Interactions between Surface Waves, Tides, and Storm-Induced Currents over Shelf Waters of the Northwest Atlantic
A coupled wave–tide–circulation model is used to investigate wave–current interactions (WCIs) over the shelf waters of the Northwest Atlantic (NWA) during Hurricane Earl (2010). WCIs have substantial impacts on hydrodynamics in the upper ocean. The significant wave heights are modulated by WCIs, par...
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ftmdpi:oai:mdpi.com:/2077-1312/11/3/555/ 2023-08-20T04:08:48+02:00 Interactions between Surface Waves, Tides, and Storm-Induced Currents over Shelf Waters of the Northwest Atlantic Shangfei Lin Jinyu Sheng agris 2023-03-06 application/pdf https://doi.org/10.3390/jmse11030555 EN eng Multidisciplinary Digital Publishing Institute Physical Oceanography https://dx.doi.org/10.3390/jmse11030555 https://creativecommons.org/licenses/by/4.0/ Journal of Marine Science and Engineering; Volume 11; Issue 3; Pages: 555 wave–current interactions tidal current storm-induced current near-inertial oscillation wave-indued forces wave-enhanced mixing wave-enhanced bottom stress Text 2023 ftmdpi https://doi.org/10.3390/jmse11030555 2023-08-01T09:07:42Z A coupled wave–tide–circulation model is used to investigate wave–current interactions (WCIs) over the shelf waters of the Northwest Atlantic (NWA) during Hurricane Earl (2010). WCIs have substantial impacts on hydrodynamics in the upper ocean. The significant wave heights are modulated by WCIs, particularly over regions with strong current gradients, with a reduction up to ~2.1 m (20%) during the storm. Noticeable decreases in surface elevations and tidal currents occur in regions with strong tides such as the Gulf of Maine, mainly due to the wave-enhanced bottom stress. Over regions with weak tidal currents, wave effects on currents are dominated by two competitive processes between wave-induced forces and wave-enhanced mixing. The former strengthens surface currents (up to ~0.55 m/s) and increases the peak storm surge (up to ~0.48 m). The latter is responsible for the reduction in storm-induced surface currents (up to ~0.94 m/s) and anticyclonic modulation of current directions. Vertically, WCIs extend the strong vertical current shear and shift it downward during the storm, which enhances the local mixing and changes the structures of near-inertial oscillations (NIOs). Moreover, tidal currents also change the magnitudes of the NIOs and subtidal currents and affect the intensity of WCIs. Text Northwest Atlantic MDPI Open Access Publishing Journal of Marine Science and Engineering 11 3 555 |
institution |
Open Polar |
collection |
MDPI Open Access Publishing |
op_collection_id |
ftmdpi |
language |
English |
topic |
wave–current interactions tidal current storm-induced current near-inertial oscillation wave-indued forces wave-enhanced mixing wave-enhanced bottom stress |
spellingShingle |
wave–current interactions tidal current storm-induced current near-inertial oscillation wave-indued forces wave-enhanced mixing wave-enhanced bottom stress Shangfei Lin Jinyu Sheng Interactions between Surface Waves, Tides, and Storm-Induced Currents over Shelf Waters of the Northwest Atlantic |
topic_facet |
wave–current interactions tidal current storm-induced current near-inertial oscillation wave-indued forces wave-enhanced mixing wave-enhanced bottom stress |
description |
A coupled wave–tide–circulation model is used to investigate wave–current interactions (WCIs) over the shelf waters of the Northwest Atlantic (NWA) during Hurricane Earl (2010). WCIs have substantial impacts on hydrodynamics in the upper ocean. The significant wave heights are modulated by WCIs, particularly over regions with strong current gradients, with a reduction up to ~2.1 m (20%) during the storm. Noticeable decreases in surface elevations and tidal currents occur in regions with strong tides such as the Gulf of Maine, mainly due to the wave-enhanced bottom stress. Over regions with weak tidal currents, wave effects on currents are dominated by two competitive processes between wave-induced forces and wave-enhanced mixing. The former strengthens surface currents (up to ~0.55 m/s) and increases the peak storm surge (up to ~0.48 m). The latter is responsible for the reduction in storm-induced surface currents (up to ~0.94 m/s) and anticyclonic modulation of current directions. Vertically, WCIs extend the strong vertical current shear and shift it downward during the storm, which enhances the local mixing and changes the structures of near-inertial oscillations (NIOs). Moreover, tidal currents also change the magnitudes of the NIOs and subtidal currents and affect the intensity of WCIs. |
format |
Text |
author |
Shangfei Lin Jinyu Sheng |
author_facet |
Shangfei Lin Jinyu Sheng |
author_sort |
Shangfei Lin |
title |
Interactions between Surface Waves, Tides, and Storm-Induced Currents over Shelf Waters of the Northwest Atlantic |
title_short |
Interactions between Surface Waves, Tides, and Storm-Induced Currents over Shelf Waters of the Northwest Atlantic |
title_full |
Interactions between Surface Waves, Tides, and Storm-Induced Currents over Shelf Waters of the Northwest Atlantic |
title_fullStr |
Interactions between Surface Waves, Tides, and Storm-Induced Currents over Shelf Waters of the Northwest Atlantic |
title_full_unstemmed |
Interactions between Surface Waves, Tides, and Storm-Induced Currents over Shelf Waters of the Northwest Atlantic |
title_sort |
interactions between surface waves, tides, and storm-induced currents over shelf waters of the northwest atlantic |
publisher |
Multidisciplinary Digital Publishing Institute |
publishDate |
2023 |
url |
https://doi.org/10.3390/jmse11030555 |
op_coverage |
agris |
genre |
Northwest Atlantic |
genre_facet |
Northwest Atlantic |
op_source |
Journal of Marine Science and Engineering; Volume 11; Issue 3; Pages: 555 |
op_relation |
Physical Oceanography https://dx.doi.org/10.3390/jmse11030555 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.3390/jmse11030555 |
container_title |
Journal of Marine Science and Engineering |
container_volume |
11 |
container_issue |
3 |
container_start_page |
555 |
_version_ |
1774721297863933952 |