Caracterización morfodinámica de las playas españolas del Golfo de Cádiz

J. Benavente; F. J. Gracia; L. Del Río; G. Anfuso; A. Rodríguez-Ramírez

doi:10.21701/bolgeomin.126.2-3.007

Authors

J. Benavente Departamento de Ciencias de la Tierra, Facultad de Ciencias del Mar y Ambientales, Universidad de Cádiz
F. J. Gracia Departamento de Ciencias de la Tierra, Facultad de Ciencias del Mar y Ambientales, Universidad de Cádiz
L. Del Río Departamento de Ciencias de la Tierra, Facultad de Ciencias del Mar y Ambientales, Universidad de Cádiz
G. Anfuso Departamento de Ciencias de la Tierra, Facultad de Ciencias del Mar y Ambientales, Universidad de Cádiz
A. Rodríguez-Ramírez Departamento de Geodinámica y Paleontología, Universidad de Huelva

DOI:

https://doi.org/10.21701/bolgeomin.126.2-3.007

Keywords:

beach classification, Gulf of Cadiz, beach morphodynamics, tidal range

Abstract

During the1980s several attempts were made to classify beaches according to their morphodynamic behaviour. Published papers proposed classifications based mainly on wave incident energy and beach characteristics, such as foreshore slopes and sediment settling velocities. In the 1990s more complex classifications appeared, where the effect of tides on wave action was included, highlighting their relevance to the determination of the morphodynamic state of the beach. In this paper we present a beach monitoring programme, in which more than 30 beaches located along the Spanish shores of the Gulf of Cadiz and the Strait of Gibraltar were surveyed for four years (2000-2004). The long study period allowed the monitoring of beach morphologies related both to fair weather (summer) and storm (winter) conditions. The coastal setting in the study area provided the opportunity for covering a wide range of tidal conditions, from high mesotidal (MSTR ca. 4 m) to microtidal (MSTR around 1 m). Furthermore, the dimensions of the study area permitted the monitoring of beaches linked to different boundary conditions, thus including both attached and detached beaches located at varying distances from main sediment sources, and influenced by different wave regimes. The analysis of the beach morphologies related to such contrasting conditions allowed the identification of the real significance of the tidal effect on beach profile morphology and hence on beach morphodynamics. Finally, we conclude that the effect of tides on wave action is the main factor determining beach morphodynamic behaviour.

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