“…This approach potentially provides further insight into the mechanisms of runoff generation. We note that selection of the sampling ranges of hydrologic parameters is a critical issue in sensitivity analysis, and hydrologic model parameter ranges for this research were selected following other studies utilizing JoFlow (Georgakakos et al, 2018;Knighton, Saia, et al, 2017b;Knighton, Steinschneider, & Walter, et al, 2017a). Further, in order to understand the sensitivity of this analysis to the parameters time-to-peak (Tp, h), a measure of the time between the onset of a precipitation event and discharge peak associated with the event, and percent impervious cover (percent impervious, %), a measure of the proportion of groundcover impervious to water infiltration, we repeated this analysis twice: (a) by increasing the range of Tp to (0, 100) hours, allowing for longer catchment flow paths (see Figures S8 and S9), and (b) by removing percent impervious from the analysis, forcing runoff processes to occur solely as a saturation-excess process (e.g., Schneiderman et al, 2007) (see Figures S10 and S11).…”