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首页> 外文期刊>The Astrophysical journal >ON THE DOPPLER SHIFT AND ASYMMETRY OF STOKES PROFILES OF PHOTOSPHERIC Fe I AND CHROMOSPHERIC Mg I LINES
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ON THE DOPPLER SHIFT AND ASYMMETRY OF STOKES PROFILES OF PHOTOSPHERIC Fe I AND CHROMOSPHERIC Mg I LINES

机译:球形Fe I和染色体Mg I线的斯托克谱的多普勒频移和不对称

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We analyzed the full Stokes spectra using simultaneous measurements of the photospheric (Fe I 630.15 and 630.25?nm) and chromospheric (Mg I b 2 517.27?nm) lines. The data were obtained with the High Altitude Observatory/National Solar Observatory (HAO/NSO) advanced Stokes polarimeter, about a near disk center sunspot region, NOAA AR 9661. We compare the characteristics of the Stokes profiles in terms of Doppler shifts and asymmetries among the three spectral lines, helping us to better understand the chromospheric lines and the magnetic and flow fields in different magnetic regions. The main results are: (1) for the penumbral area observed by the photospheric Fe I lines, Doppler velocities derived from Stokes I (ν i ) are very close to those derived from linear polarization profiles (νlp) but significantly different from those derived from Stokes V profiles (νzc), thus providing direct and strong evidence that the penumbral Evershed flows are magnetized and mainly carried by the horizontal magnetic component; (2) the rudimentary inverse Evershed effect observed by the Mg I b 2 line provides qualitative evidence on its formation height that is around or just above the temperature minimum region; (3) νzc and νlp in the penumbrae and νzc in the pores generally approach their ν i observed by the chromospheric Mg I line, which is not the case for the photospheric Fe I lines; (4) the outer penumbrae and pores show similar Stokes V asymmetry behavior that tend to change from positive values in the photosphere (Fe I lines) to negative values in the low chromosphere (Mg I line); (5) the Stokes V profiles in plage regions are highly asymmetric in the photosphere and more symmetric in the low chromosphere; and (6) strong redshifts and large asymmetries are found around the magnetic polarity inversion line within the common penumbra of the δ spot. We offer explanations or speculations to the observed discrepancies between the photospheric and chromospheric lines in terms of the three-dimensional structure of the magnetic and velocity fields. This study thus emphasizes the importance of spectropolarimetry using chromospheric lines.
机译:我们使用光球(Fe I 630.15和630.25?nm)和色球(Mg I b 2 517.27?nm)线的同时测量来分析整个斯托克斯光谱。数据是通过高空天文台/国家太阳观测台(HAO / NSO)先进的斯托克斯旋光仪获得的,它位于磁盘中心黑子附近,NOAA AR9661。我们根据多普勒频移和不对称性比较了斯托克斯剖面的特征这三个光谱线,有助于我们更好地了解色球层线以及不同磁性区域中的磁场和流场。主要结果是:(1)对于通过光球Fe I线观察到的半影区,从斯托克斯I(νi)推导的多普勒速度非常接近于从线性偏振轮廓(νlp)推导的多普勒速度,但是与从斯托克斯V型剖面(νzc),因此提供了直接而有力的证据,表明半影Evershed流已被磁化,并且主要由水平磁分量携带; (2)Mg I b 2线观察到的基本逆向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)半球上的νzc和νlp以及孔隙中的νzc通常接近色球Mg I线所观测到的νi,光球Fe I线则不是这种情况。 (4)外半影和孔隙表现出相似的斯托克斯V不对称性,其趋势从光圈中的正值(Fe I线)变为低色圈中的负值(Mg I线); (5)斑块区的Stokes V剖面在光圈中高度不对称,在低色度圈中更对称; (6)在δ点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。我们根据磁场和速度场的三维结构,对观察到的光球和色球线之间的差异进行解释或推测。因此,这项研究强调了使用色球层谱线极化法的重要性。

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