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Table 7 Variation in rainfall and mean annual temperature over the future period (2021–2100) compared with the historical period (1985–2014) at the Kolda and Wassadou stations

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

Rainfall

Casamance in Kolda

Kayanga in Wassadou

SSP1-2.6

SSP5-8.5

SSP1-2.6

SSP5-8.5

2021–2040

− 7,90

2,64

− 6,4

2,3

2041–2060

− 6,11

− 7,77

− 5,2

− 7,7

2061–2080

− 9,25

− 16,31

− 8,4

− 15,6

2081–2100

− 10,97

− 22,15

− 9,0

− 21,2

2021–2100

− 8,61

− 11,04

− 7,2

− 10,6

Temperature

SSP1-2.6

SSP5-8.5

SSP1-2.6

SSP5-8.5

2021–2040

1,43

1,18

1,59

1,29

2041–2060

1,80

2,43

1,98

2,53

2061–2080

2,09

3,77

2,25

3,87

2081–2100

1,98

5,20

2,12

5,31

2021–2100

1,84

3,18

1,99

3,25