Nature of the interrelationship between layer heights of auroral irregularities and sporadic E layers

Details Nature of the interrelationship between layer heights of auroral irregularities and sporadic E layers Nature of the interrelationship between layer heights of auroral irregularities and sporadic E layers

Apr 1985

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985ge%26ae..25..243t&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 25, Mar.-Apr. 1985, p. 243-246. In Russian.

Computer Science

Auroral Ionization, Height, Particle Precipitation, Radio Auroras, Sporadic E Layer, Auroral Electrojets, Particle Energy, Particle Flux Density

Scientific paper

The relationship of the layer heights of a diffuse radio aurora (RA) and sporadic E layers with the rigidity parameter of the accompanying auroral precipitations is investigated. The characteristic energy of precipitating fluxes was determined from observations of spectra of diffuse auroral glow in three emissions (3914, 5577, and 6300 A). It is shown that the layer heights of RA and sporadic E are uniquely defined by the precipitation rigidity parameter. Differences in the interrelationship between RA and sporadic E layer heights in the regions of the western and eastern electrojets are clarified.

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