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Mechanisms of decadal variability of the wind-driven ocean circulation

Mechanisms of decadal variability of the wind-driven ocean circulation
Mechanisms of decadal variability of the wind-driven ocean circulation
Eddy-resolving quasigeostrophic simulations of wind-driven circulation in a large ocean basin are presented. The results show that strong modes of low-frequency variability arise in many parameter regimes and that the strength of these modes depends upon the presence of inertial recirculations in the flow field. The inertial recirculations arise through advection of anomalous potential vorticity by the western boundary current and are barotropized by the effect of baroclinic eddies in the flow. The mechanism of low-frequency oscillations is explored with reference to previous studies, and it is found that the observed mode can be linked to the gyre mode but is strongly modified by the effect of eddies.
0022-3670
512-531
Hogg, A.M.
df48090a-bbe6-4929-a94a-62a0aa7e5e8b
Killworth, P.D.
9fc0c4a0-e1fb-4073-8997-436b59c74bf2
Blundell, J.R.
88114f32-6b76-46b2-b2d8-d6ef64a82b0d
Dewar, W.K.
ed3e98c6-1a77-42dc-b970-64718f4ebb97
Hogg, A.M.
df48090a-bbe6-4929-a94a-62a0aa7e5e8b
Killworth, P.D.
9fc0c4a0-e1fb-4073-8997-436b59c74bf2
Blundell, J.R.
88114f32-6b76-46b2-b2d8-d6ef64a82b0d
Dewar, W.K.
ed3e98c6-1a77-42dc-b970-64718f4ebb97

Hogg, A.M., Killworth, P.D., Blundell, J.R. and Dewar, W.K. (2005) Mechanisms of decadal variability of the wind-driven ocean circulation. Journal of Physical Oceanography, 35 (4), 512-531. (doi:10.1175/JPO2687.1).

Record type: Article

Abstract

Eddy-resolving quasigeostrophic simulations of wind-driven circulation in a large ocean basin are presented. The results show that strong modes of low-frequency variability arise in many parameter regimes and that the strength of these modes depends upon the presence of inertial recirculations in the flow field. The inertial recirculations arise through advection of anomalous potential vorticity by the western boundary current and are barotropized by the effect of baroclinic eddies in the flow. The mechanism of low-frequency oscillations is explored with reference to previous studies, and it is found that the observed mode can be linked to the gyre mode but is strongly modified by the effect of eddies.

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Published date: 2005

Identifiers

Local EPrints ID: 17405
URI: http://eprints.soton.ac.uk/id/eprint/17405
ISSN: 0022-3670
PURE UUID: 103f942b-696a-49e7-b02d-72e0b5b51dce

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Date deposited: 07 Sep 2005
Last modified: 15 Mar 2024 05:59

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Contributors

Author: A.M. Hogg
Author: P.D. Killworth
Author: J.R. Blundell
Author: W.K. Dewar

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