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Inference of magnetic fields in the very quiet Sun

机译:在非常安静的太阳下推断磁场

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Context. Over the past 20 yr, the quietest areas of the solar surface have revealed a weak but extremely dynamic magnetism occurring at small scales ( &500 km), which may provide an important contribution to the dynamics and energetics of the outer layers of the atmosphere. Understanding this magnetism requires the inference of physical quantities from high-sensitivity spectro-polarimetric data with high spatio-temporal resolution. Aims. We present high-precision spectro-polarimetric data with high spatial resolution (0.4 ′′ ) of the very quiet Sun at 1.56 μ m obtained with the GREGOR telescope to shed some light on this complex magnetism. Methods. We used inversion techniques in two main approaches. First, we assumed that the observed profiles can be reproduced with a constant magnetic field atmosphere embedded in a field-free medium. Second, we assumed that the resolution element has a substructure with either two constant magnetic atmospheres or a single magnetic atmosphere with gradients of the physical quantities along the optical depth, both coexisting with a global stray-light component. Results. Half of our observed quiet-Sun region is better explained by magnetic substructure within the resolution element. However, we cannot distinguish whether this substructure comes from gradients of the physical parameters along the line of sight or from horizontal gradients (across the surface). In these pixels, a model with two magnetic components is preferred, and we find two distinct magnetic field populations. The population with the larger filling factor has very weak ( ~ 150 G) horizontal fields similar to those obtained in previous works. We demonstrate that the field vector of this population is not constrained by the observations, given the spatial resolution and polarimetric accuracy of our data. The topology of the other component with the smaller filling factor is constrained by the observations for field strengths above 250 G: we infer hG fields with inclinations and azimuth values compatible with an isotropic distribution. The filling factors are typically below 30%. We also find that the flux of the two polarities is not balanced. From the other half of the observed quiet-Sun area ~ 50% are two-lobed Stokes V profiles, meaning that 23% of the field of view can be adequately explained with a single constant magnetic field embedded in a non-magnetic atmosphere. The magnetic field vector and filling factor are reliable inferred in only 50% based on the regular profiles. Therefore, 12% of the field of view harbour hG fields with filling factors typically below 30%. At our present spatial resolution, 70% of the pixels apparently are non-magnetised.
机译:上下文。在过去的20年中,太阳表面最安静的区域显示出小规模(小于500 km)的弱磁但极具动态磁性,这可能对大气外层的动力和能量有重要贡献。要了解这种磁性,就需要从具有高时空分辨率的高灵敏度光谱极化数据中推断出物理量。目的我们展示了使用GREGOR望远镜获得的具有1.56μm高度非常安静的太阳的高空间分辨率(0.4'')的高精度光谱极化数据,以阐明这种复杂的磁性。方法。我们在两种主要方法中使用了反演技术。首先,我们假设可以在嵌入无场介质中的恒定磁场氛围下再现观察到的轮廓。其次,我们假设分辨元件具有一个子结构,该子结构具有两个恒定的磁性气氛或一个单一的磁性气氛,且沿着光学深度具有物理量的梯度,并且都与全局杂散光分量共存。结果。分辨率元素内的磁性子结构可以更好地解释我们观测到的安静太阳区域的一半。但是,我们无法区分此子结构是来自沿视线的物理参数的梯度还是来自(整个表面的)水平梯度。在这些像素中,首选具有两个磁性成分的模型,我们发现了两个不同的磁场种群。填充因子较大的种群的水平场非常弱(〜150 G),类似于先前的工作。我们证明,鉴于我们的数据的空间分辨率和极化精度,该种群的场矢量不受观测值的限制。填充系数较小的其他组件的拓扑结构受到对250 G以上场强的观察的约束:我们推论hG场具有与各向同性分布兼容的倾斜度和方位角值。填充因子通常低于30%。我们还发现两种极性的通量不平衡。从观察到的安静太阳区域的另一半〜50%是两瓣Stokes V轮廓,这意味着23%的视野可以用嵌入非磁性气氛中的单个恒定磁场来充分解释。根据规则轮廓,仅可以可靠地推断出磁场矢量和填充因子仅为50%。因此,视野的12%包含了填充因子通常低于30%的hG场。在我们目前的空间分辨率下,70%的像素显然没有被磁化。

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