It is shown that toroidal-magnetic-field ripple-induced particle flux
can drive poloidal E x B speed to bifurcate over the local maximum of
the nonlinear poloidal (or parallel) viscosity. Here, E is the electri
c field, and B is the magnetic field. This mechanism, together with th
e turbulence suppression due to the radial gradient of the E x B and d
iamagnetic angular velocity, is employed to explain the enhanced rever
sed shear mode observed in the core region of tokamaks.