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. En-zone-littorale, la houle subit de fortes transformations par effets bathymétriques Une meilleure compréhension de ses modifications et des transferts d'énergie associés permet de mieux appréhender les problèmes de dimensionnement de structures côtières et d'aménagement du littoral

. La-première-partie, propose des méthodes de calcul, basées sur les houles de Stokes, pour la mesure d'ondes partiellement stationnaires à partir d'instruments de type électromagnétique (S4) ou acoustique (ADV) donnant des mesures synchrones de vitesses et/ou de pression. Les influences du courant , de la direction de propagation

. La-deuxième-partie, une méthode de suivi de surface libre de type SL-VOF (Semi-Lagrangian Volume Of Fluid), insérée dans un code de calcul industriel (code EOLE de la société Principia R&D). L'onde de gravité est modélisée par un soliton. L'étude de la propagation et du déferlement du soliton est effectuée pour deux applications : sur une marche (discontinuité du fond) puis sur un fond de pente constante 1/15