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Inductive seismo-electromagnetic effect in relation to seismogenic ULF emission
Natural Hazards and Earth System Sciences
During the seismic wave propagation through the crust, the electromagnetic pulse can originate due to MHD conversion in this conductive medium. On the assumption of simple models of seismic wave excitation and attenuation, the problem is reduced to the analysis of a diffusionlike equation for a vector potential function. In this way, we need to change the classical gauge condition. A semianalytical form of the solution is obtained in a case with constant ground conductivity. Dependencies of thedoi:10.5194/nhess-1-61-2001 fatcat:sgkj6zbfjrboxh5iuls6ihg3aq