Observations of ionospheric flux ropes above South Pole

Numerical techniques have been used to investigate two different models of the current flow in ionospheric flux ropes, giving attention to the problem of mapping the electric field from the ionosphere down to balloon altitudes and to the isolated event that occurred at about 1625 UT on January 3, 19...

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Bibliographic Details
Main Authors: Lin, Z. M., Benbrook, J. R., Bering, E. A., Byrne, G. J., Friis-Christensen, E., Liang, D., Liao, B., Theall, J.
Language:unknown
Published: 1990
Subjects:
46
Online Access:http://ntrs.nasa.gov/search.jsp?R=19920048648
Description
Summary:Numerical techniques have been used to investigate two different models of the current flow in ionospheric flux ropes, giving attention to the problem of mapping the electric field from the ionosphere down to balloon altitudes and to the isolated event that occurred at about 1625 UT on January 3, 1986. Also examined are Greenland magnetometer chain and Iqaluit magnetometer data, which imply that the isolated event was localized in longitude as well as 'global', in the sense that it occurred at conjugate points. IMP 8 solar wind plasma and IMF data indicate that the even occurred just as a strong southward turning of the IMF passed the earth.