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Debris-flow susceptibility assessment at regional scale: Validation on an alpine environment

Autor
Bregoli, F.; De Medina, V.; Chevalier, G.; Hurlimann, M.; Bateman, A.
Tipus d'activitat
Article en revista
Revista
Landslides
Data de publicació
2015-06-01
Volum
12
Número
3
Pàgina inicial
437
Pàgina final
454
DOI
https://doi.org/10.1007/s10346-014-0493-x Obrir en finestra nova
Projecte finançador
Análisis de los mecanismos de rotura de deslizamientos superficiales y corrientes de derrubios desencadenados por lluvias
Repositori
http://hdl.handle.net/2117/25350 Obrir en finestra nova
URL
https://link.springer.com/article/10.1007%2Fs10346-014-0493-x Obrir en finestra nova
Resum
A debris flow is an erosional process that frequently occurs in areas with steep slopes. Although the initiation can be triggered in higher and inhabited altitudes, the propagation and then the deposition can endanger urbanized areas. Frequently, the zones of generation of debris flows are placed in unattainable territories complicating field observations. Moreover, the rapid vegetation's recovery can hide the scars and tracks created by the occurrence of the flow, unlikely to be recognizable in...
Citació
Bregoli, F. [et al.]. Debris-flow susceptibility assessment at regional scale : Validation on an alpine environment. "Landslides", Agost 2014.
Paraules clau
Basin-scale, Classification, Debris flow, Gis, Landslide hazard assessment, Part, Physical models, Physically-based model, Pyrenees, Rainfall, Slope stability, Statistical model, Susceptibility assessment
Grup de recerca
CRAHI - Centre de Recerca Aplicada en Hidrometeorologia
CREMIT - Centre de Recerca de Motors i Instal·lacions Tèrmiques
GITS - Modelització Integral de Conques i Transport de Sediments
MSR - Mecànica del Sòls i de les Roques

Participants