Field measurements of wake meandering at a utility-scale wind turbine with nacelle-mounted Doppler lidars
- 1Wind Engineering and Renewable Energy Laboratory (WiRE), École Polytechnique Fedérale de Lausanne (EPFL), 1015 Lausanne, Switzerland
- 2IIHR-Hydroscience & Engineering, Department of Civil and Environmental Engineering, The University of Iowa, Iowa City, IA 52242, USA
Correspondence: Peter Brugger (firstname.lastname@example.org)
Wake meandering is a low-frequency oscillation of the entire wind turbine wake that can contribute to power and load fluctuations of downstream turbines in wind farms. Field measurements of two Doppler lidars mounted on the nacelle of a utility-scale wind turbine were used to investigate relationships between the inflow and the wake meandering as well as the effect of wake meandering on the temporally averaged wake. A correlation analysis showed a linear relationship between the instantaneous wake position and the lateral velocity that degraded with the evolution of the turbulent wind field during the time of downstream advection. A low-pass filter proportional to the advection time delay is recommended to remove small scales that become decorrelated even for distances within the typical spacing of wind turbine rows in a wind farm. The results also showed that the velocity at which wake meandering is transported downstream was slower than the inflow wind speed but faster than the velocity at the wake centre. This indicates that the modelling assumption of the wake as a passive scalar should be revised in the context of the downstream advection. Further, the strength of wake meandering increased linearly with the turbulence intensity of the lateral velocity and with the downstream distance. Wake meandering reduced the maximum velocity deficit of the temporally averaged wake and increased its width. Both effects scaled with the wake meandering strength. Lastly, we found that the fraction of the wake turbulence intensity that was caused by wake meandering decreased with downstream distance contrary to the wake meandering strength.
The wind turbine wake is a flow region of reduced wind speed and increased turbulence that extends downstream of a wind turbine for several rotor diameters. In wind farms the wake of an upstream turbine becomes the inflow of a downstream turbine, leading to power losses and increased mechanical wear, which translates into an increased cost of the energy. Therefore, understanding and predicting characteristics of wind turbine wakes has received extensive attention in the literature (see reviews by Vermeer et al., 2003; Sørensen, 2011; Sanderse et al., 2011; Mehta et al., 2014; Stevens and Meneveau, 2017; Porté-Agel et al., 2020).
One characteristic of wind turbine wakes is wake meandering, a low-frequency, large-scale oscillation of the entire wake in the lateral and vertical directions (Taylor et al., 1985). Two theories have been presented as the origin of wake meandering: (i) a passive advection of the entire wake by large-scale turbulence of the inflow (Larsen et al., 2008) and (ii) an intrinsic shear instability of the wake characterized by periodic vortex shedding (Medici and Alfredsson, 2006). Support for the passive advection hypothesis has been presented in Trujillo et al. (2011) and Keck et al. (2014) and for the shear instability hypothesis in Medici and Alfredsson (2006), Heisel et al. (2018), and Yang and Sotiropoulos (2019). The passive advection hypothesis forms the basis of the dynamic wake meandering model (Larsen et al., 2008), which assumes that wake meandering is driven by large-scale turbulence (with two rotor diameters used as a threshold). While the passive advection hypothesis assumes the inflow wind speed as the downstream propagation velocity of the wake meandering, Bingöl et al. (2010) reported better agreement between the dynamic wake meandering model and field measurements using a reduced wake velocity from the Jensen (1983) wake model.
Several characteristics of wake meandering have been reported in literature mainly from wind tunnel experiments. The strength (or amplitude) of wake meandering is larger in the lateral direction than in the vertical direction (España et al., 2012; Bastankhah and Porté-Agel, 2017), increases with downstream distance (Garcia et al., 2017), and depends on incoming boundary-layer characteristics (Bastankhah and Porté-Agel, 2017). The instantaneous horizontal wake position is correlated to the upstream transverse velocity for large wavelengths, and the correlation decreases with downstream distance (Muller et al., 2015; Aubrun et al., 2015).
In this paper, we use field measurements at a utility scale wind turbine across a wide range of turbulence intensities and wind speeds to investigate (i) the effect of the inflow state on the correlation between lateral velocity and instantaneous wake position, (ii) the downstream advection velocity of wake meandering, and (iii) the effect of wake meandering on the temporally averaged velocity deficit and the turbulence intensity of the wake. The present study extends on the investigations of Trujillo et al. (2011) on the effect of wake meandering on the mean wake and the turbulence intensity to a wider range of atmospheric conditions, validates the findings of Muller et al. (2015) from wind-tunnel-scale turbines with field experiments at a utility-scale wind turbine, and presents new insights into the limits of passive-advection-based wake meandering predictions.
This section introduces the measurement site, the measurement instruments, and the analysis approach of the measured data.
2.1 Measurement site and Doppler lidar setup
The measurement campaign was conducted at an isolated 2.5 MW Liberty C96 wind turbine from Clipper Windpower with a hub height (zhub) of 79 m and a rotor diameter (D) of 96 m located at the Kirkwood Community College campus in Cedar Rapids, Iowa, United States (Fig. 1). The immediate surroundings of the wind turbine as well as the area to the north and west are urbanized. The area to the south and east is agricultural farm land. The topography is characterized by gentle rolling hills. The data of the supervisory control and data acquisition (SCADA) system of the wind turbine are available, providing the temporal mean values of the wind speed at hub height (, where the bar indicates a temporal average), the nacelle position, and the yaw misalignment of the nacelle.
Two Doppler lidars of the type Stream Line manufactured by Halo Photonics were installed on the nacelle of the wind turbine. The Doppler lidar measures the radial (or line-of-sight) velocity along a laser beam that is emitted from a movable scanner head. The Doppler lidars were configured to measure with a sampling frequency of 3 Hz and a range gate length of 18 m. A positive value of the radial velocity corresponds to a motion away from the Doppler lidar, and a negative radial velocity is a motion towards the Doppler lidar.
The backward-facing Doppler lidar was programmed to perform 230 successive plan position indicator (PPI) scans of the wind turbine wake at hub height covering an azimuth range of from the rotor axis (Fig. 2a, red). The scanner was starting at az=168∘ and travelling at a speed of 6 ∘ s−1 to az=192∘ while continuously measuring, which resulted in an azimuth resolution of 2∘ (Fig. 2b). This scan pattern was completed within a 29 min period (a single PPI with return to the starting position took 7.2–7.6 s). A full set of 230 PPI scans will be defined as “wake scan” in the following. These wake scans were scheduled every second hour.
Coinciding with a wake scan, the forward-facing Doppler lidar was measuring in a horizontal staring mode at a 90∘ angle to the rotor axis for 14 min at a temporal resolution of 3 Hz (Fig. 2, blue). The rejection criteria for wake scans not suited for further analysis based on data quality, turbine yaw activity, and inflow characteristics will be presented at the beginning of Sect. 3.
2.2 Post-processing of measurements from the wake-scanning Doppler lidar
The wake scans are processed along the following steps to obtain the instantaneous wake position.
The remaining radial velocities are gridded on a polar coordinate system with an angular (ϕ) resolution of 2∘, a radial (r) resolution of 18 m, and a time stamp (t) aligning with the PPIs of the wake scans. The az positions of the lidar scans and the ϕ positions of the polar coordinate system can have a difference of 0.2∘ towards the end of a PPI, resulting from small variations of the scanner behaviour and fluctuations of the measurement frequency from PPI to PPI. Multiple measurements are available for the outside grid points due to a short resting time of the scanner at the turnaround point, and the measurements closest in time are used at those grid points.
The transition to a Cartesian coordinate system is made with and approximating with x=r (spatial error < 3 % based on geometry).
A instantaneous velocity deficit is computed with
where is the maximum of the velocity observed for each PPI of the wake scan at a given downstream distance. While this is not the longitudinal velocity deficit typically used in the literature, the effect of the lateral and vertical velocity on the wake centre position is negligible as shown in Appendix A. Appendix B explains our reasoning to compute the instantaneous velocity deficit relative to the instantaneous velocity outside of the wake and not relative to the mean wind speed at hub height.
The instantaneous position of the wake centre is detected in analogy to the centre of mass from the velocity deficit with
The above processing steps are applied for downstream distances between and . The double-peak shape of the near-wake was a problem for the detection of ycom for , and the decline of the SNR with increasing range led to gaps in the data for .
2.3 Post-processing of measurements from the laterally staring Doppler lidar
The time series of the lateral velocity component, v(t), is obtained from the seventh range gate at y=117 m of the Doppler lidar operating in the laterally staring mode. Range gates closer than y=117 m were either affected by near-range problems of the Doppler lidar (the first four range gates), or v(t) was biased towards motions away from the wind turbine and higher standard deviations compared to greater distances (fifth and sixth range gates). The latter might be caused by the influence of the wind turbine on the wind field. We inverted the sign of the Doppler velocity in order to have positive velocities towards the positive y direction in Fig. 2. We assume horizontal homogeneity of the inflow and that v(t) is representative for the lateral inflow velocity over the rotor area. Measurements with a SNR below −17 dB are removed from the time series, and the gaps are interpolated linearly.
Further, we derived two quantitative measures to characterize the inflow state from the laterally staring Doppler lidar. First, the lateral turbulence intensity is given by
where σ(v) is the standard deviation of v(t) over the 14 min period. It quantifies the strength of the lateral velocity fluctuations relative to the mean wind speed. Second, the integral timescale of the lateral velocity component, Ti,v, is estimated from the noise-corrected auto-correlation function of v(t) by fitting an exponential decay law (Lothon et al., 2006). It is a measure for the correlation length and can be interpreted as the scale of the dominant eddies of the turbulent wind field.
2.4 Advection velocity
Advection velocity is referring to the velocity of downstream propagation of wake meandering and is defined as
where Δx is a spatial separation in the x direction between two measuring points, and ΔTadv is the time delay between the wake meandering signals at the two points. Δx is known from the scan geometry, and ΔTadv is determined from the time lag of the maximized cross-correlation as described in the following steps. The cross-correlation is computed between v and ycom as well as between ycom at two spatially separated downstream distances. The terms upstream signal and downstream signal will refer to their relative streamwise position to each other.
Both, the upstream signal (v or ycom(x−0.5Δx)) and the downstream signal (ycom(Δx) or ycom(x+0.5Δx)), are low-pass filtered with a moving mean that has a window length of with β=3 (Cheng and Porté-Agel, 2018). The inverse proportionality of β to Iv proposed by Corrsin (1963) is not used here, because it is only valid for a convective atmospheric boundary layer, which cannot be ensured for all wake scans in our data set (e.g. at night-time).
If the upstream signal has a higher temporal resolution in the case of v(t), each time step of the downstream signal is paired with the temporally closest time step of the upstream signal for synchronization.
The cross-correlation function between the upstream signal and the downstream signal is computed for time lags between and .
If the cross-correlation function has a local maximum (i.e. not equal to the smallest or largest lag) with a correlation above 0.5, the corresponding time lag is selected as ΔTadv, and uadv is computed with Eq. (4).
The time series of ycom has a temporal resolution of Δts=7.2 s due to the time a single PPI scan takes (Sect. 2.1). Therefore, ΔTadv has to be a multiple of Δts, which results in a loss of precision (ϵ) for uadv given by
Assuming an upper limit of (Sect. 3.1.2 will show that uadv is smaller than or equal to for all cases), it is shown in Fig. 3 that the precision decreases for high wind speeds or small spatial separations. Only combinations of wind speed and spatial separation that result in a precision of at least will be used.
The scan setup described in Sect. 2.1 was implemented between 19 August and 2 October 2017. Data before 5 September 2017 are discarded due to a time synchronization problem with one of the Doppler lidars. To ensure high-quality measurement data and suitable conditions for the investigation, wake scans were rejected if
low SNR of the wake-scanning Doppler lidar led to gaps in the measurement data, which is quantified by a rejection rate of more than 0.5 % at any range gate between and (Sect. 2.2);
the SCADA data reported a non-operational wind turbine, yaw movements of the nacelle, or a mean wind speed below 5 m s−1;
the wake was partially outside of the Doppler lidar field of view, quantified by more than 25 % of either or being larger than the temporal mean of .
The remaining data set consists of 43 wake scans accompanied by measurements of the lateral velocity component of the inflow. A characterization of the data set is shown in Fig. 4. The data set covers a wind speed range between 5 and 11 m s−1 (Fig. 4a), and lateral turbulence intensities between <1 % and 8 % (Fig. 4b). The check on the wake position within the wake-scanning Doppler lidar's field of view implicitly ensured a good alignment of the wind turbine with the mean wind direction (Fig. 4c).
The results presented in the subsequent subsections are not differentiated according to the wind direction of the inflow. We assume that individual buildings in the vicinity of the wind turbine should not affect the measurements at zhub based on the blending height concept. Note that the roughness sublayer in an urban environment should not extend further than 5 times the building height (Grimmond and Oke, 1999), which is lower than zhub for an assumed building height of 10 m (two-storey and three-storey buildings).
3.1 Wake meandering
The first part of the results investigates the relationships between the instantaneous lateral velocity of the inflow and the instantaneous wake position.
3.1.1 Correlation between lateral velocity and wake position
Assuming the wake is advected passively and the turbulence field does not evolve during the downstream advection, a linear relationship between the lateral velocity at the turbine location and the wake centre position at a given downstream distance would be expected. For an evolving turbulent wind field, the autocorrelation function of a variable is expected to decay exponentially for idealized isotropic and homogeneous turbulence (Von Kármán, 1948). The rate at which the autocorrelation function decays is described by the integral timescale. Hence, we would expect a lower correlation between v(t) and ycom(t) for a given time lag (here the time delay due to advection), if the dominant features of the wind field have a short lifespan, which is equivalent to a fast decay of the autocorrelation function and a short integral timescale. Vice versa, a higher correlation is expected for a long integral timescale.
This hypothesis is confirmed in Fig. 5a, where the abscissa quantifies the aforementioned interplay of the time delay and the evolution of the turbulent field. Ti,v is the integral timescale of the lateral velocity component (Sect. 2.3), and ΔT is the time delay due to downstream advection as defined in the figure legend. Low values of the correlation between v(t) and ycom(t) are observed if the time delay is longer than the lifespan of the dominant eddies, and the correlation increases if the lifespan of the dominant eddies increases relative to the time delay. This result holds for the assumption of a downstream advection with the mean wind speed (black crosses in Fig. 5) as well as for the subset of the data set with a successful detection of the advection velocity based on the maximized cross-correlation (blue crosses in Fig. 5). The findings agree with expectation that the correlation decreases if a relatively larger amount of small-scale turbulence is included that is not expected to be correlated. Figure 6 shows an example case for a wake scan with high correlation (Fig. 6a and c) and a wake scan with low correlation (Fig. 6b and d).
Larsen et al. (2008) hypothesized that wake meandering is driven by large-scale turbulence and recommended 2 D as a low-pass-filter threshold. Applying a low-pass filter equivalent to 2 D to v(t) and ycom(t) does increase the correlation compared to the unfiltered data (Fig. 5b), supporting the assumption of large-scale turbulence as the driver of wake meandering.
Cheng and Porté-Agel (2018) proposed a low-pass-filter threshold proportional to the time delay due to downstream advection based on Taylor's diffusion theory (Taylor, 1922). Their filter size is given by with β=3 to account for the difference between Lagrangian and Eulerian scales (Angell et al., 1971). The results for this low-pass-filter threshold are similar to the ones for the threshold of 2 D at (Fig. 5c), but for this filter threshold maintains an improvement of the correlation of approximately 0.2, while the 2 D threshold decreases with downstream distance (Fig. 5d). This shows that the evolution of the turbulence field becomes important at sufficiently large downstream distances, and removing scales which are not expected to be correlated improves the correlation between v(t) and ycom(t).
Based on the above findings, we recommend using a low-pass-filter threshold based on the advection time delay as suggested by Cheng and Porté-Agel (2018) with a lower limit equivalent to 2 D for wake meandering predictions. This accounts for large-scale turbulence as the origin of wake meandering at short downstream distances but also accounts for the evolution of the turbulent wind field once it becomes relevant at larger downstream distances. The results also show that the evolution of the turbulent wind field frequently becomes relevant on scales that are similar to the distance between wind turbine rows in a wind farm.
3.1.2 Wake meandering strength and lateral turbulence intensity
The relationship between the lateral turbulence intensity of the inflow and the wake meandering strength is investigated. It can be visually observed that the fluctuations of ycom increase with the turbulence intensity of the lateral velocity component (Fig. 7). Quantifying the strength of wake meandering as the temporal standard deviation of ycom, an increase in the wake meandering strength with the lateral turbulence intensity is observed (Fig. 8a). The wake meandering strength also increases with downstream distance (Fig. 8b), which is explained with the longer downstream advection time leading to larger lateral displacement of the wake based on the lateral velocity. The range of the wake meandering strength at a given downstream distance in Fig. 8b is explained by the turbulence intensity range of the data set.
3.1.3 Downstream advection velocity of wake meandering
The advection velocity of wake meandering is investigated based on the time delay determined with a cross-correlation approach (Sect. 2.4). The majority of downstream advection velocities found from the time delay between v and ycom range between and (Fig. 9a). The majority of advection velocities found from cross-correlation of ycom at two downstream distances showed values between and (Fig. 9b). For both results, only cases with a sufficiently high cross-correlation and a distinct peak of the cross-correlation function were considered (Sect. 2.4). We assume that the results of the advection velocity reported in Fig. 9b are more robust compared to Fig. 9a, because the underlying correlations are higher, no assumptions on the origin of wake meandering are made, and any time synchronization issues between the two Doppler lidars cannot affect the result. The found advection velocities are in most cases lower then , but higher than the velocity at the wake centre (Fig. 9c). This finding is in line with Bingöl et al. (2010), who reported smaller errors of the dynamic wake meandering model if a reduced downstream advection velocity was used. The results are also in agreement with Zong and Porté-Agel (2020), who showed analytically that the advection velocity is bounded between and .
Cheng and Porté-Agel (2018) recommended the average of the mean wind speed and the velocity at the wake centre as an estimate for the advection velocity. It is given by , where is the temporal average of . A comparison of the detected advection velocities from the cross-correlation approach and shows reasonable agreement at a correlation of 0.7 (Fig. 10).
3.2 Effect on the time averaged wake
The second part of the results is investigating the effect of the wake meandering on the properties of the time-averaged wake. The effect of wake meandering is investigated by comparing the wake in the nacelle frame of reference and the meandering frame of reference following the approach of Trujillo et al. (2011). The transformation from the nacelle frame of reference to the meandering frame of reference is given by
where the tilde indicates the meandering frame of reference. After the transformation, the measurement data in the meandering frame of reference are interpolated on a regular grid using the nearest available measurement value for each grid point in the lateral direction. An example of the transformation is shown in Fig. 11a and b. This method of transformation retains fluctuations of the wake centre position smaller than the azimuth resolution of the wake scans. The irregular edge of the meandering frame of reference is caused by the limited azimuth range of the wake scans.
3.2.1 Mean velocity deficit
First, the effect of wake meandering on the longitudinal mean velocity deficit is investigated. It is given by
for the nacelle frame of reference and by
for the meandering frame of reference, where a bar indicates a temporal average. A qualitative comparison of the mean velocity deficit profile in both frames of reference shows a slightly deeper and narrower wake in the meandering frame of reference (Fig. 11c). For a quantitative investigation of the full data set, a Gaussian function given by
is fitted to the mean velocity deficit profile in both frames of reference. The fit coefficients σy and C describe the wake width and the wake depth, respectively. To assure that only cases with a Gaussian velocity deficit are considered, a correlation coefficient of at least 0.99 between fit and measurements is required or the result is discarded.
The results show that the depth of the mean wake in the nacelle frame of reference is smaller compared to the meandering frame of reference, and the difference increases with wake meandering strength (Fig. 12a). At the same time the wake is wider in the nacelle frame of reference, and the effect on the width increases with the wake meandering strength (Fig. 12b). Both observations agree with modelling results presented in Braunbehrens and Segalini (2019) and their explanation of a quasi-steady velocity deficit of the instantaneous wake that is spatially shifted and ensemble averaged to yield the time-averaged wake.
As the wake meandering strength increases with downstream distance (Fig. 8b), it could be expected that the observed differences of C and σy between the two frames of references also increase with downstream distance. For C this increase is not clearly observed (Fig. 12c), but σy shows the expected increase with downstream distance (Fig. 12d). It is possible that the expected trend for C is masked by the measurement errors, because its amplitude decreases with xD−1 due to the wake recovery. The transformation method from the nacelle frame of reference to the meandering frame of reference retains wake meandering on scales smaller than the lateral grid resolution, and, therefore, the shown results could be biased towards underestimating the effect of wake meandering on the temporally averaged wake.
3.2.2 Turbulence intensity
The effect of wake meandering on the turbulence intensity across the wake is investigated. An increase in the turbulence intensity from the meandering frame of reference to the nacelle frame of reference can be observed for the example case illustrating the transformation (Fig. 11d). This effect is quantified with the laterally averaged difference of the turbulence intensity between the two frames of reference. Lateral positions with less than 75 % data availability in the meandering frame of reference are discarded.
The results show that the turbulence intensity contributed by wake meandering increases with the strength of wake meandering (Fig. 13a). The magnitude of the turbulence intensity resulting from wake meandering decreases with downstream distance (Fig. 13b). This decrease in turbulence intensity due to wake meandering with xD−1, despite an increase in the wake meandering strength with xD−1 (Fig. 8b), could indicate that the recovery of the velocity deficit plays a more dominant role, compared with the wake meandering strength, in the far wake.
Atmospheric field measurements of the wind velocity from two Doppler lidars mounted on the nacelle of a utility-scale wind turbine were used to investigate wake meandering. The relationship between the lateral velocity component of the inflow and the instantaneous wake position and the effect of wake meandering on the time-averaged wake were analysed. The main conclusions of this study are as follows.
In agreement with previous wind tunnel studies, we observe that the strength (or amplitude) of wake meandering increases with the turbulence intensity of the inflow and with downstream distance from the wind turbine. Both trends appear to be linear.
A correlation between the lateral velocity component and the instantaneous wake position supports the passive advection hypothesis. Further, we found that the quality of the correlation depends on the ratio of the integral timescale of the lateral velocity to the time delay due to downstream advection, which can be explained by the evolution of the turbulent wind field during the downstream advection.
Applying a low-pass filter equivalent to 2 D improves the correlation between v and ycom for short downstream distances up to 5 D, supporting the hypothesis that large-scale turbulence has an important role in the origin of wake meandering. However, at large downstream distances beyond 5 D, a more suitable low-pass-filter threshold is based on the time delay due to downstream advection to remove scales that are expected to be decorrelated due to the evolution of the turbulent wind field.
The speed at which wake meandering propagates downstream is smaller than the inflow wind speed at hub height, but larger than the velocity at the wake centre. This indicates that the wake is not entirely passive and that at least for the downstream advection process the velocity deficit of the wake itself has an influence. Because the downstream advection time directly affects predictions of the instantaneous wake position, this could introduce a bias towards underestimating the wake meandering strength. The average of inflow wind speed at hub height and the average velocity at the wake centre as proposed by Cheng and Porté-Agel (2018) showed reasonable agreement with the observed advection velocities.
Wake meandering decreases the depth and increases the width of the time-averaged wake and contributes to the turbulence intensity of the wake. For all of those three quantities, the observed effect due to wake meandering was small relative to the base magnitude of the time-averaged wake itself. Only the effect on width of the time-averaged wake increased with downstream distance. The effect on the turbulence intensity decreased with downstream distance, and the effect on the wake depth did not show a clear increase or decrease with downstream distance. This suggests that adverse effects on downstream wind turbines resulting from wake meandering become less severe with increasing turbine spacing despite the wake meandering strength increasing with downstream distance.
In the future, the data set presented here could be used to validate and improve numerical models of wake meandering. These include, for example, the dynamic wake meandering model (Larsen et al., 2008) as well as the statistical wake meandering model of Thøgersen et al. (2017). Incorporating the effect of large-scale fluctuations of the wind speed on the downstream advection process and wake meandering is one lead we are planning to pursue in this direction.
The wake centre position computed with Eq. (2) uses the radial velocity instead of the longitudinal velocity. The presence of a lateral velocity component will bias the wake centre position, which will be discussed in the following.
To investigate the bias, we assumed a Gaussian wake for the longitudinal velocity component and a constant lateral velocity. The horizontal velocity vector is given by
with u0=6 m s−1, A=0.4u0, σy=40 m, and a variable lateral velocity v. Then the projected line-of-sight velocity that would be measured by the Doppler lidar is computed with
where is the unit vector in the beam direction for a PPI of the wake-scanning Doppler lidar (Fig. 2a). The resulting radial velocity profiles are shown in Fig. A1a for v=0 m s−1 (solid blue line) and v=2 m s−1 (solid black line). Then, the wake centre position was computed with Eq. (2) for both cases, and they are shown as vertical dotted lines in Fig. A1a. From the difference of wake centre positions between the two cases, a bias of the wake centre position is apparent. For the given example in Fig. A1a the difference between the two wake positions is m.
For each of the 43 cases investigated in Sect. 3, we extracted the maximum lateral velocity observed by Doppler lidar in the laterally staring mode and the mean wind speed from SCADA data. We then computed the bias of the wake position analogue to Fig. A1a for each case and compared it with the wake meandering strength in Fig. A1b. The bias of the wake position resulting from the lateral velocity is in all cases smaller than the wake meandering strength. The given biases can be regarded as an upper limit of the error, because we used the absolute maximum of the lateral velocity. Further, it should be noted that the bias of the wake position resulting from the lateral velocity is in the opposite direction to the expected wake displacement with the passive advection hypothesis. Therefore, the error would be reducing the correlations shown in Fig. 5 and not artificially inflating them.
The presence of a vertical velocity will not bias the wake position, because it will affect the radial velocity on both sides of the PPI identically.
Two definitions of the instantaneous velocity deficit are compared, and their effect on the detection of the instantaneous wake position is discussed. The first definition is relative to the mean wind speed of the inflow at hub height given by
The second definition is relative to the instantaneous ambient wind speed outside of the wake given by
where is the maximum of the radial velocity for a given time and downstream distance, which is taken as the instantaneous velocity outside of the wake. The effect that those two definitions of have on the wake position computed with Eq. (2) will be investigated by assuming a Gaussian wake given by
Both definitions yield the same velocity deficit for a stationary ambient flow outside of the wake and subsequently identical wake centre positions (Fig. B1a–c). For a non-stationary ambient wind speed, the two velocity deficit definitions lead to different results for the wake centre position (Fig. B1d–f), and only the definition given by Eq. (B2) reproduces the sinusoidal input for the wake meandering. The above observations from the idealized cases can also be found in our field measurements (Fig. B1g–i). Negative values of Δu in Fig. B1f and i were set to zero for the computation of ycom, because the centre-of-mass method (Eq. 2) does not work for negative values.
We will use the velocity deficit definition based on in this paper, because it provides a better detection of the wake centre position. However, the results presented in Sect. 3 hold for both definitions of the velocity deficit. It should be noted that the definition based on removes a portion of the inflow turbulence from the velocity deficit field of the wake, and, therefore, the turbulence intensity should be computed from directly and not .
The data are not publicly available because of the permission of the wind turbine owner.
PB contributed to the data curation, formal analysis, conceptualization, methodology, software, validation, visualization, and writing (original draft). FPA contributed to the conceptualization, funding acquisition, project administration, supervision, and writing (review and editing). CDM contributed to the funding acquisition, resources, data curation, and investigation.
The contact author has declared that neither they nor their co-authors have any competing interests.
Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
The authors would like to thank Kirkwood Community College for their cooperation and allowing access to their wind turbine. We also extend our appreciation to Clipper Windpower for granting access to technical data on the Liberty wind turbine.
This research has been supported by the Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung (grant no. 200021_172538), the Bundesamt für Energie (grant no. SI/502135-01), the National Science Foundation Iowa EPSCoR (grant no. 1101284), and the Center for Global and Regional Environmental Research, University of Iowa (Optimization of wind energy projects using experimental and computational fluid dynamics).
This paper was edited by Horia Hangan and reviewed by two anonymous referees.
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