Fig. 5.

Radial inversion of αϕϕ as a function of Co for two latitudinal strips for the HD runs (Set H) (top row) and MHD runs (Set M) (bottom row). In the first column we average αϕϕ at low latitudes, i.e., ΔΘ1 = 10° −20°, and in the second column we average over mid latitudes ΔΘ2 = 50° −60°. The zero values are indicated with a white line. All values are normalized by .
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