Velocity of magnetic holes in the solar wind from Cluster multipoint measurements

IF 1.7 4区 地球科学 Q3 ASTRONOMY & ASTROPHYSICS
H. Trollvik, T. Karlsson, S. Raptis
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引用次数: 0

Abstract

Abstract. We present the first statistical study on the velocity of magnetic holes (MHs) in the solar wind. Magnetic holes are localized depressions of the magnetic field, often divided into two classes: rotational and linear MHs. We have conducted a timing analysis of observations of MHs from the Cluster mission in the first quarter of 2005. In total, 69 events were used; out of these, there were 40 linear and 29 rotational MHs, where the limit of magnetic field rotation was set to 50∘. The resulting median velocity was 7.4 ± 45 and 25 ± 42 km s−1 for linear and rotational MHs, respectively. For both classes, around 70 % of the events had a velocity in the solar wind frame that was lower than the Alfvén velocity. Therefore, we conclude that within the observational uncertainties, both linear and rotational MHs are convected with the solar wind.
从星团多点测量太阳风中磁孔的速度
摘要我们提出了太阳风中磁孔(MHs)速度的第一个统计研究。磁孔是磁场的局部凹陷,通常分为两类:旋转磁孔和线性磁孔。我们对2005年第一季度星团任务中观测到的大质量黑洞进行了时间分析。总共使用了69个事件;其中有40个是线性的,29个是旋转的,其中磁场旋转的极限被设为50度。结果显示,线性和旋转mh的平均速度分别为7.4±45和25±42 km s−1。在这两个类别中,大约70%的事件在太阳风框架中的速度低于阿尔夫海姆的速度。因此,我们得出结论,在观测不确定性范围内,线性和旋转的大质量黑洞都与太阳风发生了对流。
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来源期刊
Annales Geophysicae
Annales Geophysicae 地学-地球科学综合
CiteScore
4.30
自引率
0.00%
发文量
42
审稿时长
2 months
期刊介绍: Annales Geophysicae (ANGEO) is a not-for-profit international multi- and inter-disciplinary scientific open-access journal in the field of solar–terrestrial and planetary sciences. ANGEO publishes original articles and short communications (letters) on research of the Sun–Earth system, including the science of space weather, solar–terrestrial plasma physics, the Earth''s ionosphere and atmosphere, the magnetosphere, and the study of planets and planetary systems, the interaction between the different spheres of a planet, and the interaction across the planetary system. Topics range from space weathering, planetary magnetic field, and planetary interior and surface dynamics to the formation and evolution of planetary systems.
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