Abstract
The evolution of the coastline is mainly driven by the gradients in the longshore sediment transport (LST). These gradients are mostly influenced by the incoming waves and the morphology of the coastline. Traditionally, the coastline is assumed to be quasi-rectilinear, and the formulations are not valid for curved shorelines. This chapter presents a new expression that not only accounts for the curvature of the shoreline but also includes the variability of the sediment size that is typically found along Mediterranean coasts. It is later applied to the study sites described in Chap. 2, and the relation between LST trends and coastline evolution is analyzed and discussed for both sites.
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Acknowledgements
This work was partially supported by the Spanish Ministry of Economy and Competitiveness (Projects CTM2012-32439 and BIA2015-65598-P). The second author was funded by the Spanish Ministry of Economy and Competitiveness (Research Contract BES-2013-062617 and Mobility Grant EEBB-I-16-11009). The authors are indebted to Gerd Masselink for his valuable suggestions and comments. Prof. Baquerizo is also acknowledged for helping in the development the LST expression for curvilinear coasts. We also thank Fátima Pereira for her support creating the bathymetric scenarios of Carchuna Beach and Cristóbal Rodríguez-Delgado for his assistance with the bathymetric data processing of Playa Granada.
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Ortega-Sánchez, M., Bergillos, R.J., López-Ruiz, A., Losada, M.A. (2017). Littoral Drift and Coastline Evolution on Mixed Sand and Gravel Coasts. In: Morphodynamics of Mediterranean Mixed Sand and Gravel Coasts. SpringerBriefs in Earth Sciences. Springer, Cham. https://doi.org/10.1007/978-3-319-52440-5_4
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DOI: https://doi.org/10.1007/978-3-319-52440-5_4
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