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.| | ||
| + | Author (L)=Youbin_Sun| | ||
| + | Author (L)=Delia_W._Oppo| | ||
| + | Author (L)=Rong_Xiang| | ||
| + | Author (L)=Weiguo_Liu| | ||
| + | Author (L)=Shu_Gao| | ||
| + | HasDOI (L)=10.1029/2004PA001061| | ||
| + | HasLink (L)=http://dx.doi.org/10.1029/2004PA001061| | ||
| + | Issue (L)=4| | ||
| + | Journal (L)=Paleoceanography| | ||
| + | PubDataUrl=doi.org| | ||
| + | PublicationYear (L)=2005| | ||
| + | Publisher=Wiley-Blackwell| | ||
| + | Title (L)=Last deglaciation in the Okinawa Trough: Subtropical northwest Pacific link to Northern Hemisphere and tropical climate| | ||
| + | Type=journal-article| | ||
| + | Volume (L)=20}} | ||
