Tidal and Storm Impacts on Hydrodynamics and Sediment Dynamics in an Energetic Ebb Tidal Delta
Bottom-mounted instrumentation was deployed at two sites on a large sandy shoal of an ebb tidal delta offshore of the Port Royal Sound of South Carolina of USA to collect hydrodynamics and sediment dynamics data. One site (“borrow site”) was 2 km offshore in a dredge pit for nearby beach nourishment...
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doaj-0e74867bd24747c2b223d1f2f7e1de722021-04-02T10:46:32ZengMDPI AGJournal of Marine Science and Engineering2077-13122020-10-01881081010.3390/jmse8100810Tidal and Storm Impacts on Hydrodynamics and Sediment Dynamics in an Energetic Ebb Tidal DeltaKehui Xu0P. Ansley Wren1Yanxia Ma2Department of Oceanography & Coastal Sciences, Louisiana State University, Baton Rouge, LA 70803, USADepartment of Marine Science, Coastal Carolina University, Conway, SC 29528, USALouisiana Legislative Auditor, Baton Rouge, LA 70802, USABottom-mounted instrumentation was deployed at two sites on a large sandy shoal of an ebb tidal delta offshore of the Port Royal Sound of South Carolina of USA to collect hydrodynamics and sediment dynamics data. One site (“borrow site”) was 2 km offshore in a dredge pit for nearby beach nourishment and the other site (“reference site”) was 10 km offshore. In situ time-series data were collected during two periods after the dredging: 15 March–12 June (spring) and 18 August–18 November (fall) of 2012. Data at the reference site indicated active migrating bedforms from centimeters to decimeters tall, and sediment concentrations were highly associated with semidiurnal and fortnightly tidal cycles. In the fall deployment, waves at the reference site were higher than those at the shallow borrow site. Both Tropical Storm Beryl and Hurricane Sandy formed high waves and strong currents but did not generate the greatest sediment fluxes. The two sites were at different depths and distances offshore, and waves contributed more to sediment mobility at the reference site whereas tidal forcing was the key controlling factor at the borrow site. This study provides valuable datasets for the selection of sites, prediction of pit infilling, and the modeling of storm impact in future beach nourishment and coastal restoration projects.https://www.mdpi.com/2077-1312/8/10/810hydrodynamicssediment dynamicsPort Royal Soundebb tidal deltabeach nourishmentbottom boundary layer |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Kehui Xu P. Ansley Wren Yanxia Ma |
spellingShingle |
Kehui Xu P. Ansley Wren Yanxia Ma Tidal and Storm Impacts on Hydrodynamics and Sediment Dynamics in an Energetic Ebb Tidal Delta Journal of Marine Science and Engineering hydrodynamics sediment dynamics Port Royal Sound ebb tidal delta beach nourishment bottom boundary layer |
author_facet |
Kehui Xu P. Ansley Wren Yanxia Ma |
author_sort |
Kehui Xu |
title |
Tidal and Storm Impacts on Hydrodynamics and Sediment Dynamics in an Energetic Ebb Tidal Delta |
title_short |
Tidal and Storm Impacts on Hydrodynamics and Sediment Dynamics in an Energetic Ebb Tidal Delta |
title_full |
Tidal and Storm Impacts on Hydrodynamics and Sediment Dynamics in an Energetic Ebb Tidal Delta |
title_fullStr |
Tidal and Storm Impacts on Hydrodynamics and Sediment Dynamics in an Energetic Ebb Tidal Delta |
title_full_unstemmed |
Tidal and Storm Impacts on Hydrodynamics and Sediment Dynamics in an Energetic Ebb Tidal Delta |
title_sort |
tidal and storm impacts on hydrodynamics and sediment dynamics in an energetic ebb tidal delta |
publisher |
MDPI AG |
series |
Journal of Marine Science and Engineering |
issn |
2077-1312 |
publishDate |
2020-10-01 |
description |
Bottom-mounted instrumentation was deployed at two sites on a large sandy shoal of an ebb tidal delta offshore of the Port Royal Sound of South Carolina of USA to collect hydrodynamics and sediment dynamics data. One site (“borrow site”) was 2 km offshore in a dredge pit for nearby beach nourishment and the other site (“reference site”) was 10 km offshore. In situ time-series data were collected during two periods after the dredging: 15 March–12 June (spring) and 18 August–18 November (fall) of 2012. Data at the reference site indicated active migrating bedforms from centimeters to decimeters tall, and sediment concentrations were highly associated with semidiurnal and fortnightly tidal cycles. In the fall deployment, waves at the reference site were higher than those at the shallow borrow site. Both Tropical Storm Beryl and Hurricane Sandy formed high waves and strong currents but did not generate the greatest sediment fluxes. The two sites were at different depths and distances offshore, and waves contributed more to sediment mobility at the reference site whereas tidal forcing was the key controlling factor at the borrow site. This study provides valuable datasets for the selection of sites, prediction of pit infilling, and the modeling of storm impact in future beach nourishment and coastal restoration projects. |
topic |
hydrodynamics sediment dynamics Port Royal Sound ebb tidal delta beach nourishment bottom boundary layer |
url |
https://www.mdpi.com/2077-1312/8/10/810 |
work_keys_str_mv |
AT kehuixu tidalandstormimpactsonhydrodynamicsandsedimentdynamicsinanenergeticebbtidaldelta AT pansleywren tidalandstormimpactsonhydrodynamicsandsedimentdynamicsinanenergeticebbtidaldelta AT yanxiama tidalandstormimpactsonhydrodynamicsandsedimentdynamicsinanenergeticebbtidaldelta |
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