186 6 Fourier Series and Integrals with Applications
The peak overshoot occurs at a local maximum of the partial sum s
n
(x)
so that
0=s
′
n
(x)=
4
π
n
k=1
cos (2k − 1) x
=
2
π sin x
n
k=1
2sinx cos (2k − 1) x
=
2
π sin x
n
k=1
[sin 2kx − sin (2k − 2) x]
=
2sinnx
π sin x
. (6.7.8)
This leads to the points of maximum at x =
π
2n
,
2π
2n
,...,(2n − 1)
π
2n
so
that the first peak to the right of the origin occurs at x =
π
2n
. So, the value
of s
n
(x)atthispointis
s
n
π
2n
=
2
π
·
π
n
n
k=1
sin (2k − 1)
π
2n
(2k − 1)
π
2n
.
In the limit as n →∞, this becomes
lim
n→∞
s
n
π
2n
=
2
π
lim
n→∞
π
n
n
k=1
sin (2k − 1)
π
2n
(2k − 1)
π
2n
=
2
π
π
0
sin x
x
dx =
2
π
(1.852) = 1.179.
Instead of a maximum value 1, it turns out to be 1.179 approximately.
If the overshoot is compared to the jump in the function it is about
1
2
(1.179 − 1) × 100% ∼ 9%. The onset of the Gibbs phenomenon is shown
in the Figure 6.7.3.
Historically, this phenomenon was first observed by a physicist A.
Michelson (1852–1931) at the end of the nineteenth century. In order to
calculate some Fou rier coefficients of a function graphically, he developed
equipment that is called a harmonic analyser and synthesizer. He calcu-
lated some partial sums, s
n
, of a given function f graphically. Michelson
also observed from this graphical representation that, for some functions,
the graphs of s
n
were very close to the function. However, for the sgn
function, the graphs of the partial sums exhibit a large error in the neigh-
borhood of the origin, x = 0 and x =+
π (the jump discontinuities of
the function) independent of the number of terms in the partial sums. It
was J.W. Gibbs (1839–1903) who first provided the explanation for this
strikingly new phenomenon and showed that these large errors were not as-
sociated with nu merical computations. Indeed, he further showed that the