2015
DOI: 10.1175/jtech-d-14-00123.1
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Addressing Spatial Variability of Surface-Layer Wind with Long-Range WindScanners

Abstract: This paper presents an analysis of mean wind measurements from a coordinated system of long-range WindScanners. From individual scan patterns the mean wind field was reconstructed over a large area, and hence it highlights the spatial variability. From comparison with sonic anemometers, the quality of the WindScanner data is high, although the fidelity of the estimated vertical velocity component is significantly limited by the elevation angles of the scanner heads. The system of long-range WindScanners presen… Show more

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Cited by 31 publications
(40 citation statements)
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References 24 publications
(20 reference statements)
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“…The maximum range of LRWSs is about 8 km, which has been typically observed in offshore conditions (Floors et al, 2016). Due to its characteristics, the long-range WindScanner system is primarily intended for measurements of mean flow fields within a large area of the atmosphere (e.g., Berg et al, 2015).…”
Section: Windscanner Systemsmentioning
confidence: 99%
See 1 more Smart Citation
“…The maximum range of LRWSs is about 8 km, which has been typically observed in offshore conditions (Floors et al, 2016). Due to its characteristics, the long-range WindScanner system is primarily intended for measurements of mean flow fields within a large area of the atmosphere (e.g., Berg et al, 2015).…”
Section: Windscanner Systemsmentioning
confidence: 99%
“…The elevation angle at which the beams were directed was in a range from about −12 to 23 • . Even though we had three independent LOS measurement along the virtual mast due to low elevation angles only the horizontal components of the wind vector (i.e., u and v) were considered in the data analysis (see explanations in Berg et al, 2015;Debnath et al, 2017). The long-range WindScanner system's scans were run in a batch mode, where each strategy was executed over a 10 min period.…”
Section: 7mentioning
confidence: 99%
“…Uncertainties in 3-D wind-field retrievals using triple-Doppler lidar techniques have also been investigated. For example, Mann et al (2009), Fuertes et al (2014 and Newman et al (2016) present a detailed analysis of 3-D winds and turbulence measurements made using staring triple-Doppler measurements, while Berg et al (2015) present validation of 3-D wind measurements made through continuous scanning.…”
Section: Introductionmentioning
confidence: 99%
“…One of these scanning lidars is the long-range WindScanner; it can be used to map the line-of-sight (LOS) wind velocities over a predetermined scanning pattern [11][12][13] and, by assuming certain flow properties in the scanned volume, the wind speed components can be estimated. Three spatially-separated WindScanners can be synchronized and the flow field estimated without making any assumptions, while with two WindScanners the horizontal wind vector can be estimated by assuming that the vertical component is zero.…”
Section: Introductionmentioning
confidence: 99%