Determination ofFregion height and peak electron density at night using airglow emissions from atomic oxygen
- 1 June 1975
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 80 (16) , 2333-2337
- https://doi.org/10.1029/ja080i016p02333
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- Equatorial airglow and the ionospheric geomagnetic anomalyJournal of Geophysical Research, 1973
- Tropical UV arcs: Comparison of brightness withƒ0F2Journal of Geophysical Research, 1973
- Oxygen ion-ion neutralization reaction as related to tropical ultraviolet nightglowJournal of Geophysical Research, 1971
- Yield of O(1D) by dissociative recombination of O2+ from night airglow observationsJournal of Atmospheric and Terrestrial Physics, 1970
- Equatorial aurora/airglow in the far ultravioletJournal of Geophysical Research, 1970
- A comparison of the oxygen ion-ion neutralization and radiative recombination mechanisms for producing the ultraviolet nightglowJournal of Geophysical Research, 1970
- quenching in the ionospheric F-regionPlanetary and Space Science, 1969
- Atmospheric electron–ion and ion–ion recombination processesCanadian Journal of Chemistry, 1969
- Ionospheric Composition and ReactionsScience, 1968
- Static diffusion models of the upper atmosphere with empirical temperature profilesSmithsonian Contributions to Astrophysics, 1965