首页> 外文会议>European Geosciences Union General Assembly >A Diagnostic diagram to understand atmosphere-ocean dynamics in the southern North Sea at high wind speeds
【24h】

A Diagnostic diagram to understand atmosphere-ocean dynamics in the southern North Sea at high wind speeds

机译:诊断图,以了解北海南北大风速度的疗效图

获取原文

摘要

Long time series of offshore meteorological measurements in the lower marine atmospheric boundary layer show dynamical regimes and variability that are forced partly by interaction with the underlying sea surface and partly by the passage of cloud systems overhead. At low wind speeds, the dynamics and stability structure of the surface layer depend mainly on the air-sea temperature difference and measured wind speed at a standard height. The physical processes are mostly understood and quantified through Monin-Obukhov (MO) similarity theory. At high wind speeds, different dynamical regimes become dominant, with breaking waves, sea spray, and organized boundary layer convection cells contributing to observed effects. Data from offshore meteorological monitoring sites typically show different behavior and regime shifts depending on the local winds and synoptic conditions. However, the regular methods to interpret time series through spectral analysis only give a partial view of the dynamics in the atmospheric boundary layer. Wind speed and the air-sea temperature difference are important factors that characterize the dynamics of the lower atmospheric boundary layer, and they provide a dynamic and thermodynamic constraint to frame observed processes, especially at high wind speeds. Early studies of long time series of automated offshore meteorological data recognized the value of the joint probability distribution on axes of wind speed and air-sea temperature difference to summarize large segments of the data. The approach can be extended to probe the marine atmospheric boundary layer conditions that are important for the loading of offshore wind turbines: turbulence intensity and wave conditions. The increasing numbers of offshore meteorological masts that are associated with the offshore wind industry are amenable to a similar approach to understand the main characteristics of the boundary layer. In this case, the diagnostic figure provides a method to 'fingerprint' the atmospheric conditions at an offshore site.
机译:较长的船舶大气边界层中近海气象测量的长时间序列显示了动态的制度和可变性,这些变化部分地被与底层海面的相互作用,部分通过云系统开销。在低风速下,表面层的动态和稳定性结构主要取决于空中海水差,并在标准高度下测量风速。通过MONIN-OBUKHOV(MO)相似性理论大多了解物理过程。在风速高,不同的动态制度变得优势,波浪,海喷雾和有组织的边界层对流细胞有助于观察到的效果。来自海上气象监测网站的数据通常显示不同的行为和方格转移,具体取决于局部风和天气条件。然而,通过光谱分析解释时间序列的规则方法仅在大气边界层中占动态的局部视图。风速和空中海洋温差是表征较低大气边界层的动态的重要因素,它们为帧观察过程提供了一种动态和热力学约束,尤其是在高风速下。关于自动近海气象数据的长时间系列的早期研究认识到风速和空中海洋温差轴上的关节概率分布的价值总结了大量数据。该方法可以扩展到探测海洋大气边界层条件,对海上风力涡轮机的负载很重要:湍流强度和波条件。与海上风力行业相关的越来越多的海上气象桅杆是可以理解边界层主要特征的类似方法。在这种情况下,诊断图提供了在近海站点的“指纹”大气条件的方法。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号