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Estimating Riparian and Agricultural Actual Evapotranspiration by Reference Evapotranspiration and MODIS Enhanced Vegetation Index

机译:通过参考蒸散量和MODIS增强植被指数估算河岸和农业实际蒸散量

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Dryland river basins frequently support both irrigated agriculture and riparian vegetation and remote sensing methods are needed to monitor water use by both crops and natural vegetation in irrigation districts. We developed an algorithm for estimating actual evapotranspiration (ETa) based on the Enhanced Vegetation Index (EVI) from the Moderate Resolution Imaging Spectrometer (MODIS) sensor on the EOS-1 Terra satellite and locally-derived measurements of reference crop ET (ETo). The algorithm was calibrated with five years of ETa data from three eddy covariance flux towers set in riparian plant associations on the upper San Pedro River, Arizona, supplemented with ETa data for alfalfa and cotton from the literature. The algorithm was based on an equation of the form ETa = ETo [a(1 − e−bEVI) − c], where the term (1 − e−bEVI) is derived from the Beer-Lambert Law to express light absorption by a canopy, with EVI replacing leaf area index as an estimate of the density of light-absorbing units. The resulting algorithm capably predicted ETa across riparian plants and crops (r2 = 0.73). It was then tested against water balance data for five irrigation districts and flux tower data for two riparian zones for which season-long or multi-year ETa data were available. Predictions were within 10% of measured results in each case, with a non-significant (P = 0.89) difference between mean measured and modeled ETa of 5.4% over all validation sites. Validation and calibration data sets were combined to present a final predictive equation for application across crops and riparian plant associations for monitoring individual irrigation districts or for conducting global water use assessments of mixed agricultural and riparian biomes.
机译:旱地流域经常支持灌溉农业和河岸植被,并且需要遥感方法来监测灌溉区的作物和自然植被的用水情况。我们基于EOS-1 Terra卫星上的中等分辨率成像光谱仪(MODIS)传感器的增强植被指数(EVI)和本地衍生的测量结果,开发了一种估算实际蒸散量(ET a )的算法参考作物ET(ET o )的数量。该算法使用来自亚利桑那州上圣佩德罗河上游河岸植物协会中的三个涡流协方差通量塔的五年ET a 数据进行了校准,并补充了ET a 数据文献中用于苜蓿和棉花。该算法基于形式为ET a = ET o [a(1- e -bEVI )-c]的方程,其中术语(1- e -bEVI )是根据比尔-朗伯定律推导出来表示冠层的光吸收,其中EVI代替叶面积指数来估计光吸收单元的密度。所得算法能够在河岸植物和农作物上预测ET a (r 2 = 0.73)。然后针对五个灌溉区的水平衡数据和两个河岸带的通量塔数据对它们进行了测试,这些河岸带具有整个季节或多年的ET a 数据。在每种情况下,预测值均在测量结果的10%以内,在所有验证位点上,平均测量值和建模ET a 之间的均无显着差异(P = 0.89)。结合了验证和校准数据集,以提供一个最终的预测方程式,可应用于各种作物和河岸植物协会,以监测单个灌溉区或对农业和河岸生物群落混合进行全球用水评估。

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