684 18 Applications of complex variables
shows that a function that is the boundary value of a function analytic and tending to zero
at infinity in the upper half-plane is automatically an eigenvector of H with eigenvalue
−i. Similarly a function that is the boundary value of a function analytic and tending
to zero at infinity in the lower half-plane will be an eigenvector with eigenvalue +i.(A
function analytic in the entire complex plane and tending to zero at infinity must vanish
identically by Liouville’s theorem.)
Returning now to our original f , which had eigenvalue −i, and decomposing it as
f (x) = f
R
(x) + if
I
(x), we find that (18.75) becomes
f
I
(x) = (Hf
R
)(x),
f
R
(x) =−(Hf
I
)(x). (18.77)
Conversely, if we are given a real function u(x) and set v (x ) = (Hu)(x ), then, under
some mild restrictions on u (that it lie in some L
p
(R), p > 1, for example, in which case
v(x) is also in L
p
(R)) the function
f (z ) =
1
2πi
∞
−∞
u(x ) + iv(x)
x − z
dx (18.78)
will be analytic in the upper half-plane, tend to zero at infinity there and have u(x)+iv(x)
as its boundary value as z approaches the real axis from above. The last line of (18.77)
therefore shows that we may recover u(x) from v(x) as u(x) =−(Hv)(x). The Hilbert
transform H : L
p
(R) → L
p
(R) is therefore invertible, and its inverse is given by
H
−1
=−H. (Note that the Hilbert transform of a constant is zero, but the L
p
(R)
condition excludes constants from the domain of H , and so this fact does not conflict
with invertibility.)
Hilbert transforms are useful in signal processing. Given a real signal X
R
(t) we can
take its Hilbert transform so as to find the corresponding imaginary part, X
I
(t), which
serves to make the sum
Z(t) = X
R
(t) + iX
I
(t) = A(t)e
iφ(t)
(18.79)
analytic in the upper half-plane. This complex function is the analytic signal.
4
The real
quantity A(t) is then known as the instantaneous amplitude,orenvelope, while φ(t) is
the instantaneous phase and
ω
IF
(t) =
˙
φ(t) (18.80)
is called the instantaneous frequency (IF). These quantities are used, for example, in
narrow-band FM radio, in NMR, in geophysics and in image processing.
4
D. Gabor, J. Inst. Elec. Eng. (Part 3), 93 (1946) 429.