Recombination of NO+ in the mid‐latitude trough and the polar ionization hole
- 1 August 1979
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 84 (A8) , 4316-4320
- https://doi.org/10.1029/ja084ia08p04316
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- The high‐latitude winter F region at 300 km: Thermal plasma observations from AE‐CJournal of Geophysical Research, 1978
- Objections to the N2+ + e− dissociative recombination coefficients inferred from analysis of Atmosphere Explorer measurementsGeophysical Research Letters, 1978
- On the chemistry of metastable atomic nitrogen in theFregion deduced from Simultaneous satellite measurements of the 5200-Å airglow and atmospheric 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
- Effects of ion speed distributions in flow-drift tube studies of ion–neutral reactionsThe Journal of Chemical Physics, 1977
- Daytime chemistry of NO+from Atmosphere Explorer-C measurementsJournal of Geophysical Research, 1977
- Variation of electron-N-ion recombination coefficient with electron temperaturePhysical Review A, 1975
- Temperature dependence of some ionospheric ion-neutral reactions from 300°-900°KJournal of Geophysical Research, 1974
- 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