arXiv · 1301.1821
An Average Supergranule: Much Larger Vertical Flows Than Expected
Abstract
Supergranules are believed to be an evidence for large-scale subsurface convection. The vertical component of the supergranular flow field is very hard to measure, but it is considered only a few m/s in and below the photosphere. Here I present the results of the analysis using three-dimensional inversion for time-distance helioseismology that indicate existence of the large-magnitude vertical upflow in the near sub-surface layers. Possible issues and consequences of this inference are also discussed.
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Michal Svanda. 2013-01-09. An Average Supergranule: Much Larger Vertical Flows Than Expected. https://arxiv.org/abs/1301.1821
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