“…Hyperspectral data were processed to atsensor radiance using calibration coefficients derived in the laboratory by the Centre for Research in Earth and Space Technology (CRESTech). Aerosol optical depth at 550 nm was derived from Micro-Tops II sunphotometer (Solar Light, Philadelphia, PA, USA) readings taken in the study area at the time of data acquisition, and subsequently used to process image data to ground-reflectance using the CAM5S atmospheric correction model (O'Neill, Zagolski, Bergeron, Royer, Miller, & Freemantle, 1997. Reflectance data were geo-referenced using GPS data collected onboard the aircraft.…”