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首页> 外文期刊>Journal of the Communications Research Laboratory >Generation of Convection in the Magne-tosphere-Ionosphere Coupling System
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Generation of Convection in the Magne-tosphere-Ionosphere Coupling System

机译:磁—气层—电离层耦合系统中对流的产生

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摘要

Based on the magnetosphere-ionosphere (M-l) coupling scheme, convection as a complex (compound) system is considered including the generation of plasma population regimes in the magnetosphere. To guarantee the self-consistency, the MHD simulation is adopted to analyze the problem. In these considerations, primary elements that must be set to a self-consistent configuration are convection flows in the magnetosphere and the ionosphere, filed aligned current (FAC) systems, ionospheric currents, energy conversion processes, and plasma pressure. Then, global current systems coupled with plasma population regimes are derived from the magnetohydrodynamic (MHD) force balance controlling the convection. The magnetospheric model derived from this consideration is the closed magnetosphere with open cusp. Based on the convection model proposed in this paper, a suggestion is given for the substorm models in the next decade that they must develop from a modular model to a globally self-consistent model.
机译:基于磁层-电离层(M-1)耦合方案,对流被认为是一个复杂的(复合)系统,包括在磁层中产生等离子体种群状态。为了保证自洽性,采用MHD仿真对问题进行了分析。考虑到这些因素,必须设置为自洽配置的主要元素是磁层和电离层中的对流,场对准电流(FAC)系统,电离层电流,能量转换过程和等离子压力。然后,从控制对流的磁流体动力学(MHD)力平衡中得出与血浆填充状态耦合的全局电流系统。从这种考虑得出的磁层模型是具有尖顶的封闭磁层。基于本文提出的对流模型,对未来十年的亚暴模型提出了一个建议,即它们必须从模块化模型发展为全球自洽模型。

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