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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Bibliographic Details
Main Authors: C. Lanni, M. Borga, R. Rigon, P. Tarolli
Format: Article
Language:English
Published: Copernicus Publications 2012-11-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/16/3959/2012/hess-16-3959-2012.pdf