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Quarter-Century Offshore Winds from SSM/I and WRF in the North Sea and South China Sea

机译:来自ssm / I的四分之一世纪海上风和北海和南海的WRF

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摘要

We study the wind climate and its long-term variability in the North Sea and South China Sea, areas relevant for offshore wind energy development, using satellite-based wind data, because very few reliable long-term in-situ sea surface wind observations are available. The Special Sensor Microwave Imager (SSM/I) ocean winds extrapolated from 10 m to 100 m using the Charnock relationship and the logarithmic profile method are compared to Weather Research and Forecasting (WRF) model results in both seas and to in-situ observations in the North Sea. The mean wind speed from SSM/I and WRF differ only by 0.1 m/s at Fino1 in the North Sea, while west of Hainan in the South China Sea the difference is 1.0 m/s. Linear regression between SSM/I and WRF winds at 100 m show correlation coefficients squared of 0.75 and 0.67, standard deviation of 1.67 m/s and 1.41 m/s, and mean difference of −0.12 m/s and 0.83 m/s for Fino1 and Hainan, respectively. The WRF-derived winds overestimate the values in the South China Sea. The inter-annual wind speed variability is estimated as 4.6% and 4.4% based on SSM/I at Fino1 and Hainan, respectively. We find significant changes in the seasonal wind pattern at Fino1 with springtime winds arriving one month earlier from 1988 to 2013 and higher winds in June; no yearly trend in wind speed is observed in the two seas.
机译:我们使用基于卫星的风数据研究北海和南海(与海上风能开发相关的地区)的风气候及其长期变化,因为很少有可靠的长期就地海面风观测可用。使用夏洛克关系和对数剖面法将特殊传感器微波成像仪(SSM / I)从10 m到100 m外推的海风与天气研究和预报(WRF)模型结果进行了比较,并与海中的实地观测进行了比较北海。来自SSM / I和WRF的平均风速在北海的Fino1仅相差0.1 m / s,而在南海的海南西部则相差1.0 m / s。 SSM / I和WRF风在100 m处的线性回归显示相关系数的平方分别为0.75和0.67,标准偏差为1.67 m / s和1.41 m / s,Fino1的平均差为-0.12 m / s和0.83 m / s和海南。源自WRF的风高估了南中国海的数值。根据Fino1和海南的SSM / I,年际风速变化估计分别为4.6%和4.4%。我们发现Fino1的季节性风向发生了重大变化,春季风从1988年到2013年提前了一个月到达,六月风向更高。在两个海洋中,没有观察到风速的年度趋势。

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