Deblurring of satellite image in flat terrain via analysis

The apparent radiance of surface features which an arbitrary spacecraft measures differs from the intrinsic surface radiance of the object, because of the presence of intervening terrestrial atmosphere bounded below by the horizontally nonuniform albedos of non-Lambertian surface in flat terrain. In the present paper it is shown how to remove such atmospheric effects on remotely sensed data. It is physically approximated by using a global approach that includes the irradiance effect from the adjacent terrain, and other effects.<
>