Baroclinic instability of quasi-geostrophic flows localized in a thin layer
This paper examines the baroclinic instability of a quasi-geostrophic flow with vertical shear in a continuously stratified fluid. The flow and density stratification are both localized in a thin upper layer. (i) Disturbances whose wavelength is much smaller than the deformation radius (based on the...
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Cambridge Univ Press
1995
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Online Access: | https://doi.org/10.1017/S002211209500111X http://ecite.utas.edu.au/3520 |
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ftunivtasecite:oai:ecite.utas.edu.au:3520 2023-05-15T18:28:20+02:00 Baroclinic instability of quasi-geostrophic flows localized in a thin layer Benilov, ES 1995 https://doi.org/10.1017/S002211209500111X http://ecite.utas.edu.au/3520 en eng Cambridge Univ Press http://dx.doi.org/10.1017/S002211209500111X Benilov, ES, Baroclinic instability of quasi-geostrophic flows localized in a thin layer, Journal of Fluid Mechanics, 288 pp. 175-199. ISSN 0022-1120 (1995) [Refereed Article] http://ecite.utas.edu.au/3520 Earth Sciences Oceanography Physical Oceanography Refereed Article PeerReviewed 1995 ftunivtasecite https://doi.org/10.1017/S002211209500111X 2019-12-13T20:51:39Z This paper examines the baroclinic instability of a quasi-geostrophic flow with vertical shear in a continuously stratified fluid. The flow and density stratification are both localized in a thin upper layer. (i) Disturbances whose wavelength is much smaller than the deformation radius (based on the depth of the upper layer) are demonstrated to satisfy an equivalent two-layer model with properly chosen parameters. (ii) For disturbances whose wavelength is of the order of, or greater than, the deformation radius we derive a sufficient stability criterion. The above analysis is applied to the subtropical and subarctic frontal currents in the Northern Pacific. The effective time of growth of disturbances (i) is found to be 1622 days, the characteristic spatial scale is 130150 km. 1995, Cambridge University Press. All rights reserved. Article in Journal/Newspaper Subarctic eCite UTAS (University of Tasmania) Pacific Journal of Fluid Mechanics 288 175 199 |
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Open Polar |
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eCite UTAS (University of Tasmania) |
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ftunivtasecite |
language |
English |
topic |
Earth Sciences Oceanography Physical Oceanography |
spellingShingle |
Earth Sciences Oceanography Physical Oceanography Benilov, ES Baroclinic instability of quasi-geostrophic flows localized in a thin layer |
topic_facet |
Earth Sciences Oceanography Physical Oceanography |
description |
This paper examines the baroclinic instability of a quasi-geostrophic flow with vertical shear in a continuously stratified fluid. The flow and density stratification are both localized in a thin upper layer. (i) Disturbances whose wavelength is much smaller than the deformation radius (based on the depth of the upper layer) are demonstrated to satisfy an equivalent two-layer model with properly chosen parameters. (ii) For disturbances whose wavelength is of the order of, or greater than, the deformation radius we derive a sufficient stability criterion. The above analysis is applied to the subtropical and subarctic frontal currents in the Northern Pacific. The effective time of growth of disturbances (i) is found to be 1622 days, the characteristic spatial scale is 130150 km. 1995, Cambridge University Press. All rights reserved. |
format |
Article in Journal/Newspaper |
author |
Benilov, ES |
author_facet |
Benilov, ES |
author_sort |
Benilov, ES |
title |
Baroclinic instability of quasi-geostrophic flows localized in a thin layer |
title_short |
Baroclinic instability of quasi-geostrophic flows localized in a thin layer |
title_full |
Baroclinic instability of quasi-geostrophic flows localized in a thin layer |
title_fullStr |
Baroclinic instability of quasi-geostrophic flows localized in a thin layer |
title_full_unstemmed |
Baroclinic instability of quasi-geostrophic flows localized in a thin layer |
title_sort |
baroclinic instability of quasi-geostrophic flows localized in a thin layer |
publisher |
Cambridge Univ Press |
publishDate |
1995 |
url |
https://doi.org/10.1017/S002211209500111X http://ecite.utas.edu.au/3520 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Subarctic |
genre_facet |
Subarctic |
op_relation |
http://dx.doi.org/10.1017/S002211209500111X Benilov, ES, Baroclinic instability of quasi-geostrophic flows localized in a thin layer, Journal of Fluid Mechanics, 288 pp. 175-199. ISSN 0022-1120 (1995) [Refereed Article] http://ecite.utas.edu.au/3520 |
op_doi |
https://doi.org/10.1017/S002211209500111X |
container_title |
Journal of Fluid Mechanics |
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288 |
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175 |
op_container_end_page |
199 |
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1766210771553878016 |