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Energetic aspects of Enceladus' magnetospheric interaction

机译:恩克拉多斯的磁性层的积极方面交互

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We present an analytical model of the Poynting flux that is generated by the interaction between the plume of Enceladus and Saturn's magnetospheric plasma. Our purpose is to analyze the influence of two key elements of Enceladus' magnetospheric interaction on the electromagnetic energy radiated away in the moon's Alfvén wings. First, the north-south asymmetry of the obstacle generates a system of hemisphere coupling currents which allows a transport of electromagnetic energy into Saturn's northern hemisphere, even if the field-aligned currents connecting to the plume are completely blocked at the non-conducting icy crust of Enceladus. Second, the presence of electron-absorbing dust grains within the plume was recently found to drastically modify the electromagnetic field configuration within Enceladus' Alfvén wings (anti-Hall effect), thereby also altering the energy flux radiated away from the interaction region. By systematically studying the impact of varying strengths of the hemisphere coupling currents and varying electron absorption fractions on the energy flux, we come to the following conclusions: (1) The integrated Poynting flux into Saturn's southern hemisphere always exceeds the integrated flux into the northern hemisphere. In particular, the power transmitted towards the south may become several orders of magnitude larger than the power transmitted towards the north. (2) The search for Enceladus' auroral footprint has so far mainly focused on Saturn's northern hemisphere. However, based on the Poynting fluxes radiated away by the interaction, detections of the footprint should occur more likely in the giant planet's southern hemisphere, if no other far-field effects play a role. (3) Electron absorption by the dust grains within the plume makes a measurable contribution to the energy flux. Key Points Analytical model of the Poynting flux in Enceladus' Alfven wings Enceladus footprint should occur more frequently in the south than in the north Electron-absorbing dust makes measurable contribution to energy budget
机译:我们现在能流密度的分析模型通量之间的相互作用产生的恩克拉多斯的羽毛和土星磁性层的等离子体。土卫二的两个关键元素的影响磁性层的电磁相互作用能量辐射在月球的阿尔芬翅膀。首先,南北不对称的障碍生成一个半球的耦合系统电流可以运输电磁能量到土星的北部半球,即使field-aligned电流连接到羽完全阻塞不导电的冰冷的土卫二的地壳。第二,electron-absorbing尘埃的存在谷物在羽最近被发现大幅修改电磁场配置在土卫二的阿尔芬翅膀(anti-Hall效应),从而也改变了能量通量辐射的相互作用地区。不同的优势半球的耦合电流和不同电子吸收分数能通量,我们来到了以下结论:(1)集成能流密度通量到土星的南半球总是超过积分通量进入北半球。向南传播可能成为一些数量级大于权力向北传播。恩克拉多斯的极光足迹迄今主要专注于土星的北半球。基于坡印亭通量辐射的相互作用,检测的足迹更有可能发生在巨行星的南部半球,如果没有其他的远场发挥影响的角色。在羽流可衡量的贡献能量流。能流密度通量在土卫二的阿尔芬翅膀恩克拉多斯足迹应该更频繁地发生在南方比北方Electron-absorbing灰尘使能源可衡量的贡献预算

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