The role of constant vorticity on weakly nonlinear surface gravity waves

Detalhes bibliográficos
Autor(a) principal: Manna, M. A.
Data de Publicação: 2021
Outros Autores: Noubissié, S., Touboul, J., Simon, B., Kraenkel, R. A. [UNESP]
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://dx.doi.org/10.1016/j.wavemoti.2020.102702
http://hdl.handle.net/11449/207138
Resumo: This manuscript describes the derivation of systems of equations for weakly nonlinear gravity waves in shallow water in the presence of constant vorticity. The derivation is based on a multi-layer generalization of the traditional columnar Ansatz. A perturbative development in a nonlinear parameter and a dispersive parameter allow us to obtain sets of equations, for the horizontal fluid velocity and the free surface, able to describe propagation of weakly nonlinear and dispersive surface waves moving in water with some prescribed initial constant vorticity. We have shown that vorticity plays a central role on the dispersive properties of the system. When it is weak, it acts as a correction in linear and nonlinear dispersive terms. When stronger, it can also influence the nondispersive behavior of the system. Explicit steady solutions of the system corresponding to zero, weak, normal or strong vorticity are obtained. They correspond to solitary waves. Evolution of the soliton celerity, amplitude and width for these four cases are discussed.
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spelling The role of constant vorticity on weakly nonlinear surface gravity wavesThis manuscript describes the derivation of systems of equations for weakly nonlinear gravity waves in shallow water in the presence of constant vorticity. The derivation is based on a multi-layer generalization of the traditional columnar Ansatz. A perturbative development in a nonlinear parameter and a dispersive parameter allow us to obtain sets of equations, for the horizontal fluid velocity and the free surface, able to describe propagation of weakly nonlinear and dispersive surface waves moving in water with some prescribed initial constant vorticity. We have shown that vorticity plays a central role on the dispersive properties of the system. When it is weak, it acts as a correction in linear and nonlinear dispersive terms. When stronger, it can also influence the nondispersive behavior of the system. Explicit steady solutions of the system corresponding to zero, weak, normal or strong vorticity are obtained. They correspond to solitary waves. Evolution of the soliton celerity, amplitude and width for these four cases are discussed.Délégation Générale pour l'ArmementFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)Agence Nationale de la RechercheLaboratoire Charles Coulomb (L2C) Univ. Montpellier CNRSInstitute of Technology University of Dschang, P.O. Box 134Université de Toulon Aix Marseille Univ. CNRS IRD MIOInstituto de Física Téorica-UNESP Universidade Estadual Paulista, Rua Dr. Bento Teobaldo Ferraz 271 Bloco IIInstituto de Física Téorica-UNESP Universidade Estadual Paulista, Rua Dr. Bento Teobaldo Ferraz 271 Bloco IIAgence Nationale de la Recherche: 13-ASTR-0007CNRSUniversity of DschangMIOUniversidade Estadual Paulista (Unesp)Manna, M. A.Noubissié, S.Touboul, J.Simon, B.Kraenkel, R. A. [UNESP]2021-06-25T10:49:35Z2021-06-25T10:49:35Z2021-04-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://dx.doi.org/10.1016/j.wavemoti.2020.102702Wave Motion, v. 102.0165-2125http://hdl.handle.net/11449/20713810.1016/j.wavemoti.2020.1027022-s2.0-85099379803Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengWave Motioninfo:eu-repo/semantics/openAccess2021-10-23T16:16:11Zoai:repositorio.unesp.br:11449/207138Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T22:09:07.619414Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv The role of constant vorticity on weakly nonlinear surface gravity waves
title The role of constant vorticity on weakly nonlinear surface gravity waves
spellingShingle The role of constant vorticity on weakly nonlinear surface gravity waves
Manna, M. A.
title_short The role of constant vorticity on weakly nonlinear surface gravity waves
title_full The role of constant vorticity on weakly nonlinear surface gravity waves
title_fullStr The role of constant vorticity on weakly nonlinear surface gravity waves
title_full_unstemmed The role of constant vorticity on weakly nonlinear surface gravity waves
title_sort The role of constant vorticity on weakly nonlinear surface gravity waves
author Manna, M. A.
author_facet Manna, M. A.
Noubissié, S.
Touboul, J.
Simon, B.
Kraenkel, R. A. [UNESP]
author_role author
author2 Noubissié, S.
Touboul, J.
Simon, B.
Kraenkel, R. A. [UNESP]
author2_role author
author
author
author
dc.contributor.none.fl_str_mv CNRS
University of Dschang
MIO
Universidade Estadual Paulista (Unesp)
dc.contributor.author.fl_str_mv Manna, M. A.
Noubissié, S.
Touboul, J.
Simon, B.
Kraenkel, R. A. [UNESP]
description This manuscript describes the derivation of systems of equations for weakly nonlinear gravity waves in shallow water in the presence of constant vorticity. The derivation is based on a multi-layer generalization of the traditional columnar Ansatz. A perturbative development in a nonlinear parameter and a dispersive parameter allow us to obtain sets of equations, for the horizontal fluid velocity and the free surface, able to describe propagation of weakly nonlinear and dispersive surface waves moving in water with some prescribed initial constant vorticity. We have shown that vorticity plays a central role on the dispersive properties of the system. When it is weak, it acts as a correction in linear and nonlinear dispersive terms. When stronger, it can also influence the nondispersive behavior of the system. Explicit steady solutions of the system corresponding to zero, weak, normal or strong vorticity are obtained. They correspond to solitary waves. Evolution of the soliton celerity, amplitude and width for these four cases are discussed.
publishDate 2021
dc.date.none.fl_str_mv 2021-06-25T10:49:35Z
2021-06-25T10:49:35Z
2021-04-01
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://dx.doi.org/10.1016/j.wavemoti.2020.102702
Wave Motion, v. 102.
0165-2125
http://hdl.handle.net/11449/207138
10.1016/j.wavemoti.2020.102702
2-s2.0-85099379803
url http://dx.doi.org/10.1016/j.wavemoti.2020.102702
http://hdl.handle.net/11449/207138
identifier_str_mv Wave Motion, v. 102.
0165-2125
10.1016/j.wavemoti.2020.102702
2-s2.0-85099379803
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Wave Motion
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.source.none.fl_str_mv Scopus
reponame:Repositório Institucional da UNESP
instname:Universidade Estadual Paulista (UNESP)
instacron:UNESP
instname_str Universidade Estadual Paulista (UNESP)
instacron_str UNESP
institution UNESP
reponame_str Repositório Institucional da UNESP
collection Repositório Institucional da UNESP
repository.name.fl_str_mv Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)
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