The oblique whistler instability in the Earth's foreshock
- 1 March 1983
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 88 (A3) , 2048-2056
- https://doi.org/10.1029/ja088ia03p02048
Abstract
No abstract availableKeywords
This publication has 44 references indexed in Scilit:
- Whistler mode turbulence in the disturbed solar windJournal of Geophysical Research, 1982
- Plasma waves associated with energetic particles streaming into the solar wind from the Earth's bow shockJournal of Geophysical Research, 1981
- Measurements of bow shock particles far upstream from the EarthJournal of Geophysical Research, 1981
- Reflected and diffuse ions backstreaming from the Earth's bow shock 1. Basic propertiesJournal of Geophysical Research, 1981
- Upstream particles observed in the Earth's foreshock regionJournal of Geophysical Research, 1981
- Backstreaming ions outside the Earth's bow shock and their interaction with the solar windJournal of Geophysical Research, 1980
- Thin sheets of energetic electrons upstream from the Earth’s bow shockGeophysical Research Letters, 1979
- Energetic electrons of terrestrial origin behind the bow shock and upstream in the solar windJournal of Geophysical Research, 1969
- Outward flow of protons from the Earth's bow shockJournal of Geophysical Research, 1968
- Energetic electrons of terrestrial origin upstream in the solar windJournal of Geophysical Research, 1968