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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorDUBARBIER, Benjamin
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCASTELLE, Bruno
IDREF: 087596520
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMARIEU, Vincent
dc.contributor.authorRUESSINK, Gerben
dc.date.accessioned2024-05-15T08:23:29Z
dc.date.available2024-05-15T08:23:29Z
dc.date.issued2015-01-01
dc.identifier.issn0378-3839en_US
dc.identifier.urihttps://www.researchgate.net/publication/267573515_Process-based_modeling_of_cross-shore_sandbar_behavior
dc.identifier.uriorcid:0000-0003-1740-7395:10.1016/j.coastaleng.2014.09.004
dc.identifier.urioai:researchgate.net:267573515
dc.identifier.urioai:crossref.org:10.1016/j.coastaleng.2014.09.004
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/199852
dc.description.abstractEnA coupled wave–current–sediment transport beach profile model is used to simulate cross-shore sandbar evolution on the time scale from days to months comprising both rapid offshore and slow onshore migrations. The discrimination of four modes of sediment transport driven by velocity and acceleration skewness, mean currents and slope effects allows addressing the dominant hydrodynamic processes governing cross-shore sandbar behavior. Acceleration–skewness-induced transport systematically results in a slow onshore sandbar migration together with a slow bar growth. Velocity–skewness-induced transport can drive onshore and offshore bar migrations with substantially larger rates. Mean–current-induced sediment transport systematically drives an offshore bar migration with either bar growth or decay. Slope effects essentially act as a damping term. The water level above the sandbar crest mainly influences the sandbar migration direction, while wave obliquity regulates the magnitude of the migration rates and is crucial to accurately simulate offshore sandbar migration during energetic obliquely incident waves. The inclusion of acceleration skewness is a necessary requirement to accurately reproduce the onshore migration of shallow sandbars. Detailed inter-site comparison of best-fit model parameters shows large differences meaning that free parameters attempt to compensate some mispecifications of the physics in the model. Although this also applies to other existing beach profile models, this suggests that this model needs further improvements including, for instance, the contribution of the injection of breaking wave turbulence onto the bed to sand stirring.
dc.language.isoENen_US
dc.sourceorcid
dc.sourceresearchgate
dc.sourcecrossref
dc.title.enProcess-based modeling of cross-shore sandbar behavior
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.coastaleng.2014.09.004en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalCoastal Engineeringen_US
bordeaux.page35-50en_US
bordeaux.volume95en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamMETHYSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04575695
hal.version1
hal.date.transferred2024-05-15T08:23:31Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
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