The Day the Solar Wind Disappeared at Mars

被引:8
作者
Halekas, J. S. [1 ]
Shaver, S. [2 ]
Azari, A. R. [3 ]
Fowler, C. M. [4 ]
Ma, Y. [5 ]
Xu, S. [3 ]
Andersson, L. [2 ]
Bertucci, C. [6 ]
Curry, S. M. [3 ]
Dong, C. [7 ]
Dong, Y. [2 ]
Fang, X. [2 ]
Garnier, P. [8 ]
Hanley, K. G. [3 ]
Hara, T. [3 ]
Howard, S. K. [9 ,10 ]
Hughes, A. [9 ]
Lillis, R. J. [3 ]
Lee, C. O. [3 ]
Luhmann, J. G. [3 ]
Madanian, H. [2 ]
Marquette, M. [3 ]
Mazelle, C. [8 ]
McFadden, J. P. [3 ]
Meziane, K. [11 ]
Mitchell, D. L. [3 ]
Rahmati, A. [3 ]
Reed, W. [2 ]
Romanelli, N. [9 ,12 ]
Schnepf, N. R. [2 ]
机构
[1] Univ Iowa, Dept Phys & Astron, Iowa City, IA 52245 USA
[2] Univ Colorado, Lab Atmospher & Space Phys, Boulder, CO USA
[3] Univ Calif Berkeley, Space Sci Lab, Berkeley, CA USA
[4] West Virginia Univ, Dept Phys & Astron, Morgantown, WV USA
[5] UCLA, Dept Earth Planetary & Space Sci, Los Angeles, CA USA
[6] UBA CONICET, IAFE, Buenos Aires, Argentina
[7] Boston Univ, Dept Astron, Boston, MA USA
[8] Univ Toulouse, UPS, CNRS, CNES,IRAP, Toulouse, France
[9] NASA, Goddard Space Flight Ctr, Greenbelt, MD USA
[10] Howard Univ, Dept Phys & Astron, Washington, DC USA
[11] Univ New Brunswick, Phys Dept, Fredericton, NB, Canada
[12] Univ Maryland, Dept Astron, College Pk, MD USA
基金
美国国家航空航天局;
关键词
Mars; magnetosphere; solar wind; space weather; ION COMPOSITION BOUNDARY; BOW SHOCK ENCOUNTERS; PILE-UP BOUNDARY; MAGNETIC-FIELD; GLOBAL-SURVEYOR; UNUSUAL LOCATIONS; PLASMA; VENUS; MAGNETOSHEATH; VARIABILITY;
D O I
10.1029/2023JA031935
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
In December 2022, an extremely low-density solar wind stream encountered first the Earth and then Mars, shortly after the radial alignment of the two planets (i.e., Mars opposition). As the low-density stream passed Mars, the properties of the Mars-solar wind interaction changed dramatically in response to the low solar wind Alfvenic Mach number and dynamic pressure. The Martian magnetosphere and its boundaries expanded by thousands of kilometers, extending outside of the nominal average bow shock location. The low upstream Mach number resulted in a low ratio of plasma to magnetic field pressure in the magnetosheath, allowing the formation of a very high but stable ion temperature anisotropy, together with a very low level of electromagnetic instabilities. Meanwhile, the decrease in solar wind dynamic pressure caused the Martian upper ionosphere at the terminator to transition from a magnetized state to an unmagnetized state. This event provides an opportunity to study a unique end-member state of the Mars-solar wind interaction. The solar wind consists of a supersonic flow of hot ionized gas (plasma) from the Sun that flows outward through the solar system. The solar wind interacts with planetary atmospheres and magnetic fields, which form shielded regions known as magnetospheres. The characteristics of the solar wind, including its density and speed, vary over a wide range. The shape, extent, and physical characteristics of planetary magnetospheres in turn respond to these changes in the solar wind. In this work, we study the response of the Martian magnetosphere to an extremely low-density solar wind stream. During the passage of this stream, the Martian magnetosphere expanded by thousands of kilometers, and its physical characteristics changed dramatically. This event reveals a unique outlier state for the Mars-solar wind interaction. An extremely low-density solar wind stream encountered the Earth and Mars just after Mars opposition in December 2022The Martian magnetosheath developed very unusual properties, with a low level of plasma instabilities and a high ion anisotropyThe Martian magnetosphere and its boundaries expanded by thousands of km, extending outside of the location of the nominal bow shock
引用
收藏
页数:14
相关论文
共 50 条
  • [31] Pickup Ions Measured near Mars: General Implications for the Planet of its Interaction with the Solar Wind
    McKenna-Lawlor, Susan
    PICKUP IONS THROUGHOUT THE HELIOSPHERE AND BEYOND, 2010, 1302 : 243 - 249
  • [32] Rosetta and Mars Express observations of the influence of high solar wind pressure on the Martian plasma environment
    Edberg, N. J. T.
    Auster, U.
    Barabash, S.
    Boesswetter, A.
    Brain, D. A.
    Burch, J. L.
    Carr, C. M.
    Cowley, S. W. H.
    Cupido, E.
    Duru, F.
    Eriksson, A. I.
    Fraenz, M.
    Glassmeier, K. -H.
    Goldstein, R.
    Lester, M.
    Lundin, R.
    Modolo, R.
    Nilsson, H.
    Richter, I.
    Samara, M.
    Trotignon, J. G.
    ANNALES GEOPHYSICAE, 2009, 27 (12) : 4533 - 4545
  • [33] Upstream proton cyclotron waves at Mars during the passage of solar wind stream interaction regions
    Zhao, Dan
    Guo, Jianpeng
    Lin, Haibo
    Meng, Weiduo
    He, Linxia
    Chen, Yan
    Wei, Yong
    Liu, Libo
    ASTRONOMY & ASTROPHYSICS, 2023, 674
  • [34] The solar wind plasma upstream of Mars observed by Tianwen-1: Comparison with Mars Express and MAVEN
    Fan, Kai
    Yan, Limei
    Wei, Yong
    Zhang, Aibing
    Kong, Linggao
    Franz, Markus
    He, Fei
    Chai, Lihui
    Yuan, Chongjing
    Wang, Yuqi
    Zhong, Jun
    Rong, Zhaojin
    Yao, Zhonghua
    Pan, Yongxin
    Cui, Jun
    He, Jiansen
    Li, Wenya
    Tang, Binbin
    Wang, Chi
    SCIENCE CHINA-EARTH SCIENCES, 2022, 65 (04) : 759 - 768
  • [35] The influence of crustal magnetism on the solar wind interaction with Mars: recent observations
    Crider, DH
    PLANETARY ATMOSPHERES, IONOSPHERES AND PLASMA INTERACTIONS, 2004, 33 (02): : 152 - 160
  • [36] The solar wind plasma upstream of Mars observed by Tianwen-1: Comparison with Mars Express and MAVEN
    Kai Fan
    Limei Yan
    Yong Wei
    Aibing Zhang
    Linggao Kong
    Markus Fränz
    Fei He
    Lihui Chai
    Chongjing Yuan
    Yuqi Wang
    Jun Zhong
    Zhaojin Rong
    Zhonghua Yao
    Yongxin Pan
    Jun Cui
    Jiansen He
    Wenya Li
    Binbin Tang
    Chi Wang
    Science China Earth Sciences, 2022, 65 : 759 - 768
  • [37] Pumping out the atmosphere of Mars through solar wind pressure pulses
    Edberg, N. J. T.
    Nilsson, H.
    Williams, A. O.
    Lester, M.
    Milan, S. E.
    Cowley, S. W. H.
    Franz, M.
    Barabash, S.
    Futaana, Y.
    GEOPHYSICAL RESEARCH LETTERS, 2010, 37
  • [38] The Impact and Solar Wind Proxy of the 2017 September ICME Event at Mars
    Ma, Yingjuan
    Fang, Xiaohua
    Halekas, Jasper S.
    Xu, Shaosui
    Russell, Christopher T.
    Luhmann, Janet G.
    Nagy, Andrew F.
    Toth, Gabor
    Lee, Christina O.
    Dong, Chuanfei
    Espley, Jared R.
    McFadden, James P.
    Mitchell, David L.
    Jakosky, Bruce M.
    GEOPHYSICAL RESEARCH LETTERS, 2018, 45 (15) : 7248 - 7256
  • [39] Solar wind dynamic pressure enhancements in upstream region near Mars
    Zhao, Dan
    Guo, Jianpeng
    Hong, Yichun
    Meng, Weiduo
    Huang, Hui
    Lin, Haibo
    Wang, Xianghan
    Chen, Yan
    He, Linxia
    Wei, Yong
    Liu, Libo
    ICARUS, 2023, 406
  • [40] Atmospheric Escape From Earth and Mars: Response to Solar and Solar Wind Drivers of Oxygen Escape
    Peterson, W. K.
    Brain, D. A.
    Schnepf, N. R.
    Dong, Y.
    Chamberlin, P.
    Yau, A. W.
    GEOPHYSICAL RESEARCH LETTERS, 2024, 51 (13)