Katabatic flow: a closed-form solution with spatially-varying eddy diffusivities

The Nieuwstadt closed-form solution for the stationary Ekman layer is generalized for katabatic flows within the conceptual framework of the Prandtl model. The proposed solution is valid for spatially-varying eddy viscosity and diffusivity (O’Brien type) and constant Prandtl number (Pr). Variations in the velocity and buoyancy profiles are discussed as a function of the dimensionless model parameters $$z_0 \equiv \hat{z}_0 \hat{N}^2 Pr \sin {(\alpha )} |\hat{b}_\mathrm{s} |^{-1}$$ and $$\lambda \equiv \hat{u}_{\mathrm{ref}}\hat{N} \sqrt{Pr} |\hat{b}_\mathrm{s} |^{-1}$$ , where $$\hat{z}_0$$ is the hydrodynamic roughness length, $$\hat{N}$$ is the Brunt-Vaisala frequency, $$\alpha $$ is the surface sloping angle, $$\hat{b}_\mathrm{s}$$ is the imposed surface buoyancy, and $$\hat{u}_{\mathrm{ref}}$$ is a reference velocity scale used to define eddy diffusivities. Velocity and buoyancy profiles show significant variations in both phase and amplitude of extrema with respect to the classic constant $$\textit{K}$$ model and with respect to a recent approximate analytic solution based on the Wentzel-Kramers-Brillouin theory. Near-wall regions are characterized by relatively stronger surface momentum and buoyancy gradients, whose magnitude is proportional to $$z_0$$ and to $$\lambda $$ . In addition, slope-parallel momentum and buoyancy fluxes are reduced, the low-level jet is further displaced toward the wall, and its peak velocity depends on both $$z_0$$ and $$\lambda $$ .

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