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首页> 外文期刊>Acta Oceanologica Sinica >Infragravity waves with internal wave characteristics in the south of the Bohai Sea of China
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Infragravity waves with internal wave characteristics in the south of the Bohai Sea of China

机译:中国渤海南部具有内波特征的次重力波

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摘要

The measurements by using ADCP (500 KH) and CTD were made during August 2000 in the south (37°5′N, 120°5′E) of the Bohai Sea, where the water depth was about 16.5 m. The data of horizontal velocity with sampling interval of 2 min in 7 layers were obtained. The power spectrum analysis of these data indicates that there are very energetic infragravity waves with a period of about 6 min. The coherence spectrum analysis and the analysis of temporal variation of shear show that these infragravity waves are mainly the free wave model (properties of edge waves), in the meantime they possess some characteristics of internal waves, which are likely due to the distinctive marine environment in this area. It is speculated on that the instability processes (chiefly shear instability) of sheared stratified tidal flow owing to the effect of sea-floor slope in the coastal area might be the main mechanism generating these infragravity waves.
机译:利用ADCP(500 KH)和CTD进行的测量是在2000年8月于渤海南部(37°5′N,120°5′E)进行的,水深约为16.5 m。获得了7层采样间隔为2 min的水平速度数据。这些数据的功率谱分析表明,存在非常高能的次重力波,周期约为6分钟。相干谱分析和剪力随时间变化的分析表明,这些次重力波主要是自由波模型(边缘波的性质),同时具有内部波的一些特征,这可能是由于独特的海洋环境在这方面。据推测,由于沿海海底斜坡的影响,剪切的分层潮汐流的失稳过程(主要是剪切失稳)可能是产生这些引力波的主要机理。

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