Issue |
A&A
Volume 682, February 2024
|
|
---|---|---|
Article Number | A62 | |
Number of page(s) | 10 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/202348186 | |
Published online | 05 February 2024 |
Impact of radial interplanetary magnetic fields on the inner coma of comet 67P/Churyumov-Gerasimenko
Hybrid simulations of the plasma environment
1
Department of Physics, Umeå University,
901 87
Umeå,
Sweden
e-mail: herbert.gunell@physics.org
2
Department of Mathematics, Physics and Electrical Engineering, Northumbria University,
Newcastle-upon-Tyne,
UK
Received:
6
October
2023
Accepted:
25
November
2023
Context. The direction of the interplanetary magnetic field determines the nature of the interaction between a Solar System object and the solar wind. For comets, it affects the formation of both a bow shock and other plasma boundaries, as well as mass-loading. Around the nucleus of a comet, there is a diamagnetic cavity, where the magnetic field is negligible. Observations by the Rosetta spacecraft have shown that, most of the time, the diamagnetic cavity is located within a solar-wind ion cavity, which is devoid of solar wind ions. However, solar wind ions have been observed inside the diamagnetic cavity on several occasions. Understanding what determines whether or not the solar wind can reach the diamagnetic cavity also advances our understanding of comet–solar wind interaction in general.
Aims. We aim to determine the influence of an interplanetary magnetic field directed radially out from the Sun – that is, parallel to the solar wind velocity – on the comet–solar wind interaction. In particular, we explore the possibility of solar wind protons entering the diamagnetic cavity under radial field conditions.
Methods. We performed global hybrid simulations of comet 67P/Churyumov-Gerasimenko using the simulation code Amitis for two different interplanetary magnetic field configurations and compared the results to observations made by the Rosetta spacecraft.
Results. We find that, when the magnetic field is parallel to the solar wind velocity, no bow shock forms and the solar wind ions are able to enter the diamagnetic cavity. A solar wind ion wake still forms further downstream in this case.
Conclusions. The solar wind can enter the diamagnetic cavity if the interplanetary magnetic field is directed radially from the Sun, and this is in agreement with observations made by instruments on board the Rosetta spacecraft.
Key words: plasmas / methods: numerical / comets: general / comets: individual: 67P/Churyumov-Gerasimenko
Note to the reader: Figure 6 was not displayed correctly. The image was rectified on 20 February 2024.
© The Authors 2024
Open Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
This article is published in open access under the Subscribe to Open model. Subscribe to A&A to support open access publication.
Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.