Average flow between ∼70 REand ∼220 REin the geomagnetic tail
- 1 April 1984
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 11 (4), 343-346
- https://doi.org/10.1029/gl011i004p00343
Abstract
No abstract availableThis publication has 17 references indexed in Scilit:
- Structure of the magnetotail at 220 RE and its response to geomagnetic activityGeophysical Research Letters, 1984
- Plasma regimes in the deep geomagnetic tail: ISEE 3Geophysical Research Letters, 1983
- Thermal and suprathermal protons and alpha particles in the Earth's plasma sheetJournal of Geophysical Research, 1983
- Evidence for Earth magnetospheric tail associated phenomena at 3100 REGeophysical Research Letters, 1979
- Transient phenomena in the magnetotail and their relation to substormsSpace Science Reviews, 1979
- Several recent findings concerning the dynamics of the Earth's magnetotailSpace Science Reviews, 1979
- The Nuclear and Ionic Charge Distribution Particle Experiments on the ISEE-1 and ISEE-C SpacecraftIEEE Transactions on Geoscience Electronics, 1978
- Fluxes of =50-keV protons and =30-keV electrons at ∼35 RE , 1. Velocity anisotropies and plasma flow in the magnetotailJournal of Geophysical Research, 1976
- Preliminary comparison of solar wind plasma observations in the geomagnetospheric wake at 1000 and 500 earth radiiPlanetary and Space Science, 1969
- Probable observations of the geomagnetic tail at 10³ Earth radii by Pioneer 7Journal of Geophysical Research, 1967