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A water vapor scaling model for improved land surface temperature and emissivity separation of MODIS thermal infrared data

机译:用于改善陆面温度和MODIS热红外数据发射率分离的水汽比例模型

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We present an improved water vapor scaling (WVS) model for atmospherically correcting MODIS thermal infrared (TIR) bands in the temperature emissivity separation (TES) algorithm. TES is used to retrieve the land surface temperature and emissivity (LST&E) from MODIS TIR bands 29, 31, and 32. The WVS model improves the accuracy of the atmospheric correction parameters in TES on a band-by-band and pixel-by-pixel basis. We used global atmospheric radiosondes profiles to generate view angle and day-night-dependent WVS coefficients that are valid for all MODIS scan angles up to 65. We demonstrate the effects of applying the improved WVS model on the retrieval accuracy of MODIS-TES (MODTES) LST&E using a case study for a granule over the southwest USA during very warm and moist monsoonal atmospheric conditions. Furthermore, a comprehensive validation of the MODTES LST&E retrieval was performed over two sites at the quartz-rich Algodones Dunes in California and a grassland site in Texas, USA using three full years of MODIS Aqua data. Results from the case study showed that absolute errors in the emissivity retrieval for the three MODIS TIR bands were reduced on average from 1.4% to 0.4% when applying the WVS method. A Radiance-based method was used to validate the MODTES LST retrievals for and the results showed that application of the WVS method with the MODTES algorithm led to significant reduction in both bias and root mean square error (RMSE) of the LST retrievals at both sites. When the WVS model was applied, LST RMSE's were reduced on average from 1.3 K to 1.0 K at the Algodones Dunes site, and from 1.2 K to 0.7 K at the Texas Grassland site. This study demonstrated that the WVS atmospheric correction model is critical for retrieving MODTES LST with <1 K accuracy and emissivity with <1% consistently for a wide range of challenging atmospheric conditions and land surface types. (C) 2016 Elsevier Inc. All rights reserved.
机译:我们提出了一种改进的水蒸气定标(WVS)模型,用于在大气中校正温度发射率分离(TES)算法中的MODIS热红外(TIR)波段。 TES用于从MODIS TIR波段29、31和32检索地面温度和辐射率(LST&E)。WVS模型提高了TES在逐波段和逐像素时的大气校正参数的准确性。像素基础。我们使用了全球大气探空仪剖面图来生成视角和昼夜相关的WVS系数,这些系数对所有MODIS扫描角(直至65°)都有效。我们展示了应用改进的WVS模型对MODIS-TES(MODTES )LST&E,以在非常温暖和潮湿的季风大气条件下美国西南部的颗粒为例的研究。此外,使用MODIS Aqua整整三年的数据,在加利福尼亚州石英含量高的Algodones沙丘和美国德克萨斯州的草原站点的两个站点上进行了MODTES LST&E检索的全面验证。案例研究的结果表明,使用WVS方法时,三个MODIS TIR波段的发射率检索中的绝对误差平均从1.4%降低到0.4%。基于辐射的方法用于验证MODTES LST检索的结果,结果表明WVS方法与MODTES算法的应用可显着降低两个站点LST检索的偏差和均方根误差(RMSE) 。使用WVS模型时,Algodones Dunes站点的LST RMSE平均从1.3 K降低到1.0 K,而德克萨斯州草地站点的LST RMSE从1.2 K降低到0.7K。这项研究表明,WVS大气校正模型对于在各种具有挑战性的大气条件和地面类型中,以<1 K的精度和小于1%的发射率始终如一地检索MODTES LST至关重要。 (C)2016 Elsevier Inc.保留所有权利。

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