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Sea level anomalies affect the ocean circulation at abyssal depths
Abyssal channels are the key points controlling bottom circulation of the World Ocean. They provide meridional transport of the coldest Antarctic Bottom Water between deep-water basins influencing the meridional overturning circulation and the climate on a global scale. Here we show that the synopti...
Autores principales: | , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2023
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10682481/ https://www.ncbi.nlm.nih.gov/pubmed/38012378 http://dx.doi.org/10.1038/s41598-023-48074-9 |
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author | Frey, D. I. Morozov, E. G. Smirnova, D. A. |
author_facet | Frey, D. I. Morozov, E. G. Smirnova, D. A. |
author_sort | Frey, D. I. |
collection | PubMed |
description | Abyssal channels are the key points controlling bottom circulation of the World Ocean. They provide meridional transport of the coldest Antarctic Bottom Water between deep-water basins influencing the meridional overturning circulation and the climate on a global scale. Here we show that the synoptic variability of deep-water flows including blocking abyssal currents between deep ocean basins is related to sea level anomalies observed over the channels. Our results demonstrate that processes at the ocean surface have a more significant connection with the bottom circulation than it was considered earlier. This study opens a discussion of the importance of mesoscale eddies and air-sea interactions on water exchange between abyssal basins, meridional heat transport in the ocean, and possible responses of the ocean to the observed sea level rise in a changing climate. |
format | Online Article Text |
id | pubmed-10682481 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2023 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-106824812023-11-30 Sea level anomalies affect the ocean circulation at abyssal depths Frey, D. I. Morozov, E. G. Smirnova, D. A. Sci Rep Article Abyssal channels are the key points controlling bottom circulation of the World Ocean. They provide meridional transport of the coldest Antarctic Bottom Water between deep-water basins influencing the meridional overturning circulation and the climate on a global scale. Here we show that the synoptic variability of deep-water flows including blocking abyssal currents between deep ocean basins is related to sea level anomalies observed over the channels. Our results demonstrate that processes at the ocean surface have a more significant connection with the bottom circulation than it was considered earlier. This study opens a discussion of the importance of mesoscale eddies and air-sea interactions on water exchange between abyssal basins, meridional heat transport in the ocean, and possible responses of the ocean to the observed sea level rise in a changing climate. Nature Publishing Group UK 2023-11-27 /pmc/articles/PMC10682481/ /pubmed/38012378 http://dx.doi.org/10.1038/s41598-023-48074-9 Text en © The Author(s) 2023 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . |
spellingShingle | Article Frey, D. I. Morozov, E. G. Smirnova, D. A. Sea level anomalies affect the ocean circulation at abyssal depths |
title | Sea level anomalies affect the ocean circulation at abyssal depths |
title_full | Sea level anomalies affect the ocean circulation at abyssal depths |
title_fullStr | Sea level anomalies affect the ocean circulation at abyssal depths |
title_full_unstemmed | Sea level anomalies affect the ocean circulation at abyssal depths |
title_short | Sea level anomalies affect the ocean circulation at abyssal depths |
title_sort | sea level anomalies affect the ocean circulation at abyssal depths |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10682481/ https://www.ncbi.nlm.nih.gov/pubmed/38012378 http://dx.doi.org/10.1038/s41598-023-48074-9 |
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