Long frontal waves and dynamic scaling in freely evolving equivalent barotropic flow

Belle Helen Burgess, David Gerard Dritschel

Research output: Contribution to journalArticle

2 Citations (Scopus)

Abstract

We present a scaling theory that links the frequency of long frontal waves to the kinetic energy decay rate and inverse transfer of potential energy in freely evolving equivalent barotropic turbulence. The flow energy is predominantly potential, and the streamfunction makes the dominant contribution to potential vorticity (PV) over most of the domain, except near PV fronts of width O(LD), where LD is the Rossby deformation length. These fronts bound large vortices within which PV is well-mixed and arranged into a staircase structure. The jets collocated with the fronts support long-wave undulations, which facilitate collisions and mergers between the mixed regions, implicating the frontal dynamics in the growth of potential-energy-containing flow features. Assuming the mixed regions grow self-similarly in time and using the dispersion relation for long frontal waves (Nycander et al., Phys. Fluids A, vol. 5, 1993, pp. 1089–1091) we predict that the total frontal length and kinetic energy decay like t-1/3, while the length scale of the staircase vortices grows like t1/3 . High-resolution simulations confirm our predictions.
Original languageEnglish
Article numberR3
Number of pages12
JournalJournal of Fluid Mechanics
Volume866
Early online date18 Mar 2019
DOIs
Publication statusPublished - 10 May 2019

Keywords

  • Quasi-geostrophic flows
  • Vortex dynamics

Fingerprint

Dive into the research topics of 'Long frontal waves and dynamic scaling in freely evolving equivalent barotropic flow'. Together they form a unique fingerprint.

Cite this