A new mechanism is proposed for the generation of Tollmien-Schlichting (T-S
) waves by free-stream turbulence. For definiteness and self-consistency, t
he mechanism is described mathematically by using a triple-deck formalism.
The free-stream turbulence is represented by convecting gusts consisting of
the so-called vortical and entropy waves of small amplitude. We show that
suitable convecting gusts can interact with sound waves in the free stream
to produce a forcing that has the same time and length scales as those of t
he T-S waves, thereby exciting such waves in the vicinity of the lower bran
ch of the neutral stability curve. The T-S waves so produced have the order
of magnitude of epsilon(2)R(5/16), where epsilon is the amplitude of the f
ree-stream disturbance and R the global Reynolds number. The scale conversi
on is achieved without resorting to any non-homogeneity on the wall, and he
nce the mechanism operates in a flat boundary layer. Furthermore, the T-S w
aves so generated do not undergo any immediate decay, as they may do in som
e other receptivity processes. For homogeneous isotropic free-stream turbul
ence, the spectrum of the T-S waves is obtained. The efficiency of the rece
ptivity mechanism is assessed by parametric studies.