Appraisement over Effect of Wave Conductivity on Selected Districts of North Shoa Zone Ionosphere During a High Solar Activity Phase

The ionospheric conductivity is an important variable determined by the mobility of the charged particles and it also dependent of the plasma, neutral number of densities and charged particles. The ionosphere has advantages to absorb the harmful radiation from the Sun for all radio communications, navigation and surveillance transmissions through it. Temperature, cloudy and precipitations are the most factors to determine the wave mobility in the ionosphere region. The conductivity of the three selected districts depends on the altitude variation during day and night time. At altitudes of about 80 to 5000 km there is a flow of a number of current systems. This study was analysis the daily, monthly and seasonal contour variations of ionospheric conductivity in selected districts with their geographic latitude and longitude value. The wave conductivity was vary and increase throughly for the selected Models of Hall, Pederson and parallel conductivities with height and time variability of the ionospheric conductivities, cloudy and the precipitation was analysed with temperature variation for each districts.