The model is validated by comparison of the numerically predicted water levels and velocities against measured water levels, stationary velocities and velocities along transects (ADCP sailed) at several locations at the coast and the Western Scheldt estuary. The performance of Scaldis-Coast is found to be good at the Belgian coast but also in The Western Scheldt. For the water levels the total RMSE increases from 9 cm in the North Sea to 13 cm in the Western Scheldt towards Antwerp. The absolute value of the bias of water levels is equal or lower than 5 cm at most stations.
The Scaldis-Coast performs good in predicting the velocities at the considered coastal locations, presenting RMSE of velocity magnitude which is in general around 0.15 m/s.
The hydrodynamic model is available at the Flanders Hydraulics Research model repository: https://wlsubversion.br>vlaanderen.be/!/#repoSpNumMod/view/head/TELEMAC/Scaldis-Kust/15_068%20Complex%20Model%20Kustvisie%202021/1_2D_HYDRODYNAMICS.