The causes of storm-time increases of the F-layer at mid-latitudes
- 30 April 1973
- journal article
- Published by Elsevier in Journal of Atmospheric and Terrestrial Physics
- Vol. 35 (4) , 593-616
- https://doi.org/10.1016/0021-9169(73)90191-8
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- L'orage magnetique du 11 fevrier 1969: Étude par diffusion incoherenteJournal of Atmospheric and Terrestrial Physics, 1972
- Measurements of horizontal drifts in theEandFregions at Millstone HillJournal of Geophysical Research, 1972
- Ionospheric movements measured by incoherent scatter: A reviewJournal of Atmospheric and Terrestrial Physics, 1972
- Observation of F Region Vertical Velocities at Millstone Hill, 1, Evidence for Drifts Due to Expansion, Contraction, and WindsRadio Science, 1971
- The June 1965 magnetic storm: Millstone Hill observationsJournal of Atmospheric and Terrestrial Physics, 1970
- F-region heating observed during the main phase of magnetic stormsJournal of Geophysical Research, 1970
- Whistler evidence of the dynamic behavior of the duskside bulge in the plasmasphereJournal of Geophysical Research, 1970
- Solution of the coupled ion and neutral air equations of the mid-latitude ionospheric F2-layerJournal of Atmospheric and Terrestrial Physics, 1969
- Electron temperature and ion composition in theF1regionJournal of Geophysical Research, 1967
- Ionospheric backscatter observationsPlanetary and Space Science, 1964