Detailed meteorological data required for the equation of FAO-56 Penman-Monteith (P-M) method that was adopted by Food and Agriculture Organization (FAO) as a standard method in estimating reference evapotranspiration (ET o ) are not often available, especially in developing countries. The Hargreaves equation (HG) has been successfully used in some locations to estimate ET o where sufficient data were not available to use the P-M method. This paper investigates the potential of two Artificial Neural Network (ANN) architectures, the multilayer perceptron architecture, in which a backpropagation algorithm (BPANN) is used, and the cascade correlation architecture (CCANN), in which Kalman's learning rule is embedded in modeling the daily ET o with minimal meteorological data. An overview of the features of ANNs and traditional methods such as P-M and HG is presented, and the advantages and limitations of each method are discussed. Daily meteorological data from three automatic weather stations located in Greece were used to optimize and test the different models. The exponent value of the HG equation was locally optimized, and an adjusted HGadj equation was used. The comparisons were based on error statistical techniques using P-M daily ET o values as reference. According to the results obtained, it was found that taking into account only the mean, maximum and minimum air temperatures, the selected ANN models markedly improved the daily ET o estimates and provided unbiased predictions and systematically better accuracy compared with the HGadj equation. The results also show that the CCANN model performed better than the BPANN model at all stations.
KEYWORDS: neural network techniques, evapotranspiration, calibration, validation.
INTRODUCTIONKnowledge of evapotranspiration, which involves the evaporation of water from land surfaces and transpiration by vegetation, is essential for estimating irrigation water requirements (Allen et al., 1998). Methods for estimating evapotranspiration are based on micrometeorological techniques (aerodynamic method, eddy covariance, etc.) or on the use of lysimeters. The methods for estimating evapotranspiration require complex and very costly instruments and are generally recommended only for specific research purposes (Allen et al., 1998). The evapotranspiration rate from a reference crop is called reference evapotranspiration (ET o ) and expresses the evaporating power of the atmosphere at a specific location and time of the year (Allen et al., 1998). The FAO-56 Penman-Monteith (P-M) equation (Allen et al., 1998) was adopted by FAO as a standard method for estimating daily ET o , as it provides more consistent ET o estimates and has been shown to perform better than other ET o methods. However, the detailed meteorological data required by the P-M equation are not often available, especially in developing countries. Under such conditions, simplified or empirical equations, which require less meteorological data, should be used. Allen et al. (1998) have proposed that when s...