Abstract
We conduct computations of rotating Rayleigh–Bénard convection in the so-called geostrophic regime, characterized by strong thermal forcing (high Rayleigh numbers) and strong rotation (small Ekman numbers). We employ the full Navier–Stokes equations in our computations and compare no-slip and stress-free boundaries for the plates. The Ekman boundary layers, that exist in the no-slip case but not for stress-free, enhance convective heat transfer and prevent the formation of large-scale flow structures.
Original language | English |
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Publication status | Published - 1 Jan 2015 |
Event | 15th European Turbulence Conference, ETC 2015 - Delft, Netherlands Duration: 25 Aug 2015 → 28 Aug 2015 Conference number: 15 |
Conference
Conference | 15th European Turbulence Conference, ETC 2015 |
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Abbreviated title | ETC 2015 |
Country/Territory | Netherlands |
City | Delft |
Period | 25/08/15 → 28/08/15 |