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A Numerical Study of Wave-Driven Mean Flows and Setup Dynamics at a Coral Reef-Lagoon System

机译:珊瑚礁泻湖系统波驱动均线流动和设置动力学的数值研究

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摘要

Two-dimensional mean wave-driven flow and setup dynamics were investigated at a reef-lagoon system at Ningaloo Reef, Western Australia, using the numerical wave-flow model, SWASH. Phase-resolved numerical simulations of the wave and flow fields, validated with highly detailed field observations (including >10 sensors through the energetic surf zone), were used to quantify the main mechanisms that govern the mean momentum balances and resulting mean current and setup patterns, with particular attention to the role of nonlinear wave shapes. Momentum balances from the phase-resolved model indicated that onshore flows near the reef crest were primarily driven by the wave force (dominated by radiation stress gradients) due to intense breaking, whereas the flow over the reef flat and inside the lagoon and channels was primarily driven by a pressure gradient. Wave setup inside the lagoon was primarily controlled by the wave force and bottom stress. The bottom stress reduced the setup on the reef flat and inside the lagoon. Excluding the bottom stress contribution in the setup balance resulted in an over prediction of the wave-setup inside the lagoon by up to 200-370%. The bottom stress was found to be caused by the combined presence of onshore directed wave-driven currents and (nonlinear) waves. Exclusion of the bottom stress contribution from nonlinear wave shapes led to an over prediction of the setup inside the lagoon by approximately 20-40%. The inclusion of the nonlinear wave shape contribution to the bottom stress term was found to be particularly relevant in reef regions that experience a net onshore mass flux over the reef crest.
机译:使用数值波动模型,旋转速度,在南澳大利亚宁大厦礁石的礁泻湖系统中研究了二维平均波动流量和设置动态。使用高度详细的现场观察(包括通过能量冲浪区的> 10个传感器)验证的波和流场的相位分辨数值模拟,用于量化控制平均动量余额的主要机制,并产生平均电流和设置模式,特别注意非线性波形的作用。来自相位分辨模型的动量余额表明,由于强烈的断裂,珊瑚礁附近的陆上流动主要由波力(由辐射应力梯度主导)驱动,而礁石和泻湖和渠道内的礁石上的流量主要是由压力梯度驱动。泻湖内的波形设置主要由波力和底部应力控制。底部压力降低了礁石和泻湖内部的礁石的设置。除了设置余量中的底部应力贡献,导致在泻湖内的波浪设置上的过度预测到200-370%。发现底部应力是由陆上定向波驱动电流的组合存在和(非线性)波引起的。从非线性波形中排除底部应力贡献导致泻湖内部的设置约20-40%。发现非线性波形对底部应力术语的贡献在珊瑚礁区域中特别相关,在珊瑚礁上经历欧式血管磁通量的珊瑚礁区域。

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  • 来源
    《Oceanographic Literature Review 》 |2021年第6期| 1190-1190| 共1页
  • 作者单位

    Environmental Fluid Mechanics Section Faculty of Civil Engineering and Geosciences Delft University of Technology Delft Netherlands;

    Environmental Fluid Mechanics Section Faculty of Civil Engineering and Geosciences Delft University of Technology Delft Netherlands;

    Environmental Fluid Mechanics Section Faculty of Civil Engineering and Geosciences Delft University of Technology Delft Netherlands;

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