no code implementations • 3 Mar 2021 • D. C. Braun, A. C. Birch, Y. Fan
We apply the helioseismic methodology of Legendre Function Decomposition to 88 months of Dopplergrams obtained by the Helioseismic and Magnetic Imager (HMI) as the basis of inferring the depth variation of the mean meridional flow, as averaged between 20 and 60 degrees latitude and in time, in both the northern and southern hemispheres.
Solar and Stellar Astrophysics
