Slow convection and fast rotation in crystallization-driven white dwarf dynamos
Sivan Ginzburg, Jim Fuller, Adela Kawka, Ilaria Caiazzo

TL;DR
This paper reanalyzes the dynamo mechanism in crystallizing white dwarfs, finding longer convective timescales and demonstrating that rapid rotation can sustain magnetic fields, explaining some observed white dwarf magnetism.
Contribution
It introduces revised convective timescales and dynamo scaling laws, providing a new model for magnetic field generation in crystallizing white dwarfs.
Findings
Convective turnover times are weeks to months, much longer than previously thought.
White dwarf spin periods are much shorter than convective timescales, placing dynamos in the fast rotation regime.
The model explains some observed magnetic fields in white dwarfs, especially in those spun-up in binaries.
Abstract
It has been recently suggested that white dwarfs generate magnetic fields in a process analogous to the Earth. The crystallization of the core creates a compositional inversion that drives convection, and combined with rotation, this can sustain a magnetic dynamo. We reanalyse the dynamo mechanism, arising from the slow crystallization of the core, and find convective turnover times of weeks to months - longer by orders of magnitude than previously thought. With white dwarf spin periods , crystallization-driven dynamos are almost always in the fast rotating regime, where the magnetic field is at least in equipartition with the convective motion and is possibly further enhanced by a factor of , depending on the assumed dynamo scaling law. We track the growth of the crystallized core using MESA and compute the magnetic…
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