1. Study of Atmospheric Ion Escape From Exoplanet TOI‐700 d: Venus Analogs.
- Author
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Nishioka, T., Seki, K., Sakata, R., Yamamoto, K., Terada, N., Sakai, S., Shinagawa, H., and Nakayama, A.
- Subjects
INTERPLANETARY magnetic fields ,VENUS (Planet) ,PLANETARY atmospheres ,MAGNETISM ,SOLAR atmosphere ,MAGNETIC fields ,EARTH currents ,HABITABLE planets ,STELLAR magnetic fields - Abstract
TOI‐700 d is the first Earth‐sized planet in the habitable zone (HZ) discovered by the Transiting Exoplanet Survey Satellite. Here, we assess whether a Venus‐like exoplanet at the TOI‐700 d location could retain an atmosphere for a time comparable to the age of the host star based on multispecies magnetohydrodynamics simulations. We investigate the effects of X‐ray and EUV (XUV) radiation from the host star, the interplanetary magnetic field (IMF) orientation, and the planetary intrinsic magnetic field. In unmagnetized cases, major ion loss is caused by O+ escape through a ring‐shaped region by the mass loading process after the ionization of the extended oxygen corona. As the IMF Parker spiral angle increases, the escape flux in the magnetotail shows stronger enhancement around the meridional current sheet, and the escape rate of molecular ions (O2+ ${\mathrm{O}}_{\mathrm{2}}^{+}$ and CO2+ $\mathrm{C}{\mathrm{O}}_{\mathrm{2}}^{+}$) increases by an order of magnitude due to acceleration in the ionosphere by magnetic tension forces. In magnetized cases, the intrinsic magnetic field suppresses ion pickup loss from the neutral oxygen corona by deflecting the stellar wind and preventing ion pickup while promoting cusp‐origin escape from the lower ionosphere. These results suggest that the unmagnetized exoplanet would have difficulty retaining its atmosphere over a few billion years under extreme conditions where XUV is 30 times stronger than at the current Earth. However, the dipole intrinsic magnetic field of 1,000 nT at the equatorial surface reduces the escape rate and would help the exoplanet to retain its atmosphere even under strong XUV conditions. Plain Language Summary: The recent discovery of Earth‐sized planets in the habitable zones (HZ) of M dwarfs has garnered attention over whether liquid water and life exist on these planets. We investigate the habitability of planets around M dwarfs in terms of atmospheric retention. Planetary atmospheres are necessary not only to retain liquid water on the surface but also to protect life from high‐energy particles and radiation. In this paper, we assess the feasibility of atmospheric retention on a Venus‐like exoplanet at the location of TOI‐700 d, which is the first Earth‐sized planet in the HZ discovered by the Transiting Exoplanet Survey Satellite. Our simulations show that the unmagnetized exoplanet cannot retain an atmosphere under extreme conditions where the planet is exposed to the intense light from the host star that energizes the upper layers of the planetary atmosphere, but the presence of an intrinsic magnetic field might make this possible. The escape rate of atmospheric ions, especially molecular ions, is suppressed by the interplanetary magnetic field nearly parallel to the stellar wind velocity, which may be typical as the planet and the host star get closer. Key Points: Stellar X‐ray and EUV (XUV) must be within 30 times that of Earth to retain a Venus‐like atmosphere for an unmagnetized exoplanetIn unmagnetized cases, the Parker spiral angle affects molecular ion escape due to the tension force of draping magnetic field linesA strong intrinsic magnetic field suppresses ion escape, allowing the atmosphere to be retained even when XUV is 50 times that of Earth [ABSTRACT FROM AUTHOR]
- Published
- 2023
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