One mechanism by which laminar flow becomes turbulence is through the insta
bility of vortex interaction. The nonlinear evolution of the interactions b
etween the h-vortex and the secondary closed vortex has been investigated.
This nonlinear instability process leads to some fundamental changes in the
topology of flows. Experimental observations are presented here showing th
e formation of a chain of ring-like vortices, which generate high-frequency
spikes on time traces in a transitional boundary layer.