Low frequency modulation of jets in quasigeostrophic turbulence

TL;DR

This study numerically investigates quasigeostrophic turbulence on a beta-plane, revealing low-frequency Rossby wave modulation of jets, spectral peaks, and energy transfer characteristics related to the deformation scale.

Contribution

It demonstrates the presence of Rossby wave modulation in jet formation and energy spectra, linking spectral features to the modified Rhines scale and dispersion relations.

Findings

Spectral peaks at higher frequencies indicate Rossby wave activity.

Energy spectra follow a -5/3 power-law distribution.

Jets are modulated by westward propagating Rossby waves.

Abstract

Quasigeostrophic turbulence on a beta-plane with a finite deformation radius is studied nu- merically, with particular emphasis on frequency and combined wavenumber-frequency do- main analyses. Under suitable conditions, simulations with small-scale random forcing and large-scale drag exhibit a spontaneous formation of multiple zonal jets. The first hint of wave-like features is seen in the distribution of kinetic energy as a function of frequency; specifically, for progressively larger deformation scales there are systematic departures in the form of isolated peaks (at progressively higher frequencies) from a power-law scaling. Con- comitantly, there is an inverse flux of kinetic energy in frequency space which extends to lower frequencies for smaller deformation scales. The identification of these peaks as Rossby waves is made possible by examining the energy spectrum in frequency-zonal wavenumber and frequency-meridional wavenumber diagrams. In fact, the modified Rhines scale turns out to be a useful measure of the dominant meridional wavenumber of the modulating Rossby waves; once this is fixed, apart from a spectral peak at the origin (the steady jet), almost all the energy is contained in westward propagating disturbances that follow the theoretical Rossby dispersion relation. Quite consistently, noting that the zonal scale of the modulating waves is restricted to the first few wavenumbers, the energy spectrum is almost entirely contained within the corresponding Rossby dispersion curves on a frequency-meridional wavenumber diagram. Cases when jets do not form are also considered; once again, there is a hint of Rossby wave activity, though the spectral peaks are quite muted. Further, the kinetic energy scaling in frequency domain follows a -5/3 power-law and is distributed much more broadly in frequency-wavenumber diagrams