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Table 2.

Rotational inversion results for different synthetic observations using ρ and χdip2 as metrics simultaneously.

Name Ωcore/(2π) σrand σref Ωenv/(2π) σrand σref ρthresh χdip, thresh2 Grid
Input 750 100
M = 1 M 749 13 5 98 14 8 0.98 500 M, αMLT
M = 1 M 752 14 4 91 15 8 0.95 500 M
[Fe/H]= − 0.1 dex 744 14 7 105 16 11 0.98 500 M, αMLT
[Fe/H]= + 0.1 dex 748 14 6 103 14 13 0.98 500 M, αMLT
Δν = 9 μHz 746 17 4 107 22 7 0.98 100 M, αMLT
Δν = 9 μHz 745 17 4 112 22 11 0.95 100 M
αMLT = 1.5 751 14 3 93 22 7 0.98 500 M, αMLT
αMLT = 1.65 746 15 8 107 18 12 0.98 500 M, αMLT
αMLT = 1.7 746 15 7 101 16 11 0.98 500 M, αMLT
M = 1.3 M 751 13 4 94 15 12 0.95 500 M
M = 1.3 M 750 13 4 95 14 10 0.98 500 M, αMLT
M = 1.7 M 751 13 7 129 13 8 0.95 1000 M
M = 1.7 M 751 12 5 127 12 7 0.98 1000 M, αMLT
Surf. pert. 747 14 8 105 17 11 0.98 500 M, αMLT
Surf. pert., surf. corr. 748 14 6 103 16 9 0.98 500 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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