Stability of gravity-capillary solitary waves on shallow water based on the fifth-order Kadomtsev-Petviashvili equation

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dc.contributor.authorCho, Yeunwooko
dc.date.accessioned2018-08-20T07:48:01Z-
dc.date.available2018-08-20T07:48:01Z-
dc.date.created2018-08-06-
dc.date.created2018-08-06-
dc.date.issued2018-07-
dc.identifier.citationPHYSICAL REVIEW E, v.98, no.1-
dc.identifier.issn2470-0045-
dc.identifier.urihttp://hdl.handle.net/10203/244831-
dc.description.abstractLongitudinal and transverse instabilities of gravity-capillary solitary waves on shallow water are investigated based on the numerical analysis of the fifth-order Kadomtsev-Petviashvili (KP) equation, which describes the wave phenomena on shallow water where the relevant Bond number is less than and close to 1/3. Two-dimensional (2D) depression gravity-capillary solitary waves are stable to longitudinal perturbations. 2D elevation gravity-capillary solitary waves are unstable to longitudinal perturbations and finally evolve into 2D depression gravity-capillary solitary waves. Three-dimensional (3D) finite-amplitude depression gravity-capillary solitary waves are stable to longitudinal perturbations. 3D finite-amplitude elevation gravity-capillary solitary waves are unstable to longitudinal perturbations and finally evolve into an oscillatory state between two different 3D finite-amplitude depression gravity-capillary solitary waves. 3D small-amplitude depression and elevation gravity-capillary solitary waves are unstable to dilation-type longitudinal perturbations and eventually evolve into an oscillatory state between two different 3D finite-amplitude depression gravity-capillary solitary waves. 3D small-amplitude depression and elevation gravity-capillary solitary waves are unstable to contraction-type longitudinal perturbations and eventually become dispersed out toward still water surface. Finally, 2D depression and elevation gravity-capillary solitary waves are unstable to transverse perturbations and eventually evolve into 3D finite-amplitude depression gravity-capillary solitary waves. Therefore, the only stable gravity-capillary solitary waves on shallow water are 3D finite-amplitude depression gravity-capillary solitary waves. In particular, based on the linear stability analysis, a theoretical proof is presented for the long-wave transverse instability of 2D depression and elevation gravity-capillary solitary waves on shallow water.-
dc.languageEnglish-
dc.publisherAMER PHYSICAL SOC-
dc.subjectAPPLIED PRESSURE DISTRIBUTION-
dc.subjectSTEADILY MOVING LOAD-
dc.subjectFREE-SURFACE FLOW-
dc.subjectDEEP-WATER-
dc.subjectTRANSVERSE INSTABILITY-
dc.subjectFLOATING ICE-
dc.subjectTENSION-
dc.subjectGENERATION-
dc.subjectDYNAMICS-
dc.titleStability of gravity-capillary solitary waves on shallow water based on the fifth-order Kadomtsev-Petviashvili equation-
dc.typeArticle-
dc.identifier.wosid000439414800004-
dc.identifier.scopusid2-s2.0-85050494947-
dc.type.rimsART-
dc.citation.volume98-
dc.citation.issue1-
dc.citation.publicationnamePHYSICAL REVIEW E-
dc.identifier.doi10.1103/PhysRevE.98.012213-
dc.contributor.localauthorCho, Yeunwoo-
dc.description.isOpenAccessN-
dc.type.journalArticleArticle-
dc.subject.keywordPlusAPPLIED PRESSURE DISTRIBUTION-
dc.subject.keywordPlusSTEADILY MOVING LOAD-
dc.subject.keywordPlusFREE-SURFACE FLOW-
dc.subject.keywordPlusDEEP-WATER-
dc.subject.keywordPlusTRANSVERSE INSTABILITY-
dc.subject.keywordPlusFLOATING ICE-
dc.subject.keywordPlusTENSION-
dc.subject.keywordPlusGENERATION-
dc.subject.keywordPlusDYNAMICS-
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