Observation and theoretical modelling of a region of downward field-aligned flow of O+ in the winter dayside polar cap
- 31 May 1985
- journal article
- Published by Elsevier in Journal of Atmospheric and Terrestrial Physics
- Vol. 47 (5) , 489-495
- https://doi.org/10.1016/0021-9169(85)90114-x
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- The generation of vertical thermospheric winds and gravity waves at auroral latitudes—I. Observations of vertical windsPlanetary and Space Science, 1984
- What auroral electron and ion beams tell us about magnetosphere-ionosphere couplingSpace Science Reviews, 1984
- A theoretical study of the distribution of ionization in the high-latitude ionosphere and the plasmasphere: first results on the mid-latitude trough and the light-ion troughJournal of Atmospheric and Terrestrial Physics, 1982
- Departures from diffusive equilibrium in the topside F-layer from satellite soundingsJournal of Atmospheric and Terrestrial Physics, 1982
- Recent advances in magnetosphere-ionosphere couplingReviews of Geophysics, 1982
- Simultaneous observations of energetic (keV) upstreaming and electrostatic hydrogen cyclotron wavesJournal of Geophysical Research, 1979
- Transversely accelerated ions: An ionospheric source of hot magnetospheric ionsJournal of Geophysical Research, 1979
- The latitudinal, diurnal, and altitudinal distributions of upward flowing energetic ions of ionospheric originGeophysical Research Letters, 1978
- Field-aligned currents in the dayside cusp observed by TriadJournal of Geophysical Research, 1976
- Contamination of the O I (³P2-¹D2) emission line by the (9-3) band of OHX²II in high-resolution measurements of the night skyJournal of Geophysical Research, 1974