UDC 550.388.2+551.510.536 We present for the first time the experimental data on the frequency of ion–neutral collisions at the altitudes of the ionospheric E layer, which were obtained by the method of resonance scattering of the radio waves by artificial periodic irregularities of the ionospheric plasma. The measurements were carried out in different time periods from 1990 to 2012. Time and altitude dependences of the collision frequency are given. The dependence of the collision frequency on the solar and geomagnetic activity has been analyzed. Collisions of electrons and ions with atoms and molecules play an important role in physics of the ionosphere and atmosphere. In particular, they determine the friction force and should be taken into account in the equations of motion of a medium when its viscosity increases. The frequency of ion–neutral collisions affects the energy and momentum transfer processes [1–4]. When propagation of internal gravity waves above 100 km is considered, it is needed to allow for dissipation due to increasing viscosity of the medium [4–7], which is directly related to collisions. The frequency νin of collisions between ions and neutral molecules should also be taken into account when the low-frequency processes associated with the plasma conductivity are analyzed (see, e. g., [8]). However, the experimental data on νin are fairly scarce. Meanwhile, considerable variations in the ion–neutral collision frequency can be observed in the upper ionosphere. These variations are due most frequently to the neutral atmosphere density variations caused by the transmission of internal gravity and tidal waves. Variations from day to day can be due to propagation of planetary waves. At the altitudes of the upper mesosphere and lower thermosphere, the neutral atmosphere density variations according to the lidar data can exceed 20%, while the temperature variations can reach 70 K [9, 10]. Observations suggest that during propagation of gravity waves the collision frequency can be changed by a factor of 1.5–2 for half an hour [9, 11]. The collision frequency variations can also be a consequence of variations in the composition of both the ion component and the neutral atoms and molecules. In particular, in the ionospheric E region, variations in the ion–neutral collision frequency can be caused by the penetration of metal meteor particles and ions that contribute to the formation of both the sporadic layers of the electron density and the layer with increased content of Na, K, Fe, etc. atoms [12–15]. In this paper, we present the results of determining the ion–molecule collision frequency obtained by the method of resonant scattering of radio waves by artificial periodic irregularities of the plasma at the altitudes of the ionospheric E region.
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