Schumann resonances (SR) are electromagnetic radiation (EMR) that constantly exist in the Earth's atmosphere, the spectrum of which is characterized by the presence of pronounced and fairly stable frequency maxima. In 1952, Schumann (1952 theoretically predicted the existence of resonant modes at frequencies close to 8, 14, 20, … Hz resulting from interference of low-frequency EMR in the Earth-ionosphere waveguide. Due to their global nature, SR can be reliably recorded in any region on the Earth's surface (Sentman & Fraser, 1991) and are an indicator of global thunderstorm activity on the planet (Clayton & Polk, 1976;Heckman et al., 1998), since the exact values of the frequency of peaks of the SR spectrum are associated with the spatiotemporal distribution and intensity of thunderstorms (