By T. Hagfors (auth.), Bengt Hultqvist, Tor Hagfors (eds.)
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In the expansion phase of the substorm, increased magnetospheric convection and high ionospheric conductivity (caused by increased electron precipitation) cause the inner edge of the plasma sheet to come nearer to the Earth on Fig. 6. Schematic of the magnetospheric-convection current circuit. The abbreviations "Rl," "R2, .. and "PRe" refer respectively to region-l Birkeland currents, region-2 Birkeland currents, and partial ring current. , 1981b). 32 R. A. WOLF AND R. W. SPIRO the nightside, and the partial ring current and region-2 Birkeland currents are large.
This configuration results in a very strong sunward convection in the central polar cap region and a similar strong antisunward convection in the morning side of the polar cap when IMF is eastward and on the evening side of the polar cap when the IMF is westward. In forming his model Lassen (1979) assumed homogeneous conductivities within greater areas of the polar cap. II .. • Figure 12. -. ~.. 5 Y in the lower row. Middle column: Possible positions of Birkeland currents associated with shears and irregularities in the flow.
High-Latitude Space Plasma Physics by T. Hagfors (auth.), Bengt Hultqvist, Tor Hagfors (eds.)