Figure 19.3. The results of a Fast Fourier transform. Illustrated are real and
imaginary parts of the Fourier transform (for the time series shown in
Figure 19.2
) and its
power spectrum. The original time signal has been converted into a frequency spectrum
where the intensity axis shows the amount of each frequency present in the signal.
Peaks
Once we have a Fourier transformed signal, which in certain contexts is called a spectrum,
the next thing to do is to analyse the frequency peaks, or at least the significant ones.
These correspond to the underlying frequency components of the signal. We would like to
determine the parameters for each peak, namely the amplitude, frequency and decay. If
there are many components then the peaks can overlap and this job becomes difficult. To
simplify our introduction we will assume here that there is no overlap between the peaks.
The frequency is the point in the spectrum where the given peak value is at its
maximum, but there are a few subtleties to this. The spectrum is specified on a grid, so at
equally spaced frequencies. Hence, it’s quite likely that the actual underlying frequency
does not lie exactly on the point of the sampled grid, but in between two such points. This
means that the maximum points need to be interpolated somehow to find the peak
frequency positions.
There is another subtle issue to do with frequency, which comes about because of the
discrete time sampling of the signal. If the signal is sampled at time intervals Δt then a
pure signal at frequency ω and another one at frequency ω + 1/Δt give the same Fourier
transform, since
. Indeed, in general we get the same Fourier transform
for frequency ω + n/Δt for any integer n. In effect, a signal at one of these frequencies
cannot be distinguished from a signal at any of the other frequencies. The frequency with
an absolute value less than 1/(2Δt) is called the fundamental frequency and the other
frequencies are said to be aliased to this one.
8
The height or intensity of a peak is the value at its maximum. This does not determine
the underlying amplitude by itself, because the observed height is also affected by the
decay parameter, and as with the frequency there is also the issue that the peak values are
only defined on a grid. The amplitude is proportional to the volume (integral) of the peak,
which is the summation of the frequency values around the peak, but there is the question
of exactly how that is done, such as how far away from the maximum position to include
in the sum. The decay parameter is determined by the linewidth of the peak, which is
roughly speaking how wide the peak is. A common way to measure this is the width at
half the peak height. These parameters can be determined by fitting the observed data to a
theoretical description of a peak.
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