Fig. 3

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(a) Properties of a vertical slice in the circumplanetary disk at the centrifugal radius, from five pressure scale heights (left) to the midplane (right). Evolution of the abundance of H2O, NH3 and CO2 ice as the parcel of gas and dust sinks to the midplane after accretion in the reset case: (b) in the partial reset case (c) and the inheritance case (d). Solid lines trace the relevant properties and abundances for the low viscosity (tvisc = 104 yr) case and the dashed line describes the high viscosity (tvisc = 103 yr) case.
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