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The morphodynamic response of a gravel barrier to unimodal and bimodal storm wave conditions
Frontiers in Marine Science, Volume: 10
Swansea University Authors: KRISTIAN IONS, Dominic Reeve , Harshinie Karunarathna
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© 2023 Ions, Ozdemir, Pender, Reeve and Karunarathna. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY)
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DOI (Published version): 10.3389/fmars.2023.1087771
Abstract
Gravel barrier beaches can offer natural protection to coastlines from adversestorm conditions. Understanding the morphodynamics of gravel barrier beachesis vital for the effective and sustainable management of these systems. Here, weuse a synthetic dataset to investigate the morphodynamic response...
Published in: | Frontiers in Marine Science |
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ISSN: | 2296-7745 |
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Frontiers Media SA
2023
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v2 65552 2024-01-31 The morphodynamic response of a gravel barrier to unimodal and bimodal storm wave conditions 0eaeea3a999ce1ef38ade9b3b5f26a22 KRISTIAN IONS KRISTIAN IONS true false 3e76fcc2bb3cde4ddee2c8edfd2f0082 0000-0003-1293-4743 Dominic Reeve Dominic Reeve true false 0d3d327a240d49b53c78e02b7c00e625 0000-0002-9087-3811 Harshinie Karunarathna Harshinie Karunarathna true false 2024-01-31 Gravel barrier beaches can offer natural protection to coastlines from adversestorm conditions. Understanding the morphodynamics of gravel barrier beachesis vital for the effective and sustainable management of these systems. Here, weuse a synthetic dataset to investigate the morphodynamic response of the gravelbarrier beach at Hurst Castle Spit, located on the Southwest coast of the UnitedKingdom, to both unimodal and bimodal storms. This spit is exposed to wind andswell waves propagating up the English Channel from the Southwest approachesand has suffered repeated storm erosion. The results are analyzed to identify thekey drivers that govern the spatio-temporal gravel barrier morphodynamicresponses to storms and to explore the morphodynamic states of the barrier.We found that the morphodynamic response of the barrier beach is stronglyinfluenced by the combination of storm wave height and still water level. Further,the presence of swell waves can be a controlling factor in the barrier response. Journal Article Frontiers in Marine Science 10 Frontiers Media SA 2296-7745 Gravel barrier, beach erosion, XBeach numerical model, bimodal wave spectrum,sediment transport 25 4 2023 2023-04-25 10.3389/fmars.2023.1087771 Data availability statement:The original contributions presented in the study are included in the article/supplementary materials. Further inquiries can be directed to the corresponding author/s. COLLEGE NANME COLLEGE CODE Swansea University External research funder(s) paid the OA fee (includes OA grants disbursed by the Library) The project was jointly funded by the Welsh Government's European Social Fund (ESF) programme for East Wales and JBA Consulting, UK. Grant number EP/R51312X/1 for the EPSRC grant. 2024-10-18T16:52:15.3094260 2024-01-31T12:45:42.5137952 Faculty of Science and Engineering School of Aerospace, Civil, Electrical, General and Mechanical Engineering - Mechanical Engineering KRISTIAN IONS 1 Khan Ozdemir 2 Douglas Pender 3 Dominic Reeve 0000-0003-1293-4743 4 Harshinie Karunarathna 0000-0002-9087-3811 5 65552__29501__d666c35f9208451eb469077123d1a36e.pdf Ions et al_2023(FMS).pdf 2024-01-31T12:50:23.3975477 Output 6526674 application/pdf Version of Record true © 2023 Ions, Ozdemir, Pender, Reeve and Karunarathna. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY) true eng http://creativecommons.org/licenses/by/4.0/ |
title |
The morphodynamic response of a gravel barrier to unimodal and bimodal storm wave conditions |
spellingShingle |
The morphodynamic response of a gravel barrier to unimodal and bimodal storm wave conditions KRISTIAN IONS Dominic Reeve Harshinie Karunarathna |
title_short |
The morphodynamic response of a gravel barrier to unimodal and bimodal storm wave conditions |
title_full |
The morphodynamic response of a gravel barrier to unimodal and bimodal storm wave conditions |
title_fullStr |
The morphodynamic response of a gravel barrier to unimodal and bimodal storm wave conditions |
title_full_unstemmed |
The morphodynamic response of a gravel barrier to unimodal and bimodal storm wave conditions |
title_sort |
The morphodynamic response of a gravel barrier to unimodal and bimodal storm wave conditions |
author_id_str_mv |
0eaeea3a999ce1ef38ade9b3b5f26a22 3e76fcc2bb3cde4ddee2c8edfd2f0082 0d3d327a240d49b53c78e02b7c00e625 |
author_id_fullname_str_mv |
0eaeea3a999ce1ef38ade9b3b5f26a22_***_KRISTIAN IONS 3e76fcc2bb3cde4ddee2c8edfd2f0082_***_Dominic Reeve 0d3d327a240d49b53c78e02b7c00e625_***_Harshinie Karunarathna |
author |
KRISTIAN IONS Dominic Reeve Harshinie Karunarathna |
author2 |
KRISTIAN IONS Khan Ozdemir Douglas Pender Dominic Reeve Harshinie Karunarathna |
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Frontiers in Marine Science |
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10 |
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2296-7745 |
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10.3389/fmars.2023.1087771 |
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Frontiers Media SA |
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Faculty of Science and Engineering |
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description |
Gravel barrier beaches can offer natural protection to coastlines from adversestorm conditions. Understanding the morphodynamics of gravel barrier beachesis vital for the effective and sustainable management of these systems. Here, weuse a synthetic dataset to investigate the morphodynamic response of the gravelbarrier beach at Hurst Castle Spit, located on the Southwest coast of the UnitedKingdom, to both unimodal and bimodal storms. This spit is exposed to wind andswell waves propagating up the English Channel from the Southwest approachesand has suffered repeated storm erosion. The results are analyzed to identify thekey drivers that govern the spatio-temporal gravel barrier morphodynamicresponses to storms and to explore the morphodynamic states of the barrier.We found that the morphodynamic response of the barrier beach is stronglyinfluenced by the combination of storm wave height and still water level. Further,the presence of swell waves can be a controlling factor in the barrier response. |
published_date |
2023-04-25T16:52:13Z |
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1813267594015145984 |
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11.037166 |