4.7 Article

Moraine-dammed glacial lakes and threat of glacial debris flows in South-East Kazakhstan

Journal

EARTH-SCIENCE REVIEWS
Volume 229, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.earscirev.2022.103999

Keywords

Debris flow; Glacial hazard; Glacial lake outburst flood; Hazard mitigation; Moraine-dammed glacial lakes; South-East Kazakhstan

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This study focuses on the formation of MGLs and the characteristics of lake outburst floods and debris flows in the Kazakh part of Tien Shan. The number of MGLs has increased since the 1970s, with 40 identified as dangerous. Outburst events mainly occurred between the end of June and the end of August, typically caused by ruptures in ice-cored moraine dams.
Glacier retreat has caused the emergence of numerous moraine-dammed glacial lakes (MGL) over the last century which have become research foci in many mountain regions of the world. Outbursts of MGLs have caused destructive floods and debris flows, leading to numerous human casualties and significant material damage. The mountains of South-Eastern Kazakhstan have also become prone to lake outburst floods and related debris flows, specifically in the second half of the 20th century. This paper presents and reviews existing surveys and knowledge along with results of own investigations on the formation of MGLs and the characteristics of lake outburst floods and debris flows in the Kazakh part of Tien Shan. We suggest a workflow to identify the most dangerous types of lakes and provide information about their morphogenetic features and hazard criteria.The number of MGLs increased since the 1970s with more than 160 existing in 2018. Forty were identified as being dangerous. Forty-eight lake outbursts occurred since 1950 with all the documented events happened between end of June and end of August. The most dangerous outbursts were caused by ruptures in ice-cored moraine dams. Outbursts of nine MGLs caused disastrous debris flows, with some occurring repeatedly. The number of outbursts decreased since the year 2000 compared to 1970-2000. However, due to ongoing glacier retreat new lakes are forming at higher altitudes. Their greater potential energy makes possible future outbursts more dangerous. Re-evaluation of existing methods to calculate the water volume and peak discharge based on bathymetric measurements and observed outbursts revealed that the applied equations provide suitable approximations and allow supporting mitigation and prevention measures. Finally, the presentation of implemented measures to lower the water level using siphons or artificial flow channels shows that they can reduce the lake outburst hazards. However, they are associated with risks and financial costs and it needs to be carefully considered whether protection measures of the endangered areas are more cost effective.

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