Earth SciencesCommunications Earth & Environment
Late Ming Dynasty weak monsoon induced a harmonized megadrought across north-to-south China
W. Yue, F. Chen, et al.
This research delves into the historical water balance changes in the middle Yangtze River over 464 years, unveiling a significant megadrought occurring between 1625 and 1644 CE that profoundly affected the Ming Dynasty. The study connects this phenomenon to Pacific sea surface temperature anomalies and other climatic factors. Discover how this work by Weipeng Yue, Feng Chen, Max C. A. Torbenson, Xiaoen Zhao, Yonghong Zheng, Yang Xu, Mao Hu, Shijie Wang, Tiyuan Hou, Heli Zhang, and Youping Chen sheds light on mitigating future droughts.
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