Dear Pete,
thank you for your reply.
If I understand well, ax, bx, cx coefficient include elevation of target via DEM ingestion.
Does ARCSI take into account the local orientation of the surface to correct the apparent reflectance (TOA reflectance)
to be used in the inversion with xa, xb amd xc coefficient?
In other words, assuming a uniform lambertian surface, the atmospherically corrected reflectance is estimate as
y=aX×(apparent reflectance)−bXsurface reflectance=y1.0+cX×y
where
apparent reflectance = pi * measured_radiance / (cos_theta * solar_flux)
theta is the actual sun zenith angle (locally defined via DEM).
Is it correct?
Thanl you in advance
Lucia