Structure of subfilter-scale fluxes in the atmospheric surface layer with application to large-eddy simulation modelling

By P. Sullivan, T. W. Horst, Donald H. Lenschow, C. Moeng, Jeffrey Weil. Journal of Fluid Mechanics, 2003

138 citations recorded by the source corpus.

Subfields: Atmospheric Science, Computational Mechanics, Environmental Engineering

View Paper: https://www.semanticscholar.org/paper/2d6d0c6f30a5213a41ea64539f55de279449a1bc

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Citations in the corpus

The Effect of Mesh Resolution on Convective Boundary Layer Statistics and Structures Generated by Large-Eddy Simulation (2011, methodology): “We are aware that the specification of the subgrid-scale fluxes using a TKE eddy viscosity model is one of many proposals available in the literature (see, e.g., Meneveau and Katz 2000; Geurts 2001; Sullivan et al. 2003; Wyngaard 2004b).”
Resistance and heat‐transfer laws for stable and neutral planetary boundary layers: Old theory advanced and re‐evaluated (2005, background): “This term was not included in prior environmental LES codes; its importance has been recognized only recently through analyses of data from atmospheric field experiments (Sullivan et al. 2003).”
Dynamics of Winds and Currents Coupled to Surface Waves (2010, background): “…Reynolds number and with a zo representation of surface roughness can be used to model the energy-containing range of outdoor flows, but with the uncertainty associated with modeling unresolved subgrid-scale motions (Hatlee & Wyngaard 2007, McWilliams et al. 1997, Moeng 1984, Sullivan et al. 2003).”
Implementation of a Nonlinear Subfilter Turbulence Stress Model for Large-Eddy Simulation in the Advanced Research WRF Model (2010, background): “This approach is fundamentally at odds with observations that the eigenvectors of the stress and strain rate tensors are generally not aligned at the scales at which LES SFS stress models are applied (e.g., Sullivan et al. 2003).”
Bridging the Transition from Mesoscale to Microscale Turbulence in Numerical Weather Prediction Models (2014, methodology): “He used data from the Horizontal Array Turbulence Study (HATS, Sullivan et al. 2003) to show that when the grid size approaches the integral length scale, there are other production terms in the transport equation for the SGS stress that can also be important. Wyngaard (2004) then suggested that the”
Toward Numerical Modeling in the “Terra Incognita” (2004, methodology): “Data are from the HATS experiment (Sullivan et al. 2003).”
Turbulence structure above a vegetation canopy (2009, background): “τ̃ij incorporates not just the conventional Reynolds stresses but also the ‘Leonard’ terms and cross-terms, which arise because spatial averaging over finite domains does not obey conventional Reynolds-averaging rules (Leonard 1974; Wyngaard 1982; Sullivan et al. 2003; Finnigan & Shaw 2008).”
Explicit Filtering and Reconstruction Turbulence Modeling for Large-Eddy Simulation of Neutral Boundary Layer Flow (2005, methodology): “Finally, we note that the mixed model (RSFS/SGS) approach could be used with other SGS models, such as static Smagorinsky, the modified version of Sullivan et al. (1994) , or 1.5-order turbulent kinetic energy–based (Deardorff 1980; Moeng 1984) closures commonly used in cloud-scale simulations with”
The Use of Large-Eddy Simulations in Lagrangian Particle Dispersion Models (2004, unknown): “Recent ﬁeld observations (Sullivan et al. 2003) show that the SFS variances are anisotropic and match measurements from the neutral surface layer with / (cid:46) 1.”