Japan Geoscience Union Meeting 2023

Presentation information

[E] Online Poster

P (Space and Planetary Sciences ) » P-PS Planetary Sciences

[P-PS05] Mars and martian moons

Tue. May 23, 2023 3:30 PM - 5:00 PM Online Poster Zoom Room (1) (Online Poster)

convener:Hideaki Miyamoto(University of Tokyo), Takeshi Imamura(Graduate School of Frontier Sciences, The University of Tokyo), Tomoki Nakamura(Department of Earth and Planetary Materials Sciences, Faculty of Science, Tohoku University), Hidenori Genda(Earth-Life Science Institute, Tokyo Institute of Technology)

On-site poster schedule(2023/5/23 17:15-18:45)

3:30 PM - 5:00 PM

[PPS05-P17] A multifluid MHD study on three-dimensional Kelvin-Helmholtz instability at Mars

*Maodong Yan1, Tong Dang1, Jiuhou Lei1, Binzheng Zhang2, Naoki Terada3, Shotaro Sakai3, François Leblanc4 (1.University of Science and Technology of China, 2.University of Hong Kong, 3.Tohoku Univ., 4.LATMOS-IPSL-CNRS)

Keywords:Mars, Kelvin-Helmholtz instability, Multifluid MHD, Hall effect

Due to the absence of intrinsic global magnetic fields, the Martian ionosphere interacts directly with the solar wind to form an induced magnetosphere. Under the strong flow shear between solar wind and ionosphere, the Kelvin-Helmholtz instability (KHI) can occur near the magnetospheric boundary layer of Mars. Although the KHI at Mars has been reported by observations and simulations, the three-dimensional (3D) configuration of this instability and its effect on ion escape are still unsettled. In this study, using a newly-developed multi-fluid MHD model, the 3D and global characteristics of Martian KHI near the boundary layer are analyzed. The influence of the Hall effect, which indicates the relative motion between ions and electrons, on the KHI is especially investigated by comparing the temporal evolution of KHI for cases with and without the Hall term. We will also focus on the ion escape processes caused by the KHI. Furthermore, these simulated results will be compared with the MAVEN observations of KHI.