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On the Doppler Shift and Asymmetry of Stokes Profiles of Photospheric FeI and Chromospheric MgI Lines

机译:关于光球stokes剖面的多普勒频移和不对称性   FeI和Chromospheric mgI线

摘要

We analyzed the full Stokes spectra using simultaneous measurements of thephotospheric (FeI 630.15 and 630.25 nm) and chromospheric (MgI b2 517.27 nm)lines. The data were obtained with the HAO/NSO Advanced Stokes Polarimeter,about a near disc center sunspot region, NOAA AR 9661. We compare thecharacteristics of Stokes profiles in terms of Doppler shifts and asymmetriesamong the three spectral lines, which helps us to better understand thechromospheric lines and the magnetic and flow fields in different magneticregions. The main results are: (1) For penumbral area observed by thephotospheric FeI lines, Doppler velocities derived from Stokes I (Vi) are veryclose to those derived from linear polarization profiles (Vlp) butsignificantly different from those derived from Stokes V profiles (Vzc), whichprovides direct and strong evidence that the penumbral Evershed flows aremagnetized and mainly carried by the horizontal magnetic component. (2) Therudimentary inverse Evershed effect observed by the MgI b2 line provides aqualitative evidence on its formation height that is around or just above thetemperature minimum region. (3) Vzc and Vlp in penumbrae and Vzc in poresgenerally approach their Vi observed by the chromospheric MgI line, which isnot the case for the photospheric FeI lines. (4) Outer penumbrae and pores showsimilar behavior of the Stokes V asymmetries that tend to change from positivevalues in the photosphere (FeI lines) to negative values in the lowchromosphere (MgI line). (5) The Stokes V profiles in plage regions are highlyasymmetric in the photosphere and more symmetric in the low chromosphere. (6)Strong red shifts and large asymmetries are found around the magnetic polarityinversion line within the common penumbra of the Delta spot. This study thusemphasizes the importance of spectro-polarimetry using chromospheric lines.
机译:我们通过同时测量光球(FeI 630.15和630.25 nm)和色球(MgI b2 517.27 nm)线来分析整个斯托克斯光谱。数据是使用HAO / NSO Advanced Stokes旋光仪获得的,其位于近盘中心太阳黑子区NOAA AR 9661处。我们比较了三谱线中斯托普斯剖面的多普勒频移和非对称性特征,这有助于我们更好地了解色球。线和不同磁场区域的磁场和流场。主要结果是:(1)对于通过光球FeI线观察到的半影区,从斯托克斯I(Vi)导出的多普勒速度与从线性偏振轮廓(Vlp)导出的多普勒速度非常接近,但与从斯托克斯V轮廓(Vzc)导出的多普勒速度非常不同。 ,这提供了直接而有力的证据,证明半影Evershed流被磁化并且主要由水平磁分量携带。 (2)MgI b2线观测到的基本逆向Evershed效应提供了关于其形成高度在最低温度区域附近或正上方的定性证据。 (3)在半球上的Vzc和Vlp和在毛孔中的Vzc通常接近色球MgI线所观察到的Vi,而光球FeI线则不是这种情况。 (4)外半影和孔隙表现出相似的Stokes V不对称行为,其趋势从光圈中的正值(FeI线)变为低色圈中的负值(MgI线)。 (5)斑块区的Stokes V剖面在光圈中高度不对称,在低色圈中更对称。 (6)在三角洲斑的共同半影内的磁极性反转线附近发现了强烈的红移和较大的不对称性。因此,这项研究强调了使用色球层线进行光谱极化的重要性。

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