Japan Geoscience Union Meeting 2025

Presentation information

[J] Poster

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

[P-EM17] Space Plasma Science

Tue. May 27, 2025 5:15 PM - 7:15 PM Poster Hall (Exhibition Hall 7&8, Makuhari Messe)

convener:Takanobu Amano(Department of Earth and Planetary Science, University of Tokyo), Yohei Miyake(Graduate School of System Informatics, Kobe University), Shogo Isayama(Interdisciplinary Graduate School of Engineering Sciences, Kyushu University), Takayuki Umeda(Information Initiative Center, Hokkaido University)

5:15 PM - 7:15 PM

[PEM17-P03] Development of a flexible fluid code for planetary sciences

*Naoki Terada1, Ryoya Sakata1 (1.Graduate School of Science, Tohoku University)

Keywords:Fluid code, Central scheme, Planetary atmospheric phenomena, Planetary ionospheric phenomena, Planetary magnetospheric phenomena

We have developed a flexible high-resolution fluid code based on a semi-discrete central scheme, which is applicable to a wide variety of planetary atmospheric/ionospheric/magnetospheric phenomena. The requirements for a next-generation fluid code for planetary sciences are threefold: non-HD/MHD terms are accommodated, sharp discontinuities are accurately resolved, and small amplitude waves (turbulence) are accurately resolved. A semi-discrete central scheme is one of the most promising solutions for these requirements. It does not require the use of a computationally expensive Riemann solver and spectral decomposition into characteristic waves, making it easy to implement in HD/MHD as well as non-HD/MHD codes. Although central schemes are generally more dissipative than upwind schemes, there has been remarkable progress in developing less dissipative central schemes. We have developed a flexible fluid code based on a high-order semi-discrete central scheme with a WENO limiter for spatial reconstruction and found it capable of resolving small amplitude/linear waves with a high wavenumber while retaining a shock-capturing capability. We will show some numerical tests and discuss the applicability of the code to planetary atmospheric/ionospheric/magnetospheric phenomena.