TY - JOUR
T1 - Small outbursts into big disasters
T2 - Earthquakes exacerbate climate-driven cascade processes of the glacial lakes failure in the Himalayas
AU - Chen, Ningsheng
AU - Liu, Mei
AU - Allen, Simon
AU - Deng, Mingfeng
AU - Khanal, Narendra Raj
AU - Peng, Taixin
AU - Tian, Shufeng
AU - Huggel, Christian
AU - Wu, Kanglin
AU - Rahman, Mahfuzur
AU - Somos-Valenzuela, Marcelo
N1 - Publisher Copyright:
© 2022 Elsevier B.V.
PY - 2023/2/1
Y1 - 2023/2/1
N2 - 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.
AB - 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.
KW - Big disasters
KW - Cascade Processes
KW - GLOFs
KW - Numerical modeling
KW - Resilient
UR - http://www.scopus.com/inward/record.url?scp=85143771112&partnerID=8YFLogxK
U2 - 10.1016/j.geomorph.2022.108539
DO - 10.1016/j.geomorph.2022.108539
M3 - Article
AN - SCOPUS:85143771112
SN - 0169-555X
VL - 422
JO - Geomorphology
JF - Geomorphology
M1 - 108539
ER -