Japan Geoscience Union Meeting 2024

Presentation information

[E] Oral

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

[P-EM10] Dynamics of Magnetosphere and Ionosphere

Mon. May 27, 2024 1:45 PM - 3:00 PM Exhibition Hall Special Setting (2) (Exhibition Hall 6, Makuhari Messe)

convener:Shun Imajo(Data Analysis Center for Geomagnetism and Space Magnetism, Graduate School of Science, Kyoto University), Akimasa Ieda(Institute for Space-Earth Environmental Research, Nagoya University), Yuka Sato(Nippon Institute of Technology), Akiko Fujimoto(Kyushu Institute of Technology), Chairperson:Masakazu Watanabe(Graduate School of Science, Kyushu University), Akira Kadokura(National Institute of Polar Research)

1:45 PM - 2:00 PM

[PEM10-11] Numerical analysis on non-local and nonlinear evolution of auroral fine structures in the magnetosphere-ionosphere coupling

*Tsuyoshi Sakaki1, Tomo-Hiko Watanabe1 (1.Nagoya University)

Keywords:Aurora, Alfvén wave, Magnetosphere-ionosphere coupling system

Our previous works on the feedback instability in the magnetosphere-ionosphere (M-I) coupling system under a local approximation have revealed that the Kelvin-Helmholtz (K-H) type instability driven by enhanced E×B flow shear deforms auroral arc-like structures and leads to vortex formation followed by turbulence transition. However, global properties of the auroral growth have not been understood well except for a few basic properties of auroral arc structure formation elongated in the longitudinal direction.
In this study, we have performed a nonlinear simulation of the feedback instability in a non-local M-I coupling with the dipole field configuration to investigate nonlinear evolution of auroral fine structures by means of a novel numerical simulation code for a set of the reduced magnetohydrodynamic equations with a non-uniform kinematic viscosity in the magnetosphere and the two-fluid equations in the ionosphere. The simulation results clearly demonstrate transition to a turbulent state after convective growth of auroral fine structures and the succeeding K-H type instability. In addition, we have observed expansion of auroral turbulent structures broadening into the latitudinal directions as well as in the wave number spectrum in the nonlinear stage.