Mechanism of negative disturbances of the f0F2 at the geomagnetic equator in the daytime

Details Mechanism of negative disturbances of the f0F2 at the geomagnetic equator in the daytime Mechanism of negative disturbances of the f0F2 at the geomagnetic equator in the daytime

Dec 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991ge%26ae..31.1027m&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 31, Nov.-Dec. 1991, p. 1027-1031. In Russian.

Computer Science

1

Equatorial Atmosphere, F 2 Region, Ionospheric Disturbances, Magnetic Equator, Magnetic Storms, Critical Frequencies, Equatorial Electrojet, Ionospheric Drift

Scientific paper

It is shown that the formation of negative disturbances of the F2-layer critical frequency (f0F2) at the geomagnetic equator during intense magnetic storms may be due to different mechanisms. Most frequently, these disturbances are connected with increases in the strength of the zonal Ey-component of the eastward electric field, leading to an intensified plasma transport from the equatorial F2-layer. Less frequently these disturbances are connected with a significant increase in the westward Ey-component, causing a displacement of the F2-layer at low heights into a region of elevated recombination rate.

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