MENG Qiang, LIU Jing-xia, LI Yu-qing, ZHANG Wen-xian
Water Saving Irrigation. 2020, (6):
61-67.
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In order to clarify the applicability of the calculation model for reference crop evapotranspiration (ET0) in the irrigation district of Tibet Plateau and to recommend the calculation model suitable for meteorological data shortage condition, in this study, based on the long series data of meteorological stations in Manla, Moda and Jiangbei irrigation district, the Penman-Monteith (FAO 56 PM) model recommended by FAO was used as the standard to evaluate the applicability of five commonly used models. The results showed that the variation trends of daily scale ET0 calculated by Makkink, Irmark-Allen, FAO 17 Penman, Hargreaves-Samani and Priestley-Taylor models was all consistent with that of the FAO 56 PM model, and the annual variation pattern of ET0 increased and then decreased, and the peak value appeared from June to July, but the applicability of each model was significantly different. The daily MAE, RMSE, and NSE values of Makkink model were 0.37 mm/d, 0.45 mm/d and 0.84, respectively, with the highest simulation accuracy and reliability. Followed was the Irmark-Allen model with the MAE, RMSE, NSE values of 0.65 mm/d, 0.71 mm/d and 0.62 respectively. The Priestley-Taylor model had the poorest performance, with the MAE value up to 4.91 mm/d and the NSE value less than 0. On the annual scale, the calculation results of each model were overestimated at different degrees, compared with FAO 56 PM model. The NSE values of FAO 17 Penman, Hargreaves-Samani, and Priestley-Taylor models were between -3 571.76 and -118.00, and the simulation results were not credible. The NSE value of Makkink model was the closest to 0, the simulation result was credible, but the error in the simulation process was large. Based on the comprehensive evaluation, the Makkink model was recommended as a simplified model of ET0 under the meteorological data shortage condition in the irrigation district of Tibetan Plateau.