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TOWARDS TIME AND SPACE EVOLVING EXTREME WIND FIELDS

机译:走向时间和空间的发展极端风田

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Time and space evolving extreme wind fields are needed to produce accurate and realistic extreme hydraulic loads. To fulfill this need, a semi-parametric method based on the theory of max-stable processes has been proposed that can be used to determine the time and space evolving wind fields associated with a given return value of wind speed at a specified reference location. The method uses wind velocity time series over a grid of locations and their location-specific extreme value distributions in order to 'lift' observed extreme events (storms) into yet unobserved and even more extreme events. Because the lifted fields are needed to force hydrodynamic models, they need to be continuous in time and space and to extend over a few days before the peak of the storm in order to allow the spin up of the hydrodynamic models. Thus, even if the original values of the wind fields are not above the threshold used to determine the location-specific extreme value distributions at a given location and instant, they still need to be lifted. This is achieved by augmenting the location-specific extreme value distributions by the empirical distributions of the observations and lifting also the values below the thresholds. Mainly as a consequence of this procedure, the resulting lifted wind fields have low temporal and spatial wind speed gradients away from the peak of the storm. These gradients have raised concerns about the validity of the fields and it has been suggested that the lifting by means of a simple scaling factor may be preferable. To address these concerns, a thorough validation of the lifted fields has been carried out assessing the ability of the lifted fields to reproduce extreme hydraulic conditions. The main recommendation of this study is that a lifting method defined as the combination of the method based on the theory of max-stable processes and a fixed factor method be considered further for the determination of temporally and spatially varying hydraulic loads.
机译:需要采用时间和空间进化极端风田,以产生准确和现实的极端液压载荷。为了满足这种需求,提出了一种基于最大稳定过程理论的半参数方法,其可用于确定与指定参考位置的给定返回值相关联的风场的时间和空间。该方法使用风速时间序列在位置的网格上和其位置特定的极值分布,以便将观察到的极端事件(暴风雨)进入尚未观察,更极端的事件。因为需要提升的田地来强制流体动力学模型,所以它们需要在时间和空间中连续,并且在暴风雨峰前几天延伸,以便允许旋转流体动力学模型。因此,即使风场的原始值不高于用于确定给定位置和瞬间的定位特定的极值分布,它们仍然需要被提升。这是通过通过观察的经验分布增强特定于特定的极值分布来实现的,并且也升降阈值以下的值。主要是由于该程序的结果,所得到的升力风场具有低的时间和空间风速梯度远离风暴的峰值。这些梯度提出了对田地的有效性的担忧,并且已经建议通过简单的缩放因子提升可能是优选的。为了解决这些问题,已经进行了彻底验证了提升的领域,评估了提升的田地再现极端液压条件的能力。本研究的主要推荐是,作为基于最大稳定工艺理论的方法的组合和固定因子方法的组合被认为是为了确定时间和空间不同的液压负载。

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