Martian Bow Shock Oscillations Driven by Solar Wind Variations: Simultaneous Observations From Tianwen‐1 and MAVEN

Author:

Cheng Long123ORCID,Lillis Robert2ORCID,Wang Yuming13ORCID,Mittelholz Anna4ORCID,Xu Shaosui2ORCID,Mitchell David L.2,Johnson Catherine5ORCID,Su Zhenpeng13ORCID,Halekas Jasper S.6ORCID,Langlais Benoit7ORCID,Zhang Tielong389ORCID,Wang Guoqiang9ORCID,Xiao Sudong9,Zou Zhuxuan13,Wu Zhiyong13ORCID,Chi Yutian10,Pan Zonghao13ORCID,Liu Kai13,Hao Xinjun13ORCID,Li Yiren13,Chen Manming13,Espley Jared11ORCID,Eparvier Frank12ORCID,Curry Shannon2

Affiliation:

1. Deep Space Exploration Laboratory/School of Earth and Space Sciences University of Science and Technology of China Hefei China

2. Space Sciences Laboratory University of California, Berkeley Berkeley CA USA

3. CAS Center for Excellence in Comparative Planetology/CAS Key Laboratory of Geospace Environment/Mengcheng National Geophysical Observatory University of Science and Technology of China Hefei China

4. Department of Earth and Planetary Sciences Harvard University Cambridge MA USA

5. Department of Earth, Ocean, and Atmospheric Sciences University of British Columbia Vancouver BC Canada

6. Department of Physics and Astronomy University of Iowa Iowa City IA USA

7. Laboratoire de Planétologie et Géosciences Nantes University University of Angers Le Mans Université CNRS Nantes France

8. Space Research Institute Austrian Academy of Sciences Graz Austria

9. Institute of Space Science and Applied Technology Harbin Institute of Technology Shenzhen China

10. Deep Space Exploration Laboratory Institute of Deep Space Sciences Hefei China

11. NASA Goddard Space Flight Center Greenbelt MD USA

12. Laboratory for Atmospheric and Space Physics University of Colorado Boulder CO USA

Abstract

AbstractThe Martian bow shock stands as the first defense against the solar wind and shapes the Martian magnetosphere. Previous studies showed the correlation between the Martian bow shock location and solar wind parameters. Here we present direct evidence of solar wind effects on the Martian bow shock by analyzing Tianwen‐1 and MAVEN data. We examined three cases where Tianwen‐1 data show rapid oscillations of the bow shock, while MAVEN data record changes in solar wind plasma and magnetic field. The results indicate that the bow shock is rapidly compressed and then expanded during the dynamic pressure pulse in the solar wind, and is also oscillated during the IMF rotation. The superposition of variations in multiple solar wind parameters leads to more intensive bow shock oscillation. This study emphasizes the importance of joint observations by Tianwen‐1 and MAVEN for studying the real‐time response of the Martian magnetosphere to the solar wind.

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

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