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Fig. 2.

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Vertical slices at r = 5.5 au in the initial hydrostatic state. Top panel: temperature profiles. Middle panels: RzΩ2 profiles compared to the corresponding values for a vertically isothermal disk (Ω = Ωiso), and different terms contributing to the vertical shear in Eq. (5) for fdg = 10−3 (second from the top) and 10−4 (third from the top) in units of the local squared Keplerian frequency . Bottom panel: squared vertical Brunt-Väisälä frequency for both fdg values in units of (solid lines) compared to their values for vertically isothermal disks (dotted lines).

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