Traveling ionospheric disturbances and the sporadic F2 layer in the midlatitude ionosphere

Details Traveling ionospheric disturbances and the sporadic F2 layer in the midlatitude ionosphere Traveling ionospheric disturbances and the sporadic F2 layer in the midlatitude ionosphere

Jun 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986ge%26ae..26..396s&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 26, May-June 1986, p. 396-400. In Russian.

Computer Science

Sound

1

F 2 Region, Ionospheric Sounding, Midlatitude Atmosphere, Solar Activity Effects, Solar Terrestrial Interactions, Traveling Ionospheric Disturbances, Annual Variations, Vertical Distribution

Scientific paper

It is shown that TIDs responsible for sickle-shaped reflections on vertical-sounding ionograms can lead to the formation of the sporadic F2 layer. In winter (the low-solar-activity period) when the F2 maximum is lowest, the F2s layer can be induced by a TID propagating in the meridional plane toward the equator. In summer (the high-solar-activity period), a mesoscale TID recorded in the NmF2 region propagates in the zonal direction and does not lead to the formation of the F2s layer.

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