Magnetic reconnection at Uranus' magnetopause

被引:47
作者
Masters, A. [1 ,2 ]
机构
[1] Japan Aerosp Explorat Agcy, Inst Space & Astronaut Sci, Sagamihara, Kanagawa 2298510, Japan
[2] Univ London Imperial Coll Sci Technol & Med, Blackett Lab, Space & Atmospher Phys Grp, London, England
关键词
PLASMA DEPLETION LAYER; BOW SHOCK; MAGNETOSHEATH PROPERTIES; RADIATION ENVIRONMENT; SHEAR EVIDENCE; OUTER PLANETS; HOT PLASMA; FIELD; WIND; MAGNETOSPHERE;
D O I
10.1002/2014JA020077
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The magnetosphere of Uranus has barely been explored by spacecraft but is distinct from other solar system magnetospheres in many respects. Determining how this magnetosphere is coupled to the solar wind is central to understanding energy flow through the system. Here we assess how the solar wind interacts with the Uranian magnetosphere via magnetic reconnection. Analytical models of conditions at the magnetopause are combined with current understanding of reconnection onset to predict where reconnection may occur on the boundary. The results suggest that conditions at Uranus' magnetopause are generally less favorable for reconnection than those at the magnetopause of any planet closer to the Sun, as a result of how typical solar wind parameters vary with heliocentric distance. The location of reconnection sites on the Uranian magnetopause is likely to be highly dependent on not only the interplanetary magnetic field orientation but also planetary longitude and season. Solarwind-magnetosphere coupling via magnetic reconnectionmay be stronger under near-solstice conditions than under near-equinox conditions. We discuss the typical reconnection electric field strength at Uranus' magnetopause and suggest that the typical reconnection voltage is considerably less than 40 kV. Complimentary assessments of other means of coupling to the solar wind (e. g., via a "viscous-like" interaction) are needed to establish the overall nature of solar wind-magnetosphere coupling at Uranus.
引用
收藏
页码:5520 / 5538
页数:19
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