Abstract

The magnetic storm of September 30 through October 1,1961, was the first severe magnetic disturbance from which data were obtained simultaneously from satellite, balloon, and ground observations [Bryant et al., 1962; Hoffman et al., 1962; Winckler et al., 1962; also ‘September Event,’ special session of the First Western National Meeting, American Geophysical Union, December 27–29, 1961, Los Angeles, California]. In view of the geophysical importance of this event it seems worth while to present the frequency-time characteristics of micropulsations (both hm emissions and noise bursts) throughout the disturbed period. Sonagrams of a 24-hour period including the storm are presented in Figures 1 and 2. The sonagrams were obtained from a magnetic tape recording of the signals detected by an induction magnetometer at Palo Alto, California. The instrumentation is described elsewhere [Tepley, 1961a]. The sonagrams include a 1-minute short-out period at the beginning of each hour, followed by a 1-minute calibration at cps.

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