Green-Naghdi dynamics of surface wind waves in finite depth
Autor(a) principal: | |
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Data de Publicação: | 2018 |
Outros Autores: | , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional da UNESP |
Texto Completo: | http://dx.doi.org/10.1088/1873-7005/aaa739 http://hdl.handle.net/11449/176140 |
Resumo: | The Miles' quasi laminar theory of waves generation by wind in finite depth h is presented. In this context, the fully nonlinear Green-Naghdi model equation is derived for the first time. This model equation is obtained by the non perturbative Green-Naghdi approach, coupling a nonlinear evolution of water waves with the atmospheric dynamics which works as in the classic Miles' theory. A depth-dependent and wind-dependent wave growth γ is drawn from the dispersion relation of the coupled Green-Naghdi model with the atmospheric dynamics. Different values of the dimensionless water depth parameter δ = gh/U 1, with g the gravity and U 1 a characteristic wind velocity, produce two families of growth rate γ in function of the dimensionless theoretical wave-age c 0: a family of γ with h constant and U 1 variable and another family of γ with U 1 constant and h variable. The allowed minimum and maximum values of γ in this model are exhibited. |
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Green-Naghdi dynamics of surface wind waves in finite depthMiles mechanismnonlinear Green-Nagdhi modelsurface waveswaves in finite depthwind-wavesThe Miles' quasi laminar theory of waves generation by wind in finite depth h is presented. In this context, the fully nonlinear Green-Naghdi model equation is derived for the first time. This model equation is obtained by the non perturbative Green-Naghdi approach, coupling a nonlinear evolution of water waves with the atmospheric dynamics which works as in the classic Miles' theory. A depth-dependent and wind-dependent wave growth γ is drawn from the dispersion relation of the coupled Green-Naghdi model with the atmospheric dynamics. Different values of the dimensionless water depth parameter δ = gh/U 1, with g the gravity and U 1 a characteristic wind velocity, produce two families of growth rate γ in function of the dimensionless theoretical wave-age c 0: a family of γ with h constant and U 1 variable and another family of γ with U 1 constant and h variable. The allowed minimum and maximum values of γ in this model are exhibited.Université de Montpellier (UM) Conseil National de la Recherche Scientifique (CNRS) Laboratoire Charles Coulomb UMR 5221Department of Physics Faculty of Sciences Qom University of TechnologyInstituto de Física Téorica UNESP - Universidade Estadual Paulista, Rua Dr. Bento Teobaldo Ferraz 27, Bloco IIInstituto de Física Téorica UNESP - Universidade Estadual Paulista, Rua Dr. Bento Teobaldo Ferraz 27, Bloco IILaboratoire Charles Coulomb UMR 5221Qom University of TechnologyUniversidade Estadual Paulista (Unesp)Manna, M. A.Latifi, A.Kraenkel, R. A. [UNESP]2018-12-11T17:19:13Z2018-12-11T17:19:13Z2018-02-08info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://dx.doi.org/10.1088/1873-7005/aaa739Fluid Dynamics Research, v. 50, n. 2, 2018.0169-5983http://hdl.handle.net/11449/17614010.1088/1873-7005/aaa7392-s2.0-850449770192-s2.0-85044977019.pdfScopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengFluid Dynamics Research0,476info:eu-repo/semantics/openAccess2023-11-24T06:18:24Zoai:repositorio.unesp.br:11449/176140Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T18:38:41.861741Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false |
dc.title.none.fl_str_mv |
Green-Naghdi dynamics of surface wind waves in finite depth |
title |
Green-Naghdi dynamics of surface wind waves in finite depth |
spellingShingle |
Green-Naghdi dynamics of surface wind waves in finite depth Manna, M. A. Miles mechanism nonlinear Green-Nagdhi model surface waves waves in finite depth wind-waves |
title_short |
Green-Naghdi dynamics of surface wind waves in finite depth |
title_full |
Green-Naghdi dynamics of surface wind waves in finite depth |
title_fullStr |
Green-Naghdi dynamics of surface wind waves in finite depth |
title_full_unstemmed |
Green-Naghdi dynamics of surface wind waves in finite depth |
title_sort |
Green-Naghdi dynamics of surface wind waves in finite depth |
author |
Manna, M. A. |
author_facet |
Manna, M. A. Latifi, A. Kraenkel, R. A. [UNESP] |
author_role |
author |
author2 |
Latifi, A. Kraenkel, R. A. [UNESP] |
author2_role |
author author |
dc.contributor.none.fl_str_mv |
Laboratoire Charles Coulomb UMR 5221 Qom University of Technology Universidade Estadual Paulista (Unesp) |
dc.contributor.author.fl_str_mv |
Manna, M. A. Latifi, A. Kraenkel, R. A. [UNESP] |
dc.subject.por.fl_str_mv |
Miles mechanism nonlinear Green-Nagdhi model surface waves waves in finite depth wind-waves |
topic |
Miles mechanism nonlinear Green-Nagdhi model surface waves waves in finite depth wind-waves |
description |
The Miles' quasi laminar theory of waves generation by wind in finite depth h is presented. In this context, the fully nonlinear Green-Naghdi model equation is derived for the first time. This model equation is obtained by the non perturbative Green-Naghdi approach, coupling a nonlinear evolution of water waves with the atmospheric dynamics which works as in the classic Miles' theory. A depth-dependent and wind-dependent wave growth γ is drawn from the dispersion relation of the coupled Green-Naghdi model with the atmospheric dynamics. Different values of the dimensionless water depth parameter δ = gh/U 1, with g the gravity and U 1 a characteristic wind velocity, produce two families of growth rate γ in function of the dimensionless theoretical wave-age c 0: a family of γ with h constant and U 1 variable and another family of γ with U 1 constant and h variable. The allowed minimum and maximum values of γ in this model are exhibited. |
publishDate |
2018 |
dc.date.none.fl_str_mv |
2018-12-11T17:19:13Z 2018-12-11T17:19:13Z 2018-02-08 |
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/10.1088/1873-7005/aaa739 Fluid Dynamics Research, v. 50, n. 2, 2018. 0169-5983 http://hdl.handle.net/11449/176140 10.1088/1873-7005/aaa739 2-s2.0-85044977019 2-s2.0-85044977019.pdf |
url |
http://dx.doi.org/10.1088/1873-7005/aaa739 http://hdl.handle.net/11449/176140 |
identifier_str_mv |
Fluid Dynamics Research, v. 50, n. 2, 2018. 0169-5983 10.1088/1873-7005/aaa739 2-s2.0-85044977019 2-s2.0-85044977019.pdf |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
Fluid Dynamics Research 0,476 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
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) |
repository.mail.fl_str_mv |
|
_version_ |
1808128959033901056 |