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《SCIENTIA ATMOSPHERICA SINICA》 2000-01
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Large Scale Atmospheric Circulation Evolutions Associated with Summer Monsoon Onset in the South China Sea

Li Chongyin and Qu Xin (State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029)  
Mainly by using NCEP/NCAR reanalysis data (1980~1996), the large scale atmospheric circulation evolutions associated with summer monsoon onset in the South China Sea are studied based on the composite analyses corresponding to the onset dates The results clearly show that there are very evident variations of the atmospheric circulation (especially in South Asia and Southeast Asia) associated with the summer monsoon onset in the South China Sea, such as the wind field in the lower troposphere, the geopotential height field in the upper troposphere, the humidity and vertical velocity fields in South Asia and Southeast Asia The development and activity of the vortex pair at 850 hPa in South Asia and Southeast Asia regions and the withdraw eastwards of the subtropical high from the South China Sea play an important role in the onset of summer monsoon in the South China Sea There are also evident increases of the integrated humidity and vertical velocity at 500 hPa in the Bay of Bengal to the South China Sea area associated with the outbreak of summer monsoon in the South China Sea region The atmospheric circulation evolutions show that the onset of summer monsoon in the South China Sea region is a part of global circulation evolution from winter to summer and also it has regional abnormal feature It is still indicated that the onset of summer monsoon in the northern South China Sea is not earlier than that in the southern South China Sea The schematic diagram on the onset dates of the Asian summer monsoon before June is also shown
【Fund】: 国家攀登计划 !“南海季风试验研究”;;中国科学院资助!KZ951- B1- 408 项目
【CateGory Index】: P434
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