Meridional heat transport variability induced by mesoscale processes in the subpolar North Atlantic

© The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Nature Communications 9 (2018): 1124, doi:10.1038/s41467-018-03134-x. The ocean’s role in global climate change largely depends on its heat transpor...

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Published in:Nature Communications
Main Authors: Zhao, Jian, Bower, Amy S., Yang, Jiayan, Lin, Xiaopei
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2018
Subjects:
Online Access:https://hdl.handle.net/1912/10125
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spelling ftwhoas:oai:darchive.mblwhoilibrary.org:1912/10125 2023-05-15T17:28:35+02:00 Meridional heat transport variability induced by mesoscale processes in the subpolar North Atlantic Zhao, Jian Bower, Amy S. Yang, Jiayan Lin, Xiaopei 2018-03-19 https://hdl.handle.net/1912/10125 en_US eng Nature Publishing Group https://hdl.handle.net/1912/10416 https://doi.org/10.1038/s41467-018-03134-x Nature Communications 9 (2018): 1124 https://hdl.handle.net/1912/10125 doi:10.1038/s41467-018-03134-x Attribution 4.0 International http://creativecommons.org/licenses/by/4.0/ CC-BY Nature Communications 9 (2018): 1124 doi:10.1038/s41467-018-03134-x Article 2018 ftwhoas https://doi.org/10.1038/s41467-018-03134-x 2022-05-28T23:00:19Z © The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Nature Communications 9 (2018): 1124, doi:10.1038/s41467-018-03134-x. The ocean’s role in global climate change largely depends on its heat transport. Therefore, understanding the oceanic meridional heat transport (MHT) variability is a fundamental issue. Prevailing observational and modeling evidence suggests that MHT variability is primarily determined by the large-scale ocean circulation. Here, using new in situ observations in the eastern subpolar North Atlantic Ocean and an eddy-resolving numerical model, we show that energetic mesoscale eddies with horizontal scales of about 10–100 km profoundly modulate MHT variability on time scales from intra-seasonal to interannual. Our results reveal that the velocity changes due to mesoscale processes produce substantial variability for the MHT regionally (within sub-basins) and the subpolar North Atlantic as a whole. The findings have important implications for understanding the mechanisms for poleward heat transport variability in the subpolar North Atlantic Ocean, a key region for heat and carbon sequestration, ice–ocean interaction, and biological productivity. J.Z. was financially supported by the Postdoctoral Scholar Program at WHOI, with funding provided by the Ocean and Climate Change Institute. This work was also supported by the US National Science Foundation (OCE-1258823 and OCE-1634886), as well as by China’s national key research and development projects (2016YFA0601803), the National Natural Science Foundation of China (41521091 and U1606402), the Qingdao National Laboratory for Marine Science and Technology (2015ASKJ01), and the Fundamental Research Funds for the Central Universities (201424001 and 201362048). Article in Journal/Newspaper North Atlantic Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Nature Communications 9 1
institution Open Polar
collection Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server)
op_collection_id ftwhoas
language English
description © The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Nature Communications 9 (2018): 1124, doi:10.1038/s41467-018-03134-x. The ocean’s role in global climate change largely depends on its heat transport. Therefore, understanding the oceanic meridional heat transport (MHT) variability is a fundamental issue. Prevailing observational and modeling evidence suggests that MHT variability is primarily determined by the large-scale ocean circulation. Here, using new in situ observations in the eastern subpolar North Atlantic Ocean and an eddy-resolving numerical model, we show that energetic mesoscale eddies with horizontal scales of about 10–100 km profoundly modulate MHT variability on time scales from intra-seasonal to interannual. Our results reveal that the velocity changes due to mesoscale processes produce substantial variability for the MHT regionally (within sub-basins) and the subpolar North Atlantic as a whole. The findings have important implications for understanding the mechanisms for poleward heat transport variability in the subpolar North Atlantic Ocean, a key region for heat and carbon sequestration, ice–ocean interaction, and biological productivity. J.Z. was financially supported by the Postdoctoral Scholar Program at WHOI, with funding provided by the Ocean and Climate Change Institute. This work was also supported by the US National Science Foundation (OCE-1258823 and OCE-1634886), as well as by China’s national key research and development projects (2016YFA0601803), the National Natural Science Foundation of China (41521091 and U1606402), the Qingdao National Laboratory for Marine Science and Technology (2015ASKJ01), and the Fundamental Research Funds for the Central Universities (201424001 and 201362048).
format Article in Journal/Newspaper
author Zhao, Jian
Bower, Amy S.
Yang, Jiayan
Lin, Xiaopei
spellingShingle Zhao, Jian
Bower, Amy S.
Yang, Jiayan
Lin, Xiaopei
Meridional heat transport variability induced by mesoscale processes in the subpolar North Atlantic
author_facet Zhao, Jian
Bower, Amy S.
Yang, Jiayan
Lin, Xiaopei
author_sort Zhao, Jian
title Meridional heat transport variability induced by mesoscale processes in the subpolar North Atlantic
title_short Meridional heat transport variability induced by mesoscale processes in the subpolar North Atlantic
title_full Meridional heat transport variability induced by mesoscale processes in the subpolar North Atlantic
title_fullStr Meridional heat transport variability induced by mesoscale processes in the subpolar North Atlantic
title_full_unstemmed Meridional heat transport variability induced by mesoscale processes in the subpolar North Atlantic
title_sort meridional heat transport variability induced by mesoscale processes in the subpolar north atlantic
publisher Nature Publishing Group
publishDate 2018
url https://hdl.handle.net/1912/10125
genre North Atlantic
genre_facet North Atlantic
op_source Nature Communications 9 (2018): 1124
doi:10.1038/s41467-018-03134-x
op_relation https://hdl.handle.net/1912/10416
https://doi.org/10.1038/s41467-018-03134-x
Nature Communications 9 (2018): 1124
https://hdl.handle.net/1912/10125
doi:10.1038/s41467-018-03134-x
op_rights Attribution 4.0 International
http://creativecommons.org/licenses/by/4.0/
op_rightsnorm CC-BY
op_doi https://doi.org/10.1038/s41467-018-03134-x
container_title Nature Communications
container_volume 9
container_issue 1
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