Effects of Force in the Martian Plasma Environment With Solar Wind Dynamic Pressure Enhancement

Author:

Song Yihui1,Lu Haoyu12ORCID,Cao Jinbin12ORCID,Li Shibang1ORCID,Yu Yiqun12,Wang Siqi1,Ge Yasong3ORCID,Zhang Xiaoxin4ORCID,Zhou Chenling1,Wang Jianxuan1

Affiliation:

1. School of Space and Environment Beihang University Beijing China

2. Key Laboratory of Space Environment Monitoring and Information Processing Ministry of Industry and Information Technology Beijing China

3. Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China

4. National Center for Space Weather China Meteorological Administration Beijing China

Abstract

AbstractDisturbed solar wind dynamic pressure is one of the important external drivers which could cause significant impacts on Martian plasma environment. In this study, a 3D multifluid multispecies numerical model is established to simulate the interaction between solar wind and Mars. Functions of electromagnetic forces applied on different ion species were analyzed. We found that the total electromagnetic force peaks near bow shock (BS) and magnetic pileup boundary (MPB) with clear asymmetry features, acting to decelerate solar wind plasma across boundary layers, and compresses heavy ions toward the planet inside the MPB. For solar wind protons, electron pressure gradient force dominates near BS and Hall electric field force dominates near MPB, controlling the location of plasma boundary. Furthermore, the morphology of motional electric field force shows clear north‐south asymmetry, leading to the formation of asymmetric structures and plasma flow in Martian space environment. The response of BS, MPB to a solar wind dynamic pressure enhancement event, as well as the effects of electromagnetic forces in this process are also investigated. After the arrival of solar wind pulse, the magnitudes of electromagnetic forces increased simultaneously to balance the enhanced solar wind dynamic pressure, while the peaks of forces moved inward with BS and MPB. The magnitudes and peaks of ion velocity in subsolar region show similar variations as well, with the greater enhancement of forces leading to the greater increase of ion velocities, indicating that the changes of forces influence boundary layers through the variation of plasma speed.

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Geophysics

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