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INTERNATIONAL JOURNAL OF GEOMAGNETISM AND AERONOMY,
VOL. 6,
GI2005,
doi:10.1029/2005GI000109,
2006
Variability of horizontal component of geomagnetic element (H) with mean quiet-day variation
F. N. Okeke
Department of Physics and Astronomy, University of Nigeria, Nsukka, Enugu, Nigeria
Abstract
[1] The variability of Sq (H) with mean quiet-day variation at equatorial electrojet latitudes and other latitudes has been studied using the correlation
between the hourly amplitudes of the H variations dH, at these stations. It was found that these hourly amplitudes of H under equatorial electrojet regions are well correlated with themselves. High significant correlation was established among
them. On the other hand, low correlation was found among pairs of equatorial electrojet stations and other latitude stations
not under the equatorial electrojet. It was discovered that most times, the variation in the current intensities of the worldwide
part of Sq (WSq) and the equatorial electrojet (EEJ) have contrasting phases. It was concluded that the very low correlation coefficients
calculated and the contrasting phases of EEJ and WSq current intensities were due to the fact that changes in EEJ current intensity are controlled mainly by E
z
, while changes in WSq current are driven mainly by E
y
.
Received 22
March
2005;
accepted 20
December
2005;
published 24
February
2006.
Keywords: Equatorial electrojet;
Geomagnetic field;
Current system.
Index Terms: 2409 Ionosphere: Current systems (2721); 2736 Magnetospheric Physics: Magnetosphere/ionosphere interactions (2431); 2712 Magnetospheric Physics: Electric fields (2411).
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Citation: Okeke, F. N.
(2006),
Variability of horizontal component of geomagnetic element (H) with mean quiet-day variation,
Int. J. Geomagn. Aeron.,
6,
GI2005,
doi:10.1029/2005GI000109.
Copyright 2006 by the American Geophysical Union.
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