arXivDaily arXiv每日学术速递 周一至周五更新
北美退伍军人节(Veterans Day),12 日无更新
arXiv 1802.07955physics.space-ph
收藏

与磁层导体相连的全球电离层导体的二维模型

2-D model of the global ionospheric conductor connected with the magnetospheric conductors

Valery V. Denisenko

摘要:

设计了电离层全球导体模型。电离层导体被认为是在一个二维近似的基础上,在磁场的方向上的高电导率的框架。在这个假设下,磁场线是等势的,它们之间的电荷转移仅由积分的Pedersen和Hall电导率决定。该模型被构造为三维电导率问题解的小参数展开的第一近似。小参数是Pedersen电导率和场向电导率的比率。用经验模型IRI、MSISE、IGRF计算了Pedersen和Hall电导率的空间分布,并应用于构造积分电导率图。分析了磁层中高电导率穿过磁场线的部分,即尖点和等离子体层。结果表明,这些磁层导体的平行连接到电离层的极光带等电位区。因此,对于电离层电场,其中发电机位于电离层或在大气中,电导率的全球问题被分成三个独立的边值问题在三个区域:两个极冠和电离层的主要部分,其中包括电离层的中纬度和低纬度的部分。该模型可用于分析全球电路的电离层部分,计算电离层发电机电场,并作为更复杂的电离层和磁层模型的一部分。

英文摘要:

A model of the ionospheric global conductor is designed. The ionospheric conductor is considered in the framework of a two-dimensional approximation based on high conductivity in the direction of the magnetic field. Under this assumption the magnetic field lines are equipotential, and the charge transfer between them is determined only by integral Pedersen and Hall conductivities. The model is constructed as the first approximation in the small parameter expansion of the solution of the three-dimensional problems of electrical conductivity. The small parameter is the ratio of Pedersen and field-aligned conductivities. The space distributions of the Pedersen and Hall conductivities are calculated using the empirical models IRI, MSISE, IGRF and applied to construct the maps of the integral conductivities. The parts of the magnetosphere with high conductivity across the magnetic field lines, namely, the cusps and the plasma layer are analyzed. It is shown that the connection of these magnetospheric conductors to the ionosphere in parallel makes the auroral zones equipotential regions. As a consequence, for the ionospheric electric fields, which generators are located in the ionosphere or in the atmosphere, the global problem of electrical conductivity is separated into three independent boundary value problems in three regions: two polar caps and the main part of the ionosphere which includes the mid- and low-latitude parts of the ionosphere. The model can be used for the analysis of the ionospheric part of the Global Electric Circuit, for calculation of the ionospheric dynamo electric field and as a fragment in more complex ionospheric and magnetospheric models.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

↑