中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Debris flows originating in the mountain cryosphere under a changing climate: A review

文献类型:期刊论文

作者Yu, Guo-An1; Yao, Weiwei2; Huang, He Qing2; Liu, Zhaofei2
刊名PROGRESS IN PHYSICAL GEOGRAPHY-EARTH AND ENVIRONMENT
出版日期2020-10-06
页码36
关键词Geo-mechanical processes glacier retreat hazard hydraulic processes initiation moraine permafrost rock glacier
ISSN号0309-1333
DOI10.1177/0309133320961705
通讯作者Yu, Guo-An(yuga@igsnrr.ac.cn) ; Liu, Zhaofei(zfliu@igsnrr.ac.cn)
英文摘要Debris flows originating in the mountain cryosphere (DFMC) are one of the most globally important, widely distributed mass flows (and natural geohazards) in mountain areas with a high altitude and/or high latitude. This is particularly the case in high mountain areas that have been undergoing rapid glacier retreat, permafrost degradation, and other melt/thaw related processes. As a consequence, the actual hazards and potential risks of DFMC have drawn increasing attention in the context of global climate change (i.e. a rising temperature and higher occurrence of strong precipitation events). Unlike debris flows at low elevations, where their occurrence is closely related to precipitation (intensity and duration), the breach of a DFMC event depends on precipitation and/or air temperature, which in turn influence melt/thaw processes, rending the formation mechanism much more complicated. Although research has been widely carried out on DFMC in past decades, there is still a long way to go before we have reached a complete understanding of the formation mechanism and triggering conditions. This review summarizes recent progress in the study of DFMC, including typical DFMC events and their causes, the failure mechanisms of rock (or ice-rock joints), the characteristics of moraine deposits, initiation through hydraulic erosion (entrainment), the relationship between DFMC initiation and meteorological conditions, and the slope stability of the mountain cryosphere under a changing climate. Several issues that should be addressed in future research are also discussed.
WOS关键词MONT-BLANC MASSIF ; SOUTHERN COAST MOUNTAINS ; ROCK-GLACIER DYNAMICS ; LAKE OUTBURST FLOOD ; BRITISH-COLUMBIA ; PERMAFROST DEGRADATION ; SEDIMENT TRANSFER ; SLOPE FAILURES ; NEW-ZEALAND ; PRECIPITATION EXTREMES
资助项目National Key R&D Program of China[2018YFC1505201] ; National Natural Science Foundation of China[41971010]
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000576578800001
出版者SAGE PUBLICATIONS LTD
资助机构National Key R&D Program of China ; National Natural Science Foundation of China
源URL[http://ir.igsnrr.ac.cn/handle/311030/157033]  
专题中国科学院地理科学与资源研究所
通讯作者Yu, Guo-An; Liu, Zhaofei
作者单位1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing, Peoples R China
2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
推荐引用方式
GB/T 7714
Yu, Guo-An,Yao, Weiwei,Huang, He Qing,et al. Debris flows originating in the mountain cryosphere under a changing climate: A review[J]. PROGRESS IN PHYSICAL GEOGRAPHY-EARTH AND ENVIRONMENT,2020:36.
APA Yu, Guo-An,Yao, Weiwei,Huang, He Qing,&Liu, Zhaofei.(2020).Debris flows originating in the mountain cryosphere under a changing climate: A review.PROGRESS IN PHYSICAL GEOGRAPHY-EARTH AND ENVIRONMENT,36.
MLA Yu, Guo-An,et al."Debris flows originating in the mountain cryosphere under a changing climate: A review".PROGRESS IN PHYSICAL GEOGRAPHY-EARTH AND ENVIRONMENT (2020):36.

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来源:地理科学与资源研究所

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