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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
hal.structure.identifierObservatoire aquitain des sciences de l'univers [OASU]
dc.contributor.authorSENECHAL, Nadia
IDREF: 077248430
dc.contributor.authorCOCO, Giovanni
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.date.accessioned2024-06-07T12:27:56Z
dc.date.available2024-06-07T12:27:56Z
dc.date.issued2015-01-01
dc.identifier.issn0169-555Xen_US
dc.identifier.urihttps://www.researchgate.net/publication/267572488_Storm_impact_on_the_seasonal_shoreline_dynamics_of_a_meso-_to_macrotidal_open_sandy_beach_Biscarrosse_France
dc.identifier.uriorcid:0000-0003-1740-7395:10.1016/j.geomorph.2014.09.025
dc.identifier.urioai:researchgate.net:267572488
dc.identifier.urioai:crossref.org:10.1016/j.geomorph.2014.09.025
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/200341
dc.description.abstractEnA three-year dataset (2007-2010) of shoreline and sandbar positions derived from video observations of an open sandy beach (Biscarrosse, France) is analyzed, to explore the impact of storms on the seasonal shoreline dynamics. The results indicate that a clear seasonality is observed in the offshore significant wave height and in the occurrence of 'winter storm' events that are defined as periods with significant wave height greater than 4 m lasting at least 12 h. Data indicate that the range of variation of the inner sandbar positions (120 m) is two and a half times larger than the range of variation of the shoreline position. Correlation analyses suggest that the offshore conditions do not conclusively explain the position of the inner bar. Shoreline positions show a clear seasonal pattern, displaying a stable position occurring in February and July, providing evidence of seasonal-recovery although analysis of storm activity indicates that the number and intensity of storms is highly variable over the three years. The Biscarrosse data show that rapid erosion can be observed also under moderate conditions, and that beach recovery after the storm season can be relatively rapid.
dc.language.isoENen_US
dc.sourceorcid
dc.sourceresearchgate
dc.sourcecrossref
dc.title.enStorm impact on the seasonal shoreline dynamics of a meso- to macrotidal open sandy beach (Biscarrosse, France)
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.geomorph.2014.09.025en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalGeomorphologyen_US
bordeaux.page448-461en_US
bordeaux.volume228en_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-04604952
hal.version1
hal.date.transferred2024-06-07T12:27:58Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geomorphology&rft.date=2015-01-01&rft.volume=228&rft.spage=448-461&rft.epage=448-461&rft.eissn=0169-555X&rft.issn=0169-555X&rft.au=SENECHAL,%20Nadia&COCO,%20Giovanni&CASTELLE,%20Bruno&MARIEU,%20Vincent&rft.genre=article


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