Surface-Layer Flux-Gradient Relationships over Inclined Terrain Derived from a Local Equilibrium, Turbulence Closure Model

Abstract

Derivation of surface-layer flux-gradient relationships from a local-equilibrium, turbulence-closure model for a forced flow over inclined terrain is presented. Results are shown as a generalization of Monin-Obukhov universal functions respesenting non-dimensional wind and temperature gradients. © 2013 The Author(s).