Other
Scientific paper
Apr 1994
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994angeo..12..226m&link_type=abstract
Annales Geophysicae (ISSN 0992-7689), vol. 12, no. 2/3, p. 226-231
Other
7
Equatorial Regions, Ionosondes, Magnetic Equator, Magnetic Storms, Neutral Gases, Anomalies, Mathematical Models, Plasma Drift, Plasma Waves
Scientific paper
Theoretical model calculations along with ground-based observations from Huancayo ionosonde station and ESRO-4 gas analyzer data, were used to estimate the contribution of neutral gas composition changes and E x B vertical plasma drift to the observed F2-layer storm effects at the geomagnetic equator. Atomic oxygen concentration increase may give the main contribution to the positive NmF2 effect when drift velocity changes are small, but negative storm effects, on the other hand, are related mostly to vertical drift variations.
Foerster Michael
Mikhailov Alexander. V.
Skoblin M. G.
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