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A comparative study of remote sensing and gene expression programming for estimation of evapotranspiration in four distinctive climates

机译:四个独特气候探测蒸发蒸散雷遥感和基因表达规划的比较研究

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摘要

An accurate estimation of Evapotranspiration (ET) is an important issue in hydrology, water resources management and irrigation scheduling. There are a wide range of methods for estimation of ET, among which, machine learning techniques and remote sensing-based approaches demonstrated more reasonable results. Accordingly, this study attempts to compare the capability of two developed models of Gene-Expression Programming (GEP) and Surface Energy Balance Algorithm for Land (SEBAL) in estimation of ET, at four different climate types of Temperate-Warm (T-W), Wet-Warm (W-W), Arid-Cold (A-C), and Arid-Warm (A-W). In this way, a-two year of daily records as weather variables (i.e., maximum and minimum temperature, dew-point temperature, vapor pressure, saturated vapor pressure, relative humidity, 24-h rainfall, sunshine hours, and wind speed) were considered as input variables, whereas ET values were computed as output variable (observed ET) by using FAO Penman-Monteith-56 method. After development of two predictive models, the statistical results were compared with well-known Hargreaves-Samani method. The results showed that while Hargreaves-Samani equation could not yield remarkable results in any of the climates, GEP and SEBAL demonstrated accurate predictions. In this way, GEP was the superior model in T-W (R-2 = 0.902 and RMSE = 0.713 mm/day) and A-W (R-2 = 0.951 and RMSE = 0.634 mm/day) climates but it dropped a bit in two other climates. However, SEBAL not only had the best performance in both climates of W-W (R-2 = 0.967 and RMSE = 0.515 mm/day) and A-C (R-2 = 0.990 and RMSE = 0.720 mm/day), but also demonstrated good predictions in T-W and A-W climates. Therefore, SEBAL is recommended as the best model for estimation of ET in all climate types.
机译:准确估计蒸散蒸腾(et)是水文,水资源管理和灌溉调度的重要问题。估计ET有很多方法,其中,机器学习技术和基于遥感的方法表现出更合理的结果。因此,该研究试图比较两种类型的基因表达编程(GEP)和地表能量平衡算法的能力和地面能量平衡算法在估计ET的估计中,以四种不同的气候温度(TW),湿润-WARM(WW),干旱的(AC),和温暖(AW)。通过这种方式,每日记录为天气变量(即最大和最小温度,露点温度,蒸气压,饱和蒸气压,相对湿度,24-H降雨,阳光小时和风速)是被视为输入变量,通过使用FAO Penman-Monteith-56方法计算ET值作为输出变量(观察到的ET)。在发展两种预测模型后,将统计结果与众所周知的Hargreaves-Samani方法进行比较。结果表明,虽然Hargreaves-Samani方程在任何气候,GEP和SEBAL中都不能产生显着的结果,但是展示了准确的预测。通过这种方式,GEP是TW(R-2 = 0.902和RMSE = 0.713 mm /天)的上级模型,AW(R-2 = 0.951和RMSE = 0.634毫米/天)气候,但它在另外两位掉了一下气候。然而,Sebal不仅具有WW的两个气候(R-2 = 0.967和RMSE = 0.515毫米/天)的最佳性能和AC(R-2 = 0.990和RMSE = 0.720 mm /天),还表现出良好的预测在tw和aw气候中。因此,Sebal建议作为在所有气候类型中估算ET的最佳模型。

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