Bibcode
                                    
                            Díaz Baso, C. J.; Martínez González, M. J.; Asensio Ramos, A.
    Referencia bibliográfica
                                    Astronomy and Astrophysics, Volume 625, id.A128, 18 pp.
Fecha de publicación:
    
                        5
            
                        2019
            
  Revista
                                    
                            Número de citas
                                    25
                            Número de citas referidas
                                    23
                            Descripción
                                    Aims: The determination of the magnetic filed vector in solar
filaments is made possible by interpreting the Hanle and Zeeman effects
in suitable chromospheric spectral lines like those of the He I
multiplet at 10 830 Å. We study the vector magnetic field of an
active region filament (NOAA 12087).  Methods: Spectropolarimetric
data of this active region was acquired with the GRIS instrument at the
GREGOR telescope and studied simultaneously in the chromosphere with the
He I 10 830 Å multiplet and in the photosphere Si I 10 827 Å
line. As has been done in previous studies, only a single-component
model was used to infer the magnetic properties of the filament. The
results are put into a solar context with the help of the Solar Dynamic
Observatory images.  Results: Some results clearly point out that
a more complex inversion had to be performed. First, the Stokes V map of
He I does not show a clear signature of the presence of the filament.
Second, the local azimuth map follows the same pattern as Stokes V; it
appears that polarity of Stokes V is conditioning the inference to very
different magnetic fields even with similar linear polarization signals.
This indication suggests that the Stokes V could be dominated from below
by the magnetic field coming from the active region, and not from the
filament itself. This evidence, and others, will be analyzed in depth
and a more complex inversion will be attempted in the second part of
this series.
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