The formation of streaky velocity structures in the near wall region o
f turbulent boundary layers is studied through a simplified two-dimens
ional computational model in the plane normal to the average velocity.
It is shown that the redistribution of the longitudinal velocity by s
treamwise vortices produces features very similar to those observed in
the experiments, and that compact streamwise vortices form naturally
from more general vorticity distributions. It is also shown, both nume
rically and analytically, that one effect of the formation of the stre
aks is to increase the average wall friction, and it is suggested that
this effect is responsible for the higher friction in turbulent bound
ary layers, as opposed to laminar ones. An approximate quantitative an
alysis of the process supports this assumption.