Infantes E, Orfila A, Simarro G, Luhar M, Terrados J, Nepf H
Marine Ecology Progress Series 456: 63-72
Publication year: 2012

ABSTRACT

We demonstrate the utility of using the equivalent bottom roughness for calculating the friction factor and the drag coefficient of a seagrass meadow for conditions in which the meadow height is small compared to the water depth. Wave attenuation induced by the seagrass Posidonia oceanica is evaluated using field data from bottom-mounted acoustic doppler velocimeters (ADVs).

Using the data from one storm event, the equivalent bottom roughness is calculated for the meadow as ks ~ 0.40 m. This equivalent roughness is used to predict the wave friction factor ƒw, the drag coefficient on the plant, CD, and ultimately the wave attenuation for other storms. Root mean squared wave height (Hrms) is reduced by around 50% for incident waves of 1.1 m propagating over ~1000 m of a meadow of P. oceanica with shoot density of ~600 shoots m−2.

Cite as: Infantes E, Orfila A, Simarro G, Luhar M, Terrados J, Nepf H. (2012) Effect of a seagrass (Posidonia oceanica) meadow on wave propagation. Marine Ecology Progress Series 456: 63-72. doi.org/10.3354/meps09754

Highlights

  • Equivalent bottom roughness is useful for calculating friction factor and drag coefficient of seagrass meadows.
  • Wave attenuation from Posidonia oceanica is evaluated with field data from bottom-mounted ADVs.
  • Equivalent bottom roughness is calculated as ks ~ 0.40 m, used to predict wave friction factor and drag coefficient.
  • Hrms is reduced by 50% for incident waves of 1.1 m propagating over 1000 m of P. oceanica meadow with shoot density of ~600 shoots m−2.

This article forms part of my research on hydrodynamics-seagrass interactions.

Learn how waves, currents, and sediment dynamics constrain seagrass persistence and resilience.

Effect of a seagrass (Posidonia oceanica) meadow on wave propagation
Effect of a seagrass (Posidonia oceanica) meadow on wave propagation

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