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Subpolar Gyre Index and the North Atlantic Meridional Overturning Circulation in a Coupled Climate Model

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dc.contributor.author Gao, Yongqi eng
dc.contributor.author Yu, Lei eng
dc.date.accessioned 2009-06-29T06:56:16Z
dc.date.available 2009-06-29T06:56:16Z
dc.date.issued 2008-11-16 eng
dc.identifier.citation http://www.iapjournals.ac.cn/aosl/ch/reader/new_year_article.aspx?year_id=2008&quarter_id=1 en
dc.identifier.issn 1674-2834 eng
dc.identifier.uri http://hdl.handle.net/1956/3302
dc.description.abstract The subpolar gyre index (SPG), derived from the analysis of sea surface height (SSH), is proposed to be a potential indicator for the North Atlantic Meridional Overturning Circulation (AMOC) based on observation as well as the Ocean General Circulation Model (OGCM). We investigated the correspondence between the SPG and the AMOC in a coupled climate model. Our results confirm that the SPG can be used as an early indicator for the AMOC in the subtropical North Atlantic. Changes in the SPG are closely related to variations in the air-sea heat exchange in the Labrador Sea, and variations in deep water formation and southward dense water transport with the deep western boundary current (DWBC) in the North Atlantic. en
dc.language.iso eng eng
dc.publisher Institute of Atmospheric Physics, Chinese Academy of Sciences en
dc.relation.ispartofseries Atmospheric and Oceanic Science Letters en
dc.relation.ispartofseries (1)1 2008 p. 29-32 en
dc.subject North Atlantic meridional overturning circulation eng
dc.subject Subpolar gyre index eng
dc.title Subpolar Gyre Index and the North Atlantic Meridional Overturning Circulation in a Coupled Climate Model en
dc.type Journal article eng
dc.subject.nsi VDP::Matematikk og Naturvitenskap: 400 nob


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