Rotational splittings for slow to moderate rotators: Latitudinal dependency or higher order effects in \Omega?
R-M. Ouazzani, M-J. Goupil

TL;DR
This paper investigates how latitudinal differential rotation and higher order rotational effects influence seismic frequency splittings in slow to moderate rotators, proposing methods to distinguish between uniform and differential rotation profiles.
Contribution
It introduces a perturbation method up to third order for mode frequency calculations and demonstrates how to extract latitudinal shear signatures from seismic data.
Findings
Third order effects are significant at moderate rotation rates.
A method to identify latitudinal shear in rotation profiles is proposed.
Data from CoRoT targets can constrain differential rotation in stars.
Abstract
Information about the rotation rate is contained in the low frequency part of power spectra, where signatures of nonuniform surface rotation are expected, as well as in the frequency splittings induced by the internal rotation rate. We wish to figure out whether the differences between the seismic rotation period as determined by a mean rotational splitting, and the rotation period measured from the low frequency peak in the Fourier spectrum (observed for some of CoRoT's targets) can provide constraints on the rotation profile. For uniform moderate rotators,perturbative corrections to second and third order in terms of the rotation angular velocity \Omega, may mimic differential rotation. We apply our perturbation method to evaluate mode frequencies accurate up to \Omega^3 for uniform rotation. Effects of latitudinal dependence are calculated in the linear approximation. In \beta Cephei…
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