Olaflow results
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nature/fig/U.pdf
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@ -123,11 +123,20 @@ the crest increases, with a zone reaching 400m long in front of the wave where t
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\centering
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\centering
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\includegraphics{fig/x.pdf}
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\includegraphics{fig/x.pdf}
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\caption{Propagation of the wave supposed to be responsible for the block displacement; highlighted zone:
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\caption{Propagation of the wave supposed to be responsible for the block displacement; highlighted zone:
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qualitatively estimated position of the wave.}\label{fig:swash_trans}
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qualitatively estimated position of the wave crest.}\label{fig:swash_trans}
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\end{figure*}
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\end{figure*}
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\subsection{Hydrodynamic conditions on the breakwater}
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\subsection{Hydrodynamic conditions on the breakwater}
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The two-dimensionnal olaFlow model near the breakwater allowed to compute the flow velocity near and on the breakwater
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during the passage of the identified wave.
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\begin{figure*}
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\centering
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\includegraphics{fig/U.pdf}
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\caption{Horizontal velocity computed with the olaFlow model at x=-20m on the breakwater armor}\label{fig:U}
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\end{figure*}
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\section{Discussion}
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\section{Discussion}
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\section{Methods}
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\section{Methods}
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