Diagnostics of isopycnal mixing in a circumpolar channel
Mesoscale eddies mix tracers along isopycnals and horizontally at the sea surface. This paper compares different methods of diagnosing eddy mixing rates in an idealized, eddy-resolving model of a channel flow meant to resemble the Antarctic Circumpolar Current. The first set of methods, the perfect...
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Online Access: | https://doi.org/10.1016/j.ocemod.2013.07.004 http://ecite.utas.edu.au/91545 |
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ftunivtasecite:oai:ecite.utas.edu.au:91545 2023-05-15T13:37:23+02:00 Diagnostics of isopycnal mixing in a circumpolar channel Abernathy, R Ferreira, D Klocker, A 2013 https://doi.org/10.1016/j.ocemod.2013.07.004 http://ecite.utas.edu.au/91545 en eng Elsevier Sci Ltd http://dx.doi.org/10.1016/j.ocemod.2013.07.004 Abernathy, R and Ferreira, D and Klocker, A, Diagnostics of isopycnal mixing in a circumpolar channel, Ocean Modelling, 72 pp. 1-16. ISSN 1463-5003 (2013) [Refereed Article] http://ecite.utas.edu.au/91545 Earth Sciences Oceanography Physical Oceanography Refereed Article PeerReviewed 2013 ftunivtasecite https://doi.org/10.1016/j.ocemod.2013.07.004 2019-12-13T21:54:45Z Mesoscale eddies mix tracers along isopycnals and horizontally at the sea surface. This paper compares different methods of diagnosing eddy mixing rates in an idealized, eddy-resolving model of a channel flow meant to resemble the Antarctic Circumpolar Current. The first set of methods, the perfect diagnostics, are techniques suitable only to numerical models, in which detailed synoptic data is available. The perfect diagnostic include flux-gradient diffusivities of buoyancy, QGPV, and Ertel PV; Nakamuraeffective diffusivity; and the four-element diffusivity tensor calculated from an ensemble of passive tracers. These diagnostics reveal a consistent picture of isopycnal mixing by eddies, with a pronounced maximum near 1000 m depth. The isopycnal diffusivity differs from the buoyancy diffusivity, a.k.a. the GentMcWilliams transfer coefficient, which is weaker and peaks near the surface and bottom. The second set of methods are observationally practical diagnostics. They involve monitoring the spreading of tracers or Lagrangian particles in ways that are plausible in the field. We show how, with sufficient ensemble size, the practical diagnostics agree with the perfect diagnostics in an average sense. Someimplications for eddy parameterization are discussed. Article in Journal/Newspaper Antarc* Antarctic eCite UTAS (University of Tasmania) Antarctic The Antarctic Ocean Modelling 72 1 16 |
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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 Abernathy, R Ferreira, D Klocker, A Diagnostics of isopycnal mixing in a circumpolar channel |
topic_facet |
Earth Sciences Oceanography Physical Oceanography |
description |
Mesoscale eddies mix tracers along isopycnals and horizontally at the sea surface. This paper compares different methods of diagnosing eddy mixing rates in an idealized, eddy-resolving model of a channel flow meant to resemble the Antarctic Circumpolar Current. The first set of methods, the perfect diagnostics, are techniques suitable only to numerical models, in which detailed synoptic data is available. The perfect diagnostic include flux-gradient diffusivities of buoyancy, QGPV, and Ertel PV; Nakamuraeffective diffusivity; and the four-element diffusivity tensor calculated from an ensemble of passive tracers. These diagnostics reveal a consistent picture of isopycnal mixing by eddies, with a pronounced maximum near 1000 m depth. The isopycnal diffusivity differs from the buoyancy diffusivity, a.k.a. the GentMcWilliams transfer coefficient, which is weaker and peaks near the surface and bottom. The second set of methods are observationally practical diagnostics. They involve monitoring the spreading of tracers or Lagrangian particles in ways that are plausible in the field. We show how, with sufficient ensemble size, the practical diagnostics agree with the perfect diagnostics in an average sense. Someimplications for eddy parameterization are discussed. |
format |
Article in Journal/Newspaper |
author |
Abernathy, R Ferreira, D Klocker, A |
author_facet |
Abernathy, R Ferreira, D Klocker, A |
author_sort |
Abernathy, R |
title |
Diagnostics of isopycnal mixing in a circumpolar channel |
title_short |
Diagnostics of isopycnal mixing in a circumpolar channel |
title_full |
Diagnostics of isopycnal mixing in a circumpolar channel |
title_fullStr |
Diagnostics of isopycnal mixing in a circumpolar channel |
title_full_unstemmed |
Diagnostics of isopycnal mixing in a circumpolar channel |
title_sort |
diagnostics of isopycnal mixing in a circumpolar channel |
publisher |
Elsevier Sci Ltd |
publishDate |
2013 |
url |
https://doi.org/10.1016/j.ocemod.2013.07.004 http://ecite.utas.edu.au/91545 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
http://dx.doi.org/10.1016/j.ocemod.2013.07.004 Abernathy, R and Ferreira, D and Klocker, A, Diagnostics of isopycnal mixing in a circumpolar channel, Ocean Modelling, 72 pp. 1-16. ISSN 1463-5003 (2013) [Refereed Article] http://ecite.utas.edu.au/91545 |
op_doi |
https://doi.org/10.1016/j.ocemod.2013.07.004 |
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Ocean Modelling |
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72 |
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1 |
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16 |
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1766091245697892352 |