首页> 外文期刊>Remote Sensing >Consistency between In Situ, Model-Derived and High-Resolution-Image-Based Soil Temperature Endmembers: Towards a Robust Data-Based Model for Multi-Resolution Monitoring of Crop Evapotranspiration
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Consistency between In Situ, Model-Derived and High-Resolution-Image-Based Soil Temperature Endmembers: Towards a Robust Data-Based Model for Multi-Resolution Monitoring of Crop Evapotranspiration

机译:基于原位,模型导出和基于高分辨率图像的土壤温度最终成员之间的一致性:建立基于数据的稳健模型,用于作物蒸发蒸腾的多分辨率监测

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Due to their image-based nature, “contextual” approaches are very attractive to estimate evapotranspiration (ET) from remotely-sensed land surface temperature (LST) data. Their application is however limited to highly heterogeneous areas where the soil and vegetation temperature endmembers (Tends) can be observed at the thermal sensor resolution. This paper aims to develop a simple theoretical approach to estimate Tends independently from LST images. Soil Tends are simulated by a soil energy balance model forced by meteorological data. Vegetation Tends are obtained from soil Tends and air temperature. Model-derived soil Tends are first evaluated with in situ measurements made over an irrigated area in Morocco. The root mean square difference (RMSD) between modeled and ground-based soil Tends is estimated as 2.4 ∘ C. Model-derived soil Tends are next compared with the soil Tends retrieved from 90-m resolution ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) data collected over two irrigated areas in Mexico and Spain. Such a comparison reveals a strong consistency between model-derived and high-resolution image-based soil Tends. A recent contextual ET model (SEB-1S) is then applied to 90-m resolution and to 1-km resolution (aggregated) ASTER data using the model-derived or image-based Tends as the input. The RMSD between 90-m resolution SEB-1S and in situ ET is estimated as 65 and 82 W·m - 2 , and the RMSD between 1-km resolution SEB-1S and aggregated SEB-1S ET is estimated as 78 and 56 W·m - 2 for the image-based and model-derived Tends, respectively. In light of the above results, Tends should be estimated a priori when contextual models are applied to low resolution images. Moreover, the consistency over highly heterogeneous areas between model-derived and high-resolution image-based Tends provides a meaningful basis for developing mixed modeling observational approaches.
机译:由于其基于图像的性质,“上下文”方法对于根据遥感地表温度(LST)数据估算蒸散量(ET)非常有吸引力。但是,它们的应用仅限于高度异质性的区域,在该区域中,可以在热传感器分辨率下观察到土壤和植被温度末端成员(Tends)。本文旨在开发一种简单的理论方法来独立于LST图像估算趋势。土壤趋势是由气象数据强迫的土壤能量平衡模型来模拟的。植被趋势是从土壤趋势和气温获得的。首先在摩洛哥的灌溉区域进行原位测量,评估模型得出的土壤趋势。建模土壤和地面土壤趋势之间的均方根差(RMSD)估计为2.4∘C。接下来,将模型衍生的土壤趋势与从90 m分辨率ASTER(高级星载热发射和反射辐射仪)获取的土壤趋势进行比较。 )在墨西哥和西班牙的两个灌溉区域收集的数据。这样的比较揭示了模型派生的和基于高分辨率图像的土壤趋向之间的强一致性。然后,使用基于模型的趋势或基于图像的趋势作为输入,将最近的上下文ET模型(SEB-1S)应用于90-m分辨率和1-km分辨率(汇总)的ASTER数据。分辨率为90 m的SEB-1S与原位ET之间的RMSD估计为65和82 W·m -2,分辨率为1 km的SEB-1S和SEB-1S ET聚合后的RMSD估计为78和56 W ·m-2分别用于基于图像的趋势和基于模型的趋势。根据上述结果,当将上下文模型应用于低分辨率图像时,应该先验估计趋势。此外,模型派生的和基于高分辨率图像的趋势之间的高度异构区域之间的一致性为开发混合建模观察方法提供了有意义的基础。

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