A geometric interpretation of eddy Reynolds stresses in barotropic ocean jets
Barotropic eddy fluxes are analyzed through a geometric decomposition of the eddy stress tensor. Specifically, the geometry of the eddy variance ellipse, a two-dimensional visualization of the stress tensor describing the mean eddy shape and tilt, is used to elucidate eddy propagation and eddy feedb...
| Main Authors: | , , , |
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| Format: | Journal article |
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American Meteorological Society
2016
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| _version_ | 1797059450897432576 |
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| author | Tamarin, T Maddison, J Heifetz, E Marshall, D |
| author_facet | Tamarin, T Maddison, J Heifetz, E Marshall, D |
| author_sort | Tamarin, T |
| collection | OXFORD |
| description | Barotropic eddy fluxes are analyzed through a geometric decomposition of the eddy stress tensor. Specifically, the geometry of the eddy variance ellipse, a two-dimensional visualization of the stress tensor describing the mean eddy shape and tilt, is used to elucidate eddy propagation and eddy feedback on the mean flow. Linear shear and jet profiles are analyzed and theoretical results are compared against fully nonlinear simulations. For flows with zero planetary vorticity gradient, analytic solutions for theeddy ellipse tilt and anisotropy are obtained that provide a direct relationship between the eddy tilt and the phasedifference of a normal-mode solution. This allows a straightforward interpretation of the eddy–mean flow interaction in terms of classical stability theory: the initially unstable jet gives rise to eddies that are tilted ‘‘against the shear’’ and extract energy from the mean flow; once the jet stabilizes, eddies become tilted ‘‘with the shear’’ and return their energy to the mean flow. For a nonzero planetary vorticity gradient, ray-tracing theory is used to predict ellipse geometry and its impact on eddy propagation within a jet. An analytic solution for the eddy tilt is found for a Rossby wave on a constant background shear. The ray-tracing results broadly agree with the eddy tilt diagnosed from a fully nonlinear simulation. |
| first_indexed | 2024-03-06T20:04:26Z |
| format | Journal article |
| id | oxford-uuid:2875fdbc-6c2b-4aac-aaaa-ccca71d7e3ad |
| institution | University of Oxford |
| last_indexed | 2024-03-06T20:04:26Z |
| publishDate | 2016 |
| publisher | American Meteorological Society |
| record_format | dspace |
| spelling | oxford-uuid:2875fdbc-6c2b-4aac-aaaa-ccca71d7e3ad2022-03-26T12:12:55ZA geometric interpretation of eddy Reynolds stresses in barotropic ocean jetsJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:2875fdbc-6c2b-4aac-aaaa-ccca71d7e3adSymplectic Elements at OxfordAmerican Meteorological Society2016Tamarin, TMaddison, JHeifetz, EMarshall, DBarotropic eddy fluxes are analyzed through a geometric decomposition of the eddy stress tensor. Specifically, the geometry of the eddy variance ellipse, a two-dimensional visualization of the stress tensor describing the mean eddy shape and tilt, is used to elucidate eddy propagation and eddy feedback on the mean flow. Linear shear and jet profiles are analyzed and theoretical results are compared against fully nonlinear simulations. For flows with zero planetary vorticity gradient, analytic solutions for theeddy ellipse tilt and anisotropy are obtained that provide a direct relationship between the eddy tilt and the phasedifference of a normal-mode solution. This allows a straightforward interpretation of the eddy–mean flow interaction in terms of classical stability theory: the initially unstable jet gives rise to eddies that are tilted ‘‘against the shear’’ and extract energy from the mean flow; once the jet stabilizes, eddies become tilted ‘‘with the shear’’ and return their energy to the mean flow. For a nonzero planetary vorticity gradient, ray-tracing theory is used to predict ellipse geometry and its impact on eddy propagation within a jet. An analytic solution for the eddy tilt is found for a Rossby wave on a constant background shear. The ray-tracing results broadly agree with the eddy tilt diagnosed from a fully nonlinear simulation. |
| spellingShingle | Tamarin, T Maddison, J Heifetz, E Marshall, D A geometric interpretation of eddy Reynolds stresses in barotropic ocean jets |
| title | A geometric interpretation of eddy Reynolds stresses in barotropic ocean jets |
| title_full | A geometric interpretation of eddy Reynolds stresses in barotropic ocean jets |
| title_fullStr | A geometric interpretation of eddy Reynolds stresses in barotropic ocean jets |
| title_full_unstemmed | A geometric interpretation of eddy Reynolds stresses in barotropic ocean jets |
| title_short | A geometric interpretation of eddy Reynolds stresses in barotropic ocean jets |
| title_sort | geometric interpretation of eddy reynolds stresses in barotropic ocean jets |
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