Thee series of experiments by Schubauer and Skramstad (1948) provided
the first experimental evidence of the role that the instability of To
llmien-Schlichting waves played in the transition of a zero pressure-g
radient flat plate boundary layer. The initial experiments studied the
oscillations in the boundary layer excited by the freestream fluctuat
ions. This was only possible after the background disturbances in the
wind tunnel had been reduced to a very low level. The background wind
tunnel environment excited a broad band of amplitude modulated disturb
ance waves that grew as they propagated downstream, eventually leading
to the formation of turbulent spots. Further experiments used artific
ial two-dimensional harmonic excitation to produce regular wavetrains
that could be directly compared with linear theory. Unfortunately, two
-dimensional harmonic excitation of this type has also been used in ma
ny of the subsequent nonlinear transition investigations; the modulati
on of the disturbance waves, essential in nonlinear studies, has been
largely ignored. Gaster and Grant (1975) used a short duration acousti
c pulse to excite the boundary layer and found that the modulated wave
packet that was created admitted bursts of high frequency oscillations
. These occurred at amplitudes that were insufficient to generate non-
linear behaviour in purely periodic wavetrains. Gaster (1980) suggeste
d that the modulation of the wavepacket played an important role in th
e non-linear region of transition. This investigation used computer ge
nerated deterministic white noise to excite the boundary layer on a fl
at plate through a single buried loudspeaker. This type of excitation
produced amplitude modulated T-S waves at some point downstream from t
he source. By repeatedly exciting the boundary layer with the same whi
te noise sequence it was possible to map the entire flow-field with a
single hot-wire probe and so study the evolution of the modulated wave
trains and the eventual development of turbulent spots. The modulated
wavetrains were found to grow initially according to linear theory. Bu
t downstream, departures from the linear pattern were observed at isol
ated time instants. The amplitude of the irregular portions of the sig
nal increased rapidly with downstream distance until bursts of oscilla
tions of frequencies five or six times the basic T-S frequency were ob
served. These regions developed even higher frequency bursts until a t
urbulent spot could be considered to have formed. Excitation signals o
f various amplitudes with different phase relations between the spectr
al components were used in these experiments. It was found that the ph
ases between the Fourier components played an important role in the hi
ghly non-linear behaviour that is the precursor to a turbulent spot. N
ovel signal processing techniques, such as the wavelet transform and S
ingular Value Decomposition were used to investigate the fine structur
e and the propagation characteristics of the high frequency disturbanc
es.