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Christian Barthlott and Corinna Hoose

.g., heat bubble, cold pool, mountain) is needed to initiate convection. As was pointed out by Noppel et al. (2010) , such idealized simulations often show different sensitivities of aerosol–cloud interactions than the simulation of real cases. In this paper, we expand this line of investigation by performing convection-resolving simulations of real weather events, but applying a novel technique of systematically modifying temperature profiles of the initial and boundary data. The modified temperature

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