Latitude of the polar wall of the main ionospheric trough as an index of geomagnetic activity level

Details Latitude of the polar wall of the main ionospheric trough as an index of geomagnetic activity level Latitude of the polar wall of the main ionospheric trough as an index of geomagnetic activity level

Jun 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989ge%26ae..29..389g&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 29, May-June 1989, p. 389-393. In Russian.

Computer Science

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Earth Ionosphere, Geomagnetism, Magnetic Effects, Polar Regions, Earth Magnetosphere, Electron Diffusion, Ionospheric Sounding, Latitude, Plasmapause, Space Plasmas

Scientific paper

Experimental data on the coincidence of the latitude of the polar wall of the main ionospheric trough with the position of the equatorial boundary of the diffuse precipitation zone of low-energy electrons indicate that this latitude can be used as an index of geomagnetic activity level. This index has a determinate time lag on the average, can be measured directly from the ground or from satellites, and has a clear physical meaning.

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