EISCAT has been used to make three types of measurement of the charact
eristics of the solar wind in the range 10-120 solar radii. The rms fl
uctuation in the total power received from a single source can be meas
ured to provide a 'scintillation index'. The cross-correlation of the
scintillations observed at two sites can be used to measure the veloci
ty of the solar wind, indicating at the same time whether one or more
velocity streams control the correlation. The rate al which the correl
ation coefficient drops as the transverse separation of the two beams
increases gives an indication of the transverse scales of the irregula
rities. Examples are given of all three types of measurement made duri
ng campaign periods between 1990 and 1993.