Ionospheric storm effects at subauroral latitudes - A case study

Details Ionospheric storm effects at subauroral latitudes - A case study Ionospheric storm effects at subauroral latitudes - A case study

Feb 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991jgr....96.1275p&link_type=abstract

Journal of Geophysical Research (ISSN 0148-0227), vol. 96, Feb. 1, 1991, p. 1275-1288.

Physics

59

Auroral Zones, F Region, Ionospheric Storms, Neutral Gases, Ionosondes, Ionospheric Electron Density

Scientific paper

An attempt is made to classify ionospheric storm effects at subauroral latitudes according to their presumed origin. The storm of December 7/8, 1982, serves as an example. It is investigated using ionosonde, electron content, and DE 2 satellite data. The following effects are distinguished: (1) positive storm effects caused by traveling atmospheric disturbances, (2) positive storm effects caused by changes in the large-scale thermospheric wind circulation, (3) positive storm effects caused by the expansion of the polar ionization enhancement, (4) negative storm effects caused by perturbations of the neutral gas composition, and (5) negative storm effects caused by the equatorward displacement of the trough region.

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