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The influence of crescentic sand bars on mean currents induced by waves is investigated. A depth integrated model is presented to solve horizontally twodimensional problems. Numerical simulations are obtained on a typical bathymetry of the aquitan coast during high and low tide, with a frontal and oblique swel1. Computed swell focalisation and breaking zone are in qualitative agreement with our observations. Moreover, on the one hand our results show the presence of stable rip currents during low tide, on the other hand a strong sensitivity of wave incidence to currents is obtained. Thus, the sea level influence over current pattern is revealed.

Modélisation des écoulements induits par la houle sur les plages d'Aquitaine