A statistical survey on the magnetic field distribution in Mercury's magnetotail current sheet based on MESSENGER observations
Ding Yuan1,2; Rong ZhaoJin1,2,3
刊名CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
2018-02-01
卷号61期号:2页码:411-422
关键词Mercury Magnetosphere Magnetotail current sheet Dawn-dusk asymmetry
ISSN号0001-5733
DOI10.6038/cjg2018L0225
文献子类Article
英文摘要In this study, we use the magnetic field data measured by MESSENGER from 2011 to 2015 to survey the average magnetic field distribution in Mercury's magnetotail current sheet. It is found that the tail current sheet coincidently lies in the magnetic equator plane due to the ignorable dipole tilt angle (<3 degrees). The magnetic field B-z component is much larger than the B-y component at the current sheet center, which suggests that the field structure is almost vertical to the equatorial plane. In comparison with the region closer to Mercury (-1.5R(M)>X>2.ORM), at the distant region (-2.0R(M)>X>-2.5R(M)) the magnetic field strength B-min as well as the B-z component are weaker, B-y component is stronger, while the signature of negative B-z tends to appear there. Thus, the distant current sheet (-2.0R(M)>X>-2. 5R(M)) is more dynamic than the closer current sheet. The distributions of B-min as well as the B-z show evident dawn-dusk asymmetry, e. B-min and B-z are relatively weaker duskward within the azimuthal angle 1200-1900 where the data points of weaker B-z(B-z <5 nT) also show higher occurrence probability. In contrast, the strong By component (vertical bar By vertical bar>5 nT) at the current sheet tends to appear at the dawnward region (Y<0). In addition, the statistical study shows that the B-y component does not have a significant correlation with the B-y, component of interplanetary magnetic field. By comparison with the Earth's magnetotail current sheet, the mechanisms to control the dawn-dusk asymmetry of magnetic field at Mercury's tail current sheet are discussed.
WOS关键词CLUSTER OBSERVATIONS ; X-LINE ; GEOTAIL ; MAGNETOSPHERE ; RECONNECTION ; MAGNETOPAUSE ; MODEL ; TAIL ; PENETRATION ; INSTRUMENT
WOS研究方向Geochemistry & Geophysics
语种英语
出版者SCIENCE PRESS
WOS记录号WOS:000425840900002
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/82898]  
专题中国科学院地质与地球物理研究所
通讯作者Rong ZhaoJin
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
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Ding Yuan,Rong ZhaoJin. A statistical survey on the magnetic field distribution in Mercury's magnetotail current sheet based on MESSENGER observations[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2018,61(2):411-422.
APA Ding Yuan,&Rong ZhaoJin.(2018).A statistical survey on the magnetic field distribution in Mercury's magnetotail current sheet based on MESSENGER observations.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,61(2),411-422.
MLA Ding Yuan,et al."A statistical survey on the magnetic field distribution in Mercury's magnetotail current sheet based on MESSENGER observations".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 61.2(2018):411-422.
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