Effects of Dynamo-Generated Large-Scale Magnetic Fields on the Surface Gravity ($f$) Mode
Rajesh Mondal, Nishant K. Singh
TL;DR
The paper investigates how self-consistently generated large-scale magnetic fields beneath the solar surface affect the surface gravity ($f$) mode. Using a 3D two-layer Cartesian model with an $oldsymbol{α}^2$ dynamo in the lower layer, the authors analyze $k$–$ ext{ω}$ diagrams from the vertical velocity at the interface and fit Lorentzians to extract $f$-mode properties. They find that during the kinematic dynamo phase the $f$-mode resembles the non-magnetic case, but once the magnetic field saturates near equipartition, the $f$-mode strengthens, shifts to higher frequencies, and broadens—particularly at larger horizontal wavenumbers $k_x$. This supports observational indications of $f$-mode strengthening by subsurface magnetic fields and highlights a potential diagnostic for mapping such fields, while acknowledging limitations from the idealized isothermal bulk and high-$ ext{ℓ}$ relevance.
Abstract
By modelling the upper layers of the Sun in terms of a two-layer setup where a free-surface exists within the computational domain, we numerically study the interaction between the surface gravity, or the fundamental ($f$) mode, and the magnetic fields. Earlier such works were idealized in the sense that the static magnetic fields were imposed below the photosphere, i.e., the free-surface, to detect signatures of sub-surface magnetic fields and flows on the $f$-mode. In this work, we perform three-dimensional (3D) numerical simulations where the interior fluid below the photosphere is stirred helically at small scales, thus facilitating an $α^2$-dynamo. This allows us to investigate how these self-consistently generated large-scale magnetic fields influence the properties of the $f$-mode. We find that when the magnetic fields saturate near the equipartition values with the turbulent kinetic energy of the flow, the $f$-mode is significantly perturbed. Compared to the non-magnetic case, or the kinematic phase of the dynamo when fields are too weak, we note that the frequencies and the strengths of the $f$-mode are enhanced in presence of saturated magnetic fields, with these effects being larger at larger wavenumbers. This qualitatively confirms the earlier findings from observational and numerical works which reported the $f$-mode strengthening due to strong sub-surface magnetic fields.
