Landsliding in response to rainfall involves physical processes that operate on disparate
timescales. Relationships between these timescales guide development of a mathematical …

In preparing this special issue of Environmental Geology, authors and reviewers pointed out
that the literature on the subject of rainfall-triggered mass movements is vast and scattered …

Many types of landslide movement are induced by large rainstorms, and empirical rainfall
intensity/duration thresholds for initiating movement have been determined for various parts …

A number of rainfall threshold models for triggering landslides have been developed in
either empirical or physical manner. The objective of an empirical rainfall threshold model is …

Rainfall‐triggered landslides are among the most widespread hazards in the world. The
hydrology in and around a landslide area is key to pore pressure buildup in the soil skeleton …

Rainfall is the most common cause of landslides. The cost of Rainfall Triggered Landslides
(RTL) is not well documented and often unobtainable. In areas where they do not pose a …

Rainfall-induced landslides are a common and significant source of damages and fatalities
worldwide. Still, we have little understanding of the quantity and properties of landsliding …

Rainfall-triggered landslides constitute a serious hazard and an important geomorphic
process in many parts of the world. Attempts have been made at various scales in a number …

To manage the hazard associated with shallow landslides, decision makers need an
understanding of where and when landslides may occur. A variety of approaches have been …

A physically based distributed slope stability model is described that utilizes a combined
surface–subsurface kinematic wave module to assess groundwater fluctuations related to …