Verification of the Reliability of Offshore Wind Resource Prediction Using an Atmosphere-Ocean Coupled Model

被引:0
|
作者
Kang, Minhyeop [1 ]
Ko, Kyungnam [2 ]
Kim, Minyeong [3 ]
机构
[1] Jeju Natl Univ, Multidisciplinary Grad Sch Program Wind Energy, 102 Jejudaehakro, Jeju 63243, South Korea
[2] Jeju Natl Univ, Fac Wind Energy Engn, 102 Jejudaehakro, Jeju 63243, South Korea
[3] Natl Typhoon Ctr, Jeju 63614, South Korea
关键词
offshore wind resource; wind power production; weather research forecasting; ocean mixed layer; sea surface temperature; prediction model; TROPICAL CYCLONE; SIMULATION; SYSTEM; WRF;
D O I
10.3390/en13010254
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
An atmosphere-ocean coupled model is proposed as an optimal numerical prediction method for the offshore wind resource. Meteorological prediction models are mainly used for wind speed prediction, with active studies using atmospheric models. Seawater mixing occurring at sea due to solar radiation and wind intensity can significantly change the sea surface temperature (SST), an important variable for predicting wind resources and energy production, considering its wind effect, within a short time. This study used the weather research forecasting and ocean mixed layer (WRF-OML) model, an atmosphere-ocean coupled model, to reflect time-dependent SST and sea surface fluxes. Results are compared with those of the WRF model, another atmospheric model, and verified through comparison with observation data of a meteorological mast (met-mast) at sea. At a height of 94 m, the wind speed predicted had a bias and root mean square error of 1.09 m/s and 2.88 m/s for the WRF model, and -0.07 m/s and 2.45 m/s for the WRF-OML model, respectively. Thus, the WRF-OML model has a higher reliability. In comparing to the met-mast observation data, the annual energy production (AEP) estimation based on the predicted wind speed showed an overestimation of 15.3% and underestimation of 5.9% from the WRF and WRF-OML models, respectively.
引用
收藏
页数:15
相关论文
共 50 条
  • [31] A coupled atmosphere-ocean model applied to the simulation of mediterranean lows and hurricanes
    Lionello, P
    Malguzzi, P
    24TH CONFERENCE ON HURRICANES AND TROPICAL METEOROLOGY/10TH CONFERENCE ON INTERACTION OF THE SEA AND ATMOSPHERE, 2000, : A35 - A36
  • [32] A model of decadal middle-latitude atmosphere-ocean coupled modes
    Goodman, J
    Marshall, J
    JOURNAL OF CLIMATE, 1999, 12 (02) : 621 - 641
  • [33] Singularly Perturbed Solution of Coupled Model in Atmosphere-ocean for Global Climate
    MO Jiaqi1
    2. Division of Computational Science
    3. Huzhou Teachers College
    4. LASG
    5. Chinese Academy of Meteorological Sciences
    Chinese Geographical Science, 2008, (02) : 193 - 196
  • [34] Application of the Ensemble Kalman Filter and Smoother to a Coupled Atmosphere-ocean Model
    Ueno, Genta
    Higuchi, Tomoyuki
    Kagimoto, Takashi
    Hirose, Naoki
    SOLA, 2007, 3 : 5 - 8
  • [35] Climate simulations for 1951-2050 with a coupled atmosphere-ocean model
    Sun, S
    Hansen, JE
    JOURNAL OF CLIMATE, 2003, 16 (17) : 2807 - 2826
  • [36] Dansgaard-Oeschger oscillations in a coupled atmosphere-ocean climate model
    Sakai, K
    Peltier, WR
    JOURNAL OF CLIMATE, 1997, 10 (05) : 949 - 970
  • [37] Evaluation of ice-albedo feedback by a coupled atmosphere-ocean model
    Chu, PC
    Chen, YC
    Lu, SH
    NINTH CONFERENCE ON INTERACTION OF THE SEA AND ATMOSPHERE, 1998, : 142 - 145
  • [38] A simple atmosphere-ocean coupled model for the north pacific interdecadal variability
    An, SI
    12TH SYMPOSIUM ON GLOBAL CHANGE AND CLIMATE VARIATIONS, 2001, : 285 - 288
  • [39] INSTABILITY AND PREDICTABILITY IN COUPLED ATMOSPHERE-OCEAN MODELS
    BATTISTI, DS
    HIRST, AC
    SARACHIK, ES
    PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1989, 329 (1604): : 237 - 247
  • [40] CLIMATE VARIABILITY IN A LOW-ORDER COUPLED ATMOSPHERE-OCEAN MODEL
    ROEBBER, PJ
    TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 1995, 47 (04): : 473 - 494