Offshore Wind Energy Analysis of Cyclone Xaver over North Europe

被引:14
作者
Christakos, Konstantinos [1 ]
Cheliotis, Ioannis [2 ]
Varlas, George [3 ,4 ]
Steeneveld, Gert-Jan [2 ]
机构
[1] Uni Res Polytec AS, Sorhauggata 128, N-5527 Haugesund, Norway
[2] Wageningen Univ, Meteorol & Air Qual Sect, NL-6700 AA Wageningen, Netherlands
[3] Harokop Univ Athens, Dept Geog, El Venizelou Str 70, Athens 17671, Greece
[4] Hellen Ctr Marine Res, Inst Marine Biol Resources & Inland Waters, Anavyssos 19013, Attica, Greece
来源
13TH DEEP SEA OFFSHORE WIND R&D CONFERENCE, EERA DEEPWIND'2016 | 2016年 / 94卷
关键词
Wind Power; Offshore Wind Energy; North Sea; Baltic Sea; Cyclone Xaver; Bodil; Sven; PLANETARY BOUNDARY-LAYER; MODEL;
D O I
10.1016/j.egypro.2016.09.187
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
Cyclone Xaver (5 December 2013; North Sea) was an extreme weather event which affected northern Europe, yielding a record of wind power generation. The most striking aspects of this atmospheric phenomenon were the gale-force winds and the upcoming abrupt increase of the wind power over the North Sea. The main objective of the study is the analysis of the impact of Xaver on offshore wind power production. In this way, the WRF numerical model was used to simulate the cyclone in a fine horizontal resolution (5km x 5km). The focus of the simulation is on the extended region of the North Sea and the Baltic Sea. The evaluation of the model outputs against observational data from 3 offshore locations denotes a sufficient agreement (SI approximate to 0.12) and supports a realistic analysis of the wind field. The simulation exposed much higher values for wind speed over the North Sea compared to the neighboring regions during the passage of the cyclone. The wind speed at the 100 m level ranged within 11-25 m/s (rated output wind speed) for 40 hours over the North Sea and 70 hours over the Baltic Sea. On the other hand, the wind speed at 100 m exceeded 25 m/s (cut out wind speed) for ca 30 hours over the North Sea. In addition, comparison of wind power density between two different height levels (100 m and 200 m) is presented. The model results indicate 15% to 20% higher wind power density at 200 m than for 100 m for the largest part of the North Sea. For some regions the difference exceeds 25%. (C) 2016 The Authors. Published by Elsevier Ltd.
引用
收藏
页码:37 / 44
页数:8
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