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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 16, issue 6
Ann. Geophys., 16, 658-666, 1998
https://doi.org/10.1007/s00585-998-0658-9
© European Geosciences Union 1998

Special issue: Electrojet

Ann. Geophys., 16, 658-666, 1998
https://doi.org/10.1007/s00585-998-0658-9
© European Geosciences Union 1998

  30 Jun 1998

30 Jun 1998

Equatorial electrojet at African longitudes: first results from magnetic measurements

V. Doumouya1, J. Vassal2, Y. Cohen3, O. Fambitakoye2, and M. Menvielle4 V. Doumouya et al.
  • 1Laboratoire de Physique de l'Atmosphère, Université d'Abidjan, Abidjan, Ivory Coast
  • 2Laboratoire de Géophysique, ORSTOM, 32 av. Henri-Varagnat, F-93143 Bondy Cedex, France
  • 3Laboratoire de Géomagnétisme, IPGP, B89, 4 Place Jussieu, F-75252 Paris Cedex 05, France
  • 4CETP CNRS, 4 Avenue de Neptune, F-94107 Saint-Maur Des Fossés Cedex,France

Abstract. In the framework of the French participation in the International Equatorial Electrojet Year (IEEY), ten magnetotelluric stations were installed between November 1992 and November 1994 along a 1200-km-long meridian profile, between Lamto (latitude 6.2°N, Côte d'Ivoire) to the south and Tombouctou (latitude 16.7°N, Mali) to the north. These stations measured digitally the three components of the magnetic field and the two components of the telluric electric field, and operated over a period of 20 months. The magnetic data is used to study the features of the equatorial electrojet (EEJ) in West African longitude. The measurement of the telluric electric field variations will be presented elsewhere. Hourly mean values are used to study the morphological structure of the regular diurnal variation SR of the three components (H, D, and Z) of the earth magnetic field and to characterize the EEJ during magnetically quiet days. The occurrences of the counter-electrojet (CEJ) are set forth, emphasizing its seasonal variability. Assumed to be a current ribbon, the EEJ main parameters (the position of its center, its width, and the amplitude of its current density at the center) are determined. A preliminary analysis of the time variations of these parameters is presented over period of 20 months (from January 1993 to August 1994). Results are compared with those obtained during previous experiments of the same kind.

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