Convective parameterizations in general circulation models (GCMs) generally only aim to simulate the mean or first-order moment of convection; higher moments associated with subgrid variability are not explicitly considered. In this study, an empirically based stochastic convective parameterization is developed that uses an assumed mixed lognormal distribution of rainfall, tuned with parameter values derived from observations, to control selected nonmean statistical properties of convection. Testing of this stochastic convective parameteri-zation reveals that large-scale model dynamics interacts heavily with the convective parameterization, in ways such that the resulting output is fundamentally different from the input. This suggests stoch...
The representation of convection in large-scale models remains one of the most difficult problems in...
The last decade has seen the success of stochastic parameterizations in short-term, medium-range and...
International audienceMany global atmospheric models have too little precipitation variability in th...
Abstract. Convective parameterizations used in general circulation models (GCMs) generally only simu...
Clouds are chaotic, difficult to predict, but above all, magnificent natural phenomena. There are di...
Many numerical models for weather prediction and climate studies are run at resolutions that are too...
Abstract In this paper it is argued that ensemble prediction systems can be devised i...
In 2005, the ECMWF held a workshop on stochastic parameterisation, at which the convection was seen ...
Idealized cloud-resolving model (CRM) simulations spanning a large part of the tropical atmosphere a...
Conditional Markov chain (CMC) models have proven to be promising building blocks for stochastic con...
The parameterization of shallow cumuli across a range of model grid resolutions of kilometrescales f...
The aim for a more accurate representation of tropical convection in global circulation models is a ...
Stochastic schemes to represent model uncertainty in the European Centre for Medium-Range Weather Fo...
AbstractUnresolved sub-grid processes, those which are too small or dissipate too quickly to be capt...
A stochastic parameterization scheme for deep convection is described, suitable for use in both clim...
The representation of convection in large-scale models remains one of the most difficult problems in...
The last decade has seen the success of stochastic parameterizations in short-term, medium-range and...
International audienceMany global atmospheric models have too little precipitation variability in th...
Abstract. Convective parameterizations used in general circulation models (GCMs) generally only simu...
Clouds are chaotic, difficult to predict, but above all, magnificent natural phenomena. There are di...
Many numerical models for weather prediction and climate studies are run at resolutions that are too...
Abstract In this paper it is argued that ensemble prediction systems can be devised i...
In 2005, the ECMWF held a workshop on stochastic parameterisation, at which the convection was seen ...
Idealized cloud-resolving model (CRM) simulations spanning a large part of the tropical atmosphere a...
Conditional Markov chain (CMC) models have proven to be promising building blocks for stochastic con...
The parameterization of shallow cumuli across a range of model grid resolutions of kilometrescales f...
The aim for a more accurate representation of tropical convection in global circulation models is a ...
Stochastic schemes to represent model uncertainty in the European Centre for Medium-Range Weather Fo...
AbstractUnresolved sub-grid processes, those which are too small or dissipate too quickly to be capt...
A stochastic parameterization scheme for deep convection is described, suitable for use in both clim...
The representation of convection in large-scale models remains one of the most difficult problems in...
The last decade has seen the success of stochastic parameterizations in short-term, medium-range and...
International audienceMany global atmospheric models have too little precipitation variability in th...