Low-level mixed-phase clouds occur frequently and persistently in the central Arctic, and thus play a key role in climate feedback mechanisms, air mass transformations, and sea ice melt. Turbulent entrainment at cloud top driven by radiative cooling modulates these clouds by affecting the boundary-layer heat budget. However, reliable measurements of this small-scale process are scarce. This study presents new insights into entrainment in radiatively-driven cloudy mixed-layers at high latitudes based on a library of daily large-eddy simulations covering the full MOSAiC drift. The simulations are based on measurements, cover a periodic and homogeneously-forced small domain representing conditions observed at the Polarstern Research Vessel, and resolve Arctic turbulence and clouds to a high degree. Approximately 1 out of 3 simulated days contain cloud mass in liquid phase. Drift-average heat budget analyses show that the full column is roughly in radiative-advective equilibrium. In contrast, the cloudy boundary layer is not, being dominated by cloud top cooling. Warming by top-entrainment only partially counters this cooling, at efficiencies of about 30 %. Such efficiencies are much lower compared to previous findings for subtropical warm marine stratocumulus. Interestingly, a few outlying MOSAiC cases show similarly high efficiencies. Analysis of turbulence energetics reveals that high entrainment efficiency can be achieved in two ways: surface coupling and strong local wind shear. The former explains the high efficiencies in the subtropics, while the latter drives the highest efficiencies encountered during MOSAiC. In general, these findings emphasize the important role played by wind shear in boosting entrainment efficiency.