Measurement of deepwater ocean waves from a subsurface mooring

J. Wood, E. Terray, B. Strong, B. Singh
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引用次数: 9

Abstract

We measured wave height and directional spectra in the open ocean from a subsurface mooring in 1400 meters water depth. Six months of data were recovered successfully at a site south of Australia where high-energy waves (with periods greater than 10 seconds) dominated the spectrum. Nondirectional wave height spectra were estimated from measurements of velocities made with an upward-looking ADCP mounted at the top of the mooring. Additional estimates of the nondirectional spectrum were obtained from a pressure sensor inside the ADCP, and from echo-location of the surface derived from the acoustic backscatter intensities measured by the ADCP. Mooring motion was removed using measurements from a second downward-looking ADCP mounted on the bottom of the float. Wave direction was determined from the velocities measured by the upward-looking ADCP using a variant of single point UVW processing, which permitted heading variations to be compensated continuously. We verified that the resulting horizontal and vertical velocities within the frequency bands containing appreciable wave energy are in quadrature, and that their coherence is close to unity. This paper describes the technique and assesses the quality of the resulting wave spectra and moments.
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从地下系泊处测量深海海浪
我们在1400米水深的水下系泊处测量了公海的波高和方向谱。在澳大利亚南部一个高能量波(周期大于10秒)占主导地位的地点成功恢复了六个月的数据。非定向波高谱是通过安装在系泊顶部的向上ADCP测量的速度来估计的。通过ADCP内部的压力传感器和ADCP测量的声波后向散射强度得出的表面回波定位,可以获得非定向谱的额外估计。通过安装在浮子底部的第二个向下的ADCP测量来消除系泊运动。波浪方向由向上的ADCP测量的速度确定,使用单点UVW处理的一种变体,允许航向变化连续补偿。我们验证了在含有可观波能的频带内得到的水平和垂直速度是正交的,并且它们的相干性接近于一致。本文介绍了该技术,并对所得的波谱和矩的质量进行了评价。
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