日本地球惑星科学連合2024年大会

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セッション記号 P (宇宙惑星科学) » P-PS 惑星科学

[P-PS09] 月の科学と探査

2024年5月27日(月) 13:45 〜 15:15 101 (幕張メッセ国際会議場)

コンビーナ:西野 真木(宇宙航空研究開発機構宇宙科学研究所)、鹿山 雅裕(東京大学大学院総合文化研究科広域科学専攻広域システム科学系)、仲内 悠祐(立命館大学)、小野寺 圭祐(東京大学地震研究所)、座長:三宅 洋平(神戸大学大学院システム情報学研究科)、長岡 央(立命館大学)


14:00 〜 14:15

[PPS09-12] The Relationship Between the Energization of Moon-originating Ions and Terrain Type on the Lunar Surface

*Jaehee Lee1Khan-Hyuk Kim1、Seul-Min Baek2、Ho Jin1Yoshifumi Saito3Masaki N Nishino3Shoichiro Yokota4 (1.Kyunghee Univ.、2.Korea Astronomy and Space Science Institute、3.Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency、4.Osaka University)

キーワード:Moon, Magnetotail, Kaguya

We analyze data acquired by the Kaguya satellite on 14 October 2008 when the Moon was in the terrestrial magnetotail lobe to gain new insight into the energization of ions originating from the Moon. The Moon-originating ions were detected over a broad range of latitudes from -80° to 50° above the Moon’s dayside at ~100 km altitude. The fluxes of the Moon-originating ions were observed at energies from ~50 to ~1000 eV. Additionally, these ions exhibited a wide distribution pitch angle spanning from ~45 to 90°. The energy levels of ions originating from the Moon show rapid changes, either increasing or decreasing by a factor of ~10 within 8 min without the solar zenith angle dependence. Such rapid energy changes were observed over the highland regions. These observations are discussed in light of possible acceleration mechanisms of Moon-originating ions, including temporal and spatial effects.