对黄河河源区多年平均和雨季降水量、年际径流量进行分析。

The annual average and rain season precipitation and yearly runoff of the source regions of the Yellow River were analyzed.

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[张杰，李栋梁，何金梅，等。地形对青藏高原丰枯水年雨季降水量空间分布的影响[J]。水科学进展，2007，18（3）：319-326。]。

Zhang Jie, Li Dong1iang, He Jin, et al. Influence of terrain onprecipitation distribution in Qingzang tableland in wet and dryyears[J]. Advances in Water Science, 2007,18(3):319-326.

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比如说，自1951年到2000年，印度雨季的强降水发生频率升高，强度增大，而温和的降水次数有所减少。

For example, from 1951 to 2000, heavy monsoons in India became more frequent and intense, while more moderate rains happened less often.

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