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系外行星视角下的未来冰巨星探测

The exoplanet perspective on future ice giant exploration.

作者信息

Wakeford H R, Dalba P A

机构信息

School of Physics, University of Bristol, HH Wills Laboratory, Tyndall Avenue, Bristol BS8 1TL, UK.

Department of Earth and Planetary Sciences, University of California Riverside, 900 University Avenue, Riverside CA 92521, USA.

出版信息

Philos Trans A Math Phys Eng Sci. 2020 Dec 25;378(2187):20200054. doi: 10.1098/rsta.2020.0054. Epub 2020 Nov 9.

DOI:10.1098/rsta.2020.0054
PMID:33161853
Abstract

Exoplanets number in their thousands, and the number is ever increasing with the advent of new surveys and improved instrumentation. One of the most surprising things we have learnt from these discoveries is not that small-rocky planets in their stars habitable zones are likely to be common, but that the most typical size of exoplanets is that not seen in our solar system-radii between that of Neptune and the Earth dubbed mini-Neptunes and super-Earths. In fact, a transiting exoplanet is four times as likely to be in this size regime than that of any giant planet in our solar system. Investigations into the atmospheres of giant hydrogen/helium dominated exoplanets has pushed down to Neptune and mini-Neptune-sized worlds revealing molecular absorption from water, scattering and opacity from clouds, and measurements of atmospheric abundances. However, unlike measurements of Jupiter, or even Saturn sized worlds, the smaller giants lack a ground truth on what to expect or interpret from their measurements. How did these sized worlds form and evolve and was it different from their larger counterparts? What is their internal composition and how does that impact their atmosphere? What informs the energy budget of these distant worlds? In this we discuss what characteristics we can measure for exoplanets, and why a mission to the ice giants in our solar system is the logical next step for understanding exoplanets. This article is part of a discussion meeting issue 'Future exploration of ice giant systems'.

摘要

系外行星的数量数以千计,而且随着新的勘测项目和改进后的仪器设备不断出现,这一数字还在持续增加。我们从这些发现中学到的最令人惊讶的事情之一,并非恒星宜居带中的小型岩石行星可能很常见,而是系外行星最典型的尺寸是在我们太阳系中未曾见过的——其半径介于海王星和地球之间,被称为迷你海王星和超级地球。事实上,一颗凌日系外行星处于这一尺寸范围的可能性是我们太阳系中任何气态巨行星的四倍。对以氢/氦为主的气态巨系外行星大气层的研究已经深入到海王星和迷你海王星大小的世界,揭示了水的分子吸收、云层的散射和不透明度,以及大气丰度的测量结果。然而,与对木星甚至土星大小的行星的测量不同,这些较小的气态巨行星缺乏一个关于从测量中预期或解释什么的基本事实依据。这些大小的行星是如何形成和演化的,与它们更大的同类行星有何不同?它们的内部组成是什么,这又如何影响它们的大气层?是什么决定了这些遥远世界的能量收支?在此,我们将讨论我们可以测量系外行星的哪些特征,以及为什么对我们太阳系中的冰巨行星进行探测是理解系外行星的合乎逻辑的下一步。本文是“冰巨行星系统的未来探索”讨论会议专题的一部分。

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