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Detailed Reference Information |
Sibeck, D.G., McEntire, R.W., Krimigis, S.M. and Baker, D.N. (1988). The magnetosphere as a sufficient source for upstream ions on November 1, 1984. Journal of Geophysical Research 93: doi: 10.1029/88JA03554. issn: 0148-0227. |
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We consider 10 tests which distinguish the source of energetic particles in upstream ion events. Some tests are definitive, and others inadequate. In particular, we note that the Fermi model requires a finite time of magnetic field line connection to the bow shock before energetic ions appear and inverse velocity dispersion when the interplanetary magnetic field rotates to a more radial direction but that these features are also expected of the leakage model under certain conditions. We present simultaneous magnetospheric, magnetosheath, and upstream energetic particle observations during two well-documented upstream events on November 1, 1984, and apply the 10 tests. The events are unusual in that they occured during a period when the magnetosphere was greatly compressed, provided for an increase in the energetic magnetospheric particle population and a decrease in the magnetosheath thickness. Magnetospheric leakage satisfactorily explains our observations on this day, but in situ Fermi acceleration does not. Consequently, we consider magnetospheric leakage a sufficient source for upstream particles during these two events. ¿ American Geophysical Union 1988 |
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Abstract |
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Keywords
Interplanetary Physics, Planetary bow shocks, Magnetospheric Physics, Magnetopause, cusp, and boundary layers, Magnetospheric Physics, Magnetosheath |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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