日本地球惑星科学連合2022年大会

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[J] ポスター発表

セッション記号 P (宇宙惑星科学) » P-CG 宇宙惑星科学複合領域・一般

[P-CG19] 惑星大気圏・電磁圏

2022年5月29日(日) 11:00 〜 13:00 オンラインポスターZoom会場 (4) (Ch.04)

コンビーナ:前澤 裕之(大阪府立大学大学院理学系研究科物理科学科)、コンビーナ:寺田 直樹(東北大学大学院理学研究科)、関 華奈子(東京大学大学院理学系研究科)、コンビーナ:今村 剛(東京大学大学院 新領域創成科学研究科)、座長:青木 翔平(宇宙航空研究開発機構 宇宙科学研究所)、関 華奈子(東京大学大学院理学系研究科)、今村 剛(東京大学大学院 新領域創成科学研究科)

11:00 〜 13:00

[PCG19-P03] Feasibility studies on Mars and Venus science for LAPYUTA

*益永 圭1堺 正太朗2村上 豪1土屋 史紀2山崎 敦1吉岡 和夫3木村 智樹4鍵谷 将人2古賀 亮一5 (1.宇宙航空研究開発機構、2.東北大学、3.東京大学、4.東京理科大学、5.名古屋大学)

キーワード:火星、金星、LAPYUTA、紫外観測、超高層大気

Life-environmentology, Astronomy, PlanetarY, Ultraviolet Telescope Assembly (LAPYUTA) is an ultraviolet space telescope mission to study habitable environments in the solar system and beyond, which we prepare to propose for a future Japanese small class mission. LAPYUTA is designed to address much larger effective area (>100 cm2) and much better angular resolution (0.1 arcsec) than those of JAXA Hisaki space telescope, and thus achieves comparable sensitivity and spatial resolution to those of the Hubble Space Telescope. Taking advantage of the long machine time, we will observe variations of UV signatures from solar system bodies, exoplanets, and astronomical bodies to explore habitable environments in the universe.

Two of the main targets of LAPYUTA are our neighboring planets, Mars and Venus. Today, these planets have extreme and inhabitable environments. Studies, however, suggest that Mars and Venus might have been habitable planets; They had much water, atmosphere, and possibly life. Then a big question immediately arises; Where did water and atmosphere go? By monitoring hydrogen, oxygen, and carbon UV emissions in their upper atmospheres, we aim to study how Mars and Venus have lost water and experienced climate changes over the history.

In this study, we conducted a feasibility study for LAPYUTA to detect hydrogen (Lyman-alpha), oxygen (1304Å and 1356Å), and carbon (CII 1335Å) emissions as water and carbon tracers in the upper atmosphere of Mars and Venus. These emissions are mainly excited by solar resonant scattering in the exosphere and/or photoelectron impact in the ionosphere. We estimated required accumulation time to accomplish the signal to noise ratio of 5 for each emission line, using measurements from previous missions such as Pioneer Venus Orbiter, MAVEN, and Hisaki. In this presentation, we report spatial and time resolutions that LAPYUTA can address for each emission line when observing the disk, limb, and corona of Mars and Venus, and discuss feasibilities of several scientific objectives.