Biblio: typos
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@ -148,7 +148,6 @@ time-domain analysis. They also stuied the influence of imperfect collocation
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of the sensors, showing that the time delay between sensors leads to a peak in
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the reflection coefficient at a frequency related to this time delta.
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%%% TODO? %%%
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% \cite{sheremet2002observations}
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\subsection{Conclusion}
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@ -479,16 +478,17 @@ boulders is sliding, rather than rolling or saltation.
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\textcite{weiss2015untangling} highlights inadequacies in the criteria that are
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generally used \parencite{nott2003waves,nandasena2011reassessment}. According
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to \textcite{weiss2015untangling}, the use of a minimum threshold on block
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displacement does not account for the possibility of a block returning to its
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movement does not account for the possibility of a block returning to its
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initial position after being slightly disloged. A new threshold is proposed on
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the minimal movement of a block, while considering the time-dependent nature of
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wave-induced flow. \textcite{weiss2015untangling} also shows the importance of
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the pre-transport conditions on block displacement.
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\textcite{kennedy2017extreme} derived new equations following the approach from
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\textcite{nandasena2011numerical} accounting for non-parallelepipedic blocks.
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The revised equations led to a lower velocity threshold for block movement.
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This highlights the importance of boulder shape in displacement considerations.
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\textcite{nandasena2011reassessment} accounting for non-parallelepipedic
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blocks. The revised equations led to a lower velocity threshold for block
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movement. This highlights the importance of boulder shape in displacement
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considerations.
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\textcite{lodhi2020role} highlighted the importance of hydrodynamic pressure in
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block displacement. A new equation was given for the threshold flow velocity
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