“…This variable is retrieved from the radiance at the 4-μm band of satellite sensors and represents the instantaneous radiative energy that is released from actively burning fires. FRP has been extensively used as a proxy of fire intensity to characterize fire types (Roy & Kumar, 2017;Wooster & Zhang, 2004), fire behaviors (Smith & Wooster, 2005), and fire regimes (Archibald et al, 2013), to predict fire danger (Freeborn et al, 2016), and to investigate interactions among biomass burning, land cover dynamics, and hydrological cycles (Ichoku et al, 2016). More importantly, FRP is related to the rate of biomass combustion (Kaufman et al, 1998;Wooster et al, 2003) and the rate of emissions (Ichoku & Kaufman, 2005), which have been subsequently applied to estimate trace gas and aerosol emissions (Kaiser et al, 2012;Kumar et al, 2011;Vermote et al, 2009;Zhang et al, 2012).…”