2017
DOI: 10.1016/j.crte.2017.09.003
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Wave forcing and morphological changes of New Caledonia lagoon islets: Insights on their possible relations

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Cited by 14 publications
(8 citation statements)
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“…Nevertheless, in the SW lagoon, where trade winds can blow over a sufficient fetch distance to generate wind waves, Jouon et al (2009) confirmed by observations that the sea state of this lagoon is clearly dominated by high-frequency wind waves. This was confirmed by Aucan et al (2017) which undertook a yearly period of observations around two islets in the SW lagoon and detected three main modes: high frequency wind waves (period 3-8s), low frequency generated by incoming swell within the passages (period 8-25s) and infragravity waves (period 25-400s). Maximum significant wave height observed in the lagoon in these two studies peaks around 1m and 1.5m.…”
Section: Lagoon Dynamicsmentioning
confidence: 62%
“…Nevertheless, in the SW lagoon, where trade winds can blow over a sufficient fetch distance to generate wind waves, Jouon et al (2009) confirmed by observations that the sea state of this lagoon is clearly dominated by high-frequency wind waves. This was confirmed by Aucan et al (2017) which undertook a yearly period of observations around two islets in the SW lagoon and detected three main modes: high frequency wind waves (period 3-8s), low frequency generated by incoming swell within the passages (period 8-25s) and infragravity waves (period 25-400s). Maximum significant wave height observed in the lagoon in these two studies peaks around 1m and 1.5m.…”
Section: Lagoon Dynamicsmentioning
confidence: 62%
“…However, for the RBR instrument, a specific package called "pyrsktools" was necessary to read the dataset, and this library is provided by the manufacturer. To process the RBR instrument data, we employed the script outlined in Aucan et al (2017). Last, for data conversion, we utilized the NetCDF4 package.…”
Section: Sampling Strategymentioning
confidence: 99%
“…To deduce wave parameters (significant wave height, peak frequency, and mean wave period), data were filtered using the Fourier transform to acquire a pressure spectrum (within the range 3-25 s). Then, the methods referenced in Aucan et al (2017), also used in Aucan et al (2021) and Andréfouët et al (2023a), were applied using the linear wave theory with a homogenous cut-off frequency (set to 0.33) to filter the high-frequency spectrum. To calculate the water level, depth measurements were subtracted from the mean sea level (longterm depth-average of the temporal series).…”
Section: Rbrduet Tdmentioning
confidence: 99%
“…This is due to the SW lagoon being large enough to allow the trade winds to generate sufficient fetch to form wind-driven waves. Further observational studies by Aucan et al (2017) in the SW lagoon define three main modes of wave-based circulation, namely: high frequency wind waves (period: 3-8 s), low frequency generated by incoming swell within the passages (period: 8-25 s), and infragravity waves (period: 25-400 s). Maximum significant wave height within the SW lagoon is observed to be between 1.0 and 1.5 m (Jouon et al, 2009;Aucan et al, 2017).…”
Section: Lagoon Dynamicsmentioning
confidence: 99%
“…For waves parameters, bursts were filtered using the Fourier transform to obtain a pressure spectrum (between 3 and 25 s period), then the linear wave theory is applied. This method uses a homogenous cut-off frequency of 0.33 to filter high frequencies spectrum (method used in Aucan et al, 2017). Furthermore, none of tail diagnostics have been applied on the higher frequency range but methods do exist (e.g., JON-SWAP spectrum tail or TMA spectrum tail) (Karimpour and Chen, 2017).…”
Section: Specific Processing Stepsmentioning
confidence: 99%