A weakly nonlinear coupled-mode model for wave-current-seabed interaction over general bottom topography

A weakly nonlinear, coupled-mode model is developed for the wave-current-seabed interaction problem, with application to wave scattering by steady currents over general bottom topography. Based on previous work by the authors (Athanassoulis & Belibassakis [1], Belibassakis et al [2]), the vertic...

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Main Authors: Belibassakis, KA, Gerostathis, ThP, Athanassoulis, GA
Format: Conference Object
Language:unknown
Published: 2008
Subjects:
Online Access:http://dspace.lib.ntua.gr/handle/123456789/35546
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spelling ftntunivathens:oai:dspace.lib.ntua.gr:123456789/35546 2023-05-15T14:20:54+02:00 A weakly nonlinear coupled-mode model for wave-current-seabed interaction over general bottom topography Belibassakis, KA Gerostathis, ThP Athanassoulis, GA 2008 http://dspace.lib.ntua.gr/handle/123456789/35546 unknown info:eu-repo/semantics/openAccess free Proceedings of the International Conference on Offshore Mechanics and Arctic Engineering - OMAE Analytical structure Bottom boundary conditions Bottom topography Coupled systems Evanescent mode Finite difference scheme Horizontal planes Nonlinear waves Numerical results One-equation model Propagating mode Scattered waves Seabed interaction Second orders Steady current Test case Variational principles Vertical distributions Vertical modes Wave current interaction Wave potentials Wave scattering Arctic engineering Boundary conditions Mechanics Ocean engineering Topography Variational techniques Wave propagation Wave equations info:eu-repo/semantics/conferenceObject 2008 ftntunivathens 2019-07-13T16:33:39Z A weakly nonlinear, coupled-mode model is developed for the wave-current-seabed interaction problem, with application to wave scattering by steady currents over general bottom topography. Based on previous work by the authors (Athanassoulis & Belibassakis [1], Belibassakis et al [2]), the vertical distribution of the scattered wave potential is represented by a series of local vertical modes containing the propagating mode and all evanescent modes, plus an additional term accounting for the bottom boundary condition when the bottom slope is not negligible. Using the above representation, in conjunction with Luke's [3] variational principle, the wave-current-seabed interaction problem is reduced to a coupled system of differential equations on the horizontal plane. If only the propagating mode is retained in the vertical expansion of the wave potential, and after simplifications, the present system is reduced to an one-equation model compatible with Kirby's [4] mild-slope model with application to the problem of wave-current interaction over slowly varying topography. The present coupled-mode system is discretized on the horizontal plane by using a second-order finite difference scheme and numerically solved by iterations. Numerical results are presented for two representative test cases, demonstrating the importance of the first evanescent modes and the sloping-bottom mode. The analytical structure of the present model facilitates its extension to treat fully non-linear waves, and it can be further elaborated to study wave propagation over random bottom topography and general currents. Copyright © 2008 by ASME. Conference Object Arctic Arctic National Technical University of Athens (NTUA): DSpace Arctic
institution Open Polar
collection National Technical University of Athens (NTUA): DSpace
op_collection_id ftntunivathens
language unknown
topic Analytical structure
Bottom boundary conditions
Bottom topography
Coupled systems
Evanescent mode
Finite difference scheme
Horizontal planes
Nonlinear waves
Numerical results
One-equation model
Propagating mode
Scattered waves
Seabed interaction
Second orders
Steady current
Test case
Variational principles
Vertical distributions
Vertical modes
Wave current interaction
Wave potentials
Wave scattering
Arctic engineering
Boundary conditions
Mechanics
Ocean engineering
Topography
Variational techniques
Wave propagation
Wave equations
spellingShingle Analytical structure
Bottom boundary conditions
Bottom topography
Coupled systems
Evanescent mode
Finite difference scheme
Horizontal planes
Nonlinear waves
Numerical results
One-equation model
Propagating mode
Scattered waves
Seabed interaction
Second orders
Steady current
Test case
Variational principles
Vertical distributions
Vertical modes
Wave current interaction
Wave potentials
Wave scattering
Arctic engineering
Boundary conditions
Mechanics
Ocean engineering
Topography
Variational techniques
Wave propagation
Wave equations
Belibassakis, KA
Gerostathis, ThP
Athanassoulis, GA
A weakly nonlinear coupled-mode model for wave-current-seabed interaction over general bottom topography
topic_facet Analytical structure
Bottom boundary conditions
Bottom topography
Coupled systems
Evanescent mode
Finite difference scheme
Horizontal planes
Nonlinear waves
Numerical results
One-equation model
Propagating mode
Scattered waves
Seabed interaction
Second orders
Steady current
Test case
Variational principles
Vertical distributions
Vertical modes
Wave current interaction
Wave potentials
Wave scattering
Arctic engineering
Boundary conditions
Mechanics
Ocean engineering
Topography
Variational techniques
Wave propagation
Wave equations
description A weakly nonlinear, coupled-mode model is developed for the wave-current-seabed interaction problem, with application to wave scattering by steady currents over general bottom topography. Based on previous work by the authors (Athanassoulis & Belibassakis [1], Belibassakis et al [2]), the vertical distribution of the scattered wave potential is represented by a series of local vertical modes containing the propagating mode and all evanescent modes, plus an additional term accounting for the bottom boundary condition when the bottom slope is not negligible. Using the above representation, in conjunction with Luke's [3] variational principle, the wave-current-seabed interaction problem is reduced to a coupled system of differential equations on the horizontal plane. If only the propagating mode is retained in the vertical expansion of the wave potential, and after simplifications, the present system is reduced to an one-equation model compatible with Kirby's [4] mild-slope model with application to the problem of wave-current interaction over slowly varying topography. The present coupled-mode system is discretized on the horizontal plane by using a second-order finite difference scheme and numerically solved by iterations. Numerical results are presented for two representative test cases, demonstrating the importance of the first evanescent modes and the sloping-bottom mode. The analytical structure of the present model facilitates its extension to treat fully non-linear waves, and it can be further elaborated to study wave propagation over random bottom topography and general currents. Copyright © 2008 by ASME.
format Conference Object
author Belibassakis, KA
Gerostathis, ThP
Athanassoulis, GA
author_facet Belibassakis, KA
Gerostathis, ThP
Athanassoulis, GA
author_sort Belibassakis, KA
title A weakly nonlinear coupled-mode model for wave-current-seabed interaction over general bottom topography
title_short A weakly nonlinear coupled-mode model for wave-current-seabed interaction over general bottom topography
title_full A weakly nonlinear coupled-mode model for wave-current-seabed interaction over general bottom topography
title_fullStr A weakly nonlinear coupled-mode model for wave-current-seabed interaction over general bottom topography
title_full_unstemmed A weakly nonlinear coupled-mode model for wave-current-seabed interaction over general bottom topography
title_sort weakly nonlinear coupled-mode model for wave-current-seabed interaction over general bottom topography
publishDate 2008
url http://dspace.lib.ntua.gr/handle/123456789/35546
geographic Arctic
geographic_facet Arctic
genre Arctic
Arctic
genre_facet Arctic
Arctic
op_source Proceedings of the International Conference on Offshore Mechanics and Arctic Engineering - OMAE
op_rights info:eu-repo/semantics/openAccess
free
_version_ 1766293375617597440