On ionic and electrostatic nature of cloudy anomalies activation above seismically active linear zones
© Belyi T.A., Zelenin Yu.A.
Onedimensional model of medium selfcoordinated electrostatic field (SF) of lower atmosphere (030 km)
has been obtained. The model has been presented by Poisson equation for selfcoordinated field of electrons within dense gas. Exact
solution has been found in approximation of constant coefficients corresponding to integrability of classical Morse oscillator.
The solution is parametrized by the values of field energy in the unit of volume. Basic functions of linear approximation, in
contrast to homogenous approximation of DebyeHuckel, are Eyre functions (Ai, Bi) which show oscillation hyperpolarizing
ability of electrons distribution in the gravity field. Within the limits of this model injectionpolarization mechanism has been
proposed of stabilization of linear cloudy anomalies (LCA) by the waves of charge density in heterogeneous (overabundant)
electronicionic subsystem of the atmosphere in vertical stratified field. Calculations demonstrated that disturbance of surface
electrostatic field from seismically active faults or edges of earthquakes sources is enough for polarization of charged subsystem
of water steam of LCA.
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