Colleagues,
I am currently calibrating my model and am getting excellent monthly Nash-Sutcliffe (N-S) values (0.88) and decent/good seasonal N-S on flow (0.6-0.9)! I have yet to run daily. However, after initial parameter modifications based on sensitivity analysis and autocalibration, I'm getting even higher N-S values but poorer PBIAS ones. It seems that N-S and PBIAS are inversely proportional on monthly and seasonal flow in my research. For instance, my initial N-S for winter flow was 0.64 with a PBIAS of 29.26%. After running autocalibration on the snowmelt parameters, my N-S shot up to 0.9 but my PBIAS also increased to 30.48%. My initial N-S for spring was 0.76 with a PBIAS of 1.6%, the autocallibration on snowmelt increased N-S to 0.77 and my PBIAS to 2.2%. My N for seasonal flow is 14 for winters and 15 for spring (it's lower for winter, defined as winter as Dec/Jan/Feb, because I'm beginning my simulation in January). I see similar patterns on monthly flow. My review of the literature indicates that N-S is most commonly used, but according to the following article, the minimization of PBIAS values is also really important:
"
Moriasi,
D. N., J. G. Arnold, M. W. Van Liew, R. L. Bingner, R. D. Harmel, and T. L.
Veith
(2007), Model
evaluation guidelines for systematic quantification of accuracy in watershed
simulations, Trans. ASABE, 50(3), 885-900.
So, I have two questions.
A) Has anyone seen a PBIAS for seasonal flow that is 30% or more? This seems a bit high to me but Moriasi et al. (2007) indicates that PBIAS up to 25% on monthly flow is acceptable.
B) Even more important: would I be correct in assuming that my primary goal should be maxmization of N-S, and then to just use PBIAS if the values fall within an acceptable range (and not work actively to calibrate based on N-S?)
Thanks very much for your insights.
-Justin