Abstract

We study the stability of a barotropic vortex strip on a rotating sphere, as a simple model of jet streams. The flow is approximated by a piecewise-continuous vorticity distribution by zonal bands of uniform vorticity. The linear stability analysis shows that the vortex strip becomes stable as the strip widens or the rotation speed increases. When the vorticity constants in the upper and the lower regions of the vortex strip have the same positive value, the inner flow region of the vortex strip becomes the most unstable. However, when the upper and the lower vorticity constants in the polar regions have different signs, a complex pattern of instability is found, depending on the wavenumber of perturbations, and interestingly, a boundary far away from the vortex strip can be unstable. We also compute the nonlinear evolution of the vortex strip on the rotating sphere and compare with the linear stability analysis. When the width of the vortex strip is small, we observe a good agreement in the growth rate of perturbation at an early time, and the eigenvector corresponding to the unstable eigenvalue coincides with the most unstable part of the flow. We demonstrate that a large structure of rolling-up vortex cores appears in the vortex strip after a long-time evolution. Furthermore, the geophysical relevance of the model to jet streams of Jupiter, Saturn and Earth is examined.

Highlights

  • Jet streams are the prominent flow structures observed in atmospheric flows on Earth and gas planets such as Jupiter & Saturn [1,2]

  • We have found that when the rotation speed is high, the boundaries do not stay on the sphere and tend to deviate from the surface of the sphere, because they are represented in three-dimensional Cartesian coordinates in the vortex contour dynamics model

  • We examine the geophysical relevance of the model for a vortex strip on a rotating sphere to jet streams in planets

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Summary

Introduction

Jet streams are the prominent flow structures observed in atmospheric flows on Earth and gas planets such as Jupiter & Saturn [1,2]. In view of the geophysical importance of zonal jets, we study the evolution of a latitudinal band region of a constant vorticity, called a vortex strip and investigate its stability. As a reference, the velocity fields induced by the piecewise constant vorticity for the vortex strip and by the vorticity distribution f (θ, φ) = 2Ω sin θ of the solid body rotation are shown as the thin (blue) curve and the dotted (red) curve, respectively. We approximate the continuous vorticity distribution induced by the solid body rotation of the sphere with the M + 1 zonal bands with piecewise-constant vorticity separated by M latitudinal boundaries.

Linear stability analysis
Nonlinear evolutions of the vortex strip
Geophysical relevance to planetary jet streams
Conclusion
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