Marine boundary layer cloud regimes and POC formation in an LES coupled to a bulk aerosol scheme

The foremost challenge in parameterizing subgrid convective clouds and cloud systems in large-scale models is the many coupled, physical processes (i.e., radiation and surface

Simulated aerosol size distributions are in reasonable agreement with obser- vations in the marine boundary layer and in the free troposphere, while the model underestimates

We perturb aerosol and meteorological properties within an observationally-constrained LES and determine the cloud response, focusing on changes in liquid water path (LWP), bulk

Warm cloud processes in the Purdue Lin scheme (Chen and Sun, 2002) were modified in the source-oriented WRF / Chem (SOWC) model to investigate the impact of aerosol mixing state on

The precipitation formation and changes in microphysical variables were investigated for a liquid cloud in the tropics (EPIC campaign) and a multi-layer mixed-phase cloud over

In this paper, an analytical solution to calculate the removal of ma- terial from a bulk to a surface layer in aerosol particles has been derived using a well established and

di ff erences due to cloud parameterization schemes, in CTL and MAC, the other is the influence of aerosol activation and associated cloud particle numbers and sizes; how- ever, the

Intuitively, an increase in the emission of primary aerosol and DMS emission in the Arctic summer should cause an increase in aerosol abundance, AOD and cloud condensation nuclei