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Validation of Physical Radiative Transfer Equation-Based Land Surface Temperature Using Landsat 8 Satellite Imagery and SURFRAD in-situ Measurements

机译:利用Landsat 8卫星图像和SURFRAD验证物理辐射传递方程的陆地温度及其原位测量

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Land Surface Temperature (LST) is a key criterion in the physics of the Earth surface that controls the interactions between the land and atmosphere. The objective of this study is to evaluate the performance of physics-based Radiative Transfer Equation (RTE) method on LST retrieval using Landsat 8 satellite imagery and simultaneous in-situ LST data. In order to validate the satellite-based LST, in-situ LST measurements were obtained from Surface Radiation Budget Network (SURFRAD) stations simultaneous with satellite data acquisitions. In the study, four SURFRAD stations (BND, FPK, TBL and GWN) and five images for each SURFRAD station, totally twenty cloud-free images, were used for RTE-based LST validation. RTE method uses the atmospheric parameters acquired from radiosounding data simultaneous with satellite pass; however, these parameters were retrieved from NASA's atmospheric correction parameter calculator since radiosounding data are not available every time. Thus, this situation is another contribution of this study. As a result of the validation process of all data, the statistical measures, namely, coefficient of determination (R-2), Root Mean Square Error (RMSE), Mean Absolute Error (MAE) and RMSE-observations standard deviation ratio (RSR) were calculated as 0.96, 3.12 K, 2.30 K and 0.33, respectively. However, the accuracy of RTE method on LST retrieval increased (R-2 = 0.97, RMSE = 2.17 K, MAE = 1.44 K and RSR = 0.25) after removing TBL station from the analysis, since LST differences in this station were high for all scenes. RSR (ranging from 0 to high positive vlues) is an important measure for model evaluation, and the lower RSR value means high performance of the model. The obtained results revealed that physics-based RTE method is an effective and practical way for LST retrieval from Landsat 8 data despite using interpolated atmospheric parameters instead of radiosounding data.
机译:陆地表面温度(LST)是控制土地与大气之间的相互作用的地球表面的关键标准。本研究的目的是评估使用Landsat 8卫星图像和同时原位LST数据对LST检索的基于物理的辐射传递方程(RTE)方法的性能。为了验证基于卫星的LST,使用卫星数据采集的表面辐射预算网络(SURFRAD)站获得原位LST测量。在该研究中,每个SURFRAD站的四个SURFRAD站(BND,FPK,TBL和GWN)和五种图像,完全二十云图像,用于基于RTE的LST验证。 RTE方法使用从卫星通行的同时从辐射数据获取的大气参数;然而,由于每次都没有放射数据,因此从NASA的大气校正参数计算器检索了这些参数。因此,这种情况是这项研究的另一个贡献。由于所有数据的验证过程,统计措施,即确定系数(R-2),根均方误差(RMSE),平均绝对误差(MAE)和RMSE观察标准偏差比(RSR)计算为0.96,3.12k,2.30 k和0.33。但是,在从分析中移除TBL站后,RTE方法对LST检索的RTE方法的准确性增加(R-2 = 0.97,RMSE = 2.17K,MAE = 1.44 k和RSR = 0.25),因为该站的LST差异很高场景。 RSR(范围从0到高正VLUES)是模型评估的重要措施,较低的RSR值意味着模型的高性能。所获得的结果表明,尽管使用内插大气参数而不是放射数据,但基于物理的RTE方法是从Landsat 8数据中的LST检索的有效和实用的方法。

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