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dc.contributor.authorKalisch, Henrik
dc.contributor.authorSenthilkumar, Amutha
dc.date.accessioned2017-06-08T12:38:59Z
dc.date.available2017-06-08T12:38:59Z
dc.date.issued2013-03-14
dc.identifier.issn1023-5809en_US
dc.identifier.urihttps://hdl.handle.net/1956/15943
dc.description.abstractThis paper is focused on finding rules for waveheight change in a solitary wave as it runs up a slowly increasing bottom. A coupled BBM system is used to describe the solitary waves. Expressions for energy density and energy flux associated with the BBM system are derived, and the principle of energy conservation is used to develop an equation relating the waveheight and undisturbed depth to the initial undisturbed depth and the incident waveheight. In the limit of zero waveheight, Boussinesq's shoaling law is recovered.en_US
dc.language.isoengeng
dc.publisherCopernicus Publicationsen_US
dc.relation.ispartof<a href="http://hdl.handle.net/1956/15946" target="_blank">On the Relation between Surface Profiles and Internal Flow Properties in Long-Wave Models</a>en_US
dc.rightsAttribution CC BYeng
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/eng
dc.titleDerivation of Boussinesq's shoaling law using a coupled BBM systemen_US
dc.typePeer reviewed
dc.typeJournal article
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2013 The Author(s)en_US
dc.identifier.doihttps://doi.org/10.5194/npg-20-213-2013
dc.identifier.cristin1038406
dc.source.journalNonlinear processes in geophysics
dc.source.4020
dc.source.pagenumber213-219


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