The EISCAT UHF radar system was used to study the characteristics of E
-region coherent backscatter at very large magnetic aspect angles (5-1
1 degrees). Data taken using 60 mu s pulses during elevation scans thr
ough horizontally uniform backscatter permitted the use of inversion t
echniques to determine height profiles of the scattering layer. The la
yer was always singly peaked, with a mean height of 104 km, and mean t
hickness (full width at half maximum) of 10 km, both independent of as
pect angle. Aspect sensitivities were also estimated, with the Sodanky
la-Tromso link observing 5 dB/degree at aspect angles near 5 degrees,
decreasing to 3 dB/degree at 10 degrees aspect angle. Observed coheren
t phase velocities from all three stations were found to be roughly co
nsistent with LOS measurements of a common E-region phase velocity vec
tor. The E-region phase velocity had the same orientation as the F-reg
ion ion drift velocity, but was approximately 50% smaller in magnitude
. Spectra were narrow with skewness of about +1 (for negative velociti
es), increasing slightly with aspect angle.