Recent analysis of the helioseismic observations indicate that the previous
ly observed surface torsional oscillations extend significantly downwards i
nto the solar convection zone.
In an attempt to understand these oscillations, we study the nonlinear coup
ling between the magnetic field and the solar differential rotation in the
context of a mean field dynamo model, in which the nonlinearity is due to t
he action of the azimuthal component of the Lorentz force of the dynamo gen
erated magnetic field on the solar angular velocity. The underlying zero or
der angular velocity is Chosen to be consistent with the most recent helios
eismic data.
The model produces butterfly diagrams which are in qualitative agreement wi
th the observations. It displays torsional oscillations that penetrate into
the convection zone, and which with time migrate towards the equator. The
period of these oscillations is found to be half that of the period of the
global magnetic fields. This is compatible with the observed period of the
surface torsional oscillations. Inside the convection zone, this is a testa
ble prediction that is not ruled out by the observations so far available.