日本地球惑星科学連合2018年大会

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[EE] 口頭発表

セッション記号 A (大気水圏科学) » A-OS 海洋科学・海洋環境

[A-OS12] 陸域海洋相互作用

2018年5月22日(火) 10:45 〜 12:15 106 (幕張メッセ国際会議場 1F)

コンビーナ:山敷 庸亮(京都大学大学院総合生存学館)、升本 順夫(東京大学大学院理学系研究科)、Behera Swadhin(Climate Variation Predictability and Applicability Research Group, Application Laboratory, JAMSTEC, 3173-25 Showa-machi, Yokohama 236-0001、共同)、佐々木 貴教(京都大学 大学院理学研究科 宇宙物理学教室)、座長:升本 順夫佐々木 貴教(京都大学大学院理学研究科宇宙物理学教室)

11:15 〜 11:30

[AOS12-09] Habitability of ice-covered ocean planets with high-pressure ices

*佐々木 貴教1上田 翔士2 (1.京都大学 大学院理学研究科 宇宙物理学教室、2.京都大学 大学院総合生存学館)

キーワード:系外惑星、ハビタビリティ、海洋、氷

Since the first discovery in 1995, over 3,700 exoplanets have been identified so far. Some of them are known to be located in the habitable zones around the central stars. Planets with plentiful water on the surface but outside the outer edge of the habitable zone would be globally covered with ice and no liquid water would exist on the surface. However, these “snowball planets” would have liquid water beneath the surface ice shell if sufficient geothermal heat flows up from the planetary interior to melt the interior ice. We discuss the conditions that must be satisfied for ice-covered ocean planets to have an internal ocean on the timescale of planetary evolution. We also investigate the structures of surface H2O layers of snowball planets by considering the effects of high-pressure ices. We found high-pressure ice layers underlying the internal ocean are likely to affect the habitability of the planet.