Auroral N2vibrational excitation and the electron density trough
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v002/i006/GL002i006p00239/GL002i006p00239.pdf
Reference31 articles.
1. NO+ and O+ in the high latitude F-region;Banks;Geophys. Res. Letters,1974
2. Full non-linear treatment of the global thermospheric wind system-II. Results and comparison with observations;Blum;J. Atmos. Terr. Phys.,1975
3. Ionization troughs below the F2-layer maximum;Bowman;Planet. Space Sci.,1969
4. Effect of atomic oxygen on the N2 vibrational temperature in the lower thermosphere;Breig;J. Geophys. Res.,1973
5. Theory of subexcitation electron scattering by molecules. II, Excitation and de-excitation of molecular vibration;Chen;J. Chem. Phys.,1964
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