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《Plateau Meteorology》 1984-01
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Wang Qianqian Wang Anyu (Lanzhou Institute of Plateau Atmospheric Physics, Academia Sinica) Li Xuefeng Li Shuren ( Department of Geology and Geography, Lanzhou University )  
In order to investigate the effects of large-scale topography and heating sources and sinks induced by it on the mean general circulation in East Asia in summer, we use a 5-layer primitive equation numerical model developed originally by Kuo and Qian to make four kinds of experiments. The topography used in the model is close to the real one. The heating sources and sinks of the model are the stationary ones' computed by Yiao et al. with the actual data of July, 1979. The initial geopotential heights used in this investigation are taken from mean July zonal average. We have done 4 experiments of simulation.The first one ( designated by HN ) has no diabatic heating but orography included and the second ( by HH ) has both diabatic and orographic factors included. Because in summer the two most important heat sources are located at the Qinghai-Xizang Plateau and Bangladesh region, respectively,in East Asia, therefore based on the HH experiment we designed the third and the fourth experiments. The third (by PN ) has no heating in Plateau, while the fourth(by MN ) has no heating in Bangladesh region. In this paper a detailed comparison of the four experiments with one another is given.
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