青藏高原(以下简称高原)积雪具有明显的季节、年际和年代际变化特征，是影响亚洲夏季风降水的重要因子之一。
The snow cover on the Tibetan Plateau has obvious seasonal, interannual and interdecadal changes, and is one of the most important factors which control the Asian summer monsoon precipitation.
ENSO事件对亚洲季风有很大影响，特别是对东亚夏季风环流有较大影响。
ENSO event has a large influence on Asian monsoon, particularly on the East Asian monsoon.
结果发现，中纬度高原的感热加热所造成的经、纬向热力差异是导致亚洲夏季风爆发的原因。
Results show that the longitudinal and latitudinal thermal contrasts caused by the middle latitude Plateau sensible heating trigger the onset of the Asian summer monsoon.
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