Sentence examples for initiation of debris flow from inspiring English sources

Locations for initiation of debris flow deposition were situated in stream orders 3 and 4 in 60% of cases.

Furthermore, the hydrologic and the hydraulic conditions for the initiation of debris flow are simulated, providing the solid liquid hydrograph of the resulting debris flow.

This susceptibility maps indicates the relative likelihood for the initiation of debris flows to be generated.

This is supported by an exponential Clausius-Clapeyron-style scaling between grain size and temperature, and also reconciles with climate dynamics and the initiation of debris flows.

The initiation of debris flows predominately by progressive entrainment of surficial and channel material has been observed in the field (DeGraff et al., 2011) and quantified in southern California (Santi et al., 2008).

This work would be helpful in understanding the initiation mechanism of debris flows induced by rainfall, and sand production in gas hydrate-bearing sediments due to increasing fluid content associated with hydrate dissociation.

Video evidence, field observations and an empirical debris flow model linked to an instantaneous rain gauge were used to ascertain the exact times of debris flow initiation.

While the mechanism of debris flow initiation could not be determined unambiguously, clearly debris flows must entrain substantial amounts of sediment along the flow path to attain the volumes estimated at the distal end of the fan.

This paper presents five important aspects of the evolution of debris flows: (1) supply of debris flow materials; (2) triggering rainfall; (3) initiation mechanisms and types of debris flows; (4) runout characteristics; and (5) elevated riverbed due to the deposited materials from the debris flows.

Debris flows occurred even in areas with an E hazard class, which was initially expected to indicate a very low likelihood of debris flow.

Other factors such as the size and shape of the valley along with variations in slope direction, properties of the subsoil, and vegetation also have an influence on the initiation and movement of debris flows.