2007
DOI: 10.1016/j.jseaes.2006.05.008
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Wave attenuation in coastal mangroves in the Red River Delta, Vietnam

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Cited by 212 publications
(163 citation statements)
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“…For instance, VoLuong and Massel (2006) found that 50-70% of the wave energy was dissipated in the first 200 m of a mangrove forest, but Massel et al (1999) found that it varied between 20 and 55%, 150 m into the forest. The projected area of mangrove vegetation is closely related to species composition and age, as both factors determine the presence of different types and densities of roots, stems and branches (Massel et al 1999, Quartel et al 2007). …”
Section: Wind and Swell Wave Attenuationmentioning
confidence: 99%
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“…For instance, VoLuong and Massel (2006) found that 50-70% of the wave energy was dissipated in the first 200 m of a mangrove forest, but Massel et al (1999) found that it varied between 20 and 55%, 150 m into the forest. The projected area of mangrove vegetation is closely related to species composition and age, as both factors determine the presence of different types and densities of roots, stems and branches (Massel et al 1999, Quartel et al 2007). …”
Section: Wind and Swell Wave Attenuationmentioning
confidence: 99%
“…Characteristics that influence the ability of mangroves to reduce storm surge levels can be assumed to be quite similar to those mentioned above (wave attenuation), albeit with less certainty. Mangrove width, vegetation characteristics (roots, stems, branches) and topography have been mentioned as the major factors (Mazda et al 1997a, Quartel et al 2007, Zhang et al 2012). The main difference with wave attenuation is that storm surges cannot be assigned linear relationship to any of these factors.…”
Section: Storm Surge Reductionmentioning
confidence: 99%
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