GSTDTAP  > 气候变化
DOI10.1029/2018GL080944
Observational Evidence of Magnetic Reconnection in the Terrestrial Bow Shock Transition Region
Wang, Shan1,2; Chen, Li-Jen2; Bessho, Naoki1,2; Hesse, Michael3,4; Wilson, Lynn B., III2; Giles, Barbara2; Moore, Thomas E.2; Russell, Christopher T.5; Torbert, Roy B.6; Burch, James L.4
2019-01-28
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2019
卷号46期号:2页码:562-570
文章类型Article
语种英语
国家USA; Norway
英文摘要

We report evidence of magnetic reconnection in the transition region of the Earth's bow shock when the angle between the shock normal and the immediate upstream magnetic field is 65 degrees. An ion-skin-depth-scale current sheet exhibits the Hall current and field pattern, electron outflow jet, and enhanced energy conversion rate through the nonideal electric field, all consistent with a reconnection diffusion region close to the X-line. In the diffusion region, electrons are modulated by electromagnetic waves. An ion exhaust with energized field-aligned ions and electron parallel heating are observed in the same shock transition region. The energized ions are more separated from the inflowing ions in velocity above the current sheet than below, possibly due to the shear flow between the two inflow regions. The observation suggests that magnetic reconnection may contribute to shock energy dissipation.


Plain Language Summary Collisionless shock and magnetic reconnection are two fundamental plasma processes where significant energy conversion between electromagnetic fields and particles occurs. Knowledge is still lacking for whether reconnection occurs at the shock transition region and whether the reconnection property at the shock is different from that which occurs elsewhere. In this letter, we report the existence of reconnection at the Earth's bow shock. Many features are consistent with those in standard reconnection, such as the electron flow and field structures in the diffusion region, and the feature of ion and electron heating in the exhaust. The results suggest reconnection to be one energy dissipation mechanism at the shock, which encourages further investigation.


领域气候变化
收录类别SCI-E
WOS记录号WOS:000458607400005
WOS关键词EARTHS MAGNETOPAUSE DEPENDENCE ; INFLOW ALFVEN SPEED ; ELECTRIC-FIELD ; DYNAMICS ; VICINITY ; SHEAR ; MMS
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/26730
专题气候变化
作者单位1.Univ Maryland, Astron Dept, College Pk, MD 20742 USA;
2.NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA;
3.Univ Bergen, Dept Phys & Technol, Bergen, Norway;
4.Southwest Res Inst, San Antonio, TX USA;
5.Univ Calif Los Angeles, Dept Earth Planetary & Space Sci, Los Angeles, CA USA;
6.Univ New Hampshire, Space Sci Ctr, Durham, NH 03824 USA
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GB/T 7714
Wang, Shan,Chen, Li-Jen,Bessho, Naoki,et al. Observational Evidence of Magnetic Reconnection in the Terrestrial Bow Shock Transition Region[J]. GEOPHYSICAL RESEARCH LETTERS,2019,46(2):562-570.
APA Wang, Shan.,Chen, Li-Jen.,Bessho, Naoki.,Hesse, Michael.,Wilson, Lynn B., III.,...&Burch, James L..(2019).Observational Evidence of Magnetic Reconnection in the Terrestrial Bow Shock Transition Region.GEOPHYSICAL RESEARCH LETTERS,46(2),562-570.
MLA Wang, Shan,et al."Observational Evidence of Magnetic Reconnection in the Terrestrial Bow Shock Transition Region".GEOPHYSICAL RESEARCH LETTERS 46.2(2019):562-570.
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