Deep water pathways in the North Pacific Ocean revealed by Lagrangian particle tracking

Lagrangian particle tracking experiments are conducted to investigate the pathways of deep water in the North Pacific Ocean. The flow field is taken from a state-of-the-art deep circulation simulation. An unprecedented number of particles are tracked to quantify the volume transport and residence ti...

Full description

Bibliographic Details
Published in:Scientific Reports
Main Authors: Kawasaki, T., Matsumura, Y., Hasumi, H.
Format: Text
Language:English
Published: Nature Publishing Group UK 2022
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9033868/
http://www.ncbi.nlm.nih.gov/pubmed/35459917
https://doi.org/10.1038/s41598-022-10080-8
id ftpubmed:oai:pubmedcentral.nih.gov:9033868
record_format openpolar
spelling ftpubmed:oai:pubmedcentral.nih.gov:9033868 2023-05-15T15:04:19+02:00 Deep water pathways in the North Pacific Ocean revealed by Lagrangian particle tracking Kawasaki, T. Matsumura, Y. Hasumi, H. 2022-04-22 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9033868/ http://www.ncbi.nlm.nih.gov/pubmed/35459917 https://doi.org/10.1038/s41598-022-10080-8 en eng Nature Publishing Group UK http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9033868/ http://www.ncbi.nlm.nih.gov/pubmed/35459917 http://dx.doi.org/10.1038/s41598-022-10080-8 © The Author(s) 2022 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/) . CC-BY Sci Rep Article Text 2022 ftpubmed https://doi.org/10.1038/s41598-022-10080-8 2022-05-01T00:37:57Z Lagrangian particle tracking experiments are conducted to investigate the pathways of deep water in the North Pacific Ocean. The flow field is taken from a state-of-the-art deep circulation simulation. An unprecedented number of particles are tracked to quantify the volume transport and residence time. Half of the North Pacific deep water returns to the Southern Ocean, and its principal pathway is along the western boundary current in the Southwest Pacific Basin in the deep layer. About 30% is exported to the Indian Ocean after upwelling to the shallow layer in the western North Pacific Ocean. The rest is transported to the Arctic Ocean through the Bering Strait or evaporates within the Pacific Ocean. Upwelling of deep water is confined in the western North Pacific Ocean owing to the strong vertical mixing. The mean residence time of deep water in the North Pacific Ocean is estimated to be several hundred years, which is consistent with the observed radiocarbon distribution. Text Arctic Arctic Ocean Bering Strait Southern Ocean PubMed Central (PMC) Arctic Arctic Ocean Bering Strait Indian Pacific Southern Ocean Scientific Reports 12 1
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Article
spellingShingle Article
Kawasaki, T.
Matsumura, Y.
Hasumi, H.
Deep water pathways in the North Pacific Ocean revealed by Lagrangian particle tracking
topic_facet Article
description Lagrangian particle tracking experiments are conducted to investigate the pathways of deep water in the North Pacific Ocean. The flow field is taken from a state-of-the-art deep circulation simulation. An unprecedented number of particles are tracked to quantify the volume transport and residence time. Half of the North Pacific deep water returns to the Southern Ocean, and its principal pathway is along the western boundary current in the Southwest Pacific Basin in the deep layer. About 30% is exported to the Indian Ocean after upwelling to the shallow layer in the western North Pacific Ocean. The rest is transported to the Arctic Ocean through the Bering Strait or evaporates within the Pacific Ocean. Upwelling of deep water is confined in the western North Pacific Ocean owing to the strong vertical mixing. The mean residence time of deep water in the North Pacific Ocean is estimated to be several hundred years, which is consistent with the observed radiocarbon distribution.
format Text
author Kawasaki, T.
Matsumura, Y.
Hasumi, H.
author_facet Kawasaki, T.
Matsumura, Y.
Hasumi, H.
author_sort Kawasaki, T.
title Deep water pathways in the North Pacific Ocean revealed by Lagrangian particle tracking
title_short Deep water pathways in the North Pacific Ocean revealed by Lagrangian particle tracking
title_full Deep water pathways in the North Pacific Ocean revealed by Lagrangian particle tracking
title_fullStr Deep water pathways in the North Pacific Ocean revealed by Lagrangian particle tracking
title_full_unstemmed Deep water pathways in the North Pacific Ocean revealed by Lagrangian particle tracking
title_sort deep water pathways in the north pacific ocean revealed by lagrangian particle tracking
publisher Nature Publishing Group UK
publishDate 2022
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9033868/
http://www.ncbi.nlm.nih.gov/pubmed/35459917
https://doi.org/10.1038/s41598-022-10080-8
geographic Arctic
Arctic Ocean
Bering Strait
Indian
Pacific
Southern Ocean
geographic_facet Arctic
Arctic Ocean
Bering Strait
Indian
Pacific
Southern Ocean
genre Arctic
Arctic Ocean
Bering Strait
Southern Ocean
genre_facet Arctic
Arctic Ocean
Bering Strait
Southern Ocean
op_source Sci Rep
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9033868/
http://www.ncbi.nlm.nih.gov/pubmed/35459917
http://dx.doi.org/10.1038/s41598-022-10080-8
op_rights © The Author(s) 2022
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/) .
op_rightsnorm CC-BY
op_doi https://doi.org/10.1038/s41598-022-10080-8
container_title Scientific Reports
container_volume 12
container_issue 1
_version_ 1766336114155585536