The dynamics of the lithospheric potential at spatially separated experimental polygons and from channels of predominant reception of different directions, mainly characterized by a high correlation, is disturbed in accordance with the periods of anomalies in the heat and humidity regime of the study region. This allows us to suggest common causes of significant anomalies in the dynamics of meteorological and lithospheric events. An analysis of such coordinated effects of the influence of factors of different scales in various components of the Earth's geosystem and the search for possible mechanisms can help to find signs and predictors of the formation of critical states in weather and climate.
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