Resistance and heat‐transfer laws for stable and neutral planetary boundary layers: Old theory advanced and re‐evaluated

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Boundary-layer development and gravity waves in conventionally neutral wind farms (2017, background): “For instance, Zilitinkevich & Esau (2003, 2005) and Zilitinkevich, Esau & Baklanov (2007) continued to improve equilibrium height formulations and similarity theory predictions for the CNBL, and Esau (2004a,b) showed the importance of the inversion-layer height for flow properties such as turbulent…”
A Conceptual View on Inertial Oscillations and Nocturnal Low-Level Jets (2010, unknown): “Usually, equilibrium models of the NBL depart from a ‘‘resistance law’’ (Zilitinkevich and Esau 2005).”
Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part I: steady-state, homogeneous regimes (2006, background): “…transports play comparatively minor roles, whereas and are reasonably accurately represented by universal functions of z/h (see, e.g., Figure 1 in Zilitinkevich and Esau, 2005); or with more confidence to its lower 10%, the so-called surface layer, where and can be taken depth-constant: τ zF τ…”