Results of measurements of the atmospheric radio noise at 27 kc/s at
                        fixed measuring stations in northern, central and south-eastern
                        Europe

Schäning, B.; Scuka, V.

doi:10.3402/tellusa.v21i1.10051

Tellus A: Dynamic Meteorology and Oceanography

1969

DOI: 10.3402/tellusa.v21i1.10051

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Results of measurements of the atmospheric radio noise at 27 kc/s at fixed measuring stations in northern, central and south-eastern Europe

B. Schäning

V. Scuka

Abstract: The paper presents measurements of the atmospheric radio noise (ARN) at 27 kcjs made between 1963 and 1966 at four unified European stations: Uppsala (60" N), Kuhlungsborn (54' N) Prague-PanskB Ves (50.5' N) and Sofia (43" N). The results concern the daily and annual variations and the latitude dependence of the mean integrated field strength. The diurnal maximum-level variations at Uppsala and Kiihlungsborn are shown by an amplitude probability-distribution function. Finally, the results are compared with the… Show more

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1974

1984

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Cited by 3 publications

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On the occurrence of very low frequency (VLF) electromagnetic radiation and its relation to some important physical conditions of the atmosphere

Bergh¹,

Israelsson

1984

Arch. Met. Geoph. Biocl., Ser. B

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SummaryContinuous recordings of VLF electromagnetic radiation were statistically compared with physical conditions of the atmosphere. The VLF level is closely associated with the distance to thunderstorms and therefore related to the dynamical weather processes. In agreement with previous studies, we found that the movement of the VLF sources is associated with the frontal system and especially with the passage of cold fronts. The VLF level is increased mainly by cold fronts of the anatype. The rainfall intensity is closely correlated to the electric discharge formation and thereby also to the VLF activity in the anafronts, while the katafronts often give rise to slight precipitation and few flashes of lightning. The atmospheric pressure changes accompanying the anafronts are largely correlated with the VLF level and the precipitation intensity. The mean diurnal and annual variations of the VLF level are determined by the occurrence of lightning activity. During the summer the daily trend is pronounced due to the insolation effect. The present study shows that the VLF level is determined to a high degree by fairly well defined areas with lightning discharges, which can be localized with automatic lightning location systems or forecasted by the weather services.

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On the occurrence of very low frequency (VLF) electromagnetic radiation and its relation to some important physical conditions of the atmosphere

Bergh¹,

Israelsson

1984

Arch. Met. Geoph. Biocl., Ser. B

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Results of ship-borne atmospheric radio noise measurements at 27 kHz on the North Atlantic during winter

Schäning¹,

Scuka²

1974

Tellus

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Results of ship-borne atmospheric radio noise measurements at 27 kHz on the North Atlantic during winter

Schäning

Scuka

1974

Tellus A: Dynamic Meteorology and Oceanography

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Ship-borne and land-station measurements of atmospheric radio noise (ARN) at 27 kHz in latitudes between GOON and 23'N during winter 1968/69 and 1970/71 are presented. The results concern the diurnal variations, the latitude dependence and the longitudinal distribution of the mean integrated field strength. The diurnal variations are explained by reference t o the prevailing meteorological and ionospheric conditions. Finallv. che results are comaared with the predictions of the ARN level made by the C.C.I. R.

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Results of measurements of the atmospheric radio noise at 27 kc/s at fixed measuring stations in northern, central and south-eastern Europe

Cited by 3 publications

References 2 publications

On the occurrence of very low frequency (VLF) electromagnetic radiation and its relation to some important physical conditions of the atmosphere

On the occurrence of very low frequency (VLF) electromagnetic radiation and its relation to some important physical conditions of the atmosphere

Results of ship-borne atmospheric radio noise measurements at 27 kHz on the North Atlantic during winter

Results of ship-borne atmospheric radio noise measurements at 27 kHz on the North Atlantic during winter

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