Persistent structures in near-surface flows from ring diagrams

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PERSISTENT STRUCTURES IN NEAR- SURFACE FLOWS FROM RING DIAGRAMS RACHEL HOWE, UNIVERSITY OF BIRMINGHAM D. BAKER, L. HARRA, MSSL R. KOMM, NSO R. BOGART, STANFORD

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Persistent structures in near-surface flows from ring diagrams. Rachel Howe, University of Birmingham D. Baker, L. Harra , MSSL R. KomM , NSO R. Bogart, Stanford. Probing the sun inside and out. Leverhulme -funded project at MSSL 1 st Workshop June 2011. Introduction. - PowerPoint PPT Presentation

Transcript of Persistent structures in near-surface flows from ring diagrams

Page 1: Persistent structures in near-surface flows from ring diagrams

PERSISTENT STRUCTURES IN NEAR-

SURFACE FLOWS FROM RING DIAGRAMS

RACHEL HOWE, UNIVERSITY OF BIRMINGHAM

D. BAKER, L. HARRA, MSSL

R. KOMM, NSO

R. BOGART, STANFORD

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PROBING THE SUN INSIDE AND OUTLeverhulme-funded project at MSSL

1st Workshop June 2011

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INTRODUCTION

• The Sun has flows at many scales, from global rotation to flows around active regions and down to granules.

• Many of these show variations with solar cycle.

• Here we are looking for persistent structures in local flow features over an extended period.

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DIFFERENTIAL ROTATION

• 2D rotation profile, based on RLS inversions

• Faster near equator, slower at poles

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ANALYSIS

• Use synoptic maps of zonal/meridional flows from ring diagrams (GONG and HMI)

• Average over all depths

• At each latitude and rotation, we subtract mean over all times/longitudes to remove differential rotation and first-order temporal variations such as the torsional oscillation (as well as systematic effects)

• Then plot residuals as longitude—time maps

• Differential rotation causes features to drift in longitude from one rotation to the next.

• Features (e.g., flows into active regions/remnants) persisting for more than one rotation will show up as diagonal streaks

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GONG ZONAL VELOCITYLONGITUDE—TIME PLOTS

Note diagonal ‘grain’

Paired light-dark streaks suggest flows into or out of feature that drifts with differential rotation.

Slope up == faster than Carrington rate

Slope down == slower than C.R.

Shallower slope means more difference.

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GONG MERIDIONAL VELOCITY

Not much to see here – quieter at minimum?

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MDI/HMI MAGNETOGRAMS(Timescale of GONG)

Note slope of features differs from that seen in flows

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GONG ZONAL VELOCITYOn HMI timescale.

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HMI ZONAL VELOCITYNote strong stripes at high latitudes.

For common data, correlation with GONG is > 80%

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HMI MERIDIONAL VELOCITYSome grain visible here too.

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HMI MAGNETOGRAMS

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DIFFERENTIAL ROTATION

Use cross-correlation analysis to translate stripes slope to rotation rate

Green – Magnetograms

Black – Global inversions

Red – HMI ring vx correlation

Blue – GONG ring vx correlation

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DIFFERENTIAL ROTATION

Use cross-correlation analysis to translate stripes slope to rotation rate

Green – Magnetograms

Black – Global inversions

Red – HMI ring vx correlation

Blue – GONG ring vx correlation

Cyan – EIT 195 Angstrom correlation

Orange – GONG PFSS coronal hole maps

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HIGH-LATITUDE VX REWRAPPED WITH ESTIMATED VELOCITY

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HIGH-LATITUDE VX REWRAPPED WITH EST. VELOCITY -5 NHZ

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DISCUSSION

• Near-surface flows –especially zonal – show signatures of features persisting from a few to many rotations, migrating as would be expected from differential rotation.

• Low latitudes traceable to active region/plage?

• Rotation rate from magnetic features not quite the same as from flows – anchoring depth?

• High latitudes – Hathaway giant cells? Looks like an l=1 structure, anticorrelated n/s.

• Correlation analysis not good enough to pick up changes in differential rotation.