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《Chinese Journal of Atmospheric Sciences》 2007-06
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The Influence of the East Asian Monsoon Stream on the Large-Scale Precipitation Course in Eastern China

JU Jian-Hua1,SUN Dan2,and L Jun-Mei31 Training Centre of China Meteorological Administration,Beijing 1000812 Department of Atmospheric Science,Yunnan University,Kunming 6500913 Chinese Academy of Meteorological Sciences,Beijing 100081  
The NCEP/NCAR 850 hPa zonal wind reanalysis data are calculated by using the band-pass filter to study the atmospheric intraseasonal oscillation,which can express the activity character of the East Asian summer monsoon stream.The results show that the mid to lower reaches of the Yangtze River and the Huaihe River basins during the flood years are characterized by the monsoon stream propagating northward.The essence of it is the Intraseasonal Oscillation(ISO) in the monsoon transfer from the tropical region to northward.In the northward propagation courses of the monsoon stream it is supplied by the ISO,which has zonal east and west propagations.The ISO in the zonal propagation will converge in 110°E-120°E,and then reinforces the ISO which propagates northward here.This reinforcement can make the ISO keep on propagating northward,which will have some influence on the summer large-scale precipitation course in eastern China.Otherwise the difference of the ISO zonal reinforcement may result in the difference of large-scale rainfall positions in eastern China.
【Fund】: 国家重点基础研究发展规划项目2006CB403603、2004CB418302;; 国家自然科学基金资助项目40675056
【CateGory Index】: P434.5
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