Average characteristics of the polar rain and their relationship to the solar wind and the interplanetary magnetic field
- 1 February 1986
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 91 (A2), 1557-1571
- https://doi.org/10.1029/ja091ia02p01557
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- Morphology of the polar rainJournal of Geophysical Research, 1984
- Intense fluxes of low‐energy electrons at geomagnetic latitudes above 85°Journal of Geophysical Research, 1984
- A theory of local and global processes which affect solar wind electrons 2. Experimental supportJournal of Geophysical Research, 1979
- A theory of local and global processes which affect solar wind electrons, 1. The origin of typical 1 AU velocity distribution functions—Steady state theoryJournal of Geophysical Research, 1979
- Satellite observations of polar, magnetotail lobe, and interplanetary electrons at low energiesReviews of Geophysics, 1978
- Dawn-dusk gradient of the precipitation of low-energy electrons over the polar cap and its relation to the interplanetary magnetic fieldJournal of Geophysical Research, 1977
- Intense uniform precipitation of low-energy electrons over the polar capJournal of Geophysical Research, 1977
- Low-energy electron intensities at large distances over the Earth's polar capJournal of Geophysical Research, 1976
- Polar cap auroral electron fluxes observed with Isis 1Journal of Geophysical Research, 1974
- Solar wind electrons: Vela 4 measurementsJournal of Geophysical Research, 1968