A geometric interpretation of Southern Ocean eddy form stress
An interpretation of eddy form stress via the geometry described by the Eliassen-Palm flux tensor is explored. Complimentary to previous works on eddy Reynolds stress geometry, this study shows that eddy form stress is fully described by a vertical ellipse, whose size, shape and orientation with res...
Published in: | Journal of Physical Oceanography |
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American Meteorological Society
2019
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Online Access: | https://doi.org/10.1175/JPO-D-18-0220.1 https://ora.ox.ac.uk/objects/uuid:a295c859-6c38-41a1-b28d-04805755e2fb |
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ftuloxford:oai:ora.ox.ac.uk:uuid:a295c859-6c38-41a1-b28d-04805755e2fb 2023-05-15T13:49:19+02:00 A geometric interpretation of Southern Ocean eddy form stress Poulsen, M Jochum, M Maddison, J Marshall, D Nuterman, R 2019-07-24 https://doi.org/10.1175/JPO-D-18-0220.1 https://ora.ox.ac.uk/objects/uuid:a295c859-6c38-41a1-b28d-04805755e2fb unknown American Meteorological Society doi:10.1175/JPO-D-18-0220.1 https://ora.ox.ac.uk/objects/uuid:a295c859-6c38-41a1-b28d-04805755e2fb https://doi.org/10.1175/JPO-D-18-0220.1 info:eu-repo/semantics/openAccess CC Attribution (CC BY) CC-BY Journal article 2019 ftuloxford https://doi.org/10.1175/JPO-D-18-0220.1 2022-06-28T20:20:02Z An interpretation of eddy form stress via the geometry described by the Eliassen-Palm flux tensor is explored. Complimentary to previous works on eddy Reynolds stress geometry, this study shows that eddy form stress is fully described by a vertical ellipse, whose size, shape and orientation with respect to the mean-flow shear determine the strength and direction of vertical momentum transfers. Following a recent proposal, this geometric framework is here used to form a Gent-McWilliams eddy transfer coefficient which depends on eddy energy and a non-dimensional geometric parameter α, bounded in magnitude by unity. α expresses the efficiency by which eddies exchange energy with baroclinic mean-flow via along-gradient eddy buoyancy flux - a flux equivalent to eddy form stress along mean buoyancy contours. An eddy-resolving ocean general circulation model is used to estimate the spatial structure of α in the Southern Ocean and assess its potential to form a basis for parameterization. α averages to a low but positive value of 0.043 within the Antarctic Circumpolar Current, consistent with an inefficient eddy field extracting energy from the mean-flow. It is found that the low eddy efficiency is mainly the result of that eddy buoyancy fluxes are weakly anisotropic on average. α is subject to pronounced vertical structure and is maximum at ∼ 3 km depth where eddy buoyancy fluxes tend to be directed most downgradient. Since α partly sets the eddy form stress in the Southern Ocean, a parameterization for α must reproduce its vertical structure to provide a faithful representation of vertical stress divergence and eddy forcing. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean ORA - Oxford University Research Archive Antarctic Southern Ocean The Antarctic Journal of Physical Oceanography 49 10 2553 2570 |
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ORA - Oxford University Research Archive |
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ftuloxford |
language |
unknown |
description |
An interpretation of eddy form stress via the geometry described by the Eliassen-Palm flux tensor is explored. Complimentary to previous works on eddy Reynolds stress geometry, this study shows that eddy form stress is fully described by a vertical ellipse, whose size, shape and orientation with respect to the mean-flow shear determine the strength and direction of vertical momentum transfers. Following a recent proposal, this geometric framework is here used to form a Gent-McWilliams eddy transfer coefficient which depends on eddy energy and a non-dimensional geometric parameter α, bounded in magnitude by unity. α expresses the efficiency by which eddies exchange energy with baroclinic mean-flow via along-gradient eddy buoyancy flux - a flux equivalent to eddy form stress along mean buoyancy contours. An eddy-resolving ocean general circulation model is used to estimate the spatial structure of α in the Southern Ocean and assess its potential to form a basis for parameterization. α averages to a low but positive value of 0.043 within the Antarctic Circumpolar Current, consistent with an inefficient eddy field extracting energy from the mean-flow. It is found that the low eddy efficiency is mainly the result of that eddy buoyancy fluxes are weakly anisotropic on average. α is subject to pronounced vertical structure and is maximum at ∼ 3 km depth where eddy buoyancy fluxes tend to be directed most downgradient. Since α partly sets the eddy form stress in the Southern Ocean, a parameterization for α must reproduce its vertical structure to provide a faithful representation of vertical stress divergence and eddy forcing. |
format |
Article in Journal/Newspaper |
author |
Poulsen, M Jochum, M Maddison, J Marshall, D Nuterman, R |
spellingShingle |
Poulsen, M Jochum, M Maddison, J Marshall, D Nuterman, R A geometric interpretation of Southern Ocean eddy form stress |
author_facet |
Poulsen, M Jochum, M Maddison, J Marshall, D Nuterman, R |
author_sort |
Poulsen, M |
title |
A geometric interpretation of Southern Ocean eddy form stress |
title_short |
A geometric interpretation of Southern Ocean eddy form stress |
title_full |
A geometric interpretation of Southern Ocean eddy form stress |
title_fullStr |
A geometric interpretation of Southern Ocean eddy form stress |
title_full_unstemmed |
A geometric interpretation of Southern Ocean eddy form stress |
title_sort |
geometric interpretation of southern ocean eddy form stress |
publisher |
American Meteorological Society |
publishDate |
2019 |
url |
https://doi.org/10.1175/JPO-D-18-0220.1 https://ora.ox.ac.uk/objects/uuid:a295c859-6c38-41a1-b28d-04805755e2fb |
geographic |
Antarctic Southern Ocean The Antarctic |
geographic_facet |
Antarctic Southern Ocean The Antarctic |
genre |
Antarc* Antarctic Southern Ocean |
genre_facet |
Antarc* Antarctic Southern Ocean |
op_relation |
doi:10.1175/JPO-D-18-0220.1 https://ora.ox.ac.uk/objects/uuid:a295c859-6c38-41a1-b28d-04805755e2fb https://doi.org/10.1175/JPO-D-18-0220.1 |
op_rights |
info:eu-repo/semantics/openAccess CC Attribution (CC BY) |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1175/JPO-D-18-0220.1 |
container_title |
Journal of Physical Oceanography |
container_volume |
49 |
container_issue |
10 |
container_start_page |
2553 |
op_container_end_page |
2570 |
_version_ |
1766251168714981376 |