Eddy saturation of equilibrated circumpolar currents

This study uses a sector configuration of an ocean general circulation model to examine the sensitivity of circumpolar transport and meridional overturning to changes in Southern Ocean wind stress and global diapycnal mixing. At eddy-permitting, and finer, resolution, the sensitivity of circumpolar...

Full description

Bibliographic Details
Main Authors: Munday, D, Johnson, H, Marshall, D
Format: Journal article
Published: American Meteorological Society 2013
_version_ 1797084702888165376
author Munday, D
Johnson, H
Marshall, D
author_facet Munday, D
Johnson, H
Marshall, D
author_sort Munday, D
collection OXFORD
description This study uses a sector configuration of an ocean general circulation model to examine the sensitivity of circumpolar transport and meridional overturning to changes in Southern Ocean wind stress and global diapycnal mixing. At eddy-permitting, and finer, resolution, the sensitivity of circumpolar transport to forcing magnitude is drastically reduced. At sufficiently high resolution, there is little or no sensitivity of circumpolar transport to wind stress, even in the limit of no wind. In contrast, the meridional overturning circulation continues to vary with Southern Ocean wind stress, but with reduced sensitivity in the limit of high wind stress. Both the circumpolar transport and meridional overturning continue to vary with diapycnal diffusivity at all model resolutions. The circumpolar transport becomes less sensitive to changes in diapycnal diffusivity at higher resolution, although sensitivity always remains. In contrast, the overturning circulation is more sensitive to change in diapycnal diffusivity when the resolution is high enough to permit mesoscale eddies.
first_indexed 2024-03-07T01:58:41Z
format Journal article
id oxford-uuid:9c9d05d6-be2f-4c3a-85fb-ff0c9aef8592
institution University of Oxford
last_indexed 2024-03-07T01:58:41Z
publishDate 2013
publisher American Meteorological Society
record_format dspace
spelling oxford-uuid:9c9d05d6-be2f-4c3a-85fb-ff0c9aef85922022-03-27T00:37:10ZEddy saturation of equilibrated circumpolar currentsJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:9c9d05d6-be2f-4c3a-85fb-ff0c9aef8592Symplectic Elements at OxfordAmerican Meteorological Society2013Munday, DJohnson, HMarshall, DThis study uses a sector configuration of an ocean general circulation model to examine the sensitivity of circumpolar transport and meridional overturning to changes in Southern Ocean wind stress and global diapycnal mixing. At eddy-permitting, and finer, resolution, the sensitivity of circumpolar transport to forcing magnitude is drastically reduced. At sufficiently high resolution, there is little or no sensitivity of circumpolar transport to wind stress, even in the limit of no wind. In contrast, the meridional overturning circulation continues to vary with Southern Ocean wind stress, but with reduced sensitivity in the limit of high wind stress. Both the circumpolar transport and meridional overturning continue to vary with diapycnal diffusivity at all model resolutions. The circumpolar transport becomes less sensitive to changes in diapycnal diffusivity at higher resolution, although sensitivity always remains. In contrast, the overturning circulation is more sensitive to change in diapycnal diffusivity when the resolution is high enough to permit mesoscale eddies.
spellingShingle Munday, D
Johnson, H
Marshall, D
Eddy saturation of equilibrated circumpolar currents
title Eddy saturation of equilibrated circumpolar currents
title_full Eddy saturation of equilibrated circumpolar currents
title_fullStr Eddy saturation of equilibrated circumpolar currents
title_full_unstemmed Eddy saturation of equilibrated circumpolar currents
title_short Eddy saturation of equilibrated circumpolar currents
title_sort eddy saturation of equilibrated circumpolar currents
work_keys_str_mv AT mundayd eddysaturationofequilibratedcircumpolarcurrents
AT johnsonh eddysaturationofequilibratedcircumpolarcurrents
AT marshalld eddysaturationofequilibratedcircumpolarcurrents