Transverse resonance in the high-latitude section of the Earth–ionosphere waveguide during the solar eclipse of March 20, 2015

The spectra of radio atmospheric signals (spherics) recorded simultaneously at two observatories of the Polar Geophysical Institute, Lovozero (67.97° N, 35.08° E) and Barentsburg (78.08° N, 14.22° E), during the solar eclipse on March 20, 2015 are presented. The peculiarities of the behavior of the...

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Bibliographic Details
Published in:Geomagnetism and Aeronomy 2017-09, Vol.57 (5), p.618-623
Main Authors: Galakhov, A. A., Akhmetov, O. I.
Format: Article
Language:English
Subjects:
Altitude
Altitude effects
Earth
Earth and Environmental Science
Earth Sciences
Earth-ionosphere waveguide
Geophysics
Geophysics/Geodesy
Ionosphere
Observatories
Solar eclipses
Wave power
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Summary:The spectra of radio atmospheric signals (spherics) recorded simultaneously at two observatories of the Polar Geophysical Institute, Lovozero (67.97° N, 35.08° E) and Barentsburg (78.08° N, 14.22° E), during the solar eclipse on March 20, 2015 are presented. The peculiarities of the behavior of the first critical frequency of the Earth-ionosphere waveguide during the eclipse are described. The effective altitude of the reflective layer of ionosphere is assessed.
ISSN:0016-7932
1555-645X
0016-7940
DOI:10.1134/S0016793217050085