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

Science Bulletin 2024年第18期69卷 2829-2832页

作者： Yanbin Lei Jing Zhou Tandong Yao broxton w.bird Yifan Yu Shujin wang Kun Yang Yinsheng Zhang Jianqing Zhai Yufeng Dai State Key Laboratory of Tibetan Plateau Earth System Environment and ResourcesInstitute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing 100101China Department of Earth Sciences Indiana University-Purdue University Indianapolis(IUPUI)Indianapolis IN 46202USA College of Resources and Environment University of Chinese Academy of SciencesBeijing 100049China Ministry of Education Key Laboratory for Earth System Modeling Department of Earth System ScienceTsinghua UniversityBeijing 100084China National Climate Center China Meteorological AdministrationBeijing 100081China

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 *** 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

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西藏最大内陆湖泊(色林错)溃决及其环境影响（英文）

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Science Bulletin 2024年第18期 2829-2832页

作者：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 State Key Laboratory of Tibetan Plateau Earth System Environment and ResourcesInstitute of Tibetan Plateau ResearchChinese Academy of Sciences Department of Earth Sciences Indiana University-Purdue University Indianapolis (IUPUI) College of Resources and Environment University of Chinese Academy of Sciences Ministry of Education Key Laboratory for Earth System Modeling Department of Earth System ScienceTsinghua University National Climate Center China Meteorological Administration

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.

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