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Table 6 Average uncertainties during the calibration and validation phases in the Casamance basin in Kolda and the Kayanga basin in 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 uncertainties

Uncertainties in validation

Kolda

9,65

9,45

Wassadou

2,77

1,78