“…Previous work has established methods for estimating debris‐flow likelihood (Staley et al., 2017) and volume (Gartner et al., 2014) at the watershed scale in the western USA based on terrain and soil characteristics, burn severity, and peak 15‐min rainfall intensity. Models for postfire debris‐flow likelihood and volume have also been developed and applied in other fire‐prone regions, including the Mediterranean and Australia (Diakakis et al., 2023; Nyman et al., 2015). However, while a number of models, such as RAMMS (Christen et al., 2010), FLO‐2D (O’Brien et al., 1993), D‐Claw (George & Iverson, 2014; Iverson & George, 2014), and ProDF (Gorr et al., 2022), simulate PFDF inundation with comparable results (Barnhart et al., 2021), debris‐flow inundation estimates are not currently standard practice in postfire hazard assessments (Barnhart, Miller, et al., 2023; Barnhart, Romero, & Clifford, 2023).…”