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Table 3
The general features of the solutions with the quasi-cylindrical rotation law. EW, PW denote equatorwards, polewards respectively for Bφ migration in a near-surface layer.
| Model | iα | m | Notes |
|
|
|||
| 1c | 3 | 2 | strong EW at low latitudes, no high latitude features |
| 2c | 0 | 2 | strong EW at low latitudes, no high latitude features |
| 3c | 2 | 2 | strong EW at low latitudes, no high latitude features |
| 4c | 6 | 2 | strong EW at low latitudes (slightly more extended than |
| above), no high latitude features | |||
| 5c | 7 | 2 | similar to Model 4c |
| 6c | 1 | 2 | similar to Model 4c |
| 7c | 3 | 4 | similar to Model 1c |
| 8c | 0 | 4 | similar to Model 2c |
| 9c | 2 | 4 | again, low lat EW |
| 10c | 6 | 4 | similar to Model 9c |
| 11c | 7 | 4 | as Model 10c |
| 12c | 1 | 4 | as Model 10c |
| 13c | 3 | 2 | Cα > 0. PW at mid-latitudes |
| 19c | 3 | 4 | Cα > 0. PW at low latitudes |
Notes. Cα = + 11.7 > 0 in Models 13 and 19.
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