Оценка скорости движения нейтральной атмосферы на высотах максимума F-области по данным некогерентного рассеяния

Abstract

The results of calculation of daytime electron densityprofile using continuity equation are presented. Experimental data of charged particle temperatures and plasma transport velocity at 300 km are used. At analysis of ionospheric parameters agreement vertical component of plasma velocity, caused by thermospheric wind is calculated.