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Geomagnetic pulsations are generated
at great distances from the Earth's surface
due to a plasmic instabilities of different
kinds and a resonance processes in the
solar wind and in the magnetospheric-
ionospheric plasma. After complex pro-
cesses of transformation and propagation
along force lines of the magnetic field to
the Earth's surface, they induce telluric
currents in the conducting earth's crust.
Geomagnetic pulsations observed on the
earth's surface carry information about
both the physical parameters of interplane-
tary medium, magnetosphere and iono-
sphere, and geoelectric features of the
Earth's crust. At the same time geomagne-
tic pulsations are natural hindrances that
should be taken into account during the
performance of precise magnetic surveys
including surveys on marine and aircraft
bearers. The research on the frequency of
geomagnetic pulsation appearance and on
the spatial-temporal distribution on their
parameters can present highly useful and
valuable material that can be considered in
a wide context depending on the direction
of investigations.
Yu. A. Kopytenko andV. S. Ismagilov
"Peculiarities of the recalculation of geomagnetic variations on-shore base stations to aquatories in auroral and subauroral latitudes", Proc. SPIE 2111, Symposium on Russian Airborne Geophysics and Remote Sensing, (1 November 1993); https://doi.org/10.1117/12.162870
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Yu. A. Kopytenko, V. S. Ismagilov, "Peculiarities of the recalculation of geomagnetic variations on-shore base stations to aquatories in auroral and subauroral latitudes," Proc. SPIE 2111, Symposium on Russian Airborne Geophysics and Remote Sensing, (1 November 1993); https://doi.org/10.1117/12.162870