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首页> 外文期刊>The Astrophysical Journal. Letters >DIRECT OBSERVATION OF SOLAR CORONAL MAGNETIC FIELDS BY VECTOR TOMOGRAPHY OF THE CORONAL EMISSION LINE POLARIZATIONS
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DIRECT OBSERVATION OF SOLAR CORONAL MAGNETIC FIELDS BY VECTOR TOMOGRAPHY OF THE CORONAL EMISSION LINE POLARIZATIONS

机译:冠状发射线极化的矢量层析成像直接观测太阳冠状磁场

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摘要

We present the first direct "observation" of the global-scale, 3D coronal magnetic fields of Carrington Rotation (CR) Cycle 2112 using vector tomographic inversion techniques. The vector tomographic inversion uses measurements of the Fe XIII 10747 HHanleeffect polarization signals by the Coronal Multichannel Polarimeter (CoMP) and 3D coronal density and temperature derived from scalar tomographic inversion of Solar Terrestrial Relations Observatory (STEREO)/Extreme Ultraviolet Imager (EUVI) coronal emission lines (CELs) intensity images as inputs to derive a coronal magnetic field model that best reproduces the observed polarization signals. While independent verifications of the vector tomography results cannot be performed, we compared the tomography inverted coronal magnetic fields with those constructed by magnetohydrodynamic (MHD) simulations based on observed photospheric magnetic fields of CR 2112 and 2113. We found that the MHD model for CR 2112 is qualitatively consistent with the tomography inverted result for most of the reconstruction domain except for several regions. Particularly, for one of the most noticeable regions, we found that the MHD simulation for CR 2113 predicted a model that more closely resembles the vector tomography inverted magnetic fields. In another case, our tomographic reconstruction predicted an open magnetic field at a region where a coronal hole can be seen directly from a STEREO-B/EUVI image. We discuss the utilities and limitations of the tomographic inversion technique, and present ideas for future developments.
机译:我们提出了使用矢量层析成像反演技术对卡林顿旋转(CR)周期2112的全球规模的3D冠状磁场进行的第一个直接“观测”。矢量断层扫描反演使用了日冕多通道旋光仪(CoMP)对Fe XIII 10747 HHanleeffect极化信号的测量以及3D冕状密度和温度,这是由太阳陆地关系天文台(STEREO)/极紫外成像仪(EUVI)冕状发射的标量层析成像反演得出的线(CEL)强度图像作为输入,以推导出最能重现观察到的极化信号的日冕磁场模型。尽管无法对矢量断层扫描结果进行独立验证,但我们将断层扫描的倒置冠状磁场与通过磁流体动力学(MHD)模拟基于观测到的CR 2112和2113的光球磁场构造的磁场进行了比较。我们发现CR 2112的MHD模型在质量上与大多数重建域的层析成像倒置结果一致,除了几个区域。特别是,对于最引人注目的区域之一,我们发现CR 2113的MHD模拟预测出的模型与矢量断层扫描反向磁场更为相似。在另一种情况下,我们的断层扫描重建预测可以从STEREO-B / EUVI图像直接看到冠状孔的区域存在开放磁场。我们讨论了层析反演技术的实用性和局限性,并提出了未来发展的思路。

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