In 2D magnetoconvection, an imposed magnetic field enlarges the traveling-roll and chaotic regimes and enables a recurrent roll-splitting mechanism tied to magnetic reconnection.
Turbulent geodynamo simulations: A leap towards Earth’s core,
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Transition to chaos in two-dimensional Rayleigh-B\'enard convection: the role of the magnetic field
In 2D magnetoconvection, an imposed magnetic field enlarges the traveling-roll and chaotic regimes and enables a recurrent roll-splitting mechanism tied to magnetic reconnection.