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dc.contributor.authorSimanesew, Abushet
dc.contributor.authorTrulsen, Karsten
dc.contributor.authorKrogstad, Harald E
dc.contributor.authorNieto Borge, José Carlos
dc.date.accessioned2018-02-07T07:53:59Z
dc.date.available2018-02-07T07:53:59Z
dc.date.created2017-04-07T08:58:32Z
dc.date.issued2017
dc.identifier.citationApplied Ocean Research. 2017, 65 79-89.nb_NO
dc.identifier.issn0141-1187
dc.identifier.urihttp://hdl.handle.net/11250/2483106
dc.description.abstractWe have employed laboratory and numerical experiments in order to investigate propagation of waves in both long and short-crested wave fields in deep water. For long-crested waves with steepness, ϵ = kcac = 0.1 (a fairly extreme case), reliable prediction can be performed with the modified nonlinear Schrödinger equation up to about 40 characteristic wavelengths. For short-crested waves the accuracy of prediction is strongly reduced with increasing directional spread.nb_NO
dc.language.isoengnb_NO
dc.publisherElseviernb_NO
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/deed.no*
dc.titleSurface wave predictions in weakly nonlinear directional seasnb_NO
dc.typeJournal articlenb_NO
dc.typePeer reviewednb_NO
dc.description.versionacceptedVersionnb_NO
dc.source.pagenumber79-89nb_NO
dc.source.volume65nb_NO
dc.source.journalApplied Ocean Researchnb_NO
dc.identifier.doi10.1016/j.apor.2017.03.009
dc.identifier.cristin1464258
dc.relation.projectNorges forskningsråd: 214556nb_NO
dc.description.localcode© 2017. This is the authors’ accepted and refereed manuscript to the article. Locked until 6.4.2019 due to copyright restrictions. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/nb_NO
cristin.unitcode194,63,15,0
cristin.unitnameInstitutt for matematiske fag
cristin.ispublishedtrue
cristin.fulltextpostprint
cristin.qualitycode1


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Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal
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