The Mars orbiter magnetometer of Tianwen-1: in-flight performance and first science results

被引:18
|
作者
Wang, YuMing [1 ,2 ]
Zhang, TieLong [2 ,3 ]
Wang, GuoQiang [4 ]
Xiao, SuDong [4 ]
Zou, ZhuXuan [1 ,2 ]
Cheng, Long [1 ,2 ]
Pan, ZongHao [1 ,2 ]
Liu, Kai [1 ,2 ]
Hao, XinJun [1 ,2 ]
Li, YiRen [1 ,2 ]
Chen, ManMing [1 ,2 ]
Zhang, ZhouBin [5 ]
Yan, Wei [5 ]
Su, ZhenPeng [1 ,2 ]
Wu, ZhiYong [1 ,2 ]
Shen, ChengLong [1 ,2 ]
Chi, YuTian [6 ]
Xu, MengJiao [6 ]
Guo, JingNan [1 ,2 ]
Du, Yang [7 ]
机构
[1] Univ Sci & Technol China, Deep Space Explorat Lab, Sch Earth & Space Sci, Hefei 230026, Peoples R China
[2] Univ Sci & Technol China, CAS Ctr Excellence Comparat Planetol, CAS Key Lab Geospace Environm, Mengcheng Natl Geophys Observ, Hefei 230026, Peoples R China
[3] Austrian Acad Sci, Space Res Inst, Graz, Austria
[4] Harbin Inst Technol, Inst Space Sci & Appl Technol, Shenzhen 518055, Peoples R China
[5] Chinese Acad Sci, Natl Astron Observ, Beijing 100012, Peoples R China
[6] Inst Deep Space Sci, Deep Space Explorat Lab, Hefei 230026, Peoples R China
[7] Shanghai Inst Satellite Engn, Shanghai 201109, Peoples R China
关键词
Mars; magnetic field; Tianwen-1; magnetometer; bow shock; SOLAR-WIND; BOW SHOCK; MISSION;
D O I
10.26464/epp2023028
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Mars Orbiter MAGnetometer (MOMAG) is a scientific instrument onboard the orbiter of China's first mission for Mars - Tianwen-1. Since November 13, 2021, it has been recording magnetic field data from the solar wind to the magnetic pile-up region surrounding Mars. Here we present its in-flight performance and first science results, based on its first one and one-half months' data. Comparing these early MOMAG observations to the magnetic field data in the solar wind from NASA's Mars Atmosphere and Volatile EvolutioN (MAVEN) mission, we report that the MOMAG magnetic field data are at the same level in magnitude, and describe the same magnetic structures with similar variations in three components. We recognize 158 clear bow shock (BS) crossings in these MOMAG data; their locations match well statistically with the modeled average BS. We also identify and compare five pairs of datasets collected when Tianwen-1's orbiter and the MAVEN probe made simultaneous BS crossings. These BS crossings confirm the global shape of modeled BS, as well as the south-north asymmetry of the Martian BS. Two cases presented in this paper suggest that the BS is probably more dynamic at flank than near the nose. So far, MOMAG performs well, and provides accurate magnetic field vectors. MOMAG is continuously scanning the magnetic field surrounding Mars. Data from MOMAG's measurements complement data from MAVEN and will undoubt edly advance our understanding of the plasma environment of Mars.
引用
收藏
页码:216 / 228
页数:13
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