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.
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.
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.
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.
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