Reducing the discrepancy between ASTER and MODIS land surface temperature products

被引:21
作者
Liu, Yuanbo [1 ,2 ]
Yamaguchi, Yasushi [1 ]
Ke, Changqing [3 ]
机构
[1] Nagoya Univ, Chikusa Ku, Grad Sch Environm Studies, Nagoya, Aichi 4648601, Japan
[2] Chinese Acad Sci, Nanjing Inst Geog & Limnol, Nanjing 210008, Peoples R China
[3] Nanjing Univ, Dept Geog Informat Sci, Nanjing 210093, Peoples R China
来源
SENSORS | 2007年 / 7卷 / 12期
关键词
land surface temperature; surface emissivity; retrieval algorithm; scale effects; terrain effects; remote sensing; ASTER; MODIS;
D O I
10.3390/s7123043
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
Human-induced global warming has significantly increased the importance of satellite monitoring of land surface temperature (LST) on a global scale. The MODerate-resolution Imaging Spectroradiometer (MODIS) provides a 1-km resolution LST product with almost daily coverage of the Earth, invaluable to both local and global change studies. The Advanced Spaceborne Thermal Emission Reflection Radiometer (ASTER) provides a LST product with a high spatial resolution of 90-m and a 16-day recurrent cycle, simultaneously acquired at the same height and nadir view as MODIS. ASTER and MODIS are complementary in resolution, offering a unique opportunity for scale-related studies. ASTER and MODIS LST have been widely used but the errors in LST were mostly disregarded. Correction of ASTER-to-MODIS LST discrepancies is essential for studies reliant upon the joint use of these sensors. In this study, we compared three correction approaches: the Wan et al.'s approach, the refined Wan et al.'s approach, and the generalized split window (GSW) algorithm based approach. The Wan et al.'s approach corrects the MODIS 1-km LST using MODIS 5-km LST. The refined approach modifies the Wan et al.'s approach through incorporating ASTER emissivity and MODIS 5-km data. The GSW algorithm approach does not use MODIS 5-km but only ASTER emissivity data. We examined the case over a semi-arid terrain area for the part of the Loess Plateau of China. All the approaches reduced the ASTER-to-MODIS LST discrepancy effectively. With terrain correction, the original ASTER-to-MODIS LST difference reduced from 2.7 +/- 1.28 K to -0.1 +/- 1.87 K for the Wan et al.'s approach, 0.2 +/- 1.57 K for the refined approach, and 0.1 +/- 1.33 K for the GSW algorithm based approach. Among all the approaches, the GSW algorithm based approach performed best in terms of mean, standard deviation, root mean square root, and correlation coefficient.
引用
收藏
页码:3043 / 3057
页数:15
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