首页> 外文会议>International conference on port and ocean engineering under arctic conditions >STATISTICALLY BASED METHOD OF REPRESENTING ICE LOADS SIGNAL AS A SUM OF SEVERAL UNCORRELATED AND STATIONARY PROCESSES
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STATISTICALLY BASED METHOD OF REPRESENTING ICE LOADS SIGNAL AS A SUM OF SEVERAL UNCORRELATED AND STATIONARY PROCESSES

机译:基于统计的冰负荷信号表示方法,用于多个不相关的平稳过程

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In the paper the method of signal processing is offered. It was developed specially for processing of ice loads observations made in ice basin. The proposed method includes numerical search of the signal oscillatory components parameters by minimization of these components covariance and model discrepancy variance. In the method the clustering procedure is used for the final frequencies estimation. Uncorrelated random processes which parameters are estimated this way appear to be useful to describe the greater part of initial signal variance. The components of particular interest are stationary stochastic processes with determined frequency and random phase. The discrepancy for such model is in general a non-stationary process, but with variance much less then variance of initial signal. The characteristic of this method is that it uses not large time intervals, for example 1 second. The selection of time interval length depends on existing noise characteristics. In the paper the offered method is applied to explain the ice loads measurements that were got in experiments with tanker and ice-breaker hulls in ice basin. In the last section of the paper some statistics values for estimated parameters and ice load signal discrepancy are given. Comparing to spectral investigation, this method do not use necessarily orthogonal trigonometric functions to describe oscillatory components. But at the same time numerically found frequencies conform to the general spectral investigation results.
机译:本文提供了信号处理的方法。它是专门为处理冰盆中的冰负荷观测而开发的。所提出的方法包括通过使这些分量的协方差和模型差异方差最小来对信号振荡分量参数进行数值搜索。在该方法中,将聚类过程用于最终频率估计。以这种方式估计参数的不相关随机过程似乎对描述初始信号方差的较大部分很有用。特别感兴趣的组件是具有确定的频率和随机相位的平稳随机过程。这种模型的差异通常是一个非平稳过程,但是方差远小于初始信号的方差。该方法的特点是它使用的时间间隔不大,例如1秒。时间间隔长度的选择取决于现有的噪声特性。在本文中,所提供的方法用于解释在冰盆中的油轮和破冰船体实验中获得的冰负荷测量结果。在本文的最后一部分中,给出了一些估计参数和冰负荷信号差异的统计值。与频谱研究相比,该方法不必使用正交三角函数来描述振荡分量。但同时在数值上发现的频率符合一般频谱研究的结果。

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