Differential rotation in fully convective stars
Steven A. Balbus, Nigel O. Weiss

TL;DR
This paper extends the thermal wind balance model to fully convective stars, deriving isorotation contours and applying them to various rotation profiles, aiding understanding of stellar rotation and internal structure.
Contribution
It generalizes solar rotation models to fully convective stars, providing a simple analytical framework for their isorotation contours and surface flow patterns.
Findings
Isorotation contours follow R^2 = A + BΦ(r) form.
Both solar-like and antisolar rotation profiles can be modeled.
The model aligns with numerical simulations and aids in stellar internal structure analysis.
Abstract
Under the assumption of thermal wind balance and effective entropy mixing in constant rotation surfaces, the isorotational contours of the solar convective zone may be reproduced with great fidelity. Even at this early stage of development, this helioseismology fit may be used to put a lower bound on the midlatitude {\em radial} solar entropy gradient, which in good accord with standard mixing length theory. In this paper, we generalize this solar calculation to fully convective stars (and potentially planets), retaining the assumptions of thermal wind balance and effective entropy mixing in isorotational surfaces. It is found that each isorotation contour is of the form , where is the radius from the rotation axis, is the (assumed spherical) gravitational potential, and and are constant along the contour. This result is applied to simple models…
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