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hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMARTINS, Kévin
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorBONNETON, Philippe
hal.structure.identifierInstitut de Mathématiques de Bordeaux [IMB]
dc.contributor.authorLANNES, David
hal.structure.identifierLaboratoire des Écoulements Géophysiques et Industriels [Grenoble] [LEGI]
dc.contributor.authorMICHALLET, Hervé
dc.date.accessioned2024-04-04T02:41:10Z
dc.date.available2024-04-04T02:41:10Z
dc.date.issued2021-11-19
dc.identifier.issn0022-3670
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/191127
dc.description.abstractEnThe inability of the linear wave dispersion relation to characterize the dispersive properties of non-linear shoaling and breaking waves in the nearshore has long been recognised. Yet, it remains widely used with linear wave theory to convert between sub-surface pressure, wave orbital velocities and the free surface elevation associated with non-linear nearshore waves. Here, we present a non-linear fully dispersive method for reconstructing the free surface elevation from sub-surface hydrodynamic measurements. This reconstruction requires knowledge of the dispersive properties of the wave field through the dominant wavenumbers magnitude κ , representative in an energy-averaged sense of a mixed sea-state composed of both free and forced components. The present approach is effective starting from intermediate water depths - where non-linear interactions between triads intensify - up to the surf zone, where most wave components are forced and travel approximately at the speed of non-dispersive shallow-water waves. In laboratory conditions, where measurements of κ are available, the non-linear fully dispersive method successfully reconstructs sea-surface energy levels at high frequencies in diverse non-linear and dispersive conditions. In the field, we investigate the potential of a reconstruction that uses a Boussinesq approximation of κ , since such measurements are generally lacking. Overall, the proposed approach offers great potential for collecting more accurate measurements under storm conditions, both in terms of sea-surface energy levels at high frequencies and wave-by-wave statistics ( e.g. wave extrema). Through its control on the efficiency of non-linear energy transfers between triads, the spectral bandwidth is shown to greatly influence non-linear effects in the transfer functions between sub-surface hydrodynamics and the sea-surface elevation.
dc.language.isoen
dc.publisherAmerican Meteorological Society
dc.rights.urihttp://creativecommons.org/licenses/by/
dc.title.enRelation between orbital velocities, pressure and surface elevation in non-linear nearshore water waves
dc.typeArticle de revue
dc.identifier.doi10.1175/JPO-D-21-0061.1
dc.subject.halPlanète et Univers [physics]/Océan, Atmosphère
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Océanographie
dc.subject.halInformatique [cs]/Modélisation et simulation
dc.subject.halInformatique [cs]/Traitement du signal et de l'image
bordeaux.journalJournal of Physical Oceanography
bordeaux.hal.laboratoriesInstitut de Mathématiques de Bordeaux (IMB) - UMR 5251*
bordeaux.institutionUniversité de Bordeaux
bordeaux.institutionBordeaux INP
bordeaux.institutionCNRS
bordeaux.peerReviewedoui
hal.identifierhal-03450890
hal.version1
hal.popularnon
hal.audienceInternationale
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-03450890v1
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Journal%20of%20Physical%20Oceanography&rft.date=2021-11-19&rft.eissn=0022-3670&rft.issn=0022-3670&rft.au=MARTINS,%20K%C3%A9vin&BONNETON,%20Philippe&LANNES,%20David&MICHALLET,%20Herv%C3%A9&rft.genre=article


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