Implementation issues in 3D wind flow predictions over complex terrain

被引:24
作者
Prospathopoulos, John [1 ]
Voutsinas, Spyros G. [1 ]
机构
[1] NTUA, Dept Fluids, Sch Mech Engn, Athens 15773, Greece
来源
JOURNAL OF SOLAR ENERGY ENGINEERING-TRANSACTIONS OF THE ASME | 2006年 / 128卷 / 04期
关键词
flow over complex terrain; micro-siting; wind energy;
D O I
10.1115/1.2346702
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
Practical aspects concerning the use of 3D Navier-Stokes solvers as prediction tools for micro-siting of wind energy installations are considered. Micro-siting is an important issue for a successful application of wind energy in sites of complex terrain. There is a constantly increasing interest in using mean wind flow predictions based on Reynolds averaged Navier-Stokes (RANS) solvers in order to minimize the number of required field measurements. In this connection, certain numerical aspects, such as the extent of the numerical flow domain, the choice of the appropriate inflow boundary conditions, and the grid resolution, can decisively affect the quality of the predictions. In the present paper these aspects are analyzed with reference to the Askervein hill data base of full scale measurements. The objective of the work is to provide guidelines with respect to the definition of appropriate boundary conditions and the construction of an adequate and effective computational grid when a RANS solver is implemented. In particular it is concluded that (a) the ground roughness affects the predictions significantly, (b) the computational domain should have an extent permitting the full development of the flow before entering the region of interest, and (c) the quality of the predictions at the local altitude maxima depends on the grid density in the main flow direction.
引用
收藏
页码:539 / 553
页数:15
相关论文
共 36 条
[1]  
[Anonymous], WIND ENG
[2]  
[Anonymous], WIND ENERGY
[3]   Flow and dispersion over hills: Comparison between numerical predictions and experimental data [J].
Apsley, DD ;
Castro, IP .
JOURNAL OF WIND ENGINEERING AND INDUSTRIAL AERODYNAMICS, 1997, 67-8 :375-386
[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]  
Bergeles G., 1996, P EUWEC 96 GOT SWED
[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]  
DUYNKERKE PG, 1988, J ATMOS SCI, V45, P865, DOI 10.1175/1520-0469(1988)045<0865:AOTTCM>2.0.CO
[9]  
2
[10]  
ENDLICH RM, 1982, J APPL METEOROL, V21, P1441, DOI 10.1175/1520-0450(1982)021<1441:ADMFEW>2.0.CO