The Rise of Active Region Flux Tubes in the Turbulent Solar Convective Envelope
Maria A. Weber, Yuhong Fan, Mark S. Miesch

TL;DR
This study models the buoyant rise of magnetic flux tubes in the solar convection zone, revealing how convection influences their emergence, tilt, and properties, with results aligning with observed solar active regions.
Contribution
It demonstrates how convection affects flux tube emergence, showing that mid-range field strengths produce properties consistent with solar observations.
Findings
Rise times are reduced from years to months with convection.
Emerging loops at certain field strengths follow Joy's Law.
Flux tube properties match observed active regions at 40-50 kG.
Abstract
We use a thin flux tube model in a rotating spherical shell of turbulent convective flows to study how active region scale flux tubes rise buoyantly from the bottom of the convection zone to near the solar surface. We investigate toroidal flux tubes at the base of the convection zone with field strengths ranging from 15 kG to 100 kG at initial latitudes ranging from 1 degree to 40 degrees with a total flux of 10^22 Mx. We find that the dynamic evolution of the flux tube changes from convection dominated to magnetic buoyancy dominated as the initial field strength increases from 15 kG to 100 kG. At 100 kG, the development of Omega-shaped rising loops is mainly controlled by the growth of the magnetic buoyancy instability. However, at low field strengths of 15 kG, the development of rising Omega-shaped loops is largely controlled by convective flows, and properties of the emerging loops…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsSolar and Space Plasma Dynamics · Geomagnetism and Paleomagnetism Studies · Oceanographic and Atmospheric Processes
