Simulations of oblique transition in the spatial domain are presented,
covering the complete transition process into the turbulent regime. I
t is conjectured that the three stages identified here and elsewhere a
re universal for oblique transition in all shear flows: first a nonlin
ear generation of a streamwise vortex by the oblique waves, second a t
ransient growth of streaks from the vortex by the lift-up effect, and
third a breakdown of the streaks due to secondary instability.