Vv. Pipin et al., THE ROTATIONAL QUENCHING OF THE ROTATION-INDUCED KINETIC ALPHA-EFFECT, Geophysical and astrophysical fluid dynamics, 83(1-2), 1996, pp. 119-133
A theory of the non-diffusive anisotropic kinetic alpha-effect (''Gamm
a-effect'') for density-stratified rotating turbulent fluids is develo
ped. No limitations on the rotation rate are imposed and the fully non
linear dependence of the Gamma-effect on the angular velocity is studi
ed. When the Coriolis number, Omega = 2 tau(corr) Omega, is small the
dimensionless ''dynamo number'', C-Gamma, characterising the power of
the Gamma-effect, grows with Omega. The dependence, however, reaches
a maximum for Omega'' similar or equal to 2. For still higher rotatio
n rates C-Gamma decreases as 1/Omega. In opposition, the correspondin
g number, C-alpha, of the hydromagnetic alpha(2)-dynamo problems remai
ns finite for very large Omega. Hence, for fast rotation the hydrodyn
amic Gamma-effect is small while the hydromagnetic alpha-effect remain
s large. In consequence, the large-scale magnetic and velocity structu
res are expected to be equal power in slowly rotating objects. In the
rapid rotators, however, generation of the large-scale flows is proble
matic.