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.
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.
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