Effect of a seagrass (Posidonia oceanica) meadow on wave propagation
By E. Infantes, A. Orfila, G. Simarro, J. Terrados, Mitul Luhar, H. Nepf. 2012
160 citations recorded by the source corpus.
Subfields: Earth-Surface Processes, Ecology, Oceanography
View Paper: https://www.semanticscholar.org/paper/85bbe66392b7b2610fd9b05bcc537c6abb692a02
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In Earth-Surface Processes
In Ecology
In Oceanography
Citations in the corpus
- Marine biodiversity and ecosystem function relationships: The potential for practical monitoring applications (2015, unknown): “…(Jenkins et al.,1999); modi fi cation of boundary conditions, sedimentation and shoreline stabilization (Hull,1987; Boudouresque et al., 2012; Infantes et al., 2012; Jackson et al., 2013) and also providing a physical structure for colonization (Epifanio et al., 2003; Rabaut et al., 2007).”
- Biogeomorphology of the Mediterranean Posidonia oceanica seagrass meadows (2017, methodology): “In this field, Infantes et al. (2012) used seafloor mounted Acoustic Doppler Velocimeters (ADVs) to evaluate wave attenuation induced by meadows directly, finding that Posidonia oceanica meadows reduce wave height reaching the beach and raised the importance of the parameters ks…”
- Wave-induced dynamics of flexible blades (2015, methodology): “It has been studied in the laboratory [11, 20, 28], in the field [5, 18], and using analytical methods or numerical models [20, 32, 31].”
- The necromass of the Posidonia oceanica seagrass meadow: fate, role, ecosystem services and vulnerability (2016, unknown): “…resulting in enhanced sand deposition, beach progradation and hence protection of beaches from erosion (Boudouresque & Jeudy de Grissac, 1983; Gacia & Duarte, 2001; Duarte, 2004; Sánchez- González et al., 2011; Stratigaki et al., 2011; Infantes et al., 2012; Manca et al., 2012) (Fig.”
- Wave damping by flexible vegetation: Connecting individual blade dynamics to the meadow scale (2019, methodology): “581 586 587 4.3 Comparison with wave decay measured in the field 588 Infantes et al. (2012) measured wave decay in the field over a Posidonia oceanica meadow for 589 waves with periods 𝑇 = 4 − 10 s. Wave heights were measured at four mooring locations across 590 a depth gradient of 6.5 m to 16.5 m.”