Geomagnetic pulsations and ionospheric inhomogeneities

Details Geomagnetic pulsations and ionospheric inhomogeneities Geomagnetic pulsations and ionospheric inhomogeneities

Jun 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980ge%26ae..20..551g&link_type=abstract

Geomagnetizm i Aeronomiia, vol. 20, May-June 1980, p. 551, 552. In Russian.

Computer Science

Geomagnetic Pulsations, Ionospheric Disturbances, Sporadic E Layer, Inhomogeneity, Ionograms, Magnetic Signatures

Scientific paper

In the present paper, experimental data are used as a basis to analyze the influence of sporadic E layers of various intensities and heights of formation on the field of long-period geomagnetic pulsations. Simultaneous analysis of ionospheric and magnetic data showed that an increase in sporadic E intensity leads to an increase in pulsation amplitude at heights between 100 and 110 km, and to a decrease in this amplitude at heights between 120 and 130 km, both in the H- and D-components. A decrease in sporadic E intensity leads to the opposite effect.

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