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Differences between central and peripheral umbral dots
Michal Sobotka1
Jan Jurcak2,1
SXT seminar, 2008/10/10, NAOJ
Astronomical Institute, Academy of Sciences of the Czech Republic
National Astronomical Observatory of Japan
Observations
Sunspot NOAA 10944 observed with Hinode SOT on February 27, 2007 between 12:00 UT and 15:00 UT. Heliocentric angle around 13 deg.
G-band images taken with cadence of 1min. 8” x 16”
Observations
Sunspot NOAA 10944 observed with Hinode SOT on February 27, 2007 between 12:00 UT and 15:00 UT. Heliocentric angle around 13 deg.
Repetitive scanning of 10” wide area with SP (normal mode).
SIR inversion
34 consecutive SP scans of area with the size of 50 x 100 pixels was inverted.
The standard version of the SIR code was used.
One-component model of atmosphere considered.
No stray-light taken into account (so far).
We allowed for the changes of plasma parameters with height. Five nodes was used for the temperature, magnetic field strength and inclination, and LOS velocity.
The results were studied at two different layers:
low atmosphere: averaged between log(tau)= -0.2 and -0.5
high atmosphere: averaged between log(tau)= -1.4 and -2.0
Maps of plasma parameters
LOWATMOSPHERE
HIGHATMOSPHERE
Penumbral grain
Event – low atmosphere
Surroundings – low atmosphere
Event – high atmosphere
Surroundings – high atmosphere
Penumbral grain – peripheral umbral dot
Event – low atmosphere
Surroundings – low atmosphere
Event – high atmosphere
Surroundings – high atmosphere
Peripheral umbral dot
Event – low atmosphere
Surroundings – low atmosphere
Event – high atmosphere
Surroundings – high atmosphere
Central umbral dot
Event – low atmosphere
Surroundings – low atmosphere
Event – high atmosphere
Surroundings – high atmosphere
Conclusions
Conclusions
In the low photosphere, CUDs have a weaker B and their LOS velocity and inclination do not differ from the surroundings.
In PGs, B is reduced with respect to the surroundings. PGs show strong upflows of 1 km/s and the magnetic field is more horizontal. PGs move into the umbra with horizontal velocities of about 400 m/s.
PUDs have a substantially higher T and a weaker B than in the surrounding umbra. They conserve the characteristic vertical upflows of PGs and higher field inclination compared to the surroundings. These parameters decreasegradually during the motion of PUDs into the umbra. The speed of horizontal motion of PUDs is practically equal to that of PGs.
In the high photosphere, the differences between the bright features and their surroundings are not so significant. The temperature excess in PUDs indicates that PUDs can penetrate higher in the photosphere than CUDs.
Evidence of convective rolls in a sunspot penumbra
V. Zakharov, J. Hirzberger, T. L. Riethmüller, S. K. Solanki, and P. Kobel
Max-Planck-Institut für Sonnensystemforschung, 37191 Katlenburg-Lindau, Germany
ObservationsNOAA 10904
2006/08/13
Θ= 40.5 deg
2 hour long sequence
SP data obtained withSolar Optical Universal Polarimeter
6 wavelengths in 123 s[-150, -75, 0, 75,150, 250]
ME inversion appliedHeLIx code
Orientation of the filament: 21 deg with the respect to the nearest limb (sin 21=0.36)
Results
Limb side of the filament shows: Center side of the filament: Velocity Blueshift Weak redshiftField strength Weker filed Strong fieldInclination Almost horizontal More verticalAzimuth Points toward the limb (20 deg) Parallel to the filament
Results
Conclusions