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Table D.1.

Rotational inversion results for different synthetic observations using ρ only.

name Ωcore/(2π) σrand σref Ωenv/(2π) σrand σref ρthresh χdip, thresh2 grid
input 750 100

M = 1 M 748 13 5 98 14 8 0.98 M, αMLT

M = 1 M 751 14 6 94 15 8 0.95 M

[Fe/H]= − 0.1 dex 744 14 8 106 16 11 0.98 M, αMLT

[Fe/H]= + 0.1 dex 748 14 6 103 14 13 0.98 M, αMLT

Δν = 9 μHz 746 17 4 107 22 7 0.98 M, αMLT

Δν = 9 μHz 751 14 6 94 15 8 0.95 M

αMLT = 1.5 751 14 3 93 22 7 0.98 M, αMLT

αMLT = 1.65 746 15 8 107 18 13 0.98 M, αMLT

αMLT = 1.7 745 15 8 102 16 12 0.98 M, αMLT

M = 1.3 M 752 13 8 90 15 14 0.95 M

M = 1.3 M 750 13 6 94 14 10 0.98 M, αMLT

M = 1.7 M 747 13 9 131 14 11 0.95 M

M = 1.7 M 750 13 6 128 13 9 0.98 M, αMLT

surf. pert. 744 14 8 108 17 11 0.98 M, αMLT

surf. pert., surf. corr. 747 14 6 105 16 10 0.98 M, αMLT

Notes. The rotational inversion results are computed with the ensemble rotational inversion described in Sect. 4. All rotation rates and uncertainties given in units of nHz.

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