Long-Term Morphological Modeling of Barrier Island Tidal Inlets

The primary focus of this study is to apply a two-dimensional (2-D) coupled flow-wave-sediment modeling system to simulate the development and growth of idealized barrier island tidal inlets. The idealized systems are drawn from nine U.S. coastal inlets representing Pacific Coast, Gulf Coast and Atl...

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Main Authors: Richard Styles, Mitchell E. Brown, Katherine E. Brutsché, Honghai Li, Tanya M. Beck, Alejandro Sánchez
Format: Article
Language:English
Published: MDPI AG 2016-09-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:http://www.mdpi.com/2077-1312/4/4/65
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author Richard Styles
Mitchell E. Brown
Katherine E. Brutsché
Honghai Li
Tanya M. Beck
Alejandro Sánchez
author_facet Richard Styles
Mitchell E. Brown
Katherine E. Brutsché
Honghai Li
Tanya M. Beck
Alejandro Sánchez
author_sort Richard Styles
collection DOAJ
description The primary focus of this study is to apply a two-dimensional (2-D) coupled flow-wave-sediment modeling system to simulate the development and growth of idealized barrier island tidal inlets. The idealized systems are drawn from nine U.S. coastal inlets representing Pacific Coast, Gulf Coast and Atlantic Coast geographical and climatological environments. A morphological factor is used to effectively model 100 years of inlet evolution and the resulting morphological state is gauged in terms of the driving hydrodynamic processes. Overall, the model performs within the range of established theoretically predicted inlet cross-sectional area. The model compares favorably to theoretical models of maximum inlet currents, which serve as a measure of inlet stability. Major morphological differences are linked to inlet geometry and tidal forcing. Narrower inlets develop channels that are more aligned with the inlet axis while wider inlets develop channels that appear as immature braided channel networks similar to tidal flats in regions with abundant sediment supply. Ebb shoals with strong tidal forcing extend further from shore and spread laterally, promoting multi-lobe development bisected by ebb shoal channels. Ebb shoals with moderate tidal forcing form crescent bars bracketing a single shore-normal channel. Longshore transport contributes to ebb shoal asymmetry and provides bed material to help maintain the sediment balance in the bay.
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spelling doaj.art-72dd5cd2a611498799f82b84a45588332022-12-21T19:46:10ZengMDPI AGJournal of Marine Science and Engineering2077-13122016-09-01446510.3390/jmse4040065jmse4040065Long-Term Morphological Modeling of Barrier Island Tidal InletsRichard Styles0Mitchell E. Brown1Katherine E. Brutsché2Honghai Li3Tanya M. Beck4Alejandro Sánchez5U.S. Army Engineer Research and Development Center, Coastal and Hydraulics Laboratory, 3909 Halls Ferry Road, Vicksburg, MS 39180, USAU.S. Army Engineer Research and Development Center, Coastal and Hydraulics Laboratory, 3909 Halls Ferry Road, Vicksburg, MS 39180, USAU.S. Army Engineer Research and Development Center, Coastal and Hydraulics Laboratory, 3909 Halls Ferry Road, Vicksburg, MS 39180, USAU.S. Army Engineer Research and Development Center, Coastal and Hydraulics Laboratory, 3909 Halls Ferry Road, Vicksburg, MS 39180, USAU.S. Army Engineer Research and Development Center, Coastal and Hydraulics Laboratory, 3909 Halls Ferry Road, Vicksburg, MS 39180, USAInstitute for Water Resources, Hydrologic Engineering Center, 609 Second Street, Davis, CA 95616, USAThe primary focus of this study is to apply a two-dimensional (2-D) coupled flow-wave-sediment modeling system to simulate the development and growth of idealized barrier island tidal inlets. The idealized systems are drawn from nine U.S. coastal inlets representing Pacific Coast, Gulf Coast and Atlantic Coast geographical and climatological environments. A morphological factor is used to effectively model 100 years of inlet evolution and the resulting morphological state is gauged in terms of the driving hydrodynamic processes. Overall, the model performs within the range of established theoretically predicted inlet cross-sectional area. The model compares favorably to theoretical models of maximum inlet currents, which serve as a measure of inlet stability. Major morphological differences are linked to inlet geometry and tidal forcing. Narrower inlets develop channels that are more aligned with the inlet axis while wider inlets develop channels that appear as immature braided channel networks similar to tidal flats in regions with abundant sediment supply. Ebb shoals with strong tidal forcing extend further from shore and spread laterally, promoting multi-lobe development bisected by ebb shoal channels. Ebb shoals with moderate tidal forcing form crescent bars bracketing a single shore-normal channel. Longshore transport contributes to ebb shoal asymmetry and provides bed material to help maintain the sediment balance in the bay.http://www.mdpi.com/2077-1312/4/4/65hydrodynamic modelingtidal inletslong-term morphological changesediment transportmorphodynamic modelingcoastal inlet evolution
spellingShingle Richard Styles
Mitchell E. Brown
Katherine E. Brutsché
Honghai Li
Tanya M. Beck
Alejandro Sánchez
Long-Term Morphological Modeling of Barrier Island Tidal Inlets
Journal of Marine Science and Engineering
hydrodynamic modeling
tidal inlets
long-term morphological change
sediment transport
morphodynamic modeling
coastal inlet evolution
title Long-Term Morphological Modeling of Barrier Island Tidal Inlets
title_full Long-Term Morphological Modeling of Barrier Island Tidal Inlets
title_fullStr Long-Term Morphological Modeling of Barrier Island Tidal Inlets
title_full_unstemmed Long-Term Morphological Modeling of Barrier Island Tidal Inlets
title_short Long-Term Morphological Modeling of Barrier Island Tidal Inlets
title_sort long term morphological modeling of barrier island tidal inlets
topic hydrodynamic modeling
tidal inlets
long-term morphological change
sediment transport
morphodynamic modeling
coastal inlet evolution
url http://www.mdpi.com/2077-1312/4/4/65
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AT honghaili longtermmorphologicalmodelingofbarrierislandtidalinlets
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