Slope Flows is a thermally driven local wind system in mountainous terrain that consists of diurnally reversing along-slope circulations—upslope (anabatic) by day and downslope (katabatic) by night—generated by differential heating and cooling of inclined surfaces relative to the surrounding air.
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The use of the Slip Circle in the Stability Analysis of Slopes
A. W. Bishop · Géotechnique · 1955 · 2.7K citations
Engineering, Civil Engineering, Geotechnical Engineering +11
A simple definition of a landslide
D. M. Crudën · Bulletin of Engineering Geology and the Environment · 1991 · 784 citations
Anthony Young, M. A. Carson, M. J. Kirkby · Geographical Journal · 1973 · 724 citations
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United States Geological Survey
Reston, United States
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53 publications
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Chinese Academy of Sciences
Beijing, China
23 h-index
112 publications
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Centre National de la Recherche Scientifique
Paris, France
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87 publications
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Oregon State University
Corvallis, United States
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University of Utah
Salt Lake City, United States
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33 publications
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Kyoto University
Kyoto, Japan
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University of Alberta
Edmonton, Canada
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Colorado State University
Fort Collins, United States
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29 publications · 1.9K citations
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