摘要
As the"Asian Water Tower"and the source of many major rivers in Asia,the Tibetan Plateau(TP)significantly affects human societies in densely-populated Asia[1].Lakes in the TP have a total area of^5×10^4 km^2 and hence they comprise an important component of the"Asian Water Tower".These lakes are sensitive to climate changes and have exhibited an overall trend of rapid expansion during recent decades[2].
As the"Asian Water Tower"and the source of many major rivers in Asia,the Tibetan Plateau(TP)significantly affects human societies in densely-populated Asia[1].Lakes in the TP have a total area of^5×10^4 km^2 and hence they comprise an important component of the"Asian Water Tower".These lakes are sensitive to climate changes and have exhibited an overall trend of rapid expansion during recent decades[2].
作者
Shuai Zhang
Jifeng Zhang
Hui Zhao
Xiangjun Liu
Fahu Chen
张帅;张继峰;赵晖;刘向军;陈发虎(Key Laboratory of Alpine Ecology,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China;University of Chinese Academy of Sciences,Beijing 100049,China;Key Laboratory of Desert and Desertification,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China;Center for Excellence in Tibetan Plateau Earth Sciences,Chinese Academy of Sciences,Beijing 100101,China;College of Geography and Environmental Science,Northwest Normal University,Lanzhou 730070,China2)
基金
the Strategic Priority Research Program of Chinese Academy of Sciences(XDA20090000)
the Second Tibetan Plateau Scientific Expedition and Research Program(2019QZKK0202,2019QZKK0601)。
