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An observational, stability-based estimate of 80 m wind speed offshore of North Carolina - seasonal patterns

机译:基于观测的基于稳定性的北卡罗莱纳州海上80 m风速估计-季节性模式

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Winds at 80 m elevation have been estimated with a stability-based height adjustment scheme to study the feasibility of utility-scale wind energy offshore of North Carolina. Data sources are the daily ASCAT 10 m wind field as measured by the METOP-A satellite, the North American Regional Reanalysis (NARR) estimates of near-surface atmospheric temperature, pressure and humidity and the National Climate Data Center's optimally-interpolated Advanced Very High Resolution Radiometer (AVHRR-OI) sea surface temperature (SST). The study focuses on the 2008???2012 time period. The COARE V3.0 algorithm is used to provide the stability-based height adjustment scheme. Data from six buoys have been used to establish validity of the remotely-sensed and modeled fields. A variety of results were produced, including long-term average wind speeds, wind power density and capacity factor at hub height, and a monthly climatology of these quantities. In this note the focus is on seasonal variations utilizing the monthly climatologies. Using the climatologies the largest differences between the neutral and stability-based schemes occur in winter and spring when and where stable atmospheric conditions are most common. There is a significant difference in the annual variation of atmospheric stability north and south of Cape Hatteras. Only the inner shelf region is prone to stable conditions during winter and spring south of Cape Hatteras, whereas the full width of the shelf is prone to stable conditions from fall into early summer north of Cape Hatteras. Where stable conditions occur the stability-based 80 m wind speeds are 2???3 m/s greater than 80 m neutral wind speeds, and where unstable conditions occur the stability-based 80 m wind speeds are 0.5???1 m/s less than the 80 m neutral wind speeds. The result is a pattern in the 80 m stability-based winds with notably greater speeds near the coastline than expected from a neutral height adjustment.
机译:已使用基于稳定性的高度调整方案估算了80 m高处的风,以研究北卡罗来纳州海上大规模使用风能的可行性。数据来源是通过METOP-A卫星测得的每日ASCAT 10 m风场,北美地区再分析(NARR)对近地表大气温度,压力和湿度的估计以及美国国家气候数据中心的最佳内插Advanced Very High分辨率辐射计(AVHRR-OI)海面温度(SST)。该研究的重点是2008年至2012年。 COARE V3.0算法用于提供基于稳定性的高度调整方案。来自六个浮标的数据已用于建立遥感和建模场的有效性。产生了各种结果,包括长期平均风速,风能密度和轮毂高度处的容量因子,以及这些数量的每月气候。在本文中,重点是利用月度气候的季节性变化。使用气候学,中性和基于稳定性的方案之间的最大差异出现在冬季和春季,那时和最稳定的大气条件最为普遍。哈特拉斯角北部和南部的大气稳定性年变化存在显着差异。在哈特拉斯角以南的冬季和春季,只有内部架子区域易于保持稳定状态,而从秋天到哈特拉斯角以北的初夏,整个架子的宽度都易于保持稳定状态。在出现稳定条件的情况下,基于稳定性的80 m风速比80 m中性风速大2到3 m / s,在出现不稳定条件的情况下,基于稳定性的80 m风速为0.5 -1 m / s。小于80 m的中性风速。结果是在基于80 m的稳定风中,海岸线附近的风速明显高于中性高度调整所预期的风向。

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