Further quantification of the sources and sinks of thermospheric O1D) atoms
- 30 June 1981
- journal article
- Published by Elsevier in Planetary and Space Science
- Vol. 29 (6), 595-600
- https://doi.org/10.1016/0032-0633(81)90107-0
Abstract
No abstract availableKeywords
This publication has 22 references indexed in Scilit:
- Collisional deactivation of O(2 1D2) by the atmospheric gasesThe Journal of Chemical Physics, 1979
- The O I (6300 Å) airglowReviews of Geophysics, 1978
- Temperature dependence of O(1D) rate constants for reactions with N2O, H2, CH4, HCl, and NH3The Journal of Chemical Physics, 1977
- A global thermospheric model based on mass spectrometer and incoherent scatter data MSIS, 2. CompositionJournal of Geophysical Research, 1977
- A global thermospheric model based on mass spectrometer and incoherent scatter data MSIS, 1. N2density and temperatureJournal of Geophysical Research, 1977
- Absolute rate constant determinations for the deactivation of O(1D) by time resolved decay of O(1D) →O(3P) emissionThe Journal of Chemical Physics, 1976
- The visible‐airglow experiment on Atmosphere ExplorerRadio Science, 1973
- The retarding‐potential analyzer on Atmosphere ExplorerRadio Science, 1973
- The cylindrical electrostatic probes for Atmosphere Explorer ‐C,‐D, and ‐ERadio Science, 1973
- The Bennett ion‐mass spectrometer on Atmosphere Explorer‐C and ‐ERadio Science, 1973