日本地球惑星科学連合2023年大会

講演情報

[E] オンラインポスター発表

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-EM13] Dynamics of the Inner Magnetospheric System

2023年5月23日(火) 09:00 〜 10:30 オンラインポスターZoom会場 (1) (オンラインポスター)

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)、三好 由純(名古屋大学宇宙地球環境研究所)、Theodore E Sarris(Democritus University of Thrace)、Evan G Thomas(Dartmouth College)

現地ポスター発表開催日時 (2023/5/23 17:15-18:45)

09:00 〜 10:30

[PEM13-P23] Possible roles of magnetospheric density ducts in controlling the shape of pulsating aurora and the energy of precipitating electrons

*伊藤 ゆり1細川 敬祐1小川 泰信2,5三好 由純3吹澤 瑞貴2土屋 史紀4村瀬 清華5大山 伸一郎3,2中村 紗都子3笠原 禎也6松田 昇也6笠原 慧7堀 智昭3横田 勝一郎8桂華 邦裕7篠原 育9 (1.電気通信大学、2.国立極地研究所、3.名古屋大学宇宙地球環境研究所、4.東北大学、5.総合研究大学院大学、6.金沢大学、7.東京大学、8.大阪大学、9.宇宙航空研究開発機構宇宙科学研究所)


キーワード:あらせ衛星、欧州非干渉散乱レーダー、脈動オーロラ、コーラス波動、ダクト

Auroras are classified into two broad categories: the discrete aurora, which has a distinct arc-like shape, and the diffuse aurora, which has an indistinct patchy shape. Most of the diffuse auroras are known to show a quasi-periodic luminosity modulation called pulsating aurora (PsA). Magnetospheric electrons causing PsA are generally scattered through wave-particle interactions with magnetospheric chorus waves and precipitated into the ionosphere, being referred to as “PsA electrons”. Previous studies clarified that sub-relativistic electrons originating from the radiation belt also precipitate down to lower altitudes together with PsA electrons, and strongly ionize the middle atmosphere (Miyoshi et al., 2015). Recent numerical simulations suggested that precipitations of PsA electrons having an energy of tens keV to sub-relativistic range require chorus waves to propagate to higher magnetic latitudes (MLAT) of ~20° and to resonate with trapped energetic electrons (Miyoshi et al., 2015, 2020). However, there are no actual cases of simultaneous observations of PsAs and chorus showing such propagation to high latitudes; thus, we still do not know under what conditions PsA electrons become harder and precipitate down to lower altitudes.
To reveal this issue, we have investigated a PsA event on January 12, 2021, during which simultaneous observations with the Arase satellite, ground-based all-sky imagers and the European Incoherent SCATter (EISCAT) radar were conducted. Through the analysis of the simultaneous measurements, we have tried to clarify the relationship between the morphology of PsA and the energy of PsA electrons, and then to understand what factors control the relationship. One of the main results is that, when the shape of PsA was patchy, the energy of the corresponding PsA electrons exceeded tens keV. In addition, during this interval of relatively harder precipitation, chorus wave was observed by Arase at MLAT higher than 20°. Furthermore, 1) the energy flux of scattered electrons, 2) the filling ratio of loss cone at the satellite location, and 3) the energy flux of PsA electrons estimated from EISCAT showed a reasonable correlation. On the basis of these observational results, we hypothesize that the spatial structure of PsA and the energy of PsA electrons are controlled by the existence of “density ducts,” which are tube-like regions where the electron density is lower or higher than the surrounding area. Those structures guide chorus waves along the magnetic field, allowing them to propagate to higher MLAT. In order to test this hypothesis, we compared the irregularity of the background electron density measured by Arase in the magnetosphere with the emission intensity of PsA patches at the footprint. The irregularity of ~2—18% in the electron density possibly due to the existence of ducts and the emission intensity of PsA patches show a good spatiotemporal correspondence, which supports the above-mentioned hypothesis. In the presentation, we show the observational results and discuss the factors controlling the morphology of PsA and the energy of PsA electrons.