Abstract
The problem of propagation of electric field disturbances from the ionosphere to the lower atmosphere is considered with allowance for a finite electrical conductivity of the Earth crust. The results of synchronous registration of the ultralow-frequency electric field on a network of stations separated in space that included the Experimental Site of Vladimir State University (VSU), the Station of the Radio Physical Faculty of VSU, and the Portable Station of the Scientific-Research Center of Remote Sensing of the Atmosphere of the Main Geophysical Observatory (Saint Petersburg) have been registered using an optimal receiver and reliable estimates of amplitudes of spectral components of the electric field in the ground atmospheric layer are given. The signal-to-noise ratios and error probabilities are calculated at frequencies of thermogravitational solar tides.
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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Fizika, No. 8, pp. 33–39, August, 2005.
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Grunskaya, L.V., Morozov, V.N., Efimov, V.A. et al. Ultralow-Frequency Electric Field in the Ground Atmospheric Layer. Russ Phys J 48, 816–823 (2005). https://doi.org/10.1007/s11182-005-0207-x
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DOI: https://doi.org/10.1007/s11182-005-0207-x