work. It is first detailed and analysed for the 2D linear advection equation and then applied
to the 2D shallow water equations. The dimensional splitting technique allows us to extend
the ideas developed in the 1D case related to source terms, boundary conditions and the
reduction of the time step in the presence of large discontinuities. The boundary conditions
treatment as well as the wet/dry fronts in the case of the 2D shallow water equations require …