The full spectral analysis (FSA) technique is investigated using both
experimental and model-generated data. The relationship between the fo
rmulae presented by different authors is discussed, and the similariti
es and differences inherent in using these formulae are evaluated. The
FSA is applied both to sample spectra calculated using individual tim
e series records and to spectra produced by the incoherent average of
the sample spectra. The results reveal that the velocities obtained us
ing sample spectra call be significantly biased in the situation where
large turbulent motions exist for two particular implementations of t
he technique. These biases are shown to decrease as the number of samp
le spectra used in the incoherent average are increased, thereby produ
cing FSA velocity estimates in excellent agreement with those produced
using the full correlation analysis (FCA) technique.