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《Plateau Meteorology》 2008-02
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Numerical Simulation of the Impact of Abnormity of Sensible Heat Flux in Northwest Arid Zone on Precipitation in China

GAO Rong1,DONG Wen-jie1,WEI Zhi-gang2 (1.Laboratory for Climate Research,National Climate Center,China Meteorological Administration,Beijing 100081,China;2.Laboratory for Climate Environment and Disasters of Western China,Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou 730000,China)  
The impact of abnormity of sensible heat flux from surface to atmosphere in spring and summer in Northwest arid zone on precipitation in China in summer has been simulated by using RegCM3 model of the up to date edition,the results showed that,after the sensible heat in Northwest arid zone has been increased,the temperature in low layer will rise,and the air density will decrease so that there has an anomaly of ascending motion in Northwest arid zone.The sinking motion is weaken in Northwest arid zone,which will lead to more precipitation in Xinjiang.The weak sinking motion in Northwest arid zone make that there has a stronger air pressure in high layer,so there has a anomaly of anticyclonic circulation,which leads to the weaken ascending motion and the precipitation decreases in Tibetan Plateau.And then it makes a center of anomaly of low air pressure in the mid-and low-reaches of Yangtze River and the north of Northeast China,so that there have anomaly of anticyclonic circulation and more precipitation.However,The precipitation is less in South China,Southwest China,southern of North China and Northeast China.
【Fund】: 国家自然科学面上基金项目(40705031 40375033);; 国家重点基础研究发展计划项目(2007CB411505)共同资助
【CateGory Index】: P426.6
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