Japan Geoscience Union Meeting 2024

Presentation information

[J] Poster

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

[P-EM17] Space Plasma Science

Thu. May 30, 2024 5:15 PM - 6:45 PM Poster Hall (Exhibition Hall 6, 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 - 6:45 PM

[PEM17-P04] Improving the Finite-Difference Time-Domain (FDTD) method: Suppressing numerical errors from current densities in higher-order methods

*Xinyu Ge1,2, Harune Sekido1,2, Takayuki Umeda3, Yoshizumi Miyoshi2 (1.Graduate School of Engineering, Nagoya University, 2.Institute for Space-Earth Environmental Research, Nagoya University, 3.Information Initiative Center, Hokkaido University)

Keywords:FDTD, Courant condition, phase velocity, dispersion relation

The objective of the present study is to suppress numerical errors arising from current densities in higher-order FDTD (Finite-Difference Time-Domain) methonds. The FDTD method is a numerical approach for solving time-development of electromagnetic fields by approximating Maxwell's equations with finite differences of second-order accuracy in both time and space (Yee 1966), which is referred to as FDTD(2,2). FDTD(2,2) has problems such as numerical oscillations in continuous waveforms. Consequently, numerical methods with higher-order finite differences were developed. However, FDTD(2,4) (Fang 1989; Petropoulos 1994) and FDTD(2,6), which uses fourth and sixth-order spatial differences, respectively, have certain issues such that the Courant conditions are more restricted and that numerical errors arise in the time-development equations including current sources. In this study, FDTD(2,6) is improved by introducing higher-degree spatial difference terms including Laplacian operators (Sekido+ 2024). This present method successfully relaxes Courant conditions and reduces numerical oscillations. Furthermore, numerical errors from current densities in FDTD(2,6) are suppressing by introducing correction terms to the time-development equations.