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arXiv 1305.2159astro-ph.SR
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磁化对流区中的磁通浮现

Flux emergence in a magnetized convection zone

R. F. Pinto, A. S. Brun

摘要:

本文研究了发电机磁场对扭曲磁通量绳上浮和出现的影响,以及它们对全球外部磁场的影响。我们运行三维MHD数值模拟使用ASH代码和分析的动态演变的浮力通量绳从底部的对流区,直到出现后的阶段。该模型的全球性质非常粗略和不准确地代表了浮力上升的局部动态,但允许研究全球效应的影响,如自洽产生的差异旋转,纬向环流和科里奥利力。虽然受到太阳背景的启发,但这个模型不能被认为是磁结构兴起及其在太阳中出现的现实模型,因为太阳的局部动力学完全不同。初始阶段的浮力上升的性质与以前的研究很好的协议。然而,背景发电机场的相互作用的影响变得越来越大的磁通绳的发展。在穿过CZ的浮力上升期间,磁通绳的磁场强度和比例为$rho^a$,与$a\lesssim 1$。流速、密度和海流的增加先于所有边界的通量出现。磁绳相对于背景磁场的几何形状、纬度和相对取向影响上升速度、纬向流振幅(在磁绳内发展)和相应的表面特征。这会影响相关的表面剪切和坡印亭通量的形态、持续时间和幅度。出现的通量影响系统的全球极性,在某些情况下导致极性反转,而在另一些情况下抑制背景发电机这样做。出现的磁通量缓慢地向极向平流,同时被背景发电机场扩散和同化。

英文摘要:

We study the influence of a dynamo magnetic field on the buoyant rise and emergence of twisted magnetic flux-ropes, and their influence on the global external magnetic field. We ran 3D MHD numerical simulations using the ASH code and analysed the dynamical evolution of such buoyant flux-ropes from the bottom of the convection zone until the post-emergence phases. The global nature of this model represents very crudely and inaccurately the local dynamics of the buoyant rise, but allows to study the influence of global effects such as self-consistently generated differential rotation, meridional circulation and Coriolis forces. Although motivated by the solar context, this model cannot be thought of as a realistic model of the rise of magnetic structures and their emergence in the Sun where the local dynamics are completely different. The properties of initial phases of the buoyant rise in good agreement with previous studies. However, the effects of the interaction of the background dynamo field become increase as the flux-ropes evolve. During the buoyant rise across the CZ, the flux-rope's magnetic field strength and scales as $rho^a$, with $a\lesssim 1$. An increase of velocity, density and current precedes flux emergence at all longitudes. The geometry, latitude and relative orientation of the flux-ropes with respect to the background magnetic field influences the rise speeds, zonal flow amplitudes (which develop within the flux-ropes) and the corresponding surface signatures. This influences the morphology, duration and amplitude of the associated surface shearing and Poynting flux. The emerged flux influences the system's global polarity, leading in some cases to a polarity reversal while inhibiting background dynamo from doing so in some others. The emerged magnetic flux is slowly advected poleward, while being diffused and assimilated by the background dynamo field.

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