Invariance in the vertical distribution of O(+)/n sub e in the 130-200 km region

Details Invariance in the vertical distribution of O(+)/n sub e in the 130-200 km region Invariance in the vertical distribution of O(+)/n sub e in the 130-200 km region

Apr 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983ge%26ae..23..213a&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 23, Mar.-Apr. 1983, p. 213-217. In Russian.

Physics

1

Ionospheric Ion Density, Oxygen Ions, Vertical Distribution, Annual Variations, Atmospheric Composition, F 1 Region, Invariance, Positive Ions

Scientific paper

The vertical distribution of O(+)/n sub e in the 130-200 km region of the upper atmosphere in conditions of ionization-recombination equilibrium is examined. The invariant property of this distribution is found which is independent of time, place, and heliogeophysical conditions for a given season. The dependence on season is associated with variations of the composition of the neutral atmosphere. Available mass-spectroscopy data on the ion composition confirm the existence of this invariance, which can be useful for refining parameters of neutral-atmosphere models.

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