Plasma convection and auroral precipitation processes associated with the main ionospheric trough at high latitudes
- 31 May 1988
- journal article
- Published by Elsevier in Journal of Atmospheric and Terrestrial Physics
- Vol. 50 (4-5) , 389-404
- https://doi.org/10.1016/0021-9169(88)90024-4
Abstract
No abstract availableKeywords
This publication has 32 references indexed in Scilit:
- Initial EISCAT observations of plasma convection at invariant latitudes 70°–77°Journal of Atmospheric and Terrestrial Physics, 1984
- The EISCAT facilityJournal of Atmospheric and Terrestrial Physics, 1984
- Millstone Hill measurements on 26 February 1979 during the solar eclipse and formation of a midday F-region troughJournal of Atmospheric and Terrestrial Physics, 1984
- EISCAT: An updated description of technical characteristics and operational capabilitiesRadio Science, 1983
- The Fossil Theory of nighttime high latitude F region troughsJournal of Geophysical Research, 1983
- Millstone Hill incoherent scatter observations of auroral convection over 60° ≤Λ≤75°, 1. Observing and data reduction proceduresJournal of Geophysical Research, 1979
- The high‐latitude winter F region at 300 km: Thermal plasma observations from AE‐CJournal of Geophysical Research, 1978
- Numerical model of the convectingF2ionosphere at high latitudesJournal of Geophysical Research, 1977
- Aurora and the poleward edge of the main ionospheric troughJournal of Geophysical Research, 1973
- Ionization troughs below the F2-layer maximumPlanetary and Space Science, 1969