Slide
As concerned of satellite effects a new approach as follows:
- Equatorial Anomaly exists in a state of margin stability
(near a level of instability). Its large-scale dynamics is determined
by penetration of the large-scale atmospheric turbulence (AGW)
inside lower ionosphere. In result large-scale plasma density IT
appears, it can be observed even at the upper ionosphere on the
satellite. This point is supported by connection of large-scale
density IT with EA and its almost classic k-distribution.