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arXiv 2402.07421astro-ph.SR
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太阳自转近表面剪切层的起源

Origin of the Near-Surface Shear Layer of Solar Rotation

Leonid Kitchatinov

AI总结:

本文研究太阳自转近表面剪切层的起源,指出其旋转状态源于近表面对流特征时间短于自转周期及对流湍流径向各向异性,平均场流体动力学解析推导与数值实验均验证了该机制,且该层为太阳发电机的全球子午流提供来源。

摘要:

日震学揭示了在薄(约30 Mm)的近表面层中,自转速率随深度增加而上升。该层的归一化旋转剪切与纬度无关。这种旋转状态被证明是近表面对流特征时间短于自转周期以及对流湍流径向各向异性的结果。平均场流体动力学内的解析推导重现了观测到的归一化旋转剪切,并与太阳对流辐射流体动力学的数值实验相一致。近表面剪切层是对太阳发电机至关重要的全球子午流的来源。

英文摘要:

Helioseismology has revealed an increase in the rotation rate with depth in a thin ($\sim$30 Mm) near-surface layer. The normalized rotational shear in this layer is independent of latitude. This rotational state is shown to be a consequence of the short characteristic time of near-surface convection compared to the rotation period, and the radial anisotropy of the convective turbulence. Analytical derivations within mean-field hydrodynamics reproduce the observed normalized rotational shear and are in agreement with numerical experiments on the radiative hydrodynamics of solar convection. The near-surface shear layer is the source of the global meridional flow important for the solar dynamo.

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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