Disaster effects of climate change in High Mountain Asia: State of art and scientific challenges

• Published in: Advances in Climate Change Research
• Main Authors: Wang, Hao, Wang, Bin-Bin, Cui, Peng, Ma, Yao-Ming, Wang, Yan, Hao, Jian-Sheng, Wang, Yu, Li, Ya-Mei, Sun, Li-Jun, Wang, Jiao, Zhang, Guo-Tao, Li, Wei-Mo, Lei, Yu, Zhao, Wen-Qing, Tang, Jin-Bo, Li, Chao-Yue
• Format: Report
• Language: English
• Published: KEAI PUBLISHING LTD 2024
• Subjects: High Mountain Asia; Climate change; Cryosphere degradation; Nature hazards; Disaster risk; LAKE OUTBURST FLOODS; TIBETAN PLATEAU; DEBRIS FLOWS; GLACIER MASS; PRECIPITATION EXTREMES; TIANSHAN MOUNTAINS; HENGDUAN MOUNTAINS; QILIAN MOUNTAINS; LARGE LANDSLIDES; SLOPE FAILURES; Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences; Environmental Sciences; Ice; permafrost; Thermokarst
• Online Access: http://ir.imde.ac.cn/handle/131551/58224; https://doi.org/10.1016/j.accre.2024.06.003

High Mountain Asia (HMA) shows a remarkable warming tendency and divergent trend of regional precipitation with enhanced meteorological extremes. The rapid thawing of the HMA cryosphere may alter the magnitude and frequency of nature hazards. We reviewed the influence of climate change on various types of nature hazards in HMA region, including their phenomena, mechanisms and impacts. It reveals that: 1) the occurrences of extreme rainfall, heavy snowfall, and drifting snow hazards are escalating; accelerated ice and snow melting have advanced the onset and increased the magnitude of snowmelt floods; 2) due to elevating trigger factors, such as glacier debuttressing and the rapid shift of thermal and hydrological regime of bedrock/snow/ice interface or subsurface, the mass flow hazards including bedrock landslide, snow avalanche, ice-rock avalanches or glacier detachment, and debris flow will become more severe; 3) increased active-layer detachment and retrogressive thaw slumps slope failures, thaw settlement and thermokarst lake will damage many important engineering structures and infrastructure in permafrost region; 4) multi-hazards cascading hazard in HMA, such as the glacial lake outburst flood (GLOF) and avalanche-induced mass flow may greatly enlarge the destructive power of the primary hazard by amplifying its volume, mobility, and impact force; and 5) enhanced slope instability and sediment supply in the highland areas could impose remote catastrophic impacts upon lowland regions, and threat hydropower security and future water shortage. In future, ongoing thawing of HMA will profoundly weaken the multiple-phase material of bedrock, ice, water, and soil, and enhance activities of nature hazards. Compounding and cascading hazards of high magnitude will prevail in HMA. As the glacier runoff overpasses the peak water, low flow or droughts in lowland areas downstream of glacierized mountain regions will became more frequent and severe. Addressing escalating hazards in the HMA region requires tackling ...