Abstract

Weakly-rotating turbulent Rayleigh-Benard convection was studied experimentally and numerically. With increasing rotation and large enough Rayleigh number an abrupt transition from a turbulent state with nearly rotation-independent heat transport to another turbulent state with enhanced heat transfer is observed at a critical inverse Rossby number 1/Roc≃0.41/Ro_c \simeq 0.4. Whereas for 1/Ro<1/Roc1/Ro < 1/Ro_c the strength of the large-scale convection-roll is either enhanced or essentially unmodified depending on parameters, its strength is increasingly diminished beyond 1/Roc1/Ro_c where it competes with Ekman vortices that cause vertical fluid transport and thus heat-transfer enhancement.

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