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Self-Similarity in Decaying Two-Dimensional Stably Stratified Adjustment

Fluid Dynamics 2015-06-26 v2 Atmospheric and Oceanic Physics

Abstract

The evolution of large-scale density perturbations is studied in a stably stratified, two-dimensional flow governed by the Boussinesq equations. As is known, intially smooth density (or temperature) profiles develop into fronts in the very early stages of evolution. This results in a frontally dominated k1k^{-1} potential energy spectrum. The fronts, initially characterized by a relatively simple geometry, spontaneously develop into severely distorted sheets that possess structure at very fine scales, and thus there is a transfer of energy from large to small scales. It is shown here that this process culminates in the establishment of a k5/3k^{-5/3} kinetic energy spectrum, although its scaling extends over a shorter range as compared to the k1k^{-1} scaling of the potential energy spectrum. The establishment of the kinetic energy scaling signals the onset of enstrophy decay which proceeds in a mildly modulated exponential manner and possesses a novel self-similarity. Specifically, the self-similarity is seen in the time invariant nature of the probability density function (\pdf{}) associated with the normalized vorticity field. Given the rapid decay of energy at this stage, the spectral scaling is transient and fades with the emergence of a smooth, large-scale, very slowly decaying, (almost) vertically sheared horizontal mode with most of its energy in the potential component -- i.e. the Pearson-Linden regime.

Keywords

Cite

@article{arxiv.physics/0607045,
  title  = {Self-Similarity in Decaying Two-Dimensional Stably Stratified Adjustment},
  author = {Jai Sukhatme and Leslie M. Smith},
  journal= {arXiv preprint arXiv:physics/0607045},
  year   = {2015}
}

Comments

18 pages. Revised text. Figures not included (due to file size limits). Version with figs is available at the first author's website

R2 v1 2026-07-22T19:11:10.801Z