Table 6.
Location | Model | Input Parameters | Output Parameter | Data Scale | Statistical Benchmarks | Key Findings | References |
---|---|---|---|---|---|---|---|
China | ANN, and Empirical regression models (Model 1, Model 2) | Sunshine percentage, and clearness index | Monthly mean daily diffuse solar radiation | 1995 to 2004 | RMSE, MPE, and MBE | ANN is superior to empirical models. ANN estimated the actual values of Zhengzhou with 94.81% accuracy. | [113] |
Türkiye (73 different locations) | ANN and MLR | Months of the year, latitude satellite-estimated LST, longitude, and altitude | Solar radiation forecasting | 2000 to 2002 | R2, RMSE, and MBE | ANN achieved high accuracy compared to MLR. | [114] |
Iran | Five empirical models, WR, GEP, and ANN | Daylight hours, extraterrestrial global solar radiation, daily mean clearness index, and daily temperature | Daily global solar radiation | 1982 to 2016 | GPI, MAE, RMSRE, MBE, RMSE, RRMSE, U95, MARE, R2, erMAX, and t-stat, | The statistical metric results gave that the best prediction performance was exhibited by the ANN method. | [115] |
Paris, France | ARMA, SIM, SVM, and NN | Global solar radiation | Hourly solar radiation | January 1, 2004, to December 31, 2015 | nRMSE | NN model gave better performance than other models. | [116] |
Kerman, Iran | 3rd degree empirical model, ANN, SVM–RBF, SVM–WT | Daily clearness index | Diffuse solar radiation | 2006 to 2012 | r, RMSE, and MABE | The SVM–WT method has better estimation accuracy than its competitors with 0.9631 of r, 0.6940 MJ/m2 of RMSE, and 0.5757 MJ/m2 of MABE. | [117] |
Tamil Nadu (India) | SVM, ANN, and empirical models | Relative humidity, longitude, day length, month, latitude, maximum and minimum temperature, and bright sunshine hours | Monthly mean daily global solar radiation | 2003 to 2012 | MBE, MAPE, RMSE, t-stat, and r-value | SVM algorithms gave better results than both those of ANN and empirical models. | [118] |
Iran | Empirical models, ordinary and coupled ANN models | Sunshine duration, minimum and maximum air temperatures, and daily global solar radiation | Daily global solar radiation | 1992 to 2015 | R2, RMSE, and MBE | The prediction performance of the ordinary ANN models was enhanced considerably after being coupled with a genetic algorithm. | [119] |
Abu Musa Island, Iran | SVR, MLFFNN, FIS RBFNN, and ANFIS | Inputs (N1): Wind speed, temperature, relative humidity, pressure, and local time Input (N2): Solar radiation |
Hourly solar radiation | 2010 to 2016 | r, RMSE, and MSE | The results of N1 give that, MLFFNN and SVR methods exhibited the best prediction performance with r = 0.9999 and 0.9795, respectively. Furthermore, ANFIS, MLFFNN, and SVR methods obtained a correlation coefficient of over 0.95 in the test data for N2. | [75] |
Four climatic zones of China | 12 ML models, and 12 versions of the Ångström–Prescott model | Daily historical data | Daily global solar radiation | 1966 to 2015 | R2, RMSE, U95 MBE, t-stat, and NRMSE | Each prediction method used the same dataset and ML methods gave lower error values than empirical models. Among the ML methods, four models come to the fore: ANFIS, ELM, LSSVM, and MARS. | [120] |
Four provinces (Şırnak, Kilis Ankara, and Karaman) in Türkiye | Angstrom type-empirical models, RSM, Holt-Winters, and ANN | Wind speed, pressure, relative humidity, ambient temperature, and sunshine duration | Monthly average daily global solar radiation | 2008 to 2018 | MAPE, RMSE, MBE, t-stat, and R2 | Each model used the same dataset, and ANN exhibited the best results for global solar radiation data with R2, MAPE, RMSE, MBE, and t-stat of 0.9911, 4.93%, 0.78 MJ/m2, 0.1323 MJ/m2, and 0.58, respectively. | [112] |
Five locations, Morocco | 22 empirical models, RF, MLP, Boost, and Bag | Relative humidity, ambient temperature, wind speed, and solar radiation | Daily global solar radiation | 2011 to 2015 | r, nMAE, and nRMSE | RF method gave the best performance. r, nMAE and nRMSE are 81.73–95.14%, 5.88–13.86%, and 8.22–18%, respectively. Among the empirical models, the TG1 model was recommended. r, nMAE and nRMSE are 72.38–93.46%, 6.96–17.94%, and 9.89–22.39%, respectively. | [41] |
Alabama, United States | KNNR, ANN, SVM, and BILSTM | Global solar radiation | Hourly solar radiation | May 1, 2011, to February 18, 2013 | RMSE, MAE, and R2 |
The BILSTM model outperformed KNNR, ANN, and SVR methods in terms of RMSE, MAE, and R2 evaluation benchmarks. | [121] |
North Carolina, and Southern Spain | MLP, ELM, GRNN, SVM, RF, and XGBoost | Temperature-based variables | Daily extraterrestrial solar radiation | 2000 to 2018 | MBE, RMSE, RRMSE, NSE, R2, and GPI | MLP and SVM are recommended for arid and semi-arid areas, while RF and XGBOOST are recommended for semi-humid and humid areas. | [122] |
Tetouan in Morocco | ARIMA, FFNN, and k-NN | Top of atmosphere radiation, clearness index, maximum, average, delta, and ratio temperature | Daily global solar radiation | January 1, 2013, to December 31, 2015 | MAPE, RMSE, MBE, NRMSE, Ts and σ | FFNN (6 × 10 × 1) gave better results than those of time series, and k-NN model with very low error magnitudes. | [123] |