Sahel rainfall is dynamically linked to the global Hadley cell and to the regional monsoon
circulation. It is therefore susceptible to forcings from remote oceans and regional land alike …

The AR5 concluded that human influence on the climate system is clear, evident from
increasing greenhouse gas concentrations in the atmosphere, positive radiative forcing …

Working Group I (WGI) of the Intergovernmental Panel on Climate Change (IPCC) assesses
the current evidence on the physical science of climate change, evaluating knowledge …

Weather and climate models approximate diabatic and sub‐grid‐scale processes in terms of
grid‐scale variables using parameterizations. Current parameterizations are designed by …

Convective parameterization is the long-lasting bottleneck of global climate modelling and
one of the most difficult problems in atmospheric sciences. Uncertainty in convective …

More than one hundred days were simulated over very large domains with fine (0.156 km to
2.5 km) grid spacing for realistic conditions to test the hypothesis that storm (kilometer) and …

Overestimation of precipitation frequency and duration while underestimating intensity, that
is, the “drizzling” bias, has been a long‐standing problem of global climate models. Here we …

This study demonstrates the maturing ability of the half‐hourly precipitation estimates from
the Integrated Multi‐satellitE Retrievals for GPM (IMERG) for use in global analyses of the …

This paper describes the first implementation of the Δx= 3.25 km version of the Energy
Exascale Earth System Model (E3SM) global atmosphere model and its behavior in a 40 …

We present the System for High‐resolution prediction on Earth‐to‐Local Domains (SHiELD),
an atmosphere model developed by the Geophysical Fluid Dynamics Laboratory (GFDL) …