Recent years have seen unprecedented rainfall and flooding in the central and eastern Sahel, even extending north into the Sahara desert. The present-day situation represents a stark contrast the drought in the 1970s and 1980s. In the presentation, it will be shown that the rainfall trends align with a northeastward shift of the West African monsoon related to a strengthening of the heat low over the East Sahara. It is hypothesised that the latter is related to a reduced heat low ventilation due to the warming of the Eastern Mediterranean sea surface temperatures and an enhanced „local“ greenhouse effect due to enhanced atmospheric humidity over the Saharo-Sahelian region. The currently development can be seen as a harbinger of the coming decades.