A method is developed to calculate nonlinear zonal, s(x), and meridional, s
(y), longitudinal advective accelerations from MU radar observations with a
ntenna beam scanning in eight directions. The results of measurements of s(
x) and s(y) at altitudes of 2 - 18 km on April 16 - 18, 1997, are presented
. The values of s(x) and s(y) are mainly between -0.01 m s(-2) and 0.01 m s
(-2) with increases up to +/-0.04 m s(-2) during tens of minutes to several
hours in regions with vertical scales up to several kilometers. Such extre
mes are more frequent at the altitudes of tropo-stratospheric jet at 10 - 1
5 km and may indicate regions of inclination from geostrophic balance and o
f increased generation of atmospheric waves.