Japan Geoscience Union Meeting 2024

Presentation information

[E] Poster

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 5:15 PM - 6:45 PM Poster Hall (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)

5:15 PM - 6:45 PM

[PEM10-P01] Multi-spacecraft observations of the magnetosphere and ionosphere under low Alfvén Mach number solar wind

*Masaki N Nishino1, Yukinaga Miyashita2,3, Motoharu Nowada4, Yoshifumi Saito1 (1.Japan Aerospace Exploration Agency, Institute of Space and Astronautical Science, 2.Korean Astronomy and Space Science Institute, 3.Korea National University of Science and Technology, Department of Astronomy and Space Science, 4.Shandong Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment, School of Space Science and Physics, Institute of Space Sciences)

Keywords:Solar wind Alfvén Mach number, Transpolar arc, Multi-satellite observations, Magnetosphere-Ionosphere coupling

The transpolar arcs (TPAs) appear in the auroral oval under the northward interplanetary magnetic field (IMF), sometimes accompanied by the change of the BY sign. Previous statistical studies showed that the solar wind magnetic field strength or the magnetic energy does not affect the occurrence of the TPAs. On the other hand, it has not been studied if the TPAs appear similarly when the solar wind density is very low, and thus, its Alfvén Mach number (MA) is very low (~2-3). Here, we show a case study of multiple TPAs during high MA solar wind observed by DMSP satellites, which was followed by TPA occurrence during very low MA solar wind. The TPA under low MA solar wind is typically single and faint, while multiple TPAs of complicated structures appeared in some cases. In this event, ARTEMIS P1 and P2 were in the mid-distant magnetotail in the same period, and their magnetopause crossings suggest a strong distortion of the magnetotail that might be related to the shape of the TPAs. We discuss the magnetosphere-ionosphere coupling under low MA solar wind and northward IMF based on multi-spacecraft observations.