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OBSERVING LARGE WAVES USING BOTTOM-MOUNTED PRESSURE AND CURRENT METERS

机译:使用底部安装压力和电流表观察大浪

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This paper compares two different methods used for processing bottom PUV data to estimate the kinematics and summary statistics of large surface waves. The first method is based on linear wave theory (LWT). The second method is based on a new approach called the Directional Hybrid Wave Method (DHWM). The PUV data featured in this paper was measured 6 km offshore the mouth of the Columbia River, during fall-winter 1999, in a nominal water depth of 35 meters. This paper examined wave-wave interaction and wave-current interaction to assess the reliability of using linear wave theory and to enhance the utility of bottom PUV data in a water depth of 35 meters. Results of applying LWT and DHWM on PUV data were compared to wave-rider data, obtained from a NOAA buoy 14 km directly offshore from the point of PUV measurement. Results indicate that a current-induced Doppler effect can bias wave estimation by 2-10% and that LWT may have under estimated wave height by 20% during storms. The DHWM appears to offer much improvement over LWT and requires further investigation and verification.
机译:本文将用于处理底部PUV数据的两种不同方法进行比较,以估算大表面波的运动学和汇总统计。第一种方法基于线性波理论(LWT)。第二种方法基于一种称为定向混合波方法(DHWM)的新方法。本文提出的PUV数据在1999年秋季冬季,哥伦比亚河口6公里处以6公里,标称水深35米。本文检查了波浪相互作用和波浪电流相互作用,以评估使用线性波理论的可靠性,并增强水深35米的底部PUV数据的效用。将LWT和DHWM应用于PUV数据的结果与波浪骑行者数据进行比较,从PUV测量点直接从NOAA浮标获得14km。结果表明,电流诱导的多普勒效应可以在风暴期间偏置波估计2-10%,并且LWT在估计波高度下可能在估计波高度下降20%。 DHWM似乎提供了更好的LWT改善,需要进一步调查和验证。

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