Table 1 Ranges of eruption source parameters required for Tephra2 were derived from literature on the 2014 eruption and used to inform ranges for optimisation during inversion. Parameters with ‘n.a’ (not applicable), are those whose values were determined from inversion optimisation rather than from available literature on the Kelud 2014 eruption.^a = Kristiansen et al. (2015), ^b = Maeno et al. (2019a), ^c = Goode et al. (2018)

From: Remotely assessing tephra fall building damage and vulnerability: Kelud Volcano, Indonesia