Abstract

Pan evapotranspiration (E) is an important physical parameter in agricultural water resources research. Many climatic factors affect E, and one of the essential challenges is to model or predict E utilizing limited climatic parameters. In this study, the performance of four different artificial neural network (ANN) algorithms i.e., multiple hidden layer back propagation (MBP), generalized regression neural network (GRNN), probabilistic neural networks (PNN), and wavelet neural network (WNN) and one empirical model namely Stephens–Stewart (SS) were employed to predict monthly E. Long-term climatic data (i.e., 1961–2013) was used for the validation of the proposed model in the Henan province of China. It was found that different models had diverse prediction accuracies in various geographical locations, MBP model outperformed other models over almost all stations (maximum R2 = 0.96), and the WNN model was the best over two sites, the accuracies of the five models ranked as MBP, WNN, GRNN, PNN, and SS. The performances of WNN and GRNN were almost the same, five-input ANN models provided better accuracy than the two-input (solar radiation (Ro) and air temperature (T)) SS empirical model (R2 = 0.80). Similarly. the two-input ANN models (maximum R2 = 0.83) also generally performed better than the two-input (Ro and T) SS empirical model. The study could reveal that the above ANN models can be used to predict E successfully in hydrological modeling over Henan Province.

Highlights

  • The transfer mechanism between liquid water and water vapor is known as evapotranspiration.The change in water vapor pressure decides the characteristics of evapotranspiration [1,2]

  • The results showed that the property of integrated artificial neural network (ANN)

  • relative humidity (RH) values of Gushi and Xin yang stations were generally greater than 72%, while RH values of San menxia stations were lower than 62%

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Summary

Introduction

The transfer mechanism between liquid water and water vapor is known as evapotranspiration. The change in water vapor pressure decides the characteristics of evapotranspiration [1,2]. In the fields of water resource information acquisition and irrigation system designing, pan evapotranspiration had become a fundamental physical variable [3]. Many climatic factors can influence the change of pan evapotranspiration including temperature, solar radiation, wind speed, and relative humidity. Few studies aimed at the quantitative influence of different climatic parameters on the changes of pan evapotranspiration in different regions [4,5,6,7,8,9]. It is necessary to accurately estimate and predict pan evapotranspiration utilizing climatic parameters in the study of hydrological modeling and water resources management

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