“…In the summer hemisphere maximum emissions in the transpolar arc (theta aurora) can range from 500 to 2000 R, in the winter hemisphere maximum emissions are less than 500 R, as measured by Polar UVI. Transpolar arcs have similar particle characteristics as the auroral oval, which suggests an origin in the plasma sheet or plasma sheet boundary layer (see also Meng, 1981;Peterson and Shelley, 1984;Frank et al, 1986;Frank and Craven, 1988;Huang et al, 1987Huang et al, , 1989. Obara et al (1996) presented the probability of average energy of precipitating electrons producing small-scale Sun-aligned arcs in the night side and day side polar cap, based on a few hundred such satellite measurements.…”