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评估气候驱动对喀喇昆仑冰川跃动的影响:一项地理空间分析,以2019 - 2022年希什佩尔冰川湖溃决洪水事件为例进行重点阐述

Assessing climate-driven impacts on Karakoram glacier surge: A geospatial analysis highlighting Shishper Glacial Lake outburst flood events (2019-2022) as prime example.

作者信息

Ali Mehtabidah

机构信息

Department of Earth and Atmospheric Sciences, Natural Sciences and Mathematics, University of Houston, Houston, TX, 77204, USA.

出版信息

Heliyon. 2024 Aug 8;10(16):e35951. doi: 10.1016/j.heliyon.2024.e35951. eCollection 2024 Aug 30.

Abstract

The Northern Areas of Pakistan encompass the Hindukush, Karakoram, and Himalayan mountain ranges witnessing glacier surging, exacerbated by climate warming. As glaciers rapidly melt, ravines experience heightened blockage and migration, obstructing stream discharges and forming expansive ice-dammed lakes. The rupture of these natural dams triggers Glacial Lake Outburst Floods downstream in the primary glacier's ravine. The catastrophic Glacial Lake Outburst Floods in 2022 across the Karakoram ranges in Northern Pakistan prompted this study. It focuses on Shishper Glacier Lake. The aim is to provide complete flood observations and their devastating effects on downstream communities. Analysis of Landsat 08 Imagery reveals the evolution of Shishper Glacier Lake from its initiation in November 2018 to the catastrophic GLOF in May 2022. The lake reached a maximum area of 0.32 km in 2019 and its successive breaches on June 22, 2019, and May 29, 2020, reduced it to 0.018 km. Draining continued until July 2021, shrinking the lake area to 0.009 km. A noteworthy 2.73 °C temperature increase in 2022 correlated with an expansion of the lake area to 0.33 km, culminating in the GLOF on May 7th, 2022. The study emphasizes the critical need for mapping, assessing, and monitoring surging glaciers and glacier-formed lakes in the Karakoram ranges to safeguard downstream communities from potential hazards.

摘要

巴基斯坦北部地区涵盖兴都库什山脉、喀喇昆仑山脉和喜马拉雅山脉,这些山脉正在经历冰川涌动,而气候变暖加剧了这一现象。随着冰川迅速融化,峡谷堵塞和迁移加剧,阻碍了溪流排放,并形成了大面积的冰坝湖。这些天然水坝的破裂引发了主要冰川峡谷下游的冰川湖溃决洪水。2022年巴基斯坦北部喀喇昆仑山脉发生的灾难性冰川湖溃决洪水促使了这项研究。它聚焦于希什佩尔冰川湖。目的是提供完整的洪水观测数据及其对下游社区的破坏性影响。对陆地卫星8号影像的分析揭示了希什佩尔冰川湖从2018年11月形成到2022年5月灾难性冰川湖溃决洪水的演变过程。该湖在2019年达到最大面积0.32平方千米,其在2019年6月22日和2020年5月29日的连续决口使其面积缩小至0.018平方千米。排水一直持续到2021年7月,湖泊面积缩小至0.009平方千米。2022年显著的2.73摄氏度升温与湖泊面积扩大到0.33平方千米相关,最终在2022年5月7日引发了冰川湖溃决洪水。该研究强调了对喀喇昆仑山脉中涌动的冰川和冰川形成的湖泊进行测绘、评估和监测的迫切需求,以保护下游社区免受潜在危害。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c29e/11369478/5324e7d59319/gr1.jpg

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