INFLUENCE OF TIDE VS WAVE ON SEDIMENT DYNAMICS AND DUNE INTERNAL ARCHITECTURE ON A MACROTIDAL INNER CONTINENTAL SHELF (EASTERN ENGLISH CHANNEL)

Seabed of continental shelf environments is regularly covered with a multitude of bedforms formed in response to interactions between fluid dynamics and sediment. These mobile sedimentary features have been widely studied in order to prevent damages on human activities and anthropogenic structures. In coastal areas, submarine dune dynamics is mainly controlled by tidal currents and wind and wave forcings (e.g. Le Bot et al., 2004; Idier et al., 2011). However, it is generally not obvious to distinguish which forcing is predominant in dune dynamics.