Analysis of scale-dependent kinetic and potential energy in sheared, stably stratified turbulence

TL;DR

This paper analyzes how kinetic and potential energy vary across scales in sheared, stratified turbulence using DNS data, revealing scale-dependent energy fluxes, the significance of sub-grid effects, and changes in flow topology.

Contribution

It provides a detailed scale-by-scale energy budget analysis in stratified turbulence, highlighting the roles of different physical mechanisms and sub-grid contributions.

Findings

Mean TKE exceeds TPE at large scales, difference decreases at smaller scales.

Buoyancy always converts TKE to TPE, no positive buoyancy observed.

PDF of flow invariants becomes symmetric at larger scales, indicating balanced vortex stretching and compression.

Abstract

Budgets of turbulent kinetic energy (TKE) and turbulent potential energy (TPE) at different scales $\ell$ in sheared, stably stratified turbulence are analyzed using a filtering approach. Competing effects in the flow are considered, along with the physical mechanisms governing the energy fluxes between scales, and the budgets are used to analyze data from direct numerical simulation (DNS) at buoyancy Reynolds number $Re_b=O(100)$. The mean TKE exceeds TPE by an order of magnitude at the large scales, with the difference reducing as $\ell$ is decreased. At larger scales, buoyancy is never observed to be positive, with buoyancy always converting TKE to TPE. As $\ell$ is decreased, the probability of locally convecting regions increases, though it remains small at scales down to the Ozmidov scale. The TKE and TPE fluxes between scales are both downscale on average and their instantaneous values are positively correlated, but not strongly so, and this occurs due to the different physical mechanisms that govern these fluxes. Moreover, the contribution to these fluxes arising from the sub-grid fields are shown to be significant, in addition to the filtered scale contributions associated with the processes of strain-self amplification, vortex stretching, and density gradient amplification. Probability density functions (PDFs) of the $Q,R$ invariants of the filtered velocity gradient are considered. Unlike isotropic turbulence, as $\ell$ increases the sheared-drop shape of the PDF disappears and the PDF becomes symmetric about $R=0$, meaning regions of vortex stretching and compression become equi-probable, as well as regions of strain amplification or suppression.