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dc.rights.licenseopenen_US
dc.contributor.authorMCCARROLL, R. Jak
dc.contributor.authorBRANDER, Robert W.
dc.contributor.authorSCOTT, Tim
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCASTELLE, Bruno
IDREF: 087596520
dc.date.accessioned2024-05-06T09:00:12Z
dc.date.available2024-05-06T09:00:12Z
dc.date.issued2018-06-01
dc.identifier.issn2169-9003en_US
dc.identifier.urioai:crossref.org:10.1029/2017jf004491
dc.identifier.uriorcid:0000-0003-1862-747X:10.1029/2017jf004491
dc.identifier.uriorcid:0000-0003-1740-7395:10.1029/2017jf004491
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/199637
dc.description.abstractEnA multibeach Lagrangian data set was used to determine bathymetric controls on flow variability within the surfzone. Seven microtidal flow regimes were examined, six containing rip channels, under moderate shore normal waves. Three selected zones exemplified varying bathymetric control: (i) a alongshore uniform zone; (ii) a shallow rip channel at an oblique angle to shore normal; and (iii) a deep, shore-normal rip channel. Bathymetric variables included alongshore nonuniformity (φ) and channel angle relative to shore normal (α). Low-frequency flow (0.01 Hz) was described by velocity (U), velocity standard deviation (σU), angular deviation (σθ), and bias in direction of eddy rotation (ζbias). Observations of the exemplar zones indicated the following: (i) near-zero mean flow with transient eddies within the alongshore uniform zone; (ii) low mean flow with high ζbias within the oblique channel; and (iii) strong mean flow with low ζbias in the deep channel. Bathymetry and flow variables were spatially averaged and linearly correlated, scaling for wave forcing. Normalized flow variables were found to be interdependent and were correlated with bathymetric variability, with [U ∝ φ], [(U/σU) ∝ φ], and [σθ ∝ − φ], all with (R2 ≥ 0.8). A correlation was determined between α and ζbias (R2 ≥ 0.7, increasing as zone width is decreased), with peak ζbias within oblique channels. Based on these results, a conceptual model is introduced to predict flow behavior for known bathymetry. Surfzone currents were found to span a dynamic continuum from transient eddies on alongshore uniform bathymetry, to channelized rip currents, forced by bathymetric three-dimensionality and mediated by channel geometry.
dc.description.sponsorshipMarier les objectifs de défense côtière avec ceux de la protection du milieu naturel grâce aux dunes sableuses - ANR-17-CE01-0014en_US
dc.language.isoENen_US
dc.sourcecrossref
dc.sourceorcid
dc.title.enBathymetric Controls on Rotational Surfzone Currents
dc.typeArticle de revueen_US
dc.identifier.doi10.1029/2017jf004491en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalJournal of Geophysical Research: Earth Surfaceen_US
bordeaux.page1295-1316en_US
bordeaux.volume123en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue6en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamMETHYSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04569123
hal.version1
hal.date.transferred2024-05-06T09:00:13Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
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