It is found at Ibadan that during the daylight hours fEs is lower on magnetically disturbed days than on quiet days. It is also found that on two or three occasions in each month a series of abnormally low values of fEs occurs. An investigation of the behaviour of the horizontal and vertical components of the earth's field during these times reveals that there is a simultaneous decrease in the magnitude of the equatorial electrojet current which is in turn responsible for the large diurnal ranges in H and Z near the equator. The behaviour of the F2 layer parameters f0F2, ymF2 and hmF2 during periods of low fEs, shows that the F2 layer always becomes denser, lower and thinner during these periods.
This indicates an immediate connection between the electrojet, the production of equatorial Es and vertical drifts in the F2 layer.