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.
从降水的谱结构上来看，南海季风和印度季风有比较大的差异。
There is a large distinction in the spectrum structure of the precipitation between the SCS monsoon and the Indian monsoon.
珠穆朗玛峰东侧东绒布冰川积累区的降水主要是由印度夏季风环流带来的。
The precipitation in the accumulation zone of the East Rongbuk Glacier on the east slope of the Mount Qomolangma is mostly brought on by Indian summer monsoon.
进一步通过遥相关和水汽输送揭示了北印度夏季风强弱与中国河套盛夏降水的联系途径。
To further reveal the relevant mechanism of the NISM on the rainfall of Hetao, we discuss the relation from two aspects of teleconnection and water vapor transport.
高原夏季风强(弱)时，印度全区及我国华北地区容易出现降水偏少(多)。
When the TPSM is strong (weak), the precipitation in all India and North China tends to be less (more) than normal.
通过进一步的诊断，揭示了亚洲夏季风降水在印度季风区出现较晚以及印度夏季风爆发的动力机制。
Further dynamic analysis reveals the dynamic mechanism for the late occurrence of ASM precipitation in Indian monsoon area and the abrupt occurrence of Indian summer monsoon onset.
利用华北和印度夏季降水资料，采用趋势分析、小波变换等方法，对两地区夏季风降水进行了对比分析。
Based on summer precipitation data, by using trend analysis, wavelet transform methods, the changes of summer rainfall in North China and in India were analyzed.
利用华北和印度夏季降水资料，采用趋势分析、小波变换等方法，对两地区夏季风降水进行了对比分析。
Based on summer precipitation data, by using trend analysis, wavelet transform methods, the changes of summer rainfall in North China and in India were analyzed.
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