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Environmental Sciences Europe

Table 4 Correlation between observed and simulated flows in calibration and validation 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

Station

Correlation coefficient for calibration

Correlation coefficient in Validation

Kolda

0,81

0,84

Wassadou

0,59

0,92

  1. If the coefficients are on an interval of 0.3 to 1, the correlation is considered positive and strong
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