2008
DOI: 10.1007/s10546-008-9285-y
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Charnock’s Roughness Length Model and Non-dimensional Wind Profiles Over the Sea

Abstract: An analysis tool for the study of wind speed profiles over the water has been developed. The profiles are analysed using a modified dimensionless wind speed and dimensionless height, assuming that the sea surface roughness can be predicted by Charnock's roughness length model. In this form, the roughness dependency on wind speed is extracted and the variations on the wind profile are due solely to atmospheric stability. The use of the Charnock's non-dimensional wind profile is illustrated using data collected … Show more

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Cited by 59 publications
(37 citation statements)
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“…In order to minimize flow blockage effects, the computational domain is set to a height L z = 1045.9 m in all the simulations. A constant streamwise pressure gradient is used to drive the flow within the boundary layer, which has a height of δ = 500 m. This value is consistent with the boundary-layer depth observed by Peña and Gryning [23] at…”
Section: Case Descriptionsupporting
confidence: 72%
“…In order to minimize flow blockage effects, the computational domain is set to a height L z = 1045.9 m in all the simulations. A constant streamwise pressure gradient is used to drive the flow within the boundary layer, which has a height of δ = 500 m. This value is consistent with the boundary-layer depth observed by Peña and Gryning [23] at…”
Section: Case Descriptionsupporting
confidence: 72%
“…In the EU-Norsewind project the vertical extrapolation is being investigated using data from an array of wind profiling lidars observing at 70 to 200 m above sea level installed in the Northern European Seas. Lidar-based results show that the wind profile deviates from the surface-layer wind profile high in the boundary layer [38][39][40][41]. Mesoscale modeling of the offshore wind resource is on-going and comparison of results is in progress, yet beyond the scope of the present paper.…”
Section: Examination Of Wind Resource Statisticsmentioning
confidence: 91%
“…Wind profiles onshore have been extensively discussed in number of the atmospheric studies so far. In addition, wind profiles offshore have been also analyzed with measurements take from offshore meteorological masts [2][3][4][5][6] , as offshore wind power generation has been increasing in northern European countries. By analyzing the measurements taken from a met mast, Lange et al (2004) [2] showed that the offshore wind profiles not only have smaller vertical wind shears than those onshore, which is attributable to the small aerodynamic roughness over the sea, but also are strongly dependent on atmospheric stability, which is determined by the temperature gradient between the air and seawater, and the surface wind speed.…”
Section: Introductionmentioning
confidence: 99%
“…However, since the log profile model, which assumes a neutral stability condition, does not take into account the stability effects, it cannot be used for offshore wind profile estimations. Thus, new wind profile models based on Monin-Obkhov similarity (MOS) theory, which adds a correction term for the stability effects to the log profile model, have been developed [4][5][6] . These previous studies have focused mainly on the winds from the open ocean, which are not significantly influenced by land.…”
Section: Introductionmentioning
confidence: 99%