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Steady States and Variability in Oceanic Zonal Flows

  • Dirk Olbers
  • Christoph Völker
Part of the NATO ASI Series book series (volume 44)

Abstract

The Antarctic Circumpolar Current (ACC) is the only oceanic flow system of large scale bearing similarity to the atmospheric zonal circulation. There is not only the obvious geometrical similarity — the zonal unboundedness of a current reaching all around the earth —, there are also deeper dynamical correspondences. Though the forcing is different, the dynamical balance of the zonal atmospheric flow and the ACC resides substantially on the excitation of and interaction with synoptic-scale eddies and the intricate correlation of the large-scale pressure field with respect to the underlying topography in shaping what is known as mountain drag in the atmospheric system and bottom form drag (or stress) in the oceanic case.

Keywords

Rossby Wave Momentum Balance Relative Vorticity Antarctic Circumpolar Current Form Stress 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer-Verlag Berlin Heidelberg 1996

Authors and Affiliations

  • Dirk Olbers
    • 1
  • Christoph Völker
    • 1
  1. 1.Alfred-Wegener-Institute for Polar and Marine ResearchBremerhavenGermany

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