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Fig. 6

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The scaling of a) G/Re2, which is proportional to the accretion rate and viscosity parameter β, decays slowly with Re while having an amplitude that varies with the rotation number RΩ (see Fig. 4). b) The effects of global rotation can be accounted for by compensating G/Re2 by the fits f(RΩ) given in Eq. (12). The measurements from Twente are shown as red squares. The Maryland data are given by black circles, except for quasi-Keplerian flows (RΩ ≤ −1), which are indicated by blue diamonds. The green continuous line is the theoretical fit given in Eq. (14) normalized by f(RΩ = −0.2755), which corresponds to Ω2 = 0.

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