日本地球惑星科学連合2022年大会

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[J] 口頭発表

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-EM15] 太陽圏・惑星間空間

2022年5月22日(日) 15:30 〜 17:00 105 (幕張メッセ国際会議場)

コンビーナ:岩井 一正(名古屋大学 宇宙地球環境研究所)、コンビーナ:成行 泰裕(富山大学学術研究部教育学系)、西野 真木(宇宙航空研究開発機構宇宙科学研究所)、コンビーナ:坪内 健(電気通信大学)、座長:岩井 一正(名古屋大学 宇宙地球環境研究所)、坪内 健(電気通信大学)

15:30 〜 15:45

[PEM15-01] Physical properties of the solar corona derived from radio scintillation observations with the Akatsuki spacecraft

*千葉 翔太1今村 剛1徳丸 宗利2塩田 大幸3、松本 琢磨4安藤 紘基5、竹内 央6、村田 泰宏6山崎 敦6、Häusler Bernd7、Pätzold Martin8岩井 一正2村上 豪6三好 由純2 (1.東京大学 新領域創成科学研究科、2.名古屋大学 宇宙地球環境研究所、3.情報通信機構、4.国立天文台、5.京都産業大学、6.宇宙航空研究開発機構 宇宙科学研究所、7.Institut für Satellitentechnik und Weltraumnutzung, Universität der Bundeswehr München、8.Rheinisches Institut für Umweltforschung an der Universität zu Köln)

キーワード:太陽風、電波掩蔽観測、金星探査機あかつき

The solar wind is a supersonic plasma flow streamed from the solar corona. The solar wind is classified into the fast wind (typically ~750 km/s) and the slow wind (~300 km/s). The acceleration of the solar wind mainly occurs in the outer corona at heliocentric distances of about 5–20 RS (= solar radii), where the coronal heating by magnetohydrodynamic waves and the wave-induced magnetic pressure are thought to play major roles in the acceleration. The mechanisms have not been fully confirmed by observations because the acceleration region is too close to the Sun to be observed by in-situ probes.
Recently, however, the inner heliosphere observation network is getting ready, such as NASA's Parker Solar Probe and ESA's Solar orbiter. The radio occultation observation covers the acceleration region fully and can obtain the large-scale process of the plasma complementary to in-situ observation. JAXA's Venus orbiter Akatsuki conducted the radio occultation observations on either side of the superior conjunction. The observations covered various solar cycle periods from solar maximum to solar minimum.
Key physical processes in the acceleration region can be observed with radio occultation. Coronal plasma traversing the ray path disturbs radio waves' amplitudes and frequency, from which we can derive physical parameters such as the flow speed and waves' amplitudes. We analyze data taken by radio occultation observations using Akatsuki's radio waves during the superior conjunction periods in 2011, 2016, 2018, and 2021.
The radial velocity and the turbulence characteristics (power-law exponent, axial ratio, and inner scale) were retrieved from the intensity scintillation time-series taken in 2016 by fitting a theoretical spectrum to the observed power spectra. In the radial distribution of the derived solar wind velocity, fast winds originating from regions near a coronal hole and slow winds from other regions were identified. We also found that the inner scale increases with the heliocentric distance and that the fast solar wind has larger inner scales than the slow solar wind. These tendencies are consistent with the inertial length model proposed by Coles and Harmon (1989).
We also applied wavelet analysis to the frequency time-series taken in 2011 to detect quasi-periodic fluctuations (QPC) that are thought to represent acoustic waves and quantify the amplitude, the period, and the coherence time of each wave event. The density amplitude and the wave energy flux were estimated following Miyamoto et al. (2014). We confirmed that the fractional density amplitude increases with distance up to ~6 RS. The amplitude reaches tens of percent, suggesting a possibility of wave breaking. The energy fluxes increase with distance up to ~6 RS, suggesting a local generation of waves. It is probable that these radial distributions indicate that the Alfvén waves propagating from the photosphere generate acoustic waves in the outer corona, and the generated acoustic waves dissipate to heat the corona, as suggested by numerical models. The wave energy fluxes in the fast solar wind were larger than those in the slow wind. The results suggest that the fast solar wind originating from the coronal hole is powered by a larger injection of wave energy than the slow wind originating from other regions. In this presentation, we will also report results from the data taken by Akatsuki.