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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Main Authors: Kehui Xu, P. Ansley Wren, Yanxia Ma
Format: Article
Language:English
Published: MDPI AG 2020-10-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/8/10/810
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spelling 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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