Estimating the Optimal Broadband Emissivity Spectral Range for Calculating Surface Longwave Net Radiation

被引:125
|
作者
Cheng, Jie [1 ,2 ]
Liang, Shunlin [1 ,3 ]
Yao, Yunjun [1 ,2 ]
Zhang, Xiaotong [1 ,2 ]
机构
[1] Beijing Normal Univ, Coll Global Change & Earth Syst Sci, Beijing 100875, Peoples R China
[2] Chinese Acad Sci, State Key Lab Remote Sensing Sci, Beijing Normal Univ & Inst Remote Sensing Applica, Beijing 100875, Peoples R China
[3] Univ Maryland, Dept Geog Sci, College Pk, MD 20742 USA
基金
中国国家自然科学基金;
关键词
Broadband emissivity (BBE); land surface model; refractive index; remote sensing; surface radiation budget; OPTICAL-CONSTANTS; MODEL; SNOW;
D O I
10.1109/LGRS.2012.2206367
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
Surface broadband emissivity (BBE) in the thermal infrared spectrum is essential for calculating the surface total longwave net radiation in land surface models. However, almost all narrowband emissivities estimated from satellite observations are in the 3-14-mu m spectral region. Previous studies converted these narrowband emissivities to BBE over different spectral ranges, such as 3-14, 8-12, 8-13.5, and 8-14 mu m. Errors in the calculated total longwave net radiation must be quantified systematically using these BBEs. Moreover, the best spectral range for longwave net radiation must be determined. The key to addressing these issues is the use of the realistic emissivity spectra. By applying modern radiative transfer tools, we derived the emissivity spectra of water, snow, and minerals at 1-200 mu m. Using these emissivity spectra, we first investigated the accuracy of replacing all-wavelength surface longwave net radiation with the surface longwave net radiation in the 3-100-, 4-100-, 2.5-100-, 2.5-200-, and 1-200-mu m spectral domains. Surface longwave net radiation at 2.5-200 mu m was found to be optimal, with a bias and root mean square (rms) of less than 0.928 and 0.993 W/m(2), respectively. We calculated the errors when estimating surface longwave net radiation at 2.5-200 mu m with BBE in different spectral ranges. The results show that BBE at 8-13.5 mu m had the lowest error and the corresponding bias and rms were less than 0.002 and 1.453 W/m(2), respectively. When the 2.5-200-mu m surface longwave net radiation calculated by the 8-13.5-mu m BBE was used to replace the all-wavelength surface longwave net radiation, the average bias and rms were 1.473 and 2.746 W/m(2), respectively. Using the most representative emissivity spectra, we derived the conversion formulas for calculating BBE at 8-13.5 mu m from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) and the Moderate Resolution Imaging Spectrometer (MODIS) narrowband emissivity products.
引用
收藏
页码:401 / 405
页数:5
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