Linear and nonlinear models in wind resource assessment and wind turbine micro-siting in complex terrain

被引:150
作者
Palma, J. M. L. M. [1 ]
Castro, F. A. [2 ]
Ribeiro, L. F. [3 ]
Rodrigues, A. H. [4 ]
Pinto, A. P. [4 ]
机构
[1] Univ Porto, Fac Engn, Res Ctr Wind Energy & Atmospher Flows, CEsA, P-4200465 Oporto, Portugal
[2] Inst Super Engn Porto, CEsA, Res Ctr Wind Energy & Atmospher Flows, P-4200072 Oporto, Portugal
[3] Inst Politecn Braganca, CEsA, Res Ctr Wind Energy & Atmospher Flows, P-5301854 Braganca, Portugal
[4] INEGI, CEsA, Res Ctr Wind Energy & Atmospher Flows, P-4200465 Oporto, Portugal
关键词
Wind energy engineering; Computational fluid dynamics; Turbine micro-siting;
D O I
10.1016/j.jweia.2008.03.012
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The current trend of increasing the electricity production from wind energy has led to the installation of wind farms in areas of greater orographic complexity, raising doubts on the use of simple, linear, mathematical models of the fluid flow equations, so common in the wind energy engineering. The present study shows how conventional techniques, linear models and cup anemometers, can be combined with flow simulation by computational fluid dynamics techniques (nonlinear models) and measurements by sonic anemometers, and discuss their relative merits in the characterisation of the wind over a coastal region-a cliff over the sea. The computational fluid dynamic techniques were particularly useful, providing a global view of the wind flow over the cliff and enabling the identification of separated flow regions. clearly unsuitable for installation of wind turbines. These locations display a pulsating flow, with periods between 1 and 7 min, in agreement with sonic anemometer measurements, and both a turbulence intensity and a gust factor well above the wind turbine design conditions. (C) 2008 Elsevier Ltd. All rights reserved.
引用
收藏
页码:2308 / 2326
页数:19
相关论文
共 31 条
[1]  
[Anonymous], 1989, EUROPEAN WIND ATLAS
[2]  
[Anonymous], BOUNDARY LAYER METEO
[3]   Observations of boundary-layer wind-tunnel flow over isolated ridges of varying steepness and roughness [J].
Ayotte, KW ;
Hughes, DE .
BOUNDARY-LAYER METEOROLOGY, 2004, 112 (03) :525-556
[4]   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
[5]  
BOWEN AJ, 2004, RISOR995EN RIS NAT L
[6]  
Burton T, 2001, Wind Energy Handbook
[7]   Simulation of the Askervein flow.: Part 1:: Reynolds averaged Navier-Stokes equations (k-ε turbulence model) [J].
Castro, FA ;
Palma, JMLM ;
Lopes, AS .
BOUNDARY-LAYER METEOROLOGY, 2003, 107 (03) :501-530
[8]  
CASTRO FA, 2002, VENTOS COMPUTER CODE
[9]  
CASTRO FA, 1997, THESIS U PORTO
[10]   Computer simulation of atmospheric flows over real forests for wind energy resource evaluation [J].
da Costa, J. C. Lopes ;
Castro, F. A. ;
Palma, J. M. L. M. ;
Stuart, P. .
JOURNAL OF WIND ENGINEERING AND INDUSTRIAL AERODYNAMICS, 2006, 94 (08) :603-620