“…This approach cannot lead to the simulation of a geosynchronous image because the spatial coverage would be too low and the viewing and solar angles are not representative of the geosynchronous configuration. A second approach is the forward model, which consists of modeling the surface reflectance and the radiance at the top of the atmosphere, as a function of ground biophysical and geometrical parameters [13]- [15]. The first advantage of this approach is that the models take into account the viewing and solar angles, which are important for non-Lambertian surface like the ocean.…”