日本地球惑星科学連合2022年大会

講演情報

[E] 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-EM13] Coupling Processes in the Atmosphere-Ionosphere System

2022年5月25日(水) 09:00 〜 10:30 302 (幕張メッセ国際会議場)

コンビーナ:Huixin Liu(九州大学理学研究院地球惑星科学専攻 九州大学宙空環境研究センター)、コンビーナ:大塚 雄一(名古屋大学宇宙地球環境研究所)、Chang Loren(Institute of Space Science, National Central University)、コンビーナ:Deng Yue(University of Texas at Arlington)、座長:Liu Huixin(九州大学理学研究院地球惑星科学専攻 九州大学宙空環境研究センター)、Chang Loren(Institute of Space Science, National Central University)、木暮 優(九州大学)


09:00 〜 09:15

[PEM13-13] Atmospheric Gravity Waves and Solar Wind-induced Fluctuations in the Thermosphere and Ionosphere of Mars

*Scott England1Hiromu Nakagawa2 (1.Virginia Tech、2.Tohoku University)

キーワード:Mars, Thermosphere-Ionosphere, Gravity Wave

Gravity waves are ubiquitous features of planetary atmospheres. They act as conduits through which energy and momentum is transported between different regions, and as they dissipate they cause net impacts on the atmosphere that are important for a variety of processes from mixing of minor species to momentum balance and thermal balance. Owing to a combination of high wind speeds near the surface, large topographic changes and no planetary-scale magnetic field, these waves achieve far larger amplitudes in the Martian thermosphere than are typically observed at Earth. Thus, at Mars such waves may play an even more important role than they do at Earth. Without a strong magnetic field, observations of ions at Mars also commonly reveal features of gravity waves that frequently track those in the neutral atmosphere. However, the solar wind is also capable of producing fluctuations in the ions that may have wavelengths similar to gravity waves and can confuse such an analysis unless data from both ions and neutrals are used simultaneously. Here we identify characteristics of both atmospheric waves and solar-wind induced fluctuations seen in MAVEN observations of the Martian thermosphere. Utilizing a multi-fluid model, we demonstrate that atmospheric waves do not explain the fluctuations attributed to impacts of the solar wind. We then present the occurrence rates of these solar-wind impacts, their relationship to the solar wind itself, and spatial distribution across the planet.