from multiscale surfaces such as ocean surfaces. It consists of combining geometrical optics
(GO) with the small-perturbation model (SPM) to be able to cope with both the small-and
large-scale components of the surface. However, well-known shortcomings of this method
are the arbitrariness of the dividing scale and the sensitivity of the scattering cross section to
the choice of this parameter. We propose to replace SPM with the first-order small-slope …