IMPROVING OUR ABILITY TO PREDICT THE PROBABILITY OF DEBRIS-FLOW OCCURRENCE IN RECENTLY BURNED AREAS OF SOUTHERN CALIFORNIA
We improve our estimates of post-fire debris-flow probability by analyzing new information related to debris-flow response and rainfall, basin morphometry (from higher resolution data), burn severity and soil characteristics from 14 burn areas. These new data increased the database from 306 records (fire years 2003 – 2006) to 1748 records (fire years 2007 – 2010). Instrumental records of debris-flow timing and associated rainfall intensities also provide new insights into the rainfall conditions that initiate post-fire debris flows. Formerly, probabilities were calculated using data from storms with durations in excess of three hours. Monitoring data highlight the importance of short-duration (≤ 30 minutes), high-intensity bursts of rainfall in generating debris flows, with little correlation between debris-flow initiation and rainfall over longer durations.
These advances warrant revisiting the current model of calculating post-fire debris-flow probability. The updated probability model incorporates readily available precipitation frequency estimates and variables derived from digital elevation, soils and burn severity data. The new empirical model of post-fire debris-flow probability outperforms earlier modeling efforts and relies upon more physically meaningful variables than earlier models. The updated model will be implemented in future post-fire debris-flow hazard assessments in southern California.