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A robust but variable lake expansion on the Tibetan Plateau

查看全文 作  者:Guoqing [1,2]Zhang;Wei [1,4]Luo;Wenfeng [1,4]Chen;Guoxiong [3,4]Zheng 高影响力作者 机构地区:[1]Key Laboratory of Tibetan Environmental Changes and Land Surface Processes.Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China;[2]Center for Excellence in Tibetan Plateau Earth Sciences,Chinese Academy of Sciences,Beijing 100101,China;[3]Xinjiang Institute of Ecology and Geography,Chinese Academy of Sciences,Urumqi 830011,China;[4]University of Chinese Academy of Sciences,Beijing 100049,China高影响力机构 出  处:《Science Bulletin》索引2019年第64卷第18期,共4页高影响力期刊 基  金:supported by the National Key R&D Program of China (2018YFB0505005);the National Natural Science Foundation of China (41871056, 21661132003, and 41571068);the Strategic Priority Research Program (A) of the Chinese Academy of Sciences (XDA20060201) 摘  要:Lakes on the Tibetan Plateau(TP)are an indicator and sentinel of climatic changes[1].We extended lake area changes on the TP from 2010[2]to 2018,and provided a long and dense lake observations between the 1970s and 2018.We found that the number of lakes,with area larger than 1 km2,has in creased to?1,400 in 2018 from?1,000 in the 1970s.The total area of these lakes decreased between the 1970s and?1995,and then showed a robust increase,with the exception of a slight decrease in 2015.This expansion of the lakes on the highest plateau in rhe world is a response to a hydrological cycle intensified by recent climate changes[3]. 关 键 词:PLATEAU TIBETAN intensified
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