On the dynamics of wind-driven circumpolar currents

The factors controlling the transport of the Antarctic Circumpolar Current (ACC) have recently been a topic of heated debate. At the latitudes of Drake Passage, potential vorticity contours are uninterrupted by coastlines, and large amplitude flows are possible even with weak forcing and dissipation...

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Main Authors: Tansley, C, Marshall, D
Format: Journal article
Language:English
Published: 2001
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author Tansley, C
Marshall, D
author_facet Tansley, C
Marshall, D
author_sort Tansley, C
collection OXFORD
description The factors controlling the transport of the Antarctic Circumpolar Current (ACC) have recently been a topic of heated debate. At the latitudes of Drake Passage, potential vorticity contours are uninterrupted by coastlines, and large amplitude flows are possible even with weak forcing and dissipation. The relationship between the dynamics of circumpolar currents and inertial recirculations in closed basins is discussed. In previous studies, Sverdrup balance and baroclinic adjustment theories have both been proposed as theories of the ACC transport. These theories predict the circumpolar transport as various simple functions of the surface wind stress. A series of experiments is performed with a simple channel model, with different wind strengths and different idealized basin geometries, to investigate the relationship between wind strenght and circumpolar transport. The results show that baroclinic adjustment theories do predict transport in the special case of a periodic channel with no topographic variations, or when the wind forcing is very weak. More generally, the transport is determined by a complex interplay between wind forcing, eddy fluxes, and topographic effects. There is no support for the idea that Sverdrup balance determines the transport through Drake Passage.
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spelling oxford-uuid:179ced3a-bf5d-4117-8fb8-bfd10a1b9fe82022-03-26T10:38:25ZOn the dynamics of wind-driven circumpolar currentsJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:179ced3a-bf5d-4117-8fb8-bfd10a1b9fe8EnglishSymplectic Elements at Oxford2001Tansley, CMarshall, DThe factors controlling the transport of the Antarctic Circumpolar Current (ACC) have recently been a topic of heated debate. At the latitudes of Drake Passage, potential vorticity contours are uninterrupted by coastlines, and large amplitude flows are possible even with weak forcing and dissipation. The relationship between the dynamics of circumpolar currents and inertial recirculations in closed basins is discussed. In previous studies, Sverdrup balance and baroclinic adjustment theories have both been proposed as theories of the ACC transport. These theories predict the circumpolar transport as various simple functions of the surface wind stress. A series of experiments is performed with a simple channel model, with different wind strengths and different idealized basin geometries, to investigate the relationship between wind strenght and circumpolar transport. The results show that baroclinic adjustment theories do predict transport in the special case of a periodic channel with no topographic variations, or when the wind forcing is very weak. More generally, the transport is determined by a complex interplay between wind forcing, eddy fluxes, and topographic effects. There is no support for the idea that Sverdrup balance determines the transport through Drake Passage.
spellingShingle Tansley, C
Marshall, D
On the dynamics of wind-driven circumpolar currents
title On the dynamics of wind-driven circumpolar currents
title_full On the dynamics of wind-driven circumpolar currents
title_fullStr On the dynamics of wind-driven circumpolar currents
title_full_unstemmed On the dynamics of wind-driven circumpolar currents
title_short On the dynamics of wind-driven circumpolar currents
title_sort on the dynamics of wind driven circumpolar currents
work_keys_str_mv AT tansleyc onthedynamicsofwinddrivencircumpolarcurrents
AT marshalld onthedynamicsofwinddrivencircumpolarcurrents