Thomson scatter radar detection of D‐region negative ions at Arecibo
- 1 February 1979
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 6 (2) , 89-92
- https://doi.org/10.1029/gl006i002p00089
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- The effect of negative ions on Thomson scattering in the presence of electron heatingGeophysical Research Letters, 1978
- Preliminary measurements of the ion component of the incoherent scatter spectrum in the 60‐90 km region over AreciboGeophysical Research Letters, 1978
- The effect of negative ions on collision‐dominated Thomson scatteringJournal of Geophysical Research, 1978
- Measurements of the diurnal tides in the 80- to 100-km altitude range at AreciboJournal of Geophysical Research, 1976
- An experimental and theoretical study of the D-region—II. A semi-empirical model for mid-latitude D-regionJournal of Atmospheric and Terrestrial Physics, 1974
- Ion composition measurements in the lower ionosphere during the November 1966 and March 1970 aolar eclipsesJournal of Atmospheric and Terrestrial Physics, 1972
- Artificial heating of the lower ionosphereJournal of Geophysical Research, 1972
- Negative ions in the lower ionosphere: A mass-spectrometric measurementJournal of Atmospheric and Terrestrial Physics, 1971
- Mass spectrometric measurements of negative ions in the D- and lower E-regionsJournal of Atmospheric and Terrestrial Physics, 1971
- Rocket measurements of upper atmospheric nitric oxide and their consequences to the lower ionosphereJournal of Geophysical Research, 1971