Vg. Vorobjev et al., EXTENDED PERIOD OF POLAR-CAP AURORAL DISPLAY - AURORAL DYNAMICS AND RELATION TO THE IMF AND THE IONOSPHERIC CONVECTION, Annales geophysicae, 13(8), 1995, pp. 854-862
An unusually extended period (5 h) of polar cap auroral display on 3 A
ugust 1986 is examined. Auroras have been investigated using ground-ba
sed data as well-as measurements from the IMP-8 space-craft in interpl
anetary space and simultaneous observations from the polar-orbiting sa
tellites Viking and DE-1 in the northern and southern hemispheres, res
pectively. It is found that visible Sun-aligned arcs are located insid
e the transpolar band of the theta-aurora observed from the satellite
in ultraviolet wavelengths,The transpolar band can contain several Sun
-aligned arcs that move inside the band toward the morning or-evening
side of the auroral oval independent of the direction of the-band move
ment. Intensifications of polar cap auroras With durations of up to ab
out 30 min are observed. No change has been found in either IMF parame
ters or substorm activity that can be related to these intensification
s. The theta-aurora occurred during a 2-h period when the B-z-componen
t of the IMF was negative. A tendency is noted for dawnward (duskward)
displacement of the transpolar band when B-y > 0 (B-y < 0) in the sou
thern hemisphere. Simultaneous observations of auroral ovals during in
terplanetary B-z < 0, B-y < 0 and B-x > 0 in both hemispheres and conv
ection patterns for B-z < 0 and B-y < 0 have been displayed using sate
llite and ground-based measurements. It was found that the transpolar
band of the theta-aurora in the sunlit hemisphere was situated in the
region of large-scale downward Birkeland currents.