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木卫三、木卫二和木卫四表面及近表面大气层的“果汁号”探测器特征研究

Characterization of the Surfaces and Near-Surface Atmospheres of Ganymede, Europa and Callisto by JUICE.

作者信息

Tosi Federico, Roatsch Thomas, Galli André, Hauber Ernst, Lucchetti Alice, Molyneux Philippa, Stephan Katrin, Achilleos Nicholas, Bovolo Francesca, Carter John, Cavalié Thibault, Cimò Giuseppe, D'Aversa Emiliano, Gwinner Klaus, Hartogh Paul, Huybrighs Hans, Langevin Yves, Lellouch Emmanuel, Migliorini Alessandra, Palumbo Pasquale, Piccioni Giuseppe, Plaut Jeffrey J, Postberg Frank, Poulet François, Retherford Kurt, Rezac Ladislav, Roth Lorenz, Solomonidou Anezina, Tobie Gabriel, Tortora Paolo, Tubiana Cecilia, Wagner Roland, Wirström Eva, Wurz Peter, Zambon Francesca, Zannoni Marco, Barabash Stas, Bruzzone Lorenzo, Dougherty Michele, Gladstone Randy, Gurvits Leonid I, Hussmann Hauke, Iess Luciano, Wahlund Jan-Erik, Witasse Olivier, Vallat Claire, Lorente Rosario

机构信息

Istituto Nazionale di Astrofisica - Istituto di Astrofisica e Planetologia Spaziali (INAF-IAPS), Rome, Italy.

Institute of Planetary Research, German Aerospace Center (DLR), Berlin, Germany.

出版信息

Space Sci Rev. 2024;220(5):59. doi: 10.1007/s11214-024-01089-8. Epub 2024 Aug 8.

Abstract

We present the state of the art on the study of surfaces and tenuous atmospheres of the icy Galilean satellites Ganymede, Europa and Callisto, from past and ongoing space exploration conducted with several spacecraft to recent telescopic observations, and we show how the ESA JUICE mission plans to explore these surfaces and atmospheres in detail with its scientific payload. The surface geology of the moons is the main evidence of their evolution and reflects the internal heating provided by tidal interactions. Surface composition is the result of endogenous and exogenous processes, with the former providing valuable information about the potential composition of shallow subsurface liquid pockets, possibly connected to deeper oceans. Finally, the icy Galilean moons have tenuous atmospheres that arise from charged particle sputtering affecting their surfaces. In the case of Europa, plumes of water vapour have also been reported, whose phenomenology at present is poorly understood and requires future close exploration. In the three main sections of the article, we discuss these topics, highlighting the key scientific objectives and investigations to be achieved by JUICE. Based on a recent predicted trajectory, we also show potential coverage maps and other examples of reference measurements. The scientific discussion and observation planning presented here are the outcome of the JUICE Working Group 2 (WG2): "".

摘要

我们介绍了对木星系冰冷卫星木卫三、木卫二和木卫四的表面及稀薄大气层的研究现状,涵盖了过去和正在进行的多个航天器太空探索以及近期的望远镜观测情况,并展示了欧洲航天局的“木星系冰卫星探测器”(JUICE)任务计划如何利用其科学载荷对这些表面和大气层进行详细探测。卫星的表面地质是其演化的主要证据,反映了潮汐相互作用提供的内部加热情况。表面成分是内生和外生过程的结果,前者提供了有关浅层地下液囊潜在成分的宝贵信息,这些液囊可能与更深的海洋相连。最后,木星系的冰冷卫星拥有由影响其表面的带电粒子溅射产生的稀薄大气层。就木卫二而言,也有关于水蒸气羽流的报道,目前其现象学尚不清楚,需要未来进行近距离探测。在本文的三个主要部分中,我们将讨论这些主题,突出 JUICE 要实现的关键科学目标和调查。基于最近预测的轨道,我们还展示了潜在覆盖图和其他参考测量示例。这里呈现的科学讨论和观测计划是 JUICE 第二工作组(WG2)的成果。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4105/11310297/efe729b2422d/11214_2024_1089_Fig1_HTML.jpg

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