An explanation of the magnetic declination effect in the ionospheric F2-layer
- 31 July 1969
- journal article
- Published by Elsevier in Journal of Atmospheric and Terrestrial Physics
- Vol. 31 (7) , 1011-1016
- https://doi.org/10.1016/0021-9169(69)90146-9
Abstract
No abstract availableKeywords
This publication has 8 references indexed in Scilit:
- Some effects of neutral air winds on the ionospheric F-layerJournal of Atmospheric and Terrestrial Physics, 1968
- Diurnal and seasonal latitudinal variations in the upper atmospherePlanetary and Space Science, 1968
- An explanation of phenomena occurring in the high latitude ionosphere at certain Universal TimesJournal of Atmospheric and Terrestrial Physics, 1968
- A numerical study of the wind system in the middle thermosphereJournal of Atmospheric and Terrestrial Physics, 1967
- Atmospheric winds between 100 and 700 km and their effects on the ionosphereJournal of Atmospheric and Terrestrial Physics, 1967
- Reconsideration of diurnal velocity oscillation in the thermosphereJournal of Geophysical Research, 1967
- Atmospheric winds in the middle latitude F-regionJournal of Atmospheric and Terrestrial Physics, 1966
- The effect of the magnetic declination on theF2layerJournal of Geophysical Research, 1963