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Evidence for an oblique magnetic solar rotator D. O. Gough
Institute of Astronomy, Madingley Road, Cambridge CB3 0HA, UK
The observation by Claverie et al.
1. of fine structure in the peaks in the power spectrum of low-degree 5-min solar oscillations has been interpreted as being a result of rotational splitting. Claverie et al.
1 claim that their measurements imply that an appropriately weighted average of the interior angular velocity (r) of the Sun is about twice the value of at the surface. At first sight their claim looks doubtful, because all 2l + 1 components of the set of modes of degree l appear in the spectrum, whereas only l + 1 of them should be detectable. However, Isaak2 has recently speculated that the additional components are produced by an intense rotating magnetic core, such as had been postulated by Dicke3,4 to account for the 12.2-day periodic component in the Princeton oblateness data5−9. Isaak2 pointed out that the mean period 2 / 15 days of the solar interior that was inferred from the Birmingham data1 is consistent with a central core rotating with the 12.2-day period and an outer envelope rotating with the photosphere. Moreover, his rough estimate of a few megagauss for the r.m.s. magnetic field that is required to support his conjecture is within about a factor 10 of that required by Dicke3. Thence he concluded that the Birmingham data1 provide the first clear empirical evidence for an intense internal solar magnetic field. Here I examine this evidence in more detail, and show that the conclusion is premature. If the magnetic core does exist, the 5-min oscillations provide no clear evidence that it is rotating rapidly. Furthermore, unless one accepts a contrived magnetic-field configuration, an explanation for the 2l + 1 components of the multiplets is still lacking.
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