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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 following 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 involving the following traits:
- 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
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
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