What the rainfall anomaly data holds
Season rainfall stated as a percentage departure from the long-term normal, for every administrative unit and season across sub-Saharan Africa, with the mean over the unit plus the driest and wettest pixel found inside it. 0 means normal, −93 means almost no rain at all against that normal, +300 means 4 times the normal. Seasons carry their own name per country; Kenya’s long rains are marmay, its short rains octdec. Country codes throughout this layer run 3 letters.
Forward only
The published product only ever carries the current state of a season, so history on the platform starts with the first stamp in June 2026 and simply lengthens by a week at a time from there. A season’s final value is whatever the last stamp read right before that season closed.
The 47 counties on 26 August
The chart ranks the long-rains departure across every Kenyan county. The coast reads well below normal: Mombasa −136, Kwale −93, Kilifi −64, Lamu −56. The western breadbasket sits below to near normal: Bungoma 26, Kakamega 39, Busia 41, Trans Nzoia 82. The central highlands, by contrast, run far above: Murang’a 837, Kiambu 762, Nairobi 546, Machakos 476, large mostly because the rain fell against a genuinely low normal there. The western figures line up exactly with the July hotspot bulletin, which had already named Bungoma, Kakamega, Uasin Gishu, Elgeyo Marakwet and Trans Nzoia for moisture stress.
Reading with the vegetation series
A below-normal vegetation anomaly in a unit whose rainfall also reads below normal is simply a rainfall story. The same anomaly under normal rainfall points somewhere else entirely: planting date, pest pressure, input availability. Both datasets key to the same unit, and rainfall tends to lead vegetation by 2 to 4 weeks, roughly the time cropland takes to respond.