Equatorial electrojet at African longitudes: first results from magnetic measurements

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 Tomb...

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Main Authors: V. Doumouya, J. Vassal, Y. Cohen, O. Fambitakoye, M. Menvielle
Format: Article
Language:English
Published: Copernicus Publications 1998-06-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/16/658/1998/angeo-16-658-1998.pdf
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author V. Doumouya
J. Vassal
Y. Cohen
O. Fambitakoye
M. Menvielle
author_facet V. Doumouya
J. Vassal
Y. Cohen
O. Fambitakoye
M. Menvielle
author_sort V. Doumouya
collection DOAJ
description 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 S<sub>R</sub> of the three components (<i>H</i>, <i>D</i>, and <i>Z</i>) 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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spelling doaj.art-edafaae18352439e966ac17376a0a09c2022-12-22T01:23:14ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761998-06-011665866610.1007/s00585-998-0658-9Equatorial electrojet at African longitudes: first results from magnetic measurementsV. Doumouya0J. Vassal1Y. Cohen2O. Fambitakoye3M. Menvielle4Laboratoire de Physique de l'Atmosph&#x00E8;re, Universit&#x00E9; d'Abidjan, Abidjan, Ivory CoastLaboratoire de G&#x00E9;ophysique, ORSTOM, 32 av. Henri-Varagnat, F-93143 Bondy Cedex, FranceLaboratoire de G&#x00E9;omagn&#x00E9;tisme, IPGP, B89, 4 Place Jussieu, F-75252 Paris Cedex 05, FranceLaboratoire de G&#x00E9;ophysique, ORSTOM, 32 av. Henri-Varagnat, F-93143 Bondy Cedex, FranceCETP CNRS, 4 Avenue de Neptune, F-94107 Saint-Maur Des Foss&#x00E9;s Cedex,FranceIn 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 S<sub>R</sub> of the three components (<i>H</i>, <i>D</i>, and <i>Z</i>) 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.https://www.ann-geophys.net/16/658/1998/angeo-16-658-1998.pdf
spellingShingle V. Doumouya
J. Vassal
Y. Cohen
O. Fambitakoye
M. Menvielle
Equatorial electrojet at African longitudes: first results from magnetic measurements
Annales Geophysicae
title Equatorial electrojet at African longitudes: first results from magnetic measurements
title_full Equatorial electrojet at African longitudes: first results from magnetic measurements
title_fullStr Equatorial electrojet at African longitudes: first results from magnetic measurements
title_full_unstemmed Equatorial electrojet at African longitudes: first results from magnetic measurements
title_short Equatorial electrojet at African longitudes: first results from magnetic measurements
title_sort equatorial electrojet at african longitudes first results from magnetic measurements
url https://www.ann-geophys.net/16/658/1998/angeo-16-658-1998.pdf
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AT ofambitakoye equatorialelectrojetatafricanlongitudesfirstresultsfrommagneticmeasurements
AT mmenvielle equatorialelectrojetatafricanlongitudesfirstresultsfrommagneticmeasurements