Table 1.
Summary of the runs in which we varied the Taylor number and latitude.
| Set | Ta (106) | Ω⋆ | AV (0° …90° ) | AH[10−3] (15° …75° ) |
|---|---|---|---|---|
| C0 | 0 | 0 | −0.54 | 0.56 |
| C02 | 0.05 | 0.02 | −0.54 | 0.73...0.57 |
| C04 | 0.15 | 0.04 | −0.54 | 0.72...0.66 |
| C06 | 0.30 | 0.06 | −0.54 | 0.16...0.32 |
| C13 | 1.40 | 0.13 | −0.54 | 0.73...0.30 |
| C24 | 4.54 | 0.24 | −0.54 ...−0.53 | 2.85...0.19 |
| C46 | 15.58 | 0.46 | −0.54 ...−0.52 | 8.84...1.41 |
| C64 | 30.54 | 0.64 | −0.54 ...−0.51 | 14.3...1.12 |
| C83 | 50.49 | 0.83 | −0.54 ...−0.50 | 20.7...1.11 |
| C1 | 75.43 | 1.01 | −0.54 ...−0.49 | 27.0...0.89 |
Notes. The grid resolution of all runs is 1443, forcing amplitudes f0 = 10−6 and f1 = 0.04, Re ≈ 13, and 
. The values of AV are shown at the equator and the pole, and the values of AH are listed at latitudes of 15° and 75°. We note that for AH, a scaling of 10−3 is applied in this table because its magnitude is much smaller than that of AV.
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