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dc.contributor.authorShenoi, S.S.C.
dc.contributor.authorMurty, C.S.
dc.date.accessioned1995-06-13T10:01:20Z
dc.date.accessioned2017-09-29T13:48:23Z
dc.date.available1995-06-13T10:01:20Z
dc.date.available2017-09-29T13:48:23Z
dc.date.issued1986
dc.identifier.citationIndian Journal of Marine Sciences, vol.15; 1986; 78-83
dc.identifier.issn0379-5136
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6277
dc.description.abstractAnalysis of wave damping in mud bank region following the process of transfer of wave energy to the interior of fluid column through the boundary layer and the energy loss computations owing to viscous shear beneath the solitary wave over a smooth horizontal surface are presented It is shown that waves can almost or completely be dissipated over a mud bank of width about 3 - 4 km when the kinematic viscosity increases to 1 cm2 sec -1 Waves of higher amplitude are dissipated much faster than those of lower amplitude
dc.languageen
dc.publisherCSIR-NISCAIR
dc.relation.ispartofIndian J Mar Sci
dc.relation.isreferencedbySCI
dc.subjectOceanography and Limnology
dc.subject.otherenergy transfer
dc.subject.otherwave energy
dc.subject.othermud banks
dc.subject.othersolitary waves
dc.subject.otherwave damping
dc.subject.otherISW, India, Kerala
dc.titleViscous damping of solitary waves in the mud banks of Kerala, West coast of India
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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