Wave transformation due to finite floating elastic plate with abrupt change in bottom topography

dc.contributor.authorPraveen, K.M.
dc.contributor.authorVenkateswarlu, V.
dc.contributor.authorKarmakar, D.
dc.date.accessioned2026-02-05T09:26:22Z
dc.date.issued2022
dc.description.abstractThe propagation of surface gravity waves in the presence of finite floating elastic plate over varying sea bottom profile is investigated using the Timoshenko-Mindlin plate theory. The continuity of velocity and pressure at the interfaces along with the continuity of deflection, slope, bending moment and shear force is employed with the support conditions at the plate edges. The numerical computation is performed to obtain the hydroelastic behaviour of the floating elastic plate due to abrupt change in bottom topography. The validation of the present analytical model is performed with the known results available in the literatures. Further, a detailed comparison of the numerical results is presented for different step bottom topography on the hydroelastic characteristics of a floating elastic platform. The present study will provide an insight into the effect of the ocean bottom profile on wave propagation due to the presence of a large floating elastic plate. © 2021 Informa UK Limited, trading as Taylor & Francis Group.
dc.identifier.citationShips and Offshore Structures, 2022, 17, 8, pp. 1824-1842
dc.identifier.issn17445302
dc.identifier.urihttps://doi.org/10.1080/17445302.2021.1946308
dc.identifier.urihttps://idr.nitk.ac.in/handle/123456789/22887
dc.publisherTaylor and Francis Ltd.
dc.subjectComputation theory
dc.subjectGravity waves
dc.subjectHydroelasticity
dc.subjectPlanetary surface analysis
dc.subjectShear flow
dc.subjectTopography
dc.subjectWave propagation
dc.subjectBottom topography
dc.subjectElastic plate
dc.subjectNumerical computations
dc.subjectNumerical results
dc.subjectSea bottom profiles
dc.subjectSupport conditions
dc.subjectSurface gravity waves
dc.subjectWave transformations
dc.subjectMindlin plates
dc.titleWave transformation due to finite floating elastic plate with abrupt change in bottom topography

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