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  • 标题:The influence of NLTE effects in Fe  I lines on an inverted atmosphere
  • 其他标题:I. 6301 Å and 6302 Å lines formed in 1D NLTE
  • 本地全文:下载
  • 作者:H. N. Smitha ; R. Holzreuter ; M. van Noort
  • 期刊名称:Astronomy & Astrophysics
  • 印刷版ISSN:0004-6361
  • 电子版ISSN:1432-0746
  • 出版年度:2020
  • 卷号:633
  • 页码:1-15
  • DOI:10.1051/0004-6361/201937041
  • 语种:English
  • 出版社:EDP Sciences
  • 摘要:Context.Ultraviolet overionisation of iron atoms in the solar atmosphere leads to deviations in their level populations based on Saha-Boltzmann statistics. This causes their line profiles to form in non-local thermodynamic equilibrium (NLTE) conditions. When inverting such profiles to determine atmospheric parameters, the NLTE effects are often neglected and other quantities are tweaked to compensate for deviations from the LTE.Aims.We investigate how the routinely employed LTE inversion of iron lines formed in NLTE underestimates or overestimates atmospheric quantities, such as temperature (T), line-of-sight velocity (vLOS), magnetic field strength (B), and inclination (γ) while the earlier papers have focused mainly onT. Our findings has wide-ranging consequences since many results derived in solar physics are based on inversions of Fe Ilines carried out in LTE.Methods.We synthesized the Stokes profiles of Fe I6301.5 Å and 6302.5 Å lines in both LTE and NLTE using a snapshot of a 3D magnetohydrodynamic simulation. The profiles were then inverted in LTE. We considered the atmosphere inferred from the inversion of LTE profiles as the fiducial model and compared it to the atmosphere resulting from the inversion of NLTE profiles. The observed differences have been attributed to NLTE effects.Results.Neglecting the NLTE effects introduces errors in the inverted atmosphere. While the errors inTcan go up to 13%, invLOSandB, the errors can go as high as 50% or above. We find these errors to be present at all three inversion nodes. Importantly, they survive degradation from the spatial averaging of the profiles.Conclusions.We provide an overview of how neglecting NLTE effects influences the values ofT, vLOS,B, andγthat are determined by inverting the Fe I6300 Å line pair, as observed, for example, by Hinode/SOT/SP. Errors are found at the sites of granules, intergranular lanes, magnetic elements, and basically in every region susceptible to NLTE effects. For an accurate determination of the atmospheric quantities and their stratification, it is, therefore, important to take the NLTE effects into account.
  • 关键词:enradiative transferline: formationline: profilesSun: magnetic fieldsSun: photospherepolarization
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