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Emergence and Evolution of Active Regions

Emergence and Evolution of Active Regions. C. Birch, H. Schunker (MPS), D. C. Braun (NWRA). Motivations. How does active region emergence work? Where do AR come from? How do emerging AR interact with convection? What are the flows associated with AR? Constrain dynamo models

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Emergence and Evolution of Active Regions

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  1. Emergence and Evolution of Active Regions C. Birch, H. Schunker (MPS), D. C. Braun (NWRA)

  2. Motivations • How does active region emergence work? • Where do AR come from? • How do emerging AR interact with convection? • What are the flows associated with AR? • Constrain dynamo models • Potentially rule out certain models (rising flux tubes?) • Converging flows associated with AR play a role in some dynamo models (e.g. Cameron & Schuessler, 2012)

  3. Previous work • Pre-emergence case studies: • Braun (1995, Hankel analysis) • Jensen et al. (2001, time-distance) • Hartlep et al. (2011, acoustic power) • Ilonidis et al. (2011, time-distance) • Many others … • Statistical studies • Komm et al. (2009, 2011, rings, 100s of regions) • Birch et al. (2013, holography, ~100 regions one day before emergence) • Open questions remain

  4. HMI Data selection • Presented by Hannah in previous talk • Additional constraints: • Less then 40 deg from central meridian • Duty cycle > 90% • Result: subsample of about 60 emerging AR

  5. Helioseismic Holography • This talk: surface focusing measurements (lower turning point 3 Mm) • Strategy: • Carry out holography for disk passage of all emerging AR and quiet Sun control regions • find clear signals first and then think about inversions

  6. Supergranulation is the dominant signal Blue = divergence; red= convergence Contours of B: 20, 40, 60 G

  7. No clear signal in individual mapsNext step: ensemble averages (60 regions)

  8. Average over AR IMPORTANT! Blue = flow towards emergence location Red = flow away from emergence location rms = 15 m/s

  9. Average over QS IMPORTANT! Blue = flow towards emergence location Red = flow away from emergence location rms = 15 m/s

  10. QS AR

  11. Average over AR

  12. Average over AR

  13. Average over AR Converging flow! Note offset.

  14. Zoom in t = -13 hr AR Max. flow 100 m/s Inner circle: 30 Mm radius

  15. AR QS

  16. Average over AR B contours 50, 100, 150 G

  17. Average over AR

  18. Average over AR

  19. Zoom in t = 34 hr AR Max. flow 150 m/s Inner circle: 30 Mm radius

  20. EW cut as a function of time:there is a feature before emergence m/s 30 m/s feature Noise ~ 10 m/s Lowest B contour 40 G Heavy contour 120 G

  21. Quiet Sun noise level ~ 10 m/s m/s

  22. NS cut shows converging flow before and during emergence m/s Lowest B contour 40 G Heavy contour 120 G

  23. Quiet Sun: noise ~ 10 m/s m/s

  24. Conclusions • There is a clear pre-emergence signature: • Near-surface flows of ~100 m/s • Converging to a location ~15 Mm East • Exists days before emergence • Flow pattern during emergence: • ~150 m/sprograde/equatorward flow in leading polarity • ~100 m/s NS converging flow between the polarities

  25. Next steps • Refine the meaning of control region • pre-emergence signature dominated by preferential emergence location within the supergranulation pattern? • Control for supergranulation pattern. • Comparison with simulations?  Doug’s talk • Deep signal?  Doug’s talk

  26. The end

  27. QS11079 and AR11079

  28. A single AR

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