We investigate the quasi-static evolution of an idealized magnetic con
figuration in the solar corona that is subjected to photospheric shear
ing motions. The initial, unsheared field in our calculations is a mag
netic dipole located at the center of the Sun. The assumed photospheri
c shearing motions are latitude-dependent and antisymmetric about the
equator. The quasi-static evolution of the coronal field is calculated
using the magneto-frictional method. A key difference between our stu
dy and previous work is that the outer computational boundary is place
d exceedingly far from the solar surface where the shearing motions ar
e applied. This is achieved by writing the basic equations of the magn
eto-frictional method in terms of the logarithm of radial distance. We
find that initially, the coronal magnetic field expands steadily as t
he footpoint displacement is increased. However, when the footpoint di
splacement exceeds a certain critical amount, the qualitative behavior
of the evolving field suddenly changes, so that the outward expansion
of the field lines becomes a much more rapidly increasing function of
the footpoint displacement. We propose that this sudden transition to
a regime with very sensitive dependence on boundary conditions plays
an important role in the onset of eruptive phenomena in the solar atmo
sphere.