2015
DOI: 10.1016/j.jweia.2014.12.008
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A comparative study of field measurements of the turbulence characteristics of typhoon and hurricane winds

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Cited by 69 publications
(32 citation statements)
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“…The estimated surface roughness ( z 0 ) varies in the range of 0.2–7 mm, which is in good agreement with the representative values of z 0 (0.2–5 mm) for sea terrain as recommended by Wieringa . Furthermore, the estimated surface roughness compares favorably to the values reported by Yu and Chowdhury and Li et al, which are z 0 = 0.2–7 mm and z 0 = 0–5 mm, respectively.…”
Section: Wind Profiles and Turbulence Parameterssupporting
confidence: 87%
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“…The estimated surface roughness ( z 0 ) varies in the range of 0.2–7 mm, which is in good agreement with the representative values of z 0 (0.2–5 mm) for sea terrain as recommended by Wieringa . Furthermore, the estimated surface roughness compares favorably to the values reported by Yu and Chowdhury and Li et al, which are z 0 = 0.2–7 mm and z 0 = 0–5 mm, respectively.…”
Section: Wind Profiles and Turbulence Parameterssupporting
confidence: 87%
“…Figure also shows comparisons of the measurements of turbulence intensity with those reported by Yu and Chowdhury and Li et al for sea terrain. On the basis of the FCMP datasets, Yu and Chowdhury suggested the mean longitudinal and lateral turbulence intensities of 0.113 and 0.1 at 10‐m height for z 0 = 0.2–1 mm, respectively, whereas the mean longitudinal turbulence intensity was 0.126 at 5‐m height.…”
Section: Wind Profiles and Turbulence Parametersmentioning
confidence: 65%
“…The profiles of wind velocity and turbulence level at the inlet were represented by exponential rates. In Figure , a comparison between the simulation values, theoretical values, and some measured values of average wind velocity and turbulence level profile at the atmospheric boundary layer is given. The fluctuating wind spectrum generated from numerical simulation was fitted and compared with Davenport spectrum, Harris spectrum, Karman spectrum, and measured spectrum, which are as shown in Figure .…”
Section: Numerical Simulation Of Mean Wind Loadmentioning
confidence: 99%
“…They differ from ordinary strong winds and hurricanes by their more intensive rotation and their convergent airflows, extreme wind speeds and turbulence intensities, ascending and sinking airflows, sharp changes in the wind direction, etc. [5,6]. Since most high-power offshore WTs were designed and produced in the US or Europe in compliance with standards for extratropical conditions, their operation under tropical typhoon conditions is subjected to a high risk of WT tower collapse and blade fracture, notwithstanding the shutdown/emergency stop measures.…”
Section: Introductionmentioning
confidence: 99%