Edge capillary-gravity waves on a sloping beach

dc.contributorMuzylev, S.V., P.P. Shirshov Inst. of Oceanology, Moscow, Russian Federation, University of Guadalajara, Guadalajara, Mexico; Bulgakov, S.N., Physics Department, Institute of Astronomy/Meteorology, University of Guadalajara, Guadalajara, Mexico; Duran-Matute, M., Physics Department, University of Guadalajara, Guadalajara, Mexico
dc.creatorMuzylev, S.V.
dc.creatorBulgakov, S.N.
dc.creatorDuran-Matute, M.
dc.date.accessioned2015-11-19T18:49:11Z
dc.date.accessioned2023-07-04T01:25:10Z
dc.date.available2015-11-19T18:49:11Z
dc.date.available2023-07-04T01:25:10Z
dc.date.created2015-11-19T18:49:11Z
dc.date.issued2005
dc.identifierhttp://hdl.handle.net/20.500.12104/64237
dc.identifier10.1063/1.1879052
dc.identifierhttp://www.scopus.com/inward/record.url?eid=2-s2.0-17444412708&partnerID=40&md5=89908539c7739771c6ee167d8a935d22
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/7257666
dc.description.abstractIt is shown how the solution for velocity potential may be determined when the effect of surface tension is included in the linearized theory of Ursell-type edge waves over a plane-sloping beach. The problem is examined without making a hydrostatic assumption. Explicit solutions for edge capillary-gravity waves are given and the dispersion equation is obtained. The influence of capillarity on gravity waves is discussed. © 2005 American Institute of Physics.
dc.relationPhysics of Fluids
dc.relation17
dc.relation4
dc.relation48103
dc.relation1-048103-4
dc.relationScopus
dc.titleEdge capillary-gravity waves on a sloping beach
dc.typeArticle


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