The O+ density trough at 5000 km altitude in the polar cap

At altitudes near 5000 km over the southern polar cap region of the terrestrial magnetosphere/ionosphere, the Thermal Ion Dynamics Experiment (TIDE) on board the Polar satellite has observed O(+) ion density trough regions, in which the densities were at least one order of magnitude lower than the s...

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Veröffentlicht in:Journal of Geophysical Research 2004-03, Vol.109 (A3), p.A03220.1-n/a
Hauptverfasser: Zeng, W., Horwitz, J. L., Craven, P. D., Rich, F. J., Moore, T. E.
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Sprache:eng
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