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Global mapping of Titan's surface using an empirical processing method for the atmospheric and photometric correction of Cassini/VIMS images

机译:使用经验处理方法对卡西尼/ VIMS图像进行大气和光度校正的泰坦表面的全局映射

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摘要

We have processed all images of Titan's surface acquired by the Visual and Infrared Mapping Spectrometer between 2004 and 2010, with the objective of producing seamless global mosaics of the surface in the six infrared atmospheric windows at 1.08, 1.27, 1.59, 2.03, 2.6-2.7 and 5 μm. A systematic study of the photometry at 5 urn, where haze scattering can be neglected, shows that the surface behaves to first order like a Lambert surface. The results at 5 um are generalized to lower wavelengths, adding an empirical correction accounting for scattering from atmospheric aerosols, using methane band wings as a proxy for the calculation of the scattering additive term. Mosaics incorporating this empirical correction for the geometry and haze scattering show significantly less seams than any previous maps integrating data acquired over such a wide range of observing geometries, and may therefore be used for the study of surface properties. We provide several suggestions for further studies aimed at improving the global mapping of the surface of Titan. With the considered thresholds limits on the acquisition parameters, we found that 13% of Titan's surface has been mapped at an instrument resolution better than 10 km/pixel, 56% of the surface was seen at a resolution between 10 and 20 km/pixel, and 24% of the coverage falls in the range 20-50 km/pixel.
机译:我们已经处理了2004年至2010年之间通过视觉和红外测绘仪获得的泰坦表面的所有图像,目的是在1.08、1.27、1.59、2.03、2.6-2.7的六个红外大气窗口中生成无缝的表面整体镶嵌图和5微米。对5微米的光度学的系统研究表明,该表面的雾度散射可以忽略不计,该表面的行为类似于朗伯表面。在5 um处的结果被推广到较低的波长,添加了一个经验校正,该校正考虑了来自大气气溶胶的散射,并使用甲烷带翼作为计算散射加法项的代理。结合了这种对几何形状和雾度散射的经验校正的马赛克显示的接缝比以前整合了在如此广泛的观察几何范围内获得的数据的任何以前的地图显示的接缝要少得多,因此可用于研究表面特性。我们为进一步研究提供了一些建议,这些研究旨在改善土卫六表面的全局贴图。考虑到采集参数的阈值限制,我们发现,Titan表面的13%的地图分辨率高于10 km /像素,而56%的表面的分辨率在10至20 km /像素之间,并且24%的覆盖范围为20-50 km /像素。

著录项

  • 来源
    《Planetary and space science》 |2012年第1期|178-190|共13页
  • 作者单位

    Laboratoire de Planetologie et Geodynamique de Nantes, CNRS UMR 6112, Universite de Nantes, 2 rue de la Houssiniere, BP 92208, 44322 Nantes, Cedex 3, France;

    Laboratoire de Planetologie et Geodynamique de Nantes, CNRS UMR 6112, Universite de Nantes, 2 rue de la Houssiniere, BP 92208, 44322 Nantes, Cedex 3, France;

    Laboratoire AIM, University Paris 7/CNRS/CEA Centre de l'Orme des Merisiers, Bat 709, 91191 Cif/Yvette Cedex, France;

    Laboratoire de Planetologie et Geodynamique de Nantes, CNRS UMR 6112, Universite de Nantes, 2 rue de la Houssiniere, BP 92208, 44322 Nantes, Cedex 3, France,Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena CA 91109, USA;

    Department of Physics, University of Idaho, Engineering-Physics Building, Moscow ID 83844, USA;

    Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena CA 91109, USA;

    Departments of Planetary Sciences and Astronomy, University of Arizona, Tucson, USA;

    Laboratoire de Planetologie et Geodynamique de Nantes, CNRS UMR 6112, Universite de Nantes, 2 rue de la Houssiniere, BP 92208, 44322 Nantes, Cedex 3, France;

    Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena CA 91109, USA;

    United States Geological Survey, Denver CO 80225, USA;

    Department of Astronomy, Cornell University, Ithaca, NY 14853, USA;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    titan; surface; infrared; cassini; VIMS; hyperspectral;

    机译:泰坦表面;红外线;卡西尼VIMS;高光谱;

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