International audienceIn 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...
International audienceIn this study we examined the influences of geomagnetic activity on the Earth ...
The newly established geomagnetic field observations in Japan, have enabled us to analyse the 1998 d...
present the analysis of 16 selected quiet days, for which a simple model of an equivalent current di...
In the framework of the French participation in the International Equatorial Electrojet Year (IEEY)...
Ten electromagnetic stations were set up as a coordinated programme for the International Equatorial...
International audienceIn the framework of the French-Ivorian participation to the IEEY, a network of...
Hourly values of the deviations in the geomagnetic X and Y field for the three years 1962-64 are stu...
An empirical model of the equatorial electrojet (EEJ), including local time and longitude dependence...
International audienceWe apply a simple linear transform, the along-track second derivative, to four...
We examined the longitudinal variability of the equatorial electrojet (EEJ) and the occurrence of i...
During the years 1993–1994, a continuous campaign of measurements has been held in the frame of the ...
International audienceThe longitudinal variation of the Equatorial Electrojet (EEJ) intensity has be...
The equatorial electrojet (EEJ) is a unique feature of the Earth's external current systems because ...
International audienceThe daytime eastward equatorial electric field (EEF) in the ionospheric E-regi...
The structure of the equatorial electrojet during disturbed condition is examined using data from 10...
International audienceIn this study we examined the influences of geomagnetic activity on the Earth ...
The newly established geomagnetic field observations in Japan, have enabled us to analyse the 1998 d...
present the analysis of 16 selected quiet days, for which a simple model of an equivalent current di...
In the framework of the French participation in the International Equatorial Electrojet Year (IEEY)...
Ten electromagnetic stations were set up as a coordinated programme for the International Equatorial...
International audienceIn the framework of the French-Ivorian participation to the IEEY, a network of...
Hourly values of the deviations in the geomagnetic X and Y field for the three years 1962-64 are stu...
An empirical model of the equatorial electrojet (EEJ), including local time and longitude dependence...
International audienceWe apply a simple linear transform, the along-track second derivative, to four...
We examined the longitudinal variability of the equatorial electrojet (EEJ) and the occurrence of i...
During the years 1993–1994, a continuous campaign of measurements has been held in the frame of the ...
International audienceThe longitudinal variation of the Equatorial Electrojet (EEJ) intensity has be...
The equatorial electrojet (EEJ) is a unique feature of the Earth's external current systems because ...
International audienceThe daytime eastward equatorial electric field (EEF) in the ionospheric E-regi...
The structure of the equatorial electrojet during disturbed condition is examined using data from 10...
International audienceIn this study we examined the influences of geomagnetic activity on the Earth ...
The newly established geomagnetic field observations in Japan, have enabled us to analyse the 1998 d...
present the analysis of 16 selected quiet days, for which a simple model of an equivalent current di...