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DOI | 10.1002/2017GL076460 |
On the Collisionless Asymmetric Magnetic Reconnection Rate | |
Liu, Yi-Hsin1; Hesse, M.2,3; Cassak, P. A.4; Shay, M. A.5; Wang, S.6; Chen, L. -J.6,7 | |
2018-04-28 | |
发表期刊 | GEOPHYSICAL RESEARCH LETTERS
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ISSN | 0094-8276 |
EISSN | 1944-8007 |
出版年 | 2018 |
卷号 | 45期号:8页码:3311-3318 |
文章类型 | Article |
语种 | 英语 |
国家 | USA; Norway |
英文摘要 | A prediction of the steady state reconnection electric field in asymmetric reconnection is obtained by maximizing the reconnection rate as a function of the opening angle made by the upstream magnetic field on the weak magnetic field (magnetosheath) side. The prediction is within a factor of 2 of the widely examined asymmetric reconnection model (Cassak & Shay, 2007, https://doi.org/10.1063/1.2795630) in the collisionless limit, and they scale the same over a wide parameter regime. The previous model had the effective aspect ratio of the diffusion region as a free parameter, which simulations and observations suggest is on the order of 0.1, but the present model has no free parameters. In conjunction with the symmetric case (Liu et al., 2017, https://doi.org/10.1103/PhysRevLett.118.085101), this work further suggests that this nearly universal number 0.1, essentially the normalized fast-reconnection rate, is a geometrical factor arising from maximizing the reconnection rate within magnetohydrodynamic-scale constraints. Plain Language Summary To understand the evolution of many space and astrophysical plasmas, it is imperative to know how fast magnetic reconnection processes the magnetic flux. Researchers found that reconnection in both symmetric and asymmetric geometries exhibits a normalized reconnection rate of order 0.1. In this work, we show that this nearly universal value in asymmetric geometry is also the maximal rate allowed in the magnetohydrodynamic scale. This result has applications to the transport process at plasma boundary layers like Earth's magnetopause. |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000435745500001 |
WOS关键词 | DAYSIDE RECONNECTION ; MAGNETOPAUSE RECONNECTION ; DIFFUSION REGION ; FIELDS ; MOTION ; SHEAR |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/28176 |
专题 | 气候变化 |
作者单位 | 1.Dartmouth Coll, Dept Phys & Astron, Hanover, NH 03755 USA; 2.Univ Bergen, Dept Phys & Technol, Bergen, Norway; 3.Southwest Res Inst, San Antonio, TX USA; 4.West Virginia Univ, Dept Phys & Astron, Morgantown, WV USA; 5.Univ Delaware, Dept Phys & Astron, Newark, DE 19716 USA; 6.Univ Maryland, Dept Astron, College Pk, MD 20742 USA; 7.NASA, Goddard Space Flight Ctr, Greenbelt, MD USA |
推荐引用方式 GB/T 7714 | Liu, Yi-Hsin,Hesse, M.,Cassak, P. A.,et al. On the Collisionless Asymmetric Magnetic Reconnection Rate[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(8):3311-3318. |
APA | Liu, Yi-Hsin,Hesse, M.,Cassak, P. A.,Shay, M. A.,Wang, S.,&Chen, L. -J..(2018).On the Collisionless Asymmetric Magnetic Reconnection Rate.GEOPHYSICAL RESEARCH LETTERS,45(8),3311-3318. |
MLA | Liu, Yi-Hsin,et al."On the Collisionless Asymmetric Magnetic Reconnection Rate".GEOPHYSICAL RESEARCH LETTERS 45.8(2018):3311-3318. |
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