Abstract
Risk assessments for potential glacial lake outburst floods (GLOFs) are primarily focused on large, rapidly expanding lakes. However, the mechanism of cascading hazards that cause small outbursts to transition into big disasters is poorly understood. We investigated the Gongbatongshaco GLOF in the Himalayas, to reveal a novel disaster model and mechanism, considering increasing regional temperature, glacial lake area, and glacial retreat. Global warming drives glacial retreat, and uncover loose sediment that can be mobilized as debris flows, triggering small glacial lake outbursts in high mountain regions. Sediment generated from earthquake-induced landslides exacerbates the flow magnitude in a valley to increase the disaster risk. Concentrations of inhabitants located in these areas are subject to socioeconomic vulnerability, leading to post-disaster poverty within these communities. A reasonable GLOFs resilient mitigation framework is proposed. The results offer new insights into risk assessment, especially for small glacial lakes in tectonically-active high mountain environments influenced by climate change and earthquake activity.
| Original language | English |
|---|---|
| Article number | 108539 |
| Journal | Geomorphology |
| Volume | 422 |
| DOIs | |
| State | Published - 1 Feb 2023 |
| Externally published | Yes |
Bibliographical note
Publisher Copyright:© 2022 Elsevier B.V.
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 1 No Poverty
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SDG 11 Sustainable Cities and Communities
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SDG 13 Climate Action
Keywords
- Big disasters
- Cascade Processes
- GLOFs
- Numerical modeling
- Resilient
ASJC Scopus subject areas
- Earth-Surface Processes
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