Fig. 5.

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(a) Dispersion relation of the HHS22 modes computed for different values of superadiabaticity near the surface δsf. The bulk of the convection zone is assumed to be adiabatic, δcz = 0. (b–e) Eigenfunctions of the m = 10 HHS22 mode computed for δsf = 10−6 (left column) and for δsf = 10−3 (right column). Panels b–d show cuts of radial velocity vr (in m s−1), entropy perturbation s1 (in erg g−1 K−1), and z-vorticity ζz (in 10−8 s−1) in the equatorial plane (along the rotational axis) seen from the north pole. The black dashed curves denote the height r = 0.95 R⊙, above which the strongly superadiabatic layer is located. (e) Mollweide projection of the radial vorticity eigenfunction ζr at the top boundary r = 0.985 R⊙ (in 10−8 s−1). All the eigenfunctions are normalized in the same way as in Fig. 2.
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