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Comparison of Remote Sensing-Based Energy Balance Methods for Estimating Crop Evapotranspiration

机译:基于遥感的能量平​​衡法估算作物蒸散量的比较

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Remote sensing of evapotranspiration has become more common during the last decade. Two of the approaches being used are the reflectance-based crop coefficient method and the energy balance method. In the energy balance approach, surface temperature is used to calculate sensible heat flux and long wave radiation and depending on the complexity of the model, different methods are used to handle the aerodynamic temperature term. This paper compares two energy balance approaches with different methodology for estimating sensible heat flux (H): (ⅰ) one layer energy balance model and (ⅱ) two-layer energy balance model called the Two Source Model. The results from the two approaches are compared using a set of comprehensive field and remote sensing measurements of model input data and actual evapotranspiration measured with a dense network of eddy covariance stations during the SMACEX campaign in central Iowa during the 2002 growing season. Results show that both methods of estimating H perform well using calibrated Landsat Thematic Mapper imagery as remotely sensed inputs.
机译:在过去十年中,对蒸散的遥感越来越普遍。使用的两种方法是基于反射率的作物系数方法和能量平衡方法。在能量平衡方法中,表面温度用于计算显热通量和长波辐射,并且根据模型的复杂性,使用不同的方法来处理空气动力学温度项。本文比较了两种用不同方法估算显热通量(H)的能量平衡方法:(ⅰ)一层能量平衡模型和(ⅱ)两层能量平衡模型,称为两源模型。使用2002年生长季节在爱荷华州中部的SMACEX活动期间,通过对模型输入数据进行全面的现场和遥感测量以及使用密集的涡动协方差站网测量的实际蒸散量,比较了这两种方法的结果。结果表明,使用校准的Landsat Thematic Mapper影像作为遥感输入,两种估算H的方法都表现良好。

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