The representation of moist convection in climate models represents a major challenge, due to the small scales involved. Using horizontal grid spacings of O(1km), convection-resolving weather and climate models allows one to explicitly resolve deep convection. However, due to their extremely demanding computational requirements, they have so far been limited to short simulations and/or small computational domains. Innovations in supercomputing have led to new hybrid node designs, mixing conventional multi-core hardware and accelerators such as graphics processing units (GPUs). One of the first atmospheric models that has been fully ported to these architectures is the COSMO (Consortium for Small-scale Modeling) model. Here we present the...
AbstractWe present a survey of physical and computational techniques that have the potential to cont...
As the demand for higher resolution and more accurate weather and climate simulations increases, the...
This paper describes the first implementation of the Δx = 3.25 km version of the Ener...
Currently comprehensive efforts are underway to refine the horizontal resolution of global and regio...
Classical numerical models for the global atmosphere, as used for numerical weather forecasting or c...
The computational cost still remains a limiting factor for performing convection-permitting climate ...
Weather and climate models applied with sufficiently fine mesh grids to enable a large part of atmos...
Here we present the first multi-model ensemble of regional climate simulations at kilometer-scale ho...
We present an analysis of the performance aspects of an atmospheric general circulation model at the...
Precipitation has a large impact on the society resulting in a high demand for precipitation project...
The increase in computing power and recent model developments allow for the use of global kilometer-...
The Model for Prediction Across Scales (MPAS) is a novel set of Earth system simulation components a...
Diurnal moist convection is an important element of summer precipitation over Central Europe and the...
The best hope for reducing long-standing global climate model biases is by increasing resolution to...
We present a survey of physical and computational techniques that have the potential to contribute t...
AbstractWe present a survey of physical and computational techniques that have the potential to cont...
As the demand for higher resolution and more accurate weather and climate simulations increases, the...
This paper describes the first implementation of the Δx = 3.25 km version of the Ener...
Currently comprehensive efforts are underway to refine the horizontal resolution of global and regio...
Classical numerical models for the global atmosphere, as used for numerical weather forecasting or c...
The computational cost still remains a limiting factor for performing convection-permitting climate ...
Weather and climate models applied with sufficiently fine mesh grids to enable a large part of atmos...
Here we present the first multi-model ensemble of regional climate simulations at kilometer-scale ho...
We present an analysis of the performance aspects of an atmospheric general circulation model at the...
Precipitation has a large impact on the society resulting in a high demand for precipitation project...
The increase in computing power and recent model developments allow for the use of global kilometer-...
The Model for Prediction Across Scales (MPAS) is a novel set of Earth system simulation components a...
Diurnal moist convection is an important element of summer precipitation over Central Europe and the...
The best hope for reducing long-standing global climate model biases is by increasing resolution to...
We present a survey of physical and computational techniques that have the potential to contribute t...
AbstractWe present a survey of physical and computational techniques that have the potential to cont...
As the demand for higher resolution and more accurate weather and climate simulations increases, the...
This paper describes the first implementation of the Δx = 3.25 km version of the Ener...