The convection–cloud chamber enables measurement of aerosol and cloud microphysics,
as well as their interactions, within a turbulent environment under steady‐state conditions …

The effect of aerosols on the properties of clouds is a large source of uncertainty in
predictions of weather and climate. These aerosol‐cloud interactions depend critically on …

Collisional growth of cloud droplets is an essential yet uncertain process for drizzle and
precipitation formation. To improve the quantitative understanding of this key component of …

In a quest to represent the Earth system, climate models have become more and more
complex. This generates problems, for example, hindering model interpretability. This study …

The traditional approach of using the Monin–Obukhov similarity theory (MOST) to model
near-surface processes in large-eddy simulations (LESs) can lead to significant errors in …

Entrainment of subsaturated air into a cloud can influence its optical and microphysical
properties in various ways, depending on the droplet evaporation and turbulent mixing time …

The role played by fluctuations of supersaturation in the growth of cloud droplets is
examined in this study. The stochastic condensation framework and the three regimes of …

Recent in situ observations show that haze particles exist in a convection cloud chamber.
The microphysics schemes previously used for large‐eddy simulations of the cloud chamber …

Mixed-phase clouds affect precipitation and radiation differently from liquid and ice clouds,
posing greater challenges to their representation in numerical simulations. Recent …

A linear non‐diffusive algorithm for advective transport is developed that greatly improves
the detail at which aerosols and clouds can be represented in atmospheric models. Linear …