The University of Southampton
University of Southampton Institutional Repository

Interdecadal variability of the Southern Ocean

Interdecadal variability of the Southern Ocean
Interdecadal variability of the Southern Ocean
The intrinsic variability of the Antarctic Circumpolar Current is investigated using an idealized wind-driven model. The model uses three quasigeostrophic layers, with steady wind stress forcing, and no diabatic effects. Despite the idealized nature of the model, the simulations display a robust mode of low-frequency variability in the flow. It is demonstrated that this variability is dependent upon the explicit simulation of the dynamics of mesoscale eddies. As such, the variability is sensitive to stratification, horizontal viscosity, bottom stress, and topography. The energetic balance of the variability is diagnosed, and a driving mechanism is proposed that involves positive feedback between the generation of eddies through baroclinic instability and the dynamics of the mean circulation.

0022-3670
1626-1645
Hogg, A.McC.
cfa79636-d52b-4626-8202-2ea66862a273
Blundell, J.R.
88114f32-6b76-46b2-b2d8-d6ef64a82b0d
Hogg, A.McC.
cfa79636-d52b-4626-8202-2ea66862a273
Blundell, J.R.
88114f32-6b76-46b2-b2d8-d6ef64a82b0d

Hogg, A.McC. and Blundell, J.R. (2006) Interdecadal variability of the Southern Ocean. Journal of Physical Oceanography, 36 (8), 1626-1645. (doi:10.1175/JPO2934.1).

Record type: Article

Abstract

The intrinsic variability of the Antarctic Circumpolar Current is investigated using an idealized wind-driven model. The model uses three quasigeostrophic layers, with steady wind stress forcing, and no diabatic effects. Despite the idealized nature of the model, the simulations display a robust mode of low-frequency variability in the flow. It is demonstrated that this variability is dependent upon the explicit simulation of the dynamics of mesoscale eddies. As such, the variability is sensitive to stratification, horizontal viscosity, bottom stress, and topography. The energetic balance of the variability is diagnosed, and a driving mechanism is proposed that involves positive feedback between the generation of eddies through baroclinic instability and the dynamics of the mean circulation.

This record has no associated files available for download.

More information

Published date: 2006

Identifiers

Local EPrints ID: 43995
URI: http://eprints.soton.ac.uk/id/eprint/43995
ISSN: 0022-3670
PURE UUID: e5eecae7-3da3-46b8-9f87-e81204ed33e7

Catalogue record

Date deposited: 06 Feb 2007
Last modified: 15 Mar 2024 08:59

Export record

Altmetrics

Contributors

Author: A.McC. Hogg
Author: J.R. Blundell

Download statistics

Downloads from ePrints over the past year. Other digital versions may also be available to download e.g. from the publisher's website.

View more statistics

Atom RSS 1.0 RSS 2.0

Contact ePrints Soton: eprints@soton.ac.uk

ePrints Soton supports OAI 2.0 with a base URL of http://eprints.soton.ac.uk/cgi/oai2

This repository has been built using EPrints software, developed at the University of Southampton, but available to everyone to use.

We use cookies to ensure that we give you the best experience on our website. If you continue without changing your settings, we will assume that you are happy to receive cookies on the University of Southampton website.

×