Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; School of Science, Tibet University, Lhasa 850011, China.
Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China.
Sci Total Environ. 2022 Apr 10;816:151652. doi: 10.1016/j.scitotenv.2021.151652. Epub 2021 Nov 13.
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 × 10 m 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 km and ~ 1.29 km 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.
冰川崩塌是亚洲水塔(AWTs)在变暖气候下一种相当新的冰川相关灾害。2018 年 10 月 16 日和 29 日,两次冰川崩塌分别发生在雅鲁藏布江(YTR)加勒村下游 7 公里处的 Sedongpu 盆地。冰川崩塌产生的冰和夹带的碎屑流阻塞了 YTR,对上下游的居民和运输线路构成潜在威胁。通过直升机和无人机(UAV)进行的事后实地调查、遥感解释以及地震、水文和气象观测,研究了冰川崩塌引发的河道堵塞(GCRB)灾害的过程和潜在机制。我们确认第一次冰川崩塌事件发生在 2018 年 10 月 16 日 22:48(北京时间),第二次发生在 29 日 08:03。大约 130×10m 的冰和碎片在冰川崩塌过程中脱离冰川,我们计算出第一次和第二次冰川崩塌事件产生的河道堵塞扇分别覆盖了约 1.36km 和 1.29km 的 YTR 主水道。我们确定 GCRB 事件代表了冰川崩塌→冰川泥石流→河道堵塞→堰塞湖→溃决洪水的灾害链。这些事件是由多种因素共同作用引起的,包括冰川活动、气候变暖、强降水、震前活动和高地形抬升。在青藏高原气候变暖的背景下,未来这种冰川崩塌诱发的灾害链将继续甚至加剧。为了防范雅鲁藏布大峡谷的冰川崩塌灾害,我们建立了一个监测和预警系统(EWS),该系统已经成功地对 GCRB 事件发出了警报。作为综合风险管理策略的一个重要组成部分,EWS 是一种可行且有前途的减轻气候变化相关风险的工具。