This work addresses the experimental study of an important aspect in the general problem of lithosphere-magnetosphere coupling, namely the correlation between the Pc1 electromagnetic waves (0.2–5 Hz) and the earthquakes. Using long time series of measurements from the catalogues of Pc1 and earthquakes, we revealed a new effect: the diurnal Pc1 activity in the middle latitudes is statistically higher the lower the diurnal global seismic activity. We assume that the influence of earthquake-related acoustic waves on the upper atmosphere suppresses the activity of the Pc1 waves.
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Polar Geophysical Institute, ApatityPolar Geophysical Institute, Apatity
Yahnina T.A.
Yahnin A.G.
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Polar Geophysical Institute, ApatityPolar Geophysical Institute, Apatity
Yahnin A.G.
Raita T.
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Sodankylä Geophysical Observatory, SodankyläPolar Geophysical Institute, Apatity
Raita T.
Manninen J.
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Sodankylä Geophysical Observatory, SodankyläPolar Geophysical Institute, Apatity
Manninen J.
Goldstein J.
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Southwest Research Institute, San Antonio, 78238, TX
Physics and Astronomy Department, University of Texas, San Antonio, 78238, TXPolar Geophysical Institute, Apatity