The effect of anthropogenic aerosol on the reflectivity of stratocumulus cloud decks through
changes in cloud amount is a major uncertainty in climate projections. In frequently …

General circulation models'(GCMs) estimates of the liquid water path adjustment to
anthropogenic aerosol emissions differ in sign from other lines of evidence. This reduces …

Quantification of the radiative adjustment of marine low clouds to aerosol perturbations,
regionally and globally, remains the largest source of uncertainty in assessing current and …

Marine stratocumuli cool the Earth effectively due to their high reflectance of incoming solar
radiation and persistent occurrence. The susceptibility of cloud albedo to droplet number …

Marine low-level clouds are key to the Earth's energy budget due to their expansive
coverage over global oceans and their high reflectance of incoming solar radiation. Their …

We explore the cloud system evolution of non-precipitating marine stratocumuli with a focus
on the impacts of the diurnal cycle and free-tropospheric (FT) humidity based on an …

Ship tracks in subtropical marine low clouds are simulated and investigated using large-
eddy simulations. Five variants of a shallow subtropical stratocumulus-topped marine …

The impact of aerosol number concentration on cloud albedo is a persistent source of
spread in global climate predictions due to multi-scale, interactive atmospheric processes …

The liquid water path (LWP) adjustment due to aerosol–cloud interactions in marine
stratocumulus remains a considerable source of uncertainty for climate sensitivity estimates …

Marine cloud brightening (MCB) has been proposed as a viable way to counteract global
warming by artificially increasing the albedo and lifetime of clouds via deliberate seeding of …