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Complementary mild-slope equations in a two-layer fluid
Published in Elsevier B.V.
2011
Volume: 48
   
Issue: 3
Pages: 223 - 234
Abstract
Mild-slope (MS) type equations are depth-integrated models, which predict under appropriate conditions refraction and diffraction of linear time-harmonic water waves. By using a streamfunction formulation instead of a velocity potential one, the complementary mild-slope equation (CMSE) was shown to give better agreement with exact linear theory compared to other MS-type equations. The main goal of this work is to extend the CMSE model for solving two-layer flow with a free-surface. In order to allow for an exact reference, an analytical solution for a two-layer fluid over a sloping plane beach is derived. This analytical solution is used for validating the results of the approximated MS-type models. It is found that the two-layer CMSE model performs better than the potential based one. In addition, the new model is used for investigating the scattering of linear surface water waves and interfacial ones over variable bathymetry. © 2010 Elsevier B.V.
About the journal
JournalData powered by TypesetWave Motion
PublisherData powered by TypesetElsevier B.V.
ISSN01652125
Open AccessNo
Concepts (16)
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    FLUID DYNAMICS
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    Surface waters
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    Surface waves
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    FREE-SURFACE WAVE
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    Interfacial waves
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    MILD SLOPE EQUATIONS
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    Streamfunctions
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    TWO LAYER MODEL
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    Water waves
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    Complementarity
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    Free surface flow
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    INTERNAL WAVE
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    Model validation
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    Numerical model
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    Two-dimensional flow
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    WAVE EQUATION