Magnetic flux concentrations from turbulent stratified convection
P. J. K\"apyl\"a (1,2,3), A. Brandenburg (3,4,5,6), N. Kleeorin (7,3),, M. J. K\"apyl\"a (1), I. Rogachevskii (7,3) ((1) ReSoLVE Center of, Excellence, Aalto, (2) University of Helsinki, (3) NORDITA, (4) Stockholm, University, (5) JILA, (6) LASP, (7) Ben-Gurion University)

TL;DR
This study investigates how turbulent stratified convection can self-organize magnetic fields into large flux concentrations, resembling sunspots, through simulations that highlight flux expulsion as a key process.
Contribution
It demonstrates that large-scale magnetic flux concentrations form via flux expulsion rather than negative effective magnetic pressure instability, with implications for sunspot formation theories.
Findings
Flux concentrations reach 3-5 kG near the surface.
Large structures up to 20 Mm form in 24 Mm deep models.
Flux growth is approximately linear over time.
Abstract
(abridged) Context: The mechanisms that cause the formation of sunspots are still unclear. Aims: We study the self-organisation of initially uniform sub-equipartition magnetic fields by highly stratified turbulent convection. Methods: We perform simulations of magnetoconvection in Cartesian domains that are - Mm deep and - Mm wide. We impose either a vertical or a horizontal uniform magnetic field in a convection-driven turbulent flow. Results: We find that super-equipartition magnetic flux concentrations are formed near the surface with domain depths of and Mm. The size of the concentrations increases as the box size increases and the largest structures ( Mm horizontally) are obtained in the 24 Mm deep models. The field strength in the concentrations is in the range of - kG. The concentrations grow approximately linearly in time. The effective…
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