Large-eddy simulation (LES) is a well-established numerical technique, which resolves the most energetic turbulent fluctuations in the planetary boundary layers. Averaging these fluctuations, high-quality profiles of mean values and turbulence statistics can be obtained in experiments with well-defined initial and boundary conditions. Hence, the LES data can be beneficial for assessment and optimization of turbulence closure schemes. A database of 80 LES runs for neutral and stably stratified PBLs (DATABASE64) is applied in this study to optimize the first-order turbulence closure (FOC). Approximations for the mixing length scale and stability correction functions have been tuned to minimise a relative root-mean square error over the entire...
Large-eddy simulation (LES) has become a well-established tool in the atmospheric boundary layer res...
Increasing computational power has enabled grid resolutions that support large-eddy simulation (LES)...
A stable atmospheric boundary layer (ABL) develops over land at night due to radiative surface cooli...
A new large eddy simulation (LES) code is developed and used to investigate non-local features of tu...
The stable boundary layer (SBL) has received less attention in atmospheric field studies, laboratory...
Abstract. This paper compares a number of one-dimensional closure models for the planetary boundary ...
Results are presented from the first intercomparison of Large-eddy simulation (LES) models for the s...
A disconnect remains between our improved physical understanding of boundary layers stabilized by bu...
Large-eddy simulations of the atmospheric boundary layer have been performed over a range of stabili...
Large-eddy simulation (LES) is used to simulate stably-stratified turbulent boundary-layer flow over...
A simulation of a diurnal cycle of atmospheric boundary layer (ABL) flow over a homogeneous terrain ...
A neutrally stratified Ekman layer limited in depth by a stress-free rigid lid has been simulated us...
Using the large eddy simulation (LES) technique, the authors study a clear-air, stably stratified at...
Monin–Obukhov similarity theory is used in large-eddy simulation (LES) models as a surface boundary ...
Observations of the dependence of the dimensionless wind speed gradient φm as a function of the Moni...
Large-eddy simulation (LES) has become a well-established tool in the atmospheric boundary layer res...
Increasing computational power has enabled grid resolutions that support large-eddy simulation (LES)...
A stable atmospheric boundary layer (ABL) develops over land at night due to radiative surface cooli...
A new large eddy simulation (LES) code is developed and used to investigate non-local features of tu...
The stable boundary layer (SBL) has received less attention in atmospheric field studies, laboratory...
Abstract. This paper compares a number of one-dimensional closure models for the planetary boundary ...
Results are presented from the first intercomparison of Large-eddy simulation (LES) models for the s...
A disconnect remains between our improved physical understanding of boundary layers stabilized by bu...
Large-eddy simulations of the atmospheric boundary layer have been performed over a range of stabili...
Large-eddy simulation (LES) is used to simulate stably-stratified turbulent boundary-layer flow over...
A simulation of a diurnal cycle of atmospheric boundary layer (ABL) flow over a homogeneous terrain ...
A neutrally stratified Ekman layer limited in depth by a stress-free rigid lid has been simulated us...
Using the large eddy simulation (LES) technique, the authors study a clear-air, stably stratified at...
Monin–Obukhov similarity theory is used in large-eddy simulation (LES) models as a surface boundary ...
Observations of the dependence of the dimensionless wind speed gradient φm as a function of the Moni...
Large-eddy simulation (LES) has become a well-established tool in the atmospheric boundary layer res...
Increasing computational power has enabled grid resolutions that support large-eddy simulation (LES)...
A stable atmospheric boundary layer (ABL) develops over land at night due to radiative surface cooli...