海岸带风行波分离方法及其在波高预报中的应用

D. S. Vlachos
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引用次数: 0

摘要

研究风产生的波浪最广泛使用和接受的方法是在一个点上检查光谱。这种方法主要基于这样的假设,即记录的地表高程、压力或速度的时间序列是小振幅振荡的线性叠加的结果,而不管它们的传播方向如何。本文利用浮标的垂直加速度和水平加速度来计算海岸带的定向波谱。所使用的方法是一种参数方法,它包含两个在不同方向上传播的波。由此产生的入射波分裂成两个主要方向,用自适应神经网络进行24小时波高预测。(©2005 WILEY-VCH Verlag GmbH &KGaA公司,Weinheim)
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Method for the Separation of Wind Generated and Traveling Waves in Coastal Zones and its Use in Wave Height Prediction

The most widely used and accepted method of studying wind generated waves is an examination of the spectra at a single point. This approach is based mostly on the assumption that recorded time series of the surface elevation, pressure or velocities are the results of linear superposition of small amplitude oscillations regardless of their directions of propagation. In this work, the vertical and horizontal accelerations of a floating buoy have been used in order to calculate the directional wave spectra in coastal zones. The method used is a parametric one, which incorporates two waves propagating in different directions. The resulting splitting of the incoming waves into two main directions is used for 24-hours wave height prediction with an adaptive neural network. (© 2005 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim)

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