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Please use this identifier to cite or link to this item: http://ntour.ntou.edu.tw:8080/ir/handle/987654321/24768

Title: Ice-volume forcing of winter monsoon climate in the South China Sea
Authors: Min-Te Chen;Chi-Yue Huang
Contributors: NTOU:Institute of Applied Geosciences
國立臺灣海洋大學:應用地球科學研究所
Keywords: WESTERN EQUATORIAL PACIFIC;NORTH-ATLANTIC;LAST GLACIATION;ACCUMULATION RATES;GREENLAND ICE;INDIAN-OCEAN;C-14 AGES;DEEP-SEA;RECORDS;LOESS
Date: 1998
Issue Date: 2011-10-20T08:17:37Z
Publisher: PALEOCEANOGRAPHY
Abstract: abstract:High-resolution studies of a planktonic foraminifer core record from the South China Sea (SCS) (31KL: 18°45.4′N, 115°52.4′E, water depth 3360 m) reveal changes driven by ice-volume forcings in the climate of the East Asian monsoon in the western Pacific marginal sea during the late Quaternary. The analyses of planktonic foraminifer faunal abundance data from the core indicate significant variations in the relative abundances of the dominant taxa over the past 100,000 years since the isotope stage 5. The transfer function estimates of faunal sea surface temperatures (SST) correlate well with a long-term (104–105 years) trend of global glaciation. About 65,000 years ago, there was an observable change in the mode of SST variability as many low-latitude records have shown. These findings suggest that the SCS surface circulation and the East Asian winter monsoon systems are mainly driven by variations in global glaciation levels. The association of surface ocean cooling in the SCS with global climatic events suggests that fluctuations in the strength of the East Asian winter monsoon may be linked to shifts in the latitudinal position of the westerly winds and the Siberian high-pressure system.
Relation: 13(6), pp.622–633
URI: http://ntour.ntou.edu.tw/handle/987654321/24768
Appears in Collections:[應用地球科學研究所] 期刊論文

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