4.2.15.7. FAST.Farm Theory¶
FAST.Farm is a multiphysics engineering tool for predicting the performance and loads of wind turbines within a wind farm. FAST.Farm uses OpenFAST to solve the aerohydroservoelastic dynamics of each individual turbine, but considers additional physics for windfarmwide ambient wind in the atmospheric boundary layer; a windfarm super controller; and wake deficits, advection, deflection, meandering, and merging. FAST.Farm is based on the principles of the DWM model – including passive tracer modeling of wake meandering – but addresses many of the limitations of previous DWM implementations.
4.2.15.7.1. Dynamic Wake Meandering Principles and Limitations Addressed¶
The main idea behind the DWM model is to capture key wake features pertinent to accurate prediction of wind farm power performance and wind turbine loads, including the wakedeficit evolution (important for performance) and the wake meandering and wakeadded turbulence (important for loads). Although fundamental laws of physics are applied, appropriate simplifications have been made to minimize the computational expense, and HFM solutions are used to inform and calibrate the submodels. In the DWM model, the wakeflow processes are treated via the “splitting of scales,” in which small turbulent eddies (less than two diameters) affect wakedeficit evolution and large turbulent eddies (greater than two diameters) affect wake meandering.
The presence of thrust from the wind turbine rotor causes the wind speed to decrease and the pressure to increase just upwind of the rotor. In the nearwake region just downwind of the rotor – illustrated in Fig. 4.61 – coherent vortices break down, the pressure recovers to free stream, the wind speed decreases further, and the wake expands radially. In the farwake region further downwind, the wake deficit is approximately Gaussian and recovers to free stream due to the turbulent transfer of momentum into the wake from the ambient wind across the wake shear layer. This flowspeed reduction and gradual recovery to free stream is known as the wakedeficit evolution. In most DWM implementations, the wakedeficit evolution is modeled via the thin shearlayer approximation of the Reynoldsaveraged NavierStokes equations under quasisteadystate conditions in axisymmetric coordinates – illustrated in Fig. 4.53. The turbulence closure is captured by using an eddyviscosity formulation, dependent on small turbulent eddies. This wakedeficit evolution solution is only valid in the far wake. This far wake is most important for wind farm analysis because wind turbines are not typically spaced closely. However, because the wakedeficit evolution solution begins at the rotor, a nearwake correction is applied at the inlet boundary condition to improve the accuracy of the farwake solution.
Wake meandering is the largescale movement of the wake deficit transported by large turbulent eddies. This wakemeandering process is treated pragmatically in DWM ([ffLeal08]) by modeling the meandering as a passive tracer, which transfers the wake deficit transversely (horizontally and vertically) to a moving frame of reference (MFoR) – as illustrated in Fig. 4.50 – based on the ambient wind (including large turbulent eddies) spatially averaged across planes of the wake.
Wakeadded turbulence is the additional smallscale turbulence generated from the turbulent mixing in the wake. It is often modeled in DWM by scaling up the background (undisturbed) turbulence.
Several variations of DWM have been implemented, e.g., by the Technical University of Denmark ([ffMeal10, ffMeal16]) and the University of Massachusetts ([ffCeal15, ffHao16, ffHeal14]). Although the exact limitations of existing DWM implementations depend on the implementation, specific limitations that are addressed in developing FAST.Farm are summarized in Table 4.15 and are discussed where appropriate in the next section.
Limitation 
Solution/Innovation 















4.2.15.7.2. FAST.Farm Theory Basis¶
FAST.Farm is a nonlinear timedomain multiphysics engineering tool composed of multiple submodels, each representing different physics domains of the wind farm. FAST.Farm is implemented as opensource software that follows the programming requirements of the FAST modularization framework ([ffJon13]), whereby the submodels are implemented as modules interconnected through a driver code. The submodel hierarchy of FAST.Farm is illustrated in Fig. 4.51. Wake advection, deflection, and meandering; nearwake correction; and wakedeficit increment are submodels of the wakedynamics (WD) model, implemented in a single module. Ambient wind and wake merging are submodels of the ambient wind and array effects (AWAE) model, implemented in a single module. Combined with the super controller (SC) and OpenFAST (OF) modules, FAST.Farm has four modules and one driver. There are multiple instances of the OF and WD modules – one instance for each wind turbine/rotor. Each submodel/module is described in the subsections below.
FAST.Farm can be compiled and run in serial or parallel mode. Parallelization has been implemented in FAST.Farm through OpenMP, which allows FAST.Farm to take advantage of multicore computers by dividing computational tasks among the cores/threads within a node (but not between nodes) to speed up a single simulation. This process is illustrated in Fig. 4.62 for a node where the number of threads (\(N_{Th}\)) is greater than the number of wind turbines (\(N_t\)). There is one instance of the AWAE and SC modules and \(N_t\) instances of the OF and WD modules. The initialization, update states, calculate output, and end calls to each module are shown. The output calculation of AWAE is parallelized across all threads. During time marching, each instance of OF is solved in parallel while the ambient wind data are read by AWAE.
The size of the wind farm and number of wind turbines is limited only by the available RAM. In parallel mode, each instance of the OpenFAST submodel can be run in parallel on separate threads. At the same time, the ambient wind within the AWAE module is being read into memory on another thread. Thus, the fastest simulations require at least one more core than the number of wind turbines in the wind farm. Furthermore, the output calculations within the AWAE module are parallelized into separate threads. To support the modeling of large wind farms, single simulations involving memory parallelization and parallelization between nodes of a multinode HPC through MPI is likely required. MPI has not yet been implemented within FAST.Farm. However, a multinode HPC can be used to run multiple serial or parallelized simulations in parallel (in batch mode) on separate nodes. In serial mode, multiple serial simulations can be run in parallel (in batch mode) on separate cores and/or nodes.
4.2.15.7.2.1. FAST.Farm Driver¶
The FAST.Farm driver, also known as the “glue code,” is the code that couples individual modules together and drives the overall timedomain solution forward. Additionally, the FAST.Farm driver reads an input file of simulation parameters, checks the validity of these parameters, initializes the modules, writes results to a file, and releases memory at the end of the simulation.
To simplify the coupling algorithm in the FAST.Farm driver and ensure computational efficiency, all module states (\(x^d\)), inputs (\(u^d\)), outputs (\(y^d\)), and functions (\(X^d\) for state updates and \(Y^d\) for outputs) in FAST.Farm are expressed in discrete time, \(t=n\Delta t\), where \(t\) is time, \(n\) is the discretetimestep counter, and \(\Delta t\) is the userspecified discrete time step (increment). Thus, the most general form of a module in FAST.Farm is simpler than that permitted by the FAST modularization framework ([ffJon13]), represented mathematically as: 1
The SC, OF, and WD modules do not have direct feedthrough of input to output, meaning that the corresponding output functions simplify to \(y^d\left[ n \right]=Y^d\left( x^d\left[ n \right],n \right)\). The ability of the OF module to be written in the above form is explained in Section 4.2.15.7.2.3. Additionally, the AWAE module does not have states, reducing the module to a feedforwardonly system and a module form that simplifies to \(y^d\left[ n \right]=Y^d\left( u^d\left[ n \right],n \right)\). For functions in this manual, square brackets \(\left[\quad\right]\) denote discrete functions and round parentheses \(\left(\quad\right)\) denote continuous functions; the brackets/parentheses are dropped when implied. The states, inputs, and outputs of each of the FAST.Farm modules (SC, OF, WD, and AWAE) are listed in Table 4.16 and explained further in the sections below.
Module 
States (Discrete Time) 
Inputs 
Outputs 

Super Controller (SC) 



OpenFAST (OF) 



Wake Dynamics (WD) 
For \(0 \le n_p \le N_p1\):


For \(0 \le n_p \le N_p1\):

Ambient Wind and Array Effects (AWAE) 

For each turbine and \(0 \le n_p \le N_p1\):

For each turbine:

After initialization and within each time step, the states of each module (SC, OF, and WD) are updated (from time \(t\) to time \(t+\Delta t\), or equivalently, \(n\) to \(n+1\)); time is incremented; and the module outputs are calculated and transferred as inputs to other modules. Because of the form simplifications, the state updates of each module can be solved in parallel; the outputtoinput transfer does not require a large nonlinear solve; and overall correction steps of the solution are not needed. The lack of a correction step is a major simplification of the coupling algorithm used within OpenFAST ([ffSeal14, ffSeal15]). Furthermore, the output calculations of the SC, OF, and WD modules can be parallelized, followed then by the output calculation of the AWAE module. 2 In parallel mode, parallelization has been implemented in FAST.Farm through OpenMP.
Because of the small timescales and sophisticated physics, the OpenFAST submodel is the computationally slowest of the FAST.Farm modules. Additionally, the output calculation of the AWAE module is the only major calculation that cannot be solved in parallel to OpenFAST. Because of this, the parallelized FAST.Farm solution at its fastest may execute only slightly more slowly than standalone OpenFAST simulations. This results in simulations that are computationally inexpensive enough to run the many simulations necessary for wind turbine/farm design and analysis.
4.2.15.7.2.2. Super Controller (SC Module)¶
Windfarmwide super controllers have the potential to achieve the global benefit of improving overall power performance and reducing turbine loads, based on modifying wake deficits through variations in blade pitch or generator torque and/or redirecting (steering) wakes through variations in nacelle yaw or tilt, as illustrated in Fig. 4.63.
The SC module of FAST.Farm provides an interface to the super controller dynamic library – essentially identical to the super controller available in SOWFA – which allows the user of FAST.Farm to implement their own windfarmwide control logic in discrete time and without direct feedthrough of input to output – perhaps developed through the application of FLORIS. The inputs to the SC module are commands or measurements from individual turbine controllers (output from the OF module). 3 The outputs of the SC module are the global controller commands and individual turbine controller commands (inputs to the OF module).
Note that at time zero, the SC module is called before the call to the OF module and the associated individual turbine controllers. So, the initial outputs from the super controller are sent as inputs to the individual turbine controllers, but the initial inputs to the super controller from the individual turbine controller outputs at time zero are always zero. At subsequent time steps, the OF module and the associated individual turbine controllers are called before the output calculation of the SC module. As a result, at each time step other than time zero, the outputs from the super controller are extrapolated in time based on past values within OF before being sent as input to the individual turbine controllers. Thus, care should be taken to ensure that the outputs from the super controller vary smoothly over time (without steps). See Fig. 4.62 for more information.
4.2.15.7.2.3. OpenFAST (OF Module)¶
FAST.Farm makes use of OpenFAST to model the dynamics (loads and motions) of distinct turbines in the wind farm. OpenFAST captures the environmental excitations (wind inflow; for offshore systems, waves, current, and ice) and coupled system response of the full system (the rotor, drivetrain, nacelle, tower, controller; for offshore systems, the substructure and stationkeeping system). OpenFAST itself is an interconnection of various modules, each corresponding to different physical domains of the coupled aerohydroservoelastic solution. The details of the OpenFAST solution are outside the scope of this document, but can be found in the hyperlink above and associated references.
The OF module of FAST.Farm is a wrapper that enables the coupling of OpenFAST to FAST.Farm – similar to the OpenFAST wrapper available in SOWFA, but with different inputs and outputs (described below). This wrapper also controls subcycling of the OpenFAST state updates. The timescales solved within OpenFAST are much smaller than those within FAST.Farm. Therefore, for accuracy and numerical stability reasons, the OpenFAST time step is typically much smaller than that required of FAST.Farm, as depicted in Fig. 4.64.
There is one instance of the OF module for each wind turbine. In parallel mode, these instances are parallelized through OpenMP. OpenFAST itself has various modules with different inputs, outputs, states, and parameters – including continuoustime, discretetime, algebraic, and other (e.g., logical) states. However, for the purposes of coupling OpenFAST to FAST.Farm, the OF module functions in discrete time and without direct feedthrough of input to output. This is achieved by calling the OF module at the rate dictated by the FAST.Farm time step, \(\Delta t\), and by introducing a onetimestep (\(\Delta t\)) delay of the output relative to the input; this onetimestep delay is not expected to be problematic because of the slow timescales solved within FAST.Farm.
At initialization, the number of wind turbines (\(N_t\), with \(n_t\) the turbine counter such that \(1\le n_t\le N_t\)), the corresponding OpenFAST primary input files, and turbine origins in the global XYZ inertialframe coordinate system are specified by the user. Turbine origins are defined as the intersection of the undeflected tower centerline and the ground or, for offshore systems, mean sea level. The global inertialframe coordinate system is defined with Z directed vertically upward (opposite gravity), X directed horizontally nominally downwind (along the zerodegree wind direction), and Y directed horizontally transversely.
The global and turbinedependent commands from the super controller (outputs from the SC module) are used as inputs to the OF module to enable the individual turbine controller to be guided by wind farmlevel effects; likewise, the turbinedependent commands or measurements are output from the OF module for access by the super controller (inputs to the SC module).
The OF module also uses the disturbed wind (ambient plus wakes of neighboring turbines) across a highresolution wind domain (in both time and space) around the turbine (output from the AWAE module – see Section 4.2.15.7.2.5 for more information), \(\vec{V}_\text{Dist}^\text{High}\), as input, to ensure that the individual turbine loads and response calculated by OpenFAST are accurately driven by flow through the wind farm, including wake and array effects. Spatially, the highresolution wind domain must be large enough to encompass yawing of the rotor, blade deflection, and motion of the support structure (the latter is especially important for floating offshore wind turbines). OpenFAST uses a fourdimensional (three space dimensions plus one time dimension) interpolation to determine the wind local to its analysis nodes.
The OF module computes several outputs needed for calculating wake dynamics (inputs to the WD module). These include:
\(\hat{x}^\text{Disk}\) – the orientation of the rotor centerline
\(\vec{p}^\text{Hub}\) – the global position of the rotor center
\(D^\text{Rotor}\) – the rotor diameter
\(\gamma^\text{YawErr}\) – the nacelleyaw error of the rotor
\(^\text{DiskAvg}V_x^\text{Rel}\) – the rotordiskaveraged relative wind speed (ambient plus wakes of neighboring turbines plus turbine motion), normal to the disk
\(^\text{AzimAvg}C_t\left( r \right)\) – the azimuthally averaged thrustforce coefficient (normal to the rotor disk), distributed radially, where \(r\) is the radius.
In this manual, an over arrow (\(\vec{\quad}\)) denotes a threecomponent vector and a hat (\(\hat{\quad}\)) denotes a threecomponent unit vector. For clarity in this manual, \(\left( r \right)\) is used to denote radial dependence as a continuous function, even though the radial dependence is stored/computed on a discrete radial finitedifference grid within FAST.Farm. Except for \(\gamma^\text{YawErr}\) and \(^\text{AzimAvg}C_t\left( r \right)\), all of the listed variables were computed within OpenFAST before the development of FAST.Farm. \(\gamma^\text{YawErr}\) is defined as the angle about global Z from the rotor centerline to the rotordiskaveraged relative wind velocity (ambient plus wakes of neighboring turbines plus turbine motion), both projected onto the horizontal global XY plane – see Fig. 4.52 for an illustration. \(^\text{AzimAvg}C_t\left( r \right)\) is computed by Equation (4.220)
where:
\(N_b\) – number of rotor blades, with \(n_b\) as the blade counter such that \(1\le n_b\le N_b\)
\(\left\{ \quad \right\}^T\) – vector transpose
\(\rho\) – air density
\(\vec{f}_{n_b}\left( r \right)\) – aerodynamic applied loads 4 distributed per unit length along a line extending radially outward in the plane of the rotor disk for blade \(n_b\).
The numerator of Equation (4.220) is the aerodynamic applied loads distributed per unit length projected normal to the rotor disk, i.e., the radially dependent thrust force. The denominator is the normalizing factor for the radially dependent thrust coefficient, composed of the circumference at the given radius, \(2\pi r\), and the dynamic pressure of the rotordiskaveraged relative wind speed, \(\frac{1}{2}\rho {{\left( ^\text{DiskAvg}V_x^\text{Rel} \right)}^2}\).
4.2.15.7.2.4. Wake Dynamics (WD Module)¶
The WD module of FAST.Farm calculates wake dynamics for an individual rotor, including wake advection, deflection, and meandering; a nearwake correction; and a wakedeficit increment. The nearwake correction treats the nearwake (pressuregradient zone) expansion of the wake deficit. The wakedeficit increment shifts the quasisteadystate axisymmetric wake deficit nominally downwind. Each submodel is described in the subsections below. There is one instance of the WD module for each rotor.
The wakedynamics calculations involve many userspecified parameters that may depend, e.g., on turbine operation or atmospheric conditions that can be calibrated to better match experimental data or HFM, e.g., by running SOWFA (or equivalent) as a benchmark. Default values have been derived for each calibrated parameter based on SOWFA simulations ([ffDeal18]), but these can be overwritten by the user of FAST.Farm.
The wakedeficit evolution is solved in discrete time on an axisymmetric finitedifference grid consisting of a fixed number of wake planes, \(N_p\) (with \(n_p\) the wakeplane counter such that \(0\le n_p\le N_p1\)). A wake plane can be thought of as a cross section of the wake wherein the wake deficit is calculated.
Three wake formulations are available forthe evolution of the wake planes. The parameter Mod_Wake is used to switch between wake formulations. There are three options available:
1) Polar [Mod_Wake=1] (default). The wake is axisymmetric, defined on a polar grid, solved using an implicit CrankNicolson scheme, satisfying both the momentum and mass conservation laws under a shear layer approximation. Each plane has a fixed radial grid of nodes. Because the wake deficit is assumed to be axisymmetric, the radial finitedifference grid can be considered a plane.
2) Curledwake model [Mod_Wake=2]. The wake is defined on a Cartesian grid, the effect of curled wake vorticies in skewed inflow is accounted for by introducing crossflow velocities, the momentum conservation is solved using a firstorder forward Euler scheme, mass conservation is not enforced, the effect of wake swirl may be accounted for. Each plane has a fixed number of nodes in the y and z direction (of the meandering frame). The wake will adopt a “curled” shape in skewed inflow.
3) Cartesian [Mod_Wake=3] This corresponds to model 2 with curledwake vortices of zero intensities, leading to an axisymmetric wake. Swirl effects can be included in this formulation.
Because the Curl and Cartesian implementations rely on a firstorder forward sheme, the implementation is less robust that the Polar implementation. An approximate stability criterion for the curledwake model is given in Equation 20 of the following paper). This criterion was adapted to provide the guidelines on dr and DT_Low given in Section 4.2.15.6.
The curledwake model implementation is described in the following reference.
The rest of this documentation concerns the Polar fomulation.
Inputs to the WD module include \(\hat{x}^\text{Disk}\), \(\vec{p}^\text{Hub}\), \(D^\text{Rotor}\), \(\gamma^\text{YawErr}\), \(^\text{DiskAvg}V_x^\text{Rel}\), and \(^\text{AzimAvg}C_t\left( r \right)\). Additional inputs are the advection, deflection, and meandering velocity of the wake planes for the rotor (\(\vec{V}_{n_p}^\text{Plane}\)); the rotordiskaveraged ambient wind speed, normal to the disk (\(^\text{DiskAvg}V_x^\text{Wind}\)); and the ambient turbulence intensity of the wind at the rotor (\(TI_\text{Amb}\)) (output from the AWAE module – see Section 4.2.15.7.2.5 for more information). \(\vec{V}_{n_p}^\text{Plane}\) is computed for \(0\le n_p\le N_p1\) by spatial averaging of the disturbed wind.
The WD module computes several outputs needed for the calculation of disturbed wind, to be used as input to the AWAE module. These outputs include:
\(\hat{x}_{n_p}^\text{Plane}\) – the orientations of the wake planes defined using the unit vectors normal to each plane, i.e., the orientation of the wakeplane centerline
\(\vec{p}_{n_p}^\text{Plane}\) – the global positions of the centers of the wake planes
\(V_{x_{n_p}}^\text{Wake}\left(r\right)\) and \(V_{r_{n_p}}^\text{Wake}\left(r\right)\) – the axial and radial wakevelocity deficits, respectively, at the wake planes, distributed radially
\(D_{n_p}^\text{Wake}\) – the wake diameters at the wake planes, each for \(0\le n_p\le N_p1\).
Though the details are left out of this manual, during startup – whereby a wake has not yet propagated through all of the wake planes – the number of wake planes is limited by the elapsed time to avoid having to set inputs, outputs, and states in the WD and AWAE modules beyond where the wake has propagated.
4.2.15.7.2.4.1. Wake Advection, Deflection, and Meandering¶
By simple extensions to the passive tracer solution for transverse (horizontal and vertical) wake meandering, the wakedynamics solution in FAST.Farm is extended to account for wake deflection – as illustrated in Fig. 4.52 – and wake advection – as illustrated in Fig. 4.53 – among other physical improvements. The following extensions are introduced:
Calculating the wake plane velocities, \(\vec{V}_{n_p}^\text{Plane}\) for \(0\le n_p\le N_p1\), by spatially averaging the disturbed wind instead of the ambient wind (see Section 4.2.15.7.2.5)
Orientating the wake planes with the rotor centerline instead of the wind direction
Lowpass filtering the local conditions at the rotor, as input to the WD module, to account for transients in inflow, turbine control, and/or turbine motion instead of considering timeaveraged conditions.
With these extensions, the passive tracer solution enables:
The wake centerline to deflect based on inflow skew. This is achieved because in skewed inflow, the wake deficit normal to the disk introduces a velocity component that is not parallel to the ambient flow.
The wake to accelerate from near wake to far wake because the wake deficits are stronger in the near wake and weaken downwind.
The wakedeficit evolution to change based on conditions at the rotor because lowpass time filtered conditions are used instead of timeaveraged.
The wake to meander axially in addition to transversely because local axial winds are considered.
The wake shape to be elliptical instead of circular in skewed flow when looking downwind (the wake shape remains circular when looking down the rotor centerline).
For item 3, lowpass time filtering is important because the wake reacts slowly to changes in local conditions at the rotor and because the wake evolution is treated in a quasisteadystate fashion. Furthermore, a correction to the wake deflection resulting from item 1 is needed to account for the physical combination of wake rotation and shear, which is not modeled directly in the WD module. This is achieved through a horizontally asymmetric correction to the wake deflection from item 1 (see Fig. 4.52 for an illustration). This horizontal wakedeflection correction is a simple linear correction with slope and offset, similar to the correction implemented in the wake model of FLORIS. It is important for accurate modeling of nacelleyawbased wakeredirection (wakesteering) wind farm control.
Mathematically, the lowpass time filter is implemented using a recursive, singlepole filter with exponential smoothing ([ffSmi06]). The discretetime recursion (difference) equation for this filter is ([ffJeal09]):
where
\(x^d\) – discretetime state storing the lowpass timefiltered value of input \(u^d\)
\(\alpha=e^{2\pi \Delta t f_c}\) – lowpass timefilter parameter, with a value between 0 (minimum filtering) and 1 (maximum filtering) (exclusive)
\(f_c\) – userspecified cutoff (corner) frequency (the time constant of the lowpass time filter is \(\frac{1}{f_c}\)).
Subscript \(n_p\) is used to denote the state associated with wakeplane \(n_p\); Equation (4.221) applies at the rotor disk, where \(n_p=0\).
To be consistent with the quasisteadystate treatment of the wakedeficit evolution (see Section 4.2.15.7.2.4.3), the conditions at the rotor are maintained as fixed states of a wake plane as the plane propagates downstream
Equations (4.221) and (4.222) apply directly to the WD module inputs \(D^\text{Rotor}\) 5, \(\gamma^\text{YawErr}\), \(^\text{DiskAvg}V_x^\text{Rel}\), and \(TI_\text{Amb}\). The associated states are \(^\text{Filt}D_{n_p}^\text{Rotor}\), \(^\text{Filt}\gamma_{n_p}^\text{YawErr}\), \(^\text{FiltDiskAvg}V_{x_{n_p}}^\text{Wind}\), and \(^\text{Filt}TI_{\text{Amb}_{n_p}}\) respectively (each for \(0\le n_p\le N_p1\)). The WD module inputs \(^\text{DiskAvg}V_x^\text{Rel}\) and \(^\text{AzimAvg}C_t\left( r \right)\) are needed for the boundary condition at the rotor, but are not otherwise needed in the wakedeficit evolution calculation and are therefore not propagated downstream with the wake planes. Therefore, Equation (4.221) applies to these inputs but Equation (4.222) does not. The associated states are \(^\text{FiltDiskAvg}V_x^\text{Rel}\) and \(^\text{FiltAzimAvg}C_t\left( r \right)\). Likewise, only Equation (4.221) is used to lowpass time filter the WD module input \(\vec{V}_{n_p}^\text{Plane}\) with state \(^\text{Filt}\vec{V}_{n_p}^\text{Plane}\) (for \(0\le n_p\le N_p1\)). Equations (4.221) and (4.222) apply in a modified form to the WD module inputs \(\hat{x}^\text{Disk}\) and \(\vec{p}^\text{Hub}\) to derive the state associated with the downwind distance from the rotor to each wake plane in the axisymmetric coordinate system (\(x_{n_p}^\text{Plane}\)), and the states and outputs associated with the orientations of the wake planes, normal to the planes, (\(\hat{x}_{n_p}^\text{Plane}\)), and the global center positions of the wake planes, (\(\vec{p}_{n_p}^\text{Plane}\)) as follows:
where:
Equation (4.223) differs from Equations (4.221) and (4.222) in that after applying Equation (4.221) to lowpass timefilter input \(\hat{x}^\text{Disk}\), the state is renormalized to ensure that the vector remains unit length; Equation (4.223) ensures that the wakeplane orientation is maintained as the planes propagate nominally downwind. Equation (4.224) expresses that each wake plane propagates downwind in the axisymmetric coordinate system by a distance equal to that traveled by the lowpass timefiltered wakeplane velocity projected along the plane orientation over the time step; 6 the initial wake plane (\(n_p=0\)) is always at the rotor disk. Equation (4.225) expresses the global center positions of the wake plane following the passive tracer concept, similar to Equation (4.224), but considering the full threecomponent movement of the wake plane, including deflection and meandering. The last term on the righthand side of Equation (4.225) for each wake plane is the horizontal wakedeflection correction, where:
\(C_{HWkDfl}^\text{O}\) – userspecified parameter defining the horizontal offset at the rotor
\(C_{HWkDfl}^\text{OY}\) – userspecified parameter defining the horizontal offset at the rotor scaled with nacelleyaw error
\(C_{HWkDfl}^\text{x}\) – userspecified parameter defining the horizontal offset scaled with downstream distance
\(C_{HWkDfl}^\text{xY}\) – userspecified parameter defining the horizontal offset scaled with downstream distance and nacelleyaw error
\(\hat{X}\), \(\hat{Y}\), and \(\hat{Z}\) – unit vectors parallel to the inertialframe coordinates X, Y and, Z respectively
\(\widehat{XY_{np}}\) – threecomponent unit vector in the horizontal global XY plane orthogonal to \(\hat{x}^\text{Plane}_{n_p}\left[ n+1 \right]\)
\(C_\text{HWkDfl}^\text{O}+C_\text{HWkDfl}^\text{OY} \ ^\text{Filt}\gamma _{n_p}^\text{YawErr}\left[ n+1 \right]\) – offset at the rotor
\(C_\text{HWkDfl}^\text{x}+C_\text{HWkDfl}^\text{xY} \ ^\text{Filt}\gamma _{n_p}^\text{YawErr}\left[ n+1 \right]\) – slope
\(d\hat{x}_{n_p1}\) – nominally downwind increment of the wake plane (from Equation (4.224))
I – threebythree identity matrix
\(\left[ I\hat{x}_{n_p1}^\text{Plane}\left[ n \right]\left\{ \hat{x}_{n_p1}^\text{Plane}\left[ n \right] \right\}^T \right]\) – used to calculate the transverse component of \(V^\text{Plane}_{n_p1}\) normal to \(\hat{x}^\text{Plane}_{n_p1}\left[ n\right]\).
It is noted that the advection, deflection, and meandering velocity of the wake planes, \(\vec{V}^\text{Plane}_{n_p1}\), is lowpass time filtered in the axial direction, but not in the transverse direction. Lowpass time filtering in the axial direction is useful for minimizing how often wake planes get close to or pass each other while they travel axially; this filtering is not needed transversely because an appropriate transverse meandering velocity is achieved through spatially averaging the disturbed wind (see Section 4.2.15.7.2.5).
The consistent output equation corresponding to the lowpass time filter of Equation (4.221) is \(y^d\left[ n \right]={x^d}\left[ n \right]\alpha +{u^d}\left[ n \right]\left( 1\alpha \right)\), i.e., \({Y^d(\quad)}=X^d(\quad)\), or equivalently, \(y^d\left[ n \right]=x^d\left[ n+1 \right]\) ([ffJeal09]). However, the output is delayed by one time step (\(\Delta t\)) to avoid having direct feedthrough of input to output within the WD module, yielding \(y^d\left[ n \right]=x^d\left[ n \right]\). This onetimestep delay is applied to all outputs of the WD module and is not expected to be problematic because of the slow timescales solved within FAST.Farm.
4.2.15.7.2.4.2. NearWake Correction¶
The nearwake correction submodel of the WD module computes the axial and radial wakevelocity deficits at the rotor disk as an inlet boundary condition for the wakedeficit evolution described in Section 4.2.15.7.2.4.3. To improve the accuracy of the farwake solution, the nearwake correction accounts for the drop in wind speed and radial expansion of the wake in the pressuregradient zone behind the rotor that is not otherwise accounted for in the solution for the wakedeficit evolution. For clarity, the equations in this section are expressed using continuous variables, but within FAST.Farm the equations are solved discretely on an axisymmetric finitedifference grid.
The nearwake correction is computed differently for low thrust conditions (\(C_T<\frac{24}{25}\)), momentum theory is valid, and high thrust conditions (\(1.1<C_T \le 2\)), where \(C_T\) is the rotor diskaveraged thrust coefficient, derived from the lowpass timefiltered azimuthally averaged thrustforce coefficient (normal to the rotor disk), \(^\text{FiltAzimAvg}{C_t}\left( r \right)\), evaluated at \(n+1\). The propeller brake region occurs for very high thrustforce coefficients (\(C_T \ge 2\)) and is not considered. Between the low and high thrust regions, a linear blending of the two solutions, based on \(C_T\), is implemented.
At low thrust (\(C_T<\frac{24}{25}\)) conditions, the axial induction at the rotor disk, distributed radially, \(a\left( r\right)\), is derived from the lowpass timefiltered azimuthally averaged thrustforce coefficient (normal to the rotor disk), \(^\text{FiltAzimAvg}{C_t}\left( r \right)\), evaluated at \(n+1\) using Equation (4.228), which follows from the momentum region of bladeelement momentum (BEM) theory.
To avoid unrealistically high induction at the ends of a blade, Equation (4.228) does not directly consider hub or tiploss corrections, but these may be accounted for in the calculation of the applied aerodynamic loads within OpenFAST (depending on the aerodynamic options enabled within OpenFAST), which have an effect on \(^\text{FiltAzimAvg}C_t\left( r \right)\). Moreover, \(^\text{FiltAzimAvg}{C_t}\left( r \right)\) is capped at \(\frac{24}{25}\) to avoid illconditioning of the radial wake expansion discussed next.
The states and outputs associated with the axial and radial wakevelocity deficits, distributed radially (\(V_{x_{n_p}}^\text{Wake}\left(r\right)\) and \(V_{r_{n_p}}^\text{Wake}\left(r\right)\)), are derived at the rotor disk (\(n_p = 0\)) from \(a\left( r\right)\) and the lowpass timefiltered rotordiskaveraged relative wind speed (ambient plus wakes of neighboring turbines plus turbine motion), normal to the disk (\(^\text{FiltDiskAvg}V_x^\text{Rel}\)), evaluated at \(n+1\) using Equations (4.229) and (4.230).
where
In Equation (4.229):
\(r^\text{Plane}\) – radial expansion of the wake associated with \(r\)
\(r'\) – dummy variable of \(r\)
\(C_\text{NearWake}\) – userspecified calibration parameter greater than unity and less than \(2.5\) which determines how far the wind speed drops and wake expands radially in the pressuregradient zone before recovering in the far wake. 7
The righthand side of Equation (4.229) represents the axialinduced velocity at the end of the pressuregradient zone; the negative sign appears because the axial wake deficit is in the opposite direction of the free stream axial wind – see Section 4.2.15.7.2.4.3 for more information. The radial expansion of the wake in the lefthand side of Equation (4.229) results from the application of the conservation of mass within an incremental annulus in the pressuregradient zone. 8 The radial wake deficit is initialized to zero, as given in Equations (4.230). Because the nearwake correction is applied directly at the rotor disk, the solution to the wakedeficit evolution for downwind distances within the first few diameters of the rotor, i.e., in the near wake, is not expected to be accurate; as a result, modifications to FAST.Farm would be needed to accurately model closely spaced wind farms.
At high thrust (\(1.1<C_T \le 2\)) conditions, the axial wakevelocity deficit, distributed radially (\(V_{x_{n_p}}^\text{Wake}\left(r\right)\)), is derived at the rotor disk (\(n_p = 0\)) by a Gaussian fit to LES solutions at high thrust per Equation (4.231), as derived by [ffMT21]. The radial wake deficit is again initialized to zero.
where
4.2.15.7.2.4.3. WakeDeficit Increment¶
As with most DWM implementations, the WD module of FAST.Farm models the wakedeficit evolution via the thin shearlayer approximation of the Reynoldsaveraged NavierStokes equations under quasisteadystate conditions in axisymmetric coordinates, with turbulence closure captured by using an eddyviscosity formulation ([ffAin88]). The thin shearlayer approximation drops the pressure term and assumes that the velocity gradients are much bigger in the radial direction than in the axial direction. With these simplifications, analytical expressions for the conservation of momentum (Equation (4.232)) and conservation of mass (continuity, Equation (4.233)) are as follows:
where \(V_x\) and \(V_r\) are the axial and radial velocities in the axisymmetric coordinate system, respectively, and \(\nu_T\) is the eddy viscosity (all dependent on \(x\) and \(r\)). The equations on the left are written in a form common in literature. The equivalent equations on the right are written in the form implemented within FAST.Farm. For clarity, the equations in this section are first expressed using continuous variables, but within FAST.Farm the equations are solved discretely on an axisymmetric finitedifference grid consisting of a fixed number of wake planes, as summarized at the end of this section. For the continuous variables, subscript \(n_p\), corresponding to wake plane \(n_p\), is replaced with \(\left( x \right)\). The subscript is altogether dropped for variables that remain constant as the wake propagates downstream, following Equation (4.222). For example, \(^\text{Filt}D_{n_p}^\text{Rotor}\), \(^\text{FiltDiskAvg}V_{x_{n_p}}^\text{Wind}\), and \(^\text{Filt}TI_{\text{Amb}_{n_p}}\) are written as \(^\text{Filt}D^\text{Rotor}\), \(^\text{FiltDiskAvg}V_{x}^\text{Wind}\), and \(^\text{Filt}TI_\text{Amb}\), respectively.
\(V_x\) and \(V_r\) are related to the lowpass timefiltered rotordiskaveraged ambient wind speed, normal to the disk (\(^\text{FiltDiskAvg}V_{x}^\text{Wind}\)), and the states and outputs associated with radially distributed axial and radial wakevelocity deficits, \(V^\text{Wake}_x(x,r)\) and \(V^\text{Wake}_r(x,r)\), respectively, by Equations (4.234) and (4.235).
\(V_x(x,r)\) and \(V_r(x,r)\) can be thought of as the change in wind velocity in the wake relative to free stream; therefore, \(V^\text{Wake}_x(x,r)\) usually has a negative value. Several variations of the eddyviscosity formulation have been used in prior implementations of DWM. The eddyviscosity formulation currently implemented within FAST.Farm is given by Equation (4.236).
where:
\(F_{\nu \text{Amb}}(x)\) – filter function associated with ambient turbulence
\(F_{\nu \text{Shr}}(x)\) – filter function associated with the wake shear layer
\(k_{\nu \text{Amb}}\) – userspecified calibration parameters weighting the influence of ambient turbulence on the eddy viscosity
\(k_{\nu \text{Shr}}\) – userspecified calibration parameters weighting the influence of the wake shear layer on the eddy viscosity
\(\frac{D^\text{Wake}(x)}{2}\) – wake halfwidth
\(\frac{\partial V_x}{\partial r}\) – absolute value of the radial gradient of the axial velocity
\(MIN_r(V_x(x,r))\) – used to denote the minimum value of \(V_x\) along the radius for a given downstream distance.
Although not matching any specific eddyviscosity formulation found in prior implementations of DWM, the chosen implementation within FAST.Farm is simple to apply and inherently tailorable, allowing the user to properly calibrate the wake evolution to known solutions. The eddyviscosity formulation expresses the influence of the ambient turbulence (first term on the righthand side) and wake shear layer (second term) on the turbulent stresses in the wake. The dependence of the eddy viscosity on \(x\) and \(r\) is explicitly given in Equations (4.236) to make it clear which terms depend on the downwind distance and/or radius. The first term on the righthand side of Equations (4.236) is similar to that given by [ffMeal10] with a characteristic length taken to be the rotor radius, \(\frac{^\text{Filt}D^\text{Rotor}}{2}\). The second term is similar to that given by [ffKeal13], but without consideration of atmospheric shear, which is considered by the AWAE module in the definition of ambient turbulence – see Section 4.2.15.7.2.5 for more information. In this second term, the characteristic length is taken to be the wake halfwidth and the \(MAX(\quad)\) operator is used to denote the maximum of the two wake shearlayer methods. The second shearlayer method is needed to avoid underpredicting the turbulent stresses from the first method at radii where the radial gradient of the axial velocity approaches zero.
The filter functions currently implemented within FAST.Farm are given by Equations (4.237) and (4.238), where \(C_{\nu \text{Amb}}^{DMax}\), \(C_{\nu \text{Amb}}^{DMin}\), \(C_{\nu \text{Amb}}^{Exp}\), \(C_{\nu \text{Amb}}^{FMin}\), \(C_{\nu \text{Shr}}^{DMax}\), \(C_{\nu \text{Shr}}^{DMin}\), \(C_{\nu \text{Shr}}^{Exp}\), and \(C_{\nu \text{Shr}}^{FMin}\) are userspecified calibration parameters for the functions associated with ambient turbulence and the wake shear layer, respectively.
The filter functions of Equations (4.237) and (4.238) represent the delay in the turbulent stress generated by ambient turbulence and the development of turbulent stresses generated by the wake shear layer, respectively, and are made general in FAST.Farm. Each filter function is split into three regions of downstream distance, including:
A fixed minimum value (between zero and unity, inclusive) near the rotor
A fixed value of unity far downstream from the rotor
A transition region for intermediate distances, where the value can transition linearly or via any rational exponent of the normalized downstream distance within the transition region.
The definition of wake diameter is somewhat ambiguous and not defined consistently in DWM literature. FAST.Farm allows the user to choose one of several methods to calculate the wake diameter, \(D^\text{Wake}\left( x \right)\), including taking the wake diameter to be:
The rotor diameter
The diameter at which the axial velocity of the wake is the \(C_\text{WakeDiam}\) fraction of the ambient wind speed, where \(C_\text{WakeDiam}\) is a userspecified calibration parameter between zero and \(0.99\) (exclusive)
The diameter that captures the \(C_\text{WakeDiam}\) fraction of the mass flux of the axial wake deficit across the wake plane
The diameter that captures the \(C_\text{WakeDiam}\) fraction of the momentum flux of the axial wake deficit across the wake plane.
Through the use of a \(MAX(\quad)\) operator, models 2 through 4 have a lower bound set equal to the rotor diameter when the wakediameter calculation otherwise returns smaller values. This is done to avoid numerical problems resulting from too few wind data points in the spatial averaging used to compute the wakemeandering velocity – see Section 4.2.15.7.2.5 for more information. Although the implementation in FAST.Farm is numerical, analytical expressions for these four methods are given in Equation (4.239). Here, \(x\) means the mean conditioned on \(x\).
The momentum and continuity equations are solved numerically in the wakedeficitincrement submodel of the WD module using a secondorder accurate finitedifference method at \(n+\frac{1}{2}\), following the implicit CrankNicolson method ([ffCN96]). Following this method, central differences are used for all derivatives, e.g., Equation (4.240) for the momentum equation.
Here,
or equivalently from Equation (4.226)
For the momentum equation, for each wake plane downstream of the rotor (\(1\le n_p\le N_p1\)), the terms \(V_x\), \(V_r\), \(\nu_T\), and \(\frac{\partial \nu_T}{\partial r}\) are calculated at \(n\) (or equivalently \(x=x_{n_p1}^\text{Plane}\left[ n \right]\)), e.g., \(V_x=^\text{FiltDiskAvg}V_{x_{n_p1}}^\text{Wind}\left[ n \right]+V_{x_{n_p1}}^\text{Wake}\left( r \right)\left[ n \right]\) and \(V_r = V_{r_{n_p1}}^\text{Wake}\left( r \right)\left[ n \right]\), to avoid nonlinearities in the solution for \(n+1\). This will prevent the solution from achieving secondorder convergence, but has been shown to remain numerically stable. Although the definition of each central difference is outside the scope of this document, the end result is that for each wake plane downstream of the rotor, \(V_{x_{n_p}}^\text{Wake}\left( r \right)\left[ n+1 \right]\) can be solved via a linear tridiagonal matrix system of equations in terms of known solutions of \(V_{x_{n_p1}}^\text{Wake}\left( r \right)\left[ n \right]\), \(V_{r_{n_p1}}^\text{Wake}\left( r \right)\left[ n \right]\), and other previously calculated states, e.g., \(^\text{FiltDiskAvg}V_{x_{n_p1}}^\text{Wind}\left[ n \right]\). The linear tridiagonal matrix system of equations is solved efficiently in FAST.Farm via the Thomas algorithm ([ffTho49]).
For the continuity equation, a different finitedifference scheme is needed because the resulting tridiagonal matrix is not diagonally dominant when the same finitedifference scheme used for the momentum equation is used for the continuity equation, resulting in a numerically unstable solution. Instead, the finitedifference scheme used for the continuity equation is based on a secondorder accurate scheme at \(n+\frac{1}{2}\) and \(n_r\frac{1}{2}\). However, the terms involving \(V_r\) and \(\frac{\partial V_r}{\partial r}\) are calculated at \(n+1\), e.g., \(V_r=\frac{1}{2}\left(V_{r_{n_p,n_r}}^\text{Wake}\left[ n+1 \right]+V_{r_{n_p,n_r1}}^\text{Wake}\left[ n+1 \right]\right)\), where \(n_r\) is the radii counter for \(N_r\) radial nodes (\(0\le n_r\le N_r1\)). 9 Although the definition of each central difference is outside the scope of this document, the end result is that for each wake plane downstream of the rotor, \(V_{r_{n_p,n_r}}^\text{Wake}\left[ n+1 \right]\) can be solved explicitly sequentially from known solutions of \(V_{x_{n_p}}^\text{Wake}\left( r \right)\left[ n+1 \right]\) (from the solution of the momentum equation), \(V_{x_{n_p1}}^\text{Wake}\left( r \right)\left[ n \right]\), and \(V_{r_{n_p,n_r1}}^\text{Wake}\left[ n+1 \right]\) for \(1\le n_r\le N_r1\). 10
4.2.15.7.2.5. Ambient Wind and Array Effects (AWAE Module)¶
The AWAE module of FAST.Farm processes ambient wind and wake interactions across the wind farm, including the ambient wind and wakemerging submodels. The ambient wind submodule processes ambient wind across the wind farm from either a highfidelity precursor simulation or an interface to the InflowWind module in OpenFAST. The wakemerging submodule identifies zones of overlap between all wakes across the wind farm and merges their wake deficits. Both submodels are described in the subsections below.
The calculations in the AWAE module make use of wake volumes, which are volumes formed by a (possibly curved) cylinder starting at a wake plane and extending to the next adjacent wake plane along a line connecting the centers of the two wake planes. If the adjacent wake planes (top and bottom of the cylinder) are not parallel, e.g., for transient simulations involving variations in nacelleyaw angle, the centerline will be curved instead of straight. Fig. 4.54 illustrates some of the concepts that will be detailed in the subsections below. The calculations in the AWAE module also require looping through all wind data points, turbines, and wake planes; these loops have been sped up in the parallel mode of FAST.Farm by implementation of OpenMP parallelization.
The AWAE module does not have states, reducing the module to a feedforwardonly system whereby the module outputs are computed directly from the module inputs (with direct feedthrough of input to output). The AWAE module uses as input \(\hat{x}_{n_p}^\text{Plane}\), \(\vec{p}_{n_p}^\text{Plane}\), \(V_{x_{n_p}}^\text{Wake}\left(r\right)\), \(V_{r_{n_p}}^\text{Wake}\left(r\right)\), and \(D_{n_p}^\text{Wake}\) (each for \(0\le n_p\le N_p1\)) as computed by the wakedynamics model for each individual wind turbine (output by the WD module). The AWAE module computes output \(\vec{V}_\text{Dist}^\text{High}\) needed for the calculation of OpenFAST for each individual wind turbine (input to the OF module) as well as outputs for \(\vec{V}_{n_p}^\text{Plane}\) for \(0\le n_p\le N_p1\), \(^\text{DiskAvg}V_x^\text{Wind}\), and \(TI_\text{Amb}\) needed for the calculation of wake dynamics for each individual wind turbine (input to the WD module).
4.2.15.7.2.5.1. Ambient Wind¶
The ambient wind data used by FAST.Farm can be generated in one of two ways. The use of the InflowWind module in OpenFAST enables the use of simple ambient wind, e.g., uniform wind, discrete wind events, or synthetically generated turbulent wind data. Synthetically generated turbulence can be from, e.g., TurbSim or the Mann model, in which the wind is propagated through the wind farm using Taylor’s frozenturbulence assumption. This method is most applicable to small wind farms or a subset of wind turbines within a larger wind farm. FAST.Farm can also use ambient wind generated by a highfidelity precursor LES simulation of the entire wind farm (without wind turbines present), such as the ABLSolver preprocessor of SOWFA. This atmospheric precursor simulation captures more physics than synthetic turbulence – as illustrated in Fig. 4.55 – including atmospheric stability, windfarmwide turbulent length scales, and complex terrain effects. It is more computationally expensive than using the ambient wind modeling options of InflowWind, but it is much less computationally expensive than a SOWFA simulation with multiple wind turbines present.
FAST.Farm requires ambient wind to be available in two different resolutions. Because wind will be spatially averaged across wake planes within the AWAE module, FAST.Farm needs a lowresolution wind domain (in both space and time) throughout the wind farm. The spatial resolution of the lowresolution domain – consisting of a structured 3D grid of wind data points – should be sufficient so that the spatial averaging is accurate, e.g., on the order of tens of meters for utilityscale wind turbines. The time step of the lowresolution domain dictates that of the FAST.Farm driver (\(\Delta t\)) and all FAST.Farm modules. It should therefore be consistent with the timescales of wake dynamics, e.g., on the order of seconds and smaller for higher mean wind speeds. Note that OpenFAST is subcycled within the OF module with a smaller time step. For accurate load calculation by OpenFAST, FAST.Farm also needs highresolution wind domains (in both space and time) around each wind turbine and encompassing any turbine displacement. The spatial and time resolution of each highresolution domain should be sufficient for accurate aerodynamic load calculations, e.g., on the order of the blade chord length and fractions of a second ([ffSeal19b]). The highresolution domains overlap portions of the lowresolution domain. For simplicity of and to minimize computational expense within FAST.Farm, the time step of the highresolution domain must be an integer divisor of the lowresolution domain time step.
When using ambient wind generated by a highfidelity precursor simulation, the AWAE module reads in the threecomponent windvelocity data across the high and lowresolution domains – \(\vec{V}_\text{Amb}^\text{High}\) for each turbine and \(\vec{V}_\text{Amb}^\text{Low}\), respectively – that were computed by the highfidelity solver within each time step. These values are stored in files for use in a given driver time step. The wind data files, including spatial discretizations, must be in VTK format and are specified by users of FAST.Farm at initialization. When using the InflowWind inflow option, the ambient wind across the high and lowresolution domains are computed by calling the InflowWind module. In this case, the spatial discretizations of these domains are specified directly within the FAST.Farm primary input file. These wind data from the combined low and highresolution domains within a given driver time step represent the largest memory requirement of FAST.Farm.
After the ambient wind is processed at a given time step, the ambient wind submodel computes as output the rotordiskaveraged ambient wind speed, normal to the disk,\(^\text{DiskAvg}V_x^\text{Wind}\), for each turbine using Equation (4.241).
In Equation (4.241), \(N_{n_p}^\text{Polar}\) is the number of points in a polar grid on wake plane \(n_p\) of the given wind turbine, \(n^\text{Polar}\) is the point counter such that \(1\le n^\text{Polar}\le N_{n_p}^\text{Polar}\) for wake plane \(n_p\), and the equation is evaluated for the wake plane at the rotor disk (\(n_p=0\)). The polar grid on wake plane \(n_p\) has a uniform radial and azimuthal discretization equal to the average XYZ spatial discretization of the lowresolution domain (independent from the radial finitedifference grid used within the WD module) and a diameter of \(C_\text{Meander}D_{n_p}^\text{Wake}\); \(C_\text{Meander}\) is discussed further in Section 4.2.15.7.2.5.2 below. Subscript \(n^\text{Polar}\) is appended to \(\vec{V}_\text{Amb}^\text{Low}\) in Equation (4.241) to identify wind data that have been trilinearly interpolated from the lowresolution domain to the polar grid on the wake plane. Intuitively, Equation (4.241) states that the rotordiskaveraged ambient wind speed, normal to the disk, for each turbine is calculated as the uniform spatial average of the ambient wind velocity on the wake plane at the rotor disk projected along the lowpass timefiltered rotor centerline.
The ambient wind submodel of the AWAE module also calculates as output the ambient turbulence intensity around each rotor, \(TI_\text{Amb}\), using Equation (4.242):
The bracketed term in Equation (4.242) is the same as in Equation (4.241), representing the uniform spatial average of the ambient wind velocity on the wake plane at the rotor disk. In contrast to the common definition of turbulence intensity used in the wind industry, which consists of a timeaveraged quantity of the axial wind component, the turbulence intensity calculated in the ambient wind submodel of the AWAE module is based on a uniform spatial average of the three vector components. Not using time averaging ensures that only ambient wind at the current time step needs to be processed, which decreases memory requirements. Moreover, any time variation in the spatial average is moderated by the lowpass time filter in the WD module. Using spatial averaging and the three vector components allows for atmospheric shear, wind veer, and other ambient wind characteristics to influence the eddy viscosity and wakedeficit evolution in the WD module. The incorporation of wakeadded turbulence is left for future work. Note that Equation (4.242) uses the eight wind data points from the lowresolution domain surrounding each point in the polar grid rather than interpolation. This is because calculating wind data in the polar grid on the wake plane via trilinear interpolation from the lowresolution domain would smooth out spatial variations and artificially reduce the calculated turbulence intensity.
4.2.15.7.2.5.2. Wake Merging¶
In previous implementations of DWM, the wind turbine and wake dynamics were solved individually or serially, not considering twoway wakemerging interactions. Additionally, there was no method available to calculate the disturbed wind in zones of wake overlap. Wake merging is illustrated by the SOWFA simulation of Fig. 4.56. In FAST.Farm, the wakemerging submodel of the AWAE module identifies zones of wake overlap between all wakes across the wind farm by finding wake volumes that overlap in space. Wake deficits are superimposed in the axial direction based on the RSS method ([ffKaticeal86]); transverse components (radial wake deficits) are superimposed by vector sum. In Katic̀ et al. ([ffKaticeal86]), the RSS method is applied to wakes with axial deficits that are uniform across the wake diameter and radial deficits are not considered. In contrast, the RSS method in FAST.Farm is applied locally at a given wind data point. The RSS method assumes that the local kinetic energy of the axial deficit in a merged wake equals the sum of the local energies of the axial deficits for each wake at the given wind data point. The RSS method only applies to an array of scalars, which works well for axial deficits because overlapping wakes likely have similar axial directions. This means, however, that only the magnitude of the vector is important in the superposition. A vector sum is applied to the transverse components (radial wake deficits) because any given radial direction is dependent on the azimuth angle in the axisymmetric coordinate system.
The disturbed (ambient plus wakes) wind velocities across the high and lowresolution domains – \(\vec{V}_\text{Dist}^\text{High}\) for each turbine and \(\vec{V}_\text{Dist}^\text{Low}\), respectively – are computed using Equations (4.243) and (4.244), respectively.
Here, \((n_{t_{n^\text{Wake}}}\ne n_t)\) signifies that wake \(n^\text{Wake}\) is not associated with the given turbine \(n_t\). The first, second, and third terms on the righthand side of Equations (4.243) and (4.244) represent the ambient wind velocity, the RSS superposition of the axial wakevelocity deficits, and the vector sum of the transverse wakevelocity deficits, respectively. Although many mathematical details are outside the scope of this document, the nomenclature of Equations (4.243) and (4.244) is as follows:
\(N^\text{Wake}\) – number of wake volumes overlapping a given wind data point in the wind domain
\(n^\text{Wake}\) – wake counter such that \(1\le n^\text{Wake}\le N^\text{Wake}\) which, when used as a subscript, is used to identify the specific point in a wake plane in place of \(\left( r \right)\) and subscript \(n_p\)
\(V_{x_{n^\text{Wake}}}^\text{Wake}\) – axial wakevelocity deficit associated with where the given wind data point lies within the specific wake volume and corresponding wake plane
\(V_{r_{n^\text{Wake}}}^\text{Wake}\) – radial wakevelocity deficit associated with where the given wind data point lies within the specific wake volume and corresponding wake plane
\(\hat{x}_{n^\text{Wake}}^\text{Plane}\) – axial orientation associated with where the given wind data point lies within the specific wake volume and corresponding wake plane
\(\hat{r}_{n^\text{Wake}}^\text{Plane}\) – radial unit vector associated with where the given wind data point lies within the specific wake volume and corresponding wake plane
\(\overline{\hat{x}}^\text{Plane}\) – weightedaverage axial orientation associated with a given point in the wind spatial domain
\(\{ \overline{\hat{x}}^\text{Plane}\}^T\) – projects \(\{ V_{x_{n^\text{Wake}}}^\text{Wake}\hat{x}_{n^\text{Wake}}^\text{Plane}+V_{r_{n^\text{Wake}}}^\text{Wake}\hat{r}_{n^\text{Wake}}^\text{Plane}\}\) along \(\hat{r}_{n^\text{Wake}}^\text{Plane}\)
\(\left[I\hat{x}_{n^\text{Wake}}^\text{Plane}\{ \overline{\hat{x}}^\text{Plane}\}^T\right]\) – calculates the transverse component of \(\{ V_{x_{n^\text{Wake}}}^\text{Wake}\hat{x}_{n^\text{Wake}}^\text{Plane}+V_{r_{n^\text{Wake}}}^\text{Wake}\hat{r}_{n^\text{Wake}}^\text{Plane}\}\) normal to \(\overline{\hat{x}}^\text{Plane}\).
Wake volumes are found by looping through all points, turbines, and wake planes and spatially determining if the given point resides in a wake volume that has a diameter equal to the radial extent of the wake planes. Wake volume \(n_p\) (for \(0\le n_p\le N_p2\)) starts at wake plane \(n_p\) and extends to wake plane \(n_p+1\). Wake volumes have a centerline determined by \(\vec{p}_{n_p}^\text{Plane}\), \(\hat{x}_{n_p}^\text{Plane}\), \(\vec{p}_{n_p+1}^\text{Plane}\), and \(\hat{x}_{n_p+1}^\text{Plane}\) – this centerline is curved if \(\hat{x}_{n_p}^\text{Plane}\) and \(\hat{x}_{n_p+1}^\text{Plane}\) are not parallel. The calculations of \(V_{x_{n^\text{Wake}}}^\text{Wake}\) and \(V_{r_{n^\text{Wake}}}^\text{Wake}\) involve bilinear interpolation of the wake deficits in the axial and radial directions. The axial interpolation is complicated when the adjacent wake planes are not parallel. The vector quantity \(\{ V_{x_{n^\text{Wake}}}^\text{Wake}\hat{x}_{n^\text{Wake}}^\text{Plane}+V_{r_{n^\text{Wake}}}^\text{Wake}\hat{r}_{n^\text{Wake}}^\text{Plane}\}\) represents the total wakevelocity deficit associated with where the given wind data point lies within the specific wake volume and corresponding wake plane. Because each wake plane may have a unique orientation, what constitutes “axial” and “radial” in the superposition at a given wind data point is determined by weightedaveraging the orientations of each wake volume overlapping that point (weighted by the magnitude of each axial wake deficit). A similar equation is used to calculate the distributed wind velocities across the highresolution domain (\(\vec{V}_\text{Dist}^\text{High}\)) for each turbine, which is needed to calculate the disturbed wind inflow to a turbine. Note that for the highresolution domain, a turbine is prevented from interacting with its own wake.
Once the distributed wind velocities across the lowresolution domain have been found, the wake merging submodel of the AWAE module computes as output the advection, deflection, and meandering velocity of each wake plane, \(\vec{V}_{n_p}^\text{Plane}\) for \(0\le n_p\le N_p1\), for each turbine as the weighted spatial average of the disturbed wind velocity across the wake plane, using Equation (4.245).
The polar grid on wake plane \(n_p\) has a uniform radial and azimuthal discretization equal to the average XYZ spatial discretization of the lowresolution domain (independent from the radial finitedifference grid used within the WD module) and a local diameter described below. Subscript \(n^\text{Polar}\) is appended to \(\vec{V}_\text{Dist}^\text{Low}\) in Equation (4.245) to identify wind data that have been trilinearly interpolated from the lowresolution domain to the polar grid on the wake plane. Unlike Equation (4.241), Equation (4.245) includes a spatial weighting factor, \(w_{n^\text{Polar}}\), dependent on the radial distance of point \(n^\text{Polar}\) from the center of the wake plane (discussed below). FAST.Farm will issue a warning if the center of any wake plane has left the boundaries of the lowresolution domain and set the meandering velocity of each wake plane, \(\vec{V}_{n_p}^\text{Plane}\), to zero for any wake plane that has entirely left the boundaries of the lowresolution domain. Qualitatively, Equation (4.245) states that the advection, deflection, and meandering velocity of each wake plane for each turbine is calculated as the weighted spatial average of the disturbed wind velocity on the wake plane. Larsen et al. ([ffLeal08]) proposed a uniform spatial average where all points within a circle of diameter \(2D_{n_p}^\text{Wake}\) are given equal weight. However, the Fourier transform of the circular function in a polar spatial domain results in a jinc function in the polar wavenumber domain, 11 implying a gentle rolloff of energy below the cutoff wave number and pockets of energy at distinct wave numbers above the cutoff wave number. Experience with FAST.Farm development has shown that this approach results in less overall wake meandering and at improper frequencies. As such, three weighted spatial averaging methods have been implemented in FAST.Farm, as defined in Equation (4.246).
The first method is a spatial average with a uniform weighting with a local polargrid diameter of \(C_\text{Meander}D_{n_p}^\text{Wake}\) at wake plane \(n_p\), resulting in a cutoff wave number of \(\frac{1}{C_\text{Meander}D^\text{Wake}}\). The second and third methods weight each point in the spatial average by a form of the jinc function dependent on the radius of the point from the wake centerline, \(r_{n^\text{Polar}}\), normalized by \(C_\text{Meander}D^\text{Wake}\). This results in a more ideal lowpass filter with a sharper cutoff of energy in the polar wavenumber domain with a cutoff wave number of \(\frac{1}{C_\text{Meander}D^\text{Wake}}\). However, because the jinc function decays slowly with increasing argument, the jinc function must be windowed to be applied in practice. The second method truncates the jinc function at its first zero crossing, corresponding to a local polargrid diameter of \(1.21967C_\text{Meander}D_{n_p}^\text{Wake}\) at wake plane \(n_p\). The third method windows the jinc function by multiplying it with a jinc function of half the argument (the polardomain equivalent of a onedimensional Lanczos/sinc window), which tapers the weighting to zero at its second zero crossing (the weighting is positive below the first zero crossing and negative past the first zero crossing until it tapers to zero). This corresponds to a local polargrid diameter of \(2.23313C_\text{Meander}D_{n_p}^\text{Wake}\) at wake plane \(n_p\). These weighted spatial averaging methods improve the overall level and frequency content of the wake meandering at the expense of a bit heavier computations due to the larger polargrid diameters (i.e., the truncated jinc method has roughly \(50\%\) more points within the polar grid than the uniform method, and the windowed jinc method has roughly five times more points than the uniform method). A value of \(C_\text{Meander}=2\), resulting in a polargrid diameter of \(2D^\text{Wake}\) and cutoff wave number of \(\frac{1}{2D^\text{Wake}}\), follows the characteristic dimension important to transverse wake meandering proposed by Larsen et al. ([ffLeal08]) \(C_\text{Meander}\) is included in all methods to enable the user of FAST.Farm to better match the meandering to known solutions. Note that the lower the value of \(C_\text{Meander}\), the more the wake will meander.
 1
\(x^d\) and \(X^d\) are identical to what is described in [ffJon13]. \(u^d\), \(y^d\), and \(Y^d\) are identical to \(u\), \(y\), and \(Y\) from [ffJon13], but are only evaluated in discrete time, \(t=n\Delta t\), and so, are marked here with superscript \(^d\).
 2
Not all of these possible parallel tasks have been implemented within FAST.Farm because profiling did not show adequate computational speedup. However, to minimize the computational expense of the output calculation of the AWAE module, the ambient wind data files are read in parallel to the state updates of the SC, OF, and WD modules. See the introduction to Section 4.2.15.7.2 for more information.
 3
The SC module also has as input a placeholder for future global (e.g., wind) measurements (output from the AWAE module) in addition to commands or measurements from the individual turbine controllers. But the global inputs are currently null.
 4
Derived using the Line2toLine2 meshmapping algorithm of FAST ([ffSeal14, ffSeal15]) to transfer the aerodynamic applied loads distributed per unit length along the deflected/curved blade as calculated within FAST.
 5
Variations in the rotor diameter, \(D^\text{Rotor}\), are possible as a result of blade deflection. These variations are likely small, but this variable is treated the same as other inputs for consistency.
 6
The absolute value is added because, as far as wake evolution is concerned, if a wake plane travels opposite of its original propagation direction (e.g., due to a localized wind gust), the total downwind distance traveled is used rather than the instantaneous downwind distance from the rotor.
 7
A value of \(C_\text{NearWake}=2\) is expected from first principles, but can be calibrated by the user of FAST.Farm to better match the far wake to known solutions.
 8
The incremental mass flow is given by:
\[d\dot{m} = 2\pi r dr \rho\ ^\text{FiltDiskAvg}V^\text{Rel}_x (1a(r)) = 2\pi r^\text{Plane} dr^\text{Plane} \rho\ ^\text{FiltDiskAvg}V^\text{Rel}_x (1C_\text{NearWake} a(r))\]Following from this, \(r^\text{Plane} dr^\text{Plane} = \frac{1a\left( r\right)}{1C_\text{NearWake} a\left( r\right)}r dr\), which can then be integrated along the radius.
 9
Subscript \(n_r\) has been used here in place of \(\left( r\right)\)
 10
Note that the radial wakevelocity deficit at the centerline of the axisymmetric coordinate system (\(n_r=0\)) is always zero (\(V_{r_{n_p}}^\text{Wake}\left( r \right)_{r=0}=0)\).
 11
In this context, the jinc function is defined as \(jinc(r)=\frac{J_1(2\pi r)}{r}\) (with the limiting value at the origin of \(jinc(0) = \pi)\), where \(J_1(r)\) is the Bessel function of the first kind and order one. The jinc function is normalized such that \(\int\limits_{0}^{\infty }{jinc\left( r \right)2\pi rdr}=1\). The jinc function is the polarequivalent of the onedimensional sinc function defined as \(\text{sinc} \left( x \right)=\frac{\sin \left( \pi x \right)}{\pi x}\) (with the limiting value at the origin of \(\text{sinc}(0)=1\), which is the Fourier transform of a rectangular function, i.e., an ideal lowpass filter, and normalized such that \(\int\limits_{\infty }^{\infty }{\text{sinc}\left( x \right)dx}=1\).