We now consider inversion of the magnitude expression to estimate
. We begin by observing the half-height width
of
the smeared peak in the FFT magnitude domain.9 Since the half height width will not necessarily occur at
an integer
value, linear or other interpolation may be used to
more accurately estimate
. If our
value is large
enough to guarantee that our approximation is valid at this point
(discussed in the previous subsection), the half height width
corresponds to
exactly. This is because the raised
cosine is at half height when its argument is
, and
solving for
in this situation yields
, or
.
As suggested previously, ensuring that our model is valid now
becomes trivial: if
for our
desired
value, the model is valid.
We now calculate
by solving the half height expression
for
. That is,
As noted above, the approximation in equation 115 will prove more reliable than the phase inversion model below due to error propagation. This is not to say that the phase inversion algorithm is devoid of merit; the error simply propagates in a less well-modeled way than in the magnitude case.