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首页> 外文期刊>Icarus: International Journal of Solar System Studies >Calibration against the Moon I: A disk-resolved lunar model for absolute reflectance calibration
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Calibration against the Moon I: A disk-resolved lunar model for absolute reflectance calibration

机译:针对月球I的校准:用于绝对反射率校准的圆盘分辨月球模型

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We present a model of the absolute radiance of the disk-resolved Moon at visible to near infrared wavelengths. It has been developed in order to use the Moon as a calibration reference, particularly by space-based sensors observing the Earth. We begin with the development of Hillier et al. (Hillier, J., Buratti, B., Hill, K. [1999]. Icarus 141, 205-225) for the reflectance as a function of phase angle and base the lunar reflectance on the Clementine 0.750μm basemap. We adopt Hapke's (Hapke, B. [2002]. Icarus 157, 523-534) expression for the multiple scattering term, including the more accurate approximation to the Chandrasekhar H function. The geometry is based on the Jet Propulsion Laboratory Lunar Ephemeris DE 421, and the topographic slope is from the Kaguya-LALT laser altimetry (Araki, H., and 10 colleagues [2009]. Science 323, 897-900). We define three types of terrain by combining the reflectance from the Clementine basemap and the topographic model to specify maria, highlands, and crater regions, and allow mixed types between each class. Parameters of the model are solved for as a function of surface type and wavelength by comparison against data " chips" from the Robotic Lunar Observatory (ROLO; Kieffer, H.H., Stone, T.C. [2005]. Astron. J. 129, 2887-2901). The reflectance in any waveband may be computed by spectral interpolation of the model predictions relative to the scaled Apollo 16 soil spectrum. The accuracy of the model, evaluated against ROLO imagery, was found to be 2-4%.
机译:我们提出了一个在可见光到近红外波长的盘分辨月球的绝对辐射率的模型。它的开发是为了将月球用作校准参考,特别是通过天基传感器观测地球。我们从Hillier等人的发展开始。 (Hillier,J.,Buratti,B.,Hill,K. [1999]。Ic​​arus 141,205-225)的反射率是相角的函数,月球反射率基于Clementine0.750μm底图。对于多重散射项,我们采用Hapke(Hapke,B. [2002]。Icarus 157,523-534)表达式,包括对Chandrasekhar H函数的更精确近似。几何形状基于喷气推进实验室的月球星历DE 421,地形坡度来自Kaguya-LALT激光测高仪(Araki,H.和10位同事[2009]。Science 323,897-900)。我们通过结合Clementine底图和地形模型的反射率来定义三种地形,以指定玛丽亚,高地和火山口区域,并允许每个类别之间混合使用。通过与来自机器人月球观测站(ROLO; Kieffer,HH,Stone,TC [2005]的数据“芯片”)进行比较,可以根据表面类型和波长来求解模型的参数。Astron。J. 129,2887-2901 )。可以通过模型预测相对于缩放的Apollo 16土壤光谱的光谱插值来计算任何波段的反射率。根据ROLO图像评估的模型准确性为2-4%。

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