The development and interaction of solitary wave pulses is critical to
understanding wavy film flows on an inclined (or vertical) surface, S
ufficiently far downstream, the wave structure consists of a generally
irregular sequence of solitary waves independent of the conditions at
the inlet. The velocity of periodic solitary waves is found to depend
on their frequency and amplitude. Larger pulses travel faster; this p
roperty, plus a strong inelasticity, causes larger pulses to absorb ot
hers during interactions, leaving a nearly flat interface behind. Thes
e wave interactions lead to the production of solitary wave trains fro
m periodic small amplitude waves. The spacings between solitary waves
can be irregular for several different reasons, including the amplific
ation of ambient noise, and the interaction process itself. On the oth
er hand, this irregularity is suppressed by the addition of periodic f
orcing.