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Read Full Article (file size: 786579 bytes) Cited by
GEOPHYSICAL RESEARCH LETTERS,
VOL. 30, NO. 6,
1344,
doi:10.1029/2002GL015866,
2003
Seasonal variations along auroral field lines: Measurements from the Polar spacecraft
M. T. Johnson
School of Physics and Astronomy,
University of Minnesota,
Minneapolis,
Minnesota,
USA
J. R. Wygant
School of Physics and Astronomy,
University of Minnesota,
Minneapolis,
Minnesota,
USA
C. A. Cattell
School of Physics and Astronomy,
University of Minnesota,
Minneapolis,
Minnesota,
USA
F. S. Mozer
Space Science Laboratory,
University of California,
Berkeley,
California,
USA
Abstract
Measurements from the Polar electric field instrument are used to study large electric fields and the ambient plasma density
as a function of altitude (1.8–6.0 RE geocentric). Results from the premidnight sector (1800–2400 MLT) along auroral field lines show roughly a fourfold increase
in the occurrence of small scale size, large amplitude electric fields (>100 mV m−1) at altitudes from 1.9 to 2.5 RE for dark compared to sunlit ionospheric conditions. Density values inferred from spacecraft potential measurements show these
electric fields to be correlated with low plasma densities (0.2 to 3.0 cm−3). An increase in the average plasma density from 10 to 60 cm−3 is also observed for sunlit compared to dark conditions for the same altitude range. In addition, the distribution of density
measurements from 1.9 to 2.2 RE also show evidence for an increase in cold ionospheric plasma (from ∼30 to 60 cm−3) for sunlit compared to dark ionospheric conditions.
Published 29
March
2003.
Index Terms: 2704 Magnetospheric Physics: Auroral phenomena (2407); 2736 Magnetospheric Physics: Magnetosphere/ionosphere interactions; 2712 Magnetospheric Physics: Electric fields (2411).
Read Full Article (file size: 786579 bytes) Cited by
Citation: Johnson, M. T., J. R. Wygant, C. A. Cattell, and F. S. Mozer
(2003),
Seasonal variations along auroral field lines: Measurements from the Polar spacecraft,
Geophys. Res. Lett.,
30(6),
1344,
doi:10.1029/2002GL015866.
Copyright 2003 by the American Geophysical Union.
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