中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Three-Dimensional Configuration of Induced Magnetic Fields Around Mars

文献类型:期刊论文

作者Zhang, Chi4,5,6; Rong, Zhaojin3,5,6; Klinger, Lucy2; Nilsson, Hans4; Shi, Zhen5,6; He, Fei5,6; Gao, Jiawei5,6; Li, Xinzhou5,6; Futaana, Yoshifumi4; Ramstad, Robin1
刊名JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
出版日期2022-08-01
卷号127期号:8页码:16
ISSN号2169-9097
关键词Mars induced magnetosphere magnetic fields ion escape
DOI10.1029/2022JE007334
英文摘要Using over 6 years of magnetic field data (October 2014-December 2020) collected by the Mars Atmosphere and Volatile EvolutioN, we conduct a statistical study on the three-dimensional average magnetic field structure around Mars. We find that this magnetic field structure conforms to the pattern typical of an induced magnetosphere, that is, the interplanetary magnetic field (IMF) which is carried by the solar wind and which drapes, piles up, slips around the planet, and eventually forms a tail in the wake. The draped field lines from both hemispheres along the direction of the solar wind electric field (E) are directed toward the nightside magnetic equatorial plane, indicating that they are "sinking" toward the wake. These "sinking" field lines from the +E-hemisphere (E pointing away from the plane) are more flared and dominant in the tail, while the field lines from the -E-hemisphere (E pointing toward) are more stretched and "pinched" toward the plasma sheet. Such highly "pinched" field lines even form a loop over the pole of the -E-hemisphere. The tail current sheet also shows an E-asymmetry: the sheet is thicker with a stronger tailward J -> xB -> $\overrightarrow{J}\times \overrightarrow{B}$ force at +E-flank, but much thinner and with a weaker J -> xB -> $\overrightarrow{J}\times \overrightarrow{B}$ (even turns sunward) at -E-flank. Additionally, we find that IMF B-x can induce a kink-like field structure at the boundary layer; the field strength is globally enhanced and the field lines flare less during high dynamic pressure.
WOS关键词SOLAR-WIND INTERACTION ; MARTIAN MAGNETOTAIL ; ION ESCAPE ; PLASMA ; VENUS ; ASYMMETRIES ; DEPENDENCE ; MORPHOLOGY ; PHOBOS-2 ; ANALYZER
资助项目National Natural Science Foundation of China[41922031] ; National Natural Science Foundation of China[41774188] ; Strategic Priority Research Program of Chinese Academy of Sciences[XDA17010201] ; Strategic Priority Research Program of Chinese Academy of Sciences[XDB41000000] ; Key Research Program of Chinese Academy of Sciences[ZDBS-SSW-TLC00103] ; Key Research Program of the Institute of Geology and Geophysics, CAS[IGGCAS-201904] ; Key Research Program of the Institute of Geology and Geophysics, CAS[IGGCAS-202102] ; China Scholarship Council[202104910297]
WOS研究方向Geochemistry & Geophysics
语种英语
出版者AMER GEOPHYSICAL UNION
WOS记录号WOS:000842848500001
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of Chinese Academy of Sciences ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council
源URL[http://ir.iggcas.ac.cn/handle/132A11/108439]  
专题地质与地球物理研究所_中国科学院地球与行星物理重点实验室
通讯作者Rong, Zhaojin
作者单位1.Univ Colorado, Lab Atmospher & Space Phys, Boulder, CO 80309 USA
2.Peking Univ, Beijing Int Ctr Math Res, Beijing, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Mohe Observ Geophys, Beijing Natl Observ Space Environm, Beijing, Peoples R China
4.Swedish Inst Space Phys, Kiruna, Sweden
5.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
6.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Chi,Rong, Zhaojin,Klinger, Lucy,et al. Three-Dimensional Configuration of Induced Magnetic Fields Around Mars[J]. JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS,2022,127(8):16.
APA Zhang, Chi.,Rong, Zhaojin.,Klinger, Lucy.,Nilsson, Hans.,Shi, Zhen.,...&Wei, Yong.(2022).Three-Dimensional Configuration of Induced Magnetic Fields Around Mars.JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS,127(8),16.
MLA Zhang, Chi,et al."Three-Dimensional Configuration of Induced Magnetic Fields Around Mars".JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS 127.8(2022):16.

入库方式: OAI收割

来源:地质与地球物理研究所

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