Abstract

Particle precipitation events coinciding with storm sudden commencements were studied for 328 events occurring during 1970–1979. The study was based on data recorded at seven riometer stations between L = 3.3 and 6.0, on ionosonde data and on IMF B z data. At L > 5, the probability of occurrence of a precipitation event is greater at night than during the day. South of this the probability is almost equal during the day and night. Generally precipitation increases when IMF B z is negative. The effect of the precipitation was limited to the D-region of the ionosphere, and no effects on foE or foF2 were detected.

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