Microphysical influence on cloud radiative effect during New Mexico deep convective cloud cases

Cloud feedbacks associated with anvil cirrus are some of the most uncertain. The Deep Convective Microphysics EXperiment (DCMEX) aims to reduce this uncertainty by improving the representation of microphysical processes in climate models. In support of this aim, we present analysis of the cloud radiative properties from cloud-resolving simulations with the Met Office Unified Model (UM). We apply the Cloud AeroSol Interacting Microphysics (CASIM) module within the UM.