High-resolution shape models of Phobos and Deimos from stereophotoclinometry.

IF 3 3区 地球科学
Earth, Planets and Space Pub Date : 2023-01-01 Epub Date: 2023-06-25 DOI:10.1186/s40623-023-01814-7
Carolyn M Ernst, R Terik Daly, Robert W Gaskell, Olivier S Barnouin, Hari Nair, Benjamin A Hyatt, Manar M Al Asad, Kielan K W Hoch
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引用次数: 1

Abstract

We created high-resolution shape models of Phobos and Deimos using stereophotoclinometry and united images from Viking Orbiter, Phobos 2, Mars Global Surveyor, Mars Express, and Mars Reconnaissance Orbiter into a single coregistered collection. The best-fit ellipsoid to the Phobos model has radii of (12.95 ± 0.04) km × (11.30 ± 0.04) km × (9.16 ± 0.03) km, with an average radius of (11.08 ± 0.04) km. The best-fit ellipsoid to the Deimos model has radii of (8.04 ± 0.08) km × (5.89 ± 0.06) km × (5.11 ± 0.05) km with an average radius of (6.27 ± 0.07) km. The new shape models offer substantial improvements in resolution over existing shape models, while remaining globally consistent with them. The Phobos model resolves grooves, craters, and other surface features ~ 100 m in size across the entire surface. The Deimos model is the first to resolve geological surface features. These models, associated data products, and a searchable, coregistered collection of images across six spacecraft are publicly available in the Small Body Mapping Tool, and will be archived with the NASA Planetary Data System. These products enable an array of future studies to advance the understanding of Phobos and Deimos, facilitate coregistration of other past and future datasets, and set the stage for planning and operating future missions to the moons, including the upcoming Martian Moons eXploration (MMX) mission.

Graphical abstract:

Supplementary information: The online version contains supplementary material available at 10.1186/s40623-023-01814-7.

Abstract Image

Abstract Image

Abstract Image

来自立体摄影测斜的火卫一和Deimos的高分辨率形状模型。
我们使用立体摄影测斜法创建了火卫一和Deimos的高分辨率形状模型,并将维京轨道飞行器、火卫二号、火星全球勘测者、火星快车和火星勘测轨道飞行器的图像合并为一个共同注册的集合。最适合火卫一模型的椭球体半径为(12.95 ± 0.04)公里 × (11:30 ± 0.04)公里 × (9.16 ± 0.03)公里,平均半径为(11.08 ± 0.04)km。最适合Deimos模型的椭球体半径为(8.04 ± 0.08)公里 × (5.89 ± 0.06)公里 × (5.11 ± 0.05)km,平均半径为(6.27 ± 0.07)公里。与现有的形状模型相比,新的形状模型在分辨率上有了实质性的提高,同时在全球范围内保持一致。火卫一模型解析了凹槽、陨石坑和其他表面特征 ~ 整个表面尺寸为100米。Deimos模型是第一个解析地质表面特征的模型。这些模型、相关数据产品以及六艘航天器的可搜索、共同注册的图像集可在小型天体测绘工具中公开获取,并将与美国国家航空航天局行星数据系统一起存档。这些产品使一系列未来的研究能够推进对火卫一和Deimos的理解,促进其他过去和未来数据集的共同注册,并为规划和运行未来的月球任务奠定基础,包括即将到来的火星月球探索(MMX)任务。图形摘要:补充信息:在线版本包含补充材料,可访问10.1186/s40623-023-01814-7。
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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来源期刊
Earth, Planets and Space
Earth, Planets and Space 地学天文-地球科学综合
CiteScore
5.80
自引率
16.70%
发文量
167
期刊介绍: Earth, Planets and Space (EPS) covers scientific articles in Earth and Planetary Sciences, particularly geomagnetism, aeronomy, space science, seismology, volcanology, geodesy, and planetary science. EPS also welcomes articles in new and interdisciplinary subjects, including instrumentations. Only new and original contents will be accepted for publication.
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