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dc.rights.licenseopenen_US
hal.structure.identifierLaboratório nacional de engenharia civil [Lisboa] = National Laboratory for Civil Engineering [Lisbon] = Laboratoire national de génie civil [Lisbonne] [LNEC]
dc.contributor.authorFORTUNATO, André
hal.structure.identifierLaboratório nacional de engenharia civil [Lisboa] = National Laboratory for Civil Engineering [Lisbon] = Laboratoire national de génie civil [Lisbonne] [LNEC]
dc.contributor.authorFREIRE, P.
hal.structure.identifierLIttoral ENvironnement et Sociétés [LIENSs]
hal.structure.identifierSAS Benoit Waeles-Consultant Génie Côtier
dc.contributor.authorMENGUAL, B.
hal.structure.identifierLIttoral ENvironnement et Sociétés [LIENSs]
dc.contributor.authorBERTIN, X.
hal.structure.identifierAGENCIA PORTUGUESA DO AMBIENTE PRT
dc.contributor.authorPINTO, C.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMARTINS, Kevin
hal.structure.identifierSAS Benoit Waeles-Consultant Génie Côtier
dc.contributor.authorGUERIN, Thomas
hal.structure.identifierLaboratório nacional de engenharia civil [Lisboa] = National Laboratory for Civil Engineering [Lisbon] = Laboratoire national de génie civil [Lisbonne] [LNEC]
dc.contributor.authorAZEVEDO, A.
dc.date.accessioned2024-02-12T08:08:19Z
dc.date.available2024-02-12T08:08:19Z
dc.date.issued2021-10
dc.identifier.issn0025-3227en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/188023
dc.description.abstractEnThe morphological evolution of the Tagus estuary inlet in the last century is analyzed in order to characterize its dynamics, explain its behavior and anticipate its future evolution. First, the evolution is characterized through a literature review, complemented by new data analyses. This review synthesizes the present understanding of the inlet's dynamics and highlights some key questions that remain unanswered. To address these questions, a 2DH process-based morphodynamic model is implemented and validated, and then used to refine the previous understanding of the inlet's dynamics. A new conceptual model, which highlights a seasonal behaviour of the inlet's morphodynamics, is proposed. During winter time, the residual sediment transport is directed seaward along the navigation channel, towards the inlet mouth along the beaches adjacent to the inlet, and towards the estuary over the southern part of the ebb delta (Cachopo Sul). During the maritime summer, residual sediment fluxes are approximately half those occurring during winter. The relative importance of tidal flows increases, leading to sediment fluxes directed towards the southwest over the Cachopo Sul. The sediment deposits formed during the summer can be mobilized under specific wave conditions and transported to the northern stretch of the beaches to the south of the inlet. A positive feedback between the erosion of the Cachopo Sul-or, similarly, sea level rise-and the sediment fluxes over this bank suggests that the evolution of the bank observed during the last decades will continue in the foreseeable future.
dc.language.isoENen_US
dc.subject.enmorphodynamics
dc.subject.enprocess-based model
dc.subject.endata analysis
dc.subject.enSCHISM
dc.title.enSediment dynamics and morphological evolution in the Tagus Estuary inlet
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.margeo.2021.106590en_US
dc.subject.halPlanète et Univers [physics]/Océan, Atmosphèreen_US
dc.subject.halPlanète et Univers [physics]/Interfaces continentales, environnementen_US
bordeaux.journalMarine Geologyen_US
bordeaux.page106590en_US
bordeaux.volume440en_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.sourcehal
hal.identifierhal-03454586
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Marine%20Geology&rft.date=2021-10&rft.volume=440&rft.spage=106590&rft.epage=106590&rft.eissn=0025-3227&rft.issn=0025-3227&rft.au=FORTUNATO,%20Andr%C3%A9&FREIRE,%20P.&MENGUAL,%20B.&BERTIN,%20X.&PINTO,%20C.&rft.genre=article


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