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Sea state and coastal ocean circulation Based on a generalized Lagrangian mean of the equations of motion, a second order approximation in powers of the wave slope yields an explicit set of evolution equations for the current momentum. Wave forcing in that that system takes the form of the mean wave-induced pressure, and a body force arising from the dissipation of waves. This set of equations is integrated over the vertical and compared to other existing sets of equations. The effects of each process that is parameterized by source term in the wave action balance are described. First applications are given for two-dimensional cases, using a modified version of the ocean circulation model ROMS. Mots cles : tensions de radiation, moyenne Lagrangienne generalisee, courants 3D

États de mer et circulation océanique en zone côtière