More Catastrophic Flow Events may Follow the Chamoli Rock and Ice Avalanche under Climate Change  

作　　者：Haijun Qiu Ya Liu Bingzhe Tang Ninglian Wang Jiading Wang 

机构地区：[1]Shaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity,College of Urban and Environmental Sciences,Northwest University,Xi’an 710127,China [2]Institute of Earth Surface System and Hazards,Northwest University,Xi’an 710127,China [3]State Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi’an 710069,China

出　　处：《Journal of Earth Science》2024年第4期1382-1384,共3页地球科学学刊（英文版）

基　　金：funded by the National Natural Science Foundation of China(No.42271078);Key Research and Development Program of Shaanxi(No.2024SF-YBXM-669).

摘　　要：0 INTRODUCTION Global warming not only exacerbates the instability of the climate system,causing more weather extremes but also has far-reaching impacts on surface systems,changing disaster environments(Qiu et al.,2024;Ye et al.,2024).The key medium between climate warming and the mountain environment is the cryosphere,whose recession increases the occurrence of chain disasters such as rock-ice avalanches and other flow events(Yang et al.,2023).

关 键 词：WARMING DISASTER climate 

分 类 号：P467[天文地球—大气科学及气象学] P426.636