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A simple axisymmetric model of magnetosphere-ionosphere coupling currents in Jupiter's polar ionosphere

机译:一个简单的轴对称模型magnetosphere-ionosphere耦合电流在木星的极地电离层

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We propose a simple illustrative axisymmetric model of the plasma flow and currents in Jupiter's polar ionosphere which are due both to internal magnetospheric plasma processes and the solar wind interaction. The plasma flow in the model is specified using a combination of observations, previous modeling, and theory, and the ionospheric and field-aligned currents are then calculated. With increasing latitude, the model represents conditions in the inner, middle, and outer magnetosphere on closed field lines and on open field lines mapping to the tail lobes. The model allows us to address three important topics, concerned with the closure of the upward field-aligned currents flowing in the middle magnetosphere region, the energy transfers from planetary rotation to polar upper atmosphere heating and to the magnetosphere, and the relative significance of auroral processes associated with the boundary of open field lines (and hence with the solar wind interaction) and with the middle magnetosphere. It is shown in particular that the energy transfers to the polar upper atmosphere and magnetosphere are of order hundreds of TW each and that discrete auroral precipitation is expected both at the boundary of open field lines and in the middle magnetosphere, though being dominated by the latter. While the initial calculations assume for simplicity a constant ionospheric conductance, we also present a development of the model in which the conductance is self-consistently increased in regions of upward field-aligned current by the precipitation of accelerated electrons. It is shown that this feedback acts to spread the upward current in the region equatorward of the open field line boundary, thus reducing the energy flux and total power of precipitating auroral electrons in this region. At the same time it concentrates the upward current in the equatorward part of the middle magnetosphere, thereby increasing the energy flux and total power of precipitating electrons in this region.
机译:我们提出一个简单的演示轴对称等离子体流的模型和电流由于木星的极地电离层和内部磁性层的等离子体过程太阳风相互作用。指定使用的组合模型观察,以前的建模和理论,电离层和field-aligned电流然后计算。模型表示的条件内,中间,和封闭的电场线和外磁气圈在开放磁力线映射到尾叶。模型允许我们解决三个重要关心的话题,向上的关闭在中间field-aligned电流流动磁气圈区域,能量转移行星旋转到极高层大气加热和磁层,极光过程的相对重要性与开放电场线的边界(因此与太阳风相互作用)与中间磁气圈。特定的能量转移到极地高层大气和磁层数以百计的TW每个离散极光降水预计的边界开放电场线和磁层中间,虽然被后者占主导地位。最初的计算假定为简单起见常数电离层电导,我们也在场开发的模型电导是自我一贯地增加向上field-aligned当前的区域降水的加速电子。表明,这种反馈传播行为当前地区朝赤道方向的向上田野边界线,从而减少了能量流和沉淀的总功率极光电子在这个地区。时间中集中向上的电流朝赤道方向中间磁气圈的一部分,从而增加了能量流和总沉淀的电子在这个地区。

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