An optimal method for in-flight calibration of the fluxgate magnetometer when the total magnetic field of Alfven waves has a drift trend

被引:3
作者
Cheng ShenNan [1 ]
Wang GuoQiang [1 ]
Pan ZongHao [2 ]
Meng LiFe [3 ]
Yi Zhong [3 ]
Zhang TieLong [1 ,4 ]
机构
[1] Harbin Inst Technol, Inst Space Sci & Appl Technol, Shenzhen 518055, Peoples R China
[2] Univ Sci & Technol China, Dept Geophys & Planetary Sci, Hefei 230026, Peoples R China
[3] Beijing Inst Spacecraft Environm Engn, Beijing 100094, Peoples R China
[4] Austrian Acad Sci, Space Res Inst, A-8042 Graz, Austria
来源
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION | 2022年 / 65卷 / 05期
关键词
Fluxgate magnetometer; In-flight calibration; Alfven wave; Zero offset; CHINA; RECONNECTION; SPACECRAFT;
D O I
10.6038/cjg2022P0362
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
High-precision magnetic field measurement is of great significance for deep space exploration. However, the zero offset of the fluxgate magnetometer on the satellite will change slowly with time, which requires in-flight calibration. Recently, a new in-flight calibration method has been proposed, namely the Wang-Pan method. It is found that there is an optimal offset line with a high linearity in the offset cube for an Alfven wave, and the zero offset of magnetometer can be calculated by using the optimal offset lines of several Alfven waves. However, this method does not take into account the drifting tendency of the total magnetic field of the selected events. Based on numerical analysis, we found that the optimal offset line will be far away from the real zero offset and even no longer has a high linearity if the total magnetic field of the Alfven wave has a drift trend, which results in calculation errors. Nevertheless, the calculation error of the Wang-Pan method can be significantly reduced after removing such a drift trend. We verify this optimal method by using the magnetic field data obtained from the Venus Express. The results of this paper will be helpful for the application of the Wang-Pan method to the terrestrial magnetospheric satellites.
引用
收藏
页码:1558 / 1570
页数:13
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