Six sounding rockets, each carrying a Langmuir probe and an impedance probe, were launched into the disturbed ionosphere from Syowa Station, Antarctica, during 1972–1973 for measuring electron density fluctuations in a frequency range from a few hertz to 160 Hz. Such low-frequency fluctuations were observed between 90 and 120 km in altitude and found to have relative amplitudes of 10% or smaller. Analysis to find the frequency power spectrum of the fluctuations shows that in most cases the spectral form obeys f−1 ∼ f−3. In this report we wish to summarize the measured characteristics of the fluctuations and briefly discuss possible generation mechanisms of them.
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Ogawa et al. (1976) studied this question.
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