Low ocean-floor rises regulate subpolar sea surface temperature by forming baroclinic jets
Sea surface temperature (SST) fronts in mid- to high-latitude oceans have significant impacts on extratropical atmospheric circulations and climate. In the western subarctic Pacific, sharp SST fronts form between the cold subarctic water and the recently found quasi-stationary jets that advect warm...
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ftpubmed:oai:pubmedcentral.nih.gov:5864925 2023-05-15T18:27:59+02:00 Low ocean-floor rises regulate subpolar sea surface temperature by forming baroclinic jets Mitsudera, H. Miyama, T. Nishigaki, H. Nakanowatari, T. Nishikawa, H. Nakamura, T. Wagawa, T. Furue, R. Fujii, Y. Ito, S. 2018-03-22 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5864925/ http://www.ncbi.nlm.nih.gov/pubmed/29568009 https://doi.org/10.1038/s41467-018-03526-z en eng Nature Publishing Group UK http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5864925/ http://www.ncbi.nlm.nih.gov/pubmed/29568009 http://dx.doi.org/10.1038/s41467-018-03526-z © The Author(s) 2018 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 license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license 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 license, visit http://creativecommons.org/licenses/by/4.0/. CC-BY Article Text 2018 ftpubmed https://doi.org/10.1038/s41467-018-03526-z 2018-04-01T00:20:51Z Sea surface temperature (SST) fronts in mid- to high-latitude oceans have significant impacts on extratropical atmospheric circulations and climate. In the western subarctic Pacific, sharp SST fronts form between the cold subarctic water and the recently found quasi-stationary jets that advect warm waters originating in the Kuroshio northeastward. Here we present a new mechanism of the jet formation paying attention to the propagation of baroclinic Rossby waves that is deflected by eddy-driven barotropic flows over bottom rises, although their height is low (~500 m) compared with the depth of the North Pacific Ocean (~6000 m). Steered by the barotropic flows, Rossby waves bring a thicker upper layer from the subtropical gyre and a thinner upper layer from the subarctic gyre, thereby creating a thickness jump, hence a surface jet, where they converge. This study reveals an overlooked role of low-rise bottom topography in regulating SST anomalies in subpolar oceans. Text Subarctic PubMed Central (PMC) Pacific Nature Communications 9 1 |
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Article Mitsudera, H. Miyama, T. Nishigaki, H. Nakanowatari, T. Nishikawa, H. Nakamura, T. Wagawa, T. Furue, R. Fujii, Y. Ito, S. Low ocean-floor rises regulate subpolar sea surface temperature by forming baroclinic jets |
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Sea surface temperature (SST) fronts in mid- to high-latitude oceans have significant impacts on extratropical atmospheric circulations and climate. In the western subarctic Pacific, sharp SST fronts form between the cold subarctic water and the recently found quasi-stationary jets that advect warm waters originating in the Kuroshio northeastward. Here we present a new mechanism of the jet formation paying attention to the propagation of baroclinic Rossby waves that is deflected by eddy-driven barotropic flows over bottom rises, although their height is low (~500 m) compared with the depth of the North Pacific Ocean (~6000 m). Steered by the barotropic flows, Rossby waves bring a thicker upper layer from the subtropical gyre and a thinner upper layer from the subarctic gyre, thereby creating a thickness jump, hence a surface jet, where they converge. This study reveals an overlooked role of low-rise bottom topography in regulating SST anomalies in subpolar oceans. |
format |
Text |
author |
Mitsudera, H. Miyama, T. Nishigaki, H. Nakanowatari, T. Nishikawa, H. Nakamura, T. Wagawa, T. Furue, R. Fujii, Y. Ito, S. |
author_facet |
Mitsudera, H. Miyama, T. Nishigaki, H. Nakanowatari, T. Nishikawa, H. Nakamura, T. Wagawa, T. Furue, R. Fujii, Y. Ito, S. |
author_sort |
Mitsudera, H. |
title |
Low ocean-floor rises regulate subpolar sea surface temperature by forming baroclinic jets |
title_short |
Low ocean-floor rises regulate subpolar sea surface temperature by forming baroclinic jets |
title_full |
Low ocean-floor rises regulate subpolar sea surface temperature by forming baroclinic jets |
title_fullStr |
Low ocean-floor rises regulate subpolar sea surface temperature by forming baroclinic jets |
title_full_unstemmed |
Low ocean-floor rises regulate subpolar sea surface temperature by forming baroclinic jets |
title_sort |
low ocean-floor rises regulate subpolar sea surface temperature by forming baroclinic jets |
publisher |
Nature Publishing Group UK |
publishDate |
2018 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5864925/ http://www.ncbi.nlm.nih.gov/pubmed/29568009 https://doi.org/10.1038/s41467-018-03526-z |
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Pacific |
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Pacific |
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Subarctic |
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Subarctic |
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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5864925/ http://www.ncbi.nlm.nih.gov/pubmed/29568009 http://dx.doi.org/10.1038/s41467-018-03526-z |
op_rights |
© The Author(s) 2018 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 license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license 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 license, visit http://creativecommons.org/licenses/by/4.0/. |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/s41467-018-03526-z |
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Nature Communications |
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9 |
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1 |
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1766210268576088064 |