“…Traditionally, burn severity has been quantified from Landsat sensors through different methods, including those based on radiative transfer models (Chuvieco et al, 2006, De Santis et al, 2009, spectral unmixing (Fernández-Manso et al, 2009, Quintano et al, 2017, or spectral indices (Chu andGuo, 2014, Fernández-García et al, 2018a). Among them, the standard method to quantify burn severity is through the delta Normalized Burn Ratio (dNBR) (Key and Benson, 2006) spectral index, and its relativized version (RdNBR) (Miller and Thode, 2007), which is less dependent on the pre-fire vegetation, and potentially more suitable than dNBR for comparisons among zones with different environmental conditions (Miller and Thode, 2007;Rahman et al, 2018). Both spectral indices are based on the change caused by fire in near infrared (NIR) and shortwave infrared (SWIR) reflectance, which are highly sensitive to canopy density and moisture content respectively (Chuvieco, 2010).…”