Table B.1.
Azimuthally averaged angular velocity and tidal amplitude Case 4: 
= 1.8, ν = 0.1 
d−1.
| k | rmid |  |
⟨ω″⟩ | Δω″ | Δv″ |
|---|---|---|---|---|---|
| R⊙ | |———- rad d−1 ——–| | km s−1 | |||
| Day 397 | |||||
| 1 | 2.941 | 0.313 | -0.006 | 0.003 | 0.079 |
| 2 | 3.352 | 0.157 | -0.011 | 0.005 | 0.135 |
| 3 | 3.762 | 0.000 | -0.015 | 0.007 | 0.225 |
| 4 | 4.172 | -0.157 | -0.018 | 0.011 | 0.371 |
| 5 | 4.583 | -0.313 | -0.021 | 0.017 | 0.614 |
| 6 | 4.993 | -0.626 | -0.024 | 0.026 | 1.033 |
| 7 | 5.404 | -0.861 | -0.025 | 0.041 | 1.803 |
| 8 | 5.814 | -1.033 | -0.027 | 0.072 | 3.387 |
| 9 | 6.224 | -1.377 | -0.029 | 0.151 | 7.574 |
| 10 | 6.635 | -1.456 | -0.046 | 0.480 | 25.634 |
Notes. Case 4 results at Day 397. 
is the initial angular velocity of each layer in the S″ reference frame and corresponds to the 
values listed for this case in Table A.1. ⟨ω″⟩ is the average angular velocity over azimuth angle at the equator. δω″ is the peak to peak amplitude of variation over azimuth angle of the angular velocity, and Δv″ is the corresponding linear velocity. The radius listed in column 2 corresponds to the midpoint of each layer and is given is R⊙.
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