Suprathermal O+ and H+ ion behavior during the March 22, 1979 (CDAW 6), substorms
- 1 February 1985
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 90 (A2) , 1263-1272
- https://doi.org/10.1029/ja090ia02p01263
Abstract
No abstract availableKeywords
This publication has 22 references indexed in Scilit:
- DP 1 and DP 2 current systems for the March 22, 1979 substormsJournal of Geophysical Research, 1985
- The role of heavy ionospheric ions in the localization of substorm disturbances on March 22, 1979: CDAW 6Journal of Geophysical Research, 1985
- Implications of the 1100 UT March 22, 1979 CDAW 6 substorm event for the role of magnetic reconnection in the geomagnetic tailPublished by Wiley ,1984
- On the Composition of the Ring Current and the Plasmasheet and what it tells about the Sources of these Hot PlasmasPublished by Springer Nature ,1983
- The possible role of ionospheric oxygen in the initiation and development of plasma sheet instabilitiesGeophysical Research Letters, 1982
- Plasma populations in a simple open model magnetosphereSpace Science Reviews, 1980
- Magnetic storm injection of 0.9‐ to 16‐keV/e solar and terrestrial ions into the high‐altitude magnetosphereJournal of Geophysical Research, 1980
- High‐energy magnetospheric protons and their dependence on geomagnetic and interplanetary conditionsJournal of Geophysical Research, 1979
- Several recent findings concerning the dynamics of the Earth's magnetotailSpace Science Reviews, 1979
- Characteristics of the plasma sheet in the Earth's magnetotailJournal of Geophysical Research, 1967