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Expanding Magnetic Canopy Structure and Parasitic Polarities in a Quiet-Sun Network Element Observed by SUNRISE III/SCIP

  • Authors: Ryan J. Campbell, Carlos Quintero Noda, Mihalis Mathioudakis, Manuel Collados, Jack McFall, David B. Jess, Sami K. Solanki, Andreas Lagg, Achim Gandorfer, Jose Carlos del Toro Iniesta, Yukio Katsukawa, Pietro Bernasconi, Thomas Berkefeld, Alex Feller, Tino L. Riethmüller, Alberto Álvarez-Herrero, Masahito Kubo, H. N. Smitha, David Orozco Suárez, Bianca Grauf, Michael Carpenter, Alexander Bell, Valentín Martínez Pillet, Francisco Javier Bailén, Julian Blanco Rodríguez, Juan Sebastián Castellanos Durán, Edvarda Harnes, Johannes Hölken, Francisco A. Iglesias, Ryohtaroh T. Ishikawa, Yusuke Kawabata, Takuma Matsumoto, Takayoshi Oba, Azaymi L. Siu-Tapia, Hanna Strecker, Dušan Vukadinović, Hirohisa Hara, Toshifumi Shimizu

Ryan J. Campbell et al 2026 The Astrophysical Journal Letters 1008 .

  • Provider: AAS Journals

Caption: Figure 3.

Illustrative magnetic structure of a quiet-Sun network element from a MURaM simulation. (a) Temperature at ﹩\mathrm{log}\tau =0﹩, showing a cool, concentrated magnetic core embedded within the granular photosphere. (b) Maximum linear polarization signal, ﹩{{\rm{\max }}}_{\lambda }\sqrt{{Q}^{2}+{U}^{2}}﹩, computed over the synthetic Fe I 8468 Å spectral window. The strongest linear polarization occurs preferentially around the boundary of the magnetic concentration rather than within the central core. (c) Transverse magnetic field strength B at ﹩\mathrm{log}\tau =-2.9﹩, with red lines indicating the magnetic azimuth directions. (d) Azimuth proxy derived from the synthesized Stokes Q and U profiles using the same methodology applied to the SCIP observations, overlaid on the synthetic linear polarization map. Red lines indicate the inferred azimuth orientation. (e) Median absolute difference between the azimuth proxy, χLP, and the ground-truth magnetic azimuth in the MURaM simulation as a function of optical depth. The shaded region denotes the 16th–84th percentile range. The minimum error occurs near ﹩\mathrm{log}\tau \approx -2.9﹩, indicating that the wavelength-integrated Fe I 8468 Å line is most sensitive to the magnetic azimuth at upper-photospheric heights.

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