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The extension of the northern jetty in 1974, designed to ensure sufficient water depths in the existing access channel to the port and to preserve the inner basin from wave agitation, resulted in the artificial interruption of the southward oriented littoral drift. It led to an important accretion of the northern beaches of Capbreton and Hossegor and erosion of the littoral located south of Capbreton. The erosion issues had direct impacts on tourism, bath activities and amenities of the City and can endanger the protection structures as well as back dune installations. The present study was aimed at providing the City Council with materials for answers about developments, preservation and protection of the littoral with respect to the future shoreline evolution. Mots-clés : Capbreton, protection littorale, transfert hydraulique de sable, SWAN, GENESIS 1.Introduction La Commune de Capbreton est située sur la côte sableuse Aquitaine à environ 45 km au nord de la frontière espagnole. Cette côte sableuse s’étend sur 240 km depuis l’estuaire de la Gironde au nord jusqu’au Cap Saint Martin au sud. C’est un littoral sauvage et préservé, bordé par des cordons dunaires stabilisés artificiellement (fig. 1).

L’utilisation de système hydrauliques de transfert de sables dans la réhabilitation d’une plage urbaine : le cas de Capbreton (Landes)