2016
DOI: 10.5194/amt-9-1993-2016
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Evaluation of three lidar scanning strategies for turbulence measurements

Abstract: Abstract.Several errors occur when a traditional Doppler beam swinging (DBS) or velocity-azimuth display (VAD) strategy is used to measure turbulence with a lidar. To mitigate some of these errors, a scanning strategy was recently developed which employs six beam positions to independently estimate the u, v, and w velocity variances and covariances. In order to assess the ability of these different scanning techniques to measure turbulence, a Halo scanning lidar, WindCube v2 pulsed lidar, and ZephIR continuous… Show more

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Cited by 64 publications
(91 citation statements)
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References 34 publications
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“…In this study we demonstrate that σ 2 u can be estimated by FL nacelle lidars, and current research demonstrates that lidar-based σ 2 u values reduce the gap between loads and power measurements, as well as simulations. It is difficult to compare our results with those from previous work on lidar turbulence measurements Newman et al, 2016). First, with a FL lidar we are able to point the beam in a direction close to the mean wind, whereas most lidars use beams pointing closer to the vertical wind component.…”
Section: Discussioncontrasting
confidence: 50%
“…In this study we demonstrate that σ 2 u can be estimated by FL nacelle lidars, and current research demonstrates that lidar-based σ 2 u values reduce the gap between loads and power measurements, as well as simulations. It is difficult to compare our results with those from previous work on lidar turbulence measurements Newman et al, 2016). First, with a FL lidar we are able to point the beam in a direction close to the mean wind, whereas most lidars use beams pointing closer to the vertical wind component.…”
Section: Discussioncontrasting
confidence: 50%
“…However, due to the equations for computing each component of the Reynolds stress tensor, the effect of noise within each individual measurement is magnified. In particular, if there is a large amount of noise in the vertical beam compared to other beams from differences in SNR, then negative values of σ 2 u and σ 2 v can be computed (Newman et al, 2016), which is not realistic. Thus, if the observations within each beam are taken at a quick enough sampling rate to resolve the inertial subrange, the autocovariance technique should be applied to variances calculated from each beam before computing the velocity variances.…”
Section: Possible Applications To Other DL Scanning Techniquesmentioning
confidence: 99%
“…Several different DL scanning strategies outlined in Sect. 1 were tested for comparison of turbulence measurements with those collected from sonic anemometers, which have been compared by (Newman et al, 2016). Herein, we focus on measurements taken between 17:00 UTC (11:00 local standard time, LST) 26 March and 15:00 UTC (09:00 LST) 28 March, when two DLs were placed within 2 m of the sonic anemometer booms on the 300 m tower.…”
Section: Experiments and Instrumentationmentioning
confidence: 99%
“…Accordingly, uncertainties in lidar-derived mean wind velocity estimates have been well characterized Lindelöw-Marsden, 2009) and methods and procedures have been developed for error reduction and uncertainty control (Clifton et al, 2013;Gottschall et al, 2012). However, use of lidar for turbulence measurements, while possible (Newman et al, 2016;Branlard et al, 2013;Mann et al, 2010), is less established (Sathe et al, 2015;Sathe and Mann, 2013). Two methods are commonly used to derive the second-order moments (i.e., velocity variances and momentum fluxes) of turbulent flow from lidar data (Sathe and Mann, 2013).…”
Section: Motivation and Approachmentioning
confidence: 99%
“…The first method can suffer from cross-contamination errors (biases) due to the correlation between the radial velocities used for wind velocity estimates (Sathe et al, 2011). Therefore, the second method is considered to be more suitable for lidar turbulence measurements (Newman et al, 2016;Sathe et al, 2015;Sathe and Mann, 2013;Mann et al, 2010) Using the second method mentioned above, errors in the estimated variances and momentum fluxes are accumulations of the following three types of errors in the estimated radial velocity variance:…”
Section: Motivation and Approachmentioning
confidence: 99%