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Classical and symmetrical horizontal convection: detaching plumes and oscillations

Philipp Reiter, Olga Shishkina

2020Journal of Fluid Mechanics26 citationsDOIOpen Access PDF

Abstract

Classical and symmetrical horizontal convection is studied by means of direct numerical simulations for Rayleigh numbers Ra up to 3 10 12 and Prandtl numbers Pr = 0.1, 1 and 10. For both set-ups, a very good agreement in global quantities with respect to heat and momentum transport is attained. Similar to Shishkina & Wagner (Phys. Rev. Lett., vol. 116, 2016, 024302), we find Nusselt number Nu versus Ra scaling transitions in a region 10 8 Ra 10 11 . Above a critical Ra, the flow undergoes either a steady-oscillatory transition (small Pr) or a transition from steady state to a transient state with detaching plumes (large Pr). The onset of the oscillations takes place at Ra Pr -1 5 10 9 and the onset of detaching plumes at Ra Pr 5/4 9 10 10 . These onsets coincide with the onsets of scaling transitions.

Topics & Concepts

MechanicsConvectionPlumeGeologyGeophysicsClassical mechanicsPhysicsMeteorologyFluid Dynamics and Turbulent FlowsMeteorological Phenomena and SimulationsWind and Air Flow Studies