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dc.contributor.authorKing, Stuart Edward
dc.contributor.authorCarr, Magda
dc.contributor.authorDritschel, David Gerard
dc.date.accessioned2011-12-05T09:33:49Z
dc.date.available2011-12-05T09:33:49Z
dc.date.issued2011-01-10
dc.identifier.citationKing , S E , Carr , M & Dritschel , D G 2011 , ' The steady-state form of large-amplitude internal solitary waves ' , Journal of Fluid Mechanics , vol. 666 , pp. 477-505 . https://doi.org/10.1017/S0022112010004301en
dc.identifier.issn0022-1120
dc.identifier.otherPURE: 471402
dc.identifier.otherPURE UUID: 2e79bf07-e74c-4480-bc5e-5d6bfa049374
dc.identifier.otherstandrews_research_output: 32423
dc.identifier.otherScopus: 79951682334
dc.identifier.otherWOS: 000287053100018
dc.identifier.otherORCID: /0000-0001-6489-3395/work/64697797
dc.identifier.urihttps://hdl.handle.net/10023/2084
dc.description.abstractA new numerical scheme for obtaining the steady-state form of an internal solitary wave of large amplitude is presented. A stratified inviscid two-dimensional fluid under the Boussinesq approximation flowing between horizontal rigid boundaries is considered. The stratification is stable, and buoyancy is continuously differentiable throughout the domain of the flow. Solutions are obtained by tracing the buoyancy frequency along streamlines from the undisturbed far field. From this the vorticity field can be constructed and the streamfunction may then be obtained by inversion of Laplace's operator. The scheme is presented as an iterative solver, where the inversion of Laplace's operator is performed spectrally. The solutions agree well with previous results for stratification in which the buoyancy frequency is a discontinuous function. The new numerical scheme allows significantly larger amplitude waves to be computed than have been presented before and it is shown that waves with Richardson numbers as low as 0.062 can be computed straightforwardly. The method is also extended to deal in a novel way with closed streamlines when they occur in the domain. The new solutions are tested in independent fully nonlinear time-dependent simulations and are verified to be steady. Waves with regions of recirculation are also discussed.
dc.language.isoeng
dc.relation.ispartofJournal of Fluid Mechanicsen
dc.rightsThis is the author's version of this article. The published version (c)Cambridge University Press is available from http://journals.cambridge.orgen
dc.subjectInternal wavesen
dc.subjectSolitary wavesen
dc.subjectStratified flowsen
dc.subjectQA Mathematicsen
dc.subject.lccQAen
dc.titleThe steady-state form of large-amplitude internal solitary wavesen
dc.typeJournal articleen
dc.contributor.sponsorEPSRCen
dc.description.versionPostprinten
dc.contributor.institutionUniversity of St Andrews. School of Mathematics and Statisticsen
dc.contributor.institutionUniversity of St Andrews. Scottish Oceans Instituteen
dc.contributor.institutionUniversity of St Andrews. Applied Mathematicsen
dc.contributor.institutionUniversity of St Andrews. Marine Alliance for Science & Technology Scotlanden
dc.identifier.doihttps://doi.org/10.1017/S0022112010004301
dc.description.statusPeer revieweden
dc.identifier.urlhttp://www.scopus.com/inward/record.url?scp=79951682334&partnerID=8YFLogxKen
dc.identifier.grantnumberEP/F030622/1en


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