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Het OWA, het open archief van het Waterbouwkundig Laboratorium heeft tot doel alle vrij toegankelijke onderzoeksresultaten van dit instituut in digitale vorm aan te bieden. Op die manier wil het de zichtbaarheid, verspreiding en gebruik van deze onderzoeksresultaten, alsook de wetenschappelijke communicatie maximaal bevorderen.

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one publication added to basket [210718]

A coupling module for tides, surges and waves Ozer, J.; Padilla-Hernandez, R.; Monbaliu, J.; Fanjul, E.A.; Albiach, J.C.C.; Osuna, P.; Yu, J.C.S.; Wolf, J. (2000). A coupling module for tides, surges and waves. Coast. Eng. 41(1-3): 95-124. dx.doi.org/10.1016/S0378-3839(00)00028-4 In: Coastal Engineering: An International Journal for Coastal, Harbour and Offshore Engineers. Elsevier: Amsterdam; Lausanne; New York; Oxford; Shannon; Tokyo. ISSN 0378-3839; e-ISSN 1872-7379, meer

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Beschikbaar in	Auteurs
VLIZ: Open Marine Archive 230266 [ download pdf ]

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Author keywords

coupling; surges; tides; waves

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Auteurs		Top
Ozer, J., meer Padilla-Hernandez, R., meer Monbaliu, J., meer Fanjul, E.A.	Albiach, J.C.C. Osuna, P., meer Yu, J.C.S. Wolf, J.

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Abstract

A generic module in which tides, surges and waves are incorporated has been developed, tested and prepared for dissemination within the framework of the MAST III PROMISE (PRe-Operational Modelling In the Seas of Europe) project. Two existing pre-operational numerical models, a wave model and a hydrodynamic model, were incorporated into a coupling framework that allows an efficient exchange of information between them. Minimal adaptation of the models was needed. The module has then been implemented and applied to the North Sea, then a series of experiments were performed to investigate the sensitivity of waves and surges to coupling. These experiments show that the sensitivity of waves to coupling increases from deep to shallow water, The sensitivity of surges is more uniformly distributed. The sensitivity of surges to coupling along the Spanish coast was also studied. The model results were less sensitive than in the North Sea. This is explained by the relative importance of the two forcing components, the atmospheric pressure and the wind stress, in both areas.

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