“…The interaction of these spheres among themselves, as well as with the sun, the moon, and the planets of the solar system, determines the geodynamics of Earth as a planet [1][2][3]. Between the individual elements of this geodynamic system there are connections that are clearly traceable in time and space, the study of which is an important element in the knowledge of our planet [4,5]. Obviously, the huge size of this geodynamic system does not allow the carrying out of area-based direct observation of its physical fields, so the role of remote-sensing methods, which have been widely developed in recent decades, is increasing [6][7][8][9][10].…”