Wave Attenuation by Restored Coral Reef Canopies: Implications for Coastal Protection

IF 3.4 2区 地球科学 Q1 OCEANOGRAPHY
Justin Geldard, Ryan J. Lowe, Marco Ghisalberti, Scott Draper
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Abstract

The significant bottom roughness of coral reefs plays a vital role in mitigating wave-driven hazards along many tropical coastlines. As reef-building corals decline globally, reef restoration has been increasingly used to re-establish reef structure that influences wave dissipation. This study investigated the hydrodynamic processes that govern wave attenuation by restored reef canopies created using a common approach involving modular structures populated with coral colonies, based on the Mars Assisted Reef Restoration System. Three different coral covers were tested in a wave flume under various wave conditions and water depths typical of coral reef flats. We found that wave attenuation increased significantly with coral cover, driven by how specific attributes of the coral geometry controlled in-canopy flows and hydrodynamic forces. Two independent measures of wave energy dissipation generated by the reef were compared: (a) the rate of work done by hydrodynamic forces (calculated from force-velocity timeseries measurements), and (b) the observed wave height attenuation across the reef. These measures agreed well over the different coral covers and wave conditions studied, demonstrating that accurate quantification of in-canopy drag forces and flows enables reliable prediction of wave dissipation. The validated predictive framework was then used to evaluate the effectiveness of coral reef restoration under varying wave conditions and coral covers, showing that well-designed reef canopies can dissipate more than 50% of the incoming wave energy under typical reef flat conditions. These findings offer new insights into the hydrodynamic processes that govern wave attenuation by restored coral reef canopies, highlighting the potential of restoration to mitigate coastal hazard risk.

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珊瑚礁冠层恢复后的波浪衰减:对海岸保护的启示
珊瑚礁显著的底部粗糙度在减轻许多热带海岸线上的海浪灾害中起着至关重要的作用。随着造礁珊瑚在全球范围内的减少,珊瑚礁恢复越来越多地用于重建影响波浪耗散的珊瑚礁结构。本研究调查了水动力过程,该过程通过使用一种常见的方法创建的修复珊瑚礁冠层来控制波浪衰减,该方法涉及珊瑚群落的模块化结构,基于火星辅助珊瑚礁恢复系统。在波浪水槽中测试了三种不同的珊瑚覆盖物,在不同的波浪条件和珊瑚礁滩典型的水深下。我们发现,珊瑚覆盖下的波浪衰减显著增加,这是由珊瑚几何形状的特定属性如何控制冠层内流动和水动力驱动的。比较了由礁石产生的波浪能量耗散的两种独立测量方法:(a)水动力所做功的速率(根据力-速度时间序列测量计算)和(b)观察到的穿过礁石的波高衰减。在不同的珊瑚覆盖和波浪条件下,这些测量结果非常一致,表明准确量化冠层内阻力和流量可以可靠地预测波浪耗散。然后使用验证的预测框架来评估不同波浪条件和珊瑚覆盖下珊瑚礁恢复的有效性,结果表明,在典型的珊瑚礁平坦条件下,设计良好的珊瑚礁冠层可以消散超过50%的入射波能。这些发现为控制恢复的珊瑚礁冠层的波浪衰减的水动力过程提供了新的见解,突出了恢复减轻沿海灾害风险的潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of Geophysical Research-Oceans
Journal of Geophysical Research-Oceans Earth and Planetary Sciences-Oceanography
CiteScore
7.00
自引率
13.90%
发文量
429
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