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摘要:
In general, micropulsation is generated by the free energy within the magnetosphere, which is mainly caused by the magnetosphere-solar wind interactions and/or magnetic field reconnections in the magnetospheric tail. In this article, we studied the types of low-frequency magnetospheric micropulsations Pc5 and Pc6 (1 - 6 mHz), during three magnetic storms, using ground magnetic observations. One of the main motivations of this study was to produce scientific knowledge on the subject in order to fill knowledge gaps in this region, collaborating with existing bibliographies. The data were recorded in a series of six Brazilian stations close to the Dip Equator (dip = 0), with using data from the Ascension Island observatory. Pulse trains were found to occur simultaneously with almost identical waveforms, with significant amplitude increase near magnetic local noon. Amplitude spectra showed a clear similarity in all equatorial seasons. The results obtained were compared with studies performed in regions with similar low latitudes. The possible mechanisms that induced these micropulsations and the peculiarities presented by these data were also discussed in this article.
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篇名 A Study of the Magnetospheric Micropulsations Pc5 and Pc6 Using Magnetic Stations at Low Latitude Northern Region of Brazil and Ascension Island during Magnetic Stormed Magnetospheric Plasma
来源期刊 电磁分析与应用期刊(英文) 学科 医学
关键词 Magnetospheric Micropulsations ELECTROJET EQUATORIAL Alfvén WAVES GEOMAGNETIC Storms
年,卷(期) 2019,(4) 所属期刊栏目
研究方向 页码范围 41-54
页数 14页 分类号 R73
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Magnetospheric
Micropulsations
ELECTROJET
EQUATORIAL
Alfvén
WAVES
GEOMAGNETIC
Storms
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研究分支
研究去脉
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期刊影响力
电磁分析与应用期刊(英文)
月刊
1942-0730
武汉市江夏区汤逊湖北路38号光谷总部空间
出版文献量(篇)
23
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0
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0
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