Large-Eddy Simulation Of The Stably Stratified Planetary Boundary Layer
By E. Saiki, C. Moeng, P. Sullivan. 2000
193 citations recorded by the source corpus.
Subfields: Atmospheric Science, Environmental Engineering, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/a863ec84b29fbeba69693344bda351db825f2db2
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
- Fernando Port'e-Agel
- Rob Stoll
- R. Banta
- P. Sullivan
- William Anderson
- S. Basu
- S. Salesky
- Jeremy A. Gibbs
In Environmental Engineering
- Fernando Port'e-Agel
- Rob Stoll
- R. Banta
- Charles Meneveau
- S. Salesky
- M. Calaf
- William Anderson
- S. Basu
In Global and Planetary Change
- R. Banta
- Fernando Port'e-Agel
- S. Salesky
- S. Basu
- Y. Pichugina
- Sutanu Sarkar
- Vincenzo Armenio
- M. Calaf
Citations in the corpus
- Structure of subfilter-scale fluxes in the atmospheric surface layer with application to large-eddy simulation modelling (2003, methodology): “While the above TKE model is the default implementation in our LES code, its structure and the numerical value of the coefficients have been adjusted to suit particular PBL flows (e.g. Moeng & Wyngaard 1988; Sullivan et al. 1994; Patton et al. 1998; Saiki et al. 2000).”
- The Parallelized Large-Eddy Simulation Model (PALM) version 4.0 for atmospheric and oceanic flows: model formulation, recent developments, and future perspectives (2015, methodology): “PALM uses the mod-ified version of Moeng and Wyngaard (1988) and Saiki et al. (2000).”
- Overview of the PALM model system 6.0 (2019, methodology): “By default, PALM employs a 1.5-order closure (LES mode) after Deardorff (1980) in the formulation by Moeng and Wyngaard (1988) and Saiki et al. (2000) (hereafter referred to as the Deardorff scheme).”
- An investigation of stably stratified turbulent channel flow using large-eddy simulation (2002, methodology): “A bottom boundary layer capped by an upper region with internal wave activity is observed by Kosovic & Curry (2000) and Saiki et al. (2000) in their simulations.”
- An Intercomparison of Large-Eddy Simulations of the Stable Boundary Layer (2004, background): “Those papers that have reported successful simulations (i.e., with resolved turbulence) are mainly for the weakly/moderately stable boundary layer: Mason and Derbyshire (1990), Brown et al. (1994), Andren (1995), Galmarini et al. (1998), Kosovic and Curry (2000) and Saiki et al. (2000).”
- Large-Eddy Simulation of the Atmospheric Boundary Layer (2020, methodology): “Saiki et al. (2000) used a similar simulation set-up to past work but with a significantly larger geostrophic wind speed and a larger domain.”
- Large-eddy simulation of stably stratified atmospheric boundary layer turbulence: A scale-dependent dynamic modeling approach (2005, methodology): “Recently, Saiki et al. (2000) attempted to simulate a moderately stable boundary layer with Sullivan et al.’s two-part eddy-viscosity model (Sullivan et al. 1994).”
- Large‐eddy simulation of a diurnal cycle of the atmospheric boundary layer: Atmospheric stability and scaling issues (2006, background): “This observation, though not new [Saiki et al., 2000], still serves to accentuate the need for improvements in SGS models for stable boundary layers.”
- Turbulent Velocity-Variance Profiles in the Stable Boundary Layer Generated by a Nocturnal Low-Level Jet (2006, methodology): “Recent large-eddy simulation (LES) results indicate a maximum of TKE (or velocity variance) very close to the surface (e.g., Kosović and Curry 2000; Saiki et al. 2000) in agreement with the aircraft profile results.”