Wildfire removes vegetation and weakens root strength, making burned areas more susceptible to erosion. Wildfire can also alter the physical and chemical characteristics of soil, creating a hydrophobic layer which increases runoff and may lead to damaging floods and debris flows in steep terrain. For example, following the 2017 Thomas Fire in Southern California, the devastating 9 January 2018 debris flows in the community of Montecito resulted in 23 deaths and nearly $1B in damages (Lancaster et al., 2021). In a meeting following the event, a Santa Barbara County resource manager made a plea to researchers: "I need to know how frequently I can expect post-fire debris flows of this magnitude in this area." Managers in other susceptible areas have expressed similar concerns for events in their area of responsibility.Impactful post-fire debris flows are not new to southern California, though the penultimate fatality event occurred in 2003 when 16 people died in debris flows emanating from the Old/Grand Prix burn areas in the San Bernardino Mountains (Oakley et al., 2017). The Montecito event renewed focus on post-fire debris-flow preparedness, with understanding the recurrence intervals of these events in the current and future climate as key concerns in planning efforts. Southern California's well-documented history of impactful post-fire debris flows compared to other susceptible regions makes it an excellent "laboratory" for research and development of decision support tools. Kean and Staley (2021) utilize Southern California's data to provide the first known framework to estimate recurrence intervals for minor and major post-fire debris flows in the region. This tool allows for evaluation of recurrence intervals in both a stationary and warming climate. Emerging research from disciplines relevant to post-fire hazards (e.g., soil, wildfire, and climate science) can be readily integrated into this framework. While regionally focused, this tool is applicable to other locations susceptible to post-wildfire debris flows provided the requisite data on rainfall triggering thresholds, burn severity, and wildfire recurrence can be collected.
Debris Flow Recurrence Interval as a Pre-Fire Decision Support ToolThe time between wildfire and precipitation events is decidedly brief in California, such that pre-fire planning presents significant advantages. For example, the 2018 Montecito debris flow occurred before the Thomas Fire was 100% contained (Lancaster et al., 2021). Observations over the past 60 years demonstrate a delayed onset of the rainy season in California (Lukovic et al., 2021). This allows dry conditions to extend into the autumn/winter offshore wind season (Abatzoglou et al., 2021;Swain, 2021), amplifying wildfire risk (Goss et al., 2020). Climate model projections suggest further "sharpening" of the precipitation Abstract Climate change will likely increase the frequency of damaging post-wildfire floods and debris flows, amplifying the threat to life, property, and infrastructure situated in susceptible are...