A Global Map of Average Electron Densities in the Magnetosphere of Saturn

IF 2.9 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS
Ulrich Taubenschuss, Ondřej Santolík, David Píša, Masafumi Imai, Georg Fischer, Siyuan Wu, Michiko W. Morooka, William S. Kurth
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Abstract

Measurements from the Cassini Radio and Plasma Wave Science (RPWS) experiment obtained during the entire orbital phase of the Cassini mission around Saturn (13.2 years) are processed into a meridional map of plasma densities, comprising the innermost region of the ring ionosphere, the Enceladus plasma torus, and the outer magnetosphere, up to a dipole L-shell of 30. We combine data from RPWS wave observations, such as whistler-mode waves and upper hybrid electrostatic emissions, and from the RPWS Langmuir probe when operated in the proxy mode, providing an estimate for the spacecraft potential. In the region between dipole L-shells of 2.4 and 30, observed electron densities are described by an analytic model that fits two functions, one for the water group ions and one for the protons, to observed densities across latitude on each magnetic field line. The derived electron density profiles are then augmented by a model for the cold core electron temperature as a function of L-shell to obtain a meridional map of the electrostatic potential of the ambipolar electric field. The potential is extrapolated to the inner region of the rings, i.e., to below L = 2.4 $L=2.4$ , to solve for the distribution of electron density in the ring ionosphere. A solution is based on a diffusive equilibrium model for the electrons and two ion species, and on observations from Cassini along the Saturn Orbit Insertion trajectory. A combination of analytic and diffusive equilibrium results finally yields an average global picture for the distribution of electron density in Saturn's magnetosphere.

Abstract Image

土星磁层平均电子密度的全球地图
卡西尼无线电和等离子体波科学(RPWS)实验在卡西尼环绕土星任务的整个轨道阶段(13.2年)获得的测量结果被处理成等离子体密度的子午线图,包括环电离层的最内层,土卫二等离子体环面和外层磁层,直到偶极子l壳层为30。我们结合RPWS波观测数据,如哨声模式波和上层混合静电发射,以及RPWS Langmuir探测器在代理模式下运行时的数据,提供了对航天器潜力的估计。在偶极l壳层为2.4和30之间的区域,观测到的电子密度用一个解析模型来描述,该模型将两个函数(一个用于水基团离子,一个用于质子)与每条磁力线上跨纬度观测到的密度相匹配。然后通过冷核电子温度作为l -壳层的函数的模型对导出的电子密度分布进行扩充,以获得双极电场静电势的子午图。将势外推到环内区域,即L=2.4$以下,求解环电离层中电子密度的分布。一个解决方案是基于电子和两种离子的扩散平衡模型,以及卡西尼号在土星轨道插入轨道上的观测结果。分析和扩散平衡结果的结合最终得出了土星磁层中电子密度分布的平均全局图。
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来源期刊
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
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