Abstract
Magnetoconvection can produce an active region without an initial coherent flux tube. A simulation was performed where a uniform, untwisted, horizontal magnetic field of 1kG strength was advected into the bottom of a computational domain 48 Mm wide by 20 Mm deep. The up and down convective motions produce a hierarchy of magnetic loops with a wide range of scales, with smaller loops riding "piggy-back" in a serpentine fashion on larger loops. When a large loop approaches the surface, it produces a small active region with a compact leading spot and more diffuse following spots.
Originalsprog | Engelsk |
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Tidsskrift | The Astrophysical Journal Letters |
Vol/bind | 753 |
Udgave nummer | 1 |
Sider (fra-til) | L13 |
ISSN | 0004-637X |
DOI | |
Status | Udgivet - 1 jul. 2012 |