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Environmental Sciences Europe

Table 5 Average robustness criteria of 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

Average performance (calibration)

Average performance (validation)

Average performance

Variation % change

Kolda

65,1

62,6

63,8

2,9

Wassadou

48,0

50,1

49,1

0

  1. The average performance used here is the average value of the three types of Nash used (Nash (Q), Nash (√Q), and Nash (ln(Q)))
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