2009 Portland GSA Annual Meeting (18-21 October 2009)

Paper No. 3
Presentation Time: 2:15 PM

MAPPING POST-WILDFIRE DEBRIS-FLOW IMPACT, SOUTHERN CALIFORNIA, USA


GARTNER, Joseph E., U.S. Geological Survey, Box 25046, MS 966, DFC, Denver, CO 80225, CANNON, Susan H., U.S. Geological Survey, P.O. Box 25046, Mail Stop 966, Denver, CO 80225-0046, BROCK, Rebecca J., Dept Geology and Geological Engineering, Colorado School of Mines, Golden, CO 80401, BERNARD, David R., Geology and Geological Engineering, Colorado School of Mines, Golden, CO 80401, SANTI, Paul, Department of Geology & Geological Engineering, Colorado School of Mines, Golden, CO 80401, WORSTELL, Bruce B., U.S. Geological Survey, 47914 252nd Street, Sioux Falls, SD 57198 and QUEIJA, Vivian R., U.S. Geological Survey, 909 1st avenue, 4th floor, Seattle, WA 98104, jegartner@usgs.gov

Wildfire is a frequent occurrence in southern California, and debris flows generated from recently burned basins can pose significant hazards to life and property. The potential impact of post-wildfire debris flows can be identified using a sequence of empirical models that first estimate potential debris-flow volumes, then identify the point where deposition becomes spatially continuous within each drainage basin, and last, by defining relations between volume and cross-sectional and planimetric deposit area. The model for calculating the volume of debris-flow material that can be expected at the basin mouth was developed using multiple linear regression analyses of a database measured from 42 basins burned by ten recent fires in southern California. Debris-flow volume is estimated using a combined function of basin relief, length of the longest flow path within the basin, the extent and severity of the fire, and peak 1-hour storm-rainfall intensity. The model to identify the upstream limit of continuous debris-flow deposition within a drainage basin was developed using field mapping of 16 post-fire, debris-flow producing channels. Field observations indicated that the location of the onset of debris-flow deposition could be consistently identified where the channel widens below the downstream-most bedrock step within each channel. The bedrock step can be identified before the passage of a debris flow on a 2-meter DEM as the downstream-most location where two or more consecutive cells (a length of four meters or more) have a gradient of 24 degrees or greater. Finally, relations between post-fire debris-flow volume and cross-sectional and planimetric area were defined from measurements of deposits of 22 post-fire debris flows in southern California. These relations can be implemented within a GIS to map the areas within the DEM that are likely to be inundated by debris flow. The resulting debris-flow inundation maps provide information necessary to identify and prioritize areas for post-fire erosion mitigation, warnings and evacuation planning in southern California.