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arXiv 2210.01460astro-ph.EPphysics.ao-ph
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通过有效的原子线辐射冷却使陆地N2-O2大气在剧烈的XUV环境中存活

Survival of Terrestrial N2-O2 Atmospheres in Violent XUV Environments through Efficient Atomic Line Radiative Cooling

Akifumi Nakayama, Masahiro Ikoma, Naoki Terada

摘要:

大气层在行星的可居住性中起着至关重要的作用。在M矮星和年轻的类太阳恒星周围,行星受到与现在地球相同的太阳辐射,暴露在强烈的恒星X射线和极紫外线(XUV)辐射下。这项研究探讨了当今地球的大气层是否能在如此恶劣的XUV环境中生存的基本问题。以前的理论研究表明,恒星的XUV辐射足够强烈,可以在短时间内完全消除这种大气。在这项研究中,我们开发了一个新的高层大气模型,并重新研究了热层结构的热和流体动力学响应的地球一样的N2-O2大气,在地球质量的行星,在XUV辐射的增加。我们的模型包括通过原子和离子的电子跃迁的辐射冷却的影响,称为原子线冷却,除了由以前的模型占的过程。我们表明,原子线冷却占主导地位的流体动力学效应在XUV辐射水平大于几倍,目前的地球水平。因此,大气层的结构几乎保持流体静力学,即使在XUV辐射水平达到目前地球辐射水平的一千倍时,其逃逸仍然缓慢。我们对N2-O2大气的Jeans逃逸率的估计表明,这些1巴的大气在类太阳恒星的早期活跃阶段幸存下来。即使在活跃的晚M矮星周围,N2-O2大气层也可以在十亿年的时间尺度上逃脱显着的热损失。这些结果为类地系外行星的可居住性和地球的气候历史提供了新的见解。

英文摘要:

Atmospheres play a crucial role in planetary habitability. Around M dwarfs and young Sun-like stars, planets receiving the same insolation as the present-day Earth are exposed to intense stellar X-rays and extreme-ultraviolet (XUV) radiation. This study explores the fundamental question of whether the atmosphere of present-day Earth could survive in such harsh XUV environments. Previous theoretical studies suggest that stellar XUV irradiation is sufficiently intense to remove such atmospheres completely on short timescales. In this study, we develop a new upper-atmospheric model and re-examine the thermal and hydrodynamic responses of the thermospheric structure of an Earth-like N2-O2 atmosphere, on an Earth-mass planet, to an increase in the XUV irradiation. Our model includes the effects of radiative cooling via electronic transitions of atoms and ions, known as atomic line cooling, in addition to the processes accounted for by previous models. We demonstrate that atomic line cooling dominates over the hydrodynamic effect at XUV irradiation levels greater than several times the present level of the Earth. Consequentially, the atmosphere's structure is kept almost hydrostatic, and its escape remains sluggish even at XUV irradiation levels up to a thousand times that of the Earth at present. Our estimates for the Jeans escape rates of N2-O2 atmospheres suggest that these 1 bar atmospheres survive in early active phases of Sun-like stars. Even around active late M dwarfs, N2-O2 atmospheres could escape significant thermal loss on timescales of gigayears. These results give new insights into the habitability of terrestrial exoplanets and the Earth's climate history.

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