正常的季风类型按时到达，带来了达到历史记录的雨量，这些降水从受灾严重的西北部地区流入印度和流域。
That more normal monsoon pattern arrived just in time to catch the record volumes of rainwater streaming down the Indus river system from the heavily hit northwest.
2010年夏季强烈的季风降水导致印度河一座大坝的崩溃，随即裂成两段。
Severe monsoon rains in the summer of 2010 led to a dam failure on the Indus River, which subsequently split in two.
汉源地区的降水主要受控于太阳辐射影响下的印度季风强度的变化。
The precipitation in Hanyuan was mainly controlled by the change of the Indian monsoon intensity under the influence of solar radiation.
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