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《Chinese Journal of Atmospheric Sciences》 2004-01
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Physical Causes of the 1999 and 2000 Summer Severe Drought in North China

Wei Jie, Zhang Qingyun, and Tao Shiyan(Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029)  
The persistent drought during the period 1999~2000 in North China is studied. The main results are as follows: The summer drought during 1999~2000 in North China are the consequence of persistent anomalous circulation over the Eurasia. The cause of 1999~2000 drought is the intensified Rossby wave over the Eurasia continent. Both diagnostic analysis and numerical experiments indicate that during the drought there is an important soil moisture feedback of the dry surface.
【Fund】: 中国科学院资源环境领域知识创新工程重要方向项目KZCX2 2 0 3;; 国家重点基础研究发展规划项目G1 9980 40 90 0资助
【CateGory Index】: P426.616
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