On the validity of downgradient eddy closures in ocean models
Results are presented from an eddy-resolving primitive equation ocean model to test the hypothesis that geostrophic eddies can be parameterized through a variety of downgradient closures. Time-mean eddy fluxes of temperature, isopycnic thickness, and quasi-geostrophic potential vorticity are diagnos...
| Main Authors: | , |
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| Format: | Journal article |
| Language: | English |
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Blackwell Publishing Ltd
2000
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| _version_ | 1797081994845224960 |
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| author | Roberts, M Marshall, D |
| author_facet | Roberts, M Marshall, D |
| author_sort | Roberts, M |
| collection | OXFORD |
| description | Results are presented from an eddy-resolving primitive equation ocean model to test the hypothesis that geostrophic eddies can be parameterized through a variety of downgradient closures. Time-mean eddy fluxes of temperature, isopycnic thickness, and quasi-geostrophic potential vorticity are diagnosed on level surfaces from 5 years of model data and are spatially correlated with the corresponding time-mean gradients. We find no discernible correlation between the absolute eddy fluxes and mean gradients. However, after decomposing the eddy fluxes into "rotational" and "divergent" components we find a positive correlation between the divergent eddy fluxes and the mean gradients, although the overall correlation coefficients remain small, typically O(0.2). The correlation between the eddy temperature fluxes and mean temperature gradients is positive only over the upper 2 km and is negative at depth, suggesting that the abyssal temperature fluxes are upgradient. In contrast, the correlations between eddy fluxes and mean gradients of isopycnic thickness and potential vorticity are positive over the most of the fluid column. The overall correlations are similar for both thickness and potential vorticity closures. We further decompose the divergent component of the eddy fluxes into components directed perpendicular and parallel to mean contours. We find that both the perpendicular and the parallel components are similar in magnitude. Copyright 2000 by the American Geophysical Union. |
| first_indexed | 2024-03-07T01:21:53Z |
| format | Journal article |
| id | oxford-uuid:90a432b3-1bdf-4d9c-a17f-0473999f6832 |
| institution | University of Oxford |
| language | English |
| last_indexed | 2024-03-07T01:21:53Z |
| publishDate | 2000 |
| publisher | Blackwell Publishing Ltd |
| record_format | dspace |
| spelling | oxford-uuid:90a432b3-1bdf-4d9c-a17f-0473999f68322022-03-26T23:13:01ZOn the validity of downgradient eddy closures in ocean modelsJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:90a432b3-1bdf-4d9c-a17f-0473999f6832EnglishSymplectic Elements at OxfordBlackwell Publishing Ltd2000Roberts, MMarshall, DResults are presented from an eddy-resolving primitive equation ocean model to test the hypothesis that geostrophic eddies can be parameterized through a variety of downgradient closures. Time-mean eddy fluxes of temperature, isopycnic thickness, and quasi-geostrophic potential vorticity are diagnosed on level surfaces from 5 years of model data and are spatially correlated with the corresponding time-mean gradients. We find no discernible correlation between the absolute eddy fluxes and mean gradients. However, after decomposing the eddy fluxes into "rotational" and "divergent" components we find a positive correlation between the divergent eddy fluxes and the mean gradients, although the overall correlation coefficients remain small, typically O(0.2). The correlation between the eddy temperature fluxes and mean temperature gradients is positive only over the upper 2 km and is negative at depth, suggesting that the abyssal temperature fluxes are upgradient. In contrast, the correlations between eddy fluxes and mean gradients of isopycnic thickness and potential vorticity are positive over the most of the fluid column. The overall correlations are similar for both thickness and potential vorticity closures. We further decompose the divergent component of the eddy fluxes into components directed perpendicular and parallel to mean contours. We find that both the perpendicular and the parallel components are similar in magnitude. Copyright 2000 by the American Geophysical Union. |
| spellingShingle | Roberts, M Marshall, D On the validity of downgradient eddy closures in ocean models |
| title | On the validity of downgradient eddy closures in ocean models |
| title_full | On the validity of downgradient eddy closures in ocean models |
| title_fullStr | On the validity of downgradient eddy closures in ocean models |
| title_full_unstemmed | On the validity of downgradient eddy closures in ocean models |
| title_short | On the validity of downgradient eddy closures in ocean models |
| title_sort | on the validity of downgradient eddy closures in ocean models |
| work_keys_str_mv | AT robertsm onthevalidityofdowngradienteddyclosuresinoceanmodels AT marshalld onthevalidityofdowngradienteddyclosuresinoceanmodels |