Bibcode
Quintero Noda, C.; Borrero, J. M.; Orozco Suárez, D.; Ruiz Cobo, B.
Referencia bibliográfica
Astronomy and Astrophysics, Volume 569, id.A73, 13 pp.
Fecha de publicación:
9
2014
Revista
Número de citas
13
Número de citas referidas
11
Descripción
Context. We analyzed spectropolarimetric data recorded with Hinode/SP in
quiet-Sun regions located at the disk center. We found single-lobed
Stokes V profiles showing highly blue- and red-shifted signals.
Oftentimes both types of events appear to be related to each other. Aims: We aim to set constraints on the nature and physical causes of
these highly Doppler-shifted signals, as well as to study their spatial
distribution, spectropolarimetric properties, size, and rate of
occurrence. Also, we plan to retrieve the variation of the physical
parameters with optical depth through the photosphere. Methods:
We have examined the spatial and polarimetric properties of these events
using a variety of data from the Hinode spacecraft. We have also
inferred the atmospheric stratification of the physical parameters by
means of the inversion of the observed Stokes profiles employing the
Stokes Inversion based on Response functions (SIR) code. Finally, we
analyzed their evolution using a time series from the same instrument.
Results: Blue-shifted events tend to appear over bright regions
at the edge of granules, while red-shifted events are seen predominantly
over dark regions on intergranular lanes. Large linear polarization
signals can be seen in the region that connects them. The magnetic
structure inferred from the time series revealed that the structure
corresponds to a Ω-loop, with one footpoint always over the edge
of a granule and the other inside an intergranular lane. The physical
parameters obtained from the inversions of the observed Stokes profiles
in both events show an increase with respect to the Harvard-Smithonian
reference atmosphere in the temperature at log τ500
∈ (-1, -3) and a strong magnetic field, B ≥ 1 kG, at the bottom
of the atmosphere that quickly decreases upward until vanishing at log
τ500 ≈ -2. In the blue-shifted events, the LOS
velocities change from upflows at the bottom to downflows at the top of
the atmosphere. Red-shifted events display the opposite velocity
stratification. The change of sign in LOS velocity happens at the same
optical depth in which the magnetic field becomes zero.
Conclusions: The physical mechanism that best explains the inferred
magnetic field configuration and flow motions is a siphon flow along an
arched magnetic flux tube. Further investigation is required, however,
as the expected features of a siphon flow cannot be unequivocally
identified.
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