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Forcing mechanism of the Pleistocene east Asian monsoon variations in a phase perspective

Science china Earth Sciences 2005年第10期48卷 1708-1717页

作者： tian jun1,2. wang pinxian1,{2., wang rujian1 & sun xiangjun1,3 1. state key laboratory of marine geology, tongji university, shanghai 2.0092. china 2. Institute of geology and Geophysics, Chinese Academy of Sciences, Beijing 10002., china 3. Institute of Botany, Chinese Academy of Sciences, Beijing 100093, china tongji {1. Chinese Academy of Sciences

The deep sea records from the ODP Sites 1.43 and 1.44 in the northern and southern South china Sea (SCS), including foraminiferal δ 1.O and δ 1.C, Opal% and pollen percentage, reveal that the variations of the east Asian monsoon have been closely correlated with the variations of the Earth’s orbital parameters (eccentricity, obliquity and precession) and the global ice volume on orbital scale. All the monsoonal proxies show strong 1.0 ka, 41.ka and {1. ka cycles. Although G. ruber δ 1.C of Site 1.43 is coherent with the ETP (ETP= normalized (eccentricity + obliquity-precession) at eccentricity, obliquity and precession bands, most of the coherent relationship focuses on the precession band, and the other monsoonal proxies are coherent with the ETP only at the precession band, which indicate that precession dominates the Pleistocene tropical climate changes. The phase relationship of the monsoonal proxies with the foraminiferal δ 1.O implies that the global ice volume changes have played a significant role in modulating the east Asian monsoon climate, at least dominating the winter monsoon. This forcing mechanism of the east Asian monsoon is apparently different from that of the Indian ocean mon-soon. The variations of the east Asian monsoon at the precession band, at least that of the winter monsoon, have been controlled not only by the sensible heating but also by the latent heating of the surface water in the South china Sea.

关键词： South china Sea, ODP, east Asian monsoon, orbital forcing, global ice volume.

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