Bibcode
Verma, M.; Denker, C.; Balthasar, H.; Kuckein, C.; Rezaei, R.; Sobotka, M.; Deng, N.; Wang, H.; Tritschler, A.; Collados, M.; Diercke, A.; Manrique, S. J. González
Referencia bibliográfica
Astronomy and Astrophysics, Volume 614, id.A2, 14 pp.
Fecha de publicación:
6
2018
Revista
Número de citas
17
Número de citas referidas
15
Descripción
Aims: Combining high-resolution spectropolarimetric and imaging
data is key to understanding the decay process of sunspots as it allows
us to scrutinize the velocity and magnetic fields of sunspots and their
surroundings. Methods: Active region NOAA 12597 was observed on
2016 September 24 with the 1.5-meter GREGOR solar telescope using
high-spatial-resolution imaging as well as imaging spectroscopy and
near-infrared (NIR) spectropolarimetry. Horizontal proper motions were
estimated with local correlation tracking, whereas line-of-sight (LOS)
velocities were computed with spectral line fitting methods. The
magnetic field properties were inferred with the "Stokes Inversions
based on Response functions" (SIR) code for the Si I and Ca I NIR lines.
Results: At the time of the GREGOR observations, the leading
sunspot had two light bridges indicating the onset of its decay. One of
the light bridges disappeared, and an elongated, dark umbral core at its
edge appeared in a decaying penumbral sector facing the newly emerging
flux. The flow and magnetic field properties of this penumbral sector
exhibited weak Evershed flow, moat flow, and horizontal magnetic field.
The penumbral gap adjacent to the elongated umbral core and the penumbra
in that penumbral sector displayed LOS velocities similar to
granulation. The separating polarities of a new flux system interacted
with the leading and central part of the already established active
region. As a consequence, the leading spot rotated 55° clockwise
over 12 h. Conclusions: In the high-resolution observations of a
decaying sunspot, the penumbral filaments facing the flux emergence site
contained a darkened area resembling an umbral core filled with umbral
dots. This umbral core had velocity and magnetic field properties
similar to the sunspot umbra. This implies that the horizontal magnetic
fields in the decaying penumbra became vertical as observed in
flare-induced rapid penumbral decay, but on a very different time-scale.
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