |
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description | The ocean currents connecting the western tropical Pacific Ocean with the eastern tropical Pacific Ocean are driven by surface winds. The surface winds are in turn driven by the sea-surface temperature (SST) differences between these two regions. This dynamic coupling between the atmosphere and ocean may limit the SST in the tropical Pacific Ocean to below 305 kelvin even in the absence of cloud feedbacks. |
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The surface winds are in turn driven by the sea-surface temperature (SST) differences between these two regions. This dynamic coupling between the atmosphere and ocean may limit the SST in the tropical Pacific Ocean to below 305 kelvin even in the absence of cloud feedbacks.</description><identifier>ISSN: 0036-8075</identifier><identifier>EISSN: 1095-9203</identifier><identifier>DOI: 10.1126/science.272.5265.1148</identifier><identifier>PMID: 8662447</identifier><identifier>CODEN: SCIEAS</identifier><language>eng</language><publisher>Washington, DC: American Society for the Advancement of Science</publisher><subject>AMBIENT TEMPERATURE ; Atmosphere ; ATMOSPHERIC CIRCULATION ; Climate ; CLIMATE MODELS ; Clouds ; Earth, ocean, space ; ENVIRONMENTAL SCIENCES ; Exact sciences and technology ; External geophysics ; Heat ; Ocean circulation models ; Ocean currents ; Ocean temperature ; Ocean-atmosphere interaction ; OCEANIC CIRCULATION ; Oceans ; Physics of the oceans ; Sea-air exchange processes ; Surface temperature ; Temperature ; Thermodynamic equilibrium ; Tropical climates ; TROPICAL REGIONS ; Water ; Water vapor</subject><ispartof>Science, 1996-05, Vol.272 (5265), p.1148-1150</ispartof><rights>Copyright 1996 American Association for the Advancement of Science</rights><rights>1996 INIST-CNRS</rights><rights>COPYRIGHT 1996 American Association for the Advancement of Science</rights><rights>COPYRIGHT 1996 American Association for the Advancement of Science</rights><rights>Copyright American Association for the Advancement of Science May 24, 1996</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c748t-efab46cc6a194e9fbd95d43c12d6794715e39b4834261529cc86af3e07dc25fc3</citedby><cites>FETCH-LOGICAL-c748t-efab46cc6a194e9fbd95d43c12d6794715e39b4834261529cc86af3e07dc25fc3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/2889939$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/2889939$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>315,781,785,804,886,2885,2886,27929,27930,58022,58255</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=3091814$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/8662447$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink><backlink>$$Uhttps://www.osti.gov/biblio/377234$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Sun, De-Zheng</creatorcontrib><creatorcontrib>Liu, Zhengyu</creatorcontrib><title>Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics</title><title>Science</title><addtitle>Science</addtitle><description>The ocean currents connecting the western tropical Pacific Ocean with the eastern tropical Pacific Ocean are driven by surface winds. The surface winds are in turn driven by the sea-surface temperature (SST) differences between these two regions. This dynamic coupling between the atmosphere and ocean may limit the SST in the tropical Pacific Ocean to below 305 kelvin even in the absence of cloud feedbacks.</description><subject>AMBIENT TEMPERATURE</subject><subject>Atmosphere</subject><subject>ATMOSPHERIC CIRCULATION</subject><subject>Climate</subject><subject>CLIMATE MODELS</subject><subject>Clouds</subject><subject>Earth, ocean, space</subject><subject>ENVIRONMENTAL SCIENCES</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Heat</subject><subject>Ocean circulation models</subject><subject>Ocean currents</subject><subject>Ocean temperature</subject><subject>Ocean-atmosphere interaction</subject><subject>OCEANIC CIRCULATION</subject><subject>Oceans</subject><subject>Physics of the oceans</subject><subject>Sea-air exchange processes</subject><subject>Surface temperature</subject><subject>Temperature</subject><subject>Thermodynamic equilibrium</subject><subject>Tropical 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for the Tropics</atitle><jtitle>Science</jtitle><addtitle>Science</addtitle><date>1996-05-24</date><risdate>1996</risdate><volume>272</volume><issue>5265</issue><spage>1148</spage><epage>1150</epage><pages>1148-1150</pages><issn>0036-8075</issn><eissn>1095-9203</eissn><coden>SCIEAS</coden><abstract>The ocean currents connecting the western tropical Pacific Ocean with the eastern tropical Pacific Ocean are driven by surface winds. The surface winds are in turn driven by the sea-surface temperature (SST) differences between these two regions. This dynamic coupling between the atmosphere and ocean may limit the SST in the tropical Pacific Ocean to below 305 kelvin even in the absence of cloud feedbacks.</abstract><cop>Washington, DC</cop><pub>American Society for the Advancement of Science</pub><pmid>8662447</pmid><doi>10.1126/science.272.5265.1148</doi><tpages>3</tpages></addata></record> |
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subjects | AMBIENT TEMPERATURE Atmosphere ATMOSPHERIC CIRCULATION Climate CLIMATE MODELS Clouds Earth, ocean, space ENVIRONMENTAL SCIENCES Exact sciences and technology External geophysics Heat Ocean circulation models Ocean currents Ocean temperature Ocean-atmosphere interaction OCEANIC CIRCULATION Oceans Physics of the oceans Sea-air exchange processes Surface temperature Temperature Thermodynamic equilibrium Tropical climates TROPICAL REGIONS Water Water vapor |
title | Dynamic Ocean-Atmosphere Coupling: A Thermostat for the Tropics |
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