Interplay of waves and eddies in rotating stratified turbulence and the link with kinetic-potential energy partition

Abstract

The interplay between waves and eddies in stably stratified rotating flows is investigated by means of world-class direct numerical simulations using up to $3072^3$ grid points. Strikingly, we find that the shift from vortex to wave dominated dynamics occurs at a wavenumber $k_R$ which does not depend on Reynolds number, suggesting that partition of energy between wave and vortical modes is not sensitive to the development of turbulence at the smaller scales. We also show that $k_R$ is comparable to the wavenumber at which exchanges between kinetic and potential modes stabilize at close to equipartition, emphasizing the role of potential energy, as conjectured in the atmosphere and the oceans. Moreover, $k_R$ varies as the inverse of the Froude number as explained by the scaling prediction proposed, consistent with recent observations and modeling of the Mesosphere-Lower Thermosphere and of the ocean.

References in corpus (4)

• Evidence for Bolgiano-Obukhov scaling in rotating stratified turbulence using high-resolution direct numerical simulations
• Large-scale anisotropy in stably stratified rotating flows
• Vortical and Wave Modes in 3D Rotating Stratified Flows: Random Large Scale Forcing
• Absorption of waves by large scale winds in stratified turbulence

Cited by in corpus (6)

• Dual constant-flux energy cascades to both large scales and small scales
• Scaling laws for mixing and dissipation in unforced rotating stratified turbulence
• Inverse cascades and resonant triads in rotating and stratified turbulence
• Single-particle Lagrangian statistics from direct numerical simulations of rotating-stratified turbulence
• Phenomenology of two-dimensional stably stratified turbulence under large-scale forcing
• Efficient kinetic Lattice Boltzmann simulation of three-dimensional Hall-MHD Turbulence