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arXiv 1607.00772astro-ph.SR
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二维反演揭示的互联网磁场

Internetwork magnetic field as revealed by 2D inversions

S. Danilovic, M. van Noort, M. Rempel

摘要:

由于光谱偏振信号相当弱,所以互联网络区域的磁场性质仍然相当未知。我们通过使用二维反演代码来解决这个问题,该代码能够检索最小空间尺度上的信息,直到衍射极限,同时比大多数以前使用的方法更不易受噪声的影响。的代码的性能和检索场分布的各种影响进行了测试,首先在现实的MHD模拟。最好的反演方案,然后应用到真正的Hinode/SP数据。模拟试验表明:(1)节点位置的最佳选择确保了所有参数的良好检索,(2)代码对于磁场的不同配置表现良好,(3)空间PSF中包括的稍微不同的噪声水平或稍微不同的散焦对结果没有显著影响,以及(4)时间积分将场分布移动到更强、更水平倾斜的场。虽然由于噪声的影响,弱场的贡献被略微高估,但是二维反演能够很好地恢复磁场强度的总体分布。二维反演代码上的Hinode/SP互联网观测的应用揭示了单调的场强分布。在光学厚度为1处的平均场强为$\sim 130$ ~G。在较高层,场强随着场变得更水平而下降。关于场倾斜的分布,测试表明,我们不能直接用手头的观测/工具来检索它,然而,在考虑观测效应后,所获得的分布与从具有准各向同性场倾斜的模拟中预期的分布是一致的。

英文摘要:

Properties of magnetic field in the internetwork regions are still fairly unknown due to rather weak spectropolarimetric signals. We address the matter by using the 2D inversion code that is able to retrieve the information on smallest spatial scales, up to the diffraction limit, while being less susceptible to noise than most of the previous methods used. Performance of the code and the impact of the various effects on the retrieved field distribution is tested first on the realistic MHD simulations. The best inversion scenario is then applied to the real Hinode/SP data. Tests on simulations show: (1) the best choice of node position ensures a decent retrieval of all parameters, (2) code performs well for different configurations of magnetic field, (3) slightly different noise level or slightly different defocus included in the spatial PSF produces no significant effect on the results and (4) temporal integration shifts the field distribution to the stronger, more horizontally inclined field. Although the contribution of the weak field is slightly overestimated due to noise, the 2D inversions are able to recover well the overall distribution of the magnetic field strength. Application of the 2D inversion code on the Hinode/SP internetwork observations reveals a monotonic field strength distribution. The mean field strength at optical depth unity is $\sim 130$~G. At the higher layers, field strength drops as the field becomes more horizontal. Regarding the distribution of the field inclination, tests show that we cannot directly retrieve it with the observations/tools at hand, however the obtained distributions are consistent with those expected from simulations with a quasi-isotropic field inclination after accounting for observational effects.

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