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Flux-Transport Dynamos with Lorentz Force Feedback on Differential Rotation and Meridional Flow: Saturation Mechanism and Torsional Oscillations

机译:具有差动旋转和子午流的洛伦兹力反馈的磁通量传输动力学:饱和机理和扭转振荡

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In this paper we discuss a dynamic flux-transport dynamo model that includes the feedback of the induced magnetic field on differential rotation and meridional flow. We consider two different approaches for the feedback: mean field Lorentz force and quenching of transport coefficients such as turbulent viscosity and heat conductivity. We find that even strong feedback on the meridional flow does not change the character of the flux-transport dynamo significantly; however, it leads to a significant reduction of differential rotation. To a large degree independent of the dynamo parameters, the saturation takes place when the toroidal field at the base of the convection zone reaches between 1.2 and 1.5?T, and the energy converted into magnetic energy corresponds to about 0.1%-0.2% of the solar luminosity. The torsional oscillations produced through Lorentz force feedback on differential rotation show a dominant poleward propagating branch with the correct phase relation to the magnetic cycle. We show that incorporating enhanced surface cooling of the active region belt (as proposed by Spruit) leads to an equatorward propagating branch in good agreement with observations.
机译:在本文中,我们讨论了一种动态磁通传输发电机模型,该模型包括感应磁场对差速旋转和子午流的反馈。我们考虑两种不同的反馈方法:平均洛伦兹力和诸如湍流粘度和热导率之类的传输系数的猝灭。我们发现,即使对子午流的强烈反馈也不会显着改变通量传输发电机的特性。但是,这会大大减少差速旋转。在很大程度上与发电机参数无关,当对流区底部的环形磁场达到1.2至1.5?T之间时,就会发生饱和,转换成磁能的能量大约相当于对流区的0.1%-0.2%。太阳光度。由洛伦兹力反馈产生的扭转振动在差速旋转中显示出一个主导的极向传播分支,该分支与磁循环具有正确的相位关系。我们表明,结合活动区域带的增强表面冷却(由Spruit提出)导致与观测良好吻合的赤道传播分支。

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