Abstract

Using high-resolution direct numerical simulation and arguments based on the kinetic energy flux ΠuΠ_u, we demonstrate that for stably stratified flows, the kinetic energy spectrum Eu(k)∼k−11/5E_u(k) \sim k^{-11/5}, the entropy spectrum Eθ(k)∼k−7/5E_θ(k) \sim k^{-7/5}, and Πu(k)∼k−4/5Π_u(k) \sim k^{-4/5} (Bolgiano-Obukhov scaling). This scaling is due to the depletion of kinetic energy because of buoyancy. For weaker buoyancy in stratified flows, Eu(k)E_u(k) follows Kolmgorov's spectrum with a constant energy flux. We also argue that for Rayleigh Bénard convection, the Bolgiano-Obukhov scaling will not hold for the bulk flow due to the positive energy supply by buoyancy and non-decreasing Πu(k)Π_u(k).

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