“…To understand how the Rädler and shear-current effects may affect large-scale dynamos in rotating shear flows, let us have a look at the mean-field dynamo problem for small-scale homogeneous turbulence forced isotropically and non-helically in the simplest possible unstratified, rotating shearing sheet configuration, , , for which and the only non-zero components of the deformation tensor are . Under these assumptions, there are no mean and effects and the kinematic evolution equations for the and components of a -dependent mean magnetic field (defined as the average over and of the total magnetic field) can be cast in the simple form where we have introduced a contracted generalised anisotropic turbulent diffusion tensor appropriate to the configuration of the problem, namely Using (4.8)–(4.10), it can be shown that where is the usual isotropic turbulent diffusion coefficient, is an anisotropic contribution to the tensor arising from the presence of the large-scale strain associated with the shear flow, and , and are contributions to the mean-field tensor arising (similarly to and ) from the presence of rotation, large-scale vorticity, and strain associated with the shear flow (for a detailed derivation, see Rädler & Stepanov 2006; Squire & Bhattacharjee 2015 a ).…”