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Magnetic field corrections to solar oscillation frequencies

Abstract

The presence of a magnetic field both deep within the Sun and in its atmosphere raises the question of the field's influence on the p- and g-modes of oscillation and the implications for helioseismology. Observations1,2 of p-modes, in particular, have permitted a theoretical determination3 of the sound speed within the solar interior, thus providing a seismological probe of the Sun's depths. Magnetic fields within the Sun are likely to be too weak to significantly affect this determination of the sound speed. Nonetheless, magnetic fields may modify the oscillation frequencies in a distinctive fashion, thereby raising the possibility of placing limits on interior field strengths through frequency measurements4. Recently, Woodard and Noyes5 have reported a slight but systematic decrease in frequencies of low-degree p-modes from 1980 to 1984. Here we argue that the frequencies of both p- and g-modes are modified by a magnetic field. In particular, we attribute the decrease in p-mode frequencies to a magnetic field within the solar interior evolving over the solar cycle. Field strengths at the base of the convection zone of at least 5×105 G are required.

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Roberts, B., Campbell, W. Magnetic field corrections to solar oscillation frequencies. Nature 323, 603–605 (1986). https://doi.org/10.1038/323603a0

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