Upwelling O+ ion source characteristics
- 1 June 1986
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 91 (A6) , 7019-7031
- https://doi.org/10.1029/ja091ia06p07019
Abstract
No abstract availableThis publication has 15 references indexed in Scilit:
- The cleft ion fountain: A two‐dimensional kinetic modelJournal of Geophysical Research, 1985
- The cleft ion fountainJournal of Geophysical Research, 1985
- Evidence for ion heat flux in the light ion polar windJournal of Geophysical Research, 1985
- A new source of suprathermal O+ ions near the dayside polar cap boundaryJournal of Geophysical Research, 1985
- A time‐dependent theoretical model of the polar wind: Preliminary resultsGeophysical Research Letters, 1985
- IMF By‐dependent plasma flow and Birkeland currents in the dayside magnetosphere: 1. Dynamics Explorer observationsJournal of Geophysical Research, 1985
- Correlated low‐frequency electric and magnetic noise along the auroral field linesJournal of Geophysical Research, 1984
- O+ ions in the polar windJournal of Geophysical Research, 1983
- Plasma injection and transport in the mid‐altitude polar cuspGeophysical Research Letters, 1982
- DE‐1 observations of the polar wind—A heated and an unheated componentGeophysical Research Letters, 1982