Sensitivity of Southern Ocean overturning to wind stress changes:Role of surface restoring time scales

The influence of different surface restoring time scales on the response of the Southern Ocean overturning circulation to wind stress changes is investigated using an idealised channel model. Regardless of the restoring time scales chosen, the eddy-induced meridional overturning circulation (MOC) is...

Full description

Bibliographic Details
Published in:Ocean Modelling
Main Authors: Zhai, Xiaoming, Munday, David
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Online Access:https://ueaeprints.uea.ac.uk/id/eprint/50472/
https://ueaeprints.uea.ac.uk/id/eprint/50472/1/so_haney5_revision_2.pdf
https://doi.org/10.1016/j.ocemod.2014.09.004
id ftuniveastangl:oai:ueaeprints.uea.ac.uk:50472
record_format openpolar
spelling ftuniveastangl:oai:ueaeprints.uea.ac.uk:50472 2023-05-15T18:24:50+02:00 Sensitivity of Southern Ocean overturning to wind stress changes:Role of surface restoring time scales Zhai, Xiaoming Munday, David 2014-12 application/pdf https://ueaeprints.uea.ac.uk/id/eprint/50472/ https://ueaeprints.uea.ac.uk/id/eprint/50472/1/so_haney5_revision_2.pdf https://doi.org/10.1016/j.ocemod.2014.09.004 en eng https://ueaeprints.uea.ac.uk/id/eprint/50472/1/so_haney5_revision_2.pdf Zhai, Xiaoming and Munday, David (2014) Sensitivity of Southern Ocean overturning to wind stress changes:Role of surface restoring time scales. Ocean Modelling, 84. pp. 12-25. ISSN 1463-5003 doi:10.1016/j.ocemod.2014.09.004 Article PeerReviewed 2014 ftuniveastangl https://doi.org/10.1016/j.ocemod.2014.09.004 2023-01-30T21:39:26Z The influence of different surface restoring time scales on the response of the Southern Ocean overturning circulation to wind stress changes is investigated using an idealised channel model. Regardless of the restoring time scales chosen, the eddy-induced meridional overturning circulation (MOC) is found to compensate for changes of the direct wind-driven Eulerian-mean MOC, rendering the residual MOC less sensitive to wind stress changes. However, the extent of this compensation depends strongly on the restoring time scale: residual MOC sensitivity increases with decreasing restoring time scale. Strong surface restoring is shown to limit the ability of the eddy-induced MOC to change in response to wind stress changes and as such suppresses the eddy compensation effect. These model results are consistent with qualitative arguments derived fromresidual-mean theory andmay have important implications for interpreting past and future observations. Article in Journal/Newspaper Southern Ocean University of East Anglia: UEA Digital Repository Southern Ocean Ocean Modelling 84 12 25
institution Open Polar
collection University of East Anglia: UEA Digital Repository
op_collection_id ftuniveastangl
language English
description The influence of different surface restoring time scales on the response of the Southern Ocean overturning circulation to wind stress changes is investigated using an idealised channel model. Regardless of the restoring time scales chosen, the eddy-induced meridional overturning circulation (MOC) is found to compensate for changes of the direct wind-driven Eulerian-mean MOC, rendering the residual MOC less sensitive to wind stress changes. However, the extent of this compensation depends strongly on the restoring time scale: residual MOC sensitivity increases with decreasing restoring time scale. Strong surface restoring is shown to limit the ability of the eddy-induced MOC to change in response to wind stress changes and as such suppresses the eddy compensation effect. These model results are consistent with qualitative arguments derived fromresidual-mean theory andmay have important implications for interpreting past and future observations.
format Article in Journal/Newspaper
author Zhai, Xiaoming
Munday, David
spellingShingle Zhai, Xiaoming
Munday, David
Sensitivity of Southern Ocean overturning to wind stress changes:Role of surface restoring time scales
author_facet Zhai, Xiaoming
Munday, David
author_sort Zhai, Xiaoming
title Sensitivity of Southern Ocean overturning to wind stress changes:Role of surface restoring time scales
title_short Sensitivity of Southern Ocean overturning to wind stress changes:Role of surface restoring time scales
title_full Sensitivity of Southern Ocean overturning to wind stress changes:Role of surface restoring time scales
title_fullStr Sensitivity of Southern Ocean overturning to wind stress changes:Role of surface restoring time scales
title_full_unstemmed Sensitivity of Southern Ocean overturning to wind stress changes:Role of surface restoring time scales
title_sort sensitivity of southern ocean overturning to wind stress changes:role of surface restoring time scales
publishDate 2014
url https://ueaeprints.uea.ac.uk/id/eprint/50472/
https://ueaeprints.uea.ac.uk/id/eprint/50472/1/so_haney5_revision_2.pdf
https://doi.org/10.1016/j.ocemod.2014.09.004
geographic Southern Ocean
geographic_facet Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_relation https://ueaeprints.uea.ac.uk/id/eprint/50472/1/so_haney5_revision_2.pdf
Zhai, Xiaoming and Munday, David (2014) Sensitivity of Southern Ocean overturning to wind stress changes:Role of surface restoring time scales. Ocean Modelling, 84. pp. 12-25. ISSN 1463-5003
doi:10.1016/j.ocemod.2014.09.004
op_doi https://doi.org/10.1016/j.ocemod.2014.09.004
container_title Ocean Modelling
container_volume 84
container_start_page 12
op_container_end_page 25
_version_ 1766205786781908992