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《Progress in Geophysics》 2012-06
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Numerical simulation of the influence of Tibetan Plateau on east asian monsoon

ZHANG Chen1,HAN Jia-rui2,LI Cong3,WANG Zi-qian4 (1.Ocean University of China,Qingdao 266100,China;2.The Centre of Strategy and Development,Beijing 100081,China; 3.Nanjing Meteorological Bureau,Nanjing 210009,China;4.LASG,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China)  
hrough simply changing terrain of the Tibetan Plateau and integrating for 15 years in CAM model,this study compares and analyzes the impact of the plateau on the East Asian monsoon in the month and pentad scale.The results show that: the uplift of Tibetan Plateau enhances northerly winds and rainfall in south China and Changjing river area before tropical monsoon.Through heating upper atmosphere significantly,the thermal difference between land and sea is strengthened,which makes the east Asian monsoon stronger.With the sourthwest wind transporting moisture to Changjiang and Jiang-huai river area,rainy seasons are earlier and last longer,which cause sub-tropical high farther western and change the distribution of monsoon rainfall.The results also show that: since July,there are less rainfall along coastal areas over north China in Tibetan experiment.Meanwhile,since there are less latent heat and more southerly air flow,the position of 337.5 °K pseudo-equivalent temperature line changes little.
【Fund】: 国家自然科学基金项目(40775069)资助
【CateGory Index】: P461
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