日本地球惑星科学連合2016年大会

講演情報

インターナショナルセッション(ポスター発表)

セッション記号 P (宇宙惑星科学) » P-EM 太陽地球系科学・宇宙電磁気学・宇宙環境

[P-EM04] Space Weather, Space Climate, and VarSITI

2016年5月22日(日) 17:15 〜 18:30 ポスター会場 (国際展示場 6ホール)

コンビーナ:*片岡 龍峰(国立極地研究所)、プルキネン アンティ(NASAゴダード宇宙飛行センター)、海老原 祐輔(京都大学生存圏研究所)、三好 由純(名古屋大学宇宙地球環境研究所)、清水 敏文(宇宙航空研究開発機構宇宙科学研究所)、浅井 歩(京都大学宇宙総合学研究ユニット)、陣 英克(情報通信研究機構)、佐藤 達彦(日本原子力研究開発機構)、草野 完也(名古屋大学宇宙地球環境研究所)、宮原 ひろ子(武蔵野美術大学造形学部)、伊藤 公紀(横浜国立大学大学院工学研究院)、塩川 和夫(名古屋大学宇宙地球環境研究所)、中村 卓司(国立極地研究所)、余田 成男(京都大学大学院理学研究科地球惑星科学専攻)、一本 潔(京都大学大学院理学研究科附属天文台)、石井 守(国立研究開発法人情報通信研究機構)

17:15 〜 18:30

[PEM04-P11] The verification experiment for aerosol nucleation focused on a kind of secondary cosmic rays

*鈴木 麻未1増田 公明1伊藤 好孝1さこ 隆志1松見 豊1中山 智喜1上田 紗也子三浦 和彦2草野 完也1 (1.名古屋大学宇宙地球環境研究所、2.東京理科大学理学部)

It is considered that the solar activity may affect the global climate, but the correlation mechanism is still not understood. One of the possible mechanisms for the correlation is the cloud formation by the galactic cosmic rays, which are modulated by the variation of solar magnetic activity. This relation was clearly indicated by the good correlation observed for the galactic cosmic-ray intensity and the global low-cloud amount. This hypothesis includes the ion-induced nucleation model, in which new particles in the atmosphere are created efficiently through atmospheric ions produced by cosmic rays, and finally these particles grow up to the size of cloud condensation nuclei. In this study, a laboratory experiment for verification of the hypothesis has been conducted with a reaction chamber. A flow of clean air with water vapor, ozone and sulfuric dioxide was introduced to a metallic chamber, where we irradiated UV light for solar irradiance and accelerator beam for cosmic rays. The beam of the heavy ion accelerator HIMAC at National Institute of Radiological Sciences was used in the present experiment.
In this presentation, I will report the results of the proton and nitrogen ion irradiation experiments. These high-energy ions have different ionization loss. The ionization loss is an index representing the ability to ionize the air molecules, that is, a parameter that contributes to the atmospheric ion generation. Furthermore, the simulation shows that the proton and the neutron contained in the secondary cosmic rays, keep the variation of solar activity even on the ground surface. Neutrons in secondary cosmic rays may generate energetic heavy ions (nucleus) through nuclear collisions with atmospheric atoms. Then, these energetic ions produce ionization ions through electronic energy loss process. Since it is considered that the aerosol particle generation would be increased according to the amount of ions produced in the energy loss, the experiment was carried out by using these heavy ions.
We will present the experimental result and discuss the difference of aerosol nucleation efficiency between different kinds of secondary cosmic rays.