EISCAT observations of the interplanetary scintillation of a single so
urce were made over an extended period of time, during which the orien
tation of the baselines between the two observing sites changed signif
icantly. Assuming that maximum correlation between the scintillations
observed at the two sites occurs when the projected baseline is parall
el to the direction of plasma flow, this technique can be used to make
a unique determination of the direction of the solar wind. In the pas
t it has usually been assumed that the plasma flow is radial, but meas
urements of eleven sources using this technique have indicated conclus
ively that in at least six cases observed at mid or high heliocentric
latitude there is a significant non-radial component directed in four
cases towards the heliocentric equator and in two cases towards the po
le.