Structure of the distant magnetotail and its dependence on the IMF By component: GEOTAIL observations
- 1 January 1997
- journal article
- Published by Elsevier in Advances In Space Research
- Vol. 20 (4-5) , 949-959
- https://doi.org/10.1016/s0273-1177(97)00503-6
Abstract
No abstract availableThis publication has 15 references indexed in Scilit:
- GEOTAIL observation of magnetospheric convection in the distant tail at 200 RE in quiet timesJournal of Geophysical Research, 1995
- Average motion, structure and orientation of the distant magnetotail determined from remote sensing of the edge of the plasma sheet boundary layer with E > 35 keV ionsJournal of Geophysical Research, 1995
- Structure of the neutral sheet in the distant tail (x=−210 Re) in geomagnetically quiet timesGeophysical Research Letters, 1994
- The Low Energy Particle (LEP) Experlment onboard the GEOTAIL Satellite.Journal of geomagnetism and geoelectricity, 1994
- A determination of twisting of the Earth's magnetotail at distances 115-220RE: ISEE 3Journal of Geophysical Research, 1992
- North‐south and dawn‐dusk plasma asymmetries in the distant tail lobes: ISEE 3Journal of Geophysical Research, 1985
- Magnetospheric asymmetries associated with the y-component of the IMFPlanetary and Space Science, 1981
- On the distribution of By in the geomagnetic tailPlanetary and Space Science, 1979
- Dayside merging and cusp geometryJournal of Geophysical Research, 1979
- Polar cap electric field structures with a northward interplanetary magnetic fieldGeophysical Research Letters, 1979