气候变暖加剧全球冰川失稳灾害过程

作     者：张太刚 王伟财 申子恒 安宝晟 Taigang Zhang;Weicai Wang;Ziheng Shen;Baosheng An

作者机构：State Key Laboratory of Tibetan Plateau Earth SystemEnvironment and ResourcesInstitute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing 100101China College of Earth and Environmental SciencesLanzhou UniversityLanzhou 730000China Center for the Pan-Third Pole EnvironmentLanzhou UniversityLanzhou 730000China School of ScienceTibet UniversityLhasa 850011China 

出 版 物：《Science Bulletin》 (科学通报（英文版）)

年 卷 期：2024年第69卷第1期

页      面：30-33页

核心收录：

学科分类：07[理学] 070601[理学-气象学] 0705[理学-地理学] 0706[理学-大气科学] 070501[理学-自然地理学] 

基　　金：the Second Tibetan Plateau Scientific Expedition and Research Program(STEP)(2019QZKK0208) International Partnership Program of the Chinese Academy of Sciences(131C11KYSB20200029) Lhasa Earth System MultiDimension Observatory Network(LEMON) 

主　　题：rock glacier floods 

摘      要：Glacier-related slope failures,including ice avalanches,ice-rock avalanches,glacier collapses,and rock avalanches on glaciers,are generally characterized by large collapse volumes,solid-liquid phase transition,and high mobility[1].They are one of the major types of geo-hazards in high mountain ***-related slope failures have cascading effects since they often evolve into glacial lake outburst floods(GLOFs),debris flows,and dammed lakes,which significantly prolong and amplify the impacts of the *** slope failures have cumulatively claimed more than tens of thousands of *** example,the 1962 and 1970 Huascaran events in the Peruvian Andes caused approximately 20,000 deaths[2],and the 2021 Chamoli ice-rock avalanche in the Indian Himalayas left more than 200 people dead or missing[3].