Les résultats sont issus d'une simulation du modèle hydrodynamique MARS et de son module de transport sédimentaire. Ils prennent en compte la marée réelle, la houle (simulée par le modèle WaveWatch3) et une couverture sédimentaire initiale réaliste.
La couche représente le transport attendu pour la fraction des galets (D=100mm) présents dans les faciès sédimentaires.
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