Electric fields, ionization of the E-layer, and the origin of coherent scattering

Details Electric fields, ionization of the E-layer, and the origin of coherent scattering Electric fields, ionization of the E-layer, and the origin of coherent scattering

Apr 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992ge%26ae..32..116k&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 32, no. 2, Mar.-Apr. 1992, p. 116-120. In Russian.

Physics

Auroral Zones, Coherent Scattering, E Region, Ionospheric Electron Density, Radio Wave Refraction, Wave Scattering, Eiscat Radar System (Europe), Radar Echoes, Radar Measurement

Scientific paper

Conditions for the appearance of coherent radio-wave scattering are investigated on the basis of EISCAT data and measurements with an 83-MHz low-potential auroral radar. It is shown that, for an electric field greater than 20 mV/m, the appearance of a radar echo is determined by the mean electron density in the region of signal formation. At E less than 20 mV/m, practically no scattering was observed, irrespective of the ionization magnitude.

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