Title: Numerical Experiment of the Influence of Tibetan Plateau on the North Edge of Asian Summer Monsoon
Abstract: Using the spectral atmospheric circulation model SAMIL(R42L9) developed by LASG/IAP,the effects on north edge of Asian summer monsoon with or without the Tibetan Plateau are simulated.The results show that the existence of the large topography resulted by the Tibetan Plateau has important impacts on the activities of Asian summer monsoon.With(without) the Tibetan Plateau,the northward wind on the east side of the Tibetan Plateau is comparatively strong(weak),which is(isn't) in favor of steering and strengthening the northward of Asian summer monsoon and thus makes on the north edge side of summer monsoon more northward(southward).At the same time,with(without) the Tibetan Plateau,the west Pacific High is northward and westward(southward and eastward),which is also beneficial for the summer monsoon′s northward movement to the Chinese mainland and thus also helpful to the more northward(southward) for the north edge side and the corresponding rainfall areas of summer monsoon.
Publication Year: 2007
Publication Date: 2007-01-01
Language: en
Type: article
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Cited By Count: 3
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