# Overview "By setting appropriate profiles for wind velocity and the turbulence quantities at the inlet, it is often assumed that the boundary layer will be maintained up to the buildings or obstructions in the flow." (HW:p. 355). However, it was quantified by (HW:p. 355) that "even in the absence of obstructions, ..., the velocity and turbulence profiles decay along the fetch" (HW:p. 355). It was shown by (HW:p. 355) that a set of modifications were required to maintain a neutral atmospheric boundary layer throughout an empty and long computational domain of a RANS computation. ## Aim - Verification of the atmospheric boundary-layer boundary conditions in terms of the maintenance of inlet quantities downstream within a RANS computation: - atmBoundaryLayerInletVelocity - atmBoundaryLayerInletK - atmBoundaryLayerInletEpsilon - atmBoundaryLayerInletOmega ## Benchmark (Physical phenomenon) - The benchmark is an empty fetch computational domain, steady-state RANS simulation. - Flow characteristics: - External flow - The surface layer portion of the neutral-stratified equilibrium atmospheric boundary layer (no Ekman layer) - Dry air - Homogeneous, smooth terrain - Spatiotemporal-invariant aerodynamic roughness length - No displacement height - Newtonian, single-phase, incompressible, non-reacting - Benchmark scenario: - Computational domain: (HW:Fig. 1) - Benchmark dataset: (HW:Fig. 6) (Obtained by the WebPlotDigitizer-4.2 (Rohatgi, 2019)) ## Resources Computational study (tag:HW): Hargreaves, D. M., & Wright, N. G. (2007). On the use of the k–ε model in commercial CFD software to model the neutral atmospheric boundary layer. Journal of wind engineering and industrial aerodynamics, 95(5), 355-369. DOI:10.1016/j.jweia.2006.08.002 Wind profile (tag:RQP): Richards, P. J., Quinn, A. D., & Parker, S. (2002). A 6 m cube in an atmospheric boundary layer flow-Part 2. Computational solutions. Wind and structures, 5(2_3_4), 177-192. DOI:10.12989/was.2002.5.2_3_4.177 # Numerics ## Physical modelling: - The governing equations for: - Steady-state, Newtonian, single-phase, incompressible fluid flows, excluding any thermal chemical, electromagnetic and scalar interactions - Mathematical approach for the turbulence modelling: - Reynolds-averaged Navier-Stokes simulation (RANS) - Turbulence closure model: - kEpsilon and kOmegaSST linear eddy viscosity closure models - The sets of input (HW:Table 1): - Reference height, Zref = 6 [m] - Aerodynamic roughness height, z0 = 0.01 [m] - Displacement height, d = 0 [m] - Reference mean wind speed, Uref = 10 [m/s] ## Computational domain modelling: - Rectangular prism - (x1, x2, x3) = (5000, 100, 500) [m] = (streamwise, spanwise, ground-normal) directions ## Computational domain discretisation: - Spatial resolution: - (x1, x2, x3) = (500, 5, 50) [cells] - Refer to the `system/blockMeshDict` for the grading details - Temporal resolution: Steady state ## Equation discretisation: - Spatial derivatives and variables: - Convection: Second order - Others: Second order with various limiters - Temporal derivatives and variables: First order ## Numerical boundary/initial conditions: - Refer to `0.orig` ## Pressure-velocity coupling algorithm: - SIMPLEC ## Linear solvers: - Refer to `system/fvSolution` ## Initialisation and sampling: - No initialisation/averaging - Sampling at the end of the simulation via `system/sampleDict` - Refer to `system/controlDict` for further details