利用轨道雷达数据拍摄的火星极地冰盖三维图像。

Frederick J Foss, Nathaniel E Putzig, Bruce A Campbell, Roger J Phillips
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引用次数: 27

摘要

自2006年初抵达火星以来,美国宇航局的火星勘测轨道飞行器(MRO)上的各种仪器一直在收集火星轨道上的各种科学和工程数据。其中包括浅层雷达(SHARAD)仪器,由意大利航天局(ASI)提供,设计用于15-25 MHz频段的地下探测。在撰写本文时,MRO已经完成了46,000多个火星近极轨道,其中30%包括活跃的SHARAD数据收集。到2009年,已经在极地地区获得了足够的SHARAD覆盖密度,以支持数据的三维处理和分析。使用陆地地震数据处理中常用的工具和技术,我们将SHARAD观测结果收集的子集处理为SHARAD 3-D卷,覆盖北极和南极地区,对北极和南极冰盖的内部进行成像,分别称为Planum Boreum和Planum Australe。在克服了三维处理和分析过程中暴露的一系列挑战之后,一个完整的Planum Boreum三维体目前正在用于科学研究。在北部工作中吸取的经验教训将用于我们目前正在进行的澳大利亚平原3-D体积的3-D处理和分析。我们讨论了我们在这些项目中的经验,并介绍了来自这些努力的结果和科学见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

3-D Imaging of Mars' Polar Ice Caps Using Orbital Radar Data.

3-D Imaging of Mars' Polar Ice Caps Using Orbital Radar Data.

3-D Imaging of Mars' Polar Ice Caps Using Orbital Radar Data.

3-D Imaging of Mars' Polar Ice Caps Using Orbital Radar Data.

Since its arrival in early 2006, various instruments aboard NASA's Mars Reconnaissance Orbiter (MRO) have been collecting a variety of scientific and engineering data from orbit around Mars. Among these is the SHAllow RADar (SHARAD) instrument, supplied by Agenzia Spaziale Italiana (ASI) and designed for subsurface sounding in the 15-25 MHz frequency band. As of this writing, MRO has completed over 46,000 nearly polar orbits of Mars, 30% of which have included active SHARAD data collection. By 2009, a sufficient density of SHARAD coverage had been obtained over the polar regions to support 3-D processing and analysis of the data. Using tools and techniques commonly employed in terrestrial seismic data processing, we have processed subsets of the resulting collection of SHARAD observations covering the north and south polar regions as SHARAD 3-D volumes, imaging the interiors of the north and south polar ice caps known, respectively, as Planum Boreum and Planum Australe. After overcoming a series of challenges revealed during the 3-D processing and analysis, a completed Planum Boreum 3-D volume is currently being used for scientific research. Lessons learned in the northern work fed forward into our 3-D processing and analysis of the Planum Australe 3-D volume, currently under way. We discuss our experiences with these projects and present results and scientific insights stemming from these efforts.

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