of breaking waves and shoreline motions. It is based on Serre Green-Naghdi equations,
solved using a time-splitting approach separating hyperbolic and dispersive parts of the
equations. The hyperbolic part of the equations is solved using Finite-Volume schemes,
whereas dispersive terms are solved using a Finite-Difference method. The idea is to switch
locally in space and time to NSWE by skipping the dispersive step when the wave is ready to …