Abstract

The incompressible 2D Euler equations on a sphere constitute a fundamental model in hydrodynamics. The long-time behaviour of solutions is largely unknown; statistical mechanics predicts a steady vorticity configuration, but detailed numerical results in the literature contradict this theory, yielding instead persistent unsteadiness. Such numerical results were obtained using artificial hyperviscosity to account for the cascade of enstrophy into smaller scales. Hyperviscosity, however, destroys the underlying geometry of the phase flow (such as conservation of Casimir functions), and therefore might affect the qualitative long-time behaviour. Here we develop an efficient numerical method for long-time simulations that preserve the geometric features of the exact flow, in particular conservation of Casimirs. Long-time simulations on a non-rotating sphere then reveal three possible outcomes for generic initial conditions: the formation of either 2, 3, or 4 coherent vortex structures. These numerical results contradict the statistical mechanics theory and show that previous numerical results, suggesting 4 coherent vortex structures as the generic behaviour, display only a special case. Through integrability theory for point vortex dynamics on the sphere we present a theoretical model which describes the mechanism by which the three observed regimes appear. We show that there is a correlation between a first integral $\gamma$ (the ratio of total angular momentum and the square root of enstrophy) and the long-time behaviour: $\gamma$ small, intermediate, and large yields most likely 4, 3, or 2 coherent vortex formations. Our findings thus suggest that the likely long-time behaviour can be predicted from the first integral $\gamma$.

Highlights

  • The motion of an ideal fluid restricted to the surface of a sphere is a fundamental model in oceanography, meteorology and astrophysics (see Majda & Bertozzi (2002); Dolzhansky (2012); Pedlosky (2013); Zeitlin (2018), and references therein)

  • We have found a different theory which explains the mechanisms by which the regimes appear: it is closely related to integrability theory for point vortex dynamics (PVD)

  • We have developed a new numerical algorithm for the Euler equations on a sphere that preserves, up to machine precision, the Casimir functions of (2.4)–(2.9) and nearly conserves the Hamiltonian

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Summary

Introduction

The motion of an ideal fluid restricted to the surface of a sphere is a fundamental model in oceanography, meteorology and astrophysics (see Majda & Bertozzi (2002); Dolzhansky (2012); Pedlosky (2013); Zeitlin (2018), and references therein). On the non-rotating sphere, Dritschel, Qi & Marston (2015) provided numerical evidence that, for randomly generated initial data, the long-time behaviour results in a non-steady interaction largely between two positive and two negative coherent vortex structures (referred to as vortex blobs in this paper) essentially governed by finite-dimensional point vortex dynamics. This is briefly how the mechanism works:. If momentum is close to zero one still obtains ‘integrable-like’ dynamics since integrable systems are stable in the sense of KAM theory for small perturbations (the small momentum configuration can be viewed as a perturbation of a zero momentum configuration) This explains why 4 vortex blobs is the stable long-time regime for fluid configurations with a small γ parameter. Our main focus is on the non-rotating sphere, we have included in appendix A numerical examples of Rossby–Haurwitz waves on a rotating sphere, to illustrate the usability of the new method in the rotating case (relevant for quasi-geostrophic flows in atmospheric dynamics)

Numerical integration algorithm
Spatial discretization via geometric quantization
The quantized system
Time discretization
Complexity
Time scaling
Initial data with zero momentum
Generic initial data
Zero momentum case
Conclusions and outlook
Full Text
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