A quasi‐static magnetospheric convection model in two dimensions
- 1 May 1992
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 97 (A5) , 6505-6522
- https://doi.org/10.1029/91ja03141
Abstract
No abstract availableKeywords
This publication has 45 references indexed in Scilit:
- The substorm event of 28 January 1983: A detailed global studyPlanetary and Space Science, 1990
- Determination of the polytropic index in the plasma sheetGeophysical Research Letters, 1989
- Computer modeling of magnetotail convectionJournal of Geophysical Research, 1985
- Correlated dynamical changes in the near‐Earth and distant magnetotail regions: ISEE 3Journal of Geophysical Research, 1984
- On the cause of X-line formation in the near-Earth plasma sheet: Results of adiabatic convection of plasma-sheet plasmaPublished by Wiley ,1984
- Field-Aligned Currents as a Diagnostic Tool: Result, a Renovated Model of the MagnetosphereJournal of Geophysical Research, 1984
- Self‐consistent theory of three‐dimensional convection in the geomagnetic tailJournal of Geophysical Research, 1983
- The effect of pressure anisotropy on the equilibrium structure of magnetic current sheetsPlanetary and Space Science, 1978
- Solar wind and substorm-related changes in the lobes of the geomagnetic tailJournal of Geophysical Research, 1973
- Mapping of the Earth's bow shock and magnetic tail by Explorer 33Journal of Geophysical Research, 1968