Abstract
This paper assesses the influence of different flow and vegetation parameters on the wave attenuation provided by two contrasting salt marsh species: Puccinellia maritima and Spartina anglica. Different water depths and wave parameters (height and period) are considered for both regular and irregular waves with and without an underlying uniform current coming from different directions. The study of the submergence ratio (h/hv) influence shows that wave damping coefficient rapidly decreases as the plant submergence ratio increases. The high nonlinearities found in the wave-current interaction lead to different wave damping patterns in comparison to wave-only conditions. A smaller wave damping is found for waves and current acting in the same direction and an increase in the wave damping rate is obtained for waves and current flowing in the opposite direction. These wave and current tests allow for the studying of the energy dissipation produced by the vegetation, increasing our knowledge about flow and plant interaction in estuarine conditions. The biomechanical properties of the two real salt marshes used in the experiments are also evaluated and related to wave damping revealing a higher attenuation for stiffer vegetation. Both, the vegetation density and the biomass strongly influence wave damping. Higher density and biomass values lead to higher attenuation rates for both species.
Original language | English |
---|---|
Pages (from-to) | 73-86 |
Number of pages | 14 |
Journal | Coastal Engineering |
Volume | 106 |
DOIs | |
Publication status | Published - 1 Dec 2015 |
Externally published | Yes |
Bibliographical note
Funding Information:M. Maza is indebted to the MEC (Ministerio de Educación, Cultura y Deporte, Spain) for the funding provided in the FPU (Formación del Profesorado Universitario) studentship ( BOE-A-2012-6238 ). This work has been partially funded under the RETOS INVESTIGACION 2014 program of the Spanish Ministry of Economy and Competitiveness ( BIA-2014-59718-R ). Part of this work has been funded by the European Regional Development Fund .
Funding Information:
J. Trinogga and T.J. Bouma are indebted to the German Ministry for Research and Education for funding via the COMTESS project (grant no. 01LL0911 A-G ). Furthermore we are grateful to Michael Kleyer for his constructive support.
Publisher Copyright:
© 2015 Elsevier B.V.
Funding
M. Maza is indebted to the MEC (Ministerio de Educación, Cultura y Deporte, Spain) for the funding provided in the FPU (Formación del Profesorado Universitario) studentship ( BOE-A-2012-6238 ). This work has been partially funded under the RETOS INVESTIGACION 2014 program of the Spanish Ministry of Economy and Competitiveness ( BIA-2014-59718-R ). Part of this work has been funded by the European Regional Development Fund . J. Trinogga and T.J. Bouma are indebted to the German Ministry for Research and Education for funding via the COMTESS project (grant no. 01LL0911 A-G ). Furthermore we are grateful to Michael Kleyer for his constructive support.
Keywords
- Collinear and non-collinear waves and currents
- Large scale 3-D experiments
- Real vegetation