Research Article
Modeling Evapotranspiration Response to Climatic Forcings Using Data-Driven Techniques in Grassland Ecosystems
Table 3
Comparisons of data-driven model performances for evapotranspiration among the training, validation and prediction periods at AT-Neu site.
| Model | Training | Validation | Prediction | | NSE | RMSE | MAE | | NSE | RMSE | MAE | | NSE | RMSE | MAE |
| ANN | 0.9298 | 0.9294 | 0.3551 | 0.2321 | 0.9407 | 0.9375 | 0.3318 | 0.2203 | 0.9355 | 0.9338 | 0.3350 | 0.2278 | GRNN | 0.9596 | 0.9595 | 0.2689 | 0.1635 | 0.9134 | 0.9118 | 0.3943 | 0.2640 | 0.9207 | 0.9186 | 0.3714 | 0.2473 | GMDH | 0.9271 | 0.9270 | 0.3610 | 0.2442 | 0.9246 | 0.9220 | 0.3707 | 0.2464 | 0.9356 | 0.9320 | 0.3394 | 0.2342 | ELM-Sig | 0.9256 | 0.9256 | 0.3644 | 0.2430 | 0.9265 | 0.9249 | 0.3639 | 0.2461 | 0.9355 | 0.9328 | 0.3376 | 0.2322 | ELM-Sin | 0.9278 | 0.9278 | 0.3591 | 0.2332 | 0.9302 | 0.9283 | 0.3554 | 0.2415 | 0.9365 | 0.9344 | 0.3335 | 0.2242 | ELM-Hard | 0.8762 | 0.8762 | 0.4702 | 0.3365 | 0.8814 | 0.8811 | 0.4577 | 0.3394 | 0.9043 | 0.9031 | 0.4053 | 0.2836 | ANFIS-Grid | 0.9407 | 0.9407 | 0.3255 | 0.2121 | 0.9237 | 0.9230 | 0.3684 | 0.2585 | 0.9247 | 0.9219 | 0.3639 | 0.2436 | ANFIS-SC | 0.9373 | 0.9373 | 0.3347 | 0.2138 | 0.9318 | 0.9304 | 0.3503 | 0.2402 | 0.9379 | 0.9355 | 0.3308 | 0.2260 | ANFIS-FCM | 0.9376 | 0.9376 | 0.3338 | 0.2151 | 0.9380 | 0.9358 | 0.3363 | 0.2314 | 0.9369 | 0.9343 | 0.3338 | 0.2282 | SVM-RBF | 0.9387 | 0.9373 | 0.3347 | 0.1928 | 0.9333 | 0.9328 | 0.3440 | 0.2357 | 0.9338 | 0.9321 | 0.3392 | 0.2286 | SVM-Poly | 0.8357 | 0.8321 | 0.5476 | 0.4007 | 0.8351 | 0.8341 | 0.5406 | 0.4287 | 0.8746 | 0.8696 | 0.4701 | 0.3579 | SVM-Sig | 0.5948 | 0.5061 | 0.9391 | 0.7203 | 0.5113 | 0.4352 | 0.9976 | 0.7997 | 0.5910 | 0.5063 | 0.9149 | 0.7275 |
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Note. The units of RMSE and MAE are mm dayā1.
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