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Crop RS-Met: A biophysical evapotranspiration and root-zone soil water content model for crops based on proximal sensing and meteorological data

机译:作物RS-MET:基于近端感测和气象数据的作物生物物理蒸发和根区土壤水分含量模型

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摘要

Assessing crops water use is essential for agricultural water management and planning, particularly in water-limited regions. Here, we present a biophysical model to estimate crop actual evapotranspiration and root-zone soil water content using proximal sensing and meteorological data (Crop RS-Met). The model, which is based on the dual FAO56 formulation, uses a water deficit factor calculated from rainfall and atmospheric demand information to constrain actual evapotranspiration and soil water content in crops growing under dry conditions. We tested the Crop RS-Met model in a dryland experimental field comprising a variety of wheat (Tridcum aestivum L. and T. durum) cultivars with diverse phenology. Crop RS-Met was shown to accurately capture seasonal changes in wheat water use during the growing season. The average R-2 of modeled vs. observed soil water content for all cultivars (N = 11) was 0.92 0.02 with average relative RMSE and bias of 9.29 1.30% and 0.13 0.03%, respectively. We found that changing the integration time period of the water deficit factor in Crop RS-Met affects the accuracy of the model implying that this factor has a vital role in modeling crop water use under dry conditions. Currently, Crop RS-Met has a simple representation of surface runoff and does not take into consideration heterogeneity in the soil profile. Thus, efforts to combine numerical models that simulate soil water dynamics with a Crop RS-Met model driven by high-resolution remote sensing data may be needed for a spatially continuous assessment of crop water use in fields with more complex edaphic characteristics.
机译:评估作物用水对于农业水管理和规划至关重要,特别是在有限地区。在这里,我们介绍了一种使用近端感测和气象数据(作物RS-Met)估计作物实际蒸发和根区土壤水分的生物物理模型。该模型基于双FAO56配方,采用从降雨和大气需求信息计算的水赤字因子,以限制在干燥条件下生长的作物中的实际蒸发和土壤含水量。我们在旱地实验领域中测试了包含各种小麦(Tridcum Aestivum L.和T.Durum)品种具有多种候选的多种小麦的作物RS-Met模型。作物RS-MET显示在生长季节期间,准确地捕获麦子用水的季节变化。为所有品种(n = 11)的平均r-2与观察到的土壤含水量(n = 11)为0.92 0.02,平均相对RMSE和偏差分别为9.29 1.30%和0.13 0.03%。我们发现改变作物RS-MET中的水赤字因子的集成时间段影响模型的准确性,这意味着该因素在在干燥条件下对作物用水建模至关重要的作用。目前,作物RS-MET具有简单的表面径流表示,并且在土壤轮廓中没有考虑异质性。因此,可以努力将模拟土壤水动态的数值模型与由高分辨率遥感数据驱动的作物RS-MET模型相结合,以便在具有更复杂的副本特性的场上的作物用水的空间连续评估。

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