The multi-beam high resolution MU radar experiments, conducted in February
2000, revealed for the first lime kilometer-scale waves in the lower E-regi
on over Shigaraki, Japan. The waves, occurring over a narrow height range o
f 92 - 97 km, have vertical wavelengths of 0.6 to 1.2 km and periods of 30
to 90 s. The signal intensities associated with these waves, with signal-to
-noise ratio values less than similar to 5 dB, are lower by about 20 dB com
pared to that of the quasi-periodic echoes occurring at higher heights. The
echoes occur with both negative and positive range rates, changing systema
tically from one to the other with values of about -25 m s(-1) and 20 m s(-
1), respectively. The Doppler velocities, ranging -50 to 25 m s(-1), are ge
nerally of the same sense as range rates, but somewhat greater in magnitude
. The periodicity and wavelength of the waves seem to resemble those reveal
ed in the equatorial electrojet by the high resolution Jicamarca radar obse
rvations and also by the nonlocal nonlinear simulations of the gradient-dri
ft instability. Behavior of the Doppler velocities, however, is found to be
different from that reported for the kilometer-scale waves in the equatori
al region.