Exospheric temperatures deduced from 7320- to 7330-Å (O+(²P) - O+(²D)) twilight observations

Author:

Yee J. H.,Abreu V. J.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference16 articles.

1. Airglow measurement of the variation of the O+(2P) ionization frequency during solar cycle 21;Abreu;Geophys. Res. Lett.,1980

2. Banks, P. M., , G., Kockarts, , Aeronomy, , Part B, 107 Academic, New York, 1973,

3. The fluorescence of solar ionizing radiation;Dalgarno;Planet. Space Sci.,1963

4. Measurement of temperatures in the region 30 to 80 km by the rocket-Grenada experiment;Ferrence;J. Meteorol.,1956

5. The velocity of sound waves and the temperature in the stratosphere in southern California;Gutenberg;Bull. Am. Meteorol. Soc.,1939

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2. Diurnal and seasonal variation of the nighttime OH (8-3) emission at low latitudes;Journal of Geophysical Research;1989

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4. The visible airglow experiment—a review;Planetary and Space Science;1988-01

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