Aerosol nucleation and its role for clouds and Earth's radiative forcing in the aerosol-climate model ECHAM5-HAM
Aerosol size-dependent below-cloud scavenging by rain and snow in the ECHAM5-HAM
Aerosols perturb mixed-phase microphysics and anvil radiative effects in deep convection
Atmospheric Chemistry and Physics Discussions European Geosciences Union