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Biblio: lead -> led

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Edgar P. Burkhart 2022-02-22 09:54:21 +01:00
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2 changed files with 3 additions and 3 deletions
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biblio/chapters/introduction.tex
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@ -11,7 +11,7 @@ of the breakwater. The simulation will be performed using the olaFlow
\parencite{olaFlow} model in a three-dimensionnal setting.
This study presents several aspects that are crucial to consider in order to
obtain accurate results. The seastate that lead to the studied event is known
obtain accurate results. The seastate that led to the studied event is known
thanks to a wave buoy located in front of the breakwater \parencite{amir}.
However, in order to input an accurate incident wave into the numerical model,
it will be necessary to extract the incident and reflected waves from the raw

4
biblio/chapters/literature.tex
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@ -86,7 +86,7 @@ and reflected waves. This method relies on two or more gauges, using a least
squares method. Results are very accurate in the absence of noise, but a small
amount of error appears when noise is added.
\textcite{inch2016accurate} noticed that the presence of noise lead to
\textcite{inch2016accurate} noticed that the presence of noise led to
overestimation of reflection coefficient. The creation of bias lookup tables is
proposed in order to account for noise-induced error in reflection coefficient
estimations.
@ -487,7 +487,7 @@ the pre-transport conditions on block displacement.
\textcite{kennedy2017extreme} derived new equations following the approach from
\textcite{nandasena2011numerical} accounting for non-parallelepipedic blocks.
The revised equations lead to a lower velocity threshold for block movement.
The revised equations led to a lower velocity threshold for block movement.
This highlights the importance of boulder shape in displacement considerations.
\textcite{lodhi2020role} highlighted the importance of hydrodynamic pressure in