Overflow of Siling Co on the central Tibetan Plateau and its environmental impacts  

西藏最大内陆湖泊(色林错)溃决及其环境影响

作　　者：Yanbin Lei Jing Zhou Tandong Yao Broxton W.Bird Yifan Yu Shujin Wang Kun Yang Yinsheng Zhang Jianqing Zhai Yufeng Dai 类延斌;周璟;姚檀栋;Broxton W.Bird;于伊凡;王淑巾;阳坤;张寅生;翟建青;戴玉凤

机构地区：[1]State Key Laboratory of Tibetan Plateau Earth System,Environment and Resources,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China [2]Department of Earth Sciences,Indiana University-Purdue University Indianapolis(IUPUI),Indianapolis IN 46202,USA [3]College of Resources and Environment,University of Chinese Academy of Sciences,Beijing 100049,China [4]Ministry of Education Key Laboratory for Earth System Modeling,Department of Earth System Science,Tsinghua University,Beijing 100084,China [5]National Climate Center,China Meteorological Administration,Beijing 100081,China

出　　处：《Science Bulletin》2024年第18期2829-2832,共4页科学通报（英文版）

基　　金：supported by the Second Tibetan Plateau Scientific Expedition and Research Program(2019QZKK0201);National Natural Science Foundation of China(41988101,41971097,and U2202208)。

摘　　要：The Tibetan Plateau(TP)and its surroundings are also referred to as“Asian Water Tower”,which is the headwater of ten major rivers in Asia and provides ecosystem service for nearly two billion people[1].The interior TP boasts the greatest concentration of high-latitude inland lakes in the world,providing essential water resources,regulating regional climate and maintaining ecological balance.Over the past 50 years,the TP has experienced rapid climate warming and overall wetting,which has led to glacier mass loss,thawing of permafrost,reduction in snow cover,and shortening of lake ice duration[1].Changes in lake water storage provide a means of assessing the regional hydrological response to recent climate change in this sparsely populated region.

关 键 词：TIBETAN GLACIER INLAND 

分 类 号：TV122.4[水利工程—水文学及水资源]