Pi1C geomagnetic pulsations in the region of the eastern electrojet

Details Pi1C geomagnetic pulsations in the region of the eastern electrojet Pi1C geomagnetic pulsations in the region of the eastern electrojet

Dec 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991ge%26ae..31..997k&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 31, Nov.-Dec. 1991, p. 997-1002. In Russian.

Computer Science

Sound

Auroral Electrojets, F 2 Region, Geomagnetic Micropulsations, Magnetic Storms, Electron Precipitation, Ionospheric Sounding, Plasmapause

Scientific paper

Pi1C pulsations, observed at postnoon hours and consisting in the fine structure of a positive magnetic bay (the eastern electrojet), are investigated on the basis of multiyear observations at auroral latitudes. On the earth's surface, the Pi1C pulsations are recorded in the region between the projection of the main ionospheric trough and the Harang discontinuity. These pulsations are not accompanied by riometric absorption and are localized in the region of their source, i.e., they do not propagate along the earth's surface.

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