For Lambertian surface albedo (cases a and c) there is a quit good agreement, small differences for aerosol and cloud cases; scalar results agree with CDISORT, which uses exactly the same setups
BRDF (Cox and Munk) results similar to SCIATRAN and CDISORT, seems different from function used in SRON
Polarized reflectance over ocean in sun glint similar to SRON results, but not exactly the same
intercomparisons/scoremip/results/mystic_acc.txt · Last modified: 2014/10/30 10:14 (external edit)