Comparison of CFD Simulation to UAS Measurements for Wind Flows in Complex Terrain: Application to the WINSENT Test Site

This investigation presents a modelling strategy for wind-energy studies in complex terrains using computational fluid dynamics (CFD). A model, based on an unsteady Reynolds Averaged Navier-Stokes (URANS) approach with a modified version of the standard k-e model, is applied. A validation study based on the Leipzig experiment shows the ability of the model to simulate atmospheric boundary layer characteristics such as the Coriolis force and shallow boundary layer. By combining the results of the model and a design of experiments (DoE) method, we could determine the degree to which the slope, the leaf area index, and the forest height of an escarpment have an effect on the horizontal velocity, the flow inclination angle, and the turbulent kinetic energy at critical positions. The DoE study shows that the primary contributor at a turbine-relevant height is the slope of the escarpment. In the second step, the method is extended to the WINSENT test site. The model is compared with measurements from an unmanned aircraft system (UAS). We show the potential of the methodology and the satisfactory results of our model in depicting some interesting flow features. The results indicate that the wakes with high turbulence levels downstream of the escarpment are likely to impact the rotor blade of future wind turbines.

[1]  Jimy Dudhia,et al.  Mesoscale modeling of offshore wind turbine wakes at the wind farm resolving scale: a composite‐based analysis with the Weather Research and Forecasting model over Horns Rev , 2015 .

[2]  Hrvoje Jasak,et al.  A tensorial approach to computational continuum mechanics using object-oriented techniques , 1998 .

[3]  F. Porté-Agel,et al.  A Modulated-Gradient Parametrization for the Large-Eddy Simulation of the Atmospheric Boundary Layer Using the Weather Research and Forecasting Model , 2017, Boundary-Layer Meteorology.

[4]  Kurt Schaldemose Hansen,et al.  Mesoscale to microscale wind farm flow modeling and evaluation , 2017 .

[5]  B. Launder,et al.  The numerical computation of turbulent flows , 1990 .

[6]  F. Fiedler,et al.  Modification of air flow over an escarpment — Results from the Hjardemål experiment , 1995 .

[7]  J. Bange,et al.  Model comparison of two different non-hydrostatic formulations for the Navier-Stokes equations simulating wind flow in complex terrain , 2017 .

[8]  Jens Bange,et al.  Calibration Procedure and Accuracy of Wind and Turbulence Measurements with Five-Hole Probes on Fixed-Wing Unmanned Aircraft in the Atmospheric Boundary Layer and Wind Turbine Wakes , 2019, Atmosphere.

[9]  J. Dudhia A Nonhydrostatic Version of the Penn State–NCAR Mesoscale Model: Validation Tests and Simulation of an Atlantic Cyclone and Cold Front , 1993 .

[10]  Charlotte Bay Hasager,et al.  Length Scales of the Neutral Wind Profile over Homogeneous Terrain , 2010 .

[11]  S. E. Haupt,et al.  A preliminary study of assimilating numerical weather prediction data into computational fluid dynamics models for wind prediction , 2011 .

[12]  N. N. Sørensen,et al.  The Bolund Experiment, Part II: Blind Comparison of Microscale Flow Models , 2011 .

[13]  Andreas Platis,et al.  Reviewing Wind Measurement Approaches for Fixed-Wing Unmanned Aircraft , 2018, Atmosphere.

[14]  H. Jørgensen,et al.  The Bolund Experiment, Part I: Flow Over a Steep, Three-Dimensional Hill , 2011 .

[15]  Jens Bange,et al.  MASC – a small Remotely Piloted Aircraft (RPA) for wind energy research , 2014 .

[16]  Po Wen Cheng,et al.  Reducing the Uncertainty of Lidar Measurements in Complex Terrain Using a Linear Model Approach , 2018, Remote. Sens..

[17]  A. Blackadar The vertical distribution of wind and turbulent exchange in a neutral atmosphere , 1962 .

[18]  D. Etling,et al.  Application of the E-ε turbulence model to the atmospheric boundary layer , 1985 .

[19]  Jens Bange,et al.  Measuring the local wind field at an escarpment using small remotely-piloted aircraft , 2017 .

[20]  Ralf Koppmann,et al.  Joint modelling of obstacle induced and mesoscale changes—Current limits and challenges , 2011 .

[21]  A. J. Bowen,et al.  A wind-tunnel investigation of the wind speed and turbulence characteristics close to the ground over various escarpment shapes , 1977 .

[22]  H. Lettau A Re‐examination of the “Leipzig Wind Profile” Considering some Relations between Wind and Turbulence in the Frictional Layer , 1950 .

[23]  H. Hangan,et al.  For wind turbines in complex terrain, the devil is in the detail , 2017 .

[24]  J. Hunt,et al.  Turbulent wind flow over a low hill , 1975 .

[25]  P. A. Taylor,et al.  Some numerical studies of surface boundary-layer flow above gentle topography , 1977 .

[26]  I. P. Castro,et al.  A LIMITED-LENGTH-SCALE k-ε MODEL FOR THE NEUTRAL AND STABLY-STRATIFIED ATMOSPHERIC BOUNDARY LAYER , 1997 .

[27]  P. J. Mason,et al.  Measurements and predictions of flow and turbulence over an isolated hill of moderate slope , 2007 .

[28]  Niels Otto Jensen,et al.  On the escarpment wind profile , 1978 .

[29]  Jens Bange,et al.  Observations of the Early Morning Boundary-Layer Transition with Small Remotely-Piloted Aircraft , 2015, Boundary-Layer Meteorology.

[30]  R. I. Sykes,et al.  An asymptotic theory of incompressible turbulent boundarylayer flow over a small hump , 1980, Journal of Fluid Mechanics.

[31]  Jens Bange,et al.  Application of Different Turbulence Models Simulating Wind Flow in Complex Terrain: A Case Study for the WindForS Test Site , 2018, Comput..

[32]  Christophe Sanz,et al.  ONE- and TWO-Equation Models for Canopy Turbulence , 2004 .