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Hybrid simulations of the decay of reconnected structures downstream of the bow shock

Hybrid simulations of the decay of reconnected structures downstream of the bow shock
Hybrid simulations of the decay of reconnected structures downstream of the bow shock

Observations by Magnetospheric Multiscale have demonstrated that magnetic reconnection occurs at Earth's bow shock, typically at thin current sheets arising from plasma instabilities and turbulence in the shock transition region. Observational surveys of both the shock transition and the magnetosheath downstream suggest that the number of current sheets in these regions may not be strongly dependent on the shock Mach number MA or the angle between the upstream magnetic field and shock normal (θBn). This result is somewhat surprising given that quasi-parallel and high Mach number shocks tend to have a more disordered and non-stationary structure. In order to investigate how shock reconnection manifests across different parameters, we perform a series of hybrid (fluid electron, kinetic ion) particle-in-cell simulations across a range of Mach numbers and orientations. Given that hybrid simulations cannot resolve electron-scale current sheets and reconnection, these simulations isolate an ion-scale mechanism for shock reconnection driven by an ion-ion beam instability in the foot. We find that this mechanism is strongly constrained to quasi-parallel shocks across all simulated Mach numbers. By quantifying reconnection using the area occupied by plasma on closed magnetic field lines, we find the number of reconnecting structures and closed field area increase with MA and decrease with θBn in the upstream and ramp regions. Downstream of the shock, however, we find a similar result to observational surveys: within the subset of quasi-parallel shocks, the decay rate of the closed field area (and hence thin current sheets) is not strongly dependent on upstream shock parameters.

1070-664X
Gingell, I.
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Schwartz, S. J.
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Kucharek, H.
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Farrugia, C. J.
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Fryer, L. J.
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Plank, J.
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Trattner, K. J.
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Gingell, I.
ba7b8113-3833-40d8-a879-aab3f987455d
Schwartz, S. J.
6e89ea4b-98a3-4a7d-900e-63dd9a64cd4c
Kucharek, H.
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Farrugia, C. J.
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Fryer, L. J.
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Plank, J.
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Trattner, K. J.
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Gingell, I., Schwartz, S. J., Kucharek, H., Farrugia, C. J., Fryer, L. J., Plank, J. and Trattner, K. J. (2023) Hybrid simulations of the decay of reconnected structures downstream of the bow shock. Physics of Plasmas, 30 (1), [012902]. (doi:10.1063/5.0129084).

Record type: Article

Abstract

Observations by Magnetospheric Multiscale have demonstrated that magnetic reconnection occurs at Earth's bow shock, typically at thin current sheets arising from plasma instabilities and turbulence in the shock transition region. Observational surveys of both the shock transition and the magnetosheath downstream suggest that the number of current sheets in these regions may not be strongly dependent on the shock Mach number MA or the angle between the upstream magnetic field and shock normal (θBn). This result is somewhat surprising given that quasi-parallel and high Mach number shocks tend to have a more disordered and non-stationary structure. In order to investigate how shock reconnection manifests across different parameters, we perform a series of hybrid (fluid electron, kinetic ion) particle-in-cell simulations across a range of Mach numbers and orientations. Given that hybrid simulations cannot resolve electron-scale current sheets and reconnection, these simulations isolate an ion-scale mechanism for shock reconnection driven by an ion-ion beam instability in the foot. We find that this mechanism is strongly constrained to quasi-parallel shocks across all simulated Mach numbers. By quantifying reconnection using the area occupied by plasma on closed magnetic field lines, we find the number of reconnecting structures and closed field area increase with MA and decrease with θBn in the upstream and ramp regions. Downstream of the shock, however, we find a similar result to observational surveys: within the subset of quasi-parallel shocks, the decay rate of the closed field area (and hence thin current sheets) is not strongly dependent on upstream shock parameters.

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Accepted/In Press date: 28 November 2022
e-pub ahead of print date: 3 January 2023
Published date: January 2023
Additional Information: Funding Information: I. Gingell was supported by the Royal Society University Research Fellowship No. URF\R1\191547. This study is also supported by NASA Award No. 80NSSC19K0849. The EPOCH code used in this work was in part funded by the UK EPSRC Grant Nos. EP/G054950/1, EP/G056803/1, EP/G055165/1, EP/M022463/1, and EP/P02212X/1. The research at LASP was supported by NASA Grant Nos. NNG04EB99C, 80NSSC19K0849, and 80NSSC20K0688. L.J.F. and J.P. were supported by the UK's Science and Technology Facilities Council (STFC) through Studentship Nos. ST/T506424/1 (2279917) and ST/V507064/1 (2502298).

Identifiers

Local EPrints ID: 476931
URI: http://eprints.soton.ac.uk/id/eprint/476931
ISSN: 1070-664X
PURE UUID: 21c9c317-a51e-43f3-aefa-70b4e7530198
ORCID for I. Gingell: ORCID iD orcid.org/0000-0003-2218-1909
ORCID for L. J. Fryer: ORCID iD orcid.org/0000-0002-5215-6942

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Date deposited: 19 May 2023 16:45
Last modified: 18 Mar 2024 03:55

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Contributors

Author: I. Gingell ORCID iD
Author: S. J. Schwartz
Author: H. Kucharek
Author: C. J. Farrugia
Author: L. J. Fryer ORCID iD
Author: J. Plank
Author: K. J. Trattner

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