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Table 1

Magnetic quantities derived from the set of magnetic maps.

Frac. year Timespan Blong Bmean Pol. en. Dipole Quad. Oct. Axi. Ωeq
(2000+) (d) (G) (G) (% tot) (% pol) (% pol) (% pol) (% tot) (rad d-1) (rad d-1)

07.5872 14.99 10 8.7 ± 7.1 69 ± 27 17 ± 3 71 ± 2 13 ± 1 9 ± 1 83 ± 3 4.8
08.0881 28.04 19 4.6 ± 3.1 30 ± 8 58 ± 6 41 ± 7 15 ± 1 15 ± 2 56 ± 1 1.13 ± 0.01 0.38 ± 0.02 1.78
09.4572 38.02 13 8.3 ± 6.4 47 ± 11 35 ± 9 41 ± 7 20 ± 1 19 ± 3 69 ± 3 1.27 ± 0.01 0.57 ± 0.03 1.37
10.0403 61.85 9 4.1 ± 5.3 38 ± 9 32 ± 9 29 ± 20 9 ± 1 8 ± 1 29 ± 6 1.3
10.4795 37.98 10 8.6 ± 3.9 36 ± 12 62 ± 2 50 ± 6 13 ± 3 7 ± 2 43 ± 8 1.055 ± 0.005 0.67 ± 0.01 2.5
10.5945 23.93 9 11.2 ± 4.2 46 ± 17 13 ± 6 48 ± 14 18 ± 4 13 ± 4 95 ± 1 1.09 ± 0.03 0.27 ± 0.05 1.64
11.0657 17.99 7 8.4 ± 3.1 43 ± 20 18 ± 4 77 ± 3 14 ± 1 4 ± 3 85 ± 2 2.19

Notes. As a function of the mean fractional year of each run, we list the timespan of successive data sets, the number of available rotation phases, the average longitudinal field (with its associated dispersion), the mean unsigned magnetic field strength (Bmean), the fraction of the large-scale magnetic energy reconstructed in the poloidal field component, the fraction of the poloidal magnetic energy in the dipolar ( = 1), quadrupolar ( = 2), and octopolar ( = 3) components, and the fraction of energy stored in the axisymmetric component (m = 0). We then list the differential rotation parameters Ωeq and dΩ and the of the magnetic models. Error bars on the ZDI magnetic quantities are derived using the method of Petit et al. (2008).

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