Why Doesn't the Observed Field-Aligned Current Saturate With Increasing Interplanetary Electric Field?

被引:0
作者
Yang, Ziyi [1 ,2 ,3 ]
Zhang, Binzheng [4 ,5 ]
Lei, Jiuhou [1 ,2 ,3 ]
Lotko, William [5 ,6 ]
机构
[1] Univ Sci & Technol China, Sch Earth & Space Sci, Deep Space Explorat Lab, Hefei, Peoples R China
[2] Univ Sci & Technol China, CAS Ctr Excellence Comparat Planetol, CAS Key Lab Geospace Environm, Mengcheng Natl Geophys Observ, Hefei, Peoples R China
[3] Collaborat Innovat Ctr Astronaut Sci & Technol, Harbin, Peoples R China
[4] Univ Hong Kong, Dept Earth Sci, Hong Kong, Peoples R China
[5] Natl Ctr Atmospher Res, High Altitude Observ, Boulder, CO USA
[6] Dartmouth Coll, Thayer Sch Engn, Hanover, NH USA
基金
中国国家自然科学基金; 中国博士后科学基金; 美国国家科学基金会;
关键词
field-aligned current; magnetosphere-ionosphere coupling; CURRENT SYSTEMS; SOLAR-WIND; MAGNETIC-FIELD; MAGNETOSPHERE; IONOSPHERE; MODEL;
D O I
10.1029/2024GL110037
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Theoretical studies indicate that electric potential saturation in a polar cap ionosphere is regulated by the limited reconnection rate at the magnetopause associated with field-aligned currents (FACs), predicting the possible saturation of FACs under large interplanetary electric field (IEF). However, recent statistical studies have shown that observed FACs increase linearly with IEF. To reconcile this disparity, numerical experiments are conducted to explore the response of FACs under large IEF. Results show that FACs may exhibit either linear or saturated responses, depending on the Alfv & eacute;n Mach number. The magnetospheric closure paths of region 1 currents differ significantly between the linear and saturated conditions. In the linear case, essential parts of the region 1 current extend toward dayside and connect to the magnetopause currents, whereas these parts of currents almost disappear in the saturation state. Saturation usually occurs under sub-Alfv & eacute;nic solar wind conditions, so the observed FACs generally grow linearly with IEF.
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页数:10
相关论文
共 45 条
[1]   ENERGY-FLOW AND CLOSURE OF CURRENT SYSTEMS IN MAGNETOSPHERE [J].
ATKINSON, G .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1978, 83 (NA3) :1089-1103
[2]  
Birkeland K., 1908, NORWEGIAN AURORA POL
[3]   Changes in the Magnetic Field Topology and the Dayside/Nightside Reconnection Rates in Response to a Solar Wind Dynamic Pressure Front: A Case Study [J].
Boudouridis, A. ;
Connor, H. K. ;
Lummerzheim, D. ;
Ridley, A. J. ;
Zesta, E. .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 2021, 126 (07)
[4]   Global Magnetic Reconnection During Sustained Sub-Alfvenic Solar Wind Driving [J].
Burkholder, B. L. ;
Chen, L. -J. ;
Sarantos, M. ;
Gershman, D. J. ;
Argall, M. R. ;
Chen, Y. ;
Dong, C. ;
Wilder, F. D. ;
Le Contel, O. ;
Gurram, H. .
GEOPHYSICAL RESEARCH LETTERS, 2024, 51 (06)
[5]  
Chan E., 2017, DawnDusk Asymmetries in Planetary Plasma Environments, P1, DOI [10.1002/9781119216346.ch1, DOI 10.1002/9781119216346.CH1]
[6]  
Chapman S., 1931, Terrestrial Magnetism and Atmospheric Electricity, V36, P171, DOI [DOI 10.1029/TE036I003P00171, 10.1029/TE036i002p00077, DOI 10.1029/TE036I002P00077, 10.1029/TE036i003p00171]
[7]  
Cowley SWH, 2000, GEOPH MONOG SERIES, V118, P91
[8]   The magnitudes of the regions 1 and 2 Birkeland currents observed by AMPERE and their role in solar wind-magnetosphere-ionosphere coupling [J].
Coxon, J. C. ;
Milan, S. E. ;
Clausen, L. B. N. ;
Anderson, B. J. ;
Korth, H. .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 2014, 119 (12) :9804-9815
[9]   FIELD-ALIGNED CURRENTS IN MAGNETOSPHERE [J].
CUMMINGS, WD ;
DESSLER, AJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1967, 72 (03) :1007-&
[10]   INTERPLANETARY MAGNETIC FIELD AND AURORAL ZONES [J].
DUNGEY, JW .
PHYSICAL REVIEW LETTERS, 1961, 6 (02) :47-&