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On the representation of Rossby waves on the β-plane by a piecewise uniform potential vorticity distribution

Published online by Cambridge University Press:  01 November 2010

DA ZHU
Affiliation:
Department of Geophysical Sciences, University of Chicago, Chicago, IL 60637, USA
NOBORU NAKAMURA*
Affiliation:
Department of Geophysical Sciences, University of Chicago, Chicago, IL 60637, USA
*
Email address for correspondence: nnn@uchicago.edu

Abstract

To bridge quasi-geostrophic dynamics and its discrete representation by a series of piecewise constant potential vorticity (PV), the dispersion relation for the Rossby wave in the single-layer β-plane is compared with that for the normal mode of edge waves straddling an infinite series of PV discontinuities (‘PV staircase’). It is shown that the edge waves over evenly spaced, uniform-height PV steps converge to the Rossby wave on the β-plane as Δ → 0, L → 0, Δ/L = βeff (Δ, L and βeff are the step size, step separation and the effective β, respectively), whereas they reduce to the single-step edge wave in the short-wave limit. For sufficiently small step separations, the difference in the phase velocities of the edge wave and the Rossby wave scales as O(L2). Two effects of increasing L on the zonal propagation are identified: (i) increased phase and group velocities in the short-wave limit due to an increased zonal wind at the PV steps and (ii) decreased phase and group velocities in the long-wave limit due to a decreased effective meridional tilt of the mode. The reduced tilt also severely limits the meridional group propagation. The relationship between the edge wave mode and the finite-difference approximation to the Rossby wave is also discussed.

Type
Papers
Copyright
Copyright © Cambridge University Press 2010

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References

REFERENCES

Dritschel, D. G. 1988 Contour surgery: a topological reconnection scheme for extended integrations using contour dynamics. J. Comput. Phys. 77, 240266.CrossRefGoogle Scholar
Dritschel, D. G. & Ambaum, M. H. P. 1997 A contour-advective semi-Lagrangian numerical algorithm for simulating fine-scale conservative dynamical fields. Q. J. R. Meteorol. Soc. 123, 10971130.Google Scholar
Dritschel, D. G. & McIntyre, M. E. 2008 Multiple jets as PV staircases: the phillips effect and the resilience of eddy-transport barriers. J. Atmos. Sci. 65, 855874.CrossRefGoogle Scholar
Dritschel, D. G. & Scott, R. K. 2009 On the simulation of nearly inviscid two-dimensional turbulence J. Comput. Phys. 228, 27072711.CrossRefGoogle Scholar
Durran, D. 1998 Numerical Methods for Wave Equations in Geophysical Fluid Dynamics. Springer.Google Scholar
Eady, E. 1949 Long waves and cyclone waves. Tellus 1, 3352.CrossRefGoogle Scholar
Hoskins, B. J., McIntyre, M. E. & Robertson, A. W. 1985 On the use and significance of isentropic potential vorticity maps. Q. J. R. Meteorol. Soc. 111, 877946.CrossRefGoogle Scholar
Juckes, M. N. 1995 Instability of surface and upper-tropospheric shear lines. J. Atmos. Sci. 52, 32473262.2.0.CO;2>CrossRefGoogle Scholar
Legras, B. & Dritschel, D. G. 1993 A comparison of the contour surgery and pseudo-spectral methods. J. Comput. Phys. 104, 287302.CrossRefGoogle Scholar
Marcus, P. S. 1993 Jupiter's great red spot and other vortices. Annu. Rev. Astron. Astrophys. 31, 523573.CrossRefGoogle Scholar
Martius, O., Schwierz, C. & Davies, H. C. 2010 Tropopause-level waveguides. J. Atmos. Sci. 67, 866879.CrossRefGoogle Scholar
Nakamura, N. 1993 An illustrative model of instabilities in meridionally and vertically sheared flows. J. Atmos. Sci. 50, 357376.2.0.CO;2>CrossRefGoogle Scholar
Nakamura, N. & Zhu, D. 2010 a Finite-amplitude wave activity and diffusive flux of potential vorticity in eddy-mean flow interaction. J. Atmos. Sci. 67, 27012716.CrossRefGoogle Scholar
Nakamura, N. & Zhu, D. 2010 b Formation of jets through mixing and forcing of potential vorticity: analysis and parameterization of beta-plane turbulence. J. Atmos. Sci. 67, 27172733.CrossRefGoogle Scholar
Rayleigh, Lord 1880 On the stability, or instability, of certain fluid motions. Proc. Lond. Math. Soc. 10, 5770.Google Scholar
Swanson, K. L. 2000 Stationary wave accumulation and the generation of low-frequency variability on zonally varying flows. J. Atmos. Sci. 57, 22622280.2.0.CO;2>CrossRefGoogle Scholar
Swanson, K. L., Kushner, P. J. & Held, I. M. 1997 Dynamics of barotropic storm tracks. J. Atmos. Sci. 54, 791810.2.0.CO;2>CrossRefGoogle Scholar