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Comparison analysis of the summer monsoon precipitation between northern and southern slopes of Tanggula Mountains, Qinghai-Xizang (Tibetan) Plateau: a case study in summer 1998

机译:青藏高原唐古拉山南北坡夏季季风降水的对比分析:以1998年夏季为例

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摘要

Based on the precipitation data obtained through GEWEX Asian Monsoon Experiment-Tibet fieldwork from May to September 1998, this study investigated the features of the summer monsoon precipitation on the northern and southern slopes of the huge Tanggula Mountains in the Qinghai-Xizang (Tibetan) Plateau. The results show that the precipitation on the southern slope is about 50% higher than on the northern slope, whereas the frequency and diurnal pattern of the precipitation are very similar. The mean precipitation intensity on the southern slope is larger than on the northern slope. In most cases, the daily precipitation showed similar variation on both slopes, demonstrating that the precipitation processes might be similar. In the summer monsoon period, the local convective precipitation contributed to the total precipitation on both slopes and such a contribution on the southern slope is larger.
机译:根据1998年5月至9月通过GEWEX亚洲季风试验-西藏实地考察获得的降水数据,本研究调查了青藏高原大唐古拉山北坡和南坡的夏季风降水特征。 。结果表明,南坡的降水量比北坡的降水量高约50%,而降水的频率和昼夜模式却非常相似。南坡的平均降水强度大于北坡。在大多数情况下,两个坡度的日降水量显示相似的变化,表明降水过程可能相似。在夏季风季期间,局部对流降水对两个坡度的总降水量都有贡献,而对南坡的这种贡献较大。

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