A WRF Ensemble for Improved Wind Speed Forecasts at Turbine Height

被引:80
作者
Deppe, Adam J. [1 ]
Gallus, William A., Jr. [1 ]
Takle, Eugene S. [1 ,2 ]
机构
[1] Iowa State Univ, Dept Geol & Atmospher Sci, Ames, IA USA
[2] Iowa State Univ, Dept Agron, Ames, IA USA
基金
美国国家科学基金会;
关键词
ATMOSPHERIC BOUNDARY-LAYER; MESOSCALE METEOROLOGICAL MODEL; NONLOCAL CLOSURE-MODEL; LAND-SURFACE MODEL; VERTICAL DIFFUSION; COMPLEX TERRAIN; PART I; PERTURBATIONS; PRECIPITATION; CONVECTION;
D O I
10.1175/WAF-D-11-00112.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The Weather Research and Forecasting Model (WEE) with 10-km horizontal grid spacing was used to explore improvements in wind speed forecasts at a typical wind turbine hub height (80 m). An ensemble consisting of WRF model simulations with different planetary boundary layer (PBL) schemes showed little spread among the individual ensemble members for forecasting wind speed. A second configuration using three random perturbations of the Global Forecast System model produced more spread in the wind speed forecasts, but the ensemble mean possessed a higher mean absolute error (MAE). A third ensemble of different initialization times showed larger model spread, but model MAE was not compromised. In addition, postprocessing techniques such as training of the model for the day 2 forecast based on day 1 results and bias correction based on observed wind direction are examined. Ramp event forecasting was also explored. An event was considered to be a ramp event if the change in wind power was 50% or more of total capacity in either 4 or 2 h or less. This was approximated using a typical wind turbine power curve such that any wind speed increase or decrease of more than 3 m s(-1) within the 6-12 m s(-1) window (where power production varies greatly) in 4 h or less would be considered a ramp. Model MAE, climatology of ramp events, and causes were examined. All PBL schemes examined predicted fewer ramp events compared to the observations, and model forecasts for ramps in general were poor.
引用
收藏
页码:212 / 228
页数:17
相关论文
共 61 条
[1]  
[Anonymous], 2007, PARAMETERIZATION SCH
[2]   A simple temporal and spatial analysis of flow in complex terrain in the context of wind energy modelling [J].
Ayotte, KW ;
Davy, RJ ;
Coppin, PA .
BOUNDARY-LAYER METEOROLOGY, 2001, 98 (02) :275-295
[3]  
Bélair S, 1999, J APPL METEOROL, V38, P1499, DOI 10.1175/1520-0450(1999)038<1499:AEOLVN>2.0.CO
[4]  
2
[5]  
Bradford K. T., 2010, 9 ANN STUD C ATL GA, pS30
[6]  
BRIGGS WM, 2004, 17 C PROB STAT ATM S
[7]  
DALCHER A, 1988, MON WEATHER REV, V116, P402, DOI 10.1175/1520-0493(1988)116<0402:MRLAF>2.0.CO
[8]  
2
[9]  
Department of Energy, 2010, DOEEIA0348
[10]  
Department of Energy, 2008, DOEGO1020082567 EN E