Biblio: boulders
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@ -426,6 +426,14 @@ porosity induced friction.
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\section{Block displacement by waves}
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\subsection{Introduction}
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Displacement of blocks or boulders by waves has been a major topic in
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understanding the influence of storm and tsunami waves in coastal regions.
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Several approaches have been taken to study this phenomenon. In a first part,
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we will discuss in-situ studies on displaced boulders. In a second part, we
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will review models of block displacements.
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\subsection{In-situ studies}
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\cite{barbano2010large}
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@ -435,6 +443,7 @@ porosity induced friction.
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\cite{biolchi2016}
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\cite{kennedy2016observations}
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\cite{erdmann2018boulder}
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\cite{cox2018extraordinary}
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\subsection{Models}
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@ -442,7 +451,7 @@ porosity induced friction.
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\cite{nott2003waves} Submerged boulder:
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\begin{equation}
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u^2 \ge \frac{2\left(\rho_s-\frac{\rho_s}{\rho_w}\right)ag}
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u^2 \ge \frac{2\left(\frac{\rho_s}{\rho_w}-1\right)ag}
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{C_d\left(\frac{ac}{b^2}\right)+C_l}
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\end{equation}
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@ -467,7 +476,7 @@ u^2 \ge \frac{2\left(\frac{\rho_s}{\rho_w}-1\right) gc
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\cite{kennedy2017extreme}
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\cite{weiss2017toward}
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\cite{bressan2018laboratory}
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\cite{bressan2018laboratory} Partially submerged boulders
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\begin{equation}
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u^2 \ge \frac{2b_wW}{\rho_w\left(b_DC_DA_{wfs}+b_LC_LA_{wbs}\right)}
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\end{equation}
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@ -1086,3 +1086,12 @@
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publisher={Wiley Online Library}
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}
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@article{cox2020systematic,
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title={Systematic review shows that work done by storm waves can be misinterpreted as tsunami-related because commonly used hydrodynamic equations are flawed},
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author={Cox, R{\'o}nadh and Ardhuin, Fabrice and Dias, Fr{\'e}d{\'e}ric and Autret, Ronan and Beisiegel, Nicole and Earlie, Claire S and Herterich, James G and Kennedy, Andrew and Paris, Rapha{\"e}l and Raby, Alison and others},
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journal={Frontiers in Marine Science},
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pages={4},
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year={2020},
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publisher={Frontiers}
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}
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