Dynamics of the solar tachocline - III. Numerical solutions of the Gough and McIntyre model
Dynamics of the solar tachocline - III. Numerical solutions of the Gough and McIntyre model
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DOI:
10.1093/mnras/stt1065
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发表时间:
2013-09-01
影响因子:
4.8
通讯作者:
Wood, T. S.
中科院分区:
文献类型:
--
作者:
Acevedo-Arreguin, L. A.;Garaud, P.;Wood, T. S.
We present the first numerical simulations of the solar interior to exhibit a tachocline consistent with the Gough and McIntyre model. We find non-linear, axisymmetric, steady-state numerical solutions in which: (1) a large-scale primordial field is confined within the radiation zone by downwelling meridional flows that are gyroscopically pumped in the convection zone; (2) the radiation zone is in almost uniform rotation, with a rotation rate consistent with observations; (3) the bulk of the high-latitude tachocline is in thermal-wind balance, and the Lorentz force plays a negligible role in its dynamics; (4) the interaction between the field and the flows takes place within a very thin magnetic boundary layer, the tachopause, located at the bottom of the tachocline. We show that the thickness of the high-latitude tachocline scales with the amplitude of the meridional flows exactly as predicted by Gough and McIntyre. We also determine the parameter range in which such solutions can be obtained, and provide a simple explanation for the failure of previous numerical attempts at reproducing the Gough and McIntyre model. Finally, we discuss the implications of our findings for future numerical models of the solar interior, and for future observations of the Sun and other stars.