Estimating index of refraction, surface temperature, and downwelling radiance using polarimetric-hyperspectral imagery (P-HSI)

Jacob A. Martin, K. Gross
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Abstract

A method for retrieving index of refraction from polarimetric hyperspectral imagery (P-HSI) has been developed using a model to describe the spectral variation of the index. Index of refraction is modeled in one of two ways to reduce the number of parameters in the problem. Additionally, MODTRAN is used to model the atmosphere, further reducing the number of variables and enabling an overdetermined solution to be found. Results from simulated data of a SiC target at 25°C, with realistic noise levels, show index is retrieved to within 0.0116 for the real component and 0.034 for the imaginary component. This also shows that the atmospheric downwelling can be accurately retrieved even without a priori knowledge.
利用偏振-高光谱成像(P-HSI)估计折射率、地表温度和下沉辐射
利用描述折射率光谱变化的模型,提出了一种从偏振高光谱图像(P-HSI)中检索折射率的方法。为了减少问题中参数的数量,我们用两种方法中的一种对折射率进行建模。此外,MODTRAN用于模拟大气,进一步减少了变量的数量,并能够找到一个超确定的解决方案。在真实噪声水平下,在25°C下对SiC目标进行模拟,结果表明,真实分量的指数恢复到0.0116以内,虚分量的指数恢复到0.034以内。这也表明,即使没有先验知识,也可以准确地反演大气下流。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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