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1 Introduction The swash zone is the region of the beach where waves run up and down the beach, connecting the submerged bed of the surf zone with the dry part of the beach. Here, the hydrodynamical forcing that drives sediment transport is not only controlled by what happens above the bed surface but, due to the porous nature of the sediment bed, is also influenced by interactions between the subsurface and surface flow (Masselink & Li, 2001).
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