Foreshock ions observed behind the Martian bow shock

被引:1
作者
Frahm, R. A. [1 ]
Yamauchi, M. [2 ]
Winningham, J. D. [1 ]
Lundin, R. [2 ]
Sharber, J. R. [1 ]
Nilsson, H. [2 ]
Coates, A. J. [3 ]
机构
[1] SW Res Inst, 6220 Culebra Rd, San Antonio, TX 78228 USA
[2] Swedish Inst Space Phys, Box 98128, S-98128 Kiruna, Sweden
[3] Univ Coll London, Mullard Space Sci Lab, Holmbury St Mary, Dorking RH5 6NT, Surrey, England
基金
美国国家航空航天局; 英国科学技术设施理事会;
关键词
Foreshock; Ions; Magnetosheath; Bow shock; Mars; PHOTOELECTRON ENERGY PEAKS; SOLAR-WIND; MAGNETIC-FIELD; IMF DIRECTION; MARS; UPSTREAM; DISTRIBUTIONS; ACCELERATION; MAGNETOSHEATH; OSCILLATIONS;
D O I
10.1016/j.pss.2015.12.011
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The Mars Express Analyzer of Space Plasmas and Energetic Atoms experiment contains ion and electron instruments for conducting plasma measurements. On January 23, 2012, during in-bound travel of Mars Express in the southern hemisphere of Mars from its dawn side toward periapsis at dusk, the plasma instruments measured foreshock-like ion beams extending from outside the bow shock and into the magnetosphere, continuing to a distance of about a proton gyroradius from the bow shock. These ion beams were mostly protons, were observed to have energies greater than solar wind protons, and were not gyrating, in agreement with reflections of the solar wind proton beam. Furthermore, in the foreshock region the ion energy gradually decreased toward the magnetosheath, in agreement with an acceleration by outward-directed electric field in the bowshock. The observations also suggest that this electric field exists even inside the magnetosheath within the distance of a proton gyroradius from the bow shock. (C) 2016 The Authors. Published by Elsevier Ltd.
引用
收藏
页码:15 / 32
页数:18
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