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The onset and advance of the Asian summer monsoon

science Bulletin 2006年第1期51卷 80-88页

作者： lü junmei1,2.4,{2., tao shiyan1 & ju jianhua3.1. state key laboratory of numerical modeling for atmospheric sci- ences and geophysical fluid dynamics, institute of atmospheric physics, chinese academy of sciences, Beijing 10002., china 2. Department of atmospheric sciences, Yunnan University, Kunming 650091, china 3. china Meteorological Administration Training Centre, Beijing 100081, china 4. Graduate School of chinese academy of sciences, Beijing 100039, china state key {2. of numerical modeling for atmospheric sciences and geophysical fluid dynamics Institute of Atmospheric Physics Chinese Academy of Sciences Beijing China Department of atmospheric sci{2. Yunnan University Kunming China Graduate School of chinese academy of {2.ences Beijing China china Meteorological Administration Training Centre Beijing China

Based on the daily outgoing longwave radiation (OlR) data from National Oceanic and At- mospheric Administration (NOAA) satellites, the Cli- mate Prediction Center’s merged analysis of pre- cipitation (CMAP) data and the National Centers for Environmental Prediction/National Center for At- mospheric Research (NCEP/NCAR) reanalysis dataset, the mean intraseasonal variability of the Asian summer monsoon (ASM) is investigated by using power spectrum analysis, band-pass filter, and diagnostic analyses. The processes of the onset and advance of monsoon over the southern part of Indo- china Peninsula, the east coast of Bay of Bengal, the South china Sea and the Indian subcontinent are explored. It is found that there is an abrupt change in OlR, precipitation and zonal wind during the onset and advance of the ASM. It is also indicated that the southern part of Indo{2. Peninsula and the adja- cent Andaman Sea is the region where the earliest onset of the ASM occurs in the 2.d pentad of May.

关键词： Asian summer monsoon intraseasonal variability onset advance.

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