Quantitative landslide risk assessment requires information about the temporal, spatial and intensity probability of hazardous processes both regarding their initiation as well as their run-out. This is followed by an estimation of the physical consequences inflicted by the hazard, preferentially quantified in monetary values. For that purpose, deterministic hazard modelling has to be coupled with information about the value of the elements at risk and their vulnerability. Dynamic run-out models for debris flows are able to determine physical outputs (extension, depths, velocities, impact pressures) and to determine the zones where the elements at risk can suffer an impact. These results can then be applied for vulnerability and risk calcul...
On 4th November 2010, a debris flow detached from a large debris cover accumulated above the lowermo...
Flow-like mass movements are one of the most serious natural hazards, systematically producing huge ...
The accurate prediction of runout distances, velocities and the knowledge of flow rheology can reduc...
Several steps need to be accomplished for a quantitative landslide risk assessment. First, an analys...
For a quantitative assessment of debris flow risk, it is essential to consider not only the hazardo...
Vulnerability assessment, as a component of the consequence analysis, represents a fundamental stage...
Vulnerability assessment, as a component of the consequence analysis, represents a fundamental stage...
Debris flow hazard modelling at medium (regional) scale has been subject of various studies in recen...
Debris flow hazard modelling at medium (regional) scale has been subject of various studies in recen...
A deterministic distributed model has been developed for large-scale debris-flow hazard analysis in...
Landslide risk assessment was carried out at local level considering runout modelling and up-scaling...
On 4th November 2010, a debris flow detached from a large debris cover accumulated above the lowermo...
On 4th November 2010, a debris flow detached from a large debris cover accumulated above the lowermo...
The accurate prediction of runout distances, velocities and the knowledge of flow rheology can reduc...
On 4th November 2010, a debris flow detached from a large debris cover accumulated above the lowermo...
On 4th November 2010, a debris flow detached from a large debris cover accumulated above the lowermo...
Flow-like mass movements are one of the most serious natural hazards, systematically producing huge ...
The accurate prediction of runout distances, velocities and the knowledge of flow rheology can reduc...
Several steps need to be accomplished for a quantitative landslide risk assessment. First, an analys...
For a quantitative assessment of debris flow risk, it is essential to consider not only the hazardo...
Vulnerability assessment, as a component of the consequence analysis, represents a fundamental stage...
Vulnerability assessment, as a component of the consequence analysis, represents a fundamental stage...
Debris flow hazard modelling at medium (regional) scale has been subject of various studies in recen...
Debris flow hazard modelling at medium (regional) scale has been subject of various studies in recen...
A deterministic distributed model has been developed for large-scale debris-flow hazard analysis in...
Landslide risk assessment was carried out at local level considering runout modelling and up-scaling...
On 4th November 2010, a debris flow detached from a large debris cover accumulated above the lowermo...
On 4th November 2010, a debris flow detached from a large debris cover accumulated above the lowermo...
The accurate prediction of runout distances, velocities and the knowledge of flow rheology can reduc...
On 4th November 2010, a debris flow detached from a large debris cover accumulated above the lowermo...
On 4th November 2010, a debris flow detached from a large debris cover accumulated above the lowermo...
Flow-like mass movements are one of the most serious natural hazards, systematically producing huge ...
The accurate prediction of runout distances, velocities and the knowledge of flow rheology can reduc...