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Mean-field and direct numerical simulations of magnetic flux concentrations from vertical field

机译:垂直磁场的磁通量密度的均值场和直接数值模拟

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Context. Strongly stratified hydromagnetic turbulence has previously been found to produce magnetic flux concentrations if the domain is large enough compared with the size of turbulent eddies. Mean-field simulations (MFS) using parameterizations of the Reynolds and Maxwell stresses show a large-scale negative effective magnetic pressure instability and have been able to reproduce many aspects of direct numerical simulations (DNS) regarding growth rate, shape of the resulting magnetic structures, and their height as a function of magnetic field strength. Unlike the case of an imposed horizontal field, for a vertical one, magnetic flux concentrations of equipartition strength with the turbulence can be reached, resulting in magnetic spots that are reminiscent of sunspots. Aims. We determine under what conditions magnetic flux concentrations with vertical field occur and what their internal structure is. Methods. We use a combination of MFS, DNS, and implicit large-eddy simulations (ILES) to characterize the resulting magnetic flux concentrations in forced isothermal turbulence with an imposed vertical magnetic field. Results. Using DNS, we confirm earlier results that in the kinematic stage of the large-scale instability the horizontal wavelength of structures is about 10 times the density scale height. At later times, even larger structures are being produced in a fashion similar to inverse spectral transfer in helically driven turbulence. Using ILES, we find that magnetic flux concentrations occur for Mach numbers between 0.1 and 0.7. They occur also for weaker stratification and larger turbulent eddies if the domain is wide enough. Using MFS, the size and aspect ratio of magnetic structures are determined as functions of two input parameters characterizing the parameterization of the effective magnetic pressure. DNS, ILES, and MFS show magnetic flux tubes with mean-field energies comparable to the turbulent kinetic energy. These tubes can reach a length of about eight density scale heights. Despite being ≤1% equipartition strength, it is important that their lower part is included within the computational domain to achieve the full strength of the instability. Conclusions. The resulting vertical magnetic flux tubes are being confined by downflows along the tubes and corresponding inflow from the sides, which keep the field concentrated. Application to sunspots remains a viable possibility.
机译:上下文。如果磁畴与湍流涡流的大小相比足够大,以前已经发现强分层的水磁湍流会产生磁通量浓度。使用雷诺应力和麦克斯韦应力参数化的平均场模拟(MFS)显示出大规模的负有效磁压不稳定性,并且已经能够再现有关增长率,最终磁结构的形状的直接数值模拟(DNS)的许多方面以及它们的高度与磁场强度的关系。与强加水平磁场不同,对于垂直磁场,可以达到与湍流等分强度的磁通量浓度,从而产生让人联想到黑子的磁点。目的我们确定在什么条件下产生具有垂直场的磁通量浓度以及它们的内部结构是什么。方法。我们使用MFS,DNS和隐式大涡模拟(ILES)的组合来描述在强等温湍流和垂直磁场作用下产生的磁通量浓度。结果。使用DNS,我们确认了较早的结果,即在大规模不稳定性的运动学阶段,结构的水平波长约为密度标高的10倍。后来,以类似于螺旋驱动的湍流中的逆光谱传递的方式生产出更大的结构。使用ILES,我们发现马赫数在0.1到0.7之间发生磁通量集中。如果域足够宽,它们也会出现,用于较弱的分层和较大的涡流。使用MFS,根据表征有效磁压参数化的两个输入参数确定磁性结构的大小和纵横比。 DNS,ILES和MFS显示的磁通量管的平均场能与湍动能相当。这些管的长度可以达到大约八个密度标高。尽管等分强度≤1%,但重要的是将它们的下部包括在计算域内,以实现不稳定性的全部强度。结论。产生的垂直磁通管受到沿管的向下流动和来自侧面的相应流入的限制,从而使磁场集中。应用于黑子仍然是可行的可能性。

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