FIELD: geophysics, short-time prediction of seismic risks. SUBSTANCE: linear cloud anomalies are recorded with specified interval. Their density and entropy as well as distance between two successive linear cloud anomalies are determined. Then temperature of surface above which linear cloud anomalies were recorded is found. Amplitude of elastic waves is established from specified relation. Temperature of surface of explored territory is determined by way of surface scanning from spacecraft. Linear cloud anomalies are also recorded from spacecraft. Recording equipment is installed in crossing points of tectonic fractures and projection of linear cloud anomaly. Opinion on presence of seismic hazard is formed when value of amplitude of elastic wave with which magnitude found by data of seismic zoning is achieved. EFFECT: raised efficiency of forecasting seismic hazard. 3 cl
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