Abstract

Context. In a recent statistical study of sunspots in 79 active regions, the vertical magnetic field component Bver averaged along the umbral boundary is found to be independent of sunspot size. The authors of that study conclude that the absolute value of Bver at the umbral boundary is the same for all spots. Aims. We investigate the temporal evolution of Bver averaged along the umbral boundary of one long-lived sunspot during its stable phase. Methods. We analysed data from the HMI instrument on-board SDO. Contours of continuum intensity at Ic = 0.5Iqs, whereby Iqs refers to the average over the quiet sun areas, are used to extract the magnetic field along the umbral boundary. Projection effects due to different formation heights of the Fe I 617.3 nm line and continuum are taken into account. To avoid limb artefacts, the spot is only analysed for heliocentric angles smaller than 60°. Results. During the first disc passage, NOAA AR 11591, Bver remains constant at 1693 G with a root-mean-square deviation of 15 G, whereas the magnetic field strength varies substantially (mean 2171 G, rms of 48 G) and shows a long term variation. Compensating for formation height has little influence on the mean value along each contour, but reduces the variations along the contour when away from disc centre, yielding a better match between the contours of Bver = 1693 G and Ic = 0.5Iqs. Conclusions. During the disc passage of a stable sunspot, its umbral boundary can equivalently be defined by using the continuum intensity Ic or the vertical magnetic field component Bver. Contours of fixed magnetic field strength fail to outline the umbral boundary.

Highlights

  • The boundary between umbra and penumbra of sunspots has long been defined in terms of the continuum intensity Ic

  • We investigate the temporal evolution of Bver averaged along the umbral boundary of one long-lived sunspot during its stable phase

  • During the disc passage of a stable sunspot, its umbral boundary can equivalently be defined by using the continuum intensity Ic or the vertical magnetic field component Bver

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Summary

Introduction

That part of the umbral boundary was observed with Hinode/SP and a |Bver| value of 1810 G measured They propose that the umbral mode of magneto-convection prevails in areas with |Bver| > Bsvtearble, whereas outside, the penumbral mode takes over. Following this line of investigation, Jurcák et al (2017) studied a pore whose |Bver| remained below this critical value. They found that a developing penumbra completely cannibalized the pore, supporting the assertion that in umbral areas with |Bver| < Bsvtearble, the penumbral mode of magneto-convection takes over the umbral mode.

Data and analysis
Results
Temporal evolution
Contours
Effect of neglecting formation heights compensations
Conclusion
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