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Calibration of the Hargreaves-Samani method for the calculation of reference evapotranspiration in different Koeppen climate classes

机译:Hargreaves-Samani方法的校准,用于计算不同科普彭气候类别中的参考蒸散量

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摘要

The Penman-Monteith equation (FAO-56) is accepted as the standard model for estimating reference evapotranspiration (ETo). However, the major obstacle to using FAO-56 widely is that it requires numerous climatic data. The Hargreaves-Samani (HS) method is frequently used for the calculation of ETo since it is based on measurements of daily minimum and maximum air temperature alone. Those are commonly recorded at many meteorological stations throughout the world. It is the objective of this paper to evaluate the quality of HS and calibrate the coefficients of this method for different climates as represented by the Koeppen classification. Estimated values are compared with Penman-Monteith ETo values in terms of the coefficient of efficiency C_(eff) as well as the root mean square error, the mean absolute error and the Bayes information criterion. The Penman-Monteith equation for ETo (FAO-56) is based on physics and known to provide best estimates of ETo. The results of our work show that the correlation between long-term monthly means of HS and FAO-56 can be improved significantly by introducing climate-class specific coefficients.
机译:Penman-Monteith方程(FAO-56)被接受为估算参考蒸散量(ETo)的标准模型。但是,广泛使用FAO-56的主要障碍是需要大量的气候数据。 Hargreaves-Samani(HS)方法经常用于计算ETo,因为它仅基于每日最低和最高气温的测量。这些通常记录在世界各地的许多气象站。本文的目的是评估Koeppen分类所代表的HS的质量,并针对不同的气候校准该方法的系数。根据效率系数C_(eff)以及均方根误差,平均绝对误差和贝叶斯信息准则,将估计值与Penman-Monteith ETo值进行比较。 ETo的Penman-Monteith方程(FAO-56)基于物理学,已知能够提供ETo的最佳估计。我们的工作结果表明,通过引入气候类别特定系数,可以大大改善HS长期每月平均值与FAO-56之间的相关性。

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