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The dispersal and migration of unipolar and bipolar magnetic regions on the Sun are quantitatively interpreted as a random-walk, diffusion-like process caused by supergranulation convection currents in the Sun's outer layers The time-dependent strength and sign of the polar fields are deduced approximately from the positions, fluxes, and axial tilts of the individual spot groups associated with the sunspot cycle. The well-known predominance of the preceding spot of a group is attributed to a characteristic field configuration which renders p spots relatively stable against fragmentation by the supergranulation currents The relation of the random-walk process to the solar cycle is briefly discussed, and the 11-year period is interpreted as the summation of five more-or-less distinct parts
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Robert B. Leighton (1964) studied this question.
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