The Influence of Idealized Heterogeneity on Wet and Dry Planetary Boundary Layers Coupled to the Land Surface.

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Large-Eddy Simulation of the Atmospheric Boundary Layer (2020, background): “1992; Dörnbrack and Schumann 1993) and efforts to use land-surface models to represent the impact of the surface energy and mass budgets (Patton et al. 2005; Huang and Margulis 2010; Shao et al. 2013).”
Examining Two-Way Grid Nesting for Large Eddy Simulation of the PBL Using the WRF Model (2007, background): “…limited to idealized physical conditions (e.g., PBLs over horizontally uniform surfaces; see review by Moeng and Sullivan 2003) or periodic striplike heterogeneous surfaces (e.g., Hadfield et al. 1991; Patton et al. 2005) where periodic boundary conditions are applied in the horizontal directions.”
The Effect of Mesh Resolution on Convective Boundary Layer Statistics and Structures Generated by Large-Eddy Simulation (2011, background): “Applications include, atmosphere–land interactions (Patton et al. 2005), boundary layers with surface water wave effects (Sullivan and McWilliams 2010; Sullivan et al. 2007, 2008), weakly stable nocturnal flows (Beare et al. 2006), flow in complex terrain (Lundquist et al. 2010), stratocumulus…”
Turbulence structure above a vegetation canopy (2009, background): “The differences between turbulent statistics in the ISL and in the canopy/RSL have been comprehensively reviewed by Raupach et al. (1996) and Finnigan (2000).”