The effectiveness with which various sources excite convective instabi
lities in a boundary layer is found by a simple method. Chosen field v
alues of the adjoint to the Tollmien-Schlichting eigensolution, normal
ized appropriately, indicate the amplitude of the unstable disturbance
which will result for direct time-harmonic forcing by sources of mome
ntum, mass and vorticity, as well as by boundary motions. For the Blas
ius boundary layer, forcing in the vicinity of the critical layer indu
ces the largest response. At this position, the response to forcing in
the wall-normal direction is typically 5% of that resulting from stre
amwise forcing of the same magnitude. At the wall, normal motions elic
it a much stronger response than streamwise motions. Forcing close to
the lower branch of the neutral stability curve leads to the largest r
esponse. The adjoint field values are equivalent to the residues of Fo
urier-inversion integrals. This equivalence is discussed for two probl
ems; the vibrating ribbon problem and excitation of an inviscid free s
hear layer by a vorticity source. The efficiency factor is calculated
for the scattering of 'acoustic' waves into Tollmien-Schlichting waves
in the presence of small surface roughness, at a finite Reynolds numb
er, based on the Orr-Sommerfeld operator. This is achieved by using th
e solution of an inhomogeneous adjoint problem. The results are compar
ed with the asymptotic solutions obtained from triple-deck theory, and
agree with previous finite-Reynolds-number calculations.