The Energetic Oxygen Ion Beams in the Martian Magnetotail Current Sheets: Hints From the Comparisons Between Two Types of Current Sheets

Author:

Zhang Chi123ORCID,Rong Zhaojin12ORCID,Li Xinzhou12,Fränz Markus4,Nilsson Hans5ORCID,Jarvinen Riku6ORCID,Persson Moa7ORCID,Futaana Yoshifumi5ORCID,Dong Chuanfei8ORCID,Yamauchi Masatoshi5ORCID,Gao Jiawei12ORCID,Zhou Yijia12ORCID,Wang Lei12ORCID,Shi Zhen12ORCID,Wei Yong12,He Fei12ORCID,Holmström Mats5ORCID,Barabash Stas5

Affiliation:

1. Key Laboratory of Earth and Planetary Physics Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China

2. College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing China

3. Now at Center for Space Physics and Department of Astronomy Boston University Boston MA USA

4. Max‐Planck‐Institute for Solar System Research Göttingen Germany

5. Swedish Institute of Space Physics Kiruna Sweden

6. Finnish Meteorological Institute Helsinki Finland

7. Swedish Institute of Space Physics Uppsala Sweden

8. Center for Space Physics and Department of Astronomy Boston University Boston MA USA

Abstract

AbstractUsing data from the Mars Atmosphere and Volatile EvolutioN (MAVEN) mission, we explore the plasma properties of Martian magnetotail current sheets (CS), to further understand the solar wind interaction with Mars and ion escape. There are some CS exhibit energetic oxygen ions that show narrow beam structures in the energy spectrum, which primarily occurs in the hemisphere where the solar wind electric field (Esw) is directed away from the planet. On average, these CS have a higher escaping flux than that of the CS without energetic oxygen ion beams, suggesting different roles in ion escape. The CS with energetic oxygen ion beams exhibits different proton and electron properties to the CS without energetic oxygen ion beams, indicating their different origins. Our analysis suggests that the CS with energetic oxygen ion beams may result from the interaction between the penetrated solar wind and localized oxygen ion plumes.

Publisher

American Geophysical Union (AGU)

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