Neutral and ion composition of the thermosphere
Author:
Publisher
American Geophysical Union (AGU)
Subject
Geophysics
Link
http://www.agu.org/journals/rg/v021/i002/RG021i002p00245/RG021i002p00245.pdf
Reference198 articles.
1. The effect on thermospheric chemistry of a resonant charge exchange reaction involving vibrationally excited N2+ ions with atomic oxygen;Abdou;J. Geophys. Res.,1982
2. Electron quenching of O+(2D;Abdou;J. Geophys. Res.,1982
3. Potential energy curves for NO+;Albritton;J. Chem. Phys.,1979
4. Production of NO+(a3Σ+) ions in the reaction of N+ ions with 02 at 300K;Albritton;J. Chem. Phys.,1979
5. The seasonal-latitudinal variation of exospheric helium from He 584-A dayglow emissions;Anderson;J. Geophys. Res.,1979
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1. The role of processes with a high threshold energy in the physics of the upper atmospheres of the planets;Journal of Optical Technology;2005-08-01
2. Sensitivity of the 6300 Å twilight airglow to neutral composition;Journal of Geophysical Research;1995
3. Ring current heating of the low latitude thermosphere connected with geomagnetic disturbances;Advances in Space Research;1993-01
4. N(2D) + O2: A source of thermospheric 6300 Å emission?;Planetary and Space Science;1992-05
5. Relationship between developments of the Huanghe and Yongding rivers and the evolution of the fossil lakes of the cenozoic era in the drainage area;Chinese Geographical Science;1991-09
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