Thickness diffusitivityin the Southern Ocean
Thickness diffusivity (κ) according to the Gent and McWilliams parameterisation which accounts for eddy-driven advection in the ocean, is estimated using output from an eddy-resolving model of the Southern Ocean. A physically meaningful definition of rotational eddy fluxes leads almost everywhere to...
Published in: | Geophysical Research Letters |
---|---|
Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
AGU (American Geophysical Union)
2006
|
Subjects: | |
Online Access: | https://oceanrep.geomar.de/id/eprint/6456/ https://oceanrep.geomar.de/id/eprint/6456/1/Eden-2006-Geophysical_Research_Letters.pdf https://doi.org/10.1029/2006GL026157 |
id |
ftoceanrep:oai:oceanrep.geomar.de:6456 |
---|---|
record_format |
openpolar |
spelling |
ftoceanrep:oai:oceanrep.geomar.de:6456 2023-05-15T18:24:45+02:00 Thickness diffusitivityin the Southern Ocean Eden, Carsten 2006 text https://oceanrep.geomar.de/id/eprint/6456/ https://oceanrep.geomar.de/id/eprint/6456/1/Eden-2006-Geophysical_Research_Letters.pdf https://doi.org/10.1029/2006GL026157 en eng AGU (American Geophysical Union) https://oceanrep.geomar.de/id/eprint/6456/1/Eden-2006-Geophysical_Research_Letters.pdf Eden, C. (2006) Thickness diffusitivityin the Southern Ocean. Open Access Geophysical Research Letters, 33 (L11606). DOI 10.1029/2006GL026157 <https://doi.org/10.1029/2006GL026157>. doi:10.1029/2006GL026157 info:eu-repo/semantics/openAccess Article PeerReviewed 2006 ftoceanrep https://doi.org/10.1029/2006GL026157 2023-04-07T14:53:01Z Thickness diffusivity (κ) according to the Gent and McWilliams parameterisation which accounts for eddy-driven advection in the ocean, is estimated using output from an eddy-resolving model of the Southern Ocean. A physically meaningful definition of rotational eddy fluxes leads almost everywhere to positive κ. Zonally averaged near surface values of κ remain smaller than 200 m2/s poleward of the polar front, increases between 60–45°S to about 600 m2/s and peak between 45–35° S at almost 3000 m2/s. κ stays high in the upper 500 m but decreases with depth and is essentially zero below 2500 m. In addition to the thickness diffusion (κ) there is eddy-induced eastward (westward) advection of isopycnal thickness at the poleward (equatorward) flank of the ACC pointing toward strong anisotropic lateral mixing. Article in Journal/Newspaper Southern Ocean OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Southern Ocean Geophysical Research Letters 33 11 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
Thickness diffusivity (κ) according to the Gent and McWilliams parameterisation which accounts for eddy-driven advection in the ocean, is estimated using output from an eddy-resolving model of the Southern Ocean. A physically meaningful definition of rotational eddy fluxes leads almost everywhere to positive κ. Zonally averaged near surface values of κ remain smaller than 200 m2/s poleward of the polar front, increases between 60–45°S to about 600 m2/s and peak between 45–35° S at almost 3000 m2/s. κ stays high in the upper 500 m but decreases with depth and is essentially zero below 2500 m. In addition to the thickness diffusion (κ) there is eddy-induced eastward (westward) advection of isopycnal thickness at the poleward (equatorward) flank of the ACC pointing toward strong anisotropic lateral mixing. |
format |
Article in Journal/Newspaper |
author |
Eden, Carsten |
spellingShingle |
Eden, Carsten Thickness diffusitivityin the Southern Ocean |
author_facet |
Eden, Carsten |
author_sort |
Eden, Carsten |
title |
Thickness diffusitivityin the Southern Ocean |
title_short |
Thickness diffusitivityin the Southern Ocean |
title_full |
Thickness diffusitivityin the Southern Ocean |
title_fullStr |
Thickness diffusitivityin the Southern Ocean |
title_full_unstemmed |
Thickness diffusitivityin the Southern Ocean |
title_sort |
thickness diffusitivityin the southern ocean |
publisher |
AGU (American Geophysical Union) |
publishDate |
2006 |
url |
https://oceanrep.geomar.de/id/eprint/6456/ https://oceanrep.geomar.de/id/eprint/6456/1/Eden-2006-Geophysical_Research_Letters.pdf https://doi.org/10.1029/2006GL026157 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_relation |
https://oceanrep.geomar.de/id/eprint/6456/1/Eden-2006-Geophysical_Research_Letters.pdf Eden, C. (2006) Thickness diffusitivityin the Southern Ocean. Open Access Geophysical Research Letters, 33 (L11606). DOI 10.1029/2006GL026157 <https://doi.org/10.1029/2006GL026157>. doi:10.1029/2006GL026157 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/2006GL026157 |
container_title |
Geophysical Research Letters |
container_volume |
33 |
container_issue |
11 |
_version_ |
1766205636735926272 |