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![]() ![]() |
刊名 | PROGRESS IN PHYSICAL GEOGRAPHY-EARTH AND ENVIRONMENT
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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 |
DOI | 10.1177/0309133320961705 |
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. |
入库方式: OAI收割
来源:地理科学与资源研究所
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