Abstract
Beach cusps are one of the most commonly observed rhythmic features in the nearshore. Their formation has been related amongst other processes to the presence of standing waves or self-organization processes. This chapter provides a short introduction to the modelling of beach cusp formation and the main feed-back mechanisms between flow, sediment transport processes and morphodynamics.
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CITATION STYLE
APA
Coco, G. (2017). Beach Cusps BT - Atlas of Bedforms in the Western Mediterranean. In J. Guillén, J. Acosta, F. L. Chiocci, & A. Palanques (Eds.) (pp. 55–57). Springer International Publishing. Retrieved from https://doi.org/10.1007/978-3-319-33940-5_10
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