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Prediction Accuracy for Projectwide Evapotranspiration Using Crop Coefficients and Reference Evapotranspiration

机译:利用作物系数和参考蒸散量进行全项目蒸散量的预测精度

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摘要

The Imperial Irrigation District is a large irrigation project in the western United States having a unique hydrogeologic structure such that only small amounts of deep percolation leave the project directly as subsurface flows. This structure is conducive to relatively accurate application of a surface water balance to the district, enabling the determination of crop evapotranspiration (ETc) as a residual of inflows and outflows. The ability to calculate ETc from discharge measurements provides the opportunity to assess the accuracy and consistency of an independently applied crop coefficient—reference evapotranspiration (Kc ET0) procedure integrated over the project. The accuracy of the annual crop evapotranspiration via water balance estimates was ±6% at the 95% confidence level. Calculations using Kc and ET0 were based on the FAO-56 dual crop coefficient approach and included separate calculation of evaporation from precipitation and irrigation events. Grass reference ET0 was computed using the CIMIS Penman equation and ETc was computed for over 30 crop types. On average, Kc-based ET computations exceeded ETc determined by water balance (referred to as ETc WB) by 8% on an annual basis over a 7 year period. The 8% overprediction was concluded to stem primarily from use of Kc that represents potential and ideal growing conditions, whereas crops in the study area were not always in full pristine condition due to various water and agronomic stresses. A 6% reduction to calculated Kc-based ET was applied to all crops, and a further 2% reduction was applied to lower value crops to bring the project-wide ET predicted by Kc-based ET into agreement with ETc WB. The standard error of estimate (SEE) for annual ETc for the entire project based on Kc, following the reduction adjustment, was 3.4% of total annual ETc, which is considered to be quite good. The SEE for the average monthly ETc was 15% of average monthly ETc. A sensitivity analysis of the computational procedure for Kc showed that relaxation from using the FAO-56 dual Kc method to the more simple mean (i.e., single) Kc curve and relaxation of specificity of planting and harvest dates did not substantially increase the projectwide prediction error The use of the mean Kc curves, where effects of evaporation from wet soil are included as general averages, predicted 5% lower than the dual method for monthly estimates and 8% lower on an annual basis, so that no adjustment was required to match annual ET derived from water balance. About one half of the reduction in estimates when applying the single (or mean) Kc method rather than the dual Kc method was caused by the lack of accounting for evaporation from special irrigations during the off season (i.e., in between crops).
机译:帝国灌溉区是美国西部的大型灌溉项目,具有独特的水文地质结构,因此只有少量的深层渗滤作为地下流量直接离开项目。这种结构有利于相对准确地将地表水平衡应用于该地区,从而能够确定作为流入和流出残留物的作物蒸散量(ETc)。根据排放量测量值计算ETc的能力为评估独立应用的作物系数(参考蒸散量(Kc ET0))程序的准确性和一致性提供了机会。在95%的置信水平下,通过水平衡估算得出的年度作物蒸散量的准确性为±6%。使用Kc和ET0进行的计算是基于FAO-56双重作物系数法,包括对降水和灌溉事件中蒸发量的单独计算。使用CIMIS Penman方程计算草参考值ET0,并针对30多种作物类型计算ETc。平均而言,在7年中,基于Kc的ET计算量每年超过由水平衡确定的ETc(称为ETc WB)8%。得出8%的高估主要是由于使用了代表潜在和理想生长条件的Kc,而研究区的作物由于各种水分和农艺胁迫而并非总是处于原始状态。将计算出的基于Kc的ET的所有作物减少6%,并将其他2%的低价作物减少2%,以使基于Kc的ET预测的整个项目范围的ET与ETc WB达成一致。减少调整后,基于Kc的整个项目的年度ETc的标准估计误差(SEE)为年度ETc的3.4%,被认为是相当不错的。平均每月ETc的SEE为平均每月ETc的15%。 Kc计算程序的敏感性分析表明,从使用FAO-56双重Kc方法放宽到更简单的均值(即单一)Kc曲线以及放宽播种和收获日期的特异性并没有显着增加整个项目范围的预测误差使用平均Kc曲线(其中将来自湿土的蒸发的影响包括在内作为一般平均值),对于每月估算而言,预测值比对偶方法低5%,而在年度基础上则低8%,因此无需进行调整以匹配年度平均值。 ET来自水平衡。采用单次(或均值)Kc方法而不是双重Kc方法时,估计值减少的一半左右是由于在淡季(即农作物之间)缺少特殊灌溉的蒸发造成的。

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