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Space-Time Extremes in Short-Crested Storm Seas

机译:短波风暴海中的时空极端

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摘要

This study develops a stochastic approach to model short-crested stormy seas as random fields both in space and time. Defining a space-time extreme as the largest surface displacement over a given sea surface area during a storm, associated statistical properties are derived by means of the theory of Euler characteristics of random excursion sets in combination with the Equivalent Power Storm model. As a result, an analytical solution for the return period of space-time extremes is given. Subsequently, the relative validity of the new model and its predictions are explored by analyzing wave data retrieved from NOAA buoy 42003, located in the eastern part of the Gulf of Mexico, offshore Naples, Florida. The results indicate that, as the storm area increases under short-crested wave conditions, space-time extremes noticeably exceed the significant wave height of the most probable sea state in which they likely occur and that they also do not violate Stokes-Miche-type upper limits on wave heights.
机译:这项研究开发了一种随机方法,可以将短波涛汹涌的海域建模为时空随机场。将时空极限定义为暴风雨期间给定海域表面上最大的表面位移,借助随机偏移集的欧拉特征理论和等效功率暴风雨模型相结合,得出相关的统计属性。结果,给出了时空极限返回期的解析解。随后,通过分析从位于佛罗里达州那不勒斯近海墨西哥湾东部的NOAA浮标42003取回的海浪数据,探索了新模型及其预测的相对有效性。结果表明,随着风暴面积在短波波浪条件下增加,时空极端明显超过了可能发生海浪的最可能海况的显着波高,而且它们也没有违反斯托克斯-米歇型波浪高度的上限。

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  • 来源
    《Journal of Physical Oceanography 》 |2012年第9期| p.1601-1615| 共15页
  • 作者

    Francesco Fedele;

  • 作者单位

    School of Civil and Environmental Engineering, and School of Electrical and Computer Engineering, Georgia Institute of Technology, Atlanta, Georgia;

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  • 正文语种 eng
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