A description is given of an airborne turbulent flux measurement system consisting of fast response sensors to measure two components of the relative wind velocity, temperature, humidity, and aircraft motion. Its performance and attendant data reduction schemes are illustrated with some data obtained during the Barbados oceanographic and meteorological experiment (Bomex) in May 1969. The nature of typical Bomex data is discussed, using spectra and cospectra obtained through this airborne sensor system.
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Miyake et al. (1970) studied this question.
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