Structure, dynamics, and seasonal variability of the Mars-solar wind interaction: MAVEN Solar Wind Ion Analyzer in-flight performance and science results

被引:228
作者
Halekas, J. S. [1 ]
Ruhunusiri, S. [1 ]
Harada, Y. [2 ]
Collinson, G. [3 ]
Mitchell, D. L. [2 ]
Mazelle, C. [4 ]
McFadden, J. P. [2 ]
Connerney, J. E. P. [3 ]
Espley, J. R. [3 ]
Eparvier, F. [5 ]
Luhmann, J. G. [2 ]
Jakosky, B. M. [5 ]
机构
[1] Univ Iowa, Dept Phys & Astron, Iowa City, IA USA
[2] Univ Calif Berkeley, Space Sci Lab, Berkeley, CA USA
[3] NASA, Goddard Space Flight Ctr, Greenbelt, MD USA
[4] Inst Rech Astrophys & Planetol, Toulouse, France
[5] Univ Colorado Boulder, Lab Atmospher & Space Phys, Boulder, CO USA
关键词
Mars; solar wind; QUASI-PARALLEL SHOCKS; HOT FLOW ANOMALIES; DIAMAGNETIC CAVITIES UPSTREAM; AMPLITUDE MAGNETIC-STRUCTURES; MARTIAN BOW SHOCK; PILE-UP BOUNDARY; GLOBAL-SURVEYOR; CROSS-HELICITY; ALFVEN WAVES; PICKUP IONS;
D O I
10.1002/2016JA023167
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We report on the in-flight performance of the Solar Wind Ion Analyzer (SWIA) and observations of the Mars-solar wind interaction made during the Mars Atmosphere and Volatile EvolutioN (MAVEN) prime mission and a portion of its extended mission, covering 0.85 Martian years. We describe the data products returned by SWIA and discuss the proper handling of measurements made with different mechanical attenuator states and telemetry modes, and the effects of penetrating and scattered backgrounds, limited phase space coverage, and multi-ion populations on SWIA observations. SWIA directly measures solar wind protons and alpha particles upstream from Mars. SWIA also provides proxy measurements of solar wind and neutral densities based on products of charge exchange between the solar wind and the hydrogen corona. Together, upstream and proxy observations provide a complete record of the solar wind experienced by Mars, enabling organization of the structure, dynamics, and ion escape from the magnetosphere. We observe an interaction that varies with season and solar wind conditions. Solar wind dynamic pressure, Mach number, and extreme ultraviolet flux all affect the bow shock location. We confirm the occurrence of order-of-magnitude seasonal variations of the hydrogen corona. We find that solar wind Alfven waves, which provide an additional energy input to Mars, vary over the mission. At most times, only weak mass loading occurs upstream from the bow shock. However, during periods with near-radial interplanetary magnetic fields, structures consistent with Short Large Amplitude Magnetic Structures and their wakes form upstream, dramatically reconfiguring the Martian bow shock and magnetosphere.
引用
收藏
页码:547 / 578
页数:32
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