Time-Dependence of Subsurface Solar Convection Using the Time-Distance Deep-Focus Method
John T. Stefan, Alexander G. Kosovichev, Gustavo Guerrero, Andrey M. Stejko
TL;DR
The study re-evaluates the deep-focus time-distance helioseismology approach for measuring subsurface solar convection near $ ilde{0.96 R_\odot$ ($\\sim 30$ Mm) by validating with GALE and EULAG simulations and applying the method to Solar Cycle 24 data. It demonstrates that the inferred convective power spectrum is reliable up to $\\ell \\approx 15$–$20$ before diverging from ground truth at higher angular degrees, and finds modest cycle-related variations with an average spectrum about $0.5$ dex higher than earlier estimates. Despite the improved calibration, the results do not resolve the Convective Conundrum, indicating persistent gaps between observations and global convection simulations. The work also outlines a plan to cross-validate with ring-diagram analyses to better constrain the subsurface convection power spectrum and guide future modeling efforts.
Abstract
We re-examine the deep-focus methodology of time-distance helioseismology previously used to estimate the power spectrum of the solar convection at a depth of about 30 Mm, which was found to be significantly weaker than predicted by theory and simulations. The Global Acoustic, Linearized Euler (GALE) and Eulerian Lagrangian (EULAG) codes are used to generate ground-truth simulations to evaluate the accuracy of the inferred convective power spectrum. This validation process shows that the power spectrum derived using the time-distance methodology diverges significantly from ground truth beyond spatial scales corresponding to the spherical harmonic degree $\ell=15$--$30$ because of the limited resolution of helioseismic measurements at that depth. However, the power estimated at larger spatial scales ($\ell<15$) is sufficiently accurate. We then apply the methodology to solar data selected from throughout Solar Cycle 24 and find some evidence that the magnitude of the convective power changes throughout the Cycle. An average of the convective power across the Solar Cycle reveals a spectrum that is qualitatively similar to previous estimates, though about half an order of magnitude greater. The disagreement between observations of solar convection and the magnitudes predicted by simulations persists.
