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An approach for analysis of reflectance spectra

机译:反射光谱的分析方法

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A band selection procedure is applied to 45 AVIRIS hyperspectral images with wavelength range 0.4-2.5 mu m, in order to establish the physical significance of individual spectral bands. Five bands (0.46-0.54 mu m, 0.61-0.69 mu m, 0.99-1.09 mu m, 1.52-1.61 mu m and 2.08-2.17 mu m), which describe 98% of the mean square spectral signal, can discriminate water, snow, fire, vegetation, and a residual class which is principally soil. For the five classes, 20 bands represent all spectra with a mean square residual of 0.1%, which approaches the noise level of the data. Atmospheric water vapor is a major source of variability for soil and vegetation spectra. Spectral bands of 0.99-1.09 mu m, 1.12-1.16 mu m, and 1.20-1.31 mu m are processed in conjunction with field and laboratory spectra and the Lowtran radiative transfer code in order to quantify this effect. Further study is required to characterize properties associated with additional bands. (C)Elsevier Science Inc., 1998. [References: 12]
机译:为了确定各个光谱带的物理意义,将波段选择程序应用于45个AVIRIS高光谱图像,波长范围为0.4-2.5μm。五个波段(0.46-0.54μm,0.61-0.69μm,0.99-1.09μm,1.52-1.61μm和2.08-2.17μm)描述了98%的均方光谱信号,可以区分水,雪,火,植被以及主要是土壤的残差类别。对于这五个类别,20个波段代表所有频谱,均方差为0.1%,接近数据的噪声水平。大气水蒸气是土壤和植被光谱变化的主要来源。结合现场和实验室光谱以及Lowtran辐射转移码处理0.99-1.09μm,1.12-1.16μm和1.20-1.31μm的光谱带,以量化这种影响。需要进一步研究来表征与其他频段相关的特性。 (C)Elsevier Science Inc.,1998年。[参考:12]

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