Morphodynamic classification of sandy beaches in low energetic marine environment

Morphodynamic classification of beaches has achieved widespread acceptance in both geological and geomorphological literature. In this sense, the present work classifies twelve Mediterranean low energetic beaches according to the dimensionless fall parameter (Ω) parameter in the Island of Mallorca....

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Detalhes bibliográficos
Autores: Gómez-Pujol, Lluís, Orfila, Alejandro, Cañellas, Bartomeu, Álvarez-Ellacuria, Amaya, Méndez, Fernando J., Medina, Raúl, Tintoré, Joaquín
Tipo de documento: artigo
Data de publicação:2007
País:España
Recursos:Consejo Superior de Investigaciones Científicas (CSIC)
Repositório:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/99324
Acesso em linha:http://hdl.handle.net/10261/99324
Access Level:Acceso aberto
Palavra-chave:Beach morphodynamics
Beach morphology
Descrição
Resumo:Morphodynamic classification of beaches has achieved widespread acceptance in both geological and geomorphological literature. In this sense, the present work classifies twelve Mediterranean low energetic beaches according to the dimensionless fall parameter (Ω) parameter in the Island of Mallorca. Propagation of 44 yr of wave data as well as a detailed sediment study allows to provide probabilities for morphodynamical beach state on an annual and seasonal basis. Consequently, beaches in Mallorca fall between three major categories which are (a) truly reflective, (b) reflective skewed to intermediate and (c) intermediate beaches. The Mallorcan beach position in the morphodynamical scheme is close related to the physiographical and geological framework. Comparison of observed values with those obtained in the analysis leads that for gross beach classification there is agreement between predicted and real state. However on a seasonal classification, mainly during summer, there is no agreement between the predicted state and the real one. As the model does not incorporate the role of summer sea breezes, beach reflective states are highlighted. Real beach configurations correspond to more energetic wave dynamic conditions and to intermediate state scenarios. © 2007 Elsevier B.V. All rights reserved.