日本地球惑星科学連合2023年大会

講演情報

[E] オンラインポスター発表

セッション記号 P (宇宙惑星科学) » P-PS 惑星科学

[P-PS04] Advancing the science of Venus in the golden age of exploration

2023年5月25日(木) 09:00 〜 10:30 オンラインポスターZoom会場 (2) (オンラインポスター)

コンビーナ:佐藤 毅彦(宇宙航空研究開発機構・宇宙科学研究本部)、はしもと じょーじ(岡山大学学術研究院自然科学学域)、Moa Persson(Graduate School of Frontier Sciences, The University of Tokyo, Kashiwa, Japan)、Kevin McGouldrick(University of Colorado Boulder)



現地ポスター発表開催日時 (2023/5/23 17:15-18:45)

09:00 〜 10:30

[PPS04-P11] Correlation analysis of Venus mesoscale UV features between 283 nm SO2 and 365 nm unknown absorber bands

★Invited Papers

*今井 正尭1、梶田 剛太1安藤 紘基1高木 征弘1 (1.京都産業大学)

キーワード:金星、あかつき、UVI、メソスケール模様

Venus shows various mesoscale features due to the absorption of solar ultraviolet (UV) radiation at the cloud-top altitude (~65 km). The Ultraviolet Imager (UVI) onboard Venus Climate Orbiter Akatsuki is equipped with two filters of 283 nm and 365 nm to visualize the spatial distribution of SO2 and unknown absorber (UA), respectively. Previous studies indicated that the UV features have a high positive correlation between the two wavelengths, suggesting SO2 and UA are closely related in the chemical cycle [Narita et al., 2022]. Therefore, it is expected that SO2 and UA are similarly affected by atmospheric motions (transport by background winds and waves). However, some observations show that the spatial structure of features differs significantly between these two wavelengths. The cause of the variation in the correlation of the features will be useful for understanding the motion and vertical distribution of materials in the Venusian atmosphere. In this study, we calculated the correlation coefficients between mesoscale features (~ 1000–2000 km) observed at the two wavelengths by UVI and investigated the dependence of the correlation coefficients on local time (LT) and latitude. As a result, the correlation coefficients in the analyzable range of LT = 8 – 16 hr were 0.7 – 0.8 as already reported, showing no significant LT dependence. On the other hand, the correlation coefficients depend on latitude and tend to be small or negative at low latitudes (15oS – 15oN). In this presentation, we also discuss the possibility that this latitudinal dependence could be caused by the planetary-scale Kelvin and Rossby waves in the equatorial region.