A. Viljanen, SOURCE EFFECT ON GEOMAGNETIC INDUCTION VECTORS IN THE FENNOSCANDIAN AURORAL REGION, Journal of Geomagnetism and Geoelectricity, 48(7), 1996, pp. 1001-1009
Geomagnetic induction vectors were calculated at the IMAGE magnetomete
r stations in Fennoscandia using hundreds of four-hour events of quiet
time variations, and of magnetic storms due to eastward and westward
electrojets. Quiet time vectors were found to be very similar to those
calculated previously using a set of carefully selected plane wave ev
ents. Due to the source effect during electrojet events, the average d
irection of the induction vectors may rotate tens of degrees compared
to the quiet time. The length generally increases tens of percent, but
at the stations MAS and SOR near the electrojet and highly-conducting
anomalies, a decrease is observed. If the quiet time induction vector
is longer than about 0.50 then the source effect does not affect the
direction of the vector remarkably even if the length may change consi
derably. If the conductivity anomaly is weaker (quiet time vector shor
ter than about 0.30) then the source effect dominates near the electro
jet (PEL, MUG, KEV, KIL), but is less important farther away (NUR, OUJ
). If a large number of magnetically quiet events are available of loc
al morning hours, no special reduction of the source effect is needed
in the research area.