The climatic relevance of aerosol–cloud interactions depends on the sensitivity of the radiative effect of clouds to cloud droplet number inline-formulaN, and liquid water path LWP. We derive the dependence of cloud fraction CF, cloud albedo inline-formulaAC, and the relative cloud radiative effect inline-formula
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on inline-formulaN and LWP from 159 large-eddy simulations of nocturnal stratocumulus. These simulations vary in their initial conditions for temperature, moisture, boundary-layer height, and aerosol concentration but share boundary conditions for surface fluxes and subsidence. Our approach is based on Gaussian-process emulation, a statistical technique related to machine learning. We succeed in building emulators that accurately predict simulated values of CF, inline-formulaAC, and rCRE for given values of inline-formulaN and LWP. Emulator-derived susceptibilities inline-formula
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and inline-formula
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cover the nondrizzling, fully overcast regime as well as the drizzling regime with broken cloud cover. Theoretical results, which are limited to the nondrizzling regime, are reproduced. The susceptibility inline-formula
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captures the strong sensitivity of the cloud radiative effect to cloud fraction, while the susceptibility inline-formula
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describes the influence of cloud amount on cloud albedo irrespective of cloud fraction. Our emulation-based approach provides a powerful tool for summarizing complex data in a simple framework that captures the sensitivities of cloud-field properties over a wide range of states.