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 from a meteorological mast installed in the Danish North Sea. The best fit with the observed mean non-dimensional wind profile under neutral atmospheric conditions is found using a value of 1.2 × 10−2 for Charnock’s parameter. The stability correction on the neutral wind profile suggested by the Businger-Dyer relations was found to perform well over the sea.
Similar content being viewed by others
References
Barthelmie R, Hansen OF, Enevoldsen K, Højstrup J, Frandsen S, Pryor S, Larsen S, Motta M, Sanderhoff P (2005) Ten years of meteorological measurments for offshore wind farms. J Sol Energy Eng 127(2): 170–176
Beran J, Calveri L, Lange B, von Bremen L (2005) Offshore wind modeling and forecast. WRF/MM5 Users Workshop (http://www.mmm.ucar.edu/wrf/users/workshops/ws2005/abstracts/session3)
Blackadar AK (1962) The vertical distribution of wind and turbulent exchange in a neutral atmosphere. J Geophys Res 67(8): 3095–3102
Businger JA, Wyngaard JC, Izumi Y, Bradley EF (1971) Flux-profile relationships in the atmospheric surface layer. J Atmos Sci 28: 181–189
Charnock H (1955) Wind stress over a water surface. Quart J Roy Meteorol Soc 81: 639–640
Deacon EL (1962) Aerodynamic roughness length of the sea. J Geophys Res 67(8): 3167–3172
Doms G, Schättler U (1999) The Non-hydrostatic limited area model (Lokalmodell) of DWD. Part I: scientific documentation. Technical report, Deutscher Wetterdienst (DWD), Offenbach, Germany
Dyer AJ (1974) A review of flux-profile relationships. Boundary-Layer Meteorol 7: 363–372
Garratt JR (1977) Review of drag coefficients over oceans and continents. Mon Wea Rev 105: 915–929
Gryning S-E, Batchvarova E, Brümmer B, Jørgensen H, Larsen S (2007) On the extension of the wind profile over homogeneous terrain beyond the surface layer. Boundary-Layer Meteorol 124: 251–268
Hara T, Belcher SE (2004) Wind profile and drag coefficient over mature ocean surface wave spectra. J Phys Oceanogr 34: 2345–2358
Hasse L (1968) Zur Bestimmung der vertikalen Transporte von Impuls und fühlbarer Wärme in der wassernahen Luftschlicht über See. (On the determination of the vertical transports of momentum and heat in the atmospheric boundary layer at sea). Hamburger Geophysikalische Einzelschriften, Heft 11
Högström U (1987) Non-dimensional wind and temperature profiles in the atmospheric surface layer: a re-evaluation. Boundary-Layer Meteorol 42: 55–78
Högström U, Smedman A-S, Bergström H (2006) Calculation of wind speed variation with height over the sea. Wind Eng 30: 269–286
Kaimal JC, Gaynor JE (1991) Another look at sonic thermometry. Boundary-Layer Meteorol 56: 401–410
Källstrand B (1998) Low level jets in a marine boundary layer during spring. Contr Atmos Phys 71: 359–373
Kraus EB (1972) Atmosphere-Ocean interaction. Oxford University Press, London, p 275 pp
Lange B, Larsen S, Højstrup J, Barthelmie R (2004a) Importance of thermal effects and the sea surface roughness for offshore wind resource assessment. J Wind Eng Ind Aerodyn 92: 959–988
Lange B, Larsen S, Højstrup J, Barthelmie R (2004b) The influence of thermal effects on the wind speed profile of the coastal marine boundary layer. Boundary-Layer Meteorol 112: 587–617
Larsén XG (2003) Air-sea exchange of momentum and sensible heat over the Baltic Sea. Acta Universitatis Upsaliensis, Comprehensive summaries of Uppsala Dissertations form the Faculty of Science and Technology 820, ISBN 91-554-5565-4. Uppsala
Mahrt L, Vickers D, Edson J, Sun J, Højstrup J, Hare J, Wilczak JM (1998) Heat flux in the coastal zone. Boundary-Layer Meteorol 86(3): 421–446
Miyake M, Donelan M, McBean G, Paulson C, Badgley F, Leavitt E (1970) Comparison of turbulent fluxes over water determined by profile and eddy covariation techniques. Quart J Roy Meteorol Soc 96(407): 132–137
Neumann T, Emeis S, Illig C (2006) Report on the research project OWID—offshore wind design parameter. DEWI Magaz 28: 51–53
Panofsky HA (1973) Tower Micrometeorogy. In: Haugeb DA (ed) Workshop on Micrometeorolgy. American Meteorology Society, pp 151–176
Peña A, Hasager CB, Gryning S-E, Courtney M, Antoniou I, Mikkelsen T (2008) Offshore wind profiling using LiDAR measurements. Wind Energy, in press
Prandtl L (1932) Meteorologische Anwendung der Strömungslehre. Beitr Physik der freien Atmosphäre, Bjerknes Festschrift 188–202
Sempreviva AM, Larsen SE, Mortensen NG, Troen I (1990) Response of neutral boundary layers to changes of roughness. Boundary-Layer Meteorol 50: 205–225
Smedman A-S, X Guo Larsén, Högström U, Kahma KK, Peterson H (2003) Effect of the sea state on the momentum exchange over the sea during neutral conditions. J Geophys Res 108(C11): 3367 doi:10.1029/2002JC001526
Smith SD (1970) Thrust-anemometer measurements of wind turbulence, Reynolds stress, and drag coefficient over the sea. J Geophys Res 75(33): 6758–6770
Smith SD (1980) Wind stress and heat flux over the ocean in the Gale force winds. J Phys Oceanogr 10: 709–726
Stull RB (1988) An introduction to boundary layer meteorology. Kluwer Academic Publishers, Dordrecht, p 666 pp
Tambke J, Lange M, Focken U, Wolff J-O, John A, Bye T (2005) Forecasting offshore wind speeds above the North Sea. Wind Energy 8: 3–16
Weiler HS, Burling RW (1967) Direct measurements of stress and spectra of turbulence in the boundary level over the sea. J Atmos Sci 24: 653–664
Zilitinkevich SS, Mironov DV (1996) A multi-limit formulation for the equilibrium depth of a stably stratified boundary layer. Boundary-Layer Meteorol 81: 325–351
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Peña, A., Gryning, SE. Charnock’s Roughness Length Model and Non-dimensional Wind Profiles Over the Sea. Boundary-Layer Meteorol 128, 191–203 (2008). https://doi.org/10.1007/s10546-008-9285-y
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s10546-008-9285-y