Fig. 9From: Hydrological response of tropical rivers basins to climate change using the GR2M model: the case of the Casamance and Kayanga-Géva rivers basinsVariation in future flow simulated by the GR2M model for the period 2021–2100 at the Wassadou station in the Kayanga-Géva basin, according to the SSP1-2.6 and 585 climate change scenarios for the periods 2021–2040, 2041–2060, 2061–2080, and 2081–2100Back to article page