The shape and position of the plasma sheet in Earth's magnetotail
- 1 April 1984
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 89 (A4) , 2169-2179
- https://doi.org/10.1029/ja089ia04p02169
Abstract
No abstract availableKeywords
This publication has 32 references indexed in Scilit:
- Self‐consistent magnetotail theory: General solution for the quiet tail with vanishing field‐aligned currentsJournal of Geophysical Research, 1979
- The magnetotail magnetic fieldJournal of Geophysical Research, 1979
- Self-consistent theory of the quiet magnetotail in three dimensionsJournal of Geophysical Research, 1977
- The Position and shape of the neutral sheet at 30-REdistanceJournal of Geophysical Research, 1976
- Open and closed magnetospheric tail configurations and their stabilityAstrophysics and Space Science, 1975
- The influence of the direction of the geomagnetic dipole on the position of the neutral sheetJournal of Geophysical Research, 1974
- The self-consistent geomagnetic tail under static conditionsPlanetary and Space Science, 1972
- Self-consistent description of the magnetotail current systemJournal of Geophysical Research, 1972
- Geometry of the geomagnetic tailJournal of Geophysical Research, 1970
- Mapping of the Earth's bow shock and magnetic tail by Explorer 33Journal of Geophysical Research, 1968