The code was run with different values of input BMRs per cycle, and the initial field was varied for each run to get a stable oscillation. The results are:
1. No. of BMRs per cycle = 7028, with a peak of 200 BMRs@5.5 yrs.
Initial field = 3.5G
The field oscillates between +2.65G and -2.55G
Difference=5.20G
2. No. of BMRs per cycle = 10722, with a peak of 300 BMRs@5.5 yrs.
Initial field = 5G
The field oscillates between +3.81G and -3.64G
Difference=7.45G
3. No. of BMRs per cycle = 14412, with a peak of 400 BMRs@5.5 yrs.
Initial field = 7G
The field oscillates between +5.31 and -5.10
Difference= 10.41G
4. No. of BMRs per cycle = 18082, with a peak of 500 BMRs@5.5 yrs.
Initial field = 10G
The field oscillates between +6.58 and -7.25
Difference=15.85G
5. No. of BMRs per cycle = 21768, with a peak of 600 BMRs@5.5yrs.
Initial field = 12G
The field oscillates between +8.66 and -8.66G
Difference=17.32G
6. No. of BMRs per cycle = 25442, with a peak of 700 BMRs@5.5yrs.
Initial field = 13.5G
The field oscillates between +10.14 and -9.75G
Difference=19.89G
Ideally, the Sun's peak magnetic field near the poles has a magnitude of about 10G. So, keeping the separation between 2 spots in a BMR to be minimum, so that they just grace each other, we obtain a field of about 10 G in the last case.
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