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Theoretical studies of penetration of magnetospheric electric fields to the ionosphere.

机译:磁层电场渗透到电离层的理论研究。

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Ionospheric disturbance electric fields of magnetospheric origin play an important role in determining the global morphology and dynamics of the ionosphere of the Earth. In this work, we present a number of numerical simulations of the transient electric fields in the middle and inner magnetosphere and the ionosphere equatorward of the auroral zone caused by idealized changes in the magnetospheric driving parameters. For these studies, we use the Rice Convection Model (RCM), a large computer code of the magnetosphere-ionosphere coupling which consistently computes the electric fields, currents, and plasma densities in the magnetosphere and the electric field and currents in the ionosphere in the quasi-static slow-flow approximation. We made substantial upgrades to the code, which include a module computing realistic solar EUV-produced ionospheric conductances and a new potential solver. Our upgraded version of the RCM also includes a time-varying magnetospheric magnetic field and a self-consistently estimated auroral zone. We first discuss numerical problems encountered in modeling electrodynamics of convection with a time-varying magnetic field, realistic ionospheric conductances, and a self-consistent auroral zone, and our solutions to those difficulties. We then present a number of "computer experiments" with the new version of the RCM with idealized changes in the magnetospheric parameters such as sudden changes in the cross polar cap potential drop, magnetic field reconfiguration corresponding to the overall changes in the high-latitude convection, as well as rotations of the electric field on the polar cap boundary. Prompt penetration ionospheric electric fields simulated with the upgraded RCM are shown to be consistent with the previous simulations. The new simulations and their results are discussed in the context of (1) possible contribution to the variability of the ionospheric electric fields, and (2) role of time-varying magnetic field on the characteristic lifetimes of prompt penetration electric fields at subauroral, middle, and low latitudes.
机译:磁层起源的电离层扰动电场在确定地球电离层的整体形态和动力学方面起着重要作用。在这项工作中,我们提供了由磁层驱动参数的理想变化引起的中,内磁层和极光区电离层赤道方向瞬态电场的许多数值模拟。对于这些研究,我们使用莱斯对流模型(RCM),这是磁层-电离层耦合的大型计算机代码,可一致地计算磁层中的电场,电流和等离子体密度以及电离层中电离层中的电场和电流。准静态慢流量近似。我们对该代码进行了重大升级,其中包括计算实际的太阳能EUV产生的电离层电导的模块和新的电势求解器。我们的RCM升级版还包括随时间变化的磁层磁场和自洽估计的极光区。我们首先讨论在对流电动力学建模中遇到的数值问题,该对流具有时变磁场,真实的电离层电导和自洽的极光区,以及我们针对这些困难的解决方案。然后,我们用新版RCM提出了许多“计算机实验”,其中磁层参数发生了理想化的变化,例如交叉极帽电位降的突然变化,对应于高纬度对流总体变化的磁场重构,以及极帽边界上的电场旋转。用升级的RCM模拟的快速穿透电离层电场显示与以前的模拟一致。在以下情况下讨论了新的模拟及其结果:(1)可能对电离层电场的变化做出的贡献,以及(2)时变磁场对耳下,中耳快速穿透电场的特征寿命的作用和低纬度地区。

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