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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
hal.structure.identifierBureau de Recherches Géologiques et Minières [BRGM]
dc.contributor.authorD'ANNA, Maurizio
hal.structure.identifierBureau de Recherches Géologiques et Minières [BRGM]
dc.contributor.authorIDIER, Déborah
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCASTELLE, Bruno
IDREF: 087596520
hal.structure.identifierUnited States Geological Survey [Reston] [USGS]
dc.contributor.authorVITOUSEK, Sean
hal.structure.identifierBureau de Recherches Géologiques et Minières [BRGM]
dc.contributor.authorLE COZANNET, Goneri
dc.date.accessioned2024-03-11T10:18:58Z
dc.date.available2024-03-11T10:18:58Z
dc.date.issued2021
dc.identifier.issn2077-1312en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/188659
dc.description.abstractEnLong-term (>decades) coastal recession due to sea-level rise (SLR) has been estimated using the Bruun Rule for nearly six decades. Equilibrium-based shoreline models have been shown to skillfully predict short-term wave-driven shoreline change on time scales of hours to decades. Both the Bruun Rule and equilibrium shoreline models rely on the equilibrium beach theory, which states that the beach profile shape equilibrates with its local wave and sea-level conditions. Integrating these two models into a unified framework can improve our understanding and predictive skill of future shoreline behavior. However, given that both models account for wave action, but over different time scales, a critical re-examination of the SLR-driven recession process is needed. We present a novel physical interpretation of the beach response to sea-level rise, identifying two main contributing processes: passive flooding and increased wave-driven erosion efficiency. Using this new concept, we analyze the integration of SLR-driven recession into equilibrium shoreline models and, with an idealized test case, show that the physical mechanisms underpinning the Bruun Rule are explicitly described within our integrated model. Finally, we discuss the possible advantages of integrating SLR-driven recession models within equilibrium-based models with dynamic feedbacks and the broader implications for coupling with hybrid shoreline models
dc.language.isoENen_US
dc.rightsAttribution 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/us/*
dc.subject.enBruun Rule
dc.subject.enequilibrium shoreline models
dc.subject.enpassive flooding
dc.subject.enwave energy efficiency
dc.subject.enSea-Level Rise
dc.title.enReinterpreting the Bruun Rule in the Context of Equilibrium Shoreline Models
dc.title.alternativeJ. Mar. Sci. Eng.en_US
dc.typeArticle de revueen_US
dc.identifier.doi10.3390/jmse9090974en_US
dc.subject.halPlanète et Univers [physics]/Interfaces continentales, environnementen_US
dc.subject.halSciences de l'environnement/Milieux et Changements globauxen_US
bordeaux.journalJournal of Marine Science and Engineeringen_US
bordeaux.page974en_US
bordeaux.volume9en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue9en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamMETHYSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-03337985
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccCC BYen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Journal%20of%20Marine%20Science%20and%20Engineering&rft.date=2021&rft.volume=9&rft.issue=9&rft.spage=974&rft.epage=974&rft.eissn=2077-1312&rft.issn=2077-1312&rft.au=D'ANNA,%20Maurizio&IDIER,%20D%C3%A9borah&CASTELLE,%20Bruno&VITOUSEK,%20Sean&LE%20COZANNET,%20Goneri&rft.genre=article


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