Nordita Astrophysics Seminars

Energetics, flux budgets and heat transport in stably stratified turbulence: theory, experiments, simulations and astrophysical applications

by Prof. Igor Rogachevskii (Ben-Gurion University of the Negev)

Europe/Stockholm
122:026

122:026

Description
We discuss physical background of the energy- and flux-budget turbulence closure based on the budget equations for the turbulent kinetic and potential energies and turbulent fluxes of momentum and buoyancy. The closure is designed for stratified geophysical and astrophysical flows from neutral to very stable stratification. In accordance to modern experimental and observational evidence, the closure implies maintaining of turbulence by the velocity shear or other source at any gradient Richardson number Ri, and distinguishes between the two principally different regimes: "strong turbulence" at Ri << 1 typical of boundary-layer flows and characterised by the practically constant turbulent Prandtl number; and "weak turbulence" at Ri > 1 typical of the free atmosphere or deep ocean, where turbulent Prandtl number asymptotically linearly increases with increasing Ri (which implies very strong suppression of the heat transfer compared to the momentum transfer). We also discuss resent experimental results on transport of temperature and velocity fluctuations in stably stratified forced turbulence. In the experiments in air flow with an imposed vertical temperature gradient, the turbulence is produced by two oscillating grids located nearby the side walls of the chamber. We demonstrated that for large frequencies of the grid oscillations, the temperature field can be considered as a passive scalar, while for smaller frequencies the temperature field behaves as an active field. The theoretical predictions based on the budget equations for turbulent kinetic energy, turbulent potential energy and turbulent heat flux, are in a good agreement with the experimental results. Finally we will discuss the results of numerical simulations and astrophysical applications.

S.S. Zilitinkevich, T. Elperin, N. Kleeorin, I. Rogachevskii, I. Esau, Boundary-Layer Meteorology, DOI:10.1007/s10546-012-9768-8