“…It is mandatory to verify that those properties remain unchanged in the passage from the impermeable to the permeable bed configuration. As a matter of fact, the presence of a finite-height bed of spheres determines a damping of the wave by introducing a wave height dissipation over the porous bed as described by Corvaro et al (2010) and Sawaragi and Deguchi (1992) in a laboratory context and by Liu and Dalrymple (1984) and Gu and Wang (1991) from a theoretical perspective. Moreover, when waves propagate over a porous bed, also their wavelength changes, because their dynamics can be assimilated to that of a wave propagating over a rigid impermeable bed with a larger effective water depth h eff , which depends mainly on the properties of the porous medium.…”