1982
DOI: 10.1007/bf02258038
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Very low frequency atmospheric radio noise field intensities

Abstract: SummarySimultaneous observations of the field strength of atmospheric radio noise at three harmonically related frequencies in the VLF band for a period of two years from October 1976 to September 1978 have been analyzed to explore the frequency spectrum of atmospherics. The results have been shown for different months and seasons of the year and interpreted in terms of source activity and propagation effect.

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Cited by 4 publications
(2 citation statements)
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“…The arrival of lightning sferics may occur directly or by reflection from the D-region of the ionosphere [6]. The amplitude of VLF sferics shows diurnal variation depending on the location of the receivers [7,8]. The diurnal nature of VLF electric field atmospherics may not always show 'Carnegie curve' in some areas of the globe depending on the atmospheric weather at the receiving location [9,10].…”
Section: Introductionmentioning
confidence: 99%
“…The arrival of lightning sferics may occur directly or by reflection from the D-region of the ionosphere [6]. The amplitude of VLF sferics shows diurnal variation depending on the location of the receivers [7,8]. The diurnal nature of VLF electric field atmospherics may not always show 'Carnegie curve' in some areas of the globe depending on the atmospheric weather at the receiving location [9,10].…”
Section: Introductionmentioning
confidence: 99%
“…Long distance propagation of such electromagnetic waves is controlled mainly by the status of the lower ionosphere and conductivity of the Earth's surface [ De et al , 2010a; Cummer et al , 1998]. Sferics are generally known to have a typical diurnal variation [ De and Sarkar , 1996; Bhattacharya et al , 1980; Sen et al , 1982] which shows variations during various geophysical events, thunderstorm activities, solar events, earthquake etc. [ De and Sarkar , 1995; Bhattacharya et al , 1997; De et al , 2010b].…”
Section: Introductionmentioning
confidence: 99%