GSTDTAP  > 气候变化
DOI10.1029/2019GL081980
Magnetic Effects of Plasma Pressure Gradients in the Upper F Region
Laundal, K. M.; Hatch, S. M.; Moretto, T.
2019-03-16
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2019
卷号46期号:5页码:2355-2363
文章类型Article
语种英语
国家Norway
英文摘要

The Swarm satellites fly at altitudes that at polar latitudes are generally assumed to only contain currents that are aligned with the local magnetic field. Therefore, disturbances along the main field direction are mainly signatures of auroral electrojet currents, with a relatively smooth structure due to the distance from the currents. Here we show that superimposed on this smooth signal is an irregular pattern of small perturbations, which are anticorrelated with the plasma density measured by the Langmuir probe. We show that the perturbations can be remarkably well reproduced by assuming they represent a jxB force, which balances the plasma pressure gradient implied by the density variations. The associated diamagnetic current, previously reported to be most important near the equator, appears to be a ubiquitous phenomenon also at polar latitudes. A spectral analysis indicates that this effect dominates magnetic field intensity variations at small-scale sizes of a few tens of kilometers.


Plain Language Summary The Swarm satellites fly at altitudes that at polar latitudes are generally assumed to only contain currents that are aligned with the local magnetic field. Therefore, disturbances in the magnetic field strength are mainly signatures of horizontal currents below the satellites. Such disturbances have a smooth structure due to the distance from the currents. Here we show that superimposed on this smooth signal is an irregular pattern of small perturbations, which are anticorrelated with the local plasma density. We show that this anticorrelation can be explained in terms of pressure balance between particles and the magnetic field. The electric currents that are associated with the magnetic field fluctuations, diamagnetic currents, have previously been reported to be most important near the equator. Our results show that they are a ubiquitous phenomenon at all latitudes and indicate that the diamagnetic effect dominates magnetic field intensity variations at small-scale sizes of a few tens of kilometers.


英文关键词polar ionosphere plasma density magnetic field fluctuations Swarm diamagnetic currents polar cap patch
领域气候变化
收录类别SCI-E
WOS记录号WOS:000462612900004
WOS关键词IONOSPHERIC CURRENTS ; CHAMP SATELLITE ; CURRENT SYSTEMS ; SWARM ; GRAVITY
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/181594
专题气候变化
作者单位Univ Bergen, Birkeland Ctr Space Sci, Bergen, Norway
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GB/T 7714
Laundal, K. M.,Hatch, S. M.,Moretto, T.. Magnetic Effects of Plasma Pressure Gradients in the Upper F Region[J]. GEOPHYSICAL RESEARCH LETTERS,2019,46(5):2355-2363.
APA Laundal, K. M.,Hatch, S. M.,&Moretto, T..(2019).Magnetic Effects of Plasma Pressure Gradients in the Upper F Region.GEOPHYSICAL RESEARCH LETTERS,46(5),2355-2363.
MLA Laundal, K. M.,et al."Magnetic Effects of Plasma Pressure Gradients in the Upper F Region".GEOPHYSICAL RESEARCH LETTERS 46.5(2019):2355-2363.
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