Slide
-Middle-small scale density-electric field turbulence appears as
a result of non-linear cascade development of the large-scale IT,
which intensified near equator (equatorial spread-F) and near
polar-ward EA gradients. We can see common k-distribution both
for large-scale and middle –small IT and latitude dependence of the
electric field “bursts” of IT on the satellites IK-24 and Aureol-3