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Open AccessArticle

Storm Waves at the Shoreline: When and Where Are Infragravity Waves Important?

Coastal Process Research Group, University of Plymouth, Drakes Circus, Plymouth L4 8AA, UK
Department of Geography and Planning, University of Liverpool, Brownlow Hill, Liverpool L69 7ZT, UK
Author to whom correspondence should be addressed.
J. Mar. Sci. Eng. 2019, 7(5), 139;
Received: 30 March 2019 / Revised: 30 April 2019 / Accepted: 7 May 2019 / Published: 11 May 2019
(This article belongs to the Special Issue Storm Erosion)
Infragravity waves (frequency, f = 0.005–0.05 Hz) are known to dominate hydrodynamic and sediment transport processes close to the shoreline on low-sloping sandy beaches, especially when incident waves are large. However, in storm wave conditions, how their importance varies on different beach types, and with different mixes of swell and wind-waves is largely unknown. Here, a new dataset, comprising shoreline video observations from five contrasting sites (one low-sloping sandy beach, two steep gravel beaches, and two compound/mixed sand and gravel beaches), under storm wave conditions (deep water wave height, H0 up to 6.6 m, and peak period, Tp up to 18.2 s), was used to assess: how the importance and dominance of infragravity waves varies at the shoreline? In this previously unstudied combination of wave and morphological conditions, significant infragravity swash heights (Sig) at the shoreline in excess of 0.5 m were consistently observed on all five contrasting beaches. The largest infragravity swash heights were observed on a steep gravel beach, followed by the low-sloping sandy beach, and lowest on the compound/mixed sites. Due to contrasting short wave breaking and dissipation processes, infragravity frequencies were observed to be most dominant over gravity frequencies on the low-sloping sandy beach, occasionally dominant on the gravel beaches, and rarely dominant on the compound/mixed beaches. Existing empirical predictive relationships were shown to parameterize Sig skillfully on the sand and gravel beaches separately. Deep water wave power was found to accurately predict Sig on both the sand and gravel beaches, demonstrating that, under storm wave conditions, the wave heights and periods are the main drivers of infragravity oscillations at the shoreline, with the beach morphology playing a secondary role. The exception to this was the compound/mixed beach sites where shoreline infragravity energy remained low. View Full-Text
Keywords: infragravity; swash; storm; gravel beach; parameter space; field observations infragravity; swash; storm; gravel beach; parameter space; field observations
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MDPI and ACS Style

Billson, O.; Russell, P.; Davidson, M. Storm Waves at the Shoreline: When and Where Are Infragravity Waves Important? J. Mar. Sci. Eng. 2019, 7, 139.

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