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Magnetic Helicity Generation by Solar Differential Rotation
Author(s) -
C. R. DeVore
Publication year - 2000
Publication title -
the astrophysical journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.376
H-Index - 489
eISSN - 1538-4357
pISSN - 0004-637X
DOI - 10.1086/309274
Subject(s) - helicity , physics , differential rotation , magnetic helicity , astrophysics , sunspot , magnetic flux , flux (metallurgy) , solar minimum , coronal mass ejection , solar cycle 22 , heliosphere , solar rotation , interplanetary spaceflight , solar cycle , solar wind , astronomy , magnetohydrodynamics , magnetic field , solar physics , plasma , nuclear physics , stars , particle physics , quantum mechanics , materials science , metallurgy
Observations of sunspots, active regions, filaments, coronal arcades, and interplanetary magnetic clouds indicate that the Sun preferentially exhibits left-handed, negative-helicity features in its northern hemisphere, and their opposite counterparts in the south, independent of sunspot cycle. We investigate quantitatively the generation of magnetic helicity by solar differential rotation actingon emerg ed bipolar sources of flux, usinganalytical and numerical methods. We find that the vast majority of bipoles absorb negative helicity in the northern hemisphere and positive helicity in the south, in accord with observations. After two to four solar rotation periods have elapsed, the helicity generated by differential rotation amounts to about 10% of the bipole’s squared flux. Thus, each of the approximately 1 × 10, of helicity, within a factor of two of the estimates for solar production of these quantities. Evidently, differential rotation actingon emerged bipolar sources of flux can account quantitatively for the magnetic helicity balance of the Sun and the heliosphere, as well as for the observed prevalence of negative-helicity magnetic features in the north and positive-helicity features in the south. Subject headings: Sun: activity — Sun: magnetic fields — solar wind –3–

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