Nonlocalized receptivity to vortical free-stream disturbances is analy
zed for a Blasius boundary layer over a wavy surface. Vortical disturb
ances are rescaled through an interaction with steady disturbances gen
erated by the surface waviness. The rescaled disturbances provide a di
stributed energy transfer to the natural eigenmodes when conditions ar
e close to resonance; this occurs in the neighborhood of the lower bra
nch of neutral stability. Downstream of the energy transfer, the trave
ling wave solution is dominated by the natural eigenmode. Forcing from
the vortical disturbances is concentrated in the outer region of the
boundary layer. This leads to a relatively weak receptivity as compare
d to the acoustic problem. Total receptivity amplitudes are approximat
ely ten times larger than for localized vortical receptivity, but appr
oximately fifty times smaller than for nonlocalized acoustic receptivi
ty.