论文标题
部分可观测时空混沌系统的无模型预测
The Rise of Buoyant Magnetic Structures through Convection with a Background Magnetic Field
论文作者
论文摘要
受到嵌入活跃区域中黑子的观察的启发,通常假定以拱形的圆柱形结构形式从太阳的深内部出现了大规模的强磁通量,该圆柱形结构被称为通量管。在这里,我们继续检查当将这些结构视为体积填充磁场中的浓度时,而不是在无野外背景中孤立的实体时,遇到的不同动态。通过2.5D数值模拟,我们考虑了从辐射区域从辐射区域通过超弹对流区的磁通浓度的浮力上升,该对流区自愿(通过磁泵)安排了一个体积填充的大规模背景字段。这项工作扩展了早期的论文,这些论文以纯绝热分层为背景字段的纯绝热分层中考虑了这种结构的演变。这项较早的工作确定了存在偏见的存在,这种偏见增加了磁性结构成功上升的可能性增加,一种(相对)的扭曲方向和对方的可能性降低。当应用于太阳背景时,这种偏见与太阳半球形螺旋性规则(SHHR)相称。本文在包含更现实的背景状态的模型中建立了这种选择机制的鲁棒性,该模型包括对流过度和湍流的平均磁场。最终,对流只会影响选择机制,因为它是在上升区边缘的上升开始时制定的。然而,对流的确增加了偏见的另一层统计波动,我们调查了这些波动,以解释SHHR中的变化。
Inspired by observations of sunspots embedded in active regions, it is often assumed that large-scale, strong magnetic flux emerges from the Sun's deep interior in the form of arched, cylindrical structures, colloquially known as flux tubes. Here, we continue to examine the different dynamics encountered when these structures are considered as concentrations in a volume-filling magnetic field rather than as isolated entities in a field-free background. Via 2.5D numerical simulations, we consider the buoyant rise of magnetic flux concentrations from a radiative zone through an overshooting convection zone that self-consistently (via magnetic pumping) arranges a volume-filling large-scale background field. This work extends earlier papers that considered the evolution of such structures in a purely adiabatic stratification with an assumed form of the background field. This earlier work established the existence of a bias that created an increased likelihood of successful rise for magnetic structures with one (relative) orientation of twist and a decreased likelihood for the other. When applied to the solar context, this bias is commensurate with the solar hemispherical helicity rules (SHHR). This paper establishes the robustness of this selection mechanism in a model incorporating a more realistic background state, consisting of overshooting convection and a turbulently-pumped mean magnetic field. Ultimately, convection only weakly influences the selection mechanism, since it is enacted at the initiation of the rise, at the edge of the overshoot zone. Convection does however add another layer of statistical fluctuations to the bias, which we investigate in order to explain variations in the SHHR.