Comparison of the atmospheric stability and wind profiles at two wind farm sites over a long marine fetch in the North Sea

A comparison of the atmospheric stability and wind profiles using data from meteorological masts located near two wind farm sites in the North Sea, Egmond aan Zee (up to 116 m) in the Dutch North Sea and Horns Rev (HR; up to 45 m) in the Danish North Sea, is presented. Only the measurements that represent long marine fetch are considered. It was observed that within a long marine fetch, the conditions in the North Sea are dominated by unstable [41% at Egmond aan Zee Offshore Wind Farm (OWEZ) and 33% at HR] and near-neutral conditions (49% at OWEZ and 47% at HR), and stable conditions (10% at OWEZ and 20% at HR) occur for a limited period. The logarithmic wind profiles with the surface-layer stability correction terms and Charnock's roughness model agree with the measurements at both sites in all unstable and near-neutral conditions. An extended wind profile valid for the entire boundary layer is compared with the measurements. For the tall mast at Egmond aan Zee, it was found that for stable conditions, the scaling of the wind profiles with respect to boundary-layer height is necessary, and the addition of another length scale parameter is preferred. At the lower mast at HR, the effect was not noticeable. Copyright © 2011 John Wiley & Sons, Ltd.

[1]  S. Gryning,et al.  Measurements and Modelling of the Wind Speed Profile in the Marine Atmospheric Boundary Layer , 2008 .

[2]  S. Gryning,et al.  Offshore wind profiling using light detection and ranging measurements , 2009 .

[3]  Stefan Emeis,et al.  Atmospheric boundary-layer structure from simultaneous SODAR, RASS, and ceilometer measurements , 2004 .

[4]  Albert A. M. Holtslag,et al.  ANALYSIS OF WIND SPEED OBSERVATIONS OVER THE NORTH SEA , 1996 .

[5]  J. Garratt Review of Drag Coefficients over Oceans and Continents , 1977 .

[6]  Wim Turkenburg,et al.  Evaluation of stability corrections in wind speed profiles over the North Sea , 1990 .

[7]  S. Larsen,et al.  On the extension of the wind profile over homogeneous terrain beyond the surface boundary layer , 2007 .

[8]  U. Högström Non-dimensional wind and temperature profiles in the atmospheric surface layer: A re-evaluation , 1988 .

[9]  Rebecca J. Barthelmie,et al.  The influence of non‐logarithmic wind speed profiles on potential power output at Danish offshore sites , 2005 .

[10]  Christopher W. Fairall,et al.  Convective Profile Constants Revisited , 2000 .

[11]  Pierre Pinson,et al.  Wind fluctuations over the North Sea , 2011 .

[12]  Alfredo Peña,et al.  Analysis of diabatic flow modification in the internal boundary layer , 2011 .

[13]  Albert A. M. Holtslag,et al.  Estimates of diabatic wind speed profiles from near-surface weather observations , 1984 .

[14]  Petra Seibert,et al.  Review and intercomparison of operational methods for the determination of the mixing height , 2000 .

[15]  Kimmo K. Kahma,et al.  Reconciling Discrepancies in the Observed Growth of Wind-generated Waves , 1992 .

[16]  W.A.A.M. Bierbooms,et al.  Influence of different wind profiles due to varying atmospheric stability on the fatigue life of wind turbines , 2007 .

[17]  Alfredo Peña,et al.  Charnock’s Roughness Length Model and Non-dimensional Wind Profiles Over the Sea , 2008 .

[18]  J. Walmsley On theoretical wind speed and temperature profiles over the sea with applications to data from sable island, Nova Scotia , 1988 .

[19]  R. Berkowicz,et al.  Evaluation of the profile method for estimation of surface fluxes of momentum and heat , 1982 .

[20]  E. F. Bradley,et al.  Flux-Profile Relationships in the Atmospheric Surface Layer , 1971 .

[21]  H. Charnock Wind stress on a water surface , 1955 .

[22]  E. F. Bradley,et al.  Cool‐skin and warm‐layer effects on sea surface temperature , 1996 .

[23]  B. Lange,et al.  Importance of thermal effects and sea surface roughness for offshore wind resource assessment , 2004 .

[24]  Jørgen Højstrup,et al.  The Influence of Thermal Effects on the Wind Speed Profile of the Coastal Marine Boundary Layer , 2004 .

[25]  Charlotte Bay Hasager,et al.  Length Scales of the Neutral Wind Profile over Homogeneous Terrain , 2010 .

[26]  Christopher W. Fairall,et al.  Dependence of the Monin–Obukhov Stability Parameter on the Bulk Richardson Number over the Ocean , 1997 .

[27]  Charlotte Bay Hasager,et al.  Comparing mixing-length models of the diabatic wind profile over homogeneous terrain , 2010 .

[28]  S. Larsen,et al.  On the Dependence of Sea Surface Roughness on Wind Waves , 1998 .

[29]  A. Dyer A review of flux-profile relationships , 1974 .

[30]  Sven-Erik Gryning,et al.  Dispersion from a continuous ground‐level source investigated by a K model , 1983 .