Enhancements of the auroral zone ionization during substorms

Details Enhancements of the auroral zone ionization during substorms Enhancements of the auroral zone ionization during substorms

Apr 1975

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1975p%26ss...23..619m&link_type=abstract

Planetary and Space Science, vol. 23, Apr. 1975, p. 619-626.

Physics

1

Auroral Ionization, Electron Precipitation, Ionospheric Electron Density, Night Sky, Polar Substorms, F Region, Faraday Effect, Geomagnetism, Kp Index, Winter

Scientific paper

During winter nights the ionization of the auroral zone increases and moves southward into the main ionospheric trough with increasing magnetic activity. The southern boundary of the ionization coincides with the southern boundary of the auroral oval. The ionization thus created remains in the ionosphere after midnight, although the precipitation of soft electrons, which is the possible source, has moved north of the auroral zone.

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