JpGU-AGU Joint Meeting 2020

講演情報

[E] 口頭発表

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-EM19] Dynamics of the Inner Magnetospheric System

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)、Aleksandr Y Ukhorskiy(Johns Hopkins University Applied Physics Laboratory)、三好 由純(名古屋大学宇宙地球環境研究所)、Lynn M Kistler(University of New Hampshire Main Campus)

[PEM19-01] Solar wind as a Source of Magnetospheric Plasma

★Invited Papers

*Robert Colby Allen1Sarah K Vines1Stefano A Livi2Don G Mitchell1Chris P Paranicas1Kareem Sorathia1Sam Bingham1 (1.Johns Hopkins University Applied Physics Laboratory、2.Southwest Research Institute)

キーワード:Plasma, Composition, Magnetosphere

Understanding the sources and subsequent evolution of plasma within a planetary magnetosphere holds intrinsic importance for magnetospheric dynamics. For example, the balance of endogenic and solar wind plasma can be used to study the relative importance of different solar wind-magnetosphere interactions (e.g., magnetic reconnection versus Kelvin-Helmholtz instabilities) as a source of magnetospheric plasma, which can provide insight into the properties and evolution of certain planetary magnetospheres. Recent observational studies have utilized ion charge state composition to determine when and where solar wind ion populations can access a magnetosphere. These populations have subsequently been observed within injection events, bringing these solar wind-originating particles to within geosychronous orbit. Additionally, recent global modeling of the Earth system has explored the various possible pathways of solar wind entry through the use of test particle simulations. Together these studies have found that solar wind-originating plasma enters the magnetosphere through both magnetic reconnection and Kelvin-Helmholtz instabilities, as well as through cusp dynamics, and can subsequently reach the inner magnetospheric region. This presentation will focus on observational and modelling results investigating these pathways of solar wind access to the magnetosphere, and the resulting effect on magnetospheric ion composition in the inner magnetosphere.