Wind tunnel experiments are performed on a body of revolution with aft-section
designed to be an axisymmetric Stratford ramp (i.e. the flow over the ‘ramp’ experiences
an adverse pressure gradient that causes it to be continuously on the verge of
separation). Digital particle image velocimetry (DPIV) measurements over the ramp
reveal a thick boundary layer that is characterized by self-similar velocity profiles with
a large wake component and organized vorticity structures. The mean skin friction
quickly drops to a value near zero.The sensitivity of the boundary layer to the degree of severity of the adverse
pressure gradient is investigated by testing two additional ramps; one is slightly more
conservative (i.e. less steep) than the Stratford ramp while the other is slightly more
radical (i.e. steeper). In comparison to the Stratford ramp, the conservative ramp is
characterized by a thinner boundary layer, with velocity profiles that start attached
and gradually develop a large wake component, a much more gradual drop in the skin
friction, and vorticity that is concentrated very close to the wall. On the other hand,
the boundary layer over the radical ramp is unsteady and separates intermittently.
Measurements of the drag force on each of the three bodies confirm that the Stratford
ramp experiences the least amount of drag.Finally, additional data are gathered on the windward and leeward sides of the
Stratford ramp when subjected to a small angle of attack. This case exhibits a more
complex flow structure: the flow remains attached over the windward side of the
ramp while separating over the leeward side.