Turbulence and Coral Reefs

被引:38
|
作者
Davis, Kristen A. [1 ,2 ]
Pawlak, Geno [3 ]
Monismith, Stephen G. [4 ]
机构
[1] Univ Calif Irvine, Dept Civil & Environm Engn, Irvine, CA 92697 USA
[2] Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USA
[3] Univ Calif San Diego, Dept Mech & Aerosp Engn, La Jolla, CA 92093 USA
[4] Stanford Univ, Dept Civil & Environm Engn, Stanford, CA 94305 USA
来源
基金
美国国家科学基金会;
关键词
turbulence; coral reefs; rough boundary layers; mass transfer; canopy flow; waves; BOUNDARY-LAYER TURBULENCE; MASS-TRANSFER; WATER-FLOW; OSCILLATORY FLOW; NUTRIENT-UPTAKE; COHERENT STRUCTURES; MADRACIS-MIRABILIS; VERTICAL STRUCTURE; SURFACE-ROUGHNESS; REYNOLDS STRESS;
D O I
10.1146/annurev-marine-042120-071823
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The interaction of coral reefs, both chemically and physically, with the surrounding seawater is governed, at the smallest scales, by turbulence. Here, we review recent progress in understanding turbulence in the unique setting of coral reefs-how it influences flow and the exchange of mass and momentum both above and within the complex geometry of coral reef canopies. Flow above reefs diverges from canonical rough boundary layers due to their large and highly heterogeneous roughness and the influence of surface waves. Within coral canopies, turbulence is dominated by large coherent structures that transport momentum both into and away from the canopy, but it is also generated at smaller scales as flow is forced to move around branches or blades, creating wakes. Future work interpreting reef-related observations or numerical models should carefully consider the influence that spatial variation has on momentum and scalar flux.
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页码:343 / 373
页数:31
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