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dc.rights.licenseopenen_US
hal.structure.identifierUniversity of Bath [Bath]
dc.contributor.authorMARTINS, Kévin
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorBONNETON, Philippe
IDREF: 059798823
hal.structure.identifierGéosciences Environnement Toulouse [GET]
dc.contributor.authorFRAPPART, Frédéric
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorDETANDT, Guillaume
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorBONNETON, Natalie
hal.structure.identifierUniversity of Bath [Bath]
dc.contributor.authorBLENKINSOPP, Chris
dc.date.accessioned2024-09-18T08:12:16Z
dc.date.available2024-09-18T08:12:16Z
dc.date.issued2017-05-10
dc.identifier.issn2072-4292en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/201640
dc.description.abstractEnThe secondary wave field associated with undular tidal bores (known as whelps) has been barely studied in field conditions: the wave field can be strongly non-hydrostatic, and the turbidity is generally high. In situ measurements based on pressure or acoustic signals can therefore be limited or inadequate. The intermittent nature of this process in the field and the complications encountered in the downscaling to laboratory conditions also render its study difficult. Here, we present a new methodology based on LiDAR technology to provide high spatial and temporal resolution measurements of the free surface of an undular tidal bore. A wave-by-wave analysis is performed on the whelps, and comparisons between LiDAR, acoustic and pressure-derived measurements are used to quantify the non-hydrostatic nature of this phenomenon. A correction based on linear wave theory applied on individual wave properties improves the results from the pressure transducer (Root mean square error, RMSE of 0.19 m against 0.38 m); however, more robust data is obtained from an upwards-looking acoustic sensor despite high turbidity during the passage of the whelps (RMSE of 0.05 m). Finally, the LiDAR scanner provides the unique possibility to study the wave geometry: the distribution of measured wave height, period, celerity, steepness and wavelength are presented. It is found that the highest wave from the whelps can be steeper than the bore front, explaining why breaking events are sometimes observed in the secondary wave field of undular tidal bores.
dc.language.isoENen_US
dc.rights.urihttp://creativecommons.org/licenses/by/
dc.subject.enundular bore non-hydrostatic processes LiDAR scanner wave-by-wave analysis
dc.subject.enundular bore
dc.subject.ennon-hydrostatic processes
dc.subject.enLiDAR scanner
dc.subject.enwave-by-wave analysis
dc.title.enHigh Frequency Field Measurements of an Undular Bore Using a 2D LiDAR Scanner
dc.typeArticle de revueen_US
dc.identifier.doi10.3390/rs9050462en_US
dc.subject.halSciences de l'ingénieur [physics]/Génie civilen_US
bordeaux.journalRemote Sensingen_US
bordeaux.page462en_US
bordeaux.volume9en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue5en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamMETHYSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-04271937
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=Remote%20Sensing&rft.date=2017-05-10&rft.volume=9&rft.issue=5&rft.spage=462&rft.epage=462&rft.eissn=2072-4292&rft.issn=2072-4292&rft.au=MARTINS,%20K%C3%A9vin&BONNETON,%20Philippe&FRAPPART,%20Fr%C3%A9d%C3%A9ric&DETANDT,%20Guillaume&BONNETON,%20Natalie&rft.genre=article


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