Fluid flowing down an inclined plane commonly exhibits a fingering ins
tability in which the. contact line corrugates. We show that below a c
ritical inclination angle the base state before the instability is lin
early stable. Several recent experiments explore inclination angles be
low this critical angle, yet all clearly show the fingering instabilit
y. We explain this paradox by showing that regardless of the long time
linear stability of the front, microscopic scale perturbations at the
contact Line grow on a transient time scale to a size comparable with
the macroscopic structure of the front. This amplification is suffici
ent to excite nonlinearities and thus initiate finger formation. The a
mplification is a result of the well-known singular dependence of the
macroscopic profiles on the microscopic length scale near the contact
line. Implications for other types of Forced contact lines are discuss
ed. (C) 1997 American Institute of Physics.