A Large Eddy Simulation Study of a Quasi-Steady, Stably Stratified Atmospheric Boundary Layer

By Branko Kosovic, J. Curry. 2000

328 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Engineering, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/e0f1941d9a1593a9b68340db84c6736cc7feb45e

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. R. Banta
2. P. Sullivan
3. Rob Stoll
4. W. A. Brewer
5. B. Galperin
6. S. Salesky
7. S. Basu
8. Sergej Zilitinkevich

In Environmental Engineering

1. Fernando Port'e-Agel
2. R. Banta
3. Dries Allaerts
4. M. Calaf
5. W. A. Brewer
6. Rob Stoll
7. S. Salesky
8. S. Basu

In Global and Planetary Change

1. R. Banta
2. Fernando Port'e-Agel
3. Albert A. M. Holtslag
4. Y. Pichugina
5. S. Basu
6. Sutanu Sarkar
7. Vincenzo Armenio
8. M. Calaf

Citations in the corpus

• ‘Application of a New Spectral Theory of Stably Stratified Turbulence to the Atmospheric Boundary Layer over Sea Ice’ (2005, methodology): “In order to understand the source of this discrepancy, recall that the SGS viscosities and diffusivities in LES by Kosovic and Curry (2000) were adopted from the neutral case thus ignoring the effect of stable stratification on SGS parameters.”
• Boundary-layer development and gravity waves in conventionally neutral wind farms (2017, methodology): “For many years, the large-eddy simulation (LES) technique has been the preferred tool for modelling atmospheric turbulence because of its detailed spatial and temporal resolution (see, e.g. Moeng 1984; Mason 1989; Mason & Derbyshire 1990; Kosović & Curry 2000).”
• Turbulent Velocity-Variance Profiles in the Stable Boundary Layer Generated by a Nocturnal Low-Level Jet (2006, methodology): “Numerical large-eddy simulation runs also reproduce this behavior with a maximum at or just above the surface (Kosović and Curry 2000; Saiki et al. 2000; Mason and Derbyshire 1990).”
• Large-eddy simulation of stably stratified atmospheric boundary layer turbulence: A scale-dependent dynamic modeling approach (2005, methodology): “Kosović and Curry (2000) simulated a clear-air, moderately stable boundary layer as it approaches quasi-steady state using the nonlinear SGS model of Kosović (1997).”
• Single-Column Model Intercomparison for a Stably Stratified Atmospheric Boundary Layer (2004, unknown): “This case is based on the simulations of an Arctic SBL by Kosovic and Curry (2000).”
• An investigation of stably stratified turbulent channel flow using large-eddy simulation (2002, methodology): “ Kosovic & Curry (2000) simulated the stable 30 V. Armenio and S. Sarkar”
• A Review of Planetary Boundary Layer Parameterization Schemes and Their Sensitivity in Simulating Southeastern U.S. Cold Season Severe Weather Environments (2015, background): “YSU MM5 similarity Monin–Obukhov; Monin and Obukhov (1954) QNSE QNSE PBL surface layer; Sukoriansky et al.”
• Large-Eddy Simulation of the Atmospheric Boundary Layer (2020, methodology): “Pioneering in these efforts was Kosović and Curry (2000) who used data from the Beaufort Sea Arctic Stratus Experiment to motivate an ensemble of LESs with a short enough inertial oscillation period to reach equilibrium fast enough with the computational power available at the time.”
• A Total Turbulent Energy Closure Model for Neutrally and Stably Stratified Atmospheric Boundary Layers (2007, background): “A weakly stable boundary layer grew against a background stratification, qualitatively resembling an Arctic stable case (Kosovic and Curry 2000).”
• Large‐eddy simulation of a diurnal cycle of the atmospheric boundary layer: Atmospheric stability and scaling issues (2006, unknown): “LES has emerged as a popular technique for simulation of ABL flows in idealized neutral, convective (daytime) and stable (nocturnal) atmospheric boundary layers [Moeng, 1984; Andrén et al., 1994; Nieuwstadt et al., 1991; Kosović and Curry, 2000].”
• Bridging the Transition from Mesoscale to Microscale Turbulence in Numerical Weather Prediction Models (2014, background): “Recent efforts involving LES modelling of stable conditions have led to an increased understanding of SBL structure and dynamics (e.g., Andrén 1995; Kosović and Curry 2000; Saiki et al. 2000; Beare et al. 2006; Basu and Porté-Agel 2006; Mirocha and Kosović 2010; Zhou and Chow 2011).”