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FIGURE 7.4. Parameter of plasma ionization versus height of the ionosphere above the ground surface.

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ionosphere at altitudes of 90 700 km. It is clearly seen that such parameters can reach great values, though, in the ordinary sense the ionospheric plasma is weakly ionized. Another argument to use this parameter as a degree of plasma ionization, is based on the fact that at altitudes under consideration of 80 500 km, which mostly affects radio propagation, Nm > Ne and Nm > Ni provides the condition of stability of a full plasma pressure necessary for the transport process of diffusion and drift. Under such circumstances different disturbances of neutral molecules or atoms and their movement do not in uence the diffusion of electrons and ions in the ionospheric plasma [8 10]. That is why, just as in References [8 10], we evaluated the degree of ionization of the ionospheric plasma by a parameter of ionization p shown in Figure 7.4 and presented in Table 7.1 for daily and nocturnal ionosphere. The increase in the degree of ionization in the ionosphere, observed in Figure 7.4, has a very simple physical explanation: with the increase of altitude the effective values of the collision frequencies of charged particles with neutrals fall, de ned by Equations (7.3) and (7.5), whereas a frequency of electron ion interactions increases, as de ned by Equation (7.4), because with the growth of the height, the number of neutral plasma components quickly decreases, while the total number of ions in the ionosphere increases. It must be noted that beginning from z > 500 km (even this fact is not so important for radio communication), the growth of the parameter p decelerates with the increase in height, while the degree of plasma magnetization (as was mentioned above) is monotonically increasing with height.

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