Formation of the daytime electron-density trough ne(m)F2 in the geomagetic-equator region

Details Formation of the daytime electron-density trough ne(m)F2 in the geomagetic-equator region Formation of the daytime electron-density trough ne(m)F2 in the geomagetic-equator region

Jun 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986ge%26ae..26..501m&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 26, May-June 1986, p. 501-503. In Russian.

Physics

Diurnal Variations, F 2 Region, Ionospheric Drift, Ionospheric Electron Density, Magnetic Equator, Troughs, Electrodynamics, Ion Recombination, Vertical Distribution

Scientific paper

Diurnal variations of f0F2 are calculated for a magnetically quiet day (August 6, 1969) for which there are data on vertical electromagnetic drift. The calculations confirm the result obtained by Leshchinskaia and Mikhailov (1980) in their investigation of the biteout phenomenon. According to this result, there exist two peaks, morning and evening, in the diurnal variations of ne(m)F2; the morning peak is connected with ionization-recombination processes, while the evening peak is connected with electrodynamic-drift variations.

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