Large-Eddy Simulation Of Neutral Turbulent Flow Over Rough Sinusoidal Ridges

By Andrew Brown, J. Hobson, Nigel Wood. 2001

133 citations recorded by the source corpus.

How researchers see this paper

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

Evaluation of Large-Eddy Simulations via Observations of Nocturnal Marine Stratocumulus (2005, methodology): “With the dynamic SGS model, a modified version of the Brown et al. (2001) model is used to treat surface layer stresses in the bottom 29 x " 70 m of the domain.”
The Role of Wave-Induced Coriolis–Stokes Forcing on the Wind-Driven Mixed Layer (2005, methodology): “The code is run in LES mode (Brown et al. 2001) using a Smagorinsky subgrid model. For further model details refer to Wood et al. (1998). The domain is periodic and isotropic in the horizontal directions spanning 120 m with a resolution of 3 m. In the vertical direction 200 grid points span 90 m wit”
Explicit Filtering and Reconstruction Turbulence Modeling for Large-Eddy Simulation of Neutral Boundary Layer Flow (2005, methodology): “Following Brown et al. (2001), Cederwall (2001), and Chow and Street (2002), we implement a near-wall stress model, based on the model given previously in Eq.”
The Bolund Experiment, Part II: Blind Comparison of Microscale Flow Models (2011, background): “…simulated the wind over the Askervein Hill (Silva Lopes et al. 2007; Chow and Street 2009; Bechmann and Sørensen 2010b) and sinusoidal ridges (Brown et al. 2001; Wan et al. 2007); however, few studies in naturally complex terrain exist (Chow et al. 2006; Weigel et al. 2006; Bechmann and…”