An upper limit to the product of NO and O densities from 105 to 120 km-Reference-Cited by-同舟云学术

An upper limit to the product of NO and O densities from 105 to 120 km

Published:1974-10-01 Issue:28 Volume:79 Page:4337-4339
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res

Author:

Donahue T. M.

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

Link

http://www.agu.org/journals/ja/v079/i028/JA079i028p04337/JA079i028p04337.pdf

Reference9 articles.

1. Nitric oxide in the upper atmosphere;Barth;Ann. Geophys.,1966

2. The mechanism of the air-afterglow NO + O → NO2 + hv;Becker;Chem. Phys. Lett.,1972

3. Distribution of atomic oxygen in the upper atmosphere deduced from Ogo 6 airglow observations;Donahue;J. Geophys. Res.,1973

4. Quenching of O(1S) by O(3P);Felder;J. Chem. Phys.,1972

5. Absolute quantum yield measurements of the NO-O reaction and its use as a standard for chemiluminescent reactions;Fontijn;J. Chem. Phys.,1964

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1. Cause of terrestrial nightglow continuum;Proceedings of the Royal Society of London. Series A: Mathematical and Physical Sciences;1993-10-08

2. Chapter 6 Airglows, Auroras, and Aeronomy;International Geophysics;1987

3. Airglow and Auroras;Applied Atomic Collision Physics;1982

4. NO2continuum in aurora;Journal of Geophysical Research;1978

5. Chapter 6 Airglows and Aeronomy;International Geophysics;1978