DocumentCode :
34353
Title :
Estimating the Optimal Broadband Emissivity Spectral Range for Calculating Surface Longwave Net Radiation
Author :
Cheng, Jie ; Liang, Shunlin ; Yao, Yunjun ; Zhang, Xiaotong
Volume :
10
Issue :
2
fYear :
2013
fDate :
Mar-13
Firstpage :
401
Lastpage :
405
Abstract :
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-μm 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 μm . 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 μm . 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-μm spectral domains. Surface longwave net radiation at 2.5-200 μm was found to be optimal, with a bias and root mean square (rms) of less than 0.928 and 0.993 W/m2, respectively. We calculated the errors when estimating surface longwave net radiation at 2.5-200 μm with BBE in different spectral ranges. The results show that BBE at 8-13.5 μm had the lowest error and the corresponding bias and rms were less than 0.002 and 1.453 W/m2, respectively. When the 2.5-200-μm surface longwave net radiation calculated by the 8-13.5-μm BBE was used to replace the all-wavelength surface longwave net radiation, the average bias and rms were 1.473 and 2.746 W/m2, respectively. Using the most representative emissivity spectra, we derived the conversion formulas for calculating BBE at 8-13.5 μm from the Advanced Spaceborne Thermal Emission and Reflection Radiomet- r (ASTER) and the Moderate Resolution Imaging Spectrometer (MODIS) narrowband emissivity products.
Keywords :
atmospheric radiation; radiative transfer; radiometry; remote sensing; ASTER; Advanced Spaceborne Thermal Emission and Reflection Radiometer; MODIS narrow- band emissivity products; Moderate Resolution Imaging Spectrometer; land surface models; narrowband emissivities; optimal broadband emissivity spectral range; radiative transfer tools; realistic emissivity spectra; root mean square; surface broadband emissivity; surface total longwave net radiation; Accuracy; Land surface; MODIS; Minerals; Remote sensing; Surface waves; Broadband emissivity (BBE); land surface model; refractive index; remote sensing; surface radiation budget;
fLanguage :
English
Journal_Title :
Geoscience and Remote Sensing Letters, IEEE
Publisher :
ieee
ISSN :
1545-598X
Type :
jour
DOI :
10.1109/LGRS.2012.2206367
Filename :
6276235
Link To Document :
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