A comparison of small-scale magnetic fluctuations in the Region 1 and 2 field-aligned current systems

被引:5
|
作者
Wu, J. [1 ]
Bryant, M. S. [1 ]
Ridley, C. G. [2 ]
Shen, Y. [1 ]
Yang, L. [3 ]
Clausen, L. B. N. [3 ]
McWilliams, K. A. [2 ]
Murphy, K. R. [4 ]
Mann, I. R. [5 ]
Ozeke, L. G. [5 ]
Korth, H. [6 ]
Anderson, B. J. [6 ]
Waters, C. L. [7 ]
机构
[1] Univ Calgary, Dept Phys & Astron, Calgary, AB, Canada
[2] Univ Saskatchewan, Inst Space & Atmospher Studies, Saskatoon, SK, Canada
[3] Univ Oslo, Dept Phys, Oslo, Norway
[4] NASA, Goddard Space Flight Ctr, Greenbelt, MD USA
[5] Univ Alberta, Dept Phys, Edmonton, AB, Canada
[6] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD USA
[7] Univ Newcastle, Dept Phys & Math Sci, Callaghan, NSW, Australia
基金
加拿大自然科学与工程研究理事会; 美国国家科学基金会;
关键词
Field-aligned current; geomagnetic activity; reconnection; solar wind drivers; substorm; SWARM CONSTELLATION; BIRKELAND CURRENTS; MAGNETOMETER DATA; AURORAL ARCS; MAGNETOSPHERE; CUSP; IONOSPHERE; GENERATION; SATELLITE; CHAMP;
D O I
10.1002/2016JA023453
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
By determining the location and size of the Region 1 (R1) and Region 2 (R2) large-scale field-aligned currents (FACs) from Active Magnetosphere and Planetary Electrodynamics Response Experiment data, we are able to study the small-scale magnetic fluctuations observed by the Swarm satellites embedded within the large-scale FACs. A statistical comparison of R1 and R2 high-frequency fluctuations is presented in terms of different solar wind conditions and geomagnetic activities. We find that (1) the amplitude of high-frequency fluctuations in both R1 and R2 increases as the large-scale R1 and R2 FACs intensify; (2) high-frequency fluctuations in R1 peak near dayside dawn and dusk, while those in R2 peak around noon; (3) the location of the largest high-frequency fluctuations in R1 shifts in local time in response to IMF B-y, indicating a connection between the R1 fluctuation and the driving solar wind most likely explained by magnetic reconnection; and (4) high-frequency fluctuations in R2 are enhanced in a small region near local noon and respond clearly to nightside drivers, as characterized by the auroral electrojet index. Our analysis shows that the intensity of R1 and R2 high-frequency magnetic fluctuations is directly connected to the intensity of FACs, which implies that the magnetic fluctuations are closely related to the magnetospheric processes that drive them.
引用
收藏
页码:3277 / 3290
页数:14
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