The Two Main Mechanisms of Glacier Lake Outburst Flood in Tibet,China  

作　　者：LIU Jing-jing TANG Chuan CHENG Zun-lan 

机构地区：[1]Key Laboratory of Mountain Hazards and Surface Process,Institute of Mountain Hazards and Environment,Chinese Academy of Sciences [2]State Key Laboratory of Geohazard Preventions [3]Graduate School of Chinese Academy of Sciences

出　　处：《Journal of Mountain Science》2013年第2期239-248,共10页山地科学学报（英文）

基　　金：supported by the National Natural Science Foundation of China (Grant No.41201010);the Technology Project of the Ministry of Transport(Grant No.201231879210);the Directional Projectof IMHE (No.SDS-135-1202-02);Opening Fund of State Key Laboratory of Geohazard Prevention and Geoenvironment Protection (Grant No.SKLGP2010K003);Open Research Fund of State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin,China Institute of Water Resources and Hydropower Research (Grant NO.IWHR-SKL-201209)

摘　　要：With the global warming,the disasters of Glacier Lake Outburst Flood(GLOF) have taken place frequently in Tibet in recent years and attracted more and more attention.A systematic survey was conducted on the 19 GLOFs in Tibet to study their two main mechanisms.Investigations indicated that all the events occurred in end-moraine lakes,and the outburst occurred partially and instantly.And the breach had the shape of an arc or a trapezoid in overflow outburst and its top width was 3-5 times more than the height.The two main mechanisms of GLOFs in Tibetan end-moraine Lake were overflow and piping,and the overflow mechanism caused by iceberg collapse was dominated in most cases.A formula was proposed to calculate the critical thickness of iceberg tongue that determines the collapse.Granular analysis of the moraine materials revealed that seepage deformation is crucial in the outburst process.Finally,we conducted a case study of the Guangxiecuo Lake to show its possible process of outburst and estimated the peak discharge of the resulted flood.

关 键 词：Glacier Lake Outburst Flood End-moraine Lake Outburst mechanism OVERFLOW Piping TIBET 

分 类 号：TV122.4[水利工程—水文学及水资源] TV697.21