Aerosols interact with radiation and clouds. Substantial progress made over the past 40
years in observing, understanding, and modeling these processes helped quantify the …

Abstract The Energy Exascale Earth System Model Atmosphere Model version 1, the
atmospheric component of the Department of Energy's Energy Exascale Earth System …

The effect of an increase in atmospheric aerosol concentrations on the distribution and
radiative properties of Earth's clouds is the most uncertain component of the overall global …

Aerosol–cloud interactions have a potentially large impact on climate but are poorly
quantified and thus contribute a substantial and long-standing uncertainty in climate …

There is debate about slowing of the Atlantic Meridional Overturning Circulation (AMOC), a
key component of the global climate system. Some focus is on the sea surface temperature …

Aerosol–cloud interactions (ACIs) are considered to be the most uncertain driver of present-
day radiative forcing due to human activities. The nonlinearity of cloud-state changes to …

The cloud droplet number concentration (N d) is of central interest to improve the
understanding of cloud physics and for quantifying the effective radiative forcing by aerosol …

A new climate model, HadGEM3 N96ORCA1, is presented that is part of the GC3. 1
configuration of HadGEM3. N96ORCA1 has a horizontal resolution of~ 135 km in the …

Isolating the Evolving Contributions of Anthropogenic Aerosols and Greenhouse Gases: A New
CESM1 Large Ensemble Community Resource in: Journal of Climate Volume 33 Issue 18 …

The cooling of the Earth's climate through the effects of anthropogenic aerosols on clouds
offsets an unknown fraction of greenhouse gas warming. An increase in the amount of water …