Modelling shallow landslide susceptibility by means of a subsurface flow path connectivity index and estimates of soil depth spatial distribution
Topographic index-based hydrological models have gained wide use to describe the hydrological control on the triggering of rainfall-induced shallow landslides at the catchment scale. A common assumption in these models is that a spatially continuous water table occurs simultaneously across the catch...
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| Principais autores: | , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Copernicus Publications
2012-11-01
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| coleção: | Hydrology and Earth System Sciences |
| Acesso em linha: | http://www.hydrol-earth-syst-sci.net/16/3959/2012/hess-16-3959-2012.pdf |
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