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Previous work has established that both buoyancy and shear are important in determining the rate of entrainment and the growth of the boundary layer through the transition. Here, we examine the impact of including longwave radiation in the simulations. Radiative cooling of the residual layer and smoothing of the temperature profile around the top of the SBL reduce the strength of the inversion above the developing mixed layer, leading to significantly faster growth of the mixed layer later in the transition. The resulting deeper and drier mixed layer exhibits better agreement with the observations.
We also discuss the impact of longwave radiation on the characteristics of the turbulence and compare the diagnosed entrainment rates with those predicted using some published parametrizations.