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STOCHASTIC FORCING OF SEDIMENT SUPPLY TO CHANNEL NETWORKS FROM LANDSLIDING AND DEBRIS FLOW (1997)
Sediment influx to channel networks is stochastically driven by rainstorms and other perturbations, which are discrete in time and space and which occur on a landscapewith its own spatial variability in topography, colluvium properties, and state of recovery from previous disturbances.
Reference:
WATER RESOURCES RESEARCH, VOL. 33, NO. 12, PAGES 2849-2863, DECEMBER 1997
WATER RESOURCES RESEARCH, VOL. 33, NO. 12, PAGES 2849-2863, DECEMBER 1997
Organization:
Earth Systems Institute, Seattle, Washington
USA, Oregon
Earth Systems Institute, Seattle, Washington
USA, Oregon
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