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A coupled-mode technique for wave-current interaction in variable bathymetry regions

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dc.contributor.author Belibassakis, KA en
dc.contributor.author Athanassoulis, GA en
dc.date.accessioned 2014-03-01T02:49:41Z
dc.date.available 2014-03-01T02:49:41Z
dc.date.issued 2004 en
dc.identifier.issn 10986189 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/34691
dc.relation.uri http://www.scopus.com/inward/record.url?eid=2-s2.0-23844444908&partnerID=40&md5=bf3b4f54fb4e936bfaab0c74c8ad4d24 en
dc.subject Coupled-modes en
dc.subject Scattering of waves by current en
dc.subject Variable bathymetry en
dc.subject Wave-current interaction en
dc.subject.other Approximation theory en
dc.subject.other Bathymetry en
dc.subject.other Boundary conditions en
dc.subject.other Electromagnetic wave scattering en
dc.subject.other Ocean currents en
dc.subject.other Problem solving en
dc.subject.other Vortex flow en
dc.subject.other Coupled-modes en
dc.subject.other Scattering of waves by current en
dc.subject.other Variable bathymetry en
dc.subject.other Wave-current interactions en
dc.subject.other Water waves en
dc.title A coupled-mode technique for wave-current interaction in variable bathymetry regions en
heal.type conferenceItem en
heal.publicationDate 2004 en
heal.abstract A coupled-mode technique for wave-current interaction is presented, with application to the problem of wave scattering by steady currents in variable bathymetry regions, and current variations on various scales. We consider obliquely incident waves on a horizontally non-homogeneous current in a variable-depth strip, which is characterized by straight and parallel bottom contours. The flow associated with the current is assumed to be parallel to the bottom contours (along-axis current) and it is considered to be known. In a finite subregion containing the bottom irregularity we assume an arbitrary horizontal current structure. Outside this region, the current is assumed to be uniform (or zero). At a first-order of approximation the wave flow is assumed to be irrotational, i.e. the vorticity of the total field is the same with the vorticity associated with the current. Then, restricting ourselves to linear, monochromatic (harmonic) waves of absolute frequency co, the wave potential, including the scattering effect by the current, is obtained as a solution to the modified Helmholtz equation, subject to the free-surface boundary condition formulated with respect to the intrinsic frequency, the bottom boundary condition, and the conditions at infinity. Based on an appropriate variational principle, in conjunction with a rapidly-convergent local-mode series expansion of the wave field in a finite subregion containing the current variation and the bottom irregularity, a coupled-mode system is obtained that can be considered as a generalization of the one derived by Athanassoulis & Belibassakis (1999). The present approach can be considered as an extension of the works by Smith (1983, 1987), and some of its main features are that it can be further elaborated to treat lateral discontinuities (e.g. vertical vortex sheets) and more general vertical current profiles with cross-jet component, and to include the effects of weak nonlinearity. Copyright © 2004 by The International Society of Offshore and Polar Engineers. en
heal.journalName Proceedings of the International Offshore and Polar Engineering Conference en
dc.identifier.spage 226 en
dc.identifier.epage 233 en


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