论文标题

在Ca I4227Å线的散射极化机翼中的磁光效应的观察性指示

Observational indications of magneto-optical effects in the scattering polarization wings of the Ca I 4227 Å line

论文作者

Capozzi, E., Ballester, E. Alsina, Belluzzi, L., Bianda, M., Dhara, S. K., Ramelli, R.

论文摘要

几种强的共振线,例如H i ly-$α$,mg ii k,ca ii k,ca i4227Å\,其特征是太阳强度谱中的深层和广泛的吸收曲线,当在接近Solar Limb附近的安静区域观察到时,显示出明显的线性散射信号。这样的信号显示了一个特征性的三胞胎峰结构,线芯和延伸的机翼叶具有尖锐的峰值。线芯峰对通过Hanle效应的磁场敏感,但是已知该效果不在线机翼中工作。最近的理论研究表明,与以前认为的相反,翼线性极化信号也通过磁光(MO)对磁场敏感。我们在Ca I4227Å线的散射极化机翼中搜索了最近发现的物理机制的观察指示。我们使用IRSOL(瑞士)的Gregory-Coudé望远镜和特内里费岛的Gregor望远镜(西班牙)的Gregory-Coudé望远镜上的苏黎世成像偏光仪(Zimpol)摄像头对这条线进行了一系列光谱图。在观测线的机翼中,总线性极化度和线性极化角的空间变化显然是可观的。我们提供了有关我们的观察结果的详细讨论,表明检测到的变化始终发生在存在纵向磁场的区域中,从而支持理论预测,即它们是由MO效应产生的。

Several strong resonance lines, such as H I Ly-$α$, Mg II k, Ca II K, Ca I 4227 Å\, which are characterized by deep and broad absorption profiles in the solar intensity spectrum, show conspicuous linear scattering polarization signals when observed in quiet regions close to the solar limb. Such signals show a characteristic triplet-peak structure, with a sharp peak in the line core and extended wing lobes. The line core peak is sensitive to the presence of magnetic fields through the Hanle effect, which however is known not to operate in the line wings. Recent theoretical studies indicate that, contrary to what was previously believed, the wing linear polarization signals are also sensitive to the magnetic field through magneto-optical effects (MO). We search for observational indications of this recently discovered physical mechanism in the scattering polarization wings of the Ca I 4227 Å line. We performed a series of spectropolarimetric observations of this line using the Zurich IMaging POLarimeter (ZIMPOL) camera at the Gregory-Coudé telescope of IRSOL (Switzerland) and at the GREGOR telescope in Tenerife (Spain). Spatial variations of the total linear polarization degree and of the linear polarization angle are clearly appreciable in the wings of the observed line. We provide a detailed discussion of our observational results, showing that the detected variations always take place in regions where longitudinal magnetic fields are present, thus supporting the theoretical prediction that they are produced by MO effects.

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