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| Titel |
Morphology of the ring current derived from magnetic field observations |
| VerfasserIn |
G. Le, C. T. Russell, K. Takahashi |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
0992-7689
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| Digitales Dokument |
URL |
| Erschienen |
In: Annales Geophysicae ; 22, no. 4 ; Nr. 22, no. 4 (2004-04-02), S.1267-1295 |
| Datensatznummer |
250014838
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| Publikation (Nr.) |
 copernicus.org/angeo-22-1267-2004.pdf |
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| Zusammenfassung |
Our examination of the 20 years of magnetospheric magnetic field data from ISEE,
AMPTE/CCE and Polar missions has allowed us to quantify how the ring current flows and
closes in the magnetosphere at a variety of disturbance levels. Using intercalibrated magnetic
field data from the three spacecraft, we are able to construct the statistical magnetic field maps
and derive 3-dimensional current density by the simple device of taking the curl of the statistically
determined magnetic field. The results show that there are two ring currents, an inner one that
flows eastward at ~3 RE and a main westward ring current at ~4–7 RE for all levels of
geomagnetic disturbances. In general, the in-situ observations show that the ring current varies as
the Dst index decreases, as we would expect it to change. An unexpected result is how
asymmetric it is in local time. Some current clearly circles the magnetosphere but much of the
energetic plasma stays in the night hemisphere. These energetic particles appear not to be able to
readily convect into the dayside magnetosphere. During quiet times, the symmetric and partial
ring currents are similar in strength (~0.5MA) and the peak of the westward ring current is
close to local midnight. It is the partial ring current that exhibits most drastic intensification as
the level of disturbances increases. Under the condition of moderate magnetic storms, the total
partial ring current reaches ~3MA, whereas the total symmetric ring current is ~1MA. Thus, the
partial ring current contributes dominantly to the decrease in the Dst index. As the ring current
strengthens the peak of the partial ring current shifts duskward to the pre-midnight sector. The
partial ring current is closed by a meridional current system through the ionosphere, mainly the
field-aligned current, which maximizes at local times near the dawn and dusk. The closure
currents flow in the sense of region-2 field-aligned currents, downward into the ionosphere near
the dusk and upward out of the ionosphere near the dawn.
Key words. Magnetospheric physics (current systems;
storms and substorms; magnetospheric configuration and dynamics) |
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