Bibcode
Requerey, I. S.; Del Toro Iniesta, Jose Carlos; Bellot Rubio, Luis R.; Bonet, J. A.; Martínez Pillet, V.; Solanki, Sami K.; Schmidt, Wolfgang
Referencia bibliográfica
The Astrophysical Journal, Volume 789, Issue 1, article id. 6, 12 pp. (2014).
Fecha de publicación:
7
2014
Revista
Número de citas
36
Número de citas referidas
31
Descripción
Isolated flux tubes are considered to be fundamental magnetic building
blocks of the solar photosphere. Their formation is usually attributed
to the concentration of magnetic field to kG strengths by the convective
collapse mechanism. However, the small size of the magnetic elements in
quiet-Sun areas has prevented this scenario from being studied in fully
resolved structures. Here, we report on the formation and subsequent
evolution of one such photospheric magnetic flux tube, observed in the
quiet Sun with unprecedented spatial resolution (0.''15-0.''18) and high
temporal cadence (33 s). The observations were acquired by the Imaging
Magnetograph eXperiment on board the SUNRISE balloon-borne solar
observatory. The equipartition field strength magnetic element is the
result of the merging of several same polarity magnetic flux patches,
including a footpoint of a previously emerged loop. The magnetic
structure is then further intensified to kG field strengths by
convective collapse. The fine structure found within the flux
concentration reveals that the scenario is more complex than can be
described by a thin flux tube model with bright points and downflow
plumes being established near the edges of the kG magnetic feature. We
also observe a daisy-like alignment of surrounding granules and a
long-lived inflow toward the magnetic feature. After a subsequent
weakening process, the field is again intensified to kG strengths. The
area of the magnetic feature is seen to change in anti-phase with the
field strength, while the brightness of the bright points and the speed
of the downflows varies in phase. We also find a relation between the
brightness of the bright point and the presence of upflows within it.
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