On the average configuraton of the geomagnetic tail
Author:
- D. H. FairfieldDFD. H. Fairfield
- 1 May 1979
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 84 (A5) , 1950-1958
Abstract
Over 3000 hours of Imp 6 magnetic field data obtained between 20 and 33 RE in the geomagnetic tail have been used in a statistical study of the tail configuration. A distribution of 2.5‐min averages of Bz as a function of position across the tail reveals that more flux crosses the equatorial plane near the dawn and dusk flanks than near midnight . The tail field projected in the solar magnetospheric equatorial plane deviates from the x axis due to flaring and solar wind aberration by an angle α = −0.9 YSM−2.7, where YSM is in earth radii and α is in degrees. After removing these effects, the By component of the tail field is found to depend on interplanetary sector structure. During an ‘away’ sector the By component of the tail field is on average 0.5γ greater than that during a ‘toward’ sector, a result that is true in both tail lobes and is independent of location across the tail. This effect means the average field reversal between northern and southern lobes of the tail is more often 178° rather than the 180° that is generally supposed.Keywords
This publication has 30 references indexed in Scilit:
- Comment on ‘Search for the magnetic neutral line in the near-Earth plasma sheet 2. Systematic study of Imp 6 magnetic field observations’ by A. T. Y. Lui, C.-I. Meng, and S.-I. AkasofuJournal of Geophysical Research, 1978
- Microstructure of a magnetotail fireballGeophysical Research Letters, 1977
- Self-consistent theory of the quiet magnetotail in three dimensionsJournal of Geophysical Research, 1977
- Solar wind and substorm-related changes in the lobes of the geomagnetic tailJournal of Geophysical Research, 1973
- A qualitative study of the reconnection between the Earth's magnetic field and an interplanetary field of arbitrary orientationRadio Science, 1973
- Outer magnetosphere near midnight at quiet and disturbed timesJournal 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
- Characteristics of the plasma sheet in the Earth's magnetotailJournal of Geophysical Research, 1967
- Magnetic storms in the Earth's magnetic tailJournal of Geophysical Research, 1966