Helioseismic Investigation of Modeled and Observed Supergranule Structure
K. DeGrave, J. Jackiewicz

TL;DR
This study compares the subsurface structure of an average supergranule derived from HMI data with a helioseismic flow model, revealing significant differences in depth extent and flow velocities, and highlighting limitations in current helioseismic techniques.
Contribution
It provides the first detailed comparison between observed supergranule structures and a helioseismic model, identifying key discrepancies and methodological limitations.
Findings
HMI supergranules are more extended in depth than models suggest.
Observed flow velocities are much smaller than model predictions.
Systematic inaccuracies in helioseismic techniques are confirmed.
Abstract
The subsurface structure of an "average" supergranule is derived from existing HMI pipeline time-distance data products and compared to the best helioseismic flow model detailed in Duvall and Hanasoge (2013). We find that significant differences exist between them. Unlike the shallow structure predicted by the model, the average HMI supergranule is very extended in depth, exhibiting horizontal outflow down to --~Mm, followed by a weak inflow reaching a depth of ~Mm below the photosphere. The maximal velocities in the horizontal direction for the average supergranule are much smaller than the model, and its near-surface flow field RMS value is about an order of magnitude smaller than the often-quoted values of ~ for supergranulation. Much of the overall HMI supergranule structure and its weak flow amplitudes can be explained by examining the…
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.
