Over the past decades, Africa has been affected by significant rainfall anomalies: for instance, both the Horn of Africa and West Africa suffered severe droughts during the 1970s and 1980s (e.g., Williams et al., 2012) and, recently, the City of Cape Town in South Africa was hit by one of the worst multi-year droughts in decades (Otto et al., 2018). On the other hand, severe floods have affected countries located in dry areas, such as Algeria, Tunisia, Egypt, and Somalia (Niang et al., 2014).The analysis and the understanding of precipitation trends and variability rely on the availability of observational records (e.g., Sun et al., 2018). Reliable observational data sets are also of paramount importance in the evaluation of climate models (e.g., Maidment et al., 2015;Tapiador et al., 2017). In fact, both general circulation models (GCMs) and regional climate models (RCMs) still show limitations in simulating various aspects of the African precipitation (e.g.,