Oceanic eddies induce a rapid formation of an internal wave continuum
Abstract Oceanic internal waves are a major driver for turbulent mixing in the ocean, which controls the global overturning circulation and the oceanic heat and carbon transport. Internal waves are observed to have a continuous energy distribution across all wave frequencies and scales, commonly kno...
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Online Access: | https://doi.org/10.1038/s43247-023-01137-1 https://doaj.org/article/e3c419981fd1459890b917168caf8803 |
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ftdoajarticles:oai:doaj.org/article:e3c419981fd1459890b917168caf8803 2024-01-21T10:08:35+01:00 Oceanic eddies induce a rapid formation of an internal wave continuum Luwei Yang Roy Barkan Kaushik Srinivasan James C. McWilliams Callum J. Shakespeare Angus H. Gibson 2023-12-01T00:00:00Z https://doi.org/10.1038/s43247-023-01137-1 https://doaj.org/article/e3c419981fd1459890b917168caf8803 EN eng Nature Portfolio https://doi.org/10.1038/s43247-023-01137-1 https://doaj.org/toc/2662-4435 doi:10.1038/s43247-023-01137-1 2662-4435 https://doaj.org/article/e3c419981fd1459890b917168caf8803 Communications Earth & Environment, Vol 4, Iss 1, Pp 1-10 (2023) Geology QE1-996.5 Environmental sciences GE1-350 article 2023 ftdoajarticles https://doi.org/10.1038/s43247-023-01137-1 2023-12-24T01:47:05Z Abstract Oceanic internal waves are a major driver for turbulent mixing in the ocean, which controls the global overturning circulation and the oceanic heat and carbon transport. Internal waves are observed to have a continuous energy distribution across all wave frequencies and scales, commonly known as the internal wave continuum, despite being forced at near-inertial and tidal frequencies at large scales. This internal wave continuum is widely thought to be developed primarily through wave-wave interactions. Here we show, using realistic numerical simulations in the subpolar North Atlantic, that oceanic eddies rapidly distribute large-scale wind-forced near-inertial wave energy across spatio-temporal scales, thereby forming an internal wave continuum within three weeks. As a result, wave energy dissipation patterns are controlled by eddies and are substantially enhanced below the mixed layer. The efficiency of this process potentially explains why a phase lag between high-frequency and near-inertial wave energy was observed in eddy-poor regions but not in eddy-rich regions. Our findings highlight the importance of eddies in forming an internal wave continuum and in controlling upper ocean mixing patterns. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Communications Earth & Environment 4 1 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
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English |
topic |
Geology QE1-996.5 Environmental sciences GE1-350 |
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Geology QE1-996.5 Environmental sciences GE1-350 Luwei Yang Roy Barkan Kaushik Srinivasan James C. McWilliams Callum J. Shakespeare Angus H. Gibson Oceanic eddies induce a rapid formation of an internal wave continuum |
topic_facet |
Geology QE1-996.5 Environmental sciences GE1-350 |
description |
Abstract Oceanic internal waves are a major driver for turbulent mixing in the ocean, which controls the global overturning circulation and the oceanic heat and carbon transport. Internal waves are observed to have a continuous energy distribution across all wave frequencies and scales, commonly known as the internal wave continuum, despite being forced at near-inertial and tidal frequencies at large scales. This internal wave continuum is widely thought to be developed primarily through wave-wave interactions. Here we show, using realistic numerical simulations in the subpolar North Atlantic, that oceanic eddies rapidly distribute large-scale wind-forced near-inertial wave energy across spatio-temporal scales, thereby forming an internal wave continuum within three weeks. As a result, wave energy dissipation patterns are controlled by eddies and are substantially enhanced below the mixed layer. The efficiency of this process potentially explains why a phase lag between high-frequency and near-inertial wave energy was observed in eddy-poor regions but not in eddy-rich regions. Our findings highlight the importance of eddies in forming an internal wave continuum and in controlling upper ocean mixing patterns. |
format |
Article in Journal/Newspaper |
author |
Luwei Yang Roy Barkan Kaushik Srinivasan James C. McWilliams Callum J. Shakespeare Angus H. Gibson |
author_facet |
Luwei Yang Roy Barkan Kaushik Srinivasan James C. McWilliams Callum J. Shakespeare Angus H. Gibson |
author_sort |
Luwei Yang |
title |
Oceanic eddies induce a rapid formation of an internal wave continuum |
title_short |
Oceanic eddies induce a rapid formation of an internal wave continuum |
title_full |
Oceanic eddies induce a rapid formation of an internal wave continuum |
title_fullStr |
Oceanic eddies induce a rapid formation of an internal wave continuum |
title_full_unstemmed |
Oceanic eddies induce a rapid formation of an internal wave continuum |
title_sort |
oceanic eddies induce a rapid formation of an internal wave continuum |
publisher |
Nature Portfolio |
publishDate |
2023 |
url |
https://doi.org/10.1038/s43247-023-01137-1 https://doaj.org/article/e3c419981fd1459890b917168caf8803 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Communications Earth & Environment, Vol 4, Iss 1, Pp 1-10 (2023) |
op_relation |
https://doi.org/10.1038/s43247-023-01137-1 https://doaj.org/toc/2662-4435 doi:10.1038/s43247-023-01137-1 2662-4435 https://doaj.org/article/e3c419981fd1459890b917168caf8803 |
op_doi |
https://doi.org/10.1038/s43247-023-01137-1 |
container_title |
Communications Earth & Environment |
container_volume |
4 |
container_issue |
1 |
_version_ |
1788699347004686336 |