Process, mechanisms, and early warning of glacier collapse-induced river blocking disasters in the Yarlung Tsangpo Grand Canyon, southeastern Tibetan Plateau

冰川 地质学 冰斗冰川 冰川物质平衡 碎片 高原(数学) 峡谷 大洪水 潮水冰川循环 冰川形态 气候变化 全球变暖 背景(考古学) 流域 自然地理学 气候学 地貌学 冰流 海洋学 地理 冰层 冰崩解 数学 怀孕 哺乳期 遗传学 考古 古生物学 海冰 数学分析 地图学 生物
作者
Baosheng An,Weicai Wang,Wei Yang,Guangjian Wu,Yanhong Guo,Haifeng Zhu,Yang Gao,Ling Bai,Fan Zhang,Chen Zeng,Lei Wang,Jing Zhou,Xin Li,Jia Li,Zhijun Zhao,Yingying Chen,Jingshi Liu,Jiule Li,Zhongyan Wang,Wenfeng Chen,Tandong Yao
出处
期刊:Science of The Total Environment [Elsevier]
卷期号:816: 151652-151652 被引量:37
标识
DOI:10.1016/j.scitotenv.2021.151652
摘要

Glacier collapse is a fairly new type of glacier-related disasters on the Asian Water Towers (AWTs) in the warming climate. On 16 October and 29 October 2018, two glacier collapses occurred in the Sedongpu Basin, 7 km downstream from Gyala Village, Paizhen Town, Miling County, on the Yarlung Tsangpo River (YTR). The ice and entrained debris flows caused by the glacier collapses blocked the YTR, resulting in a potential threat to residents and transport lines upstream and downstream. Through post-event field investigations with a helicopter and an unmanned aerial vehicle (UAV), remote sensing interpretation, and seismic, hydrological, and meteorological observations, the process and potential mechanisms of the glacier collapse-induced river blocking (GCRB) disasters were investigated. We confirmed that the first glacier collapse event occurred at 22:48 (Beijing time) on 16 October 2018 and the second began at 08:03 on 29 October 2018. Approximately 130 × 106 m3 of ice and debris detached from the glacier during the glacier collapse, and we calculated that the river blocking fans caused by the first and second glacier collapse event covered ~1.36 km2 and ~ 1.29 km2 on the main watercourse of the YTR, respectively. We determined that the GCRB incidents represent a disaster chain of glacier collapse → glacial debris flow → river blockage → dammed lake → outburst flood. These incidents arise due to a combination of factors, including glacier activity, climate warming, heavy precipitation, pre-seismic activity, and high topographic relief. In the context of climate warming on the Tibetan Plateau, such glacier collapse induced disaster chains will continue or even intensify in the future. To protect against glacier collapse disasters in the Grand Canyon on the YTR, we established a monitoring and early warning system (EWS), which has already successfully sounded alerts for GCRB incidents. As a major element of an integrated risk management strategy, the EWS represents a viable and promising tool for mitigating climate change-related risks.
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