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
Main Authors: Zhai, X, Munday, D
Format: Journal article
Language:English
Published: Elsevier 2014
_version_ 1797106110720638976
author Zhai, X
Munday, D
author_facet Zhai, X
Munday, D
author_sort Zhai, X
collection OXFORD
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 from residual-mean theory and may have important implications for interpreting past and future observations.
first_indexed 2024-03-07T06:57:03Z
format Journal article
id oxford-uuid:fe7c5e9c-dd37-42e0-ab28-d7c0b7ae8e3e
institution University of Oxford
language English
last_indexed 2024-03-07T06:57:03Z
publishDate 2014
publisher Elsevier
record_format dspace
spelling oxford-uuid:fe7c5e9c-dd37-42e0-ab28-d7c0b7ae8e3e2022-03-27T13:36:56ZSensitivity of Southern Ocean overturning to wind stress changes: Role of surface restoring time scalesJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:fe7c5e9c-dd37-42e0-ab28-d7c0b7ae8e3eEnglishSymplectic Elements at OxfordElsevier2014Zhai, XMunday, DThe 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 from residual-mean theory and may have important implications for interpreting past and future observations.
spellingShingle Zhai, X
Munday, D
Sensitivity of Southern Ocean overturning to wind stress changes: Role of surface restoring time scales
title 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_short 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
work_keys_str_mv AT zhaix sensitivityofsouthernoceanoverturningtowindstresschangesroleofsurfacerestoringtimescales
AT mundayd sensitivityofsouthernoceanoverturningtowindstresschangesroleofsurfacerestoringtimescales