INVESTIGATION OF THE RESPONSE OF THE MICROSEISMIC BACKGROUND TO GEOMAGNETIC IMPULSES AT THE MID-LATITUDE OBSERVATORY “MIKHNEVO”
https://doi.org/10.52676/1729-7885-2018-2-36-43
Abstract
The response of the seismic background to pulsed geomagnetic variations is investigated for the conditions of the midlatitude Geophysical observatory “Mikhnevo” of the Institute of Geosphere Dynamics of the Russian Academy of Sciences. During the impulse variations of the magnetic field of SSC- and SI-types, in most cases, increased variations of the seismic background are observed in the frequency range of 0.01–0.1 Hz (in some cases, 0.001–0.1 Hz). The application of methods of statistical data processing made it possible to establish that it is the perturbation of the geomagnetic field that entails a change in the microseismic background and with some delay. The significant correlation between the amplitude of the geomagnetic impulse and the amplitude of the induced variations of the seismic background was established and the quantitative relationship between them was obtained. The analysis showed that after the geomagnetic impulse with a short delay in the behavior of the magnetic tipper module, “jumplike” changes (i.e., a change in the magnitude of the induced electric currents) are observed.
About the Author
S. A. Riabova
Institute of Geosphere Dynamics of the Russian Academy of Sciences
Russian Federation
Moscow
Russian Federation
Moscow
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For citations:
Riabova S.A. INVESTIGATION OF THE RESPONSE OF THE MICROSEISMIC BACKGROUND TO GEOMAGNETIC IMPULSES AT THE MID-LATITUDE OBSERVATORY “MIKHNEVO”. NNC RK Bulletin. 2018;(2):36-43. (In Russ.) https://doi.org/10.52676/1729-7885-2018-2-36-43
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