Angular velocity ⟨ω″⟩+δω″ at the equator from a TIDES calculation for the model that is used to evaluate the shear instabilities (Case 41 in Table 2). The curves correspond to the ten layers used in these calculations, with dashes corresponding to layers closest to the surface, r/R_⊙ = 5.0 and 5.3. The abscissa is azimuth angle measured in degrees with φ′ = 0 corresponding to the sub-binary longitude.