New insights into combined surfzone, embayment, and estuarine bathing hazards

<p>Rip currents are the single largest cause of beach safety incidents globally, but where an estuary mouth intersects a beach, additional flows are created that can exceed the speed of a typical rip current, significantly increasing the hazard level for bathers. However, there is a paucity...

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Main Authors: C. Stokes, T. Poate, G. Masselink, T. Scott, S. Instance
Format: Article
Language:English
Published: Copernicus Publications 2024-11-01
Series:Natural Hazards and Earth System Sciences
Online Access:https://nhess.copernicus.org/articles/24/4049/2024/nhess-24-4049-2024.pdf
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author C. Stokes
T. Poate
G. Masselink
T. Scott
S. Instance
author_facet C. Stokes
T. Poate
G. Masselink
T. Scott
S. Instance
author_sort C. Stokes
collection DOAJ
description <p>Rip currents are the single largest cause of beach safety incidents globally, but where an estuary mouth intersects a beach, additional flows are created that can exceed the speed of a typical rip current, significantly increasing the hazard level for bathers. However, there is a paucity of observations of surfzone currents at estuary mouth beaches, and our understanding and ability to predict how the bathing hazard varies under different wave and tide conditions are therefore limited. Using field observations and process-based XBeach modelling at an embayed, estuary mouth beach, we demonstrate how surfzone currents can be driven by combinations of estuary discharge and wave-driven bathymetric and boundary rip currents under various combinations of wave and tide forcing. While previous studies have demonstrated the high hazard that rip currents pose, typically during lower stages of the tide, here we demonstrate that an estuary mouth beach can exhibit flows reaching 1.5 <span class="inline-formula">m s<sup>−1</sup></span> – up to 50 % stronger than typical rip current flows – with a high proportion (<span class="inline-formula">&gt;</span> 60 %) of simulated bathers exiting the surfzone during the upper half of the tidal cycle. The three-dimensional ebb shoal delta was found to strongly control surfzone currents by (1) providing a conduit for estuary flows that connect to headland boundary rips and (2) acting as a nearshore bar system to generate wave-driven “river channel bathymetric rips”. Despite significant spatio-temporal variability in the position of the river channels on the beach face, it was possible to hindcast the timing and severity of past bathing incidents from model simulations, providing a means to forewarn bathers of hazardous flows.</p>
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spelling doaj-art-ddb136efa3aa401699270a3b246fa8f12025-08-20T01:53:26ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812024-11-01244049407410.5194/nhess-24-4049-2024New insights into combined surfzone, embayment, and estuarine bathing hazardsC. Stokes0T. Poate1G. Masselink2T. Scott3S. Instance4School of Biological and Marine Sciences, University of Plymouth, Plymouth, Devon, PL4 8AA, England, UKSchool of Biological and Marine Sciences, University of Plymouth, Plymouth, Devon, PL4 8AA, England, UKSchool of Biological and Marine Sciences, University of Plymouth, Plymouth, Devon, PL4 8AA, England, UKSchool of Biological and Marine Sciences, University of Plymouth, Plymouth, Devon, PL4 8AA, England, UKRoyal National Lifeboat Institution, West Quay Road, Poole, Dorset, BH15 1HZ, England, UK<p>Rip currents are the single largest cause of beach safety incidents globally, but where an estuary mouth intersects a beach, additional flows are created that can exceed the speed of a typical rip current, significantly increasing the hazard level for bathers. However, there is a paucity of observations of surfzone currents at estuary mouth beaches, and our understanding and ability to predict how the bathing hazard varies under different wave and tide conditions are therefore limited. Using field observations and process-based XBeach modelling at an embayed, estuary mouth beach, we demonstrate how surfzone currents can be driven by combinations of estuary discharge and wave-driven bathymetric and boundary rip currents under various combinations of wave and tide forcing. While previous studies have demonstrated the high hazard that rip currents pose, typically during lower stages of the tide, here we demonstrate that an estuary mouth beach can exhibit flows reaching 1.5 <span class="inline-formula">m s<sup>−1</sup></span> – up to 50 % stronger than typical rip current flows – with a high proportion (<span class="inline-formula">&gt;</span> 60 %) of simulated bathers exiting the surfzone during the upper half of the tidal cycle. The three-dimensional ebb shoal delta was found to strongly control surfzone currents by (1) providing a conduit for estuary flows that connect to headland boundary rips and (2) acting as a nearshore bar system to generate wave-driven “river channel bathymetric rips”. Despite significant spatio-temporal variability in the position of the river channels on the beach face, it was possible to hindcast the timing and severity of past bathing incidents from model simulations, providing a means to forewarn bathers of hazardous flows.</p>https://nhess.copernicus.org/articles/24/4049/2024/nhess-24-4049-2024.pdf
spellingShingle C. Stokes
T. Poate
G. Masselink
T. Scott
S. Instance
New insights into combined surfzone, embayment, and estuarine bathing hazards
Natural Hazards and Earth System Sciences
title New insights into combined surfzone, embayment, and estuarine bathing hazards
title_full New insights into combined surfzone, embayment, and estuarine bathing hazards
title_fullStr New insights into combined surfzone, embayment, and estuarine bathing hazards
title_full_unstemmed New insights into combined surfzone, embayment, and estuarine bathing hazards
title_short New insights into combined surfzone, embayment, and estuarine bathing hazards
title_sort new insights into combined surfzone embayment and estuarine bathing hazards
url https://nhess.copernicus.org/articles/24/4049/2024/nhess-24-4049-2024.pdf
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