PI Chamber Simulation Case: Modeling Aerosol-Cloud-turbulence Interactions in the Cloud Chamber

The cases proposed here are focused on the cloud-aerosol-turbulence interactions in a warm cloudy environment, i.e., no ice particles. Modeling results from DNS, LES, and other numerical/theoretical models are all welcomed.
You will find more information here

Isolated cumulus congestus based on SCMS campaign: comparison between Eulerian bin and Lagrangian particle-based microphysics

Width of the droplet size distribution affects radiative properties of warm (ice-free) clouds and likely impacts formation of precipitation through collision/coalescence. One can argue that warm rain formation in bin microphysics models is affected by artificial spectral broadening in bin schemes (Morrison et al. 2018, Grabowski et al. 2019).
You will find more information here

Aerosol effect in deep convective clouds under different monsoon environments over the Indian peninsula: a CAIPEEX-Case study

Investigate the small and large domain impact on aerosol effect with a LES/CRM model using model outputs from weather model and investigate the impact on mixed-phase cloud processes in the polluted conditions.
You will find more information here

Convection in Strong Vertical Wind Shear: The 2 Aug COPE Case

The proposed modeling exercise is to conduct simulations of this case with various idealized modeling frameworks to gain insight on:

• • the effects of strong vertical wind shear on microphysical processes (e.g. collisioncoalescence, ice production, riming, rime-splintering, evaporation of falling hydrometeors, etc.)
• • the effects of strong vertical wind shear upon different representations of microphysical processes used in numerical models
  You will find more information here