Climatology and interannual variability of the Southeast Asian summer monsoon

被引:549
作者
Lau K.-M. [1 ]
Yang S. [2 ]
机构
[1] Laboratory for Atmospheres, Code 913, NASA-Goddard Space Flight Center, Greenbelt
[2] Laboratory for Atmospheres, NASA-Goddard Space Flight Center, Greenbelt
关键词
Climatology; Interannual variability; Onset; South China Sea; Southeast Asian monsoon;
D O I
10.1007/s00376-997-0016-y
中图分类号
学科分类号
摘要
In this paper, results from a pilot study for the South China Sea Monsoon Experiment are reported. Based on analyses of 9 years of pentad and monthly mean data, the climatology of subseasonal features and interannual variability of the Southeast Asian monsoon (SEAM) are documented. The present analysis is focused on the sudden onset of the South China Sea monsoon and its relation to the atmospheric and oceanic processes on the entire Asian monsoon region. It is found that the onset of the SEAM occurs around mid-May, signaling the earliest stage of the entire Asian summer monsoon system. The establishment of monsoon rainfall over the South China Sea is abrupt, being accompanied by substantial changes in the large scale atmospheric circulation and sea surface temperature in the adjacent oceans. The onset and fluctuations of SEAM involve the interaction and metamorphosis of the large scale convection over the Indo-China, the South China Sea and the southern Bay of Bengal. Results show that the onset time of the SEAM differs greatly from one year to another. The delayed (advanced) onset of the monsoon may be related to basin-wide warm (cold) events of the Pacific and Indian Oceans. We also present evidence showing that the SEAM fluctuations in May may foreshadow the development of the full-scale Asian summer morisoon during the subsequent months.
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页码:141 / 162
页数:21
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  • [1] Arkin P., Meisner B.N., The relationship between large-scale convective rainfall and cold cloud over the Western Hemisphere during 1982-85, Mon. Wea. Rev., 115, pp. 51-74, (1987)
  • [2] Chen G.T.-J., The large-scale features associated with the Meiyu over South China and Taiwan, From Atmospheric Circulation to Global Change, pp. 289-313, (1996)
  • [3] Chen L., Zhu Q., Luo H., He J., Dong M., Feng Z., East Asian Monsoon, (1991)
  • [4] Chen T.-C., Weng S.P., Some effects of the intraseasonal oscillation on the equatorial waves over the western tropical Pacific-South China Sea region during the northern summer, Mon. Wea. Rev., (1996)
  • [5] Chu P.C., Li C., Ko D., Mooers C.N.K., A numerical simulation of seasonal circulation in the South China Sea, AGU Fall Meeting, (1993)
  • [6] Ding Y., Wang Q., Yan J., Some aspects of climatology of the summer monsoon over the South China Sea, From Atmospheric Circulation to Global Change, pp. 329-339, (1996)
  • [7] Goddard L., Graham N.E., El Niño in the 1990's, J. Geophys. Res., (1996)
  • [8] He H., McGinnis J.W., Song Z., Yanai M., Onset of the Asian monsoon in 1979 and the effect of Tibetan Plateau, Mon. Wea. Rev., 115, pp. 1966-1995, (1987)
  • [9] Ho C., Et al., The abrupt transitions and multiple onsets associated with the East Asian monsoon, Mon. Wea. Rev., (1996)
  • [10] Hoskins B., On the existence and strength of the summer subtropical anticyclones, Bull. Amer. Meteor. Soc., 77, pp. 1287-1292, (1996)