CFD modelling of wave damping over a fringing reef in the Colombian Caribbean

被引:0
作者
Juan D. Osorio-Cano
Juan C. Alcérreca-Huerta
Andrés F. Osorio
Hocine Oumeraci
机构
[1] OCEANICOS,Research Group in Oceanography and Coastal Engineering
[2] Universidad Nacional de Colombia at Medellín,Department of Geosciences and Environment
[3] CONACYT-ECOSUR,Department of Systematics and Aquatic Ecology at El Colegio de la Frontera Sur
[4] Technische Universität Braunschweig,Leichtweiß Institute for Hydraulic Engineering and Water Resources
来源
Coral Reefs | 2018年 / 37卷
关键词
Wave damping; Reef roughness; CFD modelling; Fringing reefs;
D O I
暂无
中图分类号
学科分类号
摘要
The understanding of physical processes over submerged reefs represents an important ongoing research topic when considering wave energy dissipation and coastal protection that these environments provide. Detailed analyses are required to assess wave damping based on the contribution of reef roughness and wave breaking. For this purpose, the CFD (computational fluid dynamics) toolbox OpenFOAM® is applied to simulate the wave energy dissipation process over reefs with explicit accounting for the complexities of coral shape instead of commonly applied parameterized approaches for bottom roughness and wave breaking. Model validation was performed through comparison with field measurements over a reef profile of Tesoro Island in the Colombian Caribbean. Quantitative analysis of wave damping caused by wave breaking and reef roughness was conducted for (1) moderate and extreme wave conditions, (2) smooth and rough seabed configurations and (3) changes in the water depth over the reef crest. Wave height attenuation is found to vary along the reef profile reaching differences of up to 55% between smooth and rough reef surface scenarios, particularly for moderate wave conditions. Wave breaking, high turbulent flows and detachment of undertow currents are among the reef roughness effects on hydrodynamics. The fore-reef terrace and the reef crest are identified as the most critical zones where dissipation takes place. Wave breaking from rough seabeds provides a global wave attenuation of 75.4–94.8%, with the reef roughness alone accounting for ~ 4–14%. Under extreme wave height scenarios, the wave damping from reef roughness is not significant. Further predictions regarding roughness effects on the reef hydrodynamics, wave set-up and undertow currents for moderate and extreme wave climate conditions are also shown. Directions for future research using CFD are presented to address limitations that arise from the limited span-wise domain in our approach that prevents development of large lateral coherent structures.
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页码:1093 / 1108
页数:15
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共 180 条
[1]  
Andrade CA(2013)Coastal flooding hazard related to swell events in Cartagena de Indias, Colombia J Coast Res 290 1126-1136
[2]  
Thomas YF(2014)Impact of sea-level rise and coral mortality on the wave dynamics and wave forces on barrier reefs Mar Pollut Bull 83 155-164
[3]  
Lerma AN(2016)Occurrence of energetic extreme oceanic events in the Colombian Caribbean coasts and some approaches to assess their impact on ecosystems J Mar Syst 164 85-100
[4]  
Durand P(2016)Wave Setup over a Fringing Reef with Large Bottom Roughness J Phys Oceanogr 46 2317-2333
[5]  
Anselme B(2014)Numerical investigation of wave–structure interaction using OpenFOAM Ocean Eng 88 91-109
[6]  
Baldock T(2008)Field verification of a computational fluid dynamics model for wave transformation and breaking in the surf zone J Waterw Port, Coastal, Ocean Eng 134 71-80
[7]  
Golshani A(2004)Mass-transfer limitation of nutrient uptake by a wave-dominated reef flat community Limonology Oceanogr 49 1820-1831
[8]  
Callaghan DP(2014)Revisiting study on Boussinesq modeling of wave transformation over various reef profiles Water Sci Eng 7 306-318
[9]  
Saunders MI(2014)The effectiveness of coral reefs for coastal hazard risk reduction and adaptation Nat Commun 5 3794-29
[10]  
Mumby PJ(1977)Episodic circulation and exchange in a wave-driven coral reef and lagoon system The influence of wave exposure on the ecological zonation of Caribbean coral reefs. 1 23-2694