The ability of a second-moment closure to predict the three-componential me
an flow which results when a plane Couette flow is subjected to moderate an
ticyclonic system rotation is explored. The counterrotating streamwise-orie
nted roll cells, which may occur by the imposition of a destabilizing Corio
lis force field, are treated as an integral part of the steady mean motion
governed by the Reynolds-averaged Navier-Stokes equations. Near-wall effect
s are accounted for by Durbin's elliptic relaxation approach, while system
rotation only appears naturally in rotational stress-producing terms and in
the mean intrinsic vorticity in the non-linear pressure-strain model.
The model predictions mimicked the most striking effects of anticyclonic ro
tation, as observed in a series of recent direct numerical simulations. In
particular they reproduced the characteristic energetic roll-cell pattern,
which inevitably enhanced the cross-sectional mixing. The broadening of the
central core region, in which the primary mean velocity profile adjusted i
tself to make the absolute mean vorticity negligibly small, was well captur
ed by the predictions, together with the remarkable damping of the turbulen
t velocity fluctuations. The success of the predictions supports the view t
hat such large-scale structures as the rotational-induced roll cells should
be treated as a part of the resolved mean flow field, the obvious and phys
ically appealing implication being that the turbulence closure is left to r
epresent nothing but real turbulence.