The nature of radial flow during retreating blade stall on a two-bladed teetering rotor with cyclic pitch variation is investigated using laser sheet visualization and particle image velocimetry in a low-speed wind tunnel. The velocity field above the retreating blade at 270 • azimuth shows the expected development of a radially directed jet layer close to the blade surface in the otherwise separated flow region. This jet is observed to break up into discrete structures, limiting the spanwise growth of the radial velocity in the jet layer. The discrete structures are shown to derive their vorticity from the "radial jet" layer near the surface, rather than from the freestream at the edge of the separated region. The separation line determined using velocity data shows the expected spanwise variation. The results of this study are also correlated in a limited range of extrapolation to the phenomena encountered on a full-scale horizontal axis wind turbine in yaw.
Nomenclaturea o wind deficit factor c chord length, m k reduced frequency R rotor radius, m Re Reynolds number r radial/spanwise location, m V c velocity component in the plane of the wind turbine, m/s V i induced velocity for the rotor setup, m/s V n velocity component normal to the wind turbine, m/s V r radial velocity, m/s V tw tangential component of velocity to wind turbine blade, m/s V w freestream velocity for wind turbine, m/s V ∞ freestream velocity for rotor setup, m/s x chordwise location, m z axial location, m α ir induced angle of attack on rotor setup, deg α iw induced angle of attack on wind turbine, deg α pr blade pitch of rotor setup, deg α pw blade pitch of wind turbine, deg α r angle of attack of rotor setup, deg α w angle of attack of wind turbine, deg