Vortices in rotating and stratified flows: aspect ratio and sustainability

In linear stratifications, vortices have a typical flat shape that appears to be not only a compromise between the rotation and the stratification of the background flow through their Coriolis parameter f and buoyancy frequency hbox{$ar{N}$} N̅ , but also involves the buoyancy frequency Nc wit...

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Main Authors: Le Gal P., Le Bars M., Aubert O., Marcus P. S.
Format: Article
Language:English
Published: EDP Sciences 2013-04-01
Series:EPJ Web of Conferences
Online Access:http://dx.doi.org/10.1051/epjconf/20134605004
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author Le Gal P.
Le Bars M.
Aubert O.
Marcus P. S.
author_facet Le Gal P.
Le Bars M.
Aubert O.
Marcus P. S.
author_sort Le Gal P.
collection DOAJ
description In linear stratifications, vortices have a typical flat shape that appears to be not only a compromise between the rotation and the stratification of the background flow through their Coriolis parameter f and buoyancy frequency hbox{$ar{N}$} N̅ , but also involves the buoyancy frequency Nc within the vortices and their Rossby number Ro. We derive an analytical solution for the self-similar ellipsoidal shape of the vortices and the law for their aspect ratio. From this law, we show that long-lived vortices must necessary be either weakly stratified anticyclones or superstratified cyclones (which is less likely to occur). These predictions are experimentally and numerically verified and agree with published measurements for Jovian vortices and ocean meddies. This approach can be applied to a gaussian stratification to give good insights of the shape of vortices in protoplanetary disks and their sustainability.
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spelling doaj.art-93d754d53b3546dba1d705461c86f7182022-12-21T23:20:05ZengEDP SciencesEPJ Web of Conferences2100-014X2013-04-01460500410.1051/epjconf/20134605004Vortices in rotating and stratified flows: aspect ratio and sustainabilityLe Gal P.Le Bars M.Aubert O.Marcus P. S.In linear stratifications, vortices have a typical flat shape that appears to be not only a compromise between the rotation and the stratification of the background flow through their Coriolis parameter f and buoyancy frequency hbox{$ar{N}$} N̅ , but also involves the buoyancy frequency Nc within the vortices and their Rossby number Ro. We derive an analytical solution for the self-similar ellipsoidal shape of the vortices and the law for their aspect ratio. From this law, we show that long-lived vortices must necessary be either weakly stratified anticyclones or superstratified cyclones (which is less likely to occur). These predictions are experimentally and numerically verified and agree with published measurements for Jovian vortices and ocean meddies. This approach can be applied to a gaussian stratification to give good insights of the shape of vortices in protoplanetary disks and their sustainability.http://dx.doi.org/10.1051/epjconf/20134605004
spellingShingle Le Gal P.
Le Bars M.
Aubert O.
Marcus P. S.
Vortices in rotating and stratified flows: aspect ratio and sustainability
EPJ Web of Conferences
title Vortices in rotating and stratified flows: aspect ratio and sustainability
title_full Vortices in rotating and stratified flows: aspect ratio and sustainability
title_fullStr Vortices in rotating and stratified flows: aspect ratio and sustainability
title_full_unstemmed Vortices in rotating and stratified flows: aspect ratio and sustainability
title_short Vortices in rotating and stratified flows: aspect ratio and sustainability
title_sort vortices in rotating and stratified flows aspect ratio and sustainability
url http://dx.doi.org/10.1051/epjconf/20134605004
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AT marcusps vorticesinrotatingandstratifiedflowsaspectratioandsustainability