Abstract
A technique is described for obtaining the asymptotic behaviour at large
λ
of integrals having the form
I
(
λ
) = ∫
g(x) p{λf(x)} dx
, where
p
is an arbitrary periodic function with mean zero. It is based on the fact that the method of stationary phase may be applied directly to
p
{
λf(x)
}, without decomposition of
p
into Fourier components: thus a simple minimum of
f
at
x = x
0
gives a term containing a fractional integral of order one-half, proportional to
p̂
+
(
y
) = {
∞
y
{
p(x)/ (x — y)
1/2
} d
x
evaluated at
y
=
λf(x
0
)
; a simple maximum gives a similar term. In many physical problem,
f
depends linearly on a parameter, say
t
, in such a way that
I
is periodic in
t
and the quantity of interest is
q(t)
= d
l
/d
t
. The theory of how the shape of
q
is determined by that of
p
when
λ
is large but fixed is here called waveform asymptotics and its main features investigated using ‘barber’s pole’ integrals. For example, the singularity in
q
produced by a discontinuity in
p
is found explicitly as an inverse square-root multiplied by a coefficient, so need not be inferred from the tail of a Fourier series. More generally, the effect on
q
of any rapid change in
p
may be obtained by the present method of stationary phase in the time domain, without resolution into components; since Gibbs’ phenomenon is thereby avoided the method is suited to highly non-sinusoidal wave problems. An asymptotic representation of
q
by zeta functions is possible. Four extensions of the basic theory are analysed in detail: coalescence of a maximum and minimum of
f
; contributions from the end-points of the range of integration; collision of a maximum or minimum with an end-point ; and the behaviour of integrals with no stationary points or end-points. The first and third of these lead to time-domain Airy functions and Fresnel integrals, respectively, with singularity structures dual to the smooth patterns found in diffraction catastrophes; the second recovers the original waveform; and the fourth gives exponential asymptotics. The theory is illustrated throughout by analysis and computation for functions
p
describing a square wave and an intermittent
N
-wave, and by diagrams of the resulting waveforms.
Reference30 articles.
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