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The wind profile power law is a relationship between the wind speeds at one height, and those at another. The power law is often used in wind power assessments〔Elliott, D.L., C.G. Holladay, W.R. Barchet, H.P. Foote, and W.F. Sandusky, 1986, Pacific Northwest Laboratory, Richland, WA. (Wind Energy Resource Atlas of the United States )〕〔Peterson, E.W. and J.P. Hennessey, Jr., 1978, ''On the use of power laws for estimates of wind power potential'', J. Appl. Meteorology, Vol. 17, pp. 390-394〕 where wind speeds at the height of a turbine (>~ 50 metres) must be estimated from near surface wind observations (~10 metres), or where wind speed data at various heights must be adjusted to a standard height〔Robeson, S.M., and Shein, K.A., 1997, ''Spatial coherence and decay of wind speed and power in the north-central United States'', Physical Geography, Vol. 18, pp. 479-495〕 prior to use. Wind profiles are generated and used in a number of atmospheric pollution dispersion models. The wind profile of the atmospheric boundary layer (surface to around 2000 metres) is generally logarithmic in nature and is best approximated using the log wind profile equation that accounts for surface roughness and atmospheric stability. The wind profile power law relationship is often used as a substitute for the log wind profile when surface roughness or stability information is not available. The wind profile power law relationship is: : where is the wind speed (in metres per second) at height (in metres), and is the known wind speed at a reference height . The exponent () is an empirically derived coefficient that varies dependent upon the stability of the atmosphere. For neutral stability conditions, is approximately 1/7, or 0.143. In order to estimate the wind speed at a certain height ''z'', the relationship would be rearranged to: : The value of 1/7 for α is commonly assumed to be constant in wind resource assessments, because the differences between the two levels are not usually so great as to introduce substantial errors into the estimates (usually < 50 m). However, when a constant exponent is used, it does not account for the roughness of the surface, the displacement of calm winds from the surface due to the presence of obstacles (i.e., zero-plane displacement), or the stability of the atmosphere.〔Touma, J.S., 1977, ''Dependence of the wind profile power law on stability for various locations'', J. Air Pollution Control Association, Vol. 27, pp. 863-866〕〔Counihan, J., 1975, ''Adiabatic atmospheric boundary layers: A review and analysis of data from the period 1880-1972'', Atmospheric Environment, Vol.79, pp. 871-905〕 In places where trees or structures impede the near-surface wind, the use of a constant 1/7 exponent may yield quite erroneous estimates, and the log wind profile is preferred. Even under neutral stability conditions, an exponent of 0.11 is more appropriate over open water (e.g., for offshore wind farms), than 0.143,〔Hsu, S.A., E.A. Meindl, and D.B. Gilhousen, 1994, ''Determining the power-law wind-profile exponent under near-neutral stability conditions at sea'', J. Appl. Meteor., Vol. 33, pp. 757-765〕 which is more applicable over open land surfaces. ==Wind power density== Estimates of wind power density are presented as wind class, ranging from 1 to 7. The speeds are average wind speeds over the course of a year,〔(Classes of wind power density at 10 m and 50 m )〕 although the frequency distribution of wind speed can provide different power densities for the same average wind speed.〔(Comparison of annual average wind power at three sites with identical wind speeds. )〕 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「wind profile power law」の詳細全文を読む スポンサード リンク
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