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Oxygen is the most abundant element on the Sun after Hydrogen and Helium. The intensity spectrum of resonance lines of neutral Oxygen namely O {sc i} (1302, 1305 and 1306 AA,) has been studied in the literature for chromospheric diagnostics. In this paper we study the resonance scattering polarization in the O {sc i} line at 1302 AA, using two-dimensional radiative transfer in a composite atmosphere constructed using a two-dimensional magneto-hydrodynamical snapshot in the photosphere and columns of the one-dimensional FALC atmosphere in the chromosphere. The methods developed by us recently in a series of papers to solve multi-dimensional polarized radiative transfer have been incorporated in our new code POLY2D which we use for our analysis. We find that multi-dimensional radiative transfer including XRD effects is important in reproducing the amplitude and shape of scattering polarization signals of the O {sc i} line at 1302 AA,.
Magnetic fields in turbulent, convective high-$beta$ plasma naturally develop highly tangled and complex topologies---the solar photosphere being the paradigmatic example. These fields are mostly undetectable by standard diagnostic techniques with fi
Context. The scattering polarization signal observed in the photospheric Sr i 4607 {AA} line is expected to vary at granular spatial scales. This variation can be due to changes in the magnetic field intensity and orientation (Hanle effect), but also
Several strong resonance lines, such as H I Ly-$alpha$, Mg II k, Ca II K, Ca I 4227 AA, which are characterized by deep and broad absorption profiles in the solar intensity spectrum, show conspicuous linear scattering polarization signals when observ
Magnetic field measurements in the upper chromosphere and above, where the gas-to-magnetic pressure ratio $beta$ is lower than unity, are essential for understanding the thermal structure and dynamical activity of the solar atmosphere. Recent develop
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