“…At lower latitudes, they propagate upward from the bottom of the convection zone, and form almost stationary oscillatory patterns in the subsurface layer, the depth of which increases with the latitude decrease. These effects qualitatively correspond to the results of our recent helioseismology analysis (Kosovichev & Pipin 2019). Snapshots for a half of the model M1 dynamo cycle of: a) the toroidal magnetic field (background image) and streamlines of the poloidal field (contours); b) variations of the zonal acceleration (background image) and the azimuthal force caused by variations of the meridional circulation, δFU , (contour lines are plotted in the range ±50 m/s 2 ); c) variations of the azimuthal velosity and contours show streamlines of the meridional circulation, dashed lines are for the counter clockwise circulation; d) the azimuthal force caused by the dynamo-induced Λ-effect, δF H (0,ρ) (density stratification, background image), δF H (0,a) (effect of anisotropy, contours are in the same range of magnitudes), see the Eqs (10) in the upper part of the convection zone and downward in the tachocline.…”