Evaluation of four numerical wind flow models for wind resource mapping

被引:47
作者
Beaucage, Philippe [1 ]
Brower, Michael C. [1 ]
Tensen, Jeremy [1 ]
机构
[1] AWS Truepower LLC, Albany, NY USA
关键词
wind flow modeling; numerical weather prediction model; large-eddy simulation; computational fluid dynamics; wind resource assessment; wind energy; STRATIFIED BOUNDARY-LAYER; NONHYDROSTATIC ATMOSPHERIC SIMULATION; PREDICTION SYSTEM ARPS; LARGE-EDDY SIMULATION; COMPLEX TERRAIN; STABILITY; DYNAMICS; ENERGY; CFD;
D O I
10.1002/we.1568
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
A wide range of numerical wind flow models are available to simulate atmospheric flows. For wind resource mapping, the traditional approach has been to rely on linear Jackson-Hunt type wind flow models. Mesoscale numerical weather prediction (NWP) models coupled to linear wind flow models have been in use since the end of the 1990s. In the last few years, computational fluid dynamics (CFD) methods, in particular Reynolds-averaged Navier-Stokes (RANS) models, have entered the mainstream, whereas more advanced CFD models such as large-eddy simulations (LES) have been explored in research but remain computationally intensive. The present study aims to evaluate the ability of four numerical models to predict the variation in mean wind speed across sites with a wide range of terrain complexities, surface characteristics and wind climates. The four are (1) Jackson-Hunt type model, (2) CFD/RANS model, (3) coupled NWP and mass-consistent model and (4) coupled NWP and LES model. The wind flow model predictions are compared against high-quality observations from a total of 26 meteorological masts in four project areas. The coupled NWP model and NWP-LES model produced the lowest root mean square error (RMSE) as measured between the predicted and observed mean wind speeds. The RMSE for the linear Jackson-Hunt type model was 29% greater than the coupled NWP models and for the RANS model 58% greater than the coupled NWP models. The key advantage of the coupled NWP models appears to be their ability to simulate the unsteadiness of the flow as well as phenomena due to atmospheric stability and other thermal effects. Copyright (c) 2012 John Wiley & Sons, Ltd.
引用
收藏
页码:197 / 208
页数:12
相关论文
共 56 条
[1]  
Adrian G., 1991, Contributions to Atmospheric Physics, V64, P27
[2]   LARGE-EDDY SIMULATION OF A NEUTRALLY STRATIFIED BOUNDARY-LAYER - A COMPARISON OF 4 COMPUTER CODES [J].
ANDREN, A ;
BROWN, AR ;
GRAF, J ;
MASON, PJ ;
MOENG, CH ;
NIEUWSTADT, FTM ;
SCHUMANN, U .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1994, 120 (520) :1457-1484
[3]  
[Anonymous], 1989, EUROPEAN WIND ATLAS
[5]   Urban Flow and Dispersion Simulation Using a CFD Model Coupled to a Mesoscale Model [J].
Baik, Jong-Jin ;
Park, Seung-Bu ;
Kim, Jae-Jin .
JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY, 2009, 48 (08) :1667-1681
[6]   The effects of atmospheric stability on coastal wind climates [J].
Barthelmie, RJ .
METEOROLOGICAL APPLICATIONS, 1999, 6 (01) :39-47
[7]   A MIXED SPECTRAL FINITE-DIFFERENCE MODEL FOR NEUTRALLY STRATIFIED BOUNDARY-LAYER FLOW OVER ROUGHNESS CHANGES AND TOPOGRAPHY [J].
BELJAARS, ACM ;
WALMSLEY, JL ;
TAYLOR, PA .
BOUNDARY-LAYER METEOROLOGY, 1987, 38 (03) :273-303
[8]  
Berge E, 2006, P EWEC ATH GREEC
[9]   Numerical evaluation of wind flow over complex terrain:: Review [J].
Bitsuamlak, GT ;
Stathopoulos, T ;
Bédard, C .
JOURNAL OF AEROSPACE ENGINEERING, 2004, 17 (04) :135-145
[10]  
Brower M, 2004, P AM MET SOC C SEATT