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Table 2

Summary of the diagnostic quantities of Runs A–E.

Run P1 [yr] (N) P2 [yr] (N) P1 [yr] (S) P2 [yr] (S) Beq [G] Pasym

A 2.96 ± 0.22 4.04 ± 0.70 2.85 ± 0.25 4.05 ± 0.24 3931 11 412 0.119 0.066 0.052 12.1 92.4 no
B 5.45 ± 0.20 7.88 ± 0.57 6.5 ± 1.5 8.7 ± 1.4 2956 11 339 0.068 0.038 0.030 16.1 114.8 no
BC 10.6 ± 0.33 10.8 ± 0.66 2724 11 150 0.060 0.033 0.026 no
C 7.0 ± 1.1 1789 10 686 0.028 0.017 0.012 37.6 36.9 yes
D 6.9 ± 1.1 9.4 ± 1.3 3152 9220 0.120 0.064 0.053 2.2 1.2 yes
E 4.49 ± 0.38 2.60 ± 0.67 2.58 ± 0.88 3472 8792 0.156 0.080 0.076 1.9 2.2 yes

Notes. Here, Emag = ⟨ B2 ⟩ /2μ0 is the total magnetic energy, and are the poloidal and toroidal components of the energy of the azimuthally averaged magnetic field. All quantities are averaged over volume and in time over the thermally relaxed state. The last two columns show the ratios of the meridional circulation and rotational energies from hydrodynamic to the magnetic simulations.The first four columns list the candidate periods detected with the D2 statistics separately for the northern and southern hemispheres. In a multi-periodic case, the boldface font indicates the most significant period. The last column marks cycle period asymmetry between the two hemispheres.

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