Abstract
The study of diurnal variation in the frequencies and amplitudes of magnetic sudden commencements (SC /sup s/) and sudden impulses (SI/sup s/) recorded at gretta (lat. 30 deg 11'N; long. 66 deg 57'E), during the period 1953--1962 indicates that SC/sup s/ and Si/sup s/ are more frequent near the sunrise and sunset hours with maxima around 08/sup h/ and 18/sup h/ local time (L.T.). This does not conform to the curves obtained by Newton and Ferraro & others which exhibit a maximum at 13/sup h/ J.T. and two minima at 08/sup h/ and 20/sup h/ L.T. respectively. The mean hourly values of the amplitude y of SC/sup S/ g Sl/sup S/ do not seem to exhibit any marked local time effect. The daytime enhancement in y and the similarity between the diurnal variation of amplitude of SC/sup S/ & SI/sup S/ and Sq-variation found at Huancayo, Kodaikanal, and Alibag is also absent. On the other hand a sharp minimum in the amplitude curve around 07/sup h/ L.T. gives weight to Ferraro's contention that during the day-lit hemisphere the higher conductivity of the ionosphere tends to shield the station below from the external magnetic field produced by corpuscular stream. No seasonalmore » variation in the monthly frequency of SC/sup s/ & SI/sup s/ is discernible but the mean monthly amplitude curve exhibits marked enhancement in the size of SC/sup s/ & SI/sup s/ during the summer months. The curves for the annual mean number and yearly mean amplitudes of SC/sup s/ & SI/sup s/ and yearly mean Sq-range show striking similarity to the curve for the annual mean sunspot numbers. A linear relation of the type y = 11.6 + 0.097s between the amplitude y and the relative sunspot numbers s was worked out for Quetta.« less
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