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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorVANDENHOVE, Marine
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCASTELLE, Bruno
IDREF: 087596520
dc.contributor.authorNICOLAE LERMA, Alexandre
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMARIEU, Vincent
dc.contributor.authorMINGO, Ivana
dc.contributor.authorROBINET, Arthur
dc.contributor.authorMARTINS, Kévin
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorBUJAN, Stephane
dc.contributor.authorMAZEIRAUD, Vincent
dc.date.accessioned2025-02-21T09:26:18Z
dc.date.available2025-02-21T09:26:18Z
dc.date.issued2024
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/205081
dc.description.abstractEnHeadland and groyne sand bypassing greatly influences embayment dynamics at medium to long timescales, but is often disregarded or partially included in reduced-complexity shoreline models. This study explores how accounting for subaqueous sediment bypassing in a shoreline model affects mean embayed beach planshape and spatial variability. We implement a generic parametrization of sand bypassing in the LX-Shore model, with simulations on a synthetic embayment in two configurations: "full bypassing" (FB) where the sediments bypass the obstacle in the surfzone and beyond, and "shoreline bypassing" (SB) where bypassing occurs only when the shoreline extends beyond the obstacle. Time-invariant wave simulations show significant differences in updrift shoreline position between FB and SB. Simulations with time-varying wave angles and fixed wave height and period reveal that FB significantly impacts the embayment mean planform and spatial variability: FB reduces beach rotation by about 1/3, particularly under slightly oblique and slightly asymmetrical wave climates, and decreases shoreline curvature, especially under highly oblique wave climates. Downdrift shoreline erosion may be overestimated by up to 20% under SB. Our simulations provide new insight into the influence of subaqueous sand bypassing on embayed beach dynamics and emphasize the importance of including this process when modelling shoreline evolution in coastal embayments.
dc.description.sponsorshipComprendre et prévoir l'évolution contemporaine du traite de côte dans un contexte de changement climatique par assimilation de données satellite dans les modèles hybrides - ANR-21-CE01-0015en_US
dc.language.isoENen_US
dc.publisherEditions Paraliaen_US
dc.rightsAttribution 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/us/*
dc.subject.ensand bypassing
dc.subject.enembayed beach
dc.subject.enreduced-complexity shoreline model
dc.subject.enequilibrium beach planform
dc.subject.enrotation
dc.subject.encurvature
dc.titleCaractérisation de l’hydrodynamisme des plages et des petits fonds du littoral au sud de l’estuaire de la Gironde à partir de mesures in situ
dc.typeActes de congrès/Proceedingsen_US
dc.identifier.doi10.5150/jngcgc.2024.023en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.conference.titleXVIIIèmes Journées, Angleten_US
bordeaux.teamMETHYSen_US
bordeaux.inpressnonen_US
bordeaux.import.sourcecrossref
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcecrossref
dc.rights.ccCC BYen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.title=Caract%C3%A9risation%20de%20l%E2%80%99hydrodynamisme%20des%20plages%20et%20des%20petits%20fonds%20du%20littoral%20au%20sud%20de%20l%E2%80%99estuaire%20de%20la%20Gironde%2&rft.atitle=Caract%C3%A9risation%20de%20l%E2%80%99hydrodynamisme%20des%20plages%20et%20des%20petits%20fonds%20du%20littoral%20au%20sud%20de%20l%E2%80%99estuaire%20de%20la%20Gironde%&rft.date=2024&rft.au=VANDENHOVE,%20Marine&CASTELLE,%20Bruno&NICOLAE%20LERMA,%20Alexandre&MARIEU,%20Vincent&MINGO,%20Ivana&rft.genre=unknown


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