由对数值模拟与试验的结果分析得出：（1）青藏高原地形有利于高原东麓暴雨区的扩大与强度加大。
Some results are obtained as follows: (1) The heavy rain area is expanded and heavy rain is enhanced by plateau terrain in the east of plateau.
利用GCM（大气环流模式）完成的一系列改变青藏高原地形高度的数值试验说明，东亚季风气候变化非常敏感地响应于高原隆升。
Simulations of climate variables from General Circulation Models(GCMs)usually contain large deviation due to the low resolution, which makes it difficult for regional studies.
利用GCM（大气环流模式）完成的一系列改变青藏高原地形高度的数值试验说明，东亚季风气候变化非常敏感地响应于高原隆升。
Simulations of climate variables from General Circulation Models(GCMs)usually contain large deviation due to the low resolution, which makes it difficult for regional studies.
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