Flow interaction with dynamic vegetation patches: Implications for biogeomorphic evolution of a tidal landscape
By W. Vandenbruwaene, Stijn Temmerman, Tjeerd Joris Bouma, P. Klaassen, M. Vries, D. Callaghan, P. Steeg, F. Dekker, L. van Duren, E. Martini and 4 more. 2011
182 citations recorded by the source corpus.
Subfields: Earth-Surface Processes, Ecology
View Paper: https://www.semanticscholar.org/paper/049b7eab59d337aba962de718179e14dd64ae013
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In Earth-Surface Processes
In Ecology
Citations in the corpus
- Organism traits determine the strength of scale-dependent bio-geomorphic feedbacks: A flume study on three intertidal plant species (2013, unknown): “…the local positive feedback is achieved through flow reduction and sedimentation within vegetation patches (Bouma et al., 2007; Zong and Nepf, 2010; Vandenbruwaene et al., 2011), which leads there to improved plant growth (Van Wesenbeeck et al., 2008), while the long-distance negative feedback…”
- Does biogeomorphic feedback lead to abrupt shifts between alternative landscape states?: An empirical study on intertidal flats and marshes (2013, background): “[4] Tidal marshes are a clear example of a biogeomorphic system: the marsh vegetation reduces hydrodynamic forces from waves and tidal currents, hence preventing erosion and promoting sediment accretion [e.g., Bouma et al., 2007;Mudd et al., 2010; Vandenbruwaene et al., 2011].”