Clouds are the primary source of uncertainty in the prediction of climate change. To reduce
the uncertainty of cloud simulations and overcome this difficulty in prediction, many climate …

While GCM horizontal resolution has received the majority of scale improvements in recent
years, ample evidence suggests that a model's vertical resolution exerts a strong control on …

This is the second part of the description and validation of the coupling of a warm‐rain
microphysics scheme to a stochastic multi‐plume eddy‐diffusivity/mass‐flux …

Strong wind events cause significant societal damage ranging from loss of property and
disruption of commerce to loss of life. Over portions of the United States, the strongest winds …

Strong wind events can cause severe economic loss and societal impacts. Peak winds over
Wyoming and Colorado occur during the wintertime months, and in the first part of this two …

An idealized case of gradual oceanic transition from shallow to deep convection is simulated
at three different horizontal resolutions: one that resolves most of the turbulent eddies, one …

Modern general circulation models continue to require parameterizations of subgrid
transport due to planetary boundary layer (PBL) turbulence and convection. Some schemes …

The atmospheric convection is a phenomenon that has a length scale smaller than the
resolution at which the state‐of‐the‐art general circulation numerical models are running …

The eddy–diffusivity/mass–flux (EDMF) approach is based on the unification of concepts
typically used for the parameterization of turbulence in the boundary layer (eddy–diffusivity) …

Resolving atmospheric turbulent and convective processes in global climate simulations is,
and will remain for decades, an intractable computational problem. The strong influence of …