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Experimental investigation on the infragravity wave on different reef systems under irregular wave action

机译:不规则波动作用下不同礁石系统对不同珊瑚礁系统的实验研究

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This paper presents the results of a laboratory investigation into the role of infragravity motions in reef hydrodynamics over different reef systems. Laboratory experiments are performed with reef profiles of a platform reef and a fringing reef under irregular wave conditions. The propagation and the distribution of the infragravity wave are different over these two reef systems. Analysis of the measured time histories of water surface elevation shows that shorter sea-swell (SS) waves, longer infragravity (IG) wave and mean water level on the reef fiat are significantly larger in the fringing reef system. The IG wave height is much larger on the fringing reef than that on the platform reef. This marked increase of the IG wave is considered to be due to: (1) the superposition of incoming IG wave and reflected IG wave from shoreline; (2) more violent wave breaking in the surf zone that may enhance the transfer of wave energy from the frequency band of the shorter wave to IG wave. In this experiment, the wave breaking mechanism controls the relationship between IG wave height and water depth.
机译:本文介绍了在不同礁系统中礁石流体动力学中的IntraGravity Motions作用的实验室调查结果。在不规则波条件下,用平台礁的珊瑚礁曲线和流苏礁进行实验室实验。在这两个珊瑚礁系统上的传播和分布不同。水面高度测量时间历史的分析表明,珊瑚礁寿架的较短的海胀(SS)波,延长的Infravavity(IG)波和平均水位在流苏队系统中明显更大。在流苏礁上的IG波高度比平台珊瑚礁更大。 IG波的显着增加是由于:(1)来自海岸线的进料IG波的叠加和反射IG波; (2)在冲浪区中断开冲浪区的更剧烈波,其可以增强从较短波的频带到IG波的波动传递。在该实验中,波断裂机构控制IG波高度和水深之间的关系。

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    《Oceanographic Literature Review》 |2021年第5期|949-949|共1页
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