Evaluation of nonlinear numerical model performance on the wave propagation over a bar-trough profile beach

Detalhes bibliográficos
Autor(a) principal: Okamoto, T.
Data de Publicação: 2009
Outros Autores: Fortes, C. J. E. M., Neves, M. G.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://repositorio.lnec.pt:8080/jspui/handle/123456789/17319
Resumo: Knowing the vertical structure of particle velocity is very important for the sediment transportation study. Recent development of computer resources and high performance computing enable us to use numerical models with more information in the vertical direction. In this paper, the performance of multi-layered Boussinesq model (COULWAVE) and RANS model (COBRAS-UC) on a bar-trough profile beach is examined. Results, in terms of wave heights computed by both models and the time series of the horizontal velocity (computed with COBRAS-UC model) are compared with the experimental data collected by Okamoto et al. (2008) for the test case with an incident wave of period T=1.5sec and height of H=8cm, in which the detailed vertical structure of particle velocity was measured. Both models can predict the wave height change very well until the wave breaking initiates and specially COBRAS-UC model. However, it does not agree to the experimental data after the wave breaking initiation. The COBRAS-UC model calculates the horizontal velocity near the free surface very well, but it does not agree to the experimental data in the lower section of the water column.
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spelling Evaluation of nonlinear numerical model performance on the wave propagation over a bar-trough profile beachWave breakingBoussinesq type modelsRans modelExperimental workKnowing the vertical structure of particle velocity is very important for the sediment transportation study. Recent development of computer resources and high performance computing enable us to use numerical models with more information in the vertical direction. In this paper, the performance of multi-layered Boussinesq model (COULWAVE) and RANS model (COBRAS-UC) on a bar-trough profile beach is examined. Results, in terms of wave heights computed by both models and the time series of the horizontal velocity (computed with COBRAS-UC model) are compared with the experimental data collected by Okamoto et al. (2008) for the test case with an incident wave of period T=1.5sec and height of H=8cm, in which the detailed vertical structure of particle velocity was measured. Both models can predict the wave height change very well until the wave breaking initiates and specially COBRAS-UC model. However, it does not agree to the experimental data after the wave breaking initiation. The COBRAS-UC model calculates the horizontal velocity near the free surface very well, but it does not agree to the experimental data in the lower section of the water column.2009-11-20T10:47:42Z2010-04-26T10:17:08Z2014-10-20T13:38:47Z2017-04-12T13:41:18Z2009-04-01T00:00:00Z2009-04info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://repositorio.lnec.pt:8080/jspui/handle/123456789/17319engOkamoto, T.Fortes, C. J. E. M.Neves, M. G.info:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2024-01-13T03:02:04Zoai:localhost:123456789/17319Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-20T01:38:22.378320Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv Evaluation of nonlinear numerical model performance on the wave propagation over a bar-trough profile beach
title Evaluation of nonlinear numerical model performance on the wave propagation over a bar-trough profile beach
spellingShingle Evaluation of nonlinear numerical model performance on the wave propagation over a bar-trough profile beach
Okamoto, T.
Wave breaking
Boussinesq type models
Rans model
Experimental work
title_short Evaluation of nonlinear numerical model performance on the wave propagation over a bar-trough profile beach
title_full Evaluation of nonlinear numerical model performance on the wave propagation over a bar-trough profile beach
title_fullStr Evaluation of nonlinear numerical model performance on the wave propagation over a bar-trough profile beach
title_full_unstemmed Evaluation of nonlinear numerical model performance on the wave propagation over a bar-trough profile beach
title_sort Evaluation of nonlinear numerical model performance on the wave propagation over a bar-trough profile beach
author Okamoto, T.
author_facet Okamoto, T.
Fortes, C. J. E. M.
Neves, M. G.
author_role author
author2 Fortes, C. J. E. M.
Neves, M. G.
author2_role author
author
dc.contributor.author.fl_str_mv Okamoto, T.
Fortes, C. J. E. M.
Neves, M. G.
dc.subject.por.fl_str_mv Wave breaking
Boussinesq type models
Rans model
Experimental work
topic Wave breaking
Boussinesq type models
Rans model
Experimental work
description Knowing the vertical structure of particle velocity is very important for the sediment transportation study. Recent development of computer resources and high performance computing enable us to use numerical models with more information in the vertical direction. In this paper, the performance of multi-layered Boussinesq model (COULWAVE) and RANS model (COBRAS-UC) on a bar-trough profile beach is examined. Results, in terms of wave heights computed by both models and the time series of the horizontal velocity (computed with COBRAS-UC model) are compared with the experimental data collected by Okamoto et al. (2008) for the test case with an incident wave of period T=1.5sec and height of H=8cm, in which the detailed vertical structure of particle velocity was measured. Both models can predict the wave height change very well until the wave breaking initiates and specially COBRAS-UC model. However, it does not agree to the experimental data after the wave breaking initiation. The COBRAS-UC model calculates the horizontal velocity near the free surface very well, but it does not agree to the experimental data in the lower section of the water column.
publishDate 2009
dc.date.none.fl_str_mv 2009-11-20T10:47:42Z
2009-04-01T00:00:00Z
2009-04
2010-04-26T10:17:08Z
2014-10-20T13:38:47Z
2017-04-12T13:41:18Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
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dc.language.iso.fl_str_mv eng
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