Short-term daily reference evapotranspiration forecasting using temperature-based deep learning models in different climate zones in China

被引:12
作者
Zhang, Lei [1 ]
Zhao, Xin [1 ]
Zhu, Ge [2 ]
He, Jun [3 ]
Chen, Jian [1 ]
Chen, Zhicheng [4 ]
Traore, Seydou [5 ,6 ]
Liu, Junguo [1 ]
Singh, Vijay P. [5 ,7 ]
机构
[1] North China Univ Water Resources & Elect Power, Sch Water Conservat, Zhengzhou 450045, Henan, Peoples R China
[2] North China Univ Water Resources & Elect Power, Sch Informat Engn, Zhengzhou 450045, Henan, Peoples R China
[3] China Three Gorges Univ, Coll Hydraul & Environm Engn, Yichang 443002, Hubei, Peoples R China
[4] Training Ctr Zhejiang Commun Investment Grp Co Ltd, Hangzhou 310005, Zhejiang, Peoples R China
[5] Texas A&M Univ, Dept Biol & Agr Engn, Zachry Dept Civil & Environm Engn, College Stn, TX 77843 USA
[6] Metropolitan Solar Inc, Washington, DC 20032 USA
[7] UAE Univ, Natl Water & Energy Ctr, Al Ain, U Arab Emirates
基金
中国国家自然科学基金;
关键词
Deep learning; Reference evapotranspiration forecast; Temperature forecasts; Climate zones; China; ARTIFICIAL NEURAL-NETWORK; HARGREAVES-SAMANI MODEL; PENMAN-MONTEITH MODEL; CROP EVAPOTRANSPIRATION; VALIDATION;
D O I
10.1016/j.agwat.2023.108498
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
The reference evapotranspiration (ETo) pertains to the evapotranspiration of cold-season grasses with an approximate height of 0.12 m or full-covered alfalfa with a height of 0.50 m. Accurate short-term ETo forecasts are indispensable for informed irrigation decisions by relevant departments and individuals. Four deep learning (DL) models, including Long Short-Term Memory (LSTM), Gated Recurrent Unit (GRU), Bidirectional LSTM (BiLSTM), and Bidirectional GRU (Bi-GRU), as well as two calibrated empirical models (Hargreaves-Samani (HS) and reduced-set Penman-Monteith (RPM)), were used to evaluate the performance of the ETo forecast with a lead time of 1-7 d using temperature forecasts in different climates. The results reveal that the DL models and calibrated HS and RPM models exhibited comparable trends in the ETo forecasts for lead times of 1-7 d. Nonetheless, the DL models consistently outperformed the HS and RPM models across the diverse climatic regions in China. The DL models displayed an average root mean square error (RMSE) and mean absolute error (MAE) of less than 0.887 and 0.633 mm/d, respectively. Moreover, the mean correlation coefficient (R) and accuracy (ACC) exceeded 0.807% and 89.701%, respectively. Among the DL models, the LSTM model demonstrated slightly superior performance in short-term daily ETo forecasts in diverse climates. The LSTM model exhibited RMSE and MAE ranges of 0.563-0.875 mm/d and 0.418-0.626 mm/d, respectively, along with R and ACC ranges of 0.81-0.90 and 89.94-98.11%, respectively. Furthermore, even with an increase in lead time, the DL models continued to exhibit strong predictive capabilities, consistently surpassing the performance of the HS and RPM models. Overall, the trained DL models presented an exceptional ability to forecast the short-term daily ETo in various climatic regions of China. These models require only a few input variables and readily available data, making them highly advantageous for practical applications in ETo forecasting. Such models hold promise for significantly enhancing regional agricultural water-resource planning and management.
引用
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页数:19
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