Ion energization mechanisms at 1700 km in the auroral region
- 1 March 1998
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 103 (A3), 4199-4222
- https://doi.org/10.1029/97ja00855
Abstract
No abstract availableKeywords
This publication has 76 references indexed in Scilit:
- SCIFER—Structure of the Cleft Ion Fountain at 1400 km altitudeGeophysical Research Letters, 1996
- Transverse ion energization and wave emissions observed by the Freja satelliteGeophysical Research Letters, 1994
- Observation of ion‐cyclotron turbulence at small values of magnetic‐field‐aligned currentGeophysical Research Letters, 1994
- What parts of broadband spectra are responsible for ion conic production?Geophysical Research Letters, 1991
- Ion heating by broadband low‐frequency waves in the cusp/cleftJournal of Geophysical Research, 1990
- High‐resolution sounding rocket observations of large‐amplitude Alfvén wavesJournal of Geophysical Research, 1990
- Can ion acceleration by double‐cyclotron absorption produce O+ ion conics?Journal of Geophysical Research, 1989
- Transverse ion heating in multicomponent plasmas along auroral zone field linesJournal of Geophysical Research, 1988
- Local transverse ion energization in and near the polar cuspGeophysical Research Letters, 1988
- Turbulent heating of heavy ions on auroral field linesJournal of Geophysical Research, 1984