Eddy-driven transports in the Antarctic Circumpolar Current

Meridional transports in the Southern Ocean across the Antarctic Circumpolar
Current are strongly affected or even controlled by the meso-scale eddy field. In non-eddy-permitting
ocean climate models their effects are parameterised with a lateral diffusivity from which the magnitude and vertical and
horizontal structure was poorly known so far. In this project, this diffusivity was estimated from eddy-permitting models
of the Southern Ocean and a new flow-interactive closure was successfully developed, implemented and evaluated in a
non-eddy-permitting ocean model of the Southern Ocean.
To obtain a better understanding of the future changes of the meridional overturning circulation (MOC), and in particular the
future fate of the CO
2 sink of the Southern Ocean, we now assess the response of the MOC to decadal-scale trends in wind
stress and surface buoyancy forcing the Southern Ocean and the consequence of the use of the new closure versus a fixed lateral
diffusivity for model simulations of decadal trends in the Southern Ocean.
Scientists
Carsten Eden
IFM-GEOMAR
Kiel
Jan Viebahn
IFM-GEOMAR
Kiel
Stefan Riha
IFM-GEOMAR
Kiel
Research areas
Circum Antarctica
Publications
Eden C, 2006. Thickness diffusivity in the Southern Ocean. Geophys. Res. Lett. 33 (L11606).
Eden C, Greatbatch RJ, 2008. Towards a mesoscale eddy closure. Ocean Modelling 20, 223-239.
Eden C, Jochum M, Danabasoglu G, 2009. Effects of different closures for thickness diffusivity. Ocean Modelling 26, 47-59.
Eden C, 2010. Parameterising meso-scale eddy momentum fluxes based on potential vorticity mixing and a gauge term. Ocean Modelling 32, 58-71.
doi:10.1016/j.ocemod.2009.10.008
Viebahn J, Eden C, 2010. Towards the impact of eddies on the response of the Southern Ocean to climate change. Ocean Modelling 34, 150-165.
doi:10.1016/j.ocemod.2010.05.005
Riha S, Eden C, 2011. Lagrangian and Eulerian lateral diffusivities in zonal jets. Ocean Modelling (in press)
Viebahn J, Eden C, 2011. Standing eddies in the meridional overturning circulation. J. Phys. Oceangr. (submitted)
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Research funding organisation
German Research Foundation
Project number: ED 159/2
Funding period: 1.4.2007 - 31.3.2009 and 1.1.2010 – 31.12.2010