日本地球惑星科学連合2022年大会

講演情報

[E] ポスター発表

セッション記号 P (宇宙惑星科学) » P-EM 太陽地球系科学・宇宙電磁気学・宇宙環境

[P-EM11] Dynamics of the Inner Magnetospheric System

2022年6月1日(水) 11:00 〜 13:00 オンラインポスターZoom会場 (3) (Ch.03)

コンビーナ:桂華 邦裕(東京大学大学院理学系研究科地球惑星科学専攻)、コンビーナ:三好 由純(名古屋大学宇宙地球環境研究所)、Blum Lauren W(University of Colorado Boulder)、コンビーナ:Shprits Yuri(Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences)、座長:桂華 邦裕(東京大学大学院理学系研究科地球惑星科学専攻)


11:00 〜 13:00

[PEM11-P08] Are Pi2 pulsations an oscillating motion of field line dipolarization?

*坂 翁介1、Klimushkin Dmitri2 (1.オフィス ジオフィジク、2.Institute of Solar Terrestrial Physics)

キーワード:Pi2型地磁気脈動、磁場双極化、ポロイダル的振動モード

Dawn-dusk flow shears in the nightside magnetosphere associated with field line dipolarization produce tangential discontinuities in the midnight sector and the KH instability generate periodic displacement of the discontinuity surface at Pi2 cadence [Saka et al., 2010].
Wave polarizations of Pi2 pulsations thus produced in the magnetosphere by the boundary displacement are generally reversed in the polar ionosphere [Saka et al., 2012]. The polarization reversal cannot be understood through the reconfiguration of geomagnetic field lines in terms of the fundamental harmonics in the meridian planes but rather by considering the third harmonics. We show that the field line deformations associated with third harmonics matched those of field line dipolarization. The dipolarization as well as Pi2 pulsations are a result of field-aligned propagation of poloidal wave (guided poloidal mode [Radoski, 1967]) that rotated the field lines in the meridian plane.

References
Radoski, H., Highly asymmetric MHD resonances: the guided poloidal mode, J. Geophys. Res., 72, 4026, 1967.

Saka,O., Hayashi, K., and Thomsen, M., First 10 min intervals of Pi2 onset at geosynchronous altitudes during the expansion of energetic ion regions in the nighttime sector, J. Atmos. Solar Terr. Phys., 72, 1100, 2010.

Saka, O., K. Hayashi, and D. Koga, Excitation of the third harmonic mode in meridian planes for Pi2 in the auroral zone. J. Geophys. Res., 117, A12215, doi:10.1029/2012JA018003, 2012.