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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 6
Clim. Past, 9, 2777–2788, 2013
https://doi.org/10.5194/cp-9-2777-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Western Pacific paleoceanography – an ocean history...

Clim. Past, 9, 2777–2788, 2013
https://doi.org/10.5194/cp-9-2777-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 13 Dec 2013

Research article | 13 Dec 2013

The East Asian winter monsoon variability in response to precession during the past 150 000 yr

M. Yamamoto1,2, H. Sai2,3, M.-T. Chen4, and M. Zhao5 M. Yamamoto et al.
  • 1Faculty of Environmental Earth Science, Hokkaido University, Kita-10, Nishi-5, Kita-ku, Sapporo 060-0810, Japan
  • 2Graduate School of Environmental Science, Hokkaido University, Kita-10, Nishi-5, Kita-ku, Sapporo 060-0810, Japan
  • 3Present address: Hitachi Advanced Systems Corporation. Yokohama 244-0817, Japan
  • 4Institute of Applied Geosciences, National Taiwan Ocean University, Keelung 20224, Taiwan
  • 5Key Laboratory of Marine Chemistry Theory and Technology of the Ministry of Education, Ocean University of China, Qingdao 266003, China

Abstract. The response of the East Asian winter monsoon variability to orbital forcing is still unclear, and hypotheses are controversial. We present a 150 000 yr record of sea surface temperature difference (ΔSST) between the South China Sea and other Western Pacific Warm Pool regions as a proxy for the intensity of the Asian winter monsoon, because the winter cooling of the South China Sea is caused by the cooling of surface water at the northern margin and the southward advection of cooled water due to winter monsoon winds. The ΔSST showed dominant precession cycles during the past 150 000 yr. The ΔSST varies at precessional band and supports the hypothesis that monsoon is regulated by insolation changes at low-latitudes (Kutzbach, 1981), but contradicts previous suggestions based on marine and loess records that eccentricity controls variability on glacial–interglacial timescales. Maximum winter monsoon intensity corresponds to the May perihelion at precessional band, which is not fully consistent with the Kutzbach model of maximum winter monsoon at the June perihelion. Variation in the East Asian winter monsoon was anti-phased with the Indian summer monsoon, suggesting a linkage of dynamics between these two monsoon systems on an orbital timescale.

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