Atmospheric Electricity and Earth’s Microseisms

V. N. Shuleikin and G. G. Shchukin

Increase in the amplitudes of microseisms within the range from the tenths of hertz to 10 kHz leads to increase in the values of air polar conductivity and to decrease in atmospheric electric field. As the frequency of microseisms decreases, the efficiency of microseismic impact increases. In case of low amplitudes of microseisms, decrease in atmospheric electric field is observed only as a result of multi- month active impact on the geologic environment.

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