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Volume 16, issue 6
Ann. Geophys., 16, 677–697, 1998
https://doi.org/10.1007/s00585-998-0677-6
© European Geosciences Union 1998

Special issue: Electrojet

Ann. Geophys., 16, 677–697, 1998
https://doi.org/10.1007/s00585-998-0677-6
© European Geosciences Union 1998

  30 Jun 1998

30 Jun 1998

A study of transient variations in the Earth's electromagnetic field at equatorial electrojet latitudes in western Africa (Mali and the Ivory Coast)

J. Vassal*,1, M. Menvielle2,*, Y. Cohen3, M. Dukhan1, V. Doumouya4, K. Boka4, and O. Fambitakoye5 J. Vassal et al.
  • 1Laboratoire de Géophysique, ORSTOM, 72 route d'Aulnay, F-93140 Bondy, France
  • 2Equipe de Physique de la Terre et des Planètes (URA 1369), Bât. 504, Université Paris Sud, F-91405 Orsay cedex, France
  • 3Laboratoire de Géomagnétisme, IPGP, B89, 4 Place Jussieu, F-75252 Paris cedex 05, France
  • 4Laboratoire de Physique de l'Atmosphère, Université d'Abidjan, Abidjan, Cote D'Ivoire
  • 5Laboratoire de Géophysique, ORSTOM, 72 route d'Aulnay, F-93140 Bondy, France, now retired
  • *Present address: CETP/CNRS, 4 Avenue de Neptune, F-94107 Saint Maur Des Fosses Cedex, France

Abstract. In the framework of the French-Ivorian participation to the IEEY, a network of 10 electromagnetic stations were installed at African longitudes. The aim of this experiment was twofold: firstly, to study the magnetic signature of the equatorial electrojet on the one hand, and secondly, to characterize the induced electric field variations on the other hand. The first results of the magnetic field investigations were presented by Doumouya and coworkers. Those of the electric field experiment will be discussed in this study. The electromagnetic experiment will be described. The analysis of the electromagnetic transient variations was conducted in accordance with the classical distinction between quiet and disturbed magnetic situations. A morphological analysis of the recordings is given, taking into consideration successively quiet and disturbed magnetic situations, with the results interpreted in terms of the characterization of external and internal sources. Particular attention was paid to the effects of the source characteristics on the induced field of internal origin, and to the bias they may consequently cause to the results of electromagnetic probing of the Earth; the source effect in electromagnetic induction studies. During quiet magnetic situations, our results demonstrated the existence of two different sources. One of these, the SRE source, was responsible for most of the magnetic diurnal variation and corresponded to the well-known magnetic signature of the equatorial electrojet. The other source (the SR*E source) was responsible for most of the electric diurnal variation, and was also likely to be an ionospheric source. Electric and magnetic diurnal variations are therefore related to different ionospheric sources, and interpreting the electric diurnal variation as induced by the magnetic field diurnal variation is not relevant. Furthermore, the magnetotelluric probing of the upper mantle at dip equator latitudes with the electromagnetic diurnal variation is consequently impossible to perform. In the case of irregular variations, the source effect related to the equatorial electrojet is also discussed. A Gaussian model of equatorial electrojet was considered, and apparent resistivities were computed for two models of stratified Earth corresponding to the average resistive structure of the two tectonic provinces crossed by the profile: a sedimentary basin and a cratonic shield. The apparent resistivity curves were found to depend significantly on both the model used and the distance to the center of the electrojet. These numerical results confirm the existence of a daytime source effect related to the equatorial electrojet. Furthermore, we show that the results account for the observed differences between daytime and night-time apparent resistivity curves. In particular, it was shown that electromagnetic probing of the Earth using the classical Cagniard-Tikhonov magnetotelluric method is impossible with daytime recordings made at dip latitude stations.

Key words. Electromagnetics (Transient and time do- main) Geomagnetism and paleomagnetism (geomagne- tic induction) Ionosphere (equatorial ionosphere)

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