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Table 2 Results of calibration and validation of the GR2M model 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

Casamance basin in Kolda

Period

Nash (Q)

Nash (√Q)

Nash (ln(Q)) in % (ln(Q) in %)

Balance sheet

Calibration

1981–1986

70,4

73,4

51,5

1,18

Validation

1987–1992

69,0

70,3

48,4

1,09

Kayanga basin at Wassadou

Period

Nash (Q)

Nash (√Q)

Nash (ln(Q)) in % (ln(Q) in %)

Balance sheet

Calibration

1985–1988

21,5

58,9

63,5

1,40

Validation

1999–2002

83,8

52,4

14,2

0,87