Afficher la notice abrégée

dc.rights.licenseopenen_US
dc.contributor.authorNASCIMENTO, Fernanda P. S.
dc.contributor.authorVALLE-LEVINSON, Arnoldo
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSOTTOLICHIO, Aldo
IDREF: 158099699
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSENECHAL, Nadia
IDREF: 077248430
dc.date.accessioned2024-06-06T08:11:06Z
dc.date.available2024-06-06T08:11:06Z
dc.date.issued2019-02-15
dc.identifier.issn0278-4343en_US
dc.identifier.urioai:crossref.org:10.1016/j.csr.2019.01.007
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/200297
dc.description.abstractEnQuarter-diurnal tidal constituents are linked to tidal asymmetries and play a role in the morphodynamic evolution of inlets, estuaries and lagoons. A two-year non-continuous dataset of current velocities and waves was used to improve understanding on the generation of quarter-diurnal harmonics. Data analysis provides evidence for the generation of quarter-diurnal harmonics by wind-induced waves. Data were collected at the entrance to the Arcachon Lagoon, a mixed-energy tidal inlet in Southwest France. Temporal variability of the quarter-diurnal tidal current was identified through wavelet analysis of the main velocity component (alongshore velocity). Quarter-diurnal velocity amplitudes, bottom and wave stresses, and significant wave height suggested a linkage between quarter-diurnal amplification and wave action. Both significant wave height and wave stress were coherent with quarter-diurnal current amplitudes at synoptic frequencies, most markedly in winter months of both years observed. These coherences corroborated the hypothesis that wind-induced waves enhance bottom stresses that can generate and augment quarter-diurnal currents in this region.
dc.language.isoENen_US
dc.sourcecrossref
dc.title.enOvertide generation by wind-induced waves in a tidal inlet of SW France
dc.title.alternativeCont. shelf res.en_US
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.csr.2019.01.007en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalContinental Shelf Researchen_US
bordeaux.page66-75en_US
bordeaux.volume174en_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-04603019
hal.version1
hal.date.transferred2024-06-06T08:11:07Z
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=Continental%20Shelf%20Research&rft.date=2019-02-15&rft.volume=174&rft.spage=66-75&rft.epage=66-75&rft.eissn=0278-4343&rft.issn=0278-4343&rft.au=NASCIMENTO,%20Fernanda%20P.%20S.&VALLE-LEVINSON,%20Arnoldo&SOTTOLICHIO,%20Aldo&SENECHAL,%20Nadia&rft.genre=article


Fichier(s) constituant ce document

FichiersTailleFormatVue

Il n'y a pas de fichiers associés à ce document.

Ce document figure dans la(les) collection(s) suivante(s)

Afficher la notice abrégée