The interpretation of 6300 Å airglow observations of ionospheric irregularities

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Scientific paper

The variations in intensity of 6300 Å airglow throughout the ionosphere above an observor are represented by a three dimensional Fourier series. Filtering effects caused by the field of view of an observing instrument are then calculated assuming that all Fourier components move with the same velocity. The results suggest that the observations of Mullaney et al. (1972) can be interpreted as the power spectrum of horizontal structures in the airglow.

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