D-region recombination coefficients for normal and winter anomalous days

Details D-region recombination coefficients for normal and winter anomalous days D-region recombination coefficients for normal and winter anomalous days

Jan 1979

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1979jatp...41...77p&link_type=abstract

Journal of Atmospheric and Terrestrial Physics, vol. 41, Jan. 1979, p. 77-83. Research supported by the University Grants Commi

Physics

Atmospheric Ionization, D Region, Ionospheric Electron Density, Recombination Coefficient, Atmospheric Models, Cations, Ionospheric Ion Density, Reaction Kinetics, Winter

Scientific paper

A simplified positive ion model consisting of NO(+), O2(+) and their respective hydrated ions is used in the analysis of D-region ion production and loss processes to determine effective recombination coefficients. The widely used NO density profile from rocket studies is found to be satisfactory in computing NO(+) production rate for anomalous day and is large by about an order of magnitude at heights below 80 km for normal days. The results also show that the relation for proportionality between the electron production rate and electron number density does not hold good at all heights for normal and anomalous days.

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