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首页> 外文期刊>Geophysical Research Letters >Power spectra of infragravity waves in a deep ocean
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Power spectra of infragravity waves in a deep ocean

机译:深海次重力波的功率谱

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Infragravity waves (IGWs) play an important role in coupling wave processes in the ocean, ice shelves, atmosphere, and the solid Earth. Due to the paucity of experimental data, little quantitative information is available about power spectra of IGWs away from the shore. Here we use continuous, yearlong records of pressure at 28 locations on the seafloor off New Zealand's South Island to investigate spectral and spatial distribution of IGW energy. Dimensional analysis of diffuse IGW fields reveals universal properties of the power spectra observed at different water depths and leads to a simple, predictive model of the IGW spectra. While sources of IGWs off New Zealand are found to have a flat power spectrum, the IGW energy density has a pronounced dependence on frequency and local water depth as a result of the interaction of the waves with varying bathymetry.
机译:超重力波(IGW)在海洋,冰架,大气层和固体地球中的耦合波过程中起着重要作用。由于缺乏实验数据,关于离岸的IGW功率谱的定量信息很少。在这里,我们使用连续的,为期一年的连续记录来记录新西兰南岛外海底28个位置的压力,以研究IGW能量的光谱和空间分布。弥散的IGW场的尺寸分析揭示了在不同水深处观察到的功率谱的普遍性质,并导致了IGW谱的简单,可预测的模型。尽管发现新西兰以外的IGW的源具有平坦的功率谱,但是由于波浪与变化的测深法之间的相互作用,IGW的能量密度对频率和当地水深具有明显的依赖性。

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