Abstract
A model of a coastal barrier following the sea level changes is proposed. The model is applied to the Anapa Bay-bar. Its coastline retreats landward in spite of sediment accumulation due to longshore flux discharge. Modeling shows that sea level rise generated by tectonic processes can be the cause of the phenomenon. The coastal barrier follows the sea level rise and moves landward.
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Acknowledgements
This work was fulfilled in a scope of the Government assignment (Theme # 0149-2019-0005) and partially supported by RFBR (Grants ## 18-05-00741 and 18-55-3402 Cuba_t).
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Leont’yev, I.O., Akivis, T.M. (2020). A Model of a Coastal Barrier and Its Application to the Anapa Bay-Bar Coasts. In: Olegovna, C. (eds) Processes in GeoMedia—Volume I. Springer Geology. Springer, Cham. https://doi.org/10.1007/978-3-030-38177-6_5
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DOI: https://doi.org/10.1007/978-3-030-38177-6_5
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