Inverse cascades in turbulence and the case of rotating flows

Autores
Pouquet, A.; Sen, A.; Rosenberg, D.; Mininni, Pablo Daniel; Baerenzung, J.
Año de publicación
2013
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
We first summarize briefly several properties concerning the dynamics of two-dimensional (2D) turbulence, with an emphasis on the inverse cascade of energy to the largest accessible scale of the system. In order to study a similar phenomenon in 3D turbulence undergoing strong solid-body rotation, we test a previously developed large eddy simulation (LES) model against a high-resolution direct numerical simulation of rotating turbulence on a grid of 30723 points. We then describe new numerical results on the inverse energy cascade in rotating flows using this LES model and contrast the case of 2D versus 3D forcing, as well as non-helical forcing (i.e. with weak overall alignment between velocity and vorticity) versus the fully helical Beltrami case, for both deterministic and random forcing. The different scaling laws for the inverse energy cascade can be attributed to the dimensionality of the forcing, with either a k −3 ⊥ or a k −5/3 ⊥ energy spectrum of slow modes at large scales, k⊥ referring to a direction perpendicular to that of rotation. We finally invoke the role of shear in the case of a strongly anisotropic deterministic forcing, using the so-called ABC flow; in that case, a k −5/3 ⊥ is again observed for the slow modes, together with a k −1 spectrum for the total energy associated with enhanced shear at a large scale
Fil: Pouquet, A.. National Center for Atmospheric Research; Estados Unidos
Fil: Sen, A.. National Center for Atmospheric Research; Estados Unidos
Fil: Rosenberg, D.. National Center for Atmospheric Research; Estados Unidos
Fil: Mininni, Pablo Daniel. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Física de Buenos Aires; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Física; Argentina
Fil: Baerenzung, J.. No especifíca;
Materia
Rotating Flows
Swirling Flows
Inverse Cascade
Self Organization
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/2518

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network_name_str CONICET Digital (CONICET)
spelling Inverse cascades in turbulence and the case of rotating flowsPouquet, A.Sen, A.Rosenberg, D.Mininni, Pablo DanielBaerenzung, J.Rotating FlowsSwirling FlowsInverse CascadeSelf Organizationhttps://purl.org/becyt/ford/1.3https://purl.org/becyt/ford/1We first summarize briefly several properties concerning the dynamics of two-dimensional (2D) turbulence, with an emphasis on the inverse cascade of energy to the largest accessible scale of the system. In order to study a similar phenomenon in 3D turbulence undergoing strong solid-body rotation, we test a previously developed large eddy simulation (LES) model against a high-resolution direct numerical simulation of rotating turbulence on a grid of 30723 points. We then describe new numerical results on the inverse energy cascade in rotating flows using this LES model and contrast the case of 2D versus 3D forcing, as well as non-helical forcing (i.e. with weak overall alignment between velocity and vorticity) versus the fully helical Beltrami case, for both deterministic and random forcing. The different scaling laws for the inverse energy cascade can be attributed to the dimensionality of the forcing, with either a k −3 ⊥ or a k −5/3 ⊥ energy spectrum of slow modes at large scales, k⊥ referring to a direction perpendicular to that of rotation. We finally invoke the role of shear in the case of a strongly anisotropic deterministic forcing, using the so-called ABC flow; in that case, a k −5/3 ⊥ is again observed for the slow modes, together with a k −1 spectrum for the total energy associated with enhanced shear at a large scaleFil: Pouquet, A.. National Center for Atmospheric Research; Estados UnidosFil: Sen, A.. National Center for Atmospheric Research; Estados UnidosFil: Rosenberg, D.. National Center for Atmospheric Research; Estados UnidosFil: Mininni, Pablo Daniel. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Física de Buenos Aires; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Física; ArgentinaFil: Baerenzung, J.. No especifíca;IOP Publishing2013-07-16info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/2518Pouquet, A.; Sen, A.; Rosenberg, D.; Mininni, Pablo Daniel; Baerenzung, J.; Inverse cascades in turbulence and the case of rotating flows; IOP Publishing; Physica Scripta; 88; T155; 16-7-2013; 1-110031-8949enginfo:eu-repo/semantics/altIdentifier/doi/10.1088/0031-8949/2013/T155/014032info:eu-repo/semantics/altIdentifier/url/http://arxiv.org/abs/1203.0337info:eu-repo/semantics/altIdentifier/url/http://iopscience.iop.org/1402-4896/2013/T155/014032/info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:08:00Zoai:ri.conicet.gov.ar:11336/2518instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 10:08:00.438CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Inverse cascades in turbulence and the case of rotating flows
title Inverse cascades in turbulence and the case of rotating flows
spellingShingle Inverse cascades in turbulence and the case of rotating flows
Pouquet, A.
Rotating Flows
Swirling Flows
Inverse Cascade
Self Organization
title_short Inverse cascades in turbulence and the case of rotating flows
title_full Inverse cascades in turbulence and the case of rotating flows
title_fullStr Inverse cascades in turbulence and the case of rotating flows
title_full_unstemmed Inverse cascades in turbulence and the case of rotating flows
title_sort Inverse cascades in turbulence and the case of rotating flows
dc.creator.none.fl_str_mv Pouquet, A.
Sen, A.
Rosenberg, D.
Mininni, Pablo Daniel
Baerenzung, J.
author Pouquet, A.
author_facet Pouquet, A.
Sen, A.
Rosenberg, D.
Mininni, Pablo Daniel
Baerenzung, J.
author_role author
author2 Sen, A.
Rosenberg, D.
Mininni, Pablo Daniel
Baerenzung, J.
author2_role author
author
author
author
dc.subject.none.fl_str_mv Rotating Flows
Swirling Flows
Inverse Cascade
Self Organization
topic Rotating Flows
Swirling Flows
Inverse Cascade
Self Organization
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.3
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv We first summarize briefly several properties concerning the dynamics of two-dimensional (2D) turbulence, with an emphasis on the inverse cascade of energy to the largest accessible scale of the system. In order to study a similar phenomenon in 3D turbulence undergoing strong solid-body rotation, we test a previously developed large eddy simulation (LES) model against a high-resolution direct numerical simulation of rotating turbulence on a grid of 30723 points. We then describe new numerical results on the inverse energy cascade in rotating flows using this LES model and contrast the case of 2D versus 3D forcing, as well as non-helical forcing (i.e. with weak overall alignment between velocity and vorticity) versus the fully helical Beltrami case, for both deterministic and random forcing. The different scaling laws for the inverse energy cascade can be attributed to the dimensionality of the forcing, with either a k −3 ⊥ or a k −5/3 ⊥ energy spectrum of slow modes at large scales, k⊥ referring to a direction perpendicular to that of rotation. We finally invoke the role of shear in the case of a strongly anisotropic deterministic forcing, using the so-called ABC flow; in that case, a k −5/3 ⊥ is again observed for the slow modes, together with a k −1 spectrum for the total energy associated with enhanced shear at a large scale
Fil: Pouquet, A.. National Center for Atmospheric Research; Estados Unidos
Fil: Sen, A.. National Center for Atmospheric Research; Estados Unidos
Fil: Rosenberg, D.. National Center for Atmospheric Research; Estados Unidos
Fil: Mininni, Pablo Daniel. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Física de Buenos Aires; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Física; Argentina
Fil: Baerenzung, J.. No especifíca;
description We first summarize briefly several properties concerning the dynamics of two-dimensional (2D) turbulence, with an emphasis on the inverse cascade of energy to the largest accessible scale of the system. In order to study a similar phenomenon in 3D turbulence undergoing strong solid-body rotation, we test a previously developed large eddy simulation (LES) model against a high-resolution direct numerical simulation of rotating turbulence on a grid of 30723 points. We then describe new numerical results on the inverse energy cascade in rotating flows using this LES model and contrast the case of 2D versus 3D forcing, as well as non-helical forcing (i.e. with weak overall alignment between velocity and vorticity) versus the fully helical Beltrami case, for both deterministic and random forcing. The different scaling laws for the inverse energy cascade can be attributed to the dimensionality of the forcing, with either a k −3 ⊥ or a k −5/3 ⊥ energy spectrum of slow modes at large scales, k⊥ referring to a direction perpendicular to that of rotation. We finally invoke the role of shear in the case of a strongly anisotropic deterministic forcing, using the so-called ABC flow; in that case, a k −5/3 ⊥ is again observed for the slow modes, together with a k −1 spectrum for the total energy associated with enhanced shear at a large scale
publishDate 2013
dc.date.none.fl_str_mv 2013-07-16
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/2518
Pouquet, A.; Sen, A.; Rosenberg, D.; Mininni, Pablo Daniel; Baerenzung, J.; Inverse cascades in turbulence and the case of rotating flows; IOP Publishing; Physica Scripta; 88; T155; 16-7-2013; 1-11
0031-8949
url http://hdl.handle.net/11336/2518
identifier_str_mv Pouquet, A.; Sen, A.; Rosenberg, D.; Mininni, Pablo Daniel; Baerenzung, J.; Inverse cascades in turbulence and the case of rotating flows; IOP Publishing; Physica Scripta; 88; T155; 16-7-2013; 1-11
0031-8949
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1088/0031-8949/2013/T155/014032
info:eu-repo/semantics/altIdentifier/url/http://arxiv.org/abs/1203.0337
info:eu-repo/semantics/altIdentifier/url/http://iopscience.iop.org/1402-4896/2013/T155/014032/
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv IOP Publishing
publisher.none.fl_str_mv IOP Publishing
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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