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Infrared remote sensing of planetary surfaces: an overview, outstanding questions, and prospects

机译:行星表面的红外遥感:概述,尚待解决的问题和展望

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We owe a major part of our knowledge about surface composition and structure of solid planetary surfaces to infrared imaging and Fourier transform spectroscopy. Based on these methods, it succeeds to observe single planetary objects in a global geo-scientific content. The topics of infrared surface studies are mineralogical composition analyses, measurement of surface temperature, thermal inertia, and photometric observation of surface regolith texture. The comparison of infrared with photogeologic data forms the essential basis for comparative studies in planetology. The present paper summarizes outstanding results by examples of ESA experiments like VIRTIS on Venus Express and Rosetta, PFS on Mars Express, MERTIS on Bepi Colombo, and TIRVIM on ExoMars, and provides an outlook for future plans. The instruments are described, and the interplay of disciplines like planetology, IR measuring techniques, and space flight engineering is demonstrated. Infrared remote sensing provides essential knowledge about the current state of solid planetary surfaces. This allows studying fundamental questions in comparative planetology.
机译:我们将大部分关于固体行星表面的表面组成和结构的知识归功于红外成像和傅里叶变换光谱学。基于这些方法,它成功地观测了全球地球科学内容中的单个行星对象。红外表面研究的主题是矿物学组成分析,表面温度测量,热惯性和表面重石质地的光度观察。红外与光地质数据的比较构成了行星学比较研究的必要基础。本文通过ESA实验的实例总结了出色的结果,例如Venus Express和Rosetta上的VIRTIS,Mars Express上的PFS,Bepi Colombo上的MERTIS和ExoMars上的TIRVIM,并提供了未来计划的展望。描述了仪器,并论证了诸如行星学,红外测量技术和太空飞行工程等学科之间的相互作用。红外遥感提供了有关固体行星表面当前状态的基本知识。这样可以研究比较行星学中的基本问题。

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