Large‐eddy simulation of neutral atmospheric boundary layer flow over heterogeneous surfaces: Blending height and effective surface roughness

By E. Bou‐Zeid, Charles Meneveau, Marc B. Parlange. 2004

233 citations recorded by the source corpus.

Subfields: Atmospheric Science, Computational Mechanics, Environmental Engineering

View Paper: https://www.semanticscholar.org/paper/cf89449c09da06226a43fdc533d2717b1906e615

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. Fernando Port'e-Agel
2. Rob Stoll
3. E. Bou‐Zeid
4. Charles Meneveau
5. C. Talbot
6. Jim Smith
7. William Anderson
8. Marc B. Parlange

In Computational Mechanics

1. Fernando Port'e-Agel
2. Rob Stoll
3. Charles Meneveau
4. E. Bou‐Zeid
5. S. Salesky
6. M. Calaf
7. C. Talbot
8. Jim Smith

In Environmental Engineering

1. Fernando Port'e-Agel
2. Charles Meneveau
3. Rob Stoll
4. E. Bou‐Zeid
5. S. Salesky
6. M. Calaf
7. C. Talbot
8. Jim Smith

Citations in the corpus

• Dynamic subgrid‐scale models for momentum and scalar fluxes in large‐eddy simulations of neutrally stratified atmospheric boundary layers over heterogeneous terrain (2006, methodology): “A value of zero in the deviation from the plane-averaged nondimensional velocity gradient indicates that the flow is in equilibrium and can serve as a method of determining the internal boundary layer height [Bou-Zeid et al., 2004].”
• Mechanistic models of seed dispersal by wind (2011, background): “These terms represent the effect of small eddies, which are filtered out by such spatial averaging, on the resolved scales of motion (Bou-Zeid et al. 2004).”
• Nested Mesoscale Large-Eddy Simulations with WRF: Performance in Real Test Cases (2012, background): “…(Ntelekos et al. 2008), and 3) the influ-ence of abrupt changes in the local landscape and land cover on atmospheric flows and land–atmosphere exchanges (Bou-Zeid et al. 2004; Talbot et al. 2007a; Courault et al. 2007; Chan 2009; Rotunno et al. 2009; Stoll and Porte´-Agel 2009; Bou-Zeid et al.…”
• Large‐eddy simulation of a diurnal cycle of the atmospheric boundary layer: Atmospheric stability and scaling issues (2006, methodology): “The code has been modified in the subsequent work of Porte´-Agel et al. [2000a] and Bou-Zeid et al. [2004, 2005] .”
• Large-Eddy Simulation of the Atmospheric Boundary Layer (2020, background): “Further, the abrupt transition in roughness results in an abrupt rise in surface stress, and elevated production of turbulence in the fluid immediately above and downwind of the transition (Antonia and Luxton 1971; Bou-Zeid et al. 2004).”