首页> 外文期刊>The Astrophysical journal >TRANSPORT OF TOROIDAL MAGNETIC FIELD BY THE MERIDIONAL FLOW AT THE BASE OF THE SOLAR CONVECTION ZONE
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TRANSPORT OF TOROIDAL MAGNETIC FIELD BY THE MERIDIONAL FLOW AT THE BASE OF THE SOLAR CONVECTION ZONE

机译:太阳对流区底部子午流对环磁磁场的传输

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In this paper we discuss the transport of toroidal magnetic field by a weak meridional flow at the base of the convection zone. We use the differential rotation and meridional flow model developed by Rempel and incorporate feedback of a purely toroidal magnetic field in two ways: directly through the Lorentz force (magnetic tension) and indirectly through quenching of the turbulent viscosity, which affects the parameterized turbulent angular momentum transport in the model. In the case of direct Lorentz force feedback, we find that a meridional flow with an amplitude of around 2 m s~(-1) can transport a magnetic field with a strength of 20-30 kG. Quenching of turbulent viscosity leads to deflection of the meridional flow from the magnetized region and a significant reduction of the transport velocity if the magnetic field is above equipartition strength.
机译:在本文中,我们讨论了在对流区底部由弱子午流引起的环形磁场的传输。我们使用Rempel开发的微分旋转和子午流模型,并通过两种方式合并纯环形磁场的反馈:直接通过洛伦兹力(磁力)和间接通过湍流粘度的淬灭,这会影响参数化湍流角动量模型中的运输。在直接洛伦兹力反馈的情况下,我们发现子午流的振幅约为2 m s〜(-1)可以传输强度为20-30 kG的磁场。如果磁场高于均分强度,湍流粘度的淬灭会导致子午流从磁化区域偏转,并显着降低传输速度。

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