Internal Wave Dynamics Over Isolated Seamount and Its Influence on Coral Larvae Dispersion

The internal wave dynamics over Rosemary Bank Seamount (RBS), North Atlantic, were investigated using the Massachusetts Institute of Technology general circulation model. The model was forced by M2-tidal body force. The model results are validated against the in-situ data collected during the 136th...

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Published in:Frontiers in Marine Science
Main Authors: Stashchuk, Nataliya, Vlasenko, Vasiliy
Other Authors: Natural Environment Research Council
Format: Article in Journal/Newspaper
Language:unknown
Published: Frontiers Media SA 2021
Subjects:
Online Access:http://dx.doi.org/10.3389/fmars.2021.735358
https://www.frontiersin.org/articles/10.3389/fmars.2021.735358/full
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spelling crfrontiers:10.3389/fmars.2021.735358 2024-02-11T10:06:33+01:00 Internal Wave Dynamics Over Isolated Seamount and Its Influence on Coral Larvae Dispersion Stashchuk, Nataliya Vlasenko, Vasiliy Natural Environment Research Council 2021 http://dx.doi.org/10.3389/fmars.2021.735358 https://www.frontiersin.org/articles/10.3389/fmars.2021.735358/full unknown Frontiers Media SA https://creativecommons.org/licenses/by/4.0/ Frontiers in Marine Science volume 8 ISSN 2296-7745 Ocean Engineering Water Science and Technology Aquatic Science Global and Planetary Change Oceanography journal-article 2021 crfrontiers https://doi.org/10.3389/fmars.2021.735358 2024-01-26T09:57:37Z The internal wave dynamics over Rosemary Bank Seamount (RBS), North Atlantic, were investigated using the Massachusetts Institute of Technology general circulation model. The model was forced by M2-tidal body force. The model results are validated against the in-situ data collected during the 136th cruise of the RRS “James Cook” in June 2016. The observations and the modeling experiments have shown two-wave processes developed independently in the subsurface and bottom layers. Being super-critical topography for the semi-diurnal internal tides, RBS does not reveal any evidence of tidal beams. It was found that below 800-m depth, the tidal flow generates bottom trapped sub-inertial internal waves propagated around RBS. The tidal flow interacting with a cluster of volcanic origin tall bottom cones generates short-scale internal waves located in 100 m thick seasonal pycnocline. A weakly stratified layer separates the internal waves generated in two waveguides. Parameters of short-scale sub-surface internal waves are sensitive to the season stratification. It is unlikely they can be observed in the winter season from November to March when seasonal pycnocline is not formed. The deep-water coral larvae dispersion is mainly controlled by bottom trapped tidally generated internal waves in the winter season. A Lagrangian-type passive particle tracking model is used to reproduce the transport of generic deep-sea water invertebrate species. Article in Journal/Newspaper North Atlantic Frontiers (Publisher) Rosemary Bank ENVELOPE(-10.250,-10.250,59.200,59.200) Frontiers in Marine Science 8
institution Open Polar
collection Frontiers (Publisher)
op_collection_id crfrontiers
language unknown
topic Ocean Engineering
Water Science and Technology
Aquatic Science
Global and Planetary Change
Oceanography
spellingShingle Ocean Engineering
Water Science and Technology
Aquatic Science
Global and Planetary Change
Oceanography
Stashchuk, Nataliya
Vlasenko, Vasiliy
Internal Wave Dynamics Over Isolated Seamount and Its Influence on Coral Larvae Dispersion
topic_facet Ocean Engineering
Water Science and Technology
Aquatic Science
Global and Planetary Change
Oceanography
description The internal wave dynamics over Rosemary Bank Seamount (RBS), North Atlantic, were investigated using the Massachusetts Institute of Technology general circulation model. The model was forced by M2-tidal body force. The model results are validated against the in-situ data collected during the 136th cruise of the RRS “James Cook” in June 2016. The observations and the modeling experiments have shown two-wave processes developed independently in the subsurface and bottom layers. Being super-critical topography for the semi-diurnal internal tides, RBS does not reveal any evidence of tidal beams. It was found that below 800-m depth, the tidal flow generates bottom trapped sub-inertial internal waves propagated around RBS. The tidal flow interacting with a cluster of volcanic origin tall bottom cones generates short-scale internal waves located in 100 m thick seasonal pycnocline. A weakly stratified layer separates the internal waves generated in two waveguides. Parameters of short-scale sub-surface internal waves are sensitive to the season stratification. It is unlikely they can be observed in the winter season from November to March when seasonal pycnocline is not formed. The deep-water coral larvae dispersion is mainly controlled by bottom trapped tidally generated internal waves in the winter season. A Lagrangian-type passive particle tracking model is used to reproduce the transport of generic deep-sea water invertebrate species.
author2 Natural Environment Research Council
format Article in Journal/Newspaper
author Stashchuk, Nataliya
Vlasenko, Vasiliy
author_facet Stashchuk, Nataliya
Vlasenko, Vasiliy
author_sort Stashchuk, Nataliya
title Internal Wave Dynamics Over Isolated Seamount and Its Influence on Coral Larvae Dispersion
title_short Internal Wave Dynamics Over Isolated Seamount and Its Influence on Coral Larvae Dispersion
title_full Internal Wave Dynamics Over Isolated Seamount and Its Influence on Coral Larvae Dispersion
title_fullStr Internal Wave Dynamics Over Isolated Seamount and Its Influence on Coral Larvae Dispersion
title_full_unstemmed Internal Wave Dynamics Over Isolated Seamount and Its Influence on Coral Larvae Dispersion
title_sort internal wave dynamics over isolated seamount and its influence on coral larvae dispersion
publisher Frontiers Media SA
publishDate 2021
url http://dx.doi.org/10.3389/fmars.2021.735358
https://www.frontiersin.org/articles/10.3389/fmars.2021.735358/full
long_lat ENVELOPE(-10.250,-10.250,59.200,59.200)
geographic Rosemary Bank
geographic_facet Rosemary Bank
genre North Atlantic
genre_facet North Atlantic
op_source Frontiers in Marine Science
volume 8
ISSN 2296-7745
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3389/fmars.2021.735358
container_title Frontiers in Marine Science
container_volume 8
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