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dc.date.accessioned2024-02-21T18:21:01Z
dc.date.available2024-02-21T18:21:01Z
dc.date.created2023-04-13T12:33:06Z
dc.date.issued2023
dc.identifier.citationChristensen, Kai Håkon Weber, Jan Erik H. . Application of a Robin boundary condition to surface waves. Frontiers in Marine Science. 2023, 10
dc.identifier.urihttp://hdl.handle.net/10852/108412
dc.description.abstractSurface effects on deep-water gravity waves are investigated theoretically by the application of a Robin boundary condition with a complex Robin parameter, R=Rr+iRi. The Robin condition combines the shear stress and the horizontal velocity at the ocean surface. We show that this condition describes wave damping related to surface phenomena like elastic films or thin viscous fluid layers. It may also model wave generation by oscillating surface stresses depending on the signs and magnitudes of Rr and Ri.
dc.languageEN
dc.rightsAttribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleApplication of a Robin boundary condition to surface waves
dc.title.alternativeENEngelskEnglishApplication of a Robin boundary condition to surface waves
dc.typeJournal article
dc.creator.authorChristensen, Kai Håkon
dc.creator.authorWeber, Jan Erik H.
cristin.unitcode185,15,22,0
cristin.unitnameInstitutt for geofag
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.cristin2140566
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Frontiers in Marine Science&rft.volume=10&rft.spage=&rft.date=2023
dc.identifier.jtitleFrontiers in Marine Science
dc.identifier.volume10
dc.identifier.pagecount6
dc.identifier.doihttps://doi.org/10.3389/fmars.2023.1129643
dc.type.documentTidsskriftartikkel
dc.type.peerreviewedPeer reviewed
dc.source.issn2296-7745
dc.type.versionPublishedVersion
cristin.articleid1129643
dc.relation.projectNFR/280625
dc.relation.projectNFR/314449


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