In the present paper, the continuum-mechanics based code RASH3D is used to evidence the influence that three factors can have on results of a numerical analysis. These are 1) the Digital Elevation Model (DEM) res-olution; 2) the morphology and substrate influence on the rheology selection; and 3) the role of the entrainment process. The Baio Dora debris flow is back-analysed to this aim. Obtained results have evidenced that a bad quality DEM can make fail all the attempts of selecting the more appropriate rheology and calibrat-ing its parameters. On the other side, the selection of a wrong rheology can give a unrealistic runout path, that is the moving mass can go as far taking a completely incorrect flowing directions. Finally, it is obser...
In this paper an attempt is made to unravel the run-out characteristics of a mass movement in the Si...
Numerical simulation can provide a useful tool for investigating the dynamics of phenomena like rock...
Landslide run-out is a complex phenomenon, much more difficult to simulate by models than flow of fl...
In the last years, numerical modelling has emerged as a useful tool for landslide runout analysis an...
This paper analyses an important aspect of the continuum numerical modeling of rapid landslides as d...
The entrainment of channel-path material plays an important role during runout of many rapid landsli...
Runout analysis, the prediction of landslide motion and its effects, is an essential component of l...
A numerical model set up to simulate rapid flowlike landslide motion across three-dimensional terrai...
Increasing population density and development of mountainous terrains bring human settlements within...
Rapid debris flows are identified among the most dangerous of all landslides. Due to their destructi...
Rapid landslides pose a significant hazard worldwide, and there is currently no routine way of predi...
This paper analyses an important aspect of the continuum numerical modelling of rapid landslides as ...
Over the last 20 years, many tools have been developed for the prediction of the post-failure behavi...
Dynamical runout models are essential tools in landslide hazard and risk assessment, because they al...
International audienceModelling of flow-like landslides is one of the possible approaches that can b...
In this paper an attempt is made to unravel the run-out characteristics of a mass movement in the Si...
Numerical simulation can provide a useful tool for investigating the dynamics of phenomena like rock...
Landslide run-out is a complex phenomenon, much more difficult to simulate by models than flow of fl...
In the last years, numerical modelling has emerged as a useful tool for landslide runout analysis an...
This paper analyses an important aspect of the continuum numerical modeling of rapid landslides as d...
The entrainment of channel-path material plays an important role during runout of many rapid landsli...
Runout analysis, the prediction of landslide motion and its effects, is an essential component of l...
A numerical model set up to simulate rapid flowlike landslide motion across three-dimensional terrai...
Increasing population density and development of mountainous terrains bring human settlements within...
Rapid debris flows are identified among the most dangerous of all landslides. Due to their destructi...
Rapid landslides pose a significant hazard worldwide, and there is currently no routine way of predi...
This paper analyses an important aspect of the continuum numerical modelling of rapid landslides as ...
Over the last 20 years, many tools have been developed for the prediction of the post-failure behavi...
Dynamical runout models are essential tools in landslide hazard and risk assessment, because they al...
International audienceModelling of flow-like landslides is one of the possible approaches that can b...
In this paper an attempt is made to unravel the run-out characteristics of a mass movement in the Si...
Numerical simulation can provide a useful tool for investigating the dynamics of phenomena like rock...
Landslide run-out is a complex phenomenon, much more difficult to simulate by models than flow of fl...