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Fast inversion of Zeeman line profiles using central moments - II. Stokes V moments and determination of vector magnetic fields

机译:使用中央时刻 - II的塞曼线轮廓快速反转。斯托克斯v矩和矢量磁场的确定

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Context. In the case of unresolved solar structures or stray light contamination, inversion techniques using four Stokes parameters of Zeeman profiles cannot disentangle the combined contributions of magnetic and nonmagnetic areas to the observed Stokes I . Aims. In the framework of a two-component model atmosphere with filling factor f , we propose an inversion method restricting input data to Q , U, and V profiles, thus overcoming ambiguities from stray light and spatial mixing. Methods. The V -moments inversion (VMI) method uses shifts S _( V ) derived from moments of V -profiles and integrals of Q ~(2) , U ~(2) , and V ~(2) to determine the strength B and inclination ψ of a magnetic field vector through least-squares polynomial fits and with very few iterations. Moment calculations are optimized to reduce data noise effects. To specify the model atmosphere of the magnetic component, an additional parameter δ , deduced from the shape of V -profiles, is used to interpolate between expansions corresponding to two basic models. Results. We perform inversions of HINODE SOT/SP data for inclination ranges 0 & ψ & 60° and 120 & ψ & 180° for the 630.2 nm Fe? i line. A damping coefficient is fitted to take instrumental line broadening into account. We estimate errors from data noise. Magnetic field strengths and inclinations deduced from VMI inversion are compared with results from the inversion codes UNNOFIT and MERLIN. Conclusions. The VMI inversion method is insensitive to the dependence of Stokes I profiles on the thermodynamic structure in nonmagnetic areas. In the range of Bf products larger than 200 G, mean field strengths exceed 1000 G and there is not a very significant departure from the UNNOFIT results because of differences between magnetic and nonmagnetic model atmospheres. Further improvements might include additional parameters deduced from the shape of Stokes V profiles and from large sets of 3D-MHD simulations, especially for unresolved magnetic flux tubes.
机译:语境。在未解决的太阳能结构或杂散光污染的情况下,使用Zeeman Culites的四个斯托克斯参数的反转技术不能解开磁性和非磁性区域的组合贡献给观察到的斯托克。目标。在具有填充因子F的双组分模型气氛的框架中,我们提出了一种反演方法,将输入数据限制为Q,U和V型材,从而克服来自杂散光和空间混合的含糊不清。方法。 V-Moments反演(VMI)方法使用源自V -Profiles的片刻和Q〜(2),U〜(2)和V〜(2)的积分来确定强度B和通过最小二乘多项式拟合和极少的迭代倾斜ψ磁场矢量。时刻计算经过优化以降低数据噪声效果。为了指定磁性分量的模型气氛,从V -Profiles的形状推断的附加参数δ用于在对应于两个基本模型的扩展之间插值。结果。我们执行Hinode SOT / SP数据的回复,用于倾斜范围0& ψ& 60°和120℉ ψ& 630.2nm fe的180°?我线。阻尼系数适用于考虑仪器的乐器。我们估计数据噪声的错误。将磁场强度和从VMI反转推导的倾斜与来自反演码Unnofit和Merlin的结果进行比较。结论。 VMI反转方法对Stokes I曲线在非磁性区域的热力学结构上的依赖性不敏感。在大于200克的BF产品的范围内,由于磁性和非磁性模型气氛之间的差异,平均场强度超过1000克,并且由于磁性和非磁性模型环境之间的差异而言,没有非常显着的偏离。进一步的改进可能包括从Stokes V配置文件的形状和大组3D-MHD仿真推导的附加参数,特别是对于未解决的磁通量管。

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