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| Titel |
Geomagnetic control of the spectrum of traveling ionospheric disturbances based on data from a global GPS network |
| VerfasserIn |
E. L. Afraimovich, E. A. Kosogorov, O. S. Lesyuta, I. I. Ushakov, A. F. Yakovets |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
0992-7689
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| Digitales Dokument |
URL |
| Erschienen |
In: Annales Geophysicae ; 19, no. 7 ; Nr. 19, no. 7, S.723-731 |
| Datensatznummer |
250014284
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| Publikation (Nr.) |
 copernicus.org/angeo-19-723-2001.pdf |
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| Zusammenfassung |
In this paper an attempt
is made to verify the hypothesis of the role of geomagnetic disturbances as a
factor in determining the intensity of traveling ionospheric disturbances (TIDs).
To improve the statistical validity of the data, we have used the method
involving a global spatial averaging of disturbance spectra of the total
electron content (TEC). To characterize the TID intensity quantitatively, we
suggest that a new global index of the degree of disturbance should be used,
which is equal to the mean value of the rms variations in TEC within the
selected range of spectral periods (of 20– 60 min, in the present case). The
analysis has been made for a set of 100 to 300 GPS stations for 10 days with a
different level of geomagnetic activity (Dst from 0 to –350 nT; the Kp
index from 3 to 9). It was found that power spectra of daytime TEC variations
in the range of 20–60 min periods under quiet conditions have a power-law
form with the slope index k = –2.5. With an increase in the level of magnetic
disturbance, there is an increase in the total intensity of TIDs, with a
concurrent kink of the spectrum caused by an increase in oscillation intensity
in the range of 20–60 min. The TEC variation amplitude is found to be smaller
at night than during the daytime, and the spectrum decreases in slope, which is
indicative of a disproportionate increase in the amplitude of the small-scale
part of the spectrum. It was found that an increase in the level of geomagnetic
activity is accompanied by an increase in the total intensity of TEC; however,
it does not correlate with the absolute level of Dst, but rather with
the value of the time derivative of Dst (a maximum correlation
coefficient reaches –0.94). The delay of the TID response of the order of 2
hours is consistent with the view that TIDs are generated in auroral regions,
and propagate equatorward with the velocity of about 300–400 m/s.
Key words. Ionosphere (ionospheric
disturbances; auroral ionosphere; equatorial ionopshere) |
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