Costas (or others),
Do you know if ARTEMIS can capture the wave setup phenomenon in the surf zone (i.e. the seaward mean water surface slope that develops as breaking waves transfer their momentum to the surf zone)?
The theoretical note says,
The mild-slope model is a linear model...This is an important feature that evidences the limitations of that model when the bottoms have a small depth. This is because, if the bottoms come up, the shoaling process will “swell” the wave height to such an extent that it will become inconsistent with the variable water depth. In order to improve the domain validity and to broaden the range of applications of ARTEMIS, we have amended the initial mild-slope equation in order to take into account the prevailing dissipative processes in shallow water, namely bathymetric breaking and bottom friction.
So it seems that dissipation of wave energy (loss to internal energy by way of friction/turbulence) is parameterized, but I'm wondering if the onshore momentum flux is balanced. Or does ARTEMIS simply assumed a flat mean water surface?
Thanks,
Ben