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arXiv 0708.3675astro-ph
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速跃层中太阳活动的起源

The Origin of Solar Activity in the Tachocline

Kyle P. Parfrey, Kristen Menou

摘要:

由于光球层中强磁场管的出现而产生的太阳活动区被限制在太阳赤道的35度以内。产生和更新这些磁场的发电机过程的性质,因此是太阳磁场现象的原因,还没有很好的理解。我们分析了一般场几何的太阳速跃层的磁旋转稳定性。这个辐射区和对流区之间的径向和纬度差异旋转的薄区域在37度以上的纬度是不稳定的,但在赤道附近是稳定的。我们建议,小规模的磁旋转湍流防止相干磁发电机行动的速跃层,但在赤道附近,从而解释了纬度的限制活动区。将磁力发电机与速跃层联系起来,可以阐明与太阳磁性相关的物理条件和过程。

英文摘要:

Solar active regions, produced by the emergence of tubes of strong magnetic field in the photosphere, are restricted to within 35 degrees of the solar equator. The nature of the dynamo processes that create and renew these fields, and are therefore responsible for solar magnetic phenomena, are not well understood. We analyze the magneto-rotational stability of the solar tachocline for general field geometry. This thin region of strong radial and latitudinal differential rotation, between the radiative and convective zones, is unstable at latitudes above 37 degrees, yet is stable closer to the equator. We propose that small-scale magneto-rotational turbulence prevents coherent magnetic dynamo action in the tachocline except in the vicinity of the equator, thus explaining the latitudinal restriction of active regions. Tying the magnetic dynamo to the tachocline elucidates the physical conditions and processes relevant to solar magnetism.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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