Mathematics
Scientific paper
Aug 2001
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001esasp.471..369n&link_type=abstract
In: 15th ESA Symposium on European Rocket and Balloon Programmes and Related Research, 28 - 31 May 2001, Biarritz, France. Ed.:
Mathematics
Earth Atmosphere, Geodynamics
Scientific paper
The most powerful geodynamic processes are located beneath the World Ocean's bottom covering about 80% of the earth surface. Seismic excitations (i.e. disturbances of its mechanical state) in ocean lithosphere accompanied by tsunami and/or earthquakes are manifestations of these large-scale processes. Is it possible to get information about them in the form of electromagnetic (EM) signals in the atmosphere? EM signals associated by researches with seismic activity of ocean lithosphere have been detected, in particular, by ground-based magnetometers in near sea Pacific regions. Trying to clear out the mechanism of EM signals and answer the above question we formulate a mathematical model of seismo-hydro-EM field interaction and trace numerically generation and propagation of these signals.
Ershov Sergey
Mikhaylovskaya Irina
Novik Oleg
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