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DOI | 10.1029/2019GL085661 |
Turbulence-Driven Magnetic Reconnection in the Magnetosheath Downstream of a Quasi-Parallel Shock: A Three-Dimensional Global Hybrid Simulation | |
Lu Q.; Wang H.; Wang X.; Lu S.; Wang R.; Gao X.; Wang S. | |
发表日期 | 2020 |
ISSN | 0094-8276 |
卷号 | 47期号:1 |
英文摘要 | Satellite observations with high-resolution measurements have demonstrated the existence of intermittent current sheets and occurrence of magnetic reconnection in a quasi-parallel magnetosheath behind the terrestrial bow shock. In this letter, by performing a three-dimensional global hybrid simulation, we investigated the characteristics of the quasi-parallel magnetosheath of the bow shock, which is formed due to the interaction of the solar wind with the Earth's magnetosphere. Current sheets with widths of several ion inertial lengths are found to be produced in the magnetosheath after the upstream large-amplitude electromagnetic waves penetrate through the shock and are then compressed in the downstream. Magnetic reconnection consequently occurs in these current sheets, where high-speed ion flow jets are identified in the outflow region. Simultaneously, flux ropes with the extension (along the y direction) of about several Earth's radii are also observed. Our simulation shed new insight on the mechanism for the occurrence of magnetic reconnection in the quasi-parallel shocked magnetosheath. © 2020. American Geophysical Union. All Rights Reserved. |
英文关键词 | Electromagnetic waves; Magnetosphere; Plasma shock waves; Turbulence; Earth's magnetosphere; High-resolution measurements; Hybrid simulation; Magnetic reconnections; Magnetosheaths; Quasi-parallel shock; Satellite observations; Terrestrial bow shock; Magnetism; electromagnetic wave; magnetosphere; outflow; simulation; solar wind; three-dimensional modeling; turbulence |
语种 | 英语 |
来源期刊 | Geophysical Research Letters |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/170852 |
作者单位 | CAS Key Lab of Geospace Environment, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China; CAS Center for Excellence in Comparative Planetology, Hefei, China; Physics Department, Auburn University, Auburn, AL, United States; Department of Earth, Planetary, and Space Sciences, and Institute of Geophysics and Planetary Physics, University of California, Los Angeles, CA, United States |
推荐引用方式 GB/T 7714 | Lu Q.,Wang H.,Wang X.,et al. Turbulence-Driven Magnetic Reconnection in the Magnetosheath Downstream of a Quasi-Parallel Shock: A Three-Dimensional Global Hybrid Simulation[J],2020,47(1). |
APA | Lu Q..,Wang H..,Wang X..,Lu S..,Wang R..,...&Wang S..(2020).Turbulence-Driven Magnetic Reconnection in the Magnetosheath Downstream of a Quasi-Parallel Shock: A Three-Dimensional Global Hybrid Simulation.Geophysical Research Letters,47(1). |
MLA | Lu Q.,et al."Turbulence-Driven Magnetic Reconnection in the Magnetosheath Downstream of a Quasi-Parallel Shock: A Three-Dimensional Global Hybrid Simulation".Geophysical Research Letters 47.1(2020). |
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