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Ocean Science An interactive open-access journal of the European Geosciences Union
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Volume 5, issue 2
Ocean Sci., 5, 173-190, 2009
https://doi.org/10.5194/os-5-173-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: The MERSEA Project

Ocean Sci., 5, 173-190, 2009
https://doi.org/10.5194/os-5-173-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

  02 Jun 2009

02 Jun 2009

Evaluating two numerical advection schemes in HYCOM for eddy-resolving modelling of the Agulhas Current

B. C. Backeberg1,2,3, L. Bertino2,3, and J. A. Johannessen2,3,4 B. C. Backeberg et al.
  • 1Department of Oceanography, University of Cape Town, South Africa
  • 2Mohn-Sverdrup Center for Global Ocean Studies and Operational Oceanography, Norway
  • 3Nansen Environmental and Remote Sensing Center, Norway
  • 4Geophysical Institute, University of Bergen, Norway

Abstract. A 4th order advection scheme is applied in a nested eddy-resolving Hybrid Coordinate Ocean Model (HYCOM) of the greater Agulhas Current system for the purpose of testing advanced numerics as a means for improving the model simulation for eventual operational implementation. Model validation techniques comparing sea surface height variations, sea level skewness and variogram analyses to satellite altimetry measurements quantify that generally the 4th order advection scheme improves the realism of the model simulation. The most striking improvement over the standard 2nd order momentum advection scheme, is that the southern Agulhas Current is simulated as a well-defined meandering current, rather than a train of successive eddies. A better vertical structure and stronger poleward transports in the Agulhas Current core contribute toward a better southwestward penetration of the current, and its temperature field, implying a stronger Indo-Atlantic inter-ocean exchange. It is found that the transport, and hence this exchange, is sensitive to the occurrences of mesoscale features originating upstream in the Mozambique Channel and southern East Madagascar Current, and that the improved HYCOM simulation is well suited for further studies of these inter-actions.

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