The paper examines the data of geographic northward (X), eastward (Y) and vertical (Z) components of the magnetic field from a dense array of 26 vector magnetometers operated in N-NE Brazil from November 1990 to March 1991. As expected, the daily variation of X showed a minor maximum around 03:00–04:00 LT and a major maximum around 12:00 LT. The daily range of ΔY showed a strong minimum around noon at all stations. The combined ΔY and ΔX indicated the direction of the equatorial electrojet currents to be flowing along 25° north of east at the centre and 20° north of east at the edges of the equatorial electrojet (EEJ) belt. The centre of the EEJ as defined by the zero intercept of the Z versus latitude was found to be near...
Data sets collected during a few coordinated Equatorial Ionosphere-Thermosphere System (EITS) observ...
The enhancement of the diurnal range of the horizontal component (H) of the earth's magnetic field o...
The magnetic equator in the Brazilian region has moved over 1,100 km northward since 1957, passing t...
149-166The paper describes the diurnal and latitudinal variations of the horizontal (H), eastward (Y...
We examined the longitudinal variability of the equatorial electrojet (EEJ) and the occurrence of i...
The strength of the equatorial electrojet is shown to be stronger at 75°W longitudes than at 45°W lo...
The structure of the equatorial electrojet during disturbed condition is examined using data from 10...
67-74The paper describes the daily and seasonal variations of declination (or eastward geomagnetic ...
In the framework of the French participation in the International Equatorial Electrojet Year (IEEY)...
The newly established geomagnetic field observations in Japan, have enabled us to analyse the 1998 d...
International audienceHuancayo is the only equatorial electrojet station where the daytime increase ...
This paper discusses the effects of currents induced inside the Earth at equatorial latitudes due to...
present the analysis of 16 selected quiet days, for which a simple model of an equivalent current di...
Made available in DSpace on 2019-09-12T16:53:23Z (GMT). No. of bitstreams: 0 Previous issue date: ...
The equatorial electrojet (EEJ) is a narrow band of current flowing eastward at the ionospheric E re...
Data sets collected during a few coordinated Equatorial Ionosphere-Thermosphere System (EITS) observ...
The enhancement of the diurnal range of the horizontal component (H) of the earth's magnetic field o...
The magnetic equator in the Brazilian region has moved over 1,100 km northward since 1957, passing t...
149-166The paper describes the diurnal and latitudinal variations of the horizontal (H), eastward (Y...
We examined the longitudinal variability of the equatorial electrojet (EEJ) and the occurrence of i...
The strength of the equatorial electrojet is shown to be stronger at 75°W longitudes than at 45°W lo...
The structure of the equatorial electrojet during disturbed condition is examined using data from 10...
67-74The paper describes the daily and seasonal variations of declination (or eastward geomagnetic ...
In the framework of the French participation in the International Equatorial Electrojet Year (IEEY)...
The newly established geomagnetic field observations in Japan, have enabled us to analyse the 1998 d...
International audienceHuancayo is the only equatorial electrojet station where the daytime increase ...
This paper discusses the effects of currents induced inside the Earth at equatorial latitudes due to...
present the analysis of 16 selected quiet days, for which a simple model of an equivalent current di...
Made available in DSpace on 2019-09-12T16:53:23Z (GMT). No. of bitstreams: 0 Previous issue date: ...
The equatorial electrojet (EEJ) is a narrow band of current flowing eastward at the ionospheric E re...
Data sets collected during a few coordinated Equatorial Ionosphere-Thermosphere System (EITS) observ...
The enhancement of the diurnal range of the horizontal component (H) of the earth's magnetic field o...
The magnetic equator in the Brazilian region has moved over 1,100 km northward since 1957, passing t...