Results are presented of two large-eddy simulation (LES) runs of the entire year 2012 centered at the Cabauw observational supersite in the Netherlands. The LES is coupled to a regional weather model that provides the large-scale information. The simulations provide three-dimensional continuous time series of LES-generated turbulence and clouds, which can be compared in detail to the extensive observational dataset of Cabauw. The LES dataset is available from the authors on request. This type of LES setup has a number of advantages. First, it can provide a more statistical approach to the study of turbulent atmospheric flow than the more common case studies, since a diverse but representative set of conditions is covered, including numerous...
The stable boundary layer (SBL) has received less attention in atmospheric field studies, laboratory...
Deep convection is an important component of atmospheric circulations that affects many aspects of w...
Large-eddy simulations (LES) with the new ICOsahedral Non-hydrostatic atmosphere model (ICON) coveri...
Results are presented of two large-eddy simulation (LES) runs of the entire year 2012 centered at th...
We present results of two large-eddy simulation (LES) runs of the entire year 2012 centered at the C...
The low-frequency contribution to the systematic and random sampling errors in single-tower eddy-cov...
Since the advent of computers midway through the twentieth century, computational resources have inc...
The challenges of nesting large-eddy simulation (LES) within the Weather Research Forecast (WRF) mod...
Traditional weather models struggle to resolve the details of complex terrain and the strongly stabl...
Large-eddy simulation (LES) is able to capture key boundary layer (BL) turbulence and cloud processe...
As a computationally attractive alternative for global large eddy simulations (LESs), we investigate...
Large-eddy simulations of the atmospheric boundary layer have been performed over a range of stabili...
The present study aims to assess and advance the prediction skill of solar radiation in high resolut...
Large-eddy simulations (LESs) of a multi-week period during the HD(CP)2 (High-Definition Clouds and ...
The availability of suitable and reliable reference data together with the application of modelspeci...
The stable boundary layer (SBL) has received less attention in atmospheric field studies, laboratory...
Deep convection is an important component of atmospheric circulations that affects many aspects of w...
Large-eddy simulations (LES) with the new ICOsahedral Non-hydrostatic atmosphere model (ICON) coveri...
Results are presented of two large-eddy simulation (LES) runs of the entire year 2012 centered at th...
We present results of two large-eddy simulation (LES) runs of the entire year 2012 centered at the C...
The low-frequency contribution to the systematic and random sampling errors in single-tower eddy-cov...
Since the advent of computers midway through the twentieth century, computational resources have inc...
The challenges of nesting large-eddy simulation (LES) within the Weather Research Forecast (WRF) mod...
Traditional weather models struggle to resolve the details of complex terrain and the strongly stabl...
Large-eddy simulation (LES) is able to capture key boundary layer (BL) turbulence and cloud processe...
As a computationally attractive alternative for global large eddy simulations (LESs), we investigate...
Large-eddy simulations of the atmospheric boundary layer have been performed over a range of stabili...
The present study aims to assess and advance the prediction skill of solar radiation in high resolut...
Large-eddy simulations (LESs) of a multi-week period during the HD(CP)2 (High-Definition Clouds and ...
The availability of suitable and reliable reference data together with the application of modelspeci...
The stable boundary layer (SBL) has received less attention in atmospheric field studies, laboratory...
Deep convection is an important component of atmospheric circulations that affects many aspects of w...
Large-eddy simulations (LES) with the new ICOsahedral Non-hydrostatic atmosphere model (ICON) coveri...