Mansilla, G.A. (2001) Low latitude vertical drifts due to intensified electric fields on the F2-region during storm conditions. Il nuovo cimento C, 24 C (6). pp. 887-892. ISSN 1826-9885
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Abstract
The low latitude and longitude effects of an enhanced electric field on the daytime ionospheric F2-region are analyzed using a simple model. The calculations performed have been applied to the early stages of a geomagnetic storm, when the magnetospheric electric field is intensified. For storms with commencement near local noon it has been found that the electric field effect on the vertical drift and peak electron density of the F2 region is pronounced at equatorial latitudes, decreasing with increasing latitude, which indicates a smoothing of the equatorial anomaly shortly after the geomagnetic storm starts. The results obtained with the model are in concordance with experimental observations.
Item Type: | Article |
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Uncontrolled Keywords: | Geomagnetism and paleomagnetism; geoelectricity ; Geoelectricity; electromagnetic induction and conductivity (magnetotelluric effects) |
Subjects: | 500 Scienze naturali e Matematica > 550 Scienze della Terra |
Depositing User: | Marina Spanti |
Date Deposited: | 11 Mar 2020 15:42 |
Last Modified: | 11 Mar 2020 15:42 |
URI: | http://eprints.bice.rm.cnr.it/id/eprint/14737 |
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