Non-linear magnetic buoyancy instability and turbulent dynamo

Author:

Qazi Yasin1ORCID,Shukurov Anvar1,Tharakkal Devika12ORCID,Gent Frederick A134,Bendre Abhijit B5ORCID

Affiliation:

1. School of Mathematics, Statistics and Physics, Newcastle University , Newcastle upon Tyne, NE1 7RU , UK

2. Department of Physics, University of Helsinki , PO Box 64, FI-00014, Helsinki , Finland

3. Astroinformatics, Department of Computer Science, Aalto University , PO Box 15400, FI-00076, Espoo , Finland

4. Nordita, KTH Royal Institute of Technology and Stockholm University , Hannes Alfvéns väg 12, Stockholm, SE-106 , Sweden

5. Laboratoire d’Astrophysique, EPFL , CH-1290 Sauverny , Switzerland

Abstract

ABSTRACT Stratified discs with strong horizontal magnetic fields, are susceptible to magnetic buoyancy instability (MBI). Modifying the magnetic field and gas distributions, this can play an important role in galactic evolution. The MBI and the Parker instability, in which MBI is exacerbated by cosmic rays, are often studied using an imposed magnetic field. However, in galaxies and accretion discs, the magnetic field is continuously replenished by a large-scale dynamo action. Using non-ideal MHD equations, we model a section of the galactic disc (we neglect rotation and cosmic rays considered elsewhere), in which the large-scale field is generated by an imposed α-effect of variable intensity to explore the interplay between dynamo instability and MBI. The system evolves through three distinct phases: the linear (kinematic) dynamo stage, the onset of linear MBI when the magnetic field becomes sufficiently strong and the non-linear, statistically steady state. Non-linear effects associated with the MBI introduce oscillations which do not occur when the field is produced by the dynamo alone. The MBI initially accelerates the magnetic field amplification but the growth is quenched by the vertical motions produced by MBI. We construct a 1D model, which replicates all significant features of 3D simulations to confirm that magnetic buoyancy alone can quench the dynamo and is responsible for the magnetic field oscillations. Unlike similar results obtained with an imposed magnetic field, the non-linear interactions do not reduce the gas scale height, so the consequences of the magnetic buoyancy depend on how the magnetic field is maintained.

Funder

Ministry of Education and Culture

ERC

Swedish Research Council

Publisher

Oxford University Press (OUP)

Subject

Space and Planetary Science,Astronomy and Astrophysics

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