Abstract
Predicting sediment yield from recently burned areas remains a challenge but is important for hazard and resource management as wildfire impacts increase. Here we use lidar-based monitoring of two fires in southern California, USA to study the movement of sediment during pre-rainfall periods and postfire periods of flooding and debris flows over multiple storm events. Using a data-driven approach, we examine the relative importance of terrain, vegetation, burn severity, and rainfall amounts through time on sediment yield. We show that incipient fire-activated dry sediment loading and pre-fire colluvium were rapidly flushed out by debris flows and floods but continued erosion occurred later in the season from soil erosion and, in ∼9% of catchments, from shallow landslides. Based on these observations, we develop random forest regression models to predict dry ravel and incipient runoff-driven sediment yield applicable to small steep headwater catchments in southern California.
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CITATION STYLE
Guilinger, J. J., Foufoula-Georgiou, E., Gray, A. B., Randerson, J. T., Smyth, P., Barth, N. C., & Goulden, M. L. (2023). Predicting Postfire Sediment Yields of Small Steep Catchments Using Airborne Lidar Differencing. Geophysical Research Letters, 50(16). https://doi.org/10.1029/2023GL104626
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