Landslides, debris flows, and other destructive natural hazards induced by heavy rainfall in
mountainous regions are sometimes not independent but combined to form a disaster chain …

Physically based approaches for the regional assessment of slope stability using digital
elevation model (DEM) topography usually consist of one-dimensional (1D) descriptions …

This paper presents the results from the application of a regional, physically based stability
model: Transient Rainfall Infiltration and Grid-based Regional Slope-stability analysis …

Efforts to map the distribution of debris flows, to assess the factors controlling their
development, and to identify the areas susceptible to their occurrences are often hampered …

A GIS-based cell model, based on a kinematic approach is proposed to simulate debris flow
routing on a fan. The sediment–water mixture is modeled as a monophasic continuum, and …

Credible models of landslide runout are a critical component of hazard and risk analysis in
the mountainous regions worldwide. Hazard analysis benefits enormously from the number …

As for late, studies have indicated that cellular automaton (CA) models are among the most
effective solutions for simulating the extent of debris-flow run-out. However, it is currently …

Earthquake-triggered landslides are one of the major hazards in tectonically active mountain
belts, and a nowcasting (near-real-time assessment) model for rapid assessment of …

This research connects different but sequential processes of slope failure: landslide
occurrence, debris-flow initiation from landslides, and debris-flow propagation to lowlands …

Adjacent debris flows may interact in many ways: two or more concurrent debris flows may
merge; one debris flow can run out over an existing debris flow fan. Such interactions may …