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Is a third scale of motion admissible in a boundary-current region?

  • Fulvio Crisciani
  • Fabio Cavallini
  • Renzo MosettiEmail author
Regular Article
  • 24 Downloads

Abstract.

The question arises whether an intermediate scale of the motion, between those of a boundary-current region and of the interior, may take place in the inertial regime. We prove that the very geostrophic balance prevents this possibility. The same problem is investigated in the frictional regime as well.

References

  1. 1.
    J. Pedlosky, Geophysical Fluid Dynamics (Springer-Verlag, 1987) p. 710Google Scholar
  2. 2.
    F. Cavallini, F. Crisciani, Quasi-Geostrophic Theory of Oceans and Atmosphere (Springer-Verlag, 2013) p. 385Google Scholar
  3. 3.
    J. Pedlosky, Ocean Circulation Theory (Springer-Verlag, 1996) p. 453Google Scholar

Copyright information

© Società Italiana di Fisica and Springer-Verlag Berlin Heidelberg 2017

Authors and Affiliations

  1. 1.Dipartimento di FisicaUniversità di TriesteTriesteItaly
  2. 2.OGS-Istituto Nazionale di Oceanografia e di Geofisica SperimentaleTriesteItaly

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