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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方法的比较估算作物蒸散量

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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,遥感蒸散变得更加普遍。所使用的两种方法是基于反射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,并取决于模型的复杂性,使用不同的方法来处理空气动力学期限。本文将两个能量平衡方法与不同方法进行比较,用于估计可显热通量(H):(i)一层能量平衡模型和(ii)称为两个源模型的双层能量平衡模型。使用一组综合现场和遥感测量的模型输入数据和遥感测量的模型输入数据和实际蒸散测量的结果,并在2002年生长季节的SMACEX广告系列期间与涡旋协方识的密集网络测量。结果表明,两种估算H的方法都使用校准的Landsat主题映射器图像作为远程感测的输入进行良好。

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