Abstract
A trough station (Ouagadougou station) of African Equatorial Ionization Anomaly sector foF2 long term trends are carried out after the elimination of solar cycle long term variation part. For this part, foF2 is expressed as a third degree polynomial function of Rz. We analyzed diurnal, seasonal and annual foF2 long term trends during 30 years covering the period 1966-1996. Diurnal trend variation showed positive hourly trend at the morning (slope maximum value at 0400 LT: + 1.5 x 10 -3 per year) and at night (slope maximum value at 2200 LT: + 0.7 x 10 -3
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