Three-dimensional cloud simulations show that crossing the Guillot humidity threshold in low-mean-molecular-weight atmospheres collapses the dry boundary layer into a superadiabatic cloudy layer.
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Resolved convection in hydrogen-rich atmospheres
Three-dimensional cloud simulations show that crossing the Guillot humidity threshold in low-mean-molecular-weight atmospheres collapses the dry boundary layer into a superadiabatic cloudy layer.