Abstract-The disappearance of Esq type traces from ionograms a t the magnetic equator during magnetically quiet periods is related to inverted latitudinal profiles of the regular daily magnetic 8, variation (in its horizontal and vertical components). Latitude profiles obtained from a meridian chain of nine magnetometers across central Africa me compared with corresponding quarter-hourly ionogram sequences from Fort-Archambault-Sarh (Chad). Between O900 and 1500 LT, the magnetic reversal coincides exactly with the disappearance of Esq traces. This evidence gives additional weight to the hypothesis of a counter-electrojet current belt, located on exactly the same latitudes as the normal electrojet and probably flowing below it at the bottom ...
The electron density distribution in the E region during counter electrojets is investigated. Rocket...
Radar observations made at Jicamarca show that the equatorial electrojet current and the E and F reg...
164-166Changes in the horizontal drifts measured by spaced receiver technique at a low latitude stat...
The disappearance of Esq type traces from ionograms at the magnetic equator during magnetically quie...
114-118The examination of horizontal geomagnetic fields at Huancayo and Fuquene with corresponding f...
6-12Disappearances of equatorial sporadic-E (Es-q) are normally associated with depressions in the g...
Based on simultaneous observations of the horizontal geomagnetic field component H, sporadic E (Es )...
The counter-electrojet currents are evidenced by the disappearance of theq type of Es layer (Es-q) o...
67-68Published F-region vertical ion drift observations for Jicamarca are analyzed in conjunction wi...
The characteristics of different types of Sporadic E (E<SUB>S</SUB>) layers and the associated plasm...
The occurrence of sporadic E at an equatorial station during magnetically quiet daytime conditions c...
1-15The characteristics of equatorial counter electrojet events associated with the reversal of the ...
The study describes the time and space morphologies of a rather new type of counter electrojet event...
It is shown that the quiet day afternoon counter-electrojet events at equatorial stations are the re...
We examined the longitudinal variability of the equatorial electrojet (EEJ) and the occurrence of i...
The electron density distribution in the E region during counter electrojets is investigated. Rocket...
Radar observations made at Jicamarca show that the equatorial electrojet current and the E and F reg...
164-166Changes in the horizontal drifts measured by spaced receiver technique at a low latitude stat...
The disappearance of Esq type traces from ionograms at the magnetic equator during magnetically quie...
114-118The examination of horizontal geomagnetic fields at Huancayo and Fuquene with corresponding f...
6-12Disappearances of equatorial sporadic-E (Es-q) are normally associated with depressions in the g...
Based on simultaneous observations of the horizontal geomagnetic field component H, sporadic E (Es )...
The counter-electrojet currents are evidenced by the disappearance of theq type of Es layer (Es-q) o...
67-68Published F-region vertical ion drift observations for Jicamarca are analyzed in conjunction wi...
The characteristics of different types of Sporadic E (E<SUB>S</SUB>) layers and the associated plasm...
The occurrence of sporadic E at an equatorial station during magnetically quiet daytime conditions c...
1-15The characteristics of equatorial counter electrojet events associated with the reversal of the ...
The study describes the time and space morphologies of a rather new type of counter electrojet event...
It is shown that the quiet day afternoon counter-electrojet events at equatorial stations are the re...
We examined the longitudinal variability of the equatorial electrojet (EEJ) and the occurrence of i...
The electron density distribution in the E region during counter electrojets is investigated. Rocket...
Radar observations made at Jicamarca show that the equatorial electrojet current and the E and F reg...
164-166Changes in the horizontal drifts measured by spaced receiver technique at a low latitude stat...