Evaluating Eight Global Reanalysis Products for Atmospheric Correction of Thermal Infrared Sensor-Application to Landsat 8 TIRS10 Data

被引:27
|
作者
Meng, Xiangchen [1 ,2 ,3 ]
Cheng, Jie [1 ,2 ,3 ,4 ]
机构
[1] Beijing Normal Univ, State Key Lab Remote Sensing Sci, Beijing 100875, Peoples R China
[2] Chinese Acad Sci, State Key Lab Remote Sensing Sci, Inst Remote Sensing & Digital Earth, Beijing 100875, Peoples R China
[3] Beijing Normal Univ, Fac Geog Sci, Inst Remote Sensing Sci & Engn, Beijing 100875, Peoples R China
[4] ARS, USDA, Hydrol & Remote Sensing Lab, Beltsville, MD 20705 USA
基金
中国国家自然科学基金;
关键词
Landsat; atmospheric correction; NCEP; MERRA; MERRA2; JRA-55; ERA-Interim; SURFACE TEMPERATURE RETRIEVAL; EMISSIVITY SEPARATION; ALGORITHM; RESOLUTION; BAND; PROFILES; NCEP; CALIBRATION; VALIDATION;
D O I
10.3390/rs10030474
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Global reanalysis products have been widely used for correcting the atmospheric effects of thermal infrared data, but their performances have not been comprehensively evaluated. In this paper, we evaluate eight global reanalysis products (NCEP/FNL; NCEP/DOE Reanalysis2; MERRA-3; MERRA-6; MERRA2-3; MERRA2-6; JRA-55; and ERA-Interim) commonly used in the atmospheric correction of Landsat 8 TIRS10 data by referencing global radiosonde observations collected from 163 stations. The atmospheric parameters (atmospheric transmittance, upward radiance, and downward radiance) simulated with MERRA-6 and ERA-Interim were accurate than those simulated with other reanalysis products for different water vapor contents and surface elevations. When global reanalysis products were applied to retrieve land surface temperature (LST) from simulated Landsat 8 TIRS10 data, ERA-Interim and MERRA-6 were accurate than other reanalysis products. The overall LST biases and RMSEs between the retrieved LSTs and LSTs that were used to generate the top-of-atmosphere radiances were less than 0.2 K and 1.09 K, respectively. When eight reanalysis products were used to estimate LSTs from thirty-two Landsat 8 TIRS10 images covering the Heihe River basin in China, the various reanalysis products showed similar validation accuracies for LSTs with low water vapor contents. The biases ranged from 0.07 K to 0.24 K, and the STDs (RMSEs) ranged from 1.93 K (1.93 K) to 2.02 K (2.04 K). Considering the above evaluation results, MERRA-6 and ERA-Interim are recommended for thermal infrared data atmospheric corrections.
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页数:19
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