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Published on: December 3, 2019
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The solar dynamo begins near the surface.
Geoffrey M Vasil1, Daniel Lecoanet2,3, Kyle Augustson2,3
1School of Mathematics and the Maxwell Institute for Mathematical Sciences, University of Edinburgh, Edinburgh, UK. gvasil@ed.ac.uk.
Nature
|May 22, 2024
Summary
The Sun's magnetic dynamo cycle may originate in its near-surface shear layer, not deep within. This finding challenges traditional models and could improve space weather predictions.
Area of Science:
- Solar physics
- Plasma astrophysics
- Heliophysics
Background:
- The Sun's 11-year magnetic dynamo cycle involves sunspot migration and torsional oscillations.
- Previous theories proposed deep solar origins for these phenomena.
- Helioseismology localizes torsional oscillations to the Sun's near-surface shear layer.
Purpose of the Study:
- To investigate whether the solar dynamo is a near-surface instability.
- To challenge traditional models focusing on the solar tachocline.
Main Methods:
- Analysis of helioseismology data to pinpoint torsional oscillations.
- Development of simple analytic estimates for near-surface magneto-rotational instability.
- Conducting state-of-the-art numerical simulations.
Main Results:
- The near-surface magneto-rotational instability model better explains torsional oscillation scales and subsurface magnetic field amplitudes.
- Numerical simulations corroborate analytic estimates.
- Simulations reproduce hemispherical magnetic current helicity laws.
Conclusions:
- The solar dynamo is likely a near-surface instability.
- This finding contrasts with traditional models.
- Understanding this near-surface phenomenon can enhance predictions of solar magnetic cycles and space weather.
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