冰川湖和溃决洪水的特征和变化

Guoqing Zhang, Jonathan L. Carrivick, Adam Emmer, Dan H. Shugar, Georg Veh, Xue Wang, Celeste Labedz, Martin Mergili, Nico Mölg, Matthias Huss, Simon Allen, Shin Sugiyama, Natalie Lützow
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引用次数: 0

摘要

全球冰川加速流失,形成了更多、更大的冰川湖。其中许多冰川湖是冰湖溃决洪水(GLOF)的源头,对人类和基础设施构成威胁。在本《综述》中,我们对全球冰川湖泊和冰湖溃决洪水的变化进行了综述。目前,全球有超过 11 万个冰川湖泊,总面积约为 1.5 万平方公里,从 1990 年到 2020 年,冰川湖泊面积增加了约 22%。超过 1,000 万人受到冰湖溃决的影响,这些影响通常与大坝溃决或与大规模运动相关的波浪倾覆有关。虽然数据有很大的局限性,但从 850 年到 2022 年,已记录的冰湖溃决事件超过 3000 起,尤其是在阿拉斯加(24%)、亚洲高山地区(HMA;18%)和冰岛(19%),其中大多数(64.8%)来自冰坝湖泊。在世界上大多数冰川覆盖的山区,记录在案的冰湖洪水都在增加,预计持续的冰川退化和湖泊扩张将进一步增加冰湖洪水的发生频率。据预测,到 2100 年,哈马河流域的冰湖洪水灾害将增加三倍,但鉴于地形对湖泊演变的限制,其他地区的变化可能较小。未来的研究应优先考虑获取有关湖泊和大坝特性的实地数据,绘制全球协调的多时空湖泊地图,并建立稳健高效的冰湖洪水模型,以进行全面的灾害评估和应对规划。气温升高会促进冰川湖的形成,冰川湖溃决洪水(GLOF)会突然爆发,造成灾难性后果,威胁下游生命和基础设施。本综述概述了冰川湖和冰湖溃决洪水的观测和预测变化,报告指出,随着冰川的不断退化,冰川湖和冰湖溃决洪水都将增加。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Characteristics and changes of glacial lakes and outburst floods

Characteristics and changes of glacial lakes and outburst floods

Characteristics and changes of glacial lakes and outburst floods
Global glacier mass loss has accelerated, producing more and larger glacial lakes. Many of these glacial lakes are a source of glacial lake outburst floods (GLOFs), which pose threats to people and infrastructure. In this Review, we synthesize global changes in glacial lakes and GLOFs. More than 110,000 glacial lakes currently exist, covering a total area of ~15,000 km2, having increased in area by ~22% dec–1 from 1990 to 2020. More than 10 million people are exposed to the impacts of GLOFs, commonly associated with dam failure or wave overtopping associated with mass movements. Although data limitations are substantial, more than 3,000 GLOFs have been recorded from 850 to 2022, particularly in Alaska (24%), High Mountain Asia (HMA; 18%) and Iceland (19%), the majority (64.8%) being from ice-dammed lakes. Recorded GLOFs have increased in most glaciated mountain regions of the world, with ongoing deglaciation and lake expansion expected to increase GLOF frequency further. In HMA, GLOF hazards are projected to triple by 2100, but changes in other regions will likely be lower given topographic constraints on lake evolution. Future research should prioritize acquiring field data on lake and dam properties, producing globally coordinated multi-temporal lake mapping, and robust and efficient modelling of GLOFs for comprehensive hazard assessment and response planning. Warmer temperatures enhance formation of glacial lakes that can suddenly and catastrophically release as a glacial lake outburst flood (GLOF), threatening downstream lives and infrastructure. This Review outlines observed and projected changes in glacial lakes and GLOFs, reporting that both will increase with ongoing deglaciation.
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