Hydrodynamic Zone of Influence Due to a Floating Structure in a Fjordal Estuary—Hood Canal Bridge Impact Assessment
Floating structures such as barges and ships affect near-field hydrodynamics and create a zone of influence (ZOI). Extent of the ZOI is of particular interest due to potential obstruction to and impact on out-migrating juvenile fish. Here, we present an assessment of ZOI from Hood Canal (Floating) B...
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doaj-c8a37a008cf64d479ffcc2e0cfedcfed2021-04-02T18:16:54ZengMDPI AGJournal of Marine Science and Engineering2077-13122018-10-016411910.3390/jmse6040119jmse6040119Hydrodynamic Zone of Influence Due to a Floating Structure in a Fjordal Estuary—Hood Canal Bridge Impact AssessmentTarang Khangaonkar0Adi Nugraha1Taiping Wang2Pacific Northwest National Laboratory, U.S. Department of Energy, Seattle, WA 98109, USAPacific Northwest National Laboratory, U.S. Department of Energy, Seattle, WA 98109, USAPacific Northwest National Laboratory, U.S. Department of Energy, Seattle, WA 98109, USAFloating structures such as barges and ships affect near-field hydrodynamics and create a zone of influence (ZOI). Extent of the ZOI is of particular interest due to potential obstruction to and impact on out-migrating juvenile fish. Here, we present an assessment of ZOI from Hood Canal (Floating) Bridge, located within the 110-km-long fjord-like Hood Canal sub-basin in the Salish Sea, Washington. A field data collection program allowed near-field validation of a three-dimensional hydrodynamic model of Hood Canal with the floating bridge section embedded. The results confirm that Hood Canal Bridge, with a draft of 4.6 m covering ~85% of the width of Hood Canal, obstructs the brackish outflow surface layer. This induces increased local mixing near the bridge, causes pooling of water (up-current) during ebb and flood, and results in shadow/sheltering of water (down-current). The change in ambient currents, salinity, and temperature is highest at the bridge location and reduces to background levels with distance from the bridge. The ZOI extends ~20 m below the surface and varies from 2–3 km for currents, from 2–4 km for salinity, and from 2–5 km for temperature before the deviations with the bridge drop to <10% relative to simulated background conditions without the bridge present.http://www.mdpi.com/2077-1312/6/4/119Hood Canalfloating bridgeSalish SeahydrodynamicsFinite-Volume Community Ocean Model (FVCOM)circulationanthropogenic impactzone of influenceSalish Sea model |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Tarang Khangaonkar Adi Nugraha Taiping Wang |
spellingShingle |
Tarang Khangaonkar Adi Nugraha Taiping Wang Hydrodynamic Zone of Influence Due to a Floating Structure in a Fjordal Estuary—Hood Canal Bridge Impact Assessment Journal of Marine Science and Engineering Hood Canal floating bridge Salish Sea hydrodynamics Finite-Volume Community Ocean Model (FVCOM) circulation anthropogenic impact zone of influence Salish Sea model |
author_facet |
Tarang Khangaonkar Adi Nugraha Taiping Wang |
author_sort |
Tarang Khangaonkar |
title |
Hydrodynamic Zone of Influence Due to a Floating Structure in a Fjordal Estuary—Hood Canal Bridge Impact Assessment |
title_short |
Hydrodynamic Zone of Influence Due to a Floating Structure in a Fjordal Estuary—Hood Canal Bridge Impact Assessment |
title_full |
Hydrodynamic Zone of Influence Due to a Floating Structure in a Fjordal Estuary—Hood Canal Bridge Impact Assessment |
title_fullStr |
Hydrodynamic Zone of Influence Due to a Floating Structure in a Fjordal Estuary—Hood Canal Bridge Impact Assessment |
title_full_unstemmed |
Hydrodynamic Zone of Influence Due to a Floating Structure in a Fjordal Estuary—Hood Canal Bridge Impact Assessment |
title_sort |
hydrodynamic zone of influence due to a floating structure in a fjordal estuary—hood canal bridge impact assessment |
publisher |
MDPI AG |
series |
Journal of Marine Science and Engineering |
issn |
2077-1312 |
publishDate |
2018-10-01 |
description |
Floating structures such as barges and ships affect near-field hydrodynamics and create a zone of influence (ZOI). Extent of the ZOI is of particular interest due to potential obstruction to and impact on out-migrating juvenile fish. Here, we present an assessment of ZOI from Hood Canal (Floating) Bridge, located within the 110-km-long fjord-like Hood Canal sub-basin in the Salish Sea, Washington. A field data collection program allowed near-field validation of a three-dimensional hydrodynamic model of Hood Canal with the floating bridge section embedded. The results confirm that Hood Canal Bridge, with a draft of 4.6 m covering ~85% of the width of Hood Canal, obstructs the brackish outflow surface layer. This induces increased local mixing near the bridge, causes pooling of water (up-current) during ebb and flood, and results in shadow/sheltering of water (down-current). The change in ambient currents, salinity, and temperature is highest at the bridge location and reduces to background levels with distance from the bridge. The ZOI extends ~20 m below the surface and varies from 2–3 km for currents, from 2–4 km for salinity, and from 2–5 km for temperature before the deviations with the bridge drop to <10% relative to simulated background conditions without the bridge present. |
topic |
Hood Canal floating bridge Salish Sea hydrodynamics Finite-Volume Community Ocean Model (FVCOM) circulation anthropogenic impact zone of influence Salish Sea model |
url |
http://www.mdpi.com/2077-1312/6/4/119 |
work_keys_str_mv |
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