Difference between revisions of "Publication.10.1029/2004PA001061"

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Abstract=Detailed deglacial and Holocene records of planktonic d18O and Mg/Ca-based sea surface temperature (SST) from the Okinawa Trough suggest that at ~18 to 17 thousand years before present (kyr B.P.), late spring/early summer SSTs were approximately 3°C cooler than today, while surface waters were up to 1 practical salinity unit saltier. These conditions are consistent with a weaker influence of the summer East Asian Monsoon (EAM) than today. The timing of suborbital SST oscillations suggests a close link with abrupt changes in the EAM and North Atlantic climate. A tropical influence, however, may have resulted in subtle decoupling between the North Atlantic and the Okinawa Trough/EAM during the deglaciation. Okinawa Trough surface water trends in the Holocene are consistent with model simulations of an inland shift of intense EAM precipitation during the middle Holocene. Millennial-scale alternations between relatively warm, salty conditions and relatively cold, fresh conditions suggest varying influence of the Kuroshio during the Holocene.|
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Author (L)=Youbin_Sun|
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Author (L)=Delia_W._Oppo|
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Author (L)=Rong_Xiang|
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Author (L)=Weiguo_Liu|
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Author (L)=Shu_Gao|
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HasDOI (L)=10.1029/2004PA001061|
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HasLink (L)=http://dx.doi.org/10.1029/2004PA001061|
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Issue (L)=4|
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Journal (L)=Paleoceanography|
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PubDataUrl=doi.org|
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PublicationYear (L)=2005|
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Publisher=Wiley-Blackwell|
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Title (L)=Last deglaciation in the Okinawa Trough: Subtropical northwest Pacific link to Northern Hemisphere and tropical climate|
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Type=journal-article|
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Volume (L)=20}}

Latest revision as of 21:41, 16 May 2017