Multiscale electrodynamics of the ionosphere‐magnetosphere system
Multiscale electrodynamics of the ionosphere‐magnetosphere system
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DOI:
10.1029/2004ja010457
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发表时间:
2004-09
影响因子:
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通讯作者:
A. Streltsov;W. Lotko
中科院分区:
文献类型:
--
作者:
A. Streltsov;W. Lotko
(1) In this paper we investigate how the parameters of the ionosphere and the low-altitude magnetosphere mediate the formation and spatiotemporal properties of small-scale, intense electromagnetic structures commonly observed by low-altitude satellites in the auroral and subauroral magnetosphere. The study is based on numerical modeling of a time-evolving, nonlinear system that describes multiscale electrodynamics of the magnetosphere-ionosphere coupled system in terms of field-aligned currents, both quasi- static and Alfvenic. Simulations show that intense electric fields and currents with a perpendicular size of 10-20 km at 120 km altitude can be generated by a large-scale, slowly evolving current system interacting with a weakly conducting ionosphere, even without a resonant cavity in the magnetosphere. These structures form in the strong gradient in the ionospheric conductivity that develops at the boundary between the large- scale upward and downward currents when the background ionospheric Pedersen conductivity, SP, is low but higher than the Alfven conductivity, SA =1 /m0vA, above the ionosphere. When SPSA the ionosphere can generate electromagnetic waves with perpendicular sizes less than 10 km. These waves can be trapped inside the cavity of the classical ionospheric Alfven resonator, and their amplitude can be significantly amplified there by the ionospheric feedback instability. INDEX TERMS: 2736 Magnetospheric Physics: Magnetosphere/ionosphere interactions; 2704 Magnetospheric Physics: Auroral phenomena (2407); 2753 Magnetospheric Physics: Numerical modeling; 2411 Ionosphere: Electric fields (2712); 2437 Ionosphere: Ionospheric dynamics; KEYWORDS: magnetosphere-ionosphere interaction, ionospheric feedback instability, field-aligned current, Alfven wave