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@ -101,3 +101,12 @@
year={1998}, year={1998},
publisher={American Meteorological Society} publisher={American Meteorological Society}
} }
@article{dysthe2008,
title={Oceanic rogue waves},
author={Dysthe, Kristian and Krogstad, Harald E and M{\"u}ller, Peter},
journal={Annu. Rev. Fluid Mech.},
volume={40},
pages={287--310},
year={2008},
publisher={Annual Reviews}
}

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@ -85,6 +85,9 @@ Initial analysis of the buoy data plotted in Figure~\ref{fig:wave} shows that th
orbitals that correspond to an incident wave direction. These results would indicate that the identified wave is orbitals that correspond to an incident wave direction. These results would indicate that the identified wave is
essentially an incident wave, with a minor reflected component. essentially an incident wave, with a minor reflected component.
The wavelet power spectrum displayed in Figure~\ref{wavelet} highlights a primary infragravity wave in the signal, with
a period of over 30s.
\begin{figure*} \begin{figure*}
\centering \centering
\includegraphics{fig/ts.pdf} \includegraphics{fig/ts.pdf}
@ -167,7 +170,18 @@ exhibits a water level over 5m for over 40s.
\section{Discussion} \section{Discussion}
\subsection{Incident wave}
According to the criteria proposed by \textcite{dysthe2008}, rogue waves can be defined as waves with an amplitude over
twice the significant wave height over a given period.
\subsection{Reflection analysis}
The 13\% difference between those values highlights the existence of a notable amount of reflection at the buoy.
Nonetheless, the gap between the values is still fairly small and the extreme wave identified on February 28, 2017 at
17:23:08 could still be considered as an incident wave.
\subsection{}
\section{Methods} \section{Methods}
\printbibliography \printbibliography