Research Article
Modeling Evapotranspiration Response to Climatic Forcings Using Data-Driven Techniques in Grassland Ecosystems
Table 5
Comparisons of data-driven model performances for evapotranspiration among the training, validation, and prediction periods at DE-Gri site.
| Model | Training | Validation | Prediction | | NSE | RMSE | MAE | | NSE | RMSE | MAE | | NSE | RMSE | MAE |
| ANN | 0.8633 | 0.8630 | 0.3470 | 0.2426 | 0.9341 | 0.8927 | 0.3411 | 0.2336 | 0.9623 | 0.9341 | 0.2769 | 0.1942 | GRNN | 0.8612 | 0.8603 | 0.3504 | 0.2487 | 0.9294 | 0.8814 | 0.3587 | 0.2478 | 0.9585 | 0.9292 | 0.2871 | 0.2058 | GMDH | 0.8396 | 0.8396 | 0.3755 | 0.2707 | 0.9326 | 0.8724 | 0.3719 | 0.2573 | 0.9619 | 0.9253 | 0.2949 | 0.2121 | ELM-Sig | 0.8535 | 0.8535 | 0.3589 | 0.2580 | 0.9358 | 0.8885 | 0.3478 | 0.2347 | 0.9669 | 0.9392 | 0.2659 | 0.1920 | ELM-Sin | 0.8546 | 0.8546 | 0.3575 | 0.2522 | 0.9477 | 0.9066 | 0.3182 | 0.2203 | 0.9711 | 0.9398 | 0.2646 | 0.1896 | ELM-Hard | 0.8012 | 0.8012 | 0.4180 | 0.2911 | 0.8926 | 0.8724 | 0.3720 | 0.2662 | 0.9053 | 0.8765 | 0.3791 | 0.2534 | ANFIS-Grid | 0.8772 | 0.8772 | 0.3285 | 0.2304 | 0.9173 | 0.8713 | 0.3735 | 0.2447 | 0.9574 | 0.9334 | 0.2785 | 0.1961 | ANFIS-SC | 0.8637 | 0.8637 | 0.3461 | 0.2427 | 0.9230 | 0.8716 | 0.3732 | 0.2397 | 0.9501 | 0.9088 | 0.3258 | 0.2167 | ANFIS-FCM | 0.8636 | 0.8636 | 0.3462 | 0.2439 | 0.9244 | 0.8744 | 0.3691 | 0.2378 | 0.9500 | 0.9099 | 0.3238 | 0.2159 | SVM-RBF | 0.8638 | 0.8633 | 0.3466 | 0.2306 | 0.9196 | 0.8796 | 0.3614 | 0.2332 | 0.9407 | 0.9002 | 0.3408 | 0.2092 | SVM-Poly | 0.7885 | 0.7852 | 0.4345 | 0.3221 | 0.7629 | 0.7043 | 0.5662 | 0.3879 | 0.8461 | 0.8199 | 0.4578 | 0.3407 | SVM-Sig | 0.0170 | −0.0682 | 43.738 | 37.467 | 0.0001 | −0.3639 | 37.708 | 31.554 | 0.1190 | −0.2045 | 45.388 | 39.515 |
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Note. The unit of RMSE and MAE is mm day−1.
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