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Xingwen Jiang, Jianchuan Shu, Xin Wang, Xiaomei Huang, and Qing Wu

1. Introduction Southwest China (SWC), characterized by complex topography, receives considerable rainfall during summer. It contains the headwaters of many rivers, including the Yangtze, Langcang, and Nujiang, which provide as much as 46% of China’s available water resources. Because of large interannual variability of summer rainfall over SWC, droughts and floods hit SWC frequently, especially over the last decade, resulting in severe economic losses ( Wang et al. 2015a ). It is, therefore

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