Field-aligned currents in the polar cap at small IMF <formula>Bz and <formula>By inferred from SuperDARN radar observations

Details Field-aligned currents in the polar cap at small IMF <formula>Bz and <formula>By inferred from SuperDARN radar observations Field-aligned currents in the polar cap at small IMF <formula>Bz and <formula>By inferred from SuperDARN radar observations

Jan 2000

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2000jgr...105..205k&link_type=abstract

Journal of Geophysical Research, Volume 105, Issue A1, p. 205-214

Physics

4

Ionosphere: Current Systems, Ionosphere: Plasma Convection, Magnetospheric Physics: Magnetosphere/Ionosphere Interactions, Magnetospheric Physics: Solar Wind/Magnetosphere Interactions

Scientific paper

Routine SuperDARN observations of the ionospheric plasma convection and field-aligned currents (FACs) in the high-latitude ionosphere are used to study current systems established at small interplanetary magnetic field (IMF) Bz and By. By statistical averaging of available data sets we show that under this IMF condition the ionospheric convection pattern consists of two (evening and morning) convection cells that are similar in shape. The flow intensity inside the central polar cap is noticeably depressed so that plasma entering the polar cap flows around its border, predominantly along the lines of equal magnetic latitude, so that the convection cells are of a crescent-like shape. This global pattern of plasma flow is associated with the effect of the region 0 field-aligned currents coexisting with the region 1 and region 2 field-aligned currents. SuperDARN observations of FACs for individual events support this conclusion. FACs were derived by analyzing the vorticity of the SuperDARN convection maps. We show that region 0 currents for small IMF Bz and By can exist in time sectors way off the magnetic noon. Thus radar observations support earlier findings from satellite magnetometer measurements of the region 0 current system at high latitudes during both the prenoon and afternoon at small IMF intensities. Because the region 0 FACs occur during small IMF intensities, it is suggested that quasi-viscous processes play a role in their generation.

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