Debris flow induced by glacial lake break in southeast Tibet

doi:10.2495/DEB100091

CORC > 成都山地灾害与环境研究所 > 中国科学院水利部成都山地灾害与环境研究所 > 山地灾害与地表过程重点实验室

	Debris flow induced by glacial lake break in southeast Tibet
	Cheng Z. L.2,3; Liu J. J.1,2,3; Liu J. K.1,2,3
	2010
会议日期	2010
会议地点	Milano
关键词	debris flow induced by glacier-lake break climate change disaster southeast Tibet
DOI	10.2495/DEB100091
页码	101-111
国家	ITALY
英文摘要	Debris flow caused by flooding of a glacier-lake break can result in major disasters in southeast Tibet. Based on field investigation and data analysis, this paper discusses the influences of climate factors on lake break. It is found that the break is inclined to occur after abnormal changes in climate, particularly at the turn from cold-wet weather to hot-dry weather. Debris flows due to glaciers will be more active in future decades.
源文献作者	DeWrachien, D ; Brebbia, CA
产权排序	1
会议录	MONTORING, SIMULATION, PREVENTION AND REMEDIATION OF DENSE DEBRIS FLOWS III
语种	英语
ISSN号	1746-4471
ISBN号	978-1-84564-442-0
WOS记录号	WOS:000394394900009
内容类型	会议论文
源URL	[http://ir.imde.ac.cn/handle/131551/34183]
专题	成都山地灾害与环境研究所_山地灾害与地表过程重点实验室
通讯作者	Cheng Z. L.
作者单位	1.Graduate University of Chinese Academy of Sciences, China 2.Institute of Mountain Hazards and Environment, CAS, China; 3.Key Laboratory of Mountain Hazards and Surface Process, Chinese Academy of Sciences, China;
推荐引用方式 GB/T 7714	Cheng Z. L.,Liu J. J.,Liu J. K.. Debris flow induced by glacial lake break in southeast Tibet[C]. 见:. Milano. 2010.