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Meso-tidal inlets located on the Western coast of Portugal tend to evolve towards closing during winter months, challenging their sustainable management. The morphodynamic model MORSYS2D is applied to Obidos lagoon to improve understanding such a behavior. Three mechanisms are proposed: (1) the presence of a reverse longshore transport downdrift caused by wave refraction on the ebb delta; (2) the elevation of mean sea-level which tends to attenuate ebb dominance at the inlet; (3) the onshore component of wave radiation stress gradients, which increases flood currents and turns ebb dominance to flood dominance at the inlet for waves larger than 1.5-2 m.

Processus conduisant les embouchures tidales dominées par la houle au comblement- Exemple de l’embouchure d’Óbidos, Portugal