Temperature and Emissivity Separation From Ground-Based MIR Hyperspectral Data

被引:20
作者
Cheng, Jie [1 ,2 ,3 ,4 ]
Liang, Shunlin [1 ,2 ]
Liu, Qinhuo [3 ,4 ]
Li, Xiaowen [3 ,4 ,5 ,6 ]
机构
[1] Beijing Normal Univ, Coll Global Change & Earth Syst Sci, Beijing 100875, Peoples R China
[2] Univ Maryland, Dept Geog, College Pk, MD 20742 USA
[3] Chinese Acad Sci, Inst Remote Sensing Applicat, Beijing 100875, Peoples R China
[4] Beijing Normal Univ, State Key Lab Remote Sensing Sci, Beijing 100875, Peoples R China
[5] Beijing Normal Univ, Res Ctr Remote Sensing, Beijing 100875, Peoples R China
[6] Beijing Normal Univ, GIS, Beijing 100875, Peoples R China
来源
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING | 2011年 / 49卷 / 04期
基金
中国国家自然科学基金; 国家高技术研究发展计划(863计划);
关键词
Bidirectional reflectance distribution function (BRDF); hyperspectral; mid-infrared (MIR); temperature and emissivity separation (TES); LAND-SURFACE-TEMPERATURE; THERMAL INFRARED DATA; ALGORITHM; RETRIEVAL; ASTER; SPECTRA; MODIS;
D O I
10.1109/TGRS.2010.2076818
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Temperature and emissivity separation (TES) algorithms designed to work with mid-infrared (MIR) hyperspectral data are extremely limited. Two TES algorithms originally designed for long-wave infrared hyperspectral data, specifically, the iterative spectrally smooth (ISS) algorithm and the stepwise refining algorithm, are extended into MIR and renamed the extended iterative spectrally smooth (EISS) and extended stepwise refining algorithms (ESR), respectively. Numerical experiments are first conducted to evaluate their feasibility. The results of the numerical experiments indicate that the accuracy of the ESR algorithm is higher than that of the EISS algorithm. Moreover, the ESR algorithm is more robust than the EISS algorithm under sunlit conditions. Their accuracy is then validated with in situ measurements. Finally, the emissivity root mean square errors (RMSEs) of the EISS and ESR algorithms are compared with the data derived with the ISS algorithm using in situ measurements. Results show that the average emissivity RMSEs of 0.03 in 2000-2200 cm(-1) and of 0.03-0.30 in 2400-3000 cm(-1) for nighttime, and 0.02 in 2000-2200 cm(-1) and 0.03 in 2500-3000 cm(-1) for daytime, can be obtained from ground-based MIR hyperspectral data using the ESR algorithm.
引用
收藏
页码:1473 / 1484
页数:12
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