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Table 6.

Best solutions obtained for different MCMC runs.

MCMC run Ω/ΩK i (in °) f (in d−1) R (in R) M (in M)
True seismic 0.3903 45.3 0.96960 1.638 1.718 467.8 2615 3.0 × 106
0.3903 ± 0.0002 45.3 ± 0.2 0.96960 ± 0.00005 1.638 ± 0.006 1.719 ± 0.020
0.2732 ± 0.0001 86.1 ± 1.3 0.92894 ± 0.00006 1.652 ± 0.002 1.793 ± 0.007
σF = 0.01 0.3977 42.9 1.0241 1.595 1.755 468.8 1017 1.2 × 107
0.3977 ± 0.0002 42.9 ± 0.5 1.0241 ± 0.0001 1.595 ± 0.015 1.756 ± 0.049
σF = 0.05 0.2625 80.4 1.0656 1.505 1.800 412.7 2257 7.8 × 107
0.2624 ± 0.0011 82.3 ± 3.7 1.0656 ± 0.0004 1.501 ± 0.011 1.786 ± 0.041
σF = 0.05 (2017/18) 0.2599 86.0 1.0630 1.505 1.794 508.8 2017 2.8 × 107
0.2601 ± 0.0011 84.8 ± 3.2 1.0630 ± 0.0005 1.509 ± 0.009 1.809 ± 0.032
σF = 0.05 (even) 0.2742 76.5 0.9978 1.570 1.776 449.1 4723 1.3 × 108
0.2736 ± 0.0015 78.6 ± 3.6 0.9976 ± 0.0003 1.565 ± 0.015 1.758 ± 0.052
σF = 0.05 (even, 2017/18) 0.2799 79.8 0.9298 1.636 1.737 528.9 7211 9.0 × 107
0.2801 ± 0.0013 81.5 ± 3.6 0.9298 ± 0.0005 1.631 ± 0.012 1.720 ± 0.039
σF = 0.1 (even) 0.2723 89.9 0.9258 1.658 1.802 412.3 6559 6.5 × 107
0.2735 ± 0.0007 87.8 ± 1.6 0.9262 ± 0.0004 1.653 ± 0.004 1.785 ± 0.013
σF = 0.1 (even, 2017/18) 0.2723 89.2 0.9258 1.658 1.802 515.9 8049 6.2 × 107
0.2735 ± 0.0007 87.6 ± 1.6 0.9262 ± 0.0004 1.653 ± 0.004 1.785 ± 0.013

Notes. Two lines are provided for each configuration, except for the first configuration. The upper line shows the best solution (i.e., the solution that minimizes the cost function). The values given in the penultimate column have all been calculated using a frequency tolerance σF = 0.01 d−1 even if the MCMC run may have used a different value of σF. The second line gives the statistical averages and standard deviations of all of the solutions with the same mode identification as the best solution. These uncertainties therefore do not account for the dispersion resulting from other identifications, or from systematic effects that may occur as a result of limitations in the models. The third line for the first configuration corresponds to a near equator-on set of secondary solutions obtained for the first MCMC run.

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