Additional Evidence Supporting a Model of Shallow, High-Speed Supergranulation
arXiv:1404.2533 · doi:10.1007/s11207-014-0537-3
Abstract
Recently, Duvall and Hanasoge ({\it Solar Phys.} {\bf 287}, 71-83, 2013) found that large distance separation travel-time differences from a center to an annulus implied a model of the average supergranular cell that has a peak upflow of at a depth of and a corresponding peak outward horizontal flow of at a depth of . In the present work, this effect is further studied by measuring and modeling center-to-quadrant travel-time differences , which roughly agree with this model. Simulations are analyzed that show that such a model flow would lead to the expected travel-time differences. As a check for possible systematic errors, the center-to-annulus travel-time differences are found not to vary with heliocentric angle. A consistency check finds an increase of with the temporal frequency by a factor of two, which is not predicted by the ray theory.
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Cited by in corpus (13)
- Seismic Sounding of Convection in the Sun
- Relation between trees of fragmenting granules and supergranulation evolution
- Helioseismic Investigation of Modeled and Observed Supergranule Structure
- Evolution and wave-like properties of the average solar supergranule
- Time-Distance Helioseismology of Two Realistic Sunspot Simulations
- Combined helioseismic inversions for 3D vector flows and sound-speed perturbations
- Plasma flows and sound-speed perturbations in the average supergranule
- Probabilistic Inversions for Time-Distance Helioseismology
- Validating Forward Modeling and Inversions of Helioseismic Holography Measurements
- Iterative inversion of synthetic travel times successful at recovering sub-surface profiles of supergranular flows
- Characterizing the spatial pattern of solar supergranulation using the bispectrum
- Observational characterisation of large-scale transport and horizontal turbulent diffusivity in the quiet Sun
- Exploiting solar visible-range observations by inversion techniques: from flows in the solar subsurface to a flaring atmosphere