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《Plateau Meteorology》 2006-02
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Analyses on General Circulation Character of Precipitation Anomaly in Northeast China Flood Season

JIA Xiao-long,WANG Qian-qian (Department of Atmosphere Science,Nanjing University of Information Science and Technology,Nanjing 210044,China)  
To better understand and predict the flood season(July~August) precipitation in Northeast China,the general circulation in the years with above- and below the normal precipitation is analyzed.The results show that,on lower layer(850 hPa),the common action of cyclonic(anti-cyclonic) anomaly circulation in Southeast of Mongolia,the southwest(northeast) wind anomaly in East of China and anti-cyclonic(cyclonic) anomaly circulation in south of Japan have strengthened(weakened) the convergence of southwest warm and humid air flows of low layer in Northeast China region in more rain year of flood season.On middle layer(500 hPa),the meridional movement of westly belt in high-middle latitudes strengrhen(weakened),there are +-+wave train distributions from the high latitude region to the north of Baikal to the height field near Japan.The circulation pattern in August is easier resulting in severe drought and flooding than in July.The developing and weakening of blocking highs in low reach of Okhotsk and Japan seas are to cause an important facter of precipitation anomaly in August.Considering with the evolution of drought and flooding patterns,we have special attention to the \!wave train\" allocation of-+-+-westeast-ward.There are obvious differences for the divergence,vertical velocity felids,and vapour condition of high-and low-layers in more and less rain years.
【Fund】: 国家自然科学基金项目(40233037);; 973项目(2004CB418300)共同资助
【CateGory Index】: P434.5
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