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Open AccessJournal ArticleDOI

Cross‐shore sand transport by infragravity waves as a function of beach steepness

TLDR
In this paper, the influence of infragravity waves on sand suspension and cross-shore transport was investigated using two field data sets of near-bed velocity, pressure, and sediment concentration.
Abstract
Two field data sets of near-bed velocity, pressure, and sediment concentration are analyzed to study the influence of infragravity waves on sand suspension and cross-shore transport. On the moderately sloping Sand Motor beach (≈1:35), the local ratio of infragravity wave height to sea-swell wave height is relatively small (HIG/HSW 0.4), most sand is suspended during negative infragravity velocities, and qIG is offshore directed. The infragravity contribution to the total sand flux is considerably larger and reaches up to ≈60% during energetic conditions. On the whole, HIG/HSW is a good indicator for the infragravity-related sand suspension mechanism and the resulting infragravity sand transport direction and relative importance.

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Citations
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Journal ArticleDOI

Infragravity waves: From driving mechanisms to impacts

TL;DR: In this paper, the authors focus on the most common type of IG waves, those induced by the presence of groups in incident short waves, and three related mechanisms explain their generation: (1) the development, shoaling and release of waves bound to the short-wave group envelopes (2) the modulation by these envelopes of the location where short waves break, and (3) the merging of bores (breaking wave front, resembling to a hydraulic jump) inside the surfzone.
Journal ArticleDOI

Environmental and morphologic controls on wave-induced dune response

TL;DR: In this paper, a relationship was found between morphologic characteristics and dune volume changes during storm events producing high water levels, and the model simulations indicated that wave-driven dune growth may occur on low sloping beaches in cases where the dynamic still water level (still water level plus wave setup) is lower than the dune toe.
Journal ArticleDOI

A novel machine learning algorithm for tracking remotely sensed waves in the surf zone

TL;DR: In this paper, the authors used time-space images (timestacks) to detect white pixel intensity peaks generated by breaking waves and confirmed these peaks as true wave breaking events by learning from the data's true colour representation, clusters individual waves, and obtains optimal wave paths.
Journal ArticleDOI

Transfer and dissipation of energy during wave group propagation on a gentle beach slope

TL;DR: In this paper, the propagation of bichromatic wave groups over a constant 1:100 beach slope and the influence of the group modulation is presented, where modulation is controlled by varying the group frequency, fg, which is shown to remarkably affect the energy transfer to high and low frequency components.
References
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MonographDOI

Quantile Regression: Name Index

Roger Koenker
Journal ArticleDOI

A gentle introduction to quantile regression for ecologists

TL;DR: Quantile regression is a way to estimate the conditional quantiles of a response variable distribution in the linear model that provides a more complete view of possible causal relationships between variables in ecological processes.
Journal ArticleDOI

Observations of sand bar evolution on a natural beach

TL;DR: Waves, currents, and the location of the seafloor were measured on a barred beach for about 2 months at nine locations along a cross-shore transect extending 255 m from 1 to 4 m water depth as discussed by the authors.
Journal ArticleDOI

Swash oscillations on a natural beach

TL;DR: In this paper, run-up energy spectra at wind wave frequencies show an ƒ−3 dependence and energy levels that are independent of incident wave height, which suggests saturation.
Journal ArticleDOI

Bar-generating cross-shore flow mechanisms on a beach

TL;DR: In this paper, random waves normally incident on a dissipative beach induce a variety of cross-shore flows, such as asymmetric oscillatory flow, wave grouping-induced long-wave flow, breaking-induced turbulent flow, and momentum decay-induced undertow.
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