Physics
Scientific paper
Feb 2005
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005jgra..11002304c&link_type=abstract
Journal of Geophysical Research, Volume 110, Issue A2, CiteID A02304
Physics
8
Ionosphere: Auroral Ionosphere (2704), Magnetospheric Physics: Auroral Phenomena (2407), Magnetospheric Physics: Magnetosphere: Outer, Ionosphere: Ionosphere/Magnetosphere Interactions (2736), Magnetospheric Physics: Energetic Particles: Precipitating
Scientific paper
High-latitude transpolar arcs (TPAs) are often observed during northward interplanetary magnetic field (IMF); of these, theta aurora are seen when transpolar arcs move in the dawn or dusk direction across the entire polar region in response to IMF By changes. Periods of study were chosen when By changes sign during steady northward IMF in order to determine the influence of IMF Bx, By, the strength of the IMF, the solar wind, and Earth dipole tilt on the occurrence and motion of high-latitude TPAs forming theta aurora. For a 4.5-year period there are 55 events for which IMF Bz is northward for at least 2 hours before and at least 3 hours after a By sign change. Of these, 19 occurred when the Polar satellite was over the Northern Hemisphere for the duration of the event. We find that for northward IMF and a By sign change theta aurora are almost always formed in the Northern Hemisphere, regardless of Bx and dipole tilt. This implies that theta aurorae form simultaneously in both hemispheres. IMF By does not appear to influence the intensity and duration of the arc. Strongest UV emissions occur in the summer hemisphere. Evolution time has a fairly complex dependence on solar wind parameters.
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