Skip to Main Content
Table 8

Goodness-of-fit statistics of daily hydrological extremes simulated by the SWAT model in the tropical river basins

BasinLow discharge (Q95) statistics
High discharge (Q5) statistics
R2wR2NSER2RSR
Bago, Myanmara – – 0.666 0.981 0.578 
Belu, Myanmar 0.955 0.002 0.836 0.953 0.405 
Sekong, Laos 0.959 0.457 0.711 0.935 0.537 
Sesan, Vietnam 0.862 0.162 0.141 0.841 0.927 
Srepok, Cambodia 0.936 0.435 0.155 0.982 0.919 
3S (Laos, Cambodia and Vietnam) 0.453 0.243 −2.464 0.992 1.861 
BasinLow discharge (Q95) statistics
High discharge (Q5) statistics
R2wR2NSER2RSR
Bago, Myanmara – – 0.666 0.981 0.578 
Belu, Myanmar 0.955 0.002 0.836 0.953 0.405 
Sekong, Laos 0.959 0.457 0.711 0.935 0.537 
Sesan, Vietnam 0.862 0.162 0.141 0.841 0.927 
Srepok, Cambodia 0.936 0.435 0.155 0.982 0.919 
3S (Laos, Cambodia and Vietnam) 0.453 0.243 −2.464 0.992 1.861 

aThe observed low discharge data (Q95) mostly comprises zero discharge values; consequently, the statistics could not be calculated.

Close Modal

or Create an Account

Close Modal
Close Modal