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DERIVATION OF WATER PARTICLE KINEMATICS IN THE NEAR SURFACE ZONE BY THE EFFECTIVE WATER DEPTH PROCEDURE

机译:用有效水深过程推导水粒子运动学在近地表中的水粒子运动学

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Linear Random Wave Theory (LRWT) is frequently used to simulate water particle kinematics at different nodes of an offshore structure from a reference surface elevation record. However, it is well known that LRWT leads to water particle kinematics with exaggerated high-frequency components in the vicinity of mean water level (MWL). To avoid this problem, empirical techniques (such as Wheeler & vertical stretching methods) are frequently used to provide a more realistic representation of the wave kinematics in the near surface zone. In this paper, a modified version of LRWT, based on the derivation of an effective water depth, is introduced. The proposed technique leads to predicted kinematics (in the near surface zone) which lie between corresponding values from the Wheeler and the vertical stretching methods. Furthermore, it does not suffer from exaggerated high-frequency components in the near surface zone.
机译:线性随机波理论(LRWT)经常用于模拟从参考表面仰角记录的离岸结构的不同节点的水粒子运动学。然而,众所周知,LRWT导致水粒子运动学,在平均水位(MWL)附近具有夸大的高频分量。为了避免这个问题,经常使用经验技术(例如轮车和垂直拉伸方法)来提供近地表区域中的波浪运动学的更现实的表示。本文介绍了基于有效水深的推导的改进版本的LRWT版本。所提出的技术导致预测的运动学(在近表面区域中),其位于轮式器和垂直拉伸方法之间的相应值之间。此外,它不会遭受近近表面区的夸张的高频分量。

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