Debris Flows
Debris Flow is a type of rapid mass wasting characterized by a saturated, heterogeneous mixture of water, rock fragments, soil, and organic material that moves downslope under gravity as a cohesive, viscous fluid, distinguished from other slope failures by its high density, mobility, and ability to transport large solid particles en masse.
2.7K
Publications
170.4K
Citations
5.9K
Authors
1.6K
Institutions
Publications per year
2017–2026
823
2.7K
1–5 of 2.7K
5.9K
Swiss Federal Institute for Forest, Snow and Landscape Research, Switzerland
42 publications · 3.8K citations
33
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31
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28
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27
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26
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1.6K
United States Geological Survey
Reston, United States
73 h-index
359 publications
43.1K citations

Chinese Academy of Sciences
Beijing, China
54 h-index
729 publications
28.1K citations
Institute of Mountain Hazards and Environment
Chengdu, China
54 h-index
736 publications
29.2K citations

Centre National de la Recherche Scientifique
Paris, France
46 h-index
198 publications
17.1K citations
Swiss Federal Institute for Forest, Snow and Landscape Research
Birmensdorf, Switzerland
45 h-index
133 publications
12.3K citations

Chengdu University of Technology
Chengdu, China
40 h-index
287 publications
17.2K citations
University of Chinese Academy of Sciences
Beijing, China
40 h-index
284 publications
10.6K citations

Hong Kong University of Science and Technology
Hong Kong, Hong Kong
39 h-index
142 publications
9.4K citations
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121 publications · 10.8K citations
63
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100 publications · 8.5K citations
54
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122 publications · 8.9K citations
54
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127 publications · 9.3K citations
48
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88 publications · 6.4K citations
46
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