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Our study concerns the flow generated in the vicinity of an horizontal wall set in a bidimensional wave flow, in order /0 damp down il. This wall generates IWo swirling layers. One of them develops from the upper stream edge of the wall (relatively to the direction ofpropagation of the swell) and is propagated towards the free surface. The other develops from the downstream edge and is propagatedtowards the bottom. The downstream layer participates to a large amplitude recirculation under the wall and generates a washout. phenomena which may be prejudicial to the stability of the structure.

Ecoulement tourbillonnaire et zone d'affouillement générés par la houle en présence d'une plaque immergée