Environmental Sciences Europe

Table 3 Average flows observed and simulated (mm) by the GR2M model in the Casamance basin at Kolda and the Kayanga basin at Wassadou

From: Hydrological response of tropical rivers basins to climate change using the GR2M model: the case of the Casamance and Kayanga-Géva rivers basins

Descriptors	Calibration			Validation
Descriptors	Observed flow	Simulated flow	Difference	Observed flow	Simulated flow	Difference
Kolda	17,4	14,8	− 2,6	17,6	19,2	1,6
Wassadou	0,007	0,005	− 0,001	0,013	0,015	− 0,002

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