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首页> 外文期刊>Earth System Science Data Discussions >High-resolution global grids of revised Priestley–Taylor and Hargreaves–Samani coefficients for assessing ASCE-standardized reference crop evapotranspiration and solar radiation
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High-resolution global grids of revised Priestley–Taylor and Hargreaves–Samani coefficients for assessing ASCE-standardized reference crop evapotranspiration and solar radiation

机译:修订的Priestley-Taylor和Hargreaves-Samani系数的高分辨率全球网格,用于评估ASCE标准化参考作物的蒸散量和太阳辐射

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The objective of the study is to provide global grids (0.5°) of revised annual coefficients for the Priestley–Taylor (P-T) and Hargreaves–Samani (H-S) evapotranspiration methods after calibration based on the ASCE (American Society of Civil Engineers)-standardized Penman–Monteith method (the ASCE method includes two reference crops: short-clipped grass and tall alfalfa). The analysis also includes the development of a global grid of revised annual coefficients for solar radiation (Rs) estimations using the respective Rs formula of H-S. The analysis was based on global gridded climatic data of the period 1950–2000. The method for deriving annual coefficients of the P-T and H-S methods was based on partial weighted averages (PWAs) of their mean monthly values. This method estimates the annual values considering the amplitude of the parameter under investigation (ETo and Rs) giving more weight to the monthly coefficients of the months with higher ETo values (or Rs values for the case of the H-S radiation formula). The method also eliminates the effect of unreasonably high or low monthly coefficients that may occur during periods where ETo and Rs fall below a specific threshold. The new coefficients were validated based on data from 140 stations located in various climatic zones of the USA and Australia with expanded observations up to 2016. The validation procedure for ETo estimations of the short reference crop showed that the P-T and H-S methods with the new revised coefficients outperformed the standard methods reducing the estimated root mean square error (RMSE) in ETo values by 40 and 25?%, respectively. The estimations of Rs using the H-S formula with revised coefficients reduced the RMSE by 28?% in comparison to the standard H-S formula. Finally, a raster database was built consisting of (a)?global maps for the mean monthly ETo values estimated by ASCE-standardized method for both reference crops, (b)?global maps for the revised annual coefficients of the P-T and H-S evapotranspiration methods for both reference crops and a global map for the revised annual coefficient of the H-S radiation formula and (c)?global maps that indicate the optimum locations for using the standard P-T and H-S methods and their possible annual errors based on reference values. The database can support estimations of ETo and solar radiation for locations where climatic data are limited and it can support studies which require such estimations on larger scales (e.g. country, continent, world). The datasets produced in this study are archived in the PANGAEA database (https://doi.org/10.1594/PANGAEA.868808) and in the ESRN database (http://www.esrn-database.org or http://esrn-database.weebly.com).
机译:该研究的目的是根据ASCE(美国土木工程师学会)标准化后的校准结果,为Priestley-Taylor(PT)和Hargreaves-Samani(HS)蒸散方法提供经修订的年度系数的全球网格(0.5°) Penman–Monteith方法(ASCE方法包括两种参考作物:短剪草和高苜蓿)。该分析还包括使用H-S的各个Rs公式开发一个修订后的年度年度太阳辐射(Rs)估计系数的全球网格。该分析基于1950-2000年期间的全球栅格气候数据。 P-T和H-S方法的年度系数的推导方法是基于它们的平均月度值的偏加权平均值(PWA)。该方法考虑被调查参数的振幅(ETo和Rs)来估算年值,从而给具有较高ETo值(或H-S辐射公式的Rs值)的月份的月度系数赋予更多权重。该方法还消除了在ETo和Rs降至特定阈值以下期间可能出现的不合理的月度系数过高或过低的影响。基于来自美国和澳大利亚不同气候区的140个站点​​的数据对新系数进行了验证,并扩展了至2016年的观测值。对短期参考作物的ETo估算的验证程序表明,采用新修订的PT和HS方法系数优于标准方法,可将ETo值的估计均方根误差(RMSE)分别降低40%和25%。与标准的H-S公式相比,使用具有修正系数的H-S公式对Rs的估算将RMSE降低了28%。最后,建立了一个栅格数据库,其中包括:(a)通过两种参考作物的ASCE标准化方法估算的月平均ETo值的全球地图,(b)PT和HS蒸散方法的修订年度系数的全球地图。参考作物和HS辐射公式的修订年度系数的全球地图以及(c)?全球地图,这些地图指示使用标准PT和HS方法的最佳位置以及基于参考值的可能年度误差。该数据库可以支持对气候数据有限的位置的ETo和太阳辐射的估算,并且可以支持需要在较大规模(例如国家,大陆,世界)进行估算的研究。本研究产生的数据集存储在PANGEA数据库(https://doi.org/10.1594/PANGAEA.868808)和ESRN数据库(http://www.esrn-database.org或http:// esrn中) -database.weebly.com)。

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