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On a flat shallow seabed, sand spits and cuspate forelands with rhythmic shapes may develop and a barrier island can elongate alongshore which significantly differs from the beach changes on coasts facing a deep ocean. In this study, the interaction between two circular islands on a flat shallow seabed due to waves was investigated by the numerical simulations, focusing on the wave-sheltering effect of the islands themselves. The topographic changes caused by the interaction between two sandy islands were predicted using the BG model.

Interaction of Two Circular Sandy Islands on Flat Shallow Seabed due to Waves