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Data · dataset · 2026

Validating time-distance helioseismology with realistic quiet-sun simulations

Listed in National Center for Atmospheric Research

Linear time-distance helioseismic inversions are carried out for vector flow velocities using travel times measured from two ~100² Mm² × 20 Mm realistic magnetohydrodynamic quiet-Sun simulations of about 20 hr.

Description

The goal is to test current seismic methods on these state-of-the-art simulations. Using recent three-dimensional inversion schemes, we find that inverted horizontal flow maps correlate well with the simulations in the upper ~3 Mm of the domains for several filtering schemes, including phase-speed, ridge, and combined phase-speed and ridge measurements.

In several cases, however, the velocity amplitudes from the inversions severely underestimate those of the simulations, possibly indicating nonlinearity of the forward problem. We also find that, while near-surface inversions of the vertical velocities are best using phase-speed filters, in almost all other example cases these flows are irretrievable due to noise, suggesting a need for statistical averaging to obtain better inferences.

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Geophysics 73%
Provenance · 1 source records, 8 field assertions
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National Center for Atmospheric Research0329770f-b27e-494d-8d9b-3f02d260fef511 d agoJSON v1
FieldAssertionExtractorEvidence
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concepts[field].local:field:ocean-atmosphericmapping · data ucar educonnector:data_ucar_edu@1.0.0
created_datesource · data ucar educonnector:data_ucar_edu@1.0.0
descriptionsource · data ucar educonnector:data_ucar_edu@1.0.0/notes
publication_datesource · data ucar educonnector:data_ucar_edu@1.0.0
titlesource · data ucar educonnector:data_ucar_edu@1.0.0/title
updated_datesource · data ucar educonnector:data_ucar_edu@1.0.0