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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/2518
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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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13.13397 |