The generation of zonal jets by large-scale mixing

R. K. Scott*, A. -S. Tissier

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

9 Citations (Scopus)

Abstract

The development of zonal flows on a midlatitude beta-plane subject to a time-varying topographic forcing is investigated in a series of numerical integrations in which the forcing is concentrated at large scales, and in which the usual two-dimensional inverse energy cascade is absent. In contrast to the case of small-scale forcing, where mixing of potential vorticity occurs largely through the action of small-scale eddies, mixing of potential vorticity in this case occurs predominantly in latitudinally localized Rossby wave critical layer regions, whose width grows continuously in time due to the entrainment of background fluid. The potential vorticity is found to organize into a piecewise constant staircase-like profile, monotonic in latitude, provided the ratio L-Rh/L-f greater than or similar to 1, where L-Rh is the usual Rhines scale and L-f is the scale of the forcing; this may be regarded as supplemental to the condition L-Rh/L-epsilon greater than or similar to 6, where L-epsilon = (epsilon/beta(3))(1/5) and epsilon is the rate of energy input, obtained recently [R. K. Scott and D. G. Dritschel, "The structure of zonal jets in geostrophic turbulence," J. Fluid Mech. 711, 576-598 (2012)] for the case of small-scale forcing. The numerical results further suggest that the nature of the potential vorticity mixing is controlled by the ratio L-epsilon/L-f, and occurs predominantly in critical layers when L-epsilon/L-f less than or similar to 1/6. A combined condition for staircase formation may therefore be expressed as L-Rh/L-epsilon greater than or similar to max{6, L-f/L-epsilon}. Finally, in a separate set of experiments it is shown that when forcing is represented by an additive source term in the evolution equation, as is common practice in numerical investigations of two-dimensional turbulence, the effect of non-conservation of potential vorticity may obscure the development of the staircase profile in the critical layer mixing dominated regime. (C) 2012 American Institute of Physics. [http://dx.doi.org/10.1063/1.4771991]

Original languageEnglish
Article number126601
Number of pages15
JournalPhysics of Fluids
Volume24
Issue number12
DOIs
Publication statusPublished - Dec 2012

Keywords

  • BETA-PLANE TURBULENCE
  • BAROTROPIC MODEL
  • BREAKING
  • WAVES
  • STRATOSPHERE
  • TRANSPORT
  • SPECTRA
  • FLOWS

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