Japan Geoscience Union Meeting 2021

Presentation information

[E] Oral

P (Space and Planetary Sciences ) » P-EM Solar-Terrestrial Sciences, Space Electromagnetism & Space Environment

[P-EM08] Space Weather and Space Climate

Fri. Jun 4, 2021 3:30 PM - 5:00 PM Ch.06 (Zoom Room 06)

convener:Ryuho Kataoka(National Institute of Polar Research), A Antti Pulkkinen(NASA Goddard Space Flight Center), Kanya Kusano(Institute for Space-Earth Environmental Research, Nagoya University), Kaori Sakaguchi(National Institute of Information and Communications Technology), Chairperson:Antti A Pulkkinen(NASA Goddard Space Flight Center), Ryuho Kataoka(National Institute of Polar Research)

3:30 PM - 3:45 PM

[PEM08-07] Impacts of solar energetic particles at Mars: Global diffuse aurora and atmospheric chemistry

★Invited Papers

*Yuki Nakamura1,2, Naoki Terada1, Francois Leblanc2, Hiromu Nakagawa1, Shotaro Sakai1, Sayano Hiruba1, Ryuho Kataoka3, Kiyoka Murase4 (1.Department of Geophysics, Graduate School of Science, Tohoku University, 2.LATMOS, Sorbonne University, 3.National Institute of Polar Research, 4.The Graduate University for Advanced Studies)

Keywords:Mars, Solar energetic particle, Aurora

After 2020s, human activities in space exploration will be extended to Mars. For future exploration, it is important to assess the impacts of solar energetic particles (SEPs) on spacecraft and biological systems (e.g., radiation doses to crews, prebiotic synthesis of organic compounds) in the near-Mars environment.

The space environment of Mars is remarkably different from that of the Earth. Energetic particles can easily penetrate deep into the atmosphere to reach the surface owing to insufficient magnetospheric and atmospheric shielding of Mars. Recently, the Mars Atmosphere and Volatile EvolutioN (MAVEN) spacecraft discovered a new type of diffuse aurora that spanned across nightside Mars, resulting from the interaction of SEPs with the Martian atmosphere [Schneider et al., 2015, 2018]. This new type of diffuse aurora on Mars is characterized by global brightening and by its low peak altitude of ~ 60 km, which indicates more energy is deposited deep in the Martian atmosphere than previously thought. This presentation will provide an overview of the impacts of SEPs on the Martian environment observed by orbiters and rovers, and give some implications for the effect of crustal magnetic fields and atmospheric chemistry based on our Monte-Carlo and photochemical models.