2010
DOI: 10.1016/j.coastaleng.2009.09.013
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Estimation of infragravity waves at intermediate water depth

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Cited by 15 publications
(19 citation statements)
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“…Although, distinguishable energy distributions that are bimodal can be observed during the energetic sea states, as they have peaks in 5 the shore-normal onshore and offshore propagation (corresponding to 0 and ±180 degrees). In contrast to the Herbers et al (1995b) observations, Reniers et al (2010) observational plot depicts that the infragravity wave energy is more prevalent in the propagation sector incident to the coast, but their numerical simulations produced more dominant energy distributed in the reflected wave sector. The observed dominant energy distributions in disparate directional sectors may be related to their measurement depths; Herbers et al (1995b) derived their directional spectra in the 13 m depth of water, and Reniers et al…”
mentioning
confidence: 56%
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“…Although, distinguishable energy distributions that are bimodal can be observed during the energetic sea states, as they have peaks in 5 the shore-normal onshore and offshore propagation (corresponding to 0 and ±180 degrees). In contrast to the Herbers et al (1995b) observations, Reniers et al (2010) observational plot depicts that the infragravity wave energy is more prevalent in the propagation sector incident to the coast, but their numerical simulations produced more dominant energy distributed in the reflected wave sector. The observed dominant energy distributions in disparate directional sectors may be related to their measurement depths; Herbers et al (1995b) derived their directional spectra in the 13 m depth of water, and Reniers et al…”
mentioning
confidence: 56%
“…-An estimation of bound wave energy: there are numerous studies, which demonstrate that the statistics related to the 10 bispectrum can be used to estimate the bound wave energy (Herbers et al, 1994;Reniers et al, 2002), however, the statistical uncertainty in the bispectral estimates is relatively large when the nonlinearity is weak (Herbers et al, 1994), and the method becomes unreliable for high waves when the assumption of a slowly varying wave group is no longer valid (Reniers et al, 2002(Reniers et al, , 2010. Accordingly, we have focused on the total infragravity wave heights and their dependence to the wind-generated wave integrated parameters.…”
Section: Correlation Analysis Interpretationmentioning
confidence: 99%
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