Landslides are generated by natural causes and by human action, causing various
geomorphological changes as well as physical and socioeconomic loss of the environment …

The characteristics of debris flows (eg, velocity, discharge, kinematic energy) are highly
dependent on surges incurring abrupt changes to flow height, velocity, and boulder …

The existing empirical models do not consider the influence of material composition of
landslide deposits on the peak breach flow due to the uncertainty in the material …

Debris flows usually occur in steep mountain channels and can be extremely hazardous as
a result of their destructive power, long travel distance, and high velocity. However, their …

Many debris flows have significant amounts of entrainment, resulting in a substantially larger
final volume than their initial volume and more complicated mechanics and characteristics of …

Debris flows gain much of their mass by entraining material as they descend a steep
channel, growing many times before the deposition begins on gentler terrain downstream …

As water flow erodes bed sediment in a steep channel, a partly saturated debris flow, which
has an unsaturated layer in its upper part, develops while interacting with a subsurface flow …

What factors influence natural vegetation recovery in debris flow-prone areas, and how do
sediment dynamics play a role? This study investigates these questions in the Ohya debris …

The characteristics of debris flows (eg, mobility, sediment concentration, erosion, and
deposition of sediment) are dependent on the pore water pressure in the flows. Therefore …

A depth-averaged quasi single-phase mixture model is proposed for debris flows over
inclined bed slopes based on the shallow water hydrosediment-morphodynamic theory with …