“…Obviously, the observed extremes in West African rainfall (especially the Guinea Coast) is likely to increase owing to the strong impacts of climate variability, environmental changes, influence of tropical Atlantic sea surface temperature (SST) anomalies, and the nature of West African Monsoon, which is largely controlled by interactions between continental surfaces and the oceans (see, e.g., Rodríguez‐Fonseca et al, ; Losada et al, ; Redelsperger and Lebel, ; Polo, Rodríguez‐Fonseca, Losada & García‐Serrano, ; Redelsperger et al, ). The overarching outcomes of a plethora of related studies in West Africa (see, e.g., Ndehedehe, Awange, Corner, Kuhn & Okwuashi, ; Diatta and Fink, ; Nicholson, ; Paeth et al, ; Bader and Latif, ; Joly and Voldoire, ; Losada et al, ; Ali and Lebel, ; Giannini et al, ; Reason and Rouault, ), be it region‐specific or basin scale, overwhelmingly agree on the roles of climatic variations through changes in the global oceans, mesoscale convective systems, and indices of climate variability (e.g., ENSO, Atlantic Multi‐decadal Oscillation [AMO], PDO, etc.) on precipitation patterns and other water fluxes (e.g., stream flow).…”