Research Article
Modeling Evapotranspiration Response to Climatic Forcings Using Data-Driven Techniques in Grassland Ecosystems
Table 4
Comparisons of data-driven model performances for evapotranspiration among the training, validation and prediction periods at CA-Let site.
| Model | Training | Validation | Prediction | | NSE | RMSE | MAE | | NSE | RMSE | MAE | | NSE | RMSE | MAE |
| ANN | 0.7593 | 0.7590 | 0.3791 | 0.2541 | 0.8553 | 0.7671 | 0.5690 | 0.3546 | 0.7859 | 0.7334 | 0.5911 | 0.3607 | GRNN | 0.8417 | 0.8176 | 0.3298 | 0.1997 | 0.8112 | 0.6472 | 0.7002 | 0.4096 | 0.7415 | 0.6307 | 0.6957 | 0.3919 | GMDH | 0.6673 | 0.6673 | 0.4454 | 0.3036 | 0.8303 | 0.6887 | 0.6577 | 0.4018 | 0.6931 | 0.6343 | 0.6922 | 0.4134 | ELM-Sig | 0.7159 | 0.7159 | 0.4115 | 0.2821 | 0.8038 | 0.7045 | 0.6409 | 0.4057 | 0.7469 | 0.6907 | 0.6367 | 0.3913 | ELM-Sin | 0.7163 | 0.7163 | 0.4113 | 0.2805 | 0.8423 | 0.7570 | 0.5811 | 0.3582 | 0.7530 | 0.6998 | 0.6272 | 0.3787 | ELM-Hard | 0.5615 | 0.5615 | 0.5113 | 0.3602 | 0.6843 | 0.5572 | 0.7845 | 0.4758 | 0.6013 | 0.5446 | 0.7725 | 0.4733 | ANFIS-Grid | 0.7820 | 0.7820 | 0.3605 | 0.2418 | 0.8480 | 0.7869 | 0.5443 | 0.3473 | 0.7805 | 0.7380 | 0.5859 | 0.3527 | ANFIS-SC | 0.7691 | 0.7691 | 0.3711 | 0.2495 | 0.8467 | 0.7712 | 0.5639 | 0.3507 | 0.7855 | 0.7311 | 0.5936 | 0.3492 | ANFIS-FCM | 0.7649 | 0.7649 | 0.3744 | 0.2532 | 0.8628 | 0.7879 | 0.5429 | 0.3405 | 0.7805 | 0.7287 | 0.5962 | 0.3554 | SVM-RBF | 0.7936 | 0.7912 | 0.3528 | 0.2111 | 0.8453 | 0.7668 | 0.5693 | 0.3418 | 0.7762 | 0.7225 | 0.6030 | 0.3577 | SVM-Poly | 0.6888 | 0.6772 | 0.4387 | 0.2888 | 0.8489 | 0.7824 | 0.5500 | 0.3326 | 0.7528 | 0.7053 | 0.6214 | 0.3676 | SVM-Sig | 0.0244 | −0.0790 | 290.02 | 241.69 | 0.0616 | −0.1655 | 263.96 | 225.25 | 0.0226 | −0.0104 | 298.60 | 248.78 |
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Notes. The unit of RMSE and MAE is mm day−1.
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